SUNY ¥ AA, Y ‘ See A f 3 Ng i? Cha Nw yay CONUS ray ro, of PU WR nical ay i Kae UM ab ed ian X: vy 1 AN i By Bue hat mil iat evn a bayianha sh) Wh th AY oa = A at SR Aa 7 a ‘i Ny A i ea x in Vali ¥ i a) Fay th fA th WN, ‘i uae ae ip Ra Bidet ce ana ‘th j ? i vv) ala Ha ) Natty x tai wae MEN Ny te abana iy oh Gly bas i 8 APA WA uh sjonane . y , ee i ae . A pase inh ies pi ua . . hy an ui % WA - nh aes soni oe me a AN hahy on as at HH AY i ae ieee ah ae uty in Sas shi atti : wis SiN a) ona a Ge FI r Bean hh aes - mae a ‘i a9 sai Rast? x a HI 3 2 i HIE Be eee sah Rie } PSR i an ‘s Dy ey i4 3 i} att eats ( shu mt aye "4 the ih) met oe Casas “+4 Wg 7 SF Rola 5 at op 9 Fite, ase Eee ri aN ye, TRANSACTIONS w7Ww63 OF THE WISCONSIN ACADEMY OF SCIENCES, ARTS, AND LETTERS. Vor. II. 1875—76. Published by Authority of Law. MADISON, Wis.: E. B. BOLENS, STATE PRINTER. 1876. CONTENTS. TITLES OF PAPERS PUBLISHED IN THIS VOLUME DEPARTMENT OF THE NATURAL SCIENCES. oO fF ww 13. 14. . Kaolin in Wisconsin. By Roland Irving, A. M. E.M.......... . Oconomowoc and other Small Lakes of Wisconsin. By I.A.Lapham . Fish Culture. By P. R. Hoy, M. D.....-... eee eee eee eee eee . Notes on the Geology of Northern Wisconsin. By E. T. Sweet, M.S . The rapid disappearance of Wisconsin Wild-flowers. By Thure IRM 6 peo dou oes sooo Osseo Une Od oDOUUO DUONOUOS UP conOoG . The Ancient Civilization of America. By W. J. L. Nicodemus, _ Extent of the Wisconsin Fisheries. By P. R. Hoy, M. D.....- ° . Leveling with the Barometer. By John Nader, C. E........--. . On Kerosene Oil. By E. T. Sweet, M.S. ....---eeeee eee eee . The Improvement of the Mouth of the Mississippi River. By John Nader, C. H..... 0. ccc ee cece eee e reece eres eee eee _ The Catocale of Racine County. By P. R. Hoy, M. 2... . Copper-tools found in the State of Wisconsin. By J. D. But- ise, 1U)Up IDs So apnb ode nsoooddeuC bonus ne OUUD OO Qn 0006. nUGb. Report of Committee on Exploration of Indian Mounds in the Vi- cinity of Madison. ..... 02.2: eee eee e tenes cere ee eee e eens TA. Wapham, LE. Di 2.5.2 wees eee es eee eet weno DEPARTMENT OF LETTERS. 1. Studies in Comparative Grammar. By J. B. Feuling, Ph. D... DEPARTMENT OF THE SociaAL AND PoLiTicaAL SCIENCES. 1. United States’ Sovereignty: whence derived and when vested. By Prof. W. F. Allen... 22... 0.2252 esten sere seeceerserecee _ The Formal Commendation of Government Officials. By J. W. ww eo lon j=} Qu. i= n or 4 foe iS) =i leo) a oa ie) i) = ee [o} 5 ise] g ee) ra) = ie] a i jo} —_ = i=) B Qs eveecrcpeveperece ‘a a _ (42) rd @ fo} uo} oe (a) bs} j=} a + =a oO 28) 5 =D il ° r=) Q ea ise) ) 8) (4?) a Q Q r) <4 oO 5 l=} 9 Embryonic Development the same in Plants as in Animals. By 37-39 40-55 56-57 58-64 65-67 68-76 7-83 84-95 96-98 99-104 105-109 110-113 117-121 125-132 133-135 136-142 143-150 4 CONTENTS. - Page. 5. The Boa-Constrictor of Politics. By Rev. F. M. Holland...... 151-160 6. The Revolutionary Movement among Women. By J. W. Hoyt, INE SAD icc oie othco: Slo'sccle ts Daveraree-o'e wlaielgy oie eis ates ave le cae eee eer 161-176 DEPARTMENT OF SPECULATIVE PHILOSOPHY. 1. Were the Stoics Utilitarians? By Rev. F. M. Holland..,...... 179-195 2. An Examination of Prof. 8. H. Carpenter’s Theory of Evolution. By Herbert 22 Hubbel, Wanonali. « < «0. lent teeter 196-202 MATHEMATICAL AND PHYSICAL PAPERS. - 1 Recent Progress in: Theoretical Physics. By John E. Davies, J \ap i he Ue ae nOneE ERT coRAGod cock soo wodonds 205-221 PROCEEDINGS OF THE ACADEMY. IReportion the) President. << <1 <1.) 21 =\\s elimieltel tei ete ee 225-229 Report of the Secretary =) eletalsieecielereist steers 231-232 Sixth Regular Annual Meeting..... dw wie bs lia aps ah) CORSE een 233-237 Report of the Librarian....... Weuedpododaeo coosoc ¢ nddooo bor 238-239 © istiof, Officersiand: Members... (1)... «+ « wl. « sislereisfesvoeneletere areas 241-248 CHARTER, CONSTITUTION AND By-Laws. peg Hartenstein -l-)-1-1-1- Jar aer'a ugyes aie 18 017 Blache OCR ICR Ne aeeeaeae 251-252 Wonstitution sey sicseites choses doen asd So's vie dueleie ls Soo ere Ae oe ee 253-255 BY STAWSo oer oe 15.0, 015. die ee ni ele elaleialca.s 0+ sole Srei ete Se ene eee 255-256 IREPORT OF ‘THE COUNCID: «6.0 ois :..cjcteisidieinc © sieehe eee ae eee 257 Prof.) Peter Englemann. | {By 1: R--belands-)----ere eee eee eee 258-263 Tnerease A. Lapham, bh... .By P:R. Hoy.- steric eee 264-267 Inerease A. Lapham, LL. D. By E.R. Leland...........-..+-- 268-269 GENERAL OFFICERS § ACADEMY. PRESIDENT: Dr. P. R. HOY, Racine. VICE-PRESIDENTS: Dr. S. H. CARPENTER, - - - - - Madison. Pror. T. C. CHAMBERLIN. - - - - - Beloit. Rey. G. M. STEELE, D. D. - - - - - Appleton. Hon. J. I. CASE, - - - - - - - Racine. Rey. A. L. CHAPIN, D. D. - - - - - Beloit. Dre. W.. HOYT, - - - - - - Madison GENERAL SECRETARY: Pror. J. KE. DAVIES, M. D., University of Wisconsin. _ TREASURER: GEO. P. DELAPLAINE, Esq., Madison. DIRECTOR OF THE MUSEUM: K. T. SWEET, Esq., Sun Prairie. LIBRARIAN: CHARLES N. GREGORY, Madison. COUNSELORS EX-OFFICIO: HIS EXCELLENCY THE GOVERNOR OF THE STATE. THE LIEUTENANT GOVERNOR. THE SUPERINTENDENT OF PUBLIC INSTRUCTION. THE PRESIDENT OF THE STATE UNIVERSITY. THE PRESIDENT OF THE STATE AGRICULTURAL SOCIETY. THE SECRETARY OF THE STATE AGRICULTURAL SOCIETY. OFFICERSOF THE DEPARTM ENS Department of Speculative Philosophy. President Hx-Oficio—THE PRESIDENT OF THE ACADEMY. Vice-President.—_S. H. CARPENTER, LL. D., State University. Secretary. REV. F. M. HOLLAND, Baraboo. Counselors —PRESIDENT BASCOM, State University, PROF. O. AREY, Whitewater, and REV. A. O. WRIGHT, Fez Lake. Department of the Natural Sciences. President Ex-Oficio.—THE PRESIDENT OF THE ACADEMY. Vice-President. PROF. T. C. CHAMBERLIN, Beloit. Secretary. PROF. J. H. EATON, Beloit. Counselors—PROF. W. W. DANIELLS, State University, PROF. J. C. FOYE, Appleton, and PROF. THURE KUMLEIN, Albion College. Department of the Social and Political Sciences. President Ex-Officio THE PRESIDENT OF THE ACADEMY. Vice-President—_REV. G. M. STEELE, Appleton. Secretary.—K. R. LELAND, Haw Claire. Counselors.—DR. E. B. WOLCOTT, Milwaukee, REV. CHARLES CAVENRO, Lombard, Ili., and PROF. J. B. PARKINSON, Madison. Department of the Mechanic Arts President Lx-Oficico THE PRESIDENT OF THE ACADEMY. Vice-President —J. 1. CASE, Racine. Secretary — PROF. W J. lL. NICODEMUS, State University. Counselors CHAS. H. HASKINS, Milwaukee, HON. J. L. MITCHELL, Mil- waukee, and CAPT. JOHN NADER, Madison. Department of Letters. President Ex-Oficio THE PRESIDENT OF THE ACADEMY. Vice-President. REV. A. L. CHAPIN, D. D., Beloit. Secretary.— PROF. J. B. FEULING, State University. Counselors—PROF. W. F: ALLEN, Madisun, PROF. EMERSON, Beloit, and HON. L. C. DRAPER, Madison. Department of the Fine Arts. President Ex-Oficio THE PRESIDENT OF THE ACADEMY. Vice-President —DR. J. W. HOYT, Madison. Secretary.— HON. J. EK. THOMAS, Sheboygan. Counselore—J. R. STUART, MRS. S. F. DEAN, and MRS. H. M. LEWIS, Hadison. = syr en, = c oOo Cr DEPARTMENT OF UREN INGLE AL iSelences. TITLES OF PAPERS READ BEFORE THIS DEPARTMENT. . Kaolin in Wisconsin. By Rotanp Irvine, A. M., E. M. . Oconomowoc and Other Small Lakes of Wisconsin. By I. A. LAPHAM. . Fish-culture. By P. R. Hoy, M. D. . Notes on the Geology of Northern Wisconsin. By E. T. SwEeEt, M. S. . On the Rapid Disappearance of Wisconsin Wild-flowers; a Contrast of the Pres- ent Time with Thirty Years Ago. By Toure KUMLEIN. . On the Ancient Civilization of America. By W.J.L. Nicoprmus, A. M.,C. E. . Extent of Wisconsin Fisheries. By P. R. Hoy, M. D. | . Leveling with the Barometer. By Jonn Naver, C. E. . On Kerosene Oil. . By E. T. Sweet, M. S. . Improvement of the Mouth of the Mississippi River. By Jomn NAveEr, C. E. . On the Catocale of Racine County. By P. R. Hoy, M. D. . Copper-tools found in the State of Wisconsin. By Prof. J. D. Burien, LL. D. . Report of Committee on Exploration of Indian Mounds in Vicinity of Madison. Department of Natural Sciences. ON KAOLIN IN WISCONSIN. BY ROLAND IRVING, A. M., E. M. Professor of Geology, ete., in the State University. I.—NATURE, ORIGIN, AND OCCURRENCE OF KAOLIN. : Origin of the word “ kaolin.’—The word kaolin is a corruption of the Chinese kao-ling* or kau-ling,’ meaning “ high-ridge,” the name of a place near Jauchau Fu, in China, where for many centu- ries the Chinese have obtained the material for the manufacture of their famous porcelain. According to Von Richthofen,{ however, the Chinese material is not the same as that to which the term kaolin is applied in Europe and America, but is on the contrary a solid rock, which is exported in a pulverized condition under the name of kao-ling. The application of this name to the European porcelain-clay by Berzelius, was, according to Von Richthofen, made on the erroneous supposition that the white powder which he re- ceived from China occurred naturally in that state. _ What is kaolin?—However this may be, since Berzelius, the word has been applied in Hurope to a white clay-like substance which, from its peculiar composition and freedom from any ingredients tending to lessen the whiteness of the wares burnt from it, or its refractoriness to heat, is especially adapted to form the base of the finer kinds of pottery known as porcelain, whence its name of * Baron Von Richthofen, American Journal Science, ‘‘ On the Porcelain Rocks of China,’ III i 179. Comp. also Percy’s Metallurgy, volume on Fuels, p. 92. 7Dana’s “‘ System of Mineralogy,’’ p. 75—S. W. Williams’ ‘‘ Middle Kingdom,” WO, LOT oe iG. t Loe: cit. = WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. “ yorcelain-clay.”” An exact statement of the geological and chem- ical application of the term is not so easily given. Geologists have commonly designated as kaolins only those clays resulting directly from the disintegration of felspar-bearing rocks in place, as distin- guished from the bedded orsedimentary clays. It is true that most all of the kaolins used for porcelain making are obtained from de- posits of the former nature, but it is equally true that beds, or patches in beds, of sedimentary clays have the same composition and properties as the ordinary kaolins. It has long been noticed that clays possessing these properties tend to approach a type com- position, and that they are frequently separable by a process of ley- igation into a fine white scaly clay, and a sand composed of parti- cles of quartz and undecomposed felspar. The white clay thus sep- arable has always a definite composition, and, as shown by Messrs. Johnson and Blake,* is seen under the microscope to consist of translucent or transparent, rhomboidal or hexagonal plates, which are flexible and inelastic, isolated or aggregated in prismatic, curved, or fan-shaped bundles, and referable to the orthorhombic system. The bases of these scales are marked with lines arismg from the edges of super-imposed laminae. The hardness varies from that of tale to about midway between that of selenite and calcite. The mineral whose existence is thus rendered certain, has been designated as kaolinite by these gentlemen, from the kaolin in which it is most commonly found. ‘These crystalline scales are however found to occur, not only in the real kaolins, which they chiefly make up, but also in small quantities in many ordi- nary sedimentary fire-clays, or even in common brick-clays. In these, however, they appear to be associated with other silicates of alumina, or at least with an excess of silica over the amount necessary to form kaolinite, which cannot be proved to exist in the free state. The ordinary clays cannot therefore as yet be re- garded as having a base of kaolinite. The composition of kaolin- ite, Messrs. Johnson and Blake showed to be as follows: a P. cent MSU GaS reer tetera rete acer eter aise ar Mae ou cocadee cee eet toe ogee 25 46.3 GAL tara TAS eevee Wis eed hatchs, btohe oie. le dees aga eds. RACER 0 ee ane a aL ae ad 39.8 VV ST eer co 2ll, covey see Et ee etiece le 13.9 100.0 *“ On Kaoliniteand Pholerite.’”” Am. Jour. Sci. IT. xliii. p. 391 et seq, as quot- ed in Percy, p. 92 volume on Fuels ete. KAOLIN IN WISCONSIN. 5 These figures correspond to the formula Alz Os, 2 Si Oz + 2 He O, one deduced by Forchhammer for kaolin as long ago as 1830, from a comparison of a series of analyses of crude and washed articles. We may then designate as kaolin any native hydrated silicate of alumina having the above percentage composition, or any native material composed of a mixture of such a silicate with quartz fragments, and fragments of undecomposed rock. Some of the raw kaolins are almost pure kaolinite, whilst others contain as much as fifty to sixty per cent. of foreign matter. Origin of Kaolinite—The mineral kaolinite, when considered as the base of large clay masses, appears always to have resulted from the decomposition of minerals of the felspar group. In very small quantities, it is true, the same substance is known to be an altera- tion product of other minerals than the felspars, e.g. beryl, stauro- lite, leucite; still all of the large kaolinite masses have originated by the alteration of some of the felspars. This alteration may have been caused by several agents, by far the most important of which has, however, been carbonated water, or water carrying carbonic acid in solution. ‘The felspars are silicates of alumina with an al- kaline ingredient, which may be either potash, soda, or lime. Ob- taining carbonic acid from the atmosphere, and to some slight ex- tent from direct organic decay, the surface waters, thus reinforced, infiltrating through the seams of the felspar-bearing rocks, (gran- ite, gneiss, porphyry,) act gradually upon the alkaline silicates, forming first carbonate of lime, if lime be present in the rock, which dissolving as bicarbonate in the carbonated water, is carried away. Moreslowly are taken up and leeched out the alkalies as car- bonates, or as silicates, if the amount of carbonic acid is only small, which will be the more usual case. Part of the silica thus set free always remains as colloid or hydrated silica, and may be detected in samples by its solubility in alkali. The amount of colloid sil- icay remaining will depend directly on the supply of carbonic acid, being greater as the carbonic acid is more plenty. Still remaining after the leeching process are now certain proportions of alumina and silica, to which is added a certain proportion of water. These three combining and crystallizing, form the hydrated silicate of al- umina, kaolinite. The theoretical change from orthoclase felspar * Dana’s Mineralogy—under orthoclase, p. 361. , 7 Bischof Chem. Geol. Vol. II, p. 183. 6 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. to kaolinite is well shown by the following figures, which are per- centages by weight, calculated on the original orthoclase: { : Fe ET | Constituents. Orthoclase.} Removed.| Remain. | Added. | Kaolinite. OUIVCAlRr ue ees Aeros e 64.6 43.1 QED) Oy Pha ee 21.5 Ylhohaan ee) asc ao Soe mec Theses ail feaeheey enc aie bese 9 Mee (eR Eeok ches 18.5 PR Otashimemee tet eines cess 16.9 1 ee ee MIE ocdllia cana daosot AVG Pe Ty eect oscce: I Sioenul naeterercte ac AIM ic He ic Pree a ae 7.4 eee Total enlace 100.0 60 40 7.4 AT 4 The last column corresponds to the composition already given for kaolinite, viz., silica, 43.3; alumina, 39.8; water, 13.9. The change may also be conveniently indicated from the formulae as follows: Orthoclase = ~ = = = 6K,0+6A1,0,7-86510, Removed - - = - - - 6K,0+ i 24510, Mer ns ees he May OME 6A1,0,+128i0, Which corresponds to PON gee fy hi A],0,2810, Added - - - = = = 2H,0 Resulting Kaolinite - = = = Al,0,,2510,+-2H 0 These calculations are made on the assumption that the alumina is not removed. It appears however in some cases to be partially removed.* The soluble substances resulting from this decomposi- tion, the carbonates and silicates of potash and soda, and the bi- carbonate of lime, pass off with the infiltrating waters, and reach- ing the surface again, give rise to mineral springs, or add to the solid contents of the drainage waters of the region. The felspar may alter so as to produce certain zeolites when all of the protoxyd bases are not removed,+ and if the infiltrating waters carry mag- nesia in traces a steatitic change may result. These are however much rarer changes, and do not affect the object of the present paper. Should the felspathic rock be contaminated with iron pyrites; its decay may be much hastened.{ This may be in part due to a direct action upon the silicate by the acid waters resulting from * Dana, loc. cit. 7 Bischof. Chem. Geol., p. 211—Dana, loc. cit. { Dana’s Mineralogy, p. 360. Geology of New Jersey, p. 68. KAOLIN IN WISCONSIN. ie oxydation of the sulphid, but is rather due chiefly to the disintegra- tion of the rock produced by this oxydation, which leaves it more easily permeable to the carbonated waters. The felspars which appear especially to have given rise to kao- lin masses are orthoclase and albite, the potash and soda felspars. This must be attributed rather to their greater abundance as com- pared with oligoclase and andesite—the soda-lime felspars—since these latter change much more easily to kaolin, whilst orthoclase changes with the least readiness of any of the felspars, being found often unaltered, when oligoclase occurring in the same rock is com- pletely kaolinized.* Labradorite does not commonly alter to ka- olinite.t . Origin of clay deposits in general.—All clays and indeed most shales (clay shales) may be said to have resulted primarily from the alteration more or less completely carried out, of the felspar of felspar bearing rocks. The disintegrated material resultmg from this alteration may either have remained where formed, still occu- pying the position and retaining the lamination of the original unchanged rock, or may have been subsequently removed by the ordinary eroding forces and deposited elsewhere as a bedded clay. This removal, if merely for a short distance, may have been unac- companied by any assorting of the clay and rocky materials; as for instance is obseryed in the “kaolin” of the Cretaceous beds of eastern New Jersey. Such an assorting appears however most commonly to have taken place, the clay having been washed out from the quartz and undecomposed rock fragments accompanying it, having had more or less of foreign material mingled with it during the process of sedimentation, and having thus resulted in a bed of ordinary clay. Again in other cases the action of eroding forces on the unaltered felspathic rocks may have resulted in a sed- iment of powdered felspathic material which by subsequent altera- tion has become a clay. In some one of these ways all true clays would seem to haye been formed. Fragments ‘of felspar still re- maining in many of them, and the alkaline ingredients shown by analyses, testifiy to this general origin. Of course bedded clays may have been again and again removed and redeposited, mingled with various impurities, or introduced as impurity into other’ sedi- em aS A align eae EE At eT I A * Dana, p. 348. 7 Dana, p, 361. 8 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. ments—e. g. limestone—by whose subsequent solution and removal the clay may be left alone and pure. Whatever the exact origin, we may then group all clays conven- iently into the bedded clays, and the clays accurring as disintegrated rocks in place. In both of these ways kaolin occurs. A brief con- sideration of each mode of occurrence will be of interest in the present connection. Kaolin as a disintegrated rock in place-—Most kaolin of com- merce comes from this kind of a deposit. Gneissic and other felspathic rocks, frequently placed with their bedding planes verti- cal, admit of deep penetration by the surface carbonated waters. Their felspathic ingredient being thus decomposed, the whole rock is converted into a soft admixture of kaolinite, quartz fragments, particles of partly decomposed, and entirely undecomposed felspar, and more or less altered particles of mica. This alteration has been noticed to as great a depth as seventy feet and over. The eneissic rocks of the Blue Ridge in Virginia, North Carolina, and Georgia, are found altered to this depth over considerable areas, re- taining still their original lamination and highly inclined position.* Similar changes and to much greater depth are reported from Bra- zil.t In such cases the once quartz veins are often seen occupying their original position as great sheets in the soft clay. Should now the felspar be a largely predominating constituent of the rock, or should the mica be present in inconsiderable quan- tities only, there will result on decomposition a mixture of a very pure white kaolinite with more or less quartz sand and undecom- posed felspar fragments, which can readily be removed by leviga- tion, and a valuable article obtained. Should, on the other hand, the mica be largely present, or should there be any quantity of hornblende or pyrite in the rock, the resulting clay will be largely contaminated with non-separable alkalies from the mica, or oxyd of iron fromthe mica, hornblende or pyrite, and will be a mere red brick-clay of no value. Thus it happens that whilst many locali- ties of disintegrating granite are known, but few of them yield good kaolin. In the case of much pyrite or other ferruginous con- stituent in the rock, the weathering and leeching by the carbon- ated waters, may result in the formation of deposits of the hydrat- ed sesquioxyd of iron, in the shape of “ bog iron ore.” Such Dr. * Am. Jour. Sci. III. vii p. 60. 7 Hartt as quoted by Hunt, Loe. cit. KAOLIN IN WISCONSIN. 9 T. 8. Hunt* regards as having been the origin of some of the bog- ore deposits in the vicinity of the disintegrating gneissic rocks of the Southern States. I allude to this here since it is a fact that bog-ores of considerable value occurs in the Wisconsin kaolin dis- trict and may be supposed to have had a similar origin. In as much as the decomposition of the felspar in such a process is hardly ever so completely carried out as to leave none of it un- altered, it results that the kaolins used in the arts show either in their crude or washed state almost always a certain amount of al- kali on analysis. This alkali may be present partly as entirely un- decomposed felspar fragments, in which state it can be completely removed by levigation, and partly as felspar in different degrees of change. All of the latter cannot be separated. Many of the best kaolins aspear to have resulted from the decom- position of a rock consisting chiefly of felspar with as small admix- ture of quartz and no mica, known as peginatite.y These, from their great richness in felspar, tend to produced an especially pure kao- lin. The ordinary gneisses and granites on the other hand, by their decay yield a very coarse sandy clay, which may be quite impure from foreign admixtures, or if free from any hurtful impurity, so largely mingled with quartz, as to be very lean in pure kaolinite. In some regions it is noticed that those granitic or gneissic layers more largely composed of felspar than the adjoining beds, tend to alter whilst the rest stand firm. Since these alternating beds are al- ways inclined at high angles, their outcropping edges strike across the country in groups of narrow parallel bands. Thus it comes that kaolin is sometimes found following long straight lines, hav- ing aconstant bearing. This fact may be made use of in “ prospect- ing” for kaolin. Examples of the occurrence of kaolinized rock.—Most of the authorities that I have been able to consult agree in describing the Chinese kaolin. used many centuries before porcelain-making was introduced into Europe, as a result of the disintegration of a grani- toid rock, though I have not seen any detailed account. A recent paper{ by Baron Von Richthroten, as already said, gives a different account of the nature of the Chinese article. He says: “I visited * * * * the famous King-te-chin, where the Chinese have made nearly all their porcelain for almost three thousand years. I * Loe. cit. + Von Cotta’s Lithology p. 206, English Ed. { Am. Jour. Sci., cit. 10 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. examined the places from which they take the material. * * * T have to record the unexpected fact that the material from which the porcelain of King-te-chin is made, is taken from certain strata intercalated between these slates, and occurring at several places, separated ‘from each other laterally, 1. e., at right angles; with the strike of the rocks. It is a rock of the hardness of felspar (inferior kinds are not so hard) and of a green color, which gives 1b to some extent, the appearence of jade to which the Chinese too, compare it. The rock is reduced by stamping to a white powder, of which the finest portion is ingeniously and repeatedly separated. ‘This is then moulded into small bricks. The Chinese distinguish chiefly two kinds of this material. Hither of them is sold in King-te-chin in the shape of bricks, and as either is a white earth, they offer no visible differences. ‘They are made in different places by pounding hard rock, but the aspect of the rock is alike in both cases. For one of these two kinds of material, the place “ Kaoling ” was in an- cient times in high repute, * * * * and the Chinese still designate by the name “ kaoling” the kind of earth which was for- merly derived fromthere. * “* * * The second kind of material bears the name pe-tun-tse, (‘‘ white clay.”) 5S. W Will- iams, in his “ Middle Kingdom,” speaks* of the kaolin as a dis- integrated granite, which is almost all felspar—and of the “ pe- tun-tse "as nearly pure quartz—but his account does not appear to be based on personal inspection. One of the most famous kaolin localities of Europe is that at St. Yrieix-la-perche, near Limoges, in France. Here is obtained the material for the famous Sevres porcelain manufactory.+ The kaolin occurs as a result of the disintegration of masses of pegmatite partly interstratified with the gneiss and partly intersecting it in cross veins. ‘The gneiss is also decomposed, but to a red clayey mass of no value. The pegmatite, consisting chiefly of felspar, wherever decomposed has given rise to an excellent kaolin, moder- ately free from quartz and rocky particles, these forming only about ten per cent. of the whole. Another famous Huropean occurrence of kaolin is that of the vicinity of St. Austlein Cornwall. This is a weathered mixture of orthoclase and quartz, chiefly on Tregoning hill near Helstone,{ in eh Mop Goes } Dana’s Mineralogy, p.475; Knapp’s ‘Chemis’y Applied to Arts,” vol. fi, p. 230. { Wagner's Chem. Technol, Eng. Ed. Sia, »P KAOLIN IN WISCONSIN. al various stages of decomposition. The kaolinite portion is removed from the weathered rock by allowing streams of water to run over it. The clay thus washed out settles in a series of large catch-pools. The weathered rock itself is used to a considerable extent in the ceramic arts in England, under the name of Cornish stone. At Aue in Saxony the source of the kaolin was a rounded mass of granite very much decomposed on the surface and surrounded by the kaolin as by a cap.* The deposit is exhausted. At Mionia im Saxony, the kaolin is decomposed porphyry, and is used in the Dresden inanufactories.- At the Hinigheit mine near Freiberg, Saxony, it is in nests in gneiss.[ The kaolin of La Bresse, France, is an altered andesite.|| That of Bayonne, France, is a graphic granite in every stage of decomposition.4{ At Passau the occur- rence is exactly like that of St. Yrieix in France.§ The following are analyses of crude European kaolins:** Place. eck | Silica. | Alumina.| Water. Shin: NCIGISTDS, OSC RCRA Ia Es REN Cet 9.7 41.9 34.6 1G) Cormac cela iie ose ese ereiaviels 19.6 46.5 24.0 Say ID CHO MBNC Sig BORGO UMA OS abe ons 4.3 44,1 26.8 19,7 YNDVE Ss det oes I ONTO ORES AE RIES AA 18.0 385.9 34.1 11.0 RAGSAUIEN Ve ree eee a ete 4.5 46.4 BY AA) 12.8 Mort near Hralle............ ba eae 43.8 26.0 Op) 15) Tab A few occurrences of kaolinized rock are known in the United States, of such a nature as to supply a good article. An excellent material is found in the graphic granite of Brunswick, Maine, and also at Haddam, Connecticut. At each place the rock is a coarse mixture of very pure quartz and felspar. At the latter locality it has been of late mined and broken up for making kaolin for white ware at Williamsburg, N. Y.tr Near Trenton in New Jersey the gneissic rocks are more felspathic than usual in the region, and the felspar is entirely changed to kaolin, which is dug to be used in making fire-brick.j{ This clay contains zirconia. Kaolin as a bedded clay.—As x bedded clay kaolin is known in * Knapp, vol. I, p. 230. { Knapp, Loe. cit. + Wagner Chem. Technol, p. 230. ? Dana’s Mineralogy, p. 348. t Percy’s Metallurgy, Vol. on Fuels, p. 96. ** Wagner, Loc. cit. } || Ure’s Dictionary, Vol. 1, p. 427. ++ Appleton’s Encyclopedia, Art. Clay. tt Geology of New Jersey, p. 323. 12 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. two occurrences: (1) as a coarse admixture of felspar, kaolinite ete. removed but a short distance from where it resulted by disintegra- tion; and (2) as a fine-grained clay washed from its coarse material, and not directly traceable to its origin. In New Jersey the great thicknesses of plastic clays, forming the lowest member of the Cre- taceous series, stretch in a wide band south westward across the state from Staten Island Sound to the Delaware River. In places these clays come into contact with the gneisses of the Archaean belt crossing the state from northeast to southwest, and have eyi- dently derived their material from the wear of the previously dis- integrated gneissic rocks. In these clay beds kaolin-like clays oc- cur both in the assorted and unassorted conditions. The coarse or unassorted kaolin * is dug at several places on both the main land and island sides of Staten Island Sound. The bed is from two to twelve feet thick, and is composed of coarse angular fragments of quartz mingled with decomposed felspar and mica scales. It is interstratified with other clay and sand layers, and lignite. The finer New Jersey clays of the same series are largely used for mak- ing fire-brick and the rougher kinds of pottery. Some of them ap- pear to be sufficiently pure for the manufacture of porcelain. Or- dinary stoneware, porcelain knobs ete. are extensively manufac™ tured at Trenton.t The purity of these bedded clays as compared with most others would appear to be directly due to their deriva- tion from the disintegration of the eneissic rocks of the region, and deposition near by where first formed. A recent discovery in Indiana has brought to light what appears to be a valuable bedded clay, occurring under peculiar circum- stances. The kaolin bed lies at the base of the coal measure con- elomerate, in Lawrence county, Indiana, having a thickness of five to six feet, one of which is pure white kaolin, the remainder being more or less stained with iron and manganese oxides. Immediate- ly beneath the clay is a bed of Jimonite iron ore. This clay appears to replace a bed of limestone which has been dissolved away by the action of carbonated waters. It has almost exactly the com- position of kaolinite. With it are found lumps of the mineral allophane, another hydrated silicate of alumina, with a larger per- centage of water than kaolinite. * Geology of New Jersey p. 249. _ +t Geology of New Jersey loc. cit. t Geology of New Jersey p. 685. KAOLIN IN WISCONSIN. if ey) A similar occurrence to the one just described is mentioned by Jukes* as existing in the tilted bottom-beds of the Carboniferous Limestone, on Cork Harbor, Ireland. Here, over a small area, the limestone has been almost entirely removed, leaving the clay-like substance behind. This clay has been used considerably in the Eng- lish potteries. The following are analyses of those of the Indiana and New Jersey bedded clays, which approach to kaolinite in com- position: Constituents. I. Mt. II. IV. Sle appraiser evr sicosi yates faites cusverous erate alee 43.2 45.30 45.90 47.05 Alumina........ 5 Cone DOMODOUDSdSaOs0000 39.71 37.10 40.34 37.14 \WEMIGE on So pO Cae AOC EORTC aera 14.25 1SR40F | 135260 labo Otel erotm Wan Sameser tral asaya acini stereo sco jelllece sree heel ysieeigeraieveillnoe are e 0s 0.03 DESUMORV OP OPMMITOME sie < ce wicie a wees ee tele 0.74 Hae alaniae Heal eae I2GIEREIN. Sone 4 docs BODO OCR eee ees 37 U1 Op tWaccvesson t-te Daley eevege MPETGNO. 5 6) odO0b OS EOS OO Oe eo Mone barat al lun sia Bee On PBR Nobnlon ood U TUTTO! sol go OCOD COD CCI CRE ae (erie eee ORL eee { 0.08 PREC OMI 5 ccs.0ie =): APT r eee esi ekeusk oral ate vousvave for oi tus 1.40 MAO lies exctets: sosyliotstatebeyas MO taller sak Mavscere the wisies eevee susieve tlecaie 99.67 100.19 99.50 99.80 I. is a fine white clay from Burts Creek, near South Amboy, New Jersey, analysed just as it came from the pit. II. is a kaolin-like clay analyzed after washing to free from particles of quartz, mica, and feldspar. It is from Trenton, New Jersey. III. and IV. are the Lawrence county, Indiana, kaolin, analyzed without washing. II.—KAOLIN IN WISCONSIN. Geographical position of the kaolin district—The fact of the exis- tence of kaolin in Wisconsin has been known for many years. The material has however only very recently attracted much atten- tion and become the object of actual exploitation. The first pub- lished mention I find of it is in the report of Dr. J. G. Norwood in Owen’s Geological Survey of Minesota, lowa, and Wisconsin.t He says, in describing the last Archaean exposure seen in descending the Wisconsin River: “ Above the granite at the old mill-dam,f{ is a bed of ferruginous argillite four feet thick, succeeded by five feet of decomposed felspar, above which is a bed two feet thick of well di- gested kaolin, or porcelain clay, with * * * ™* quartz dissemi- nated through it in veins and containing a notable quantity of *Jukes and Geikie’s Manual of Geology, p. 130. ire eels ¢ Near Point Bass, Wood county. 14 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. pyrites. Then succeeds a variegated white and yellow sand-stone * * * * 77 Th this account Dr. Norwood conveys the erroneous impression that the kaolin of the Wisconsin occurs as a bedded clay, which it does not do. The various localities at which kaolin has been noticed in the state, so far-as my knowledge extends, all occur in a belt of country about fifty miles in length and fifteen in breadth, stretching eastward from Black river in Jackson county to the Wisconsin, in the vicin- ity of the city of Grand Rapids, in Wood county. This district in- cludes more or less of townships 21, 22, and 23 north, and ranges 1, 2, 3,4 west, and 1, 2,3, 4, 5, 6, 7 east,“of the meridian. It is crossed from north to south by three streams of considerable size; Black River on the west, the Wisconsin on the east, and Yellow River towards the centre. The kaolin discoveries have, I believe been made almost entirely in the vicinity of these streams. Geology of the kaolin district—The district thus described, lies for most of its extent just south of the main boundary-line between the Potsdam sandstone, which underlies so large an area to the south, east, and west, and the Archaean rocks, which form the sub-structure of all the region to the northward. In places the boundary, which is a very irregular one, lies within this district. The country in this part of the state is generally level, with a gradual rise to the northward. In the more southern portion of the belt, the sandstone is nearly everywhere the surface rock, ex- cept along the beds of the rivers, where the strata of Archaean gneiss granite and diorite are laid bare. The sandstone is therefore, where it occurs, only a very thin covering over the crystalline rocks, and indeed these occasionally rise through it in bold isolated bluffs of eranite and quartzite, which, though sometimes as much as two hundred feet in height, cover but a small area. Interspersed with these are other bluffs of similar height and dimensions, of horizon- tal sandstone, bearing witness to the great thickness of that rock which has suffered denudation. Further north, the gradual rise of the country seems to be due in some measure to the shape of the surface of the underlying Archaean rocks, which finally rise from beneath the sandstone and become the surface formation. The boundary between the two terranes is traced with great difficulty. Barometrical elevations are no guide at all. for the sandstone hay- ing once covered the region so deeply may be found at the very KAOLIN IN WISCONSIN. 15 highest levels, whilst the irregular upper surface of the gneissic rocks is apt to bring them up through the sandstone at any place. A geological map, including Portage, Wood, Clark, and Jackson counties, would show on the south the sandstone as the surface formation, on the north the crystalline rocks, whilst where the two meet they would be shown dovetailing into each other, the Archaean extending many miles south in the stream beds, the sand- stone penetrating as far north on the divides. As we trace the rivers southward towards where the last crystalline rocks are seen, these are found confining themselves more and more closely to the vicinity of the streams until they are finally restricted to their beds, the sandstone forming the banks. Thus the Wisconsin River, for ten miles above Point Bass, and the Black for a greater distance above the falls, present strips of crystalline rocks only as wide as their own currents. Another feature in the geology of the kaolin district seems worthy of notice in the present connection. I refer to the fact that the boundary line between the ‘“‘driftless”” area of the south west- ern quarter of the State, and the “ drift-bearing ” area to the north and east, crosses the district in a nearly east and west line from Grand Rapids to Black River Station, on Black river. Nature and mode of occurrence of the Wisconsin kaolin.—The Wisconsin kaolin occurs entirely as ‘“ kaolinized” rock. As al- ready stated it has been noticed only in the vicinity of the large streams. This is so because elsewhere the crystalline rocks are for the most part covered by the sandstone. Nearly always it occupies exactly the original position, retaining sometimes even the minute structure, of the unaltered rock. A few cases were noticed im- mediately on the river banks, where the structure of the clay seemed to have been modified slightly by water action. The rocks from which the kaolin has been formed, and into which it can fre- quently be traced throush every degree of alteration, are beds inter- stratified with the series of Archean strata which have over wide areas a common strike. Only the out-cropping edges of these beds are decomposed, and as a consequence it follows that the resulting kaolin forms narrow bands crossing the country in straight lines parallel to the general strike. It is exceedingly common to find overlying the kaolin a few layers of sandstone, sometimes a few inches only, at others, a score or so of feet. In such cases the 16 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. purer kaolin is found immediately below the sandstone, next be- low a partially kaolinized rock, and next below again the entirely unaltered rock. Such sections are common in the district. The kaolin localities appear to be almost entirely within the drift- less area, or at least where the drift is very thin and the glacial action has been insignificant, This fact becomes a significant one, when we consider that over all the great Archaean region of the north half of the state, which is drift covered, no occurrence of kaolin is known; all the known occurrences being confined to that comparatively small district where the Archaean rocks are found within the driftless area. I am inclined to attribute this absence of kaolinized rock in the northern portion of the state to the de- nuding agency of the drift forces, following Dr. T. 5. Hunt, who has made the same suggestion™ in explanation of the non-disinte- grated condition of the gneissic rocks of the Blue Ridge in the northern Atlantic States, the same rocks further south being con- stantly found decomposed to considerable depths. Where and how to search for kaolin in Wisconsin.—If it be a fact that the drift forces have removed all kaolinized rock they have encoun- tered, then at once we may conclude that search at any considera- ble distance north of the drift limit is not lkely to be rewarded with success. An exception to this might be where the kaolin has been formed underneath protecting masses of sandstone. Within the thus restricted district, moreover, the labor of the search may be much lessened by the recognition of a few simple guiding facts. The ex- plorer should visit the known outcrops of kaolin, note the rock from which it has decomposed, measure carefully its strike and then follow the line thus obtained until other patches are found. Having once noted the kind of rock tending to produce the kaolin, (in this region usually a pinkish felspathic gneiss or granite,) by following the strike of any similar bed kaolin will probably sooner or later be found. The search would be best made with a boring- tool of some simple kind. Should sandstone be struck in the bor- ing the kaolin may yet underlie it. The explorer should at the outset divest himself of the idea that the kaolin occurs in a continuous horizontal bed. Kaolin on the Wisconsin River.—The best known kaolin deposits in Wisconsin are those that occur on and near the Wisconsin Riy- * Loe. cit. KAOLIN IN WISCONSIN. IY( er, in the vicinity of the city of Grand Rapids, in Wood county. The Archaean gneissic rocks here occur chiefly in the bed of the stream, which for many miles makes bold rapids over their upturned edges. Elsewhere they are mostly covered with sandstone. The predominating gneissic rocks have associated with them both inter- bedded, and clearly intrusive granite and diorite. Of the gneiss and granite there are many varieties, according to the predominance of one or other mineral ingredient, both rocks being formed sometimes of a largely predominating pinkish felspar. These beds are the ones most commonly weathered, though some of the dark micaceous kinds show the same tendency. All of the beds strike between N. 50° E. and N. 80° K. with a dip of about 50° ei- ther 8. E. or N. W. On the southwest quarter of section 5, town 22, range 6 east, on the land of Mr. Garrison, considerable digging has been done in borrowing for the road-bed of the railroad near by. The removal of about two feet of earth has exposed the kaolin in a number of places extending along the railroad for some rods. The clay is here in some places quite white, in others much stained with iron sesquixoyd, the stained portions being those nearest the surface. Much of it appears to have lost all sign of the original rock structure, whilst in many places the spade turned up masses as distinctly laminated as any of the gneiss in the vicinity. All of the kaolin here is quite gritty from the presence of quartz and undecomposed felspar fragments, a statement which will apply to all of the Wisconsin kaolins that have come under my notice. Scales of silvery mica appear to be largely present. Aver- age samples of the whiter clay, selected by the writer, yielded Mr. Sweet, of the State Geological Survey, by whom all the analyses of Wisconsin kaolins quoted in this paper were made, the following results: 2——W AS 18 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Constituents. : J. UL, II. STUTKCR YS BiG od dea Gee OR ECICRDT Ete ETO nee cic ot Orci COloNa.ad.3.c 78.83 | 49.94 92.86 GAVIA EL Penne See DE Rate sc) cn cata Bp, seve revanetete Aa rated eReete retetehetione 13.43 | 36.80 2.08 Sesquiomy@ lof Tron... 2.0.0 ens «ines wie isle mmielalels 0.74 mle 74 A hisa(sveie tere SEER CMRP eae atric St Roin a picket Cit dis ecuintraoce 0.64] trace .96 WEIN as Sage PosaseonEses bor sooocdobdsoeagonan OsO i eies5 oc 5 10 (POtASHRR ees eich viele Sit eee Ree ole eee AGI 51 .28 GO awe ee cneatis, lashes SRO ae Eee aes ac .07 .08 .05 GarbontevAcids:2 fel Saget ee Re eee 201 |. scaler Water tise oc kaa BUS See eee eer ee 5.45 | 11.62 2.53 EO tall ee Shae er evens avai ARE ee ene eR eae To ea 99.60 | 99.67 99.60 SJAAOUUG Carhniny Aaescodgaooudsobo osaaninoodqoBdono€ Deol || eee 2.749 I. is the clay just as it came from the pit, after drying at 100° C. If. is the fine or kaolinite portion of I. washed from the coarse matter by repeated decantation and stirring. The separa- tion is not perfect, but imitates what would be done in washing on a large scale. III. is the coarse residue from this washing, its com- position being calculated from the two preceding analyses after finding that it constituted 67.1 per cent. of the whole clay. The carbonic acid remains as a silent witness of the agency by which the clay was formed. The following show II. and IIL., caleulated in percentages on the original unwashed clay, and indicate how the various ingredients distribute themselves between.the fine clay and coarse residue: TT. Til. if RIGA siciate. “or ecyemecievaletd alte wl eeteete ne eae eee 16.33+62 .50=78.83 MUTI AL ae aap ehe Souter EEE A bip\odial oro oo oc 12.03-+ 1.40=13.43 DesQuiox Miron. ih, ak eile Ja dts Weiiee a ee 241 © .50= .74 MGA 7. Jaroiale wee ees b's sve a Keo aot ea Eee .00+ .64= .64 IMAP NESIR Eo Ugare ey selina a done.) ele Caen ee 00+ .07= .07 Tots Ay Siis'e ose Sic ales. ehciask eit agate aie: UE See 12+ .25= .37 OOS sie eter egtere sii) dycsaprieieis: han ne a siento oie ee 038+ .04= .07 WV GET Micrieler ia. siete lois sais evap Gree cohen ee 3.754+. 17.0= 5.45 GUC ENDS Lc OE MNOMP mer hl EN 32.50-1-67.10=99. 60 KAOLIN IN WISCONSIN. 19 The fluxing ingredients, iron oxide, lime, magnesia, potash, soda, very small in the original clay, have thus been removed largely (five-sixths) by washing. The following are other determinations made on saniples from the same locality, all in the raw state: Constituents. IV. Vv. VI. WAU Sesquioxyd of limon... ... 6.2.56... 1.69 DinSe esterase ae a ates TRG Gg dees a ge 0a ea area Cote iW 78 2.14 SOG Es bo SSSI ais OS SIG I RO ETO EAS Arner oar (ape ate .03 330i NINVERIIGIE, (G6 oso, ch a see Sue a RAS Ce Nes PES SC DO Os ee ee eee 56 IV. is the bright yellowish clay from near the surface; V. is some- what less yellow but apparently more ferruginous. It is the most abundant kind. VI. is white clay, still retaining, to a marked de- gree, the lamination of the original rock. It would appear, how- ever, to be much more thoroughly decomposed than much of the more homogeneous clay of the region. VII. is a highly micaceous weathering granite from the river bank near by the kaolin pits. On the northwest quarter of the southwest qnarter of section 4, town 22, range 6 east, on the east side of the Wisconsin river, near the centre of the section, kaolin occurs overlaid by ten feet of friable sandstone. Most of it has lost the rock structure, though this ap- pears very distinctly in places. This clay is one of the whitest looking noticed. It has been used for making hearth at the Grand Rapids foundry. The following are Mr. Sweet’s analyses of sam- ples from this place: Constituents. VIII. IX. xe XI. HOEK WECSTIONC Ls ss). 2 elves sees ADRS OM ey atersrresnaea eteyenee trance evel leteneie «axons PINE PPOLUOM Acs aces Loi ose saith BST Asde ee arta call eta Ag Net ells aon ws esacere os HES OLAS ie et orcy esos: Se dvajones ale aieconsysl|isiaietetedearete 0.38 1.21 .87 OCP Re elec areola eiaiierore ihe avail ovary yeeros 0.08 0.46 00 VIII. is the raw clay; 1X. the same washed. X. is raw clay taken from the box at the foundry, and said to come from the same place; XI is the fine portion of X. The removal of alkalies by washing is here evident. 20 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. In digging for the turn-table at the Green Bay and Min- uj nesota depot, at Grand Rapids, a few lay- I| ers of compact sandstone were first pene- E Ys au trated, this giving place suddenly to a J. = ‘ white kaolin through which piles had to Ne Gi vu be driven five or six feet (?) before becom- WeYye & & ing firmly placed ae Ia ing firmly placed. S Ao Immediately north of the Rablin House, ae at Grand Rapids, kaolin is exposed in the a7 ral dss cut made for grading the street, which re : é here runs immediately along the river bank. x 3 s e The following section was obtained at this iS K & me point—Fig. 1—:* RK Vy The decomposed rock is in most places 3 \{I))) quite firm, though often a soft clay. It is all whitish, aud without any appearance of the unaltered rock except the lamination. = A specimen of the former kind yielded: XII S Potash. siaie.s ties ois eeeyeteteleterers leis elec teeter tee Relea 7.56 = Sodas. ccniee gals cand oletsiee wacbeee pel ee eee 5.03 SWIAteD’. Sioteic su sie, olan lercleis slenetace lolehetotelo vers letete lene teneeas 3.55 S The decomposition had not yet removed = = much of the alkalies, although the rock = was quite white. On lot 5, section 24, town 22,range 5east, onthe westside of the river, on the land of Mr. L. P. Powers, kaolin occurs in the river bank. The clay has been dug here to aconsiderableextent. Itshows here as elsewhere every degree of decomposition. The pure white is of inconsiderable thickness before a firmer rocky kind is reached. At the waters edge below are seen ledges of unchanged rock. At the time of my examination the locality had been less developed than since that time; but the several outcrops along the river bank in- dicated a considerable quantity. From this place all of the clay that has been shipped away from Grand Rapids has been taken. Places were noticed here where bunches of highly ferruginous clay *The engraver has omitted the word ‘kaolin,’ in Fig. 1, underneath “ sand- stone,”? and also the word ‘gneiss ”’ after ‘‘ decomposed.’’? ‘‘ Unaltered gneis”’ should read, “‘ unaltered gneiss.’ KAOLIN IN WISCONSIN. a occurred in the midst of the whiter kind. The following are analy- ses of samples from this place: earthen: XII. | XIV. XY. XVI. | XVIL. | XVITI.} XIX. ROilGalt. be sveiels as FOE Soe |Pyetare tote rell Moca ahora: Nase lDerelanaiuiceare Tea) i Gomedc 69.34 Alumina ...... SOS A Weeca el els evens s0.heee te wtegiy Sele Wi. GSy \tenoenci < 19,19 Sesquiox. Iron.! 1.24 |........ Boal) IIsadooon Pigses ll se Sco at Hee 1 Dra oa easton UU) lh acti at le Macs oe Deane N83} Wscbosooo 0.44 Magnesia...... @ 02 Iocooncuallooococ dolacouucer INA ON Wee seperevet= 0.31 ‘Potash! fas. ose: 2.49 1.22 2.30 1.96 1.69 O) 333) 3.30 Sodantaeseoe 0.10 | trace trace 0.05 0.39 10 2.43 Carbonic acid .. OR OD iy aeeycaiees ON pie Cal aA Oe traces lee ec Aeece | pee evetees Wraters.o.2..%: 5.45 OAM Pa wrath ota ciel Shere coesve.s SGI leas Neate 2ECT “WomMlasoese 99.31 10.06 4.60 2.01 99.76 2.43 99.43 XIII. is the raw clay from the exposure furthest down stream. It was averaged from an apparent thickness of three feet. XIV. is the fine portion of XIII. XV. is the raw clay from the next ex- posure above along the river bank. It represents an approximate thickness of two and a half feet. XVI. is the fine portion of XV. XVII. and XVIII. are the raw and washed clay from the exposure furthest up stream, still showing the rock structure. XIX. is only partly kaolinized rock from thesame place. These analyses nearly all indicate the material lessening in percentage of the alkalies ef fected by levigation. On the west side of the northeast quarter of section 26, town 22, range 5 east, on Mr. Canning’s land, several pits and a well have been sunk into kaolinized rock. The decomposition did not appear to extend to any great depth. The following are analyses: Constituents. PRONG | RONG |S NENG PRONG ane F SHEED. ood 50.5 Sb BE be EE SEU bid UBIGGO ng tian IMnitre iairol Inseclactiercc Iorerscioion 54.87 DARL LITANIA RMA hy Pa te eClub tree ses, alah alle evel a.ajeyaiel|'s: oveleiel'eeleslaysrerate: ele 28 .87 Sesquioxyd of Iron..............- Mesogeon eee alleeG anes bl lgonouaoS 1.54 lPigorenaGl Gr IKON 5 sooneosD boob ovODOUDOCOdOODE oPhe Payer ovepay aval ci cuctejistotare .95 JDINIG.S Song Che eee NS haere ears literati sta tararaves lire eiaterere aleve eveeeverel= 1.62 MIGGRIGSIBS |, 5 so obo ORDA DODD ne OOO ERE e Oe IOC DO Cnn bu oooan Copm Onion .99 TPO EA © cod 5 Sate Bo Eee ODODE pee oa 1.84 2.65 2.95 2.57 SOON 3S BORo io oO OUOS CHEE RS DD De tieioerar 0.27 21 83 07 \AVattigie Ghb.Bs So's Ceara SEO tore Oo Cae ero rol Lao nomic Te QO) lis evarteyotans - 69.48 ANGeallsdoncegadcos aon oSURboREouDOcr 4.06 10.35 3.78 100.56 22 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. XX. and XXI. are crude and washed clay from Mr. Canning’s well. XXII. and XXIII. are both washed samples, from different pits. XXIII. was 43.39 per cent. of the unwashed clay. All of these clays are very white, but appear to be much charged with alkali even after washing. On the northwest quarter of section 10, town 21, range 5 east, on the land of Mr. Moses M. Strong, on the west bank of the river, kaolin occurs underlying sandstone. ‘The clay shows at a number of places at different levels above the water, but these do not prob- ably indicate’ a continuous mass. Two samples were taken from the opening at this place, one at a higher level than the other. The following are analyses: Constituents. XXIV.| XXV. | XXVI.|XXVII. IROtaSW ere ysialesie wie eats < ein Ree en Cae 1.25 2.18 1.51 1.54 SOU: te vatatels cwiste else asld s bette eine ere ents 0.08 trace. 0.81 0.22 XXIV. and XXV.are the sameclay, before and after washing, taken from the upper portion of the opening. XX VI. and XXVII. are crude and washed clay from a lower level. The percentage of alkalies does not appear to be lessened by washing. About half a mile below this place the last Archaean rocks are seen in the bed of the stream, and resting directly upon them the sandstone. Sections showing the exact junction of the two ter- ranes are common in this vicinity. A detatied section across the river was taken at one place, the water being very low. It is an interesting one, and I have condensed it in Fig. 2. KAOLIN IN WISCONSIN. 93 Kaolin on Yellow River.—Kaolin is reported in quantity on Yel- low River. The localities are above Dexterville in Wood county. The Archaean rocks are exposed finely Si for many miles along the bed of the | stream. They show everywhere a ten- dency to weather, consisting largely 71° of a pinkish felspar. In places I no- ticed the weathermg carried to the condition of clay, but did not see any of the white clay that is said to exist. Kaolin on Black River.—On this stream, in Jackson county, kaolin oc- curs between Black River Falls and Black River Station. As on the Wis- consin, the Archaean rocks are found here forming the bed of the stream, the sandstone overlying them in the banks. In many places the gneissic rocks are decomposed. At the lower end of the rapidsat the town of Black River Falls, the gneisses disappear be- neath the sandstone. A section very like that on the Wisconsin, at Point Bas, occurs here; and exhibits the mode of formation of the kaolin hand- somely. usjony if “ISUDOIST/| auUOISPURS Ve AOATY GC PLT UID On the west bank of the river at Ledyard’s old mill, is a high cliff of sandstone overlying gneiss, (Fig. 3.,) g the exposures of both rocks extend- \& ing seyeral hundred feet. The surface AN of the gneiss is irregular, its de- N pressions being filled by the over- e ‘ lymg sandstone. The gneisS is very 3 1) 1°) /auunya distinctly seamed—the seams striking north 37 degrees west, (magnetic,) and dipping southwest about sixty de- grees—is moderately coarse, micace- ous, and has much pinkish orthoclase felspar, which occurs some- euoIspUuDS — 24 WISCONSIN ACADEMY SCIENCHS, ARTS, AND LETTERS. times in nests of some size. Near the water-level the gneiss is but little changed, but as as it is traced up to the sandstone it is found getting more and more decomposed, until it becomes a soft, grey- ish kaolin, retaining most markedly the laminated structure of the eneiss. FTE. 3 Bary j Sandstone cliff 20’ J Conglomerate 8 Kaolinized rock 52 Sa \\\\ \ ne ANY ey &; Quantity of kaolin obtainable in Wisconsin.—Taking the whole district together, a very large amount of kaolin undoubtedly exists. There is no reason why what has been seen should he all there is. It must always however be expected that any one deposit will vary much in character, both as to purity, and as to thickness. Num- bers of instances came to my notice where boring showed two feet of kaolin, and no kaolin at all, within afew feet of one another. The fact that the kaolin is apt to occur in continuous lines will however counter-balance the disadvantage of its lack of uniformity, since it can be searched for with assurance of success. In my opinion the indications are such as would warrant the outlay of money in exploitation. TII.—USES OF KAOLIN. Having thus shown the existence of kaolin in Wisconsin in quantity, it becomes pertinent to ask what it is good for. Its chief 4 KAOLIN IN WISCONSIN. BS use has always been in the ceramic arts. It is also used to make fire-brick and refractory vessels, and to some extent in making alum. The two former of these uses are the important ones. Use of kaolin in the ceramic arts —For making the finer kinds of pottery the important qualities of the kaolin are its color after burning; plasticity; and capacity of hardening well under heat without fusion. The plasticity is necessary for the moulding, the last named property for the perfect retention of the moulded form. Pure kaolinite is almost absolutely infusible under heat, simply losing its water and becoming an anhydrous silicate of alumina. This refractory property is lessened by the addition of any other bases; least by magnesia, more by lime, still more by iron oxyds, and most by the alkalies. The table of analyses of foreign clays given below, will serve to indicate how the Wisconsin clays rank in this regard. % The many kinds of clay-ware may be grouped conveniently into the dense and porous kinds,* according to the internal texture of the mass. Certain kinds of the dense wares are the ones for which kaolin is chiefly used. The ordinary “true” or “hard” porcelain consists of (1) a body of previously washed kaolin, and (2) a fusi- ble binding material, which by its fusion fills the pores of the baked clay and thus renders the ware homogeneous and translucent. This binding material, or ‘‘ flux,” is composed chiefly of felspar, to which are added other ingredients, such as quartz, gypsum, ete. In general, the three ingredients of porcelain are kaolin, felspar and quartz. ‘True porcelain has usually no external glaze placed upon it, its glaze being imparted by the flux which renders it translu- cent. To give an idea of the amount of kaolin needed in making porcelain, I select the following admixtures used at some of the famous Huropean manufactories:} * Wagner’s Chemical Technology. + Knapp. Chem. app. to Arts p. 229, 26 WISCONSIN ACADEMY SCIENCES, ARTS, AND.LETTERS. s o a g = £0 Hieila]s E Constituents. S| ae a es 3 2 os A ie) a 5 mm | 3 eles | 1 4 eels = 32) - Ss o oe = el\ei2| 2 | 2/613) 8 | & ea |] A | Ae (eo aaa AON 4138. cacys tise eee 7176 |72| 87 | 72 | 48/50 | 65] 40 IRE EVE GaGo Baodocapadooead0s os TUS IT O42 lth OCs eS le 12"). QDiti|sle cake aes QuieiRid eGgccugaakenos aeoanaso5ce Oe eeallaoas Sie oe Ne piay |) DI 33 1 ihn ae eA ASG Ser oS Noch coe Ibo daloooaltar ot VE ASMA SSB Goal) sacl ose (End GUSSsboon den odGHus0 Qos allnods\lo0 sollooaclonouce 4 5 Chalk iis 2Obs We ree anal eae dspace) [cues liaise cases 4. ||:siaverell Moneta nls Broken ware.......... La eieres ae ltomenalnieees 9 Be ea Cm aly 5 Sand separated from kaolin.......|....|.-..|..-.|....04 -.| 48 4 POA vets Saks Geir 100 {100 |100 | 100 {100 |100 /100 |100 | 100 Kaolin is used to a considerable extent also for other dense wares than true porcelain. In the manufacture of the so called English or “tender” porcelain are used kaolin, plastic clay, ‘* Cornish stone, ” burnt bones, and steatite. The ‘*Cornish stone” is the partially weathered granite, which by its complete kaolinization affords the famous kaolin of Cornwall. Preparation of kaolin for porcelain making.—The crude kaolin is always first washed to free it from quartz and felspar fragments. This is effected by simply breaking up the clay, stirring in water, and decanting the suspended matter. The coarse residue from this washing is frequently of value, since it contains two essential ingredients of the porcelain, viz. felspar and quartz. Use of kaolin as a refractory material—As a-fire clay or for making fire-clay articles, I cannot find that kaolinized rock has been much used. The chief difficulties in the way of such use ap- pear to lie in the lack of uniformity so characteristic of this kind of deposit, and in the fact that where of fine quality the material is too valuable for other purposes. The use of kaolinized rock from near Trenton, New Jersey, as an ingredient of fire-bricks, has al- ready been alluded to. The only other instance I find recorded is that of the so-called ‘‘ Lee Moor Porcelain Brick,’ made in Deyon- shire, England, by mixing a small quantity of inferior kaolin with an excess of the coarse residue obtained from washing the same kaolm. This residue consists chiefly of angular fragments of KAOLIN IN WISCONSIN. 27 ho quartz. The bricks are reported as of extraordinary refractoriness, and are even compared with the famous Dinas silica bricks. Practical suggestions as to the use of the Wisconsin kaolin to make fire-brick.—There appears to be every reason why a kaolin brick, if properly made, should be of unusual value. A few sug- gestions are given here as to its manufacture. First, then, the clay must be selected in the pit, the red and bluish portions being re- jected. The pure white are the best kinds, whilst some of the yel- lowish kinds are much better than they appear at first sight. After selecting, the kaolin should always be washed, to free it from fels- pathic particles, which contain a large amount of fluxing alkalies. The raw clay will never prove uniform in its capacity of withstand- ing heat. This is what theory would teach, and, as [ am informed by Mr. J. J. Hagerman, of the Milwaukee Iron Works, is found in practice to be the chief obstacle in the way of using the Wiscon- sin clay. The fine clay obtained by washing should next be mixed with a large excess of tolerably coarse angular quartz, for which might be substituted in part, fragments of fire-brick. The mass should now be moulded or baked carefully. In this way I am per- suaded that an unusually good quality of biick might be prepared. It will not do to make brick from this clay as the ordinary fire- brick are made, on account of its extraordinary shrinkage on heat- ing. Prepared in the manner I have suggested the kaolin brick would far excel: ordinary fire-brick for all purposes, save where contact with a highly basic slag is necessary, when it would be inapplicahle on account of its high content of free silica. I might say in this connection that a number of places exist in Wisconsin where the quartz for mixing with the kaolin might be obtained. I am informed that since my examination of the Grand Rapids lo- calities, a number of fire-brick have been made without great suc- cess, the clay being used raw and mixed with wood-ashes as a coun- ter-shrinkage ingredient. No worse admixture, of course, could be imagined, since the ingredient most desirable to avoid is thus di- rectly introduced into the clay. IV.—TABLES OF ANALYSES OF WISCONSIN AND FOREIGN KAOLINS AND FIRE CLAYS. These tables are given so that a comparison between the Wis- consin clays and the already well known clays of Europe and the 28 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. United States may be readily made. The analyses in Table I of Wisconsin kaolins are those already giyen, and have the same num- bers as before. In Table II., analyses J.,1L., U1.,1V., V., VI., and VIL, are taken from the “ Geology of New Jersey, pp 683-688. J.is the average composition of the best white clay of the Cretaceous, near South Amboy, analyzed just as taken from the pit. II. is the clay from Trenton, New Jersey, analyzed after washing to free from quartz sand, also Cretaceous. III. and IV. ure clays imported from Coblentz, Germany, for making glass-pots. V. and VI. are the St. Louis, Mo., glass-pot clay, raw and prepared. VII. and VIII. are New Jersey potters-clays (Cretaceous), and undergo some vitrification on burn- ing. Analyses IX. to XIX. are taken are taken from Percy’s Metal- lurgy, Volume on Fuels, p. 99. IX. is a true kaolin from Pool, Dor- setshire, used in making Cornish crucibles. X.is also a true kaolin, from Ireland. Small crucibles made from it were kept for hours with melted steel in them, without changing form. XI. is also an Irish kaolin. XII. and XIII. are the finest Cornish kaolin; analyzed by different chemists—washed before analyzing. XIV, is the best Stourbridge fire-clay; XV. a poorer kind of Stourbridge clay. XVI. is the best Dowlais clay; XVII. a poorer Dowlais clay. XVIII. is a greenish kaolin, with red spots, from Neweastle, Dela- ware; used for making glass-pots and porcelain saggars. Analyses XIX. to XXV. are from the Indiana Geological Report for 1874. XIX., XX., and XXT. are the Lawrence county, Indiana, porcelain clay, analyzed raw. XXII. is from Golconda, Illinois; oceurs in pockets in the Carboniferous rocks. XXIII, is washed Chinese kaolin. XXIV. is washed kaolin from St. Yrieix, France. XXV. is Missouri “ ball clay.” XX VI. and XXVII. are kaolins from Saarau, Silesia, analysed raw and washed; quoted from the second supple- ment to Watt’s Chemical Dictionary p. 354. In comparing the Wisconsin clay with these foreign clays it should be borne in mind that for porcelain making the qualities desired are whiteness after burning and refractoriness to heat; and for making firebrick refrac- toriness only. The coloration will increase directly with the con- tent of oxyds of iron. The refractoriness will decrease* with the increase of the ratio of fluxes (iron protoxyd, lime, magnesia, pot- * Watt’s Chem. Dictionary, Second Supplament, p. 354. KAOLIN IN WISCONSIN. 29 ash, and soda) to the silica and alumina together, and with the dec- rease of the proportion of the alumina to the silica. Of the fluxes the alkalies are the most, the alkaline earths the least harmful. TasLE I1.—Wéisconsin kaolins. (Analysed by HE. T. Sweet, M. 8.) Constituents. Ne JOE, JY Vi. Velie) |) VUES eS TEXe: x. Sula Revav.cccuceerssoeettesss IROtaSh rc eeeccleeccsskoe secs Protoxyd ef Iron. Carbonic acid.............008 HOLE cone bepeee cere eee Coarse sand SHIN =CVAY ta oersis cesses se aces Constituents. | XI. | XITIT. | XIV. | XV. | XVI. | XVID. |XVIIT.| XIX. SITING Seasntenoa neh encene aor el nau 70.83 OE2 DY eeeeneeecee 69.3 PAV raniateee: Syicecscsaceucestiel| Covccucasese 18.98 WG Bint esses ees “19.19 Sesquioxyd of Iron........]...........- 1.24 DEB SAE eee. 1.75 Lime 03335 | eae 0.44 Magnesia EAGT |e 0.31 Potash 4 i 1.22 2.30 1.96 1.69 2.33 3.00 Soda es d i Trace | Trace 0.05 0.39 0.10 2.43 Water So OH Eee eeAM loner eepreees OS OLE | eee 2.67 TPRMGOS VG OIE LIRONT ooreiccsten | booSeeocdcos | Au@eeaooecoo| fonccon anc eal laasonoSucken |b" eeobaceces! laagmeecoocdd | |agouocbocees! | socaneinacon (Obie S@HaI KOR YONG arreeeaoearosseol Aasoup sooo enn 770l lAsanqueoasdal eesaeeped lscddaacaceen MR eEEXeX Sin age eeeeescl debe: Baosteo eye ei || Miee seers [bosveseeess GOTO ees acteeess 99.42 WowEseySantGicsac.ccenscccecees Sp fc [fee oe a [Reel Pepe ee a ene aie ARE ie ae TRIG OAC? oleqcacn so W Sie RN eRe RM | ARE Bm a Bee aS een eee eececeeed| |coenoancecea! cboscceaceno) ocde ceca PROT ch ers eee ee elle eee nal aleaics koa Mc eeat halted | Bene ay, ateal lant. Sycpea lider ctreieoni| eteemeccacrall casleeazetens TO LOmy Avatar Omen nice in |orececey cenllbaneocve cose neesesv ees SO syoolge! 5. NOMS cl Us toa a | ee (CRE S@TTING GiGi sen oc oateecol eoaceebeacen | Ceocneen duel leecooeecoec | Isccaaceeonen| |cscca-ecaasal lascect odesoo! esscoceedoolc-rccochec oo MG talpewaleckse EF Pe FA tes Ee TUOLGGY Nelost ied eau cate | Opes tes | abana Woarse Sand nee e i csce. sone al. Seal acta Eee ~ 56.61 es Sued. seteae SPA Be Gre aaitca| Deeeeeer eats [pene eees ans: PHN = Clay, Meee ee ete eal onacesesceoslneStosccests ZIG} a ia ean see InR Ol Beeeecoscecna| lecececicceL ea ARG alter ates vceee teers llésbasoosveseliuccestedees TUCO 00)" | cet ere aetel (ee eetecoas| UseccBeeeecral lacteooe seca |-cearéeresnd 30 WISCONSIN ACADEMY SCIENCES, ARTS, AND, LETTERS. Taste IL—VFire-clays and kaolins from various localities. if, Constituents. CoH eaceodcee tac Sesquiox Lime... why tont to AYA AIT) Psa: Resaeeeere Protox. Iron. ... ZixcCON1a.. ...+-+s. Sulphur, ......... Phosphoricacid SMG eee agescess Combin’d water Hygros’pic wa’r |... Organic matter Total 100.00 100.32 Constituents. Ke BAIT UMCB cota sssnceces 78 40 74.44 J nile carb eehs Sereercno 12.25 19.04 Sesquiox. [ron.. 1.30 0.61 bynes) Saa-crrcenporro 0.50 0.45 Maegnesia.........]..... 2 Potash Soda Wialter eo .ccses Protox. Iron. .. Zirconia ..........|.. Sail har ee eseescesceselllecceses Phosphoricacid |\......::....|/...ccnenese OATES Bee 2 ae vee it eaareeseae es Combin’d water 5.20 5.71 ye TrOSADIChWaic las sealenssa|lesceseuesees Oxeamichma iberiliee veces dee saseece een Mota cceseee 98.65 | 100.59 SRST. | XSI TSG | EXSY 46.32 46.29 | 65.10 39.74 | 40.09 | 22.22 se weeceer see | weweeeeseeee Cree eles Wali. 59.60 26.41 1.61 1.00 0.07 0,29 0.19 10.36 VEL. || YeEDE |) eee: 71.80 | 65.62 48.99 19.95 | 20,88 32.11 1.31 1.23 2.54 OFS seeaeaeesees 0.34 0.79 0.30 0.22 0.61 1.95 3.3 63 2.33 99.88 KY. 99.95 | 98.08'} 99.36 XVL. | XVUL XV ILE. 67.12 | 44.25 72.23 21,18} 354.75 16.75 1.85 3.41 1,29 0.32 0.34 2.00 0.84 1,18 0.07 2.02 5 Constituents. | XIX. | XX. SHU rcnncbecs 45.90 47.05 Alumina.......... 40.34 37.14 Sesquiox. Iron..}......... trace UMN eee coca eee trace Magnesia.........| .ccccacee ; 0.03 Potashy teense Soda Mv es Mere ol Neer ters ee es scence noe IWiaiber is ctectere: sce 13.26 | 15.55 POLO Xe PUOM erase beret altace ol. ceece Zireouia.... Sulphur... Phosph’ric acid Sardseae eee , Combin’d water |. Hygros’pic wa’r |. Organic matter 99.50 XXII. 47.13 42.28 50.50 36.76 43.05 33.70 traAce:|| Pees 1.80 0,04 | trace 0.80 Peeerrrcel oecelccca 1.90 15.13 14.66 11.22 XXVIJXXVIT 48.37 | 65.69 | 19.99 45.39 34.95 | 24.87 | 17.31 39.34 1.26 2.54 0.56 1.23 DAD ae vasetaaes 0.46 1.04 12.62 | 16.60 5.70 12.95 99.91 | 100.00 SScuxx ——s LZ cM. & St.P Raitway e \ i) y, ? h a a, | & . Pas) “o } 6 a z j Abe a 2 ot a : oS ms wm adh %6 = \ oO Sir, N}), ,, (POLE > 5) \ ae ‘\ ind B me : A SP? fs thugkda, ete. The consonant-changes are due partly to assimilation, partly to dissimi- lation. In briggan (root brag, ef. fra-n-go), the 7 is a weakening of the originala. Inthe other dialects the derivative 7 (7) caused Um- laut in the present which remained after the j had disappeared (after stems long by nature or position) by syncope as in Old High German, or by assimilation as in the Anglo-Saxon. Butin the pre- terite Riick-umlaut takes place on account of the syncopated 7, which vowel-change, in addition to the consonant-changes, forms the peculiar characteristic of these verbs. This vowel-change is not the Ablaut, as some grammarians teach. ; Old High German—prenkan (prinkan), pret. prahta, p. p. praht. This verb belonged originally to the strong conjugation, (Class XII, Grimm), for we find the following forms: prank, prunkumés, prunkan; in the Gothic documents strong forms do not oceur. Its present stem was formed with the infix -na-, shortened -n-, which was originally a suffix. This verb is an example of a primitive verb in the transition-period to the weak conjugation, and Language remained conscious of its primitive character in retaining the strong form which occurs for the pret. participle in the dialects of New High German. Denchan (thenkan), pret. ddhta, p. p daht and denchit; dunchan, dithta, dtht; furhtan or forhtan, forhta, forht and furhtit; wurchan (wirchan), worhta, worht and wurchit (wurht). Old High German rejects the Umlaut of «; forhta and worhta have ~ weakened ~ into 0 on account of the following a, but when the succeeding syllable has 2, the original w reappears in the root, hence Surhtit and wurchit. In Middle High German the vowels 7 and w are sheltered by the liquids m and n, followed by another consonant. While the Um- STUDIES IN COMPARATIVE GRAMMAR. 119 laut wis unknown in Old High German, it appears in Middle High German without excluding entirely « (0); we observe therefore a fluctuation between w (0) and. Bringen, brdhte, brdht; the strong forms branq, brungen are occasionally found in documents of the twelfth century. The strong pret. participle ge-brunge(n) by the side of gebrocht for gebracht is found in dialects of New High Ger- man. Denken, ddhte, ge-daht (gedenkt, New High German patois); dunken, dihte (dunkte). gedtht (gedunket); viirhten, vurhten, vorh- ten, pret. vorhie, p. p. gevorht, geviirhtet, gevorhten; the o flattened into d(d), continues in New High German patois. Warken, wurken, wirken, pret. worhte, (warhte) wurhte, p. p. geworht, gewurht, ge- wiirket. In Anglo-Saxon the a has weakened into 2, as in Gothic, e.g. bringan. The 7, not only original, but also weakened, passes into e, hence the form brengan, by the side of bringan; the ein brengan might be considered as the Umlaut of the original a, on account of the syncopated derivative 7. I prefer, however, to take e asa weakening of 7, because this verb does not seem to have established itself entirely as a weal verb, as indicated by the existence of the strong forms brang, brungon. It forms the preterite bréhte, not brohte, as the comparison with other dialects shows. Although the Anglo-Saxon 6 is identical with the Gothic 6, it corresponds here to the Gothic @; an interchange between 6 and 4 is peculiar to Anglo- Saxon (Low German.) In bycgan the y is Umlaut of the original u, which passes into oin the preterite. The consonant combination eg represents the gemination of g, which takes place before a syncopated j according to Holtzmann, Altdeutsche Grammatik, p. 919, 5. But it is preferable to assume an assimilation of the deri- vated j to the preceding g: bygjan> byggan> bycgan. This deri- vative g (assimilated 7) is dropped before the suffix of the preterite, which causes the reappearance of the original w—weakened 0: boc(q )-de> boc-te>boh-te; the sonant d is assimilated to the surd c, and “when two mutes come together, one of them often becomes continuous for more easy utterance.” Of hycgan hycte> hyhte, which could not have been distinguished from hyhte, the preterite of hyhtan, to hope. It is evident that hogde with the Riick-umlaut is a later form than hygde, if not, there is no reason why we should not have hohte. The cognate hogjan (Class II.), pret. hogéde, may have been the cause, that hygde adopted Riick- umlaut. In thyncan the y is Umlaut of wu; in the preterite Riick- umlaut takes place; thahte worhte; the o is therefore not the effect of the h, as Dr. March assumes in the article above mentioned, (p. 112, 3); for the original yi would have the breaking eo. The lecgan and secgan arise through assimilation and umlaut from lagjan and sagjan. As the derivative j (g), Anglo-Saxon e, disap- pears in the preterite of stems long by nature or position, which causes Riick-umlaut,—the preterite of these verbs is “lagede,*sagede >laegde, saegde, contra., laéde, saéde; ae is the regular weakening of a. The e in segede, legde is bad spelling for ae. In Old Norse we observe similar euphonic changes, e. g. sockja from sékja, oe (ae) being umlaut of ¢, forms the preterite with Riick-umlaut sétta. We should expect sékta, tor kt never assimi- lates into tf, as Helfenstein says; but as & represents an original h, which with ¢ assimilates into tt, the form sdtta is entirely regular. In Old Swedish we find sékt by the side of sott. In yrkja y is the umlaut of o (a); its preterite is orta and orkta (varkta). Of three consonants one is sometimes dropped, cf. mart for margt; morni for morgni, apni for aptni; thykkja or thykja, kk—nk, pret. thétta from théhta< tkok(n)hta; thekkja, e is the umlaut of a, pret. thdtta from thahta»., ii, 6, 14.) * Duty is always performed when the advantage of mankind is con- sulted.” (Do., in, 6, 15.) “Although nothing is so contrary to nature as depravity, yet nothing is so much in accordanee with nature as utility, and certainly depravity and utility cannot be found together.” (Do., mi, 8,2.) ‘This is the law of nature which you should obey and follow, that your interest is the universal, and the universal one your own.” (Do., i, 12, 7, and 6, 1.) “ Heis a good man who bene efits as many people as possible and harms no- body.” (Do., mi, 18, 9.) ‘ Those who separate utility and morality overthrow ey fu me principles of nature. We all seek ntil- ity, are carried away by it, and cannot do otherwise. For who flees away from what is oe Who does not rather pursue ib most diligently?” (Do., 11, 25. 1,2.) ‘*‘ Whatever is useful is vir- tuous, though if does not at fis rst seem so.” (Do.; ii, 28, 9, and 30, 10.) These quotations show how fully the Stoies reeognized utility as the imseparable and characteristic result of virtue; though their position cannot be further explained, until we have considered their language about happiness and pleasure. . The following passages are in harmony with the two about hap- piness, already quoted from Seneca. ‘All men wish to live happily bat cannot discern the proper way.’ (Seneca, De Vita Beata, I. 1.) “To live happily is the same as to live according to nature.” (do, do, 8, 3, also 3, 3, and Kp. 124, 7.) ‘“ He has reached the perfection of wisdom, who dees not place his happiness in another’s power.” (do, Ep. 23, 2.) ‘* Make yourself happy.” (do Ep. 31,9.) ‘‘ All men seek happiness. In what do they err? In taking its conditions for itself.” (do Ep. 44.7.) “He who is not happy, has not attained the supreme good.” (do Ep. 71, 18.) What is the business of virtue? A life truly ~ WERE THE STOICS UTILITARIANS? 185 prosperous.” (Hpictetus, Dise. I, 4, Higginson, p. 14) ‘Suppose then, I should prove to you that you are deficient in what is most necessary and important to happiness, and that hitherto you haye taken care ot everything rather than your duty.” (doii, 14, Hig- bo einson, p. 137.) “Show me some one who is always happy, for I long to see a Stoic.” (do 1,19) ‘You were not created to be de- eraded or miserable with others, but to be happy with them. For God made all men to enjoy happiness and peace.” (do iii, 24, 1.) “ Be contented with asound mind and a happy life.” (do ui, 24, 118.) 9 * Our struggle is for prosperity and happiness itself.” (do iii, 25.) “You have applied yourself to philosophy only in name, and lave disgraced her principles, as much as you could, by showing that they are unprofitable and useless to these who study them. You have never made peace, tranquillity and equanimity the object of your desires.” (do ii, 26, 13.) * What isthe object you should seek except a happy life?” (do iv, 4, 4) “ Be mindful, morning, noon and night, that the only way to happiness is this.” (do iv, 4, 39.) “Meditate upon your actions. What have [ omitted that is con- ducive to happiness? What have I done contrary to the interests of my friends or of my race? (do iv, 6,85.) ‘“ It is better that your servant should be bad than you unhappy.” (do HEnehiridion xii, Higeinson, p. 379.) “To be happy is.a good object and in your .) own power.” (do Fragment, xix Didot.) ‘It is better to contract yourself within the compass of asmall fortune and be happy, than to have a great one and be wretched.” (do Frag. xxiv, Didot, xxi, Higginson.) | In the original of the last passage the verb is the one translated be of good cheer, or be merry, in our Bible, (Acts xxvii, 22 and 25; James v., 13.) and corresponding to the adverb rendered cheerfully (Acts xxiv., 10), as well as to the noun selected by Democritus, as the mark of the system thence called Huthumism by Miss Cuobbe, (Essay on Intuitive Morals, p. 221.) and signifying “the pursuit of virtue for its intrinsic 7. e. moral pleasure.” In the other quota- tion from Stobseus, and in all those from the third book, the terms are those familiar ones, whose use by the ancient advocates of Util- itarianism,leads Miss Cobbe to eall thats ystem Hudaimonism, mean- ing “the pursuit of virtue for the sake of the extrinsic, affectional, intellectual and sensual pleasure resulting from it’ (do. p. 219). In other passages, however, isfound a word peculiar to the Stoics, 186 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. who thought so much of happiness that they invented for it a new term, Huroia. Their yiews of this favorite idea appear nowhere more clearly than in a long passage of Epictetus (Discourses, book II, ch. xvii., Higg'nson, p. 151), where the student, who has learned to desire nothing but freedom from passion and trouble, is said to have passed through the first class in philosophy, whence he enters the second class in his desire to know his duties to for- eigners, his country, his parents and the Gods. Thus the first de- gree in Stoicism was to make one’s self hsppy, and the second to be useful to others; which second and higher degree is that mainly dwelt on by Cicero and Mareus Aurelius, as has been already shown. The Tusculan Disputations and De Finibus of Cicero state at some length, that the Stoics agreed with the Peripatetics, Hpicu- reans and other acknowledged Utilitarians, in honoring happiness as the greatest good and highest aim of man, and differed from them mainly in declaring that the sole and sufficient means of ac- quiring it was virtue, or, in other words, both active and submis- sive obedience to the commands, prohibitions and decrees of nature, their favorite watchword being “ sustine et abstine.” The peculiar bitterness of the controversy between the Stoics and Epicureans was partly due to the attempts made by the latter, to overthrow the established opinions about theology, politics and metaphysics, and partly to their assertions, that pleasure was not only the means but the synonyme of happiness, that the virtues are chosen for the sake of pleasure and not on their own account.* It does not appear from Lucretius, Diogenes Laertius, or Cicero, that regard to any happiness but our own was ever inculeated by the Epicureans, and it is certain that they committed the danger- ous error of using Greek and Latiu terms for pleasure which have an extremely sensual signification, hedone being rightly trans- lated lust in our New Testament, (Titus Iil, 3, James IV, 13,) and voluptas bemg used in a sense even grosser than that of our derivative voluptuous. Mr. J. §. Mill does not “‘consider the Hpicu- reans to have been by any means faultless in drawing out their scheme of consequences froin the utilitarian principle” (Utilitarian- ism p. 11;) Professor Bain “* cannot but remark that the title or for- mula of the theory was ill chosen, and was really a misnomer,” *See Diogenes Laertius, p. 470—3. WERE THE STOICS UTILITARIANS? 187 (Moral Science, p. 140.) Bishop Cumberland, one of the earliest modern advocates of the greatest happiness principle, attacks Kpi- curus and his followers vigorously, and two of the best known among the ancient expounders of that principle, Aristotle and Theophrastus, take similar ground, the former denying that pleasure is the chief good or synonyme of happiness and warning his disci- ples against snares, (Hthics I, 9, and X,3,) while the latter speaks so strongly of the peculiar guilt of sins committed with pleasure, that his language is quoted with hearty approval by Marcus Aurelius (Ii, 10.) Weshould not therefore infer that the Stoics were not Utilitarians, because they opposed Hpicureanism, which system in- deed had become, before any exposition ot their views now extant was written, little else than a cloak for indolenee, servility, protl- gacy, and indifference to the claims of patriotism and philanthropy, as indeed the lives and writings of the best known of the successors of Hpicurus prove only too plainly. Marcus Aurelius, Epictetus and Seneca saw these facts so clearly, and loved practical morality so faithfully, as often to speak of pleasure with unqualified aversion. Seneca, however, frequently distinguish- es the voluptas which is brevis, tenuis, corporalis, vana, nimia, poenitenda ac in contrarium abitura, from that which is vera, sta- bilis, naturalis, necessaria, in animo, ete., (De Vita Beata iv, 2; vi, 1; Ep. 18,10: 21, 11; 78, 22;) and Epictetus uses hedone with sim- ilar caution (Disc. ui, 7.) These two terms are also employed in some remarkable passages which may be regarded as foreshadowing the discovery, now the bulwark of utilitarianism, that pains are the correlatives of actions injurious to the organism, while pleasures are the correlatives of actions conducive to its welfare. ‘Pleasures are the incentives to life-supporting acts, and pains the deterrents from life-destroying acts. (Herbert Spencer’s Psychology, Ed. of 1872, Vol. i, p. 279-284.) With these statements should be care- fully compared the following: ‘Nature has mingled pleasure with necessary actions, not in or- der to have us seek after it, but that what we cannot live without may with this addition, become more attractive.” (Seneca Hp. 116 3.) Pleasure is the companion, though not the leader, of a virtu- ous will. When virtue leads, pleasure follows like a shadow.” (do, de Vita Beata, viii, 1 and xiii, 5.) ‘“ Our nature is to be free, noble and modest. And pleasure should be subjected to these virtues, as 188 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. a servant and assistant, and sustain us in doing what is commanded by nature.” (Epictetus, Discourses im, 7, 28.) ‘ We do not think that pleasure is commanded us by ae . but that it is a result of what is so commanded, namely. justice, temperance, and freedom.” (do Fragment lu, Didot.) soe who speak thus cannot be charged with ignoring the value of pleasure, which indeed they sometimes acknowledge even more ds ‘Our pleasure is doing good.” (Seneea, De Beneficiis iv, 13, 2.) * We shall not have any the less pleasure for giving virtue the pre- oN cedence, but shall be its masters and governors.” ‘(do De Vita Beata xiv, 1.) ‘It is a great pleasure for me to think of the charac- ter of Scipio.” (do Hp. 86,5.) “I permit you to enjoy pleasures, which will come to you more plentifully if yon rule them than if you obey them.” (do Ep. 116, 1.) Usually, however, terms, which denote only mental pleasure, like gaudium, leetitia and various forms and derivatives of the verbs chairo and euphraino are preferred, of which common prac- tice a few instances will be given. “ He has reached the height of wisdom who knows what to re- joice in. Learn this, first of all, O Tene (Seneca Ep., 23, 2.) ‘*T am not depriving you of many pleasures” ae ‘but desiring that joy may never fail you.” (Do. Ep., 23,3.) “ Nothing which-is not right can please anybody sara (Do. Ep., 20, 5.) You can see that you are not yet sufficiently wise, for the wise man is always joyous. Joy belongs to ae alone, and this is the reason that you should wish for wisdom.” (Do. Ep., 59, see. 2, 14 and 16.) ‘“ The wicked find a fleeting aa eset in what gives the wise man enduring joy.” (Do. Ep., 59, 24.) “It is right and natu- al for the good man to be joyful.” (Do. De iis 6.5.) 7% Min= joy the present and accept all things in their season.” (Epictetus’ night My Oe Dise. [V, 4,45.) “ Take continua] pleasure in passing from one philanthropic action to ae thinking of God.” (Mareus Aure- lius VI., 7.) ‘* What remains, except to enjoy life by joming one good thing to another, so as not to leave even the scale interval between.” (Do., XII, 29. Long. See also VIIT, 26, and X 33.) The reader may charge the Stoics with self-contradiction in their language about mental pleasure, but he can find none in their re- fusal to admit bodily pleasure as a legitimate motive or as any part WERE THE STOICS UTILITARIANS? 189 of happiness. Here, indeed, they differed from the Epicureans, but they agreed fully with the keen-signted Peripatetics. The philoso- phers of both these schools were wise enough to know that the best way to be happy is to disregard bodily pains and pleasures, and cultivate ec: kindness of heart, and nobleness of though. I[é was also characteristic of both Stoics and Peripatetics, hough no&of the Epicureans, to aim at universal, and not merely personal happiness, and to believe that virtue should be practised for its own sake, that is simply on account of its ees with the laws of nature. Indeed, the Peripateties charged the Stoies with stealing all their teachings, merely altering the terms, as thieves do the ear-murks of stolen cattie.* The position that virtue is su ficient oe happpiness. however, was 7: further differed from the Peripateties & eonfined to the Stoies, who as did the Epicure sans also, in refusing to accept the judgment of the wisest as the moral standard, and spa all other ptiloso- phers. nob only in teaching disinterestedness, but in importing that regard for all the interests of their race which has Since been called the enthusiasm of humanity. Stoicisim is thus seen to have preierred universal to individual happiness, disregarded bodily pleasures. demurred to accepting even mental ones as motives. believed in following virtue for her own sake, and placed morality on a disinterested basis, scarcely any ot which views would be thought compatible with being utilitarian by those who, hke Mr. Lecky, consider that term as a synonyme of selfish. Even he, however, makes some discrimination in favor of what he calls “the refined sensuality ” of the Mills, Tucker and Anstin, while Miss Cobbe distinguishes plainly between the two schools of Private and Public Hudaimonists, as she styles them, in a description much coufased by her taking, as the representative of the last named class, Jereny Bentham, who really belongs, with Paley, the French naturalists of the last century, and the Epicu- reans, among what we may call the self-regarding or individualistic Utilitarians, who did not believe in disinterestedness or in caring for others’ happiness except as a condition of one’s own. No won- der that Stoicism appeared trash to a man who finaliy discarded the last four words of his own famous formula, ‘‘ the greatest hap- * See Ac. Quaest. 115. De Finibus II, 23, 27. ILI, 3. IV, 26, 28: V, 13, 16, 17, 25, 26, 29. 190 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. piness of the greatest number,” and who, if we may trust the Deon- tology so far, even declared that “‘ A man can no more cast off re- gard to his own happiness, meaning the happiness of the moment, than he can cast Off his own skin.” The progress of psychology is rapidly destroying the arguments on which these egotists rested, and showing that the real repre- sentatiyes of Utilitarianism are those who, like Bain, Mill, Spencer and others of its most recent advocates, plant themselves on disin- terested social sympathy so firmly, and teach regard to universal happiness so plainly, that they deserve no worse epithet than that of humanitarian or philanthropic. Their position is so little un- derstood, that a few characteristic passages must here be quoted from the little book, called “ Utilitarianism,” by John Stuart Mill, published in 1863, and since reprinted among the Dissertations and Discussions. ‘This it is, which, when once the general happiness is recogniz- ed as the ethical standard, will constitute the strength ot the utili- tarian morality. This firm foundation is that of the social feelings of mankind, the desire to be in unity with our fellow creatures, &e., (p. 45). “Rew but those whose mind is a moral blank, could bear to lay out their course of life on the plan of paying no regard to others except so far as their own private interests compels” (Do. end ch. iii., p. 50.) “ The utilitarian standard is not the agent’s own great- est happiness, but the greatest amount of happiness altogether ”’ (Do. p. 16). The happiness which forms the utilitarian standard of what is right in conduct, is not the agent’s own happiness, but that of ail concerned. As between his own happiness and that of others, utilitarianism requires him to be as strictly impartial as a disinterested and benevolent specator. In the gelden rule of Jesus of Nazareth, we read the complete spirit of the ethics of utility,” (p. 24). “ Utilitarianism could only attain its end by the general cultivation of nobleness of character” (p. 16). “ It maintains not only that virtue is to be desired, but that it is to be desired disin- terestedly, for itself” (p' 53). ‘‘ Readiness to serve the happiness of others by the absolute sacrifice of his own, is the highest virtue which can be found in man ” (p. 23), “ Virtue in those who love t disinterestedly is desired and cherished, not as a means to happi- WERE THE STOICS UTILITARIANS? 191 ness, but as a part of their happiness” (p. 538-4). “Virtue, above all things important to the general happiness” (p. 58). With the above passages should b2 cited these two from the articles on Comte. “ No one, who understands any morality at all, would object to the proposition that egoism is bound, and should always be taught to give way to the well understood interests of enlarged altruism. It is an error often, but falsely, charged against the whole class of utilitarian moralists” to require ‘ that the test of conduct should also be the exclusive motive to it” (p. 125-6 of the Reprint). Sir James Mackintosh also maintained (according to Bain’s Moral Science, p. 264), that ** the utility is the remote and final justifica- tion of ali actions accounted right, but not the immediate motive in the mind of the agent.” These passages give, with but incidental differences, the views not only of Bain and Spencer, but of Hume, Locke and Cumber- land, and with these philanthropic utilitarians, the Stoics and Per- ipatetics would have agreed much more readily than the Hpicure- ans. ‘The Stoical literature is especially rich in passages honoring the social feelings and teaching universal philanthropy. “Nature endears man to man,” (De officiis I. 44.) “ Nothing is more natural to man than kindness,” (do J, 14,1.) ‘All men are plainly in union with each other,” (do I, 16, 5.) “Knowledge 1s empty and isolated, unless accompanied by Jove of all mankind, and of universal brotherhood,” (do I. 44,8.) ‘The brotherhood of the whole human race is especially in accordance with nature.” (do [il. 5, 2.) They say that we should love our fel ow citizens, but not foreigners, destroy the universal fellowship of mankind, with which would perish kindness, benovolence and justice,” (do 1il. 6, 6.) “The same law of nature joins us all together,” (do ILI. 6.3) “Care for other men and serve the human brotherhood,” (do JIL. 12, 7.) ‘‘Nature has inclined us to love our fellow men, and this is the foundation of the law.” (De Legibus1, 15.) ‘* Nature so endears us to each other that no man should ever be unfriendly to another, simply because he is a man,” (De Finibus III. 19.) “Nature bids us prefer the general advantage to our own; for all the uni- yerse is one common city of men and gods,” (do do.) ‘ We are im- pelled by nature to benefit as many people as possible, born for hu- man brotherhood, and joined together in one great community,” 192 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. (do 20.) “The aim of the Stoic is to be useful. not to himself alone but to all men, both collectively and individually, (Seneca, De Clem. Il. 5,3.) “Guard religiously the bond which unites man to man and establishes the common rights of all the race,” (do ep., 48, 3.) raphy bilesop ey teaches reverence for the gods and love of man, (do ep., 90,3.) “This isthe rule of duty. Nature has made us kindred, implanted in as mutual love, and made us kindly affectioned, so ful for us to injure than to be injured. She bids that it is more pain our heipfui hands be ever ready. Have this verse ever on your lips and in your heart. ‘lam human, and [think no other maa a strang ty We are born to live together. Humanity is an areh which falls unless each part sustaias the rest,” (do ep. 95, 52, 3.) ‘The wise man thinks himself the citizen and soldier of the uni- verse, and labors as if under orders.” (do ep. 120, 12.) “IT owe more to the human race than to any individual, (do De Ben., VIL. 19, 9.) **Men by mattis endeared to each other,” (Epictetus Il, 24. Higginson, p. 266.) ‘“ Man’s nature is to be gentle and sociable,and to do good,” (do IV. 1, 122, 6.) “U would have death find me doing something benovelent, public-spirited, noble. (do 1V 10, 12.) “Noth- a is nobler than magnanimity, meekness, and philanthropy,” lo Fragment LL.) ‘I would lay aside all self love, (Marcus Au- oe IL. 5.) “ Rational creatures exist for each other,’ (do IV. 3.) * The sole fruit of this’earthly life is a pious disposition and philan- thropie activity, (do VI. 39.) “Oaly what is useful to Rome and to the universe is useful to me,” (do VL. 44.) “One thing here is of great worth, to live in fellowship with trath and justice, and yet be benovelent to Hars and unjust men,” (do VI. 47.) “tis peculiarly human to love even those who ilo wrong,” (do, Vil. 22.) ‘ Love mankind,” (do VIL. 31. ‘ Benevolence to our fellow men is peeu- liarly human,” (VU. 26.) “Itis not fit that I should give my-elf pain, for I have never given pain intentionally to anyone else,” (do VILL 42.) “ Among the properties of the rational son! is love of one’s neighbor,” (do X.1,1.) “Have I done anything for the general interest? I have had my reward,” (do XI. 4.) No wonder that J’ S. Mill calls the commentaries of Mareus Au- relius ‘‘ the highest ethical product of the ancient mind.” Indeed the writings of these two philosophers are admirably in harmony, like their lives. It is true that before the discovery, but little more than a cen- WERE THE STOICS UTILITARIANS? 193 tury ago, of the doctrine of association of ideas, so liltle was known of the process by which we rise, from desiring certain qualities, as means to happiness, to desiring them for their own sake, and rec- ognizing them as virtuous, that the Stoics were obliged to content themselves with sometimes enjoining disinterestedness, but not giving any adequate reason, and sometimes demonstrating the ten- dency of virtue to produce happiness without showing how knowl- edge of this is compatible with the duty of being disinterested. Similar ignorance of the fact, perhaps never yet made sufficiently prominent, that no happiness can be universal, except that which consists mostly in the enjoyment of the higher pleasures, because these are the only ones which can become objects of common de- sire, without exciting general strife, compelled the defenders of the Portico to maintain that virtue was the only means of happiness, though they occasionally admitted that mental pleasure can become felicity. In the same way their tack of knowledge of the full psy- chological value of pleasure, as an indication of utility, as well as of the distinction afterwards made by Mill and Mackintosh, between taking utility as a test or as a motive, forced them either to deny as stoutly that it is the best motive as to disparage its value as a test, or else to use 1: as a test so inconsiderately as almost to sanction it as a motive. They stated all the facts in turn of the Utilitarian theory, as held by its most advanced modern advocate, but without being able to see the relations of these parts so accurately as to present the whole truth. Their zeal for practical moral culture and universal progress in virtue was another chief cause of these inconsistencies, which, indeed, in that age could scarcely be avoided, except either by the recklessness with which the Epicureans de- clared pleasure to be the best of motives as well as tests, and even in its grossest forms the equivalent of happiness, or by the insipid understatements which prevented the Peripatetics, despite the consummate genius of their mighty founder, from leaving any deep imprint, except his own, on either literature or history. The tact that only one school of ancient philosophy was able to produce a crowded series of noble patriots and philanthrophists, among whom Tiberius Gracchus, Cato, Portia, Thrasea, Epictetus, Dion Chrysostom, the younger Pliny, Trajan, Antoninus Pius, and Marcus Aurelius are merely the best known instances, shows that stoicism was able to do the practical work of utilitarianism with a 13 Was 194 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. , success so peculiar as searcely to be compatible with serious defects in theory. But these heroes became martyrs so commonly, and uniformly struggled agamst tyranny and profligacy with such self- denial and self-devotion, as necessarily gave the Stoics a peculiar tendency to asceticism, which, indeed, never hindered their being studious, patriotic and philanthropic beyond comparison, but which often prevented them from weighing the worth of pleasure with scientific accuracy. Of these struggles and martyrdoms, Mr. Lecky has given us so beautiful, and, despite mistakes, like calling Brutus a Stoic,so val- uabie a narrative in his History of European Morals, that it is all the more remarkable that he did not see how completely he has answered his own arguments against the value of utilitarianism, which fill a large part of his first volume, by showing, in the re- muinder of it, what a noble work was done by the obnoxious theory, in the ethical elevation and influence of the most zealous of its ancient advocates. Failure to see the resemblance of stoic- ista to utilitarianismis, however, to be expected from a writer who so far ignored the position of Mill, Bain, and Spencer, as to call the system, of which they were the leading expositors, selfish. And this failure was much more excusable in works written, like Miss Cobbe’s essay on Intuitive Morals, before the broad school of happiness moralists had gained its present prominence. How early in life J. 8. Mill accepted Hpicurus as the first utilitarian in pre- ference even to Aristotle, we need not inquire, nor how far this view was imbibed from Jeremy Bentham. The common misunderstanding of the true relationship of the Stoies has been much promoted, among other causes, by the fact that, like other ancient philosophers, they paid such regard to what they called Nature, as to satisty themselves with appealing to her fancied authority instead of pushing derivative analysis to the last results. Hvidence has, however, already been offered to prove that in following Nature the Stoies not only conformed to the principal precepts of the most enlightened Utilitarians, but even used their method, so far as to call only useful qualities and actions natural, a term by which, indeed, they meant little more than that the origin of the claims of utility was a sacred mystery. Indeed, modern science has been obliged to exert all her powers in order to solve this mystery so far as to show that the enlargement and ennoble- ’ WERE THE STOICS UTILITARIANS ? 195 ment of human happiness is the realization of all our finest im- pulses, dearest wishes and highest hopes. Ancient philosophers, however, were so blinded by this illusion, as Well as so ignorant of the real value of pleasure, that perhaps none of them can, in strictness, be called utilitarian, and it is “searcely worth our while to consider whether the title of founder of the greatest happiness theory should be given, on acount of pri- ority of time, to Aristotle, rather than to either EKpicurus or Zeno, or whether his claim also should yield to that of Socrates, whose regard for utility appears in many passages of the Memorabilia. It is enough to say that the Stoics, despite their noble inconsist- ences, maintained the most important principles of Utilitarianism in such purity and power, that they must hold the highest place among its forerunners, if not among its originators. Recognition of this fact would not only encourage the use of their writings as introductions, and even in some respects as supplements to those of Mill and Spencer, but would help us value justly the system of philanthropic Utilitarianism by showing how much was done for moral culture by one of its rudimentary forms. 196 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. AN EXAMINATION OF PROF. 5. H. CARPENTER’S POSI- TION IN REGARD TO EVOLUTION. BY HERBERT P. HUBBELL, WINONA, MINN. If we were called upon to define the position oceupied by Dr. Carpenter, in his paper before the February meeting of the Acade- my of Seience, Arts and Latters, we should say that he was an Evo- lutionist bub not a Darwinian. To make this distinction plain, and to show more clearly his po- sition, we should say that an eyolutionist, as generally understood, is one- who believes in evolution as taught by Spencer; that is to say, that matter, inorganic and organic, has arrived at its present degree of complexity by evolution from a simple state through a series of differentiations governed by some unknown law. That countless facts in nature substantiate this position, and that whilst recognizing the present state of nature as forming one extreme of the series, it finds, at present at least, in nebulous matter the other extreme. Starting as it does with matter in its highest state of complexity it pursues it, by a process of strict inductive reasoning through its ever- varying phases of decreasing complexity until the mind loses itself in an an illimitable expanse of nebulous matter. Darwinism is an at- tempt to show that in so far as organic nature is concerned, evolution is dependent upon some occult law of generation co-operating with those conditions in nature necessary toits developmen. Evolution and Darwinianism, then, are in one sense materialistic; they deal wholly with the facts of nature and look to material causes to pro- duce material effects. But Dr. Carpenter does not de this. Though he believes that in nature there is an evolution of matter, the recognition of this fact does not suffice: he goes beyond matter, beyond its nebulous state and finds there 1 Supreme Intelligence ‘¢ which is the highest generalization of which matter and mind are capable of.” This Intelligence, like all intelligences, must be, and is, governed by the laws of rationality, and must in its mental ac- EXAMINATION OF PROF. CARPENTERS EVOLUTION. 197 tion, proceed either inductively or deductively. Constituting as it does the highest generalization, it is debarred from mental activity in the énductive direction, and is, consequently, obliged to manifest itself deductively. But mind is subjective. 1t can only manifest itself objectively, and hence, nvitter is such objective manifestation. Matter, therefore, on this hypothesis becomes nothing but the symbol of thought. The Supreme mind man- festing itself according to deductive laws proceeds in a series from the simple to the complex. Hence, matter symbolizing this thought will proceed in the same manner. Differentiations then in matter are not due to generative forces residing in “the organism but to thought existing in the supreme mind. And thus it is that Dr. Carpenter is an Evolulionist but not a Darwinian. The key-stone of Dr. Carpenter’s logic is found in a Supreme In- telligence,—not the Supreme Intelligence as generally conceived, but as specially conceived by men, that is to say, as being the high- est possible generalization—as governed by the same rational laws that govern us—and as manifesting his thoughts in material forms. It is evident that the surest way to weaken this logical structure will be to weaken this conception. Let us grant that the mind must proceed either deductively or inductively, the question arises which process has precedence. Is it possible to reason deductively before we have inductively arrived at our deductive stand point, or to reason inductively be- fore we have deductively reached our induction stand point? or in other words do we reason naturally from the particular to the - general or from the general to the particular? A moments consid- eration will inform us that before we can reason deductively, we must have reasoned inductively. The growth of the child’s mind is the natural growth, and it is from the individual to the general. The individual facts begiu to form into groups of animate and in- animate, and these into subordinate groups, and these into others; there is in fact a constant sinking of individual characteristics into those that are specific, and of these latter into those that are gen- eric, and of these into broader divisions, and thus, step by step, the highesé generalization of which matter is capable is reached, which is, as Dr. Carpenter truly says, the highest knowledge. No deductive standpoint, therefore, can be reached save only through induction; but once attained through the instrumentality of a few facts, we may use the deductive method to discover the many. 198 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. _ “Comp*ete generalization is complete knowledge” not because the generalization contains the potential attributes necessary to constitute individualities, but because it is the generaliza- tion stripped of its individualizing attributes. The indi- vidual must exist before the genus, there can be no generaliza- tion unless there be a preceding individualization. The individ- ual is lost in the species, the species in the genus, the genus in the order, the order in the class, and the class in the kingdom. The two kingdoms, vegetable and animal, have properties in common which classify them as organic. Organic and inorganic bedies hav® elements in common which unite them under the head of matter. Matter has weight and density and dimension; if we rise in our generalization we must in some measure eliminate these properties these individualities. In order to do this we conceive of matter reduced to a state of the greatest rarity—as filling all space—as be- ing, in fact, a homogeneous, illimitabie, imponderable. chaotic mass. But let our conceptions be at their best we must still think of mat- ter as having limits, elements and adegree of density. Our high- est generalization is reached when we think of matter as existing in this nebulous state. Now, conceive a Supreme Intelligence, and what is the effect in ourmind? Immediately, our conceptions from being most indis- tinct and general, are concentrated upon one object having many attributes. For we cannot think of intelligence apart from mind, of mind apart from body, of body apart from members and of mem- bers apart from functions. In what sense then can the Supreme Intelligence be considered the * highest generalization,” surely not in a logical one, for instead of widening our generalization it nar- rows it. Following the strict rules of inductive reasoning we must stop with nebulous matter. A Supreme Intelligence is not a higher generalization. Ifsought by reason at all it must be teleologically and not by the rules of induction. Assuming, however, that the Supreme Intelligence exists and that it is absolutely the highest generalizatiou possible, are we to con- sider it as a generalization containing potential individualizations, or as a generalization stripped of its individualizing attributes? It is evident from Dr. Carpenter’s reasoning that he considers it the former, whereas, if it could be reached by a process of inductive reasoning, as he assumes, it is equally evident that it would be the EXAMINATION OF PROF. CARPENTER’S EVOLUTION. 199 latter. Can we conceive of a Supreme intelligence as being sub- ject to the laws of mental growth—of beiug wiser to-day than yes- terday? Is not the wisdom infinite, and the same yesterday, to-day. and forever? How then can we conceive of potentialities? Or on the other hand can we think of any attributes which could be added to it? Is net the Divine mind perfect in all things so far as our conceptions go? How, then, if we can conceive of nothing which can be added to it, can we conceive of it as existing stripped - of attributes? The Supreme Intelligence is not a generalization, but is, on the contrary, so to speak, @ strongly individualized human intelligence. Vivery mental faculty which we possess we conceive as being held by the Divine Mind in a perfected state. Wisdom, knowledge, justice, in infinite c.mpleteness go to make up our con- ception of God. If we increase in wisdom, knowledge and justice, we advance towards him; thats to say, the more strongly individu- alized our minds become, the nearer do we approach in likeness unto God. But if God were the “highest generalization” the more individualized we became the farther would we be from Him, and this is doubtless a result which Dr. Carpenter would be among the last to desire. “Tf the Supreme Intelligence is to communicate with man,” says Dr. Carpenter, “it must be in obedience to the laws which con- trol onr mental activities. The divine thought must then, like human conceptions, be communicated by means of physical sym- bols.” The error, (for we think there is one.) which lurks in this assumption is the error of all theologians, and forms the basis of all their reasonings and of all their conceptions; viz: That man is the object of creation—the end sought through the formation of mat- ter, and that the Supreme Intelligence is desirous of conveying his thoughts to the consciousness of man. Dr. Carpenter had just been speaking of the purely subjective nature of the conceptions of the artists, and that it was necessary before those conceptions could be communicated to others, that they should, through the instrumen- tality of the canvas or the marble, seek an objective expression, and to follow this remark with-that above quoted is to place the Sup- preme Intelligence in the artist’s position with conceptions to com- municate, and implies, before they can be communicated, an object- ive medium and another consciousness to which the communication is to be made. If man is the highest product of matter—of creative 200 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. forces—and if we assume a Supreme Intelligence, then the object of creation, if discoverable at all, is discoverable by man, or at least it is complete in him. But if, taking the other view, we look upon man as but a link in the chain of being—if we conceive of the forces of nature which in the past have evolved a higher type of matter as working for the same end to-day, our thoughts cease to dwell upon the present, and project themselves into a distant, but ever-perfecting future. The imperfections which surround us and which are the stumbling-blocks in the way to our conception of a perfect God, fade out, in the evolving ages, and the mind rests in the thought of a coming time when the divine idea shall be accom- plished and when the mysteries which now shroud all things shall have passed away and the “ glory of the Lord” shall be revealed. Prof. Carpenter admits an evoiucion of matter; he even admits that man is the highest product of evolution; he believes that the su- preme intelligence existed alone in his own consciousness, and that before he could exist in any other consciousness he must seek an objective material medium through which to express himself. If the supreme intelligence is purely subjective, as Dr. Carpenter claims, then anything external to and apart from that intelligence must be objective. Man, then, whether considered as matter or mind, is objective. The object of creation, according to Dr. Car- penter, is to communicate subjectivity to subjectivity through ob- jectivity, or in other words the divine conceptions to consciousness through matter. But human consciousness, as we have just seen, is objective to the divine consciousness; hence, the object of crea- tion is not to communicate subjectivity to subjectivity, but subjec- tivity to objectivity through objectivity, which is nothing more than saying that man is but one of the nicer touches from the hand of the painter; one of the finishing strokes from the hand of the sculptor; one of the pages from the book of the thinker. God is the artist, the universe, the canvas, and man but a pigment which, with other material, goes to further the divine conception. If matter is objective and the expression of thought, then man, being matter, is objective and an expression of thought. If he is an expression of thought he stands in the same relation to the su- preme intelligence that any expression of thought stands. Every ovject in nature, on Dr. Carpenter’s hypothesis, is an expression of thought. Man, then, bears to the supreme intelligence the same EXAMINATION OF PROF. CARPENTERS EVOLUTION. 201 relation that any animal or any plant bears. That relation is inscrutible, aud so is the relation of man. We believe in a Supreme Intelligence, and we believe in Hvolu- tion. We also believe that evolution in nature exists because the Supreme Intelligence has willed that it should exist; but we can- not believe with Dr. Carpenter that it exists, because there was no other way by which the Supreme Intelligence could manifest itself. For this would be to prescribe bounds for that which is infinite. It is true that we cannot think of God asa rational being without thinking of him as governed by the laws of rationality, nor can we think of Him as a just God, without being governed by the laws of justice, nor can we think of Him as possessing any mental! attribute without thinking of the law governing the manifestation of it. Yet these conceptions of God ,are but human, they are efforts of the finite to measure the Infinite, and taking them at their best, our reason tells us that they fall far short of God himself. It is true that in nature there is such an orderly sequence of events, that in recognizing it, we call it law, but to say that this law-exists because God designed it, and to say that it exists. becanse a rational God cannot manifest himself in any other way, are two very different things. Nor can we see, if the Supreme Intelligence is governed by the law of rationality, and if it manifest itself in material form, why there should be such enormous interyals of time between the different steps in the divine consciousness as is evidenced by the physical symbols. For if evolution in matter is but the reflection of evolution in the Divine mind, as Dr. Carpenter teaches, then ev- olution in both is simultaneous. There could, consequently, have been no conception of man in the Divine consciousness before his advent physically—for his advent physically is but the reflection of an evolved conecpt in the Divine mind. There could, therefore, have been no plan of creation embracing man, for man is the last of the series—is the complex as opposed to the simple—the particular as opposed to the general. But the last term in a deductive series must be reached by the law of rationality, that is to say, it must be derived from the first term by a differentiating process, consisting in the addition af attributes not found in the preceding terms. Ac- cording to Dr. Carpenter, if man had been conceived by the Divine consciousness it must have been by some rational process and such process would have been immediately symbolized in matter. But 202 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. because it was not thus symbolfzed we are bound to believe that no conception of man existed in the Divine mind until the time of his physical advent. But we cannot assent to this conclusion; we prefer to believe that before the nebulous mist arose, there existed in the Divine Consciousness a perfect conception of creation—the end to be com- passed, and the means to accomplish it. That when the fiat went forth, matter became endowed with certain principles which, act- ing constantly and uniformly, have evolved the countless forms that people the universe; and that they will continue to be evolved until the divine conception is wrought out. We recognize the ge- netic force as one of those principle; we recognize the tendency of organisms occasionally to depart slightly from their parent forms as the natural result of this principle; we can believe a departure from this departure as natural; and if we recognize two variations, we can recognize a third—a fourth—and any number. We can conceive it possible that a departure, and a continnal redeparture from the parent form might give rise to varieties so different as to be classed as species; we can conceive of species varying to such a degree as to constitute genera; and we can conceive of this “ func- tional impulse” working through countless ages with ever varying effects, as redounding more to the wisdom and glory of God than any number of successive creations, be they of the nature of dis- tinct fiats, or the symbols of evolution in the Divine Conscious- ness. SECTION OF THE Mathematical and Physt- Cal SCLeTLces. TITLE OF PAPER READ BEFORE THIS SECTION Recent Progress in Theoretical Physics. By John E. Davies, A. M., M. D. Professor of Physics in the University of Wisconsin. RECENT PROGRESS IN THEORETICAL PHYSICS. - 205 RECENT PROGRESS IN THEORETICAL PHYSICS. BY JOHN E. DAVIES, A. M., M. D., Professor of Physics in the University of Wisconsin. The present paper is the first of a series intended to give, in a collected and condensed form, the results of recent theoretical ad- vances in the Physical Sciences. The researches by which these advances have been made are partly experimental and partly math- ematical. Some of them are most lucidly presented by Prof. P. G. Tait in his ‘Recent Advances in Physical Science,” while those which I skall present are only briefly mentioned by him, or else are omit- ted altogether. Prof. Tait, however, alludes to those which he does mention, in such terms as to imply that he regards them, nevertheless, as of the greatest importance, and te be omitted chiefly on account of want of time. A complete review of these researches would include Clausius'’ remarkable theorems upon the mechanics of a great number of molecules, and Boltzmann’s results in the same direction, together with their application to the theory of heat; the studies of Helmholtz and Thompson upon the vortex motion of fluids and their analogues among magnetic forces and electric currents; Thompson's ex- planation of the magnetic rotation of the plane of polarization of circularly polarized light, first experimentally shown by Fara- day; the experimental researches of Jamin, Rowland, Stoletow, Bouty, and others, in magnetism; Rankine’s hypothesis of molecu- lar vortices; Clerk Maxwell’s wonderful electro-magnetic theory of light, with the experimental researches thereon by Boltzmann and others; the explanation of anomalous dispersion by Ketteler of Bonn; the mathematical relations of vibratory and translatory motions in fluids, by Challis; the explanation of the blue color and polarization of the sky by Lord Rayleigh; as also his remarka- ble results upon Resonance and Sound generally; the mathe- 206 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. matico-physical discoveries of Kirchoff; the Kinetic Theory ot Diffusion, Conduction and Radiation by Maxwell; the thermo- electrical researches of ‘Tait; and many other researches as well, all tending to the simplification and unity of the Physical Sciences, by showing a probable similarity or identity of cause for the most diverse phenomena. In the present paper I shall merely begin with certain remarika- ble relations between the formule of electro-magnetism and those of fluid motion, first pointed out, so far as I know, by Helmholtz.* VORTEX MOTION. In magnetism we have the following formula for the value of V the SCALAR POTENTIAL of a magnet of finite dimensions Dene O 9 VaSf GIS4AS Sf dadyde A. x,y, and z, being the coordinates of any point of the magnetic mass, 6, being what is called the surface density of the mag- netic matter, and, 9, the volume density of the same. The surface density 6, is the resolved part of the intensity of magnetization in the direction of anormal to the surface of the magnet, and the volume-density 9, is what Maxwell has designated as the ‘‘ convergence ” of the magnetization at a given point within the magnet. This expression for V is similar to that for the electric potential at any point, due to the electrification of a body on whose surface there is electricity of density 6, and within its substance a bodily electrification whose density is 9. In both cases, V satisfies La- place’s equation for points outside of the electrical or magnetic mass, and Poisson’s equation for points inside of the same. That is, for the first case, CV eV, eV 2 de! apt dz * In the paper as read before the Academy, a somewhat complete synopsis was given of Thompson’s explanation of Faraday’ 3 experiment on the Magnetic Rotation of Polarized Light; of Clerk Maxwell’s Electro- -magnetic Theory of. Light; and of the Hypothesis of Molecular Vortices. Many points, also, only briefly summar- ized in this printed paper were elaborated by oral explanations and diagrams, and the terms used in the paper were for the most part carefully defined. RECENT PROGRESS IN THEORHTICAL PHYSICS. 207 and, for the second case, = — 4tn*9 C. The ordinary magnetic and electric forces are derived from these potentials by the application of Hamilton’s operator, 5 @! NG d == k 2 Vise pa au! ap = a that is, to find the magnetic or electrical attraction or repulsion along a line, we take the differential coefficient of the potential (magnetic or electrical) with reference to the direction of that line. For ordinary magnets the potential V,is single-valued for any given point of space; for electro-magnets V is many-valued like —ly tan having, in fact, an infinite series of values at any given point; these values differing by 4n*? where? is the intensity, or strength of the electric current in the electro-magnetic wire. Carefully to be distinguished from V is another quantity, which. in the case of solenoidal distributions of magnetism at least, also fulfills Laplace’s Equation. This quantity may be designated by I. Lis a quantity so related to the magnetization that, calling the components of the latter in three directions at right angles to each other, A, B, and C, we have ReaD Bay all nal D. A “Ge” B dy . I, which determines the magnetization (not the magnetic force ) at any point, is called the Potential of Magnetization. i» But, besides the scanar (or non-directed) POTENTIAL, V. and the Potential of Magnetization, I, mentioned above, we have, when con- sidering not only the magnetic force but likewise also the magnetic induction, a VECTOR (or directed) POTENTIAL. The magnetic znduction is derived from this VECTOR POTENTIAL in a precisely similar man- ner to the derivation of the magnetic force from the SCALAR PO- TENTIAL, namely: by the application of Hamilton’s operator Vy, If three quantities /’, G, and H, be regarded as the components, in three directions, at right angles to each other, of the scalar *Qwing to the want of Greek type the printer has placed this letter n to represent 3.1416 the ratio of the circumference ofa circle to its diameter. 203 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. potential V, then these quantities wili satisfy the following con- ditions: dH aG dF di dG dF dx ‘ay =(. &£. But if /, G, H, be taken to represent the components of the vector-potential, they will satisfy the conditions GBEE NV GON vo oe a dr all fe ge dG dF dy dz ; dz dx ; dz dy where a, b, c, are the components of the magnetic induction. In words, the line integral of the vector-potential round a closed curve representing any circuit, is numerically equal to the surface- integral of the magnetic induction over a surface, bounded by the curve representing the circuit. We have also, if a, b, ¢, represent components of magnetic force, and u,v, w, components of electric current, a de db 4n*u = dy a ; da de 2, 4n*v = om : G. db da Si a END ied Am *y = Te a as the equations of electric currents: or, in words, the line-integral of magnetic force round aclosed curve is numerically equal to the current through the closed curve multiplied by 4*. The values of I’, G, H, are also given by the following equations i 1 Gaff f — dz dy dz H. 1 w Haff f — % dy dz where xu is the quantity known as the specific inductive capacity of a medium. or its permeahility to mugnetic lines of force. *The letter m is put for 3.1416. RECENT PROGRESS IN THEORETICAL PHYSICS. 209 The components of the vector-potential are related to those of the sealar- potential as follows: ET Gan dV dy dz dz dF ad dV 2a8 aia a I dz dx dy qaG dF VG dz dy Raa cae i a, b, ¢, being as before the components of magnetic force, derived from the scalar-potential V by differentiation along LY, 2 The components of the electric current, w, v,w, are known to satisfy the condition The components of magnetic induction a, b, ¢, also satisfy asim- ilar equation On a careful study of these formule, which have been deduced for the potentials and forces of ordinary magnets and electro- magnets, we are impressed with their similarity to the formule that express the ordinary motions of an incompressible frictionless fluid. For example, in fluid motion, where w, v, and 1, represent the component velocities of an élement of he fluid in Gr ree rectangu- lar directions, and D represents the density of the fluid, we have the following so-called ‘“‘ Equation of Continuity” of the fluid: Gap eh) Gl 10) dD , J. feds Digt Bra jtete We v5 oe =0. This equation is proven for ordinary motions of fluids, in all works upon the dynamics of fluids. It is merely an analytical statement that in all motions of fluids, however they may expand or contract, and move about in currents or otherwise, there is no change in the mass of the fluid caused by such motions. If the fluid be incompressible, there can also be no variation in its 14——_w AB 210 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. density, caused either by its own motions or by the lapse of time. Then, the total differential of D in the preceding equation, will be zero, and there will be left du dv dw te K. dx dig eda: ees which is the simplified form of the ‘equation of continuity” for in- incompressible fluids. KHquation (K), is an equation of condition which all incompressible fluids are required to fulfill. If u, v, w, be made to depend upon the variations of a quantity Q, such that aQ d@ ae 0, PTE Mag eos altuna 2 Waa we may call Q the velocity potential of the velocities wu, v, and w; be- cause it is a quantity the first differential co-efficient of which along a line, x, y, or 2, gives the velocity of the fluid along that line. This quantity Y, must, in incompressible fluids, which, since w, v, w, as has been said, satisfy Equation (K), therefore also give 2 2 2 ds2 dy2 dz2 ; or, in other words, like the scalar magnetic and electric potential V,or the potential of magnetization I,it must satisfy Laplace’s equation. Returning to magnets, and electro-magnets, we have seen that the general expression for the value of the potential of any magnet of finite dimensions, at any point in space whose co-ordinates are x’, y’, 2’, is, designating the potential by V, Vi = Sf 2a 84 Pacayaz where the surface part of the integral extends over the whole sur- face of the magnet, designated by S, and the solid part of it (every element of which =dz, dy, dz) extends to all portions within the surface. r= the distance from the magnet to the point, x’, y’, 2’, where the value of VF is taken; I[=l1A+ mB + nC i. e., the intensity of magnetization normal to the surface of the magnet; because RECENT PROGRESS IN THEORETICAL PHYSICS. 211 A, B, and C, represent the intensities of the magnetization, along the three co-ordinate axes; and l,m, n, are the direction-cosines with reference to these axes, of. anormal to the surface. 6 is often called, as was said betore, the surface-density of the magnetic matter; and 9=interior-density of magnetic matter;—9 is also @A @B dC See ay ae 0, when the magnetization is solenoidal. Now, since A, B, C, are the components of the magnetization of the magnet, if we take a quantity J such that dl dl dl —— : n= JR 8 —— = (CO). dx # dy then, also, as was said before, I may be called the potential of mag- netization, and it is evident that when the magnetization is sole- noidal, we shali here also have the condition (a a dx? ' dy?" dz? — as in the case given above, [Hquation (M)], of the velocity potential of fluid flow. Hence the velocities «, v, w, in the case of fluid flow in incompres- sible fluids, are the analogues of the electric and magnetic forces in free space, and of the components of magnetization in the case of solenoidal magnets. At least, all three sets of quantities are subject to the same analytical conditions. I the Potential of Magnetization gives, Ul Soe dx2 dy2 dz N. Q, the Velocity Potential of an incompressible fluid, gives HQ PQ ql a2O Vn. dz? ee dy? a az 9. V, the electric potential gives dV , d#V, d?V aa" age ae — © In magnetic and electric distributions, the rate at which V varies along a line, determines the electric or magnetic force in free space along that line. J12 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. In magnetization, the rate at which I varies along a line, determ- ines the intensity of the magnetization, at any given point within the magnet, in the direction of that line. In fluid motion, the rate at which Q varies along a line, determ- ines the velocity of the fluid, at any given point, in the direction of that line. In the case of ordinary fluid motion, moreover, if the conditions d¢ d d Fi paige penne. pees. O Ep dz an. had uin Vn diei dies dg ines yh da ae ee as 1s well known. We have seen [| Eqs. (D) and (E] that precisely similar conditions obtain in the case cf ordinary distributions of electricity and mag- netism, so long as we confine ourselves to the space outside of that which contains the so-called magnetic or electric matter. The motions of fluids heretofore discussed in treatises on the dynamics of fluids are such as fulfill the conditions imposed by equations (O) and(P.) They are motions of translation, or of expansion and contraction; oscillatory movements being merely periodic movements of translation, of greater or less extent. All such mo- tions have assumed for them a velocity potential, the differential coef- ficients of which with reference to the coordinates, are the com- ponent velocities of the fluid in the direction of the zoordinates. The assumption of a velocity potential necessitates the set of conditions given above in equations (OQ) and (P.) But Helmholtz in a remarkable memoir on “ Integrals Express- ing Vortex Motion” to be found translated by Prof. Tait, in the Philosophical Mag., for 1887, has shown that these conditions do not hold if there be some of the elements of the fluid in rotation. In such cases if w', w”, w*, represent the angular velocities of the rotating fluid element about the coordinate axes, then we have du au, ae A i 2w dw du dz dz 0 Q dv d — — — = Dy} RECENT PROGRESS IN THEORETICAL PHYSICS. 213 For these cases there is no velocity potential. ‘It is only when there is no velocity potential that some fluid elements can rotate and that others can move round along a closed curve in a simply- connected space.” Helmholtz calls the motions that have no velocity potential, generally, vortex motions. He shows that in a frictionless fluid, these vortices when once instituted in the fluid, have a wonderful tenacity of existence; that they may go on widening, changing their form under the influence of other vortices, moving about, attracting and re- pelling each other in consequence of combining their motions; and that they may play amongst themselves all sorts of fantastic eames, yet preserve unchanged their identity and living force (i. e. their kinetic energy) so as to be the very types of the unchanging atoms of matter, which are never destroyed. One simple instance of Helmholtz’ results I will state, to make the matter plain. If there be, for example, a single circular vortex ring set up in an indefinitely extended fluid, the center of gravity of the section of the ring (section supposed small) will have from the commencement an approximately constant and very great velocity parallel to the axis of the ring, and this will be directed toward the side to which the fluid flows through the ring. Two ring-formed vortex-filaments having the same axis would mutually affect each other, since each, in addition to its own proper motion has that of its elements of fluid as produced by the other. If they have the same direction of rotation, they travel in the same direction; the foremost ring widens and travels more slowly, the pursuer shrinks and travels faster, till finally, if their velocities are not too different, it overtakes the first and penetrates it. Then the same game goes on in the opposite order, so that the rings pass through each other alternately. If they have equal radii and equal and opposite angular velocities, they will approach each other and widen oue another. So also one will widen on coming to a fixed wall. ‘The motions of circular vortex rings can be studied by drawing rapidly for a short space along the surface of a fluid a half immersed circular disk, or the nearly semi-circular point of a spoon, and quickly withdrawing it. There remain in the fluid half-vortex rings whose axis isin the free surface. These vortex rings travel and widen when they come to a wall, and are widened 214 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. or contracted by other vortex rings exactly as deduced from theory.”* In this memoir it is also demonstrated that the product of the ve- locity of rotation into the cross section of a vortex-filament is constant throughout the whole length of the filament. Moreover, that a vortex-filament can never end within a fluid, but must either re- turn ring shaped into itself within the fluid, or reach to the bound- aries of the fluid. Precisely similar theorems had been announced by Sir Wm. Thompson in a paper on the Mathematical Theory of Electro- Magnetism in 1847. Thompson, in this paper, designates the strength of an electric current by ({, and then says: “In a con- tinuous current this quantity is of course the same for every section; and, as it is impossible that a continuons stream of electricity can emanate from one body, and be discharged into another, the current must be 7¢e-entering, or every continuous current must form what is called ‘*a closed circuit.” It is found by experiment that what- ever be the dimensions or material of the different parts of the conductor along which the current flows, provided always the di- mensions of the section be sma!l compared with the distances through which the electro-magnetic action is observed, the quan- tity ( has the same value for all parts of it; and even in the places where the electro-motive force operates, as has been shown by Faraday, as in the liquid of any ordinary galvanic battery, or in a conductor in motion in the neighborhood of a magnet, the electro-magnetic effects are observable, and, probably to exactly the same degree; so that it would probably be found that a galvanic circuit, consisting of a battery of small cells, arranged in a cireu- Jar arc, and a wire completing the circuit by joining the poles, would produce the same electro-magnetic effects at all points sym- metrically situated with reference to the circle, irrespectively of the part of the circuit, wnether the cells or the wire; provided always, that the distanees considered be great, compared with either the dimensions of a,section of the wire, or of any of the cells made by planes perpendicular to the plane of the circle, through its cen ter.”’ * Professor Tait’s book on ‘‘ The Recent Advances in Physical Science’? has two figures, one showing how these vortex rings can be produced, and the other what he direztions of rotation anl move n2at will be in a ring once formal. + See Thompson’s ‘‘ Reprint of Papers on Electro-Statics and Magnetism’’—p. 409 et seq. {For current strength Thompson uses the Greek letter gamma. RECENT PROGRESS IN THEORETICAL PHYSICS. 215 The precise character of the movement within the wire, is also shown to be entirely irrelevant in this estimate of the current strength. For “in the theory of electro-magnetism it is unnecessary to adopt any such hypothesis as this [ that the electric current consists of matter flowing, | however probable or improbable it may be as an ulterior theory; and all that we could introduce as depending up- on it is that, for a linear circuit of varying section or material, the quantity () is the same throughout the circuit, and that all finite circuits possessing continuous currents are necessarily closed; two facts which cannot be assumed a priori, but which are in reality established by satisfactory experimental evidence.’’* {, the current strength here alluded to, is the product of the so ealled intensity of the current, into the area of the cross-section of the conductor. It may be measured of course by the work it will do in a definite time, either as electrolysis, heat, or other form of work. Helmholtz’ angular velocity of the vortex-filament in a fluid, affords a means of forming a mental conception of intensity of current, in electricity. by assimilating it to the rotatory energy in a vortex-filament, which is far superior to any of the illustra- tions ordinarily used; and this without in any way necessarily implying that the electric current actually involves such rotating elements, although this may really be. As a linear electro-magnet is com pletely specified when the form of the closed curve of the current, and , the strength, are given; so also a vortex filament is completely specified when the form of its axis and the product of its angular velocity into the area of its cross section are given. In electro-magnetism we have 7A=7'A’ for the same circuit. In vortex filaments qA=q'A' for the same filament; g being the an- gular velocity; A, A,’ areas of cross sections; 7,2’, current intensi- ties. In electricity, magnets are known to circulate around cur- rent-conducting wires, and wires reciprocally around magnets. In fluids, vortex-filaments that are straight circulate around each other and their mutual center of gravity; vortex filaments that are cir- cular also revolve around each other, as is shown by the peculiar action described above where the rings alternately pass through each other, by contracting and accelerating their speed, and then wid- ening and moving slower, while the one following contracts and passes throngh in turn. * Reprint—p. 410 216 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Helmholtz further shows, in the memoir above alluded to, how to find the velocities, w, v, w, of any portion or element of the fluid when we know w’, w’, w*, the angular velocities of a vortex-fila- ment established in it, by the following method: Let there be given within a mass of fluid which includes the space §, the values of w’, w’, w*, satisfying the “equation of conti- nuity ” dw} dw2 dw a =e a ail: (1) Also, u, v, and 2, must satisfy a similar equation, du dv dw és Wea dy dee (2) And likewise also, these conditions, dv dw j dw du cares du dita aut SSS SE dye tute (ae (3) == 74! dz Per idipena 2? ide dz The conditions for the bounding surface S are supposed to be given according to the particular problem. a, b, c, can be taken as the three angles made with a normal to the surface S; q as the re- sultant angular velocity of the three components ww’, w*, w®; 7, the angle between the normalsto the surface S and the axis of the ro- tating filament; then we shall have wl cos a + w? cos b + w cos c = q cos. T= 0. over the whole of this surface S, or if this surface S cuts any of he vortex-filaments, over the whole of some larger surface S', which includes all the filaments, and their continuations, if there be any» in the first surface S. Now we can find values of w, v, and w, satisfying equations (2) and (8), if ge ec ec (4) RECENT PROGRESS IN THEORETICAL PHYSICS. DT and if the functions L, MW, N, and P, be taken so as to satisfy also within the larger space 8’, the couditions 7L Ly 2L il du? a dy? a dz= ~~ aw d?M d? AL d?M a =v gp oo te (5) aN dN d2N 2 — ZW dx? a dy? a dz? 2 @P @P a2P aah Srey an ap dx dy dz The analogy of these equations (5) to Poisson’s equation (C) is at once apparent if wi w2 w? Qny Qn? 2m’ be each taken equal to 9. L,M, N, are quantities which satisfy the same equations as the vector potentials of electric currents. They stand in the same relation, in vortex fluid motion, to the angular velocities of the core of the vortex filament, as do in electricity the vector- potentials of electric currents, to what might guardedly be called the mass of the currents which give rise to these potentials; thus again showing the help we may derive in our notions of electrical strength, mass, density, or whatever we choose to call it, by com- paring the ‘‘current-penetrated space,” to the core of a vortex fila- ment. It moreover prominently calls our altention to what may be going on in the space outside the wire, as well as in the sub- stance of the wire itself. Indeed, if + be the distance of a point a, b, c, from a point x, y, 2, on the axis of a vortex-filament; andif wi, w2, w, be the values which w!, w?, w*, have at this point, a, 0, c, then we will have | 1 AoE Le Ml dadbde 1, » Wa 6 Ma — 1 * yp “edadbac (6) N SE ig dbde P54) ¢ Rs —_——— * n represents the ratio 3.1416. 218 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Equations which are analogous to equations init which suggest 1 that, since Tina here takes the place of ame % in those equations, Fe M, or the magnetic permeability, may be equal to w* wu’, divided by 9, generally, while here definitely equal to the fi 2 That equation (2) is satished by the values of w, v, and w given above in equations (4) is shown by differentiating equations (4) and adding; we thus get Ghiy | GRIP Oy CVE dw dP first ee a aaa ay oe an = eauame dx dx dy dy dz dz" 1 then, on adding dz dy dz That equations (3) are likewise satisfied, 1s also shown by differen- tiating equations (4), and then making the necessary subtractions; noticing the values Qu”, 2w*, 2w*, given by equations (5). We thus get: do_dw oa 4 [ab aM, aw 2 ahi dz | dx dy dz } Cian Ny a Ae raee ania (7) dz” dz dy | dx dy dz J du _W@ os d (dL , dM, dN) Se ee — + dy dz dy |\dx — dy dy J which, if the second terms of the second members are zero, show equations (3), and likewise equations (Q), to be completely satisfied. That these second terms are zero is shown by first differentiating equations (6) with respect to x, y, and 2 successively; thus getting results of the form 1 — hi See da db de for each coordinate. And then, on integrating these latter results by parts, we get the following three equations: w 1 dw3 en gal Bae MY Ge 88 dM 1 we dwz ayer 2 da ade — fff —. 8 dadb de (8) aN a apes i ie dz 27 iL Tr dadb — on SIF ai See db de Paces eee eer ean ee eS eS ee *The letter n represents the ratio 3.1416. RECENT PROGRESS IN THEORETICAL PHYSICS. 219 which, if added, and dS be put for the element of surface, give 1 es Sh \w8 cos. 1+ w2 cos. b+ wa cos. ¢ dS === fiir = [e xg Le Bae dwwa va Ala, 6b lp. In the second member of this last equation the factors in paren- theses in each of the two terms, are known to be equal to zero; con- sequently, dL dM dx a dy dz = 0. Therefore the equations dv dw z dw du eat du dv — —— = 2; SS SSS = SSS SSS SP dz Dyn ee ea, ieee sa Gent eh et we give correctly the relations between the angular velocities of the core of a vortex-filament, and the velocities in the fluid at points outside of, but surrounding the core. The values of L, M. N, taken from equations (6), being substitut- ed in equations (4), give certain results, the interpretation of which will appear from the next paragraph. These results are Au(zt—a)+ Av (y—b)+ Av (2—e) =0, (9) indicative of a right angle with 7’; waht + warv-+ waav=0, (10) indicative of aright angle with the axis of the rotating filament; and gr. cosV = (x —a)wa + (y—b)wg + (2 —c) wg (12) Where q is the resultant of wa, 2, Wa, and V the angle which q makes with the radius-vector 1. Now it is proven in works on electricity and magnetism* that “the vector-potential at a given point, due to a magnetized particle placed at the origin of co-ordinates, is numerically equal to the magnetic moment of the particle, divided by the square of the radius vector to the point, and multiplied by the sine of the angle between the * Clerk Maxwell’s ‘‘Electricity and Magnetism,’ Vol. i1., p. 28. 220 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. axis of magnetization and the radius vector; and the direction of the vector-potential is perpendicular to the plane of the axis of magnetization and the radius-vector, and is such that to an eye looking in the positive direction along the axis of magnetization, the vector-potential will be drawn in the direction of rotation of the hands of a watch.’ The results just referred to above, show that the distance-action of vortex-filaments is similar to the electro- magnetic action of current-conducting wires; for they prove that “each rotating element of fluid (a) implies in each other element (b) of the same fluid mass, a velocity whose direction is perpendicular to the plane through (b) and the axis of rotation (a). The magnitude of this velocity is directly proportional to the volume of (a), iis angu- lar velocity. and the sine of the angle between the line (a) (b) and that axis of rotation, and inversely proportional to the square of the dis- tance between (a) and (b).” Thus the vector-potential of the electric-current, in free space surrounding the wire, has for its analogue the velocity of the fluid element, due to a vortex-filament supposed to occupy the place of the current. Many other curious analogies between vortex-motions in fluids and the action of magnets and electric currents have been pointed cut by Sir Wm. Thompson.* Of course it_is possible that these analogies may be merely for- mal, and that they arise from the fulfillment of similar mathematical conditions by both the electric current and vortex-motion in fluids. But whether the relationship shall or shall not ultimately be found to consist in a closer connection than mere formal analogy, one thing is certain. The discoyery of the laws governing vortex- motion in fluids constitutes an era in physical science. The differen- tial equations of the motions of fluids although*handled by such masters as LaGrange, LaPlace, Euler, and Green, had only been in- tegrated on the special assumption of a velocity-potential; which condition we have seen to hold only in the space outside of those portions ot the fluid which are in rotation. It remained for Helmholtz to make the next great step by integrating these equations under the supposition that no velocity-potential exists; and to show that while the establishment of vertex-motion in fluids, is, on the one hand, a consequence of fluid friction, on the other.that when vortex-fila- * Sir Wm. Thompson’s “Papers on Electrostatics and Magnetism.’ RECENT PROGRESS IN THEORETICAL PHYSICS. 991 ments are once set up in a frictionless fluid they are absolutely in- destructible save by the power that originated them. Only an in- finite power can set up vortex movement in a perfect fluid without friction,and only an infinite power can destroy such motion when once set up. On this idea Sir Wm. Thompson has based his famous spec- ulation that the atoms of matter are merely so many vortex-rings of variable but definite shape for each elementary kind of matter. Such rings possess all the qualities usually attributed to the atoms of. matter, being absolutely impenetrable, and possessing when set in vibration that characteristic periodicity of vibration which the spec- troscope shows to be the case with the atoms of the elements of matter, As Professor Tait says, ‘* not only can these vortex-rings in a perfect fluid not be cut, but we cannot even so much as get at them, to try to cut them.” They rebound from the sharpest edge. Thus it will be seen that there is at least an analogy between vor- tex-filaments in a perfect fluid and magnetism caused by electric currents. The equations of the electro-magnetic field show this, when compared with the equations of vortex filaments. But this is by no means all. In Faraday’s beautiful experiment of the rotation of the plane of polarized light when passing through a medium which is under the influence of magnetic strain, we have a means of testing whether any- thing of the nature of rotation of small elements, either of gross mat- ter or of some incompressible frictionless fluid be going on in the magnetic field. For, if the magnetic force be in any way the con- sequence of such minute rotations, we might expect a@ priori that the minute motions which cause light, at least those circular oscil- lations that constitute circularly polarized light, could in some way be compounded with the minute rotations involved in magnetic phenomena, and be influenced by them. And thus, although we could not directly observe these vortex movements by the senses, we yet might have the means of exploring the magnetic field, by an agent of almost superhuman delicacy in the shape of the oscilla- tions of light. The possibility of the compounding of the mag- netic rotations with those of circularly polarized light, which con- stitutes the explanation Thompson gives of the Magnetic Rotation of Polarized Light, I will take up next.* * This subject was fully treated in the paper as read before the Academy, but its publication is delayed until cuts can be prepared to illustrate it, and Greek type obtained for the formulz. nd Be re mh me 3 h a with 1 Ue sige ae - PROCHEDINGS OF THE OLA 1G NEW SINCE FEBRUARY, 1874. Report of the President. His Excertency Harrison Lupineron, Governor of Wisconsin: SIR:—Since the date of my last report, the Wisconsin Academy of Sciences, Arts, and Letters has steadily advanced in prosperity. It has not made large additions to its permanent fund, nor greatly increased the list of its working members. But the very consid- erable number of scholars and scientists holding memberships, have devoted themselves with increased zeal to the work of the work of the Academy in original investigation, and have produced payers embodying the results of their inquiries which are of cons:derable value, and must yet more favorably commend the Academy to the respect and confidence of the literary and scientific public. The Academy is no longer an experiment. The past six years have demonstrated; first, that Wisconsin embraces a large number of persons both competent and experienced as laborers in various fields of research and investigation; and secondly, that it is posible and easy, through such an organization as this, to hold them to- gether in systematic and profitable oc-operation, for the advance- ment of the arts and sciences. as well as for the intellectual and social progress of the commonwealth. The present volume of transactions will be found to consist largely of papers in the Department of the Natural Sciences. While all are interesting and valuable, it will appear upon exami- nation that some of these are the fruit of extensive observations in the field, as well as of laborious investigations in the laboratory. Since it is this department which so directly touches the material progress of the State, and which would also especially contribute to the establishment of advantageous relations with kindred organ- izations in all parts of the world, it will be to the friends and pat- 15——-w as 226 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. rons of the academy a ground of satisfaction that its development has been characterized by so strong a bent in this particular direc- tion. In the other departments there have been fewer laborers. Still, it will not escape observation that many of the best thinkers and investigators of the State have given to the Academy the results of careful and protracted inquiry in the several feids embraced within the broad domain of the Academy. In this country, Speculative Philosophy finds comparatively lit- tle recognition as a means of scientific progress, and is therefore without the cultivation it merits. Nevertheless, it is not without creditable representation in this, as it was not in our last volume ~ of Transactions. The Department of Social and Political Sciences embraces so vast a range of subjects for inquiry, and appeals so directly and strongly tothe public mind that a more rapid growth of it might reasonably have been expected. It is not wanting in activity, however, and gives promise of more substantial progress in the future, through the reinforcements hkely to come to it from the learned professions and from special students of Social Philosophy, and of statesman- ship. The Department of Letters is also in need of reinforcements. The contributions heretofore made have been both interesting and valuable, however; some of them justly insuring commendation from distinguished European savans. At the late annual meeting, the department of the arts was di- vided into the ** Department of Practical Arts” and the ‘“* Depart- ment of the Fine Arts.” Neither of these has yet received much development. Still itis believed that the creation of separate de- partments will prove advantageous. ‘There are numerous invent- ors, scientific artizans and practical observers and experimenters in Wisconsin, who, if brought together within the pale of. a depart- ment of the Academy exclusively devoted to the progress of the useful arts, would make it eminently successful. So, too, there are artists and cultivators of art in sufficient number, if united, to make the Department of the Fine Arts at once a means of mutual advan- tage, and of increasing art culture in the State, as well as of initia- ting the formation at the seat of the Academy, and in joint con- nection with it and the State University, of a alley of Art, coupled with an Academy of Design. REPORT OF THE PRESIDENT. _ 997 Leaving out of view the present paucity of artists within our own State, and the difficulty, supposed to be necessary, of finding adequate patronage outside of the cities, there could hardly be found anywhere in this country, a more suitable or more desira- ble spot for an institution of the kind suggested. And even the objection alluded to would affect only such artists as are limited to one or two of the several branches of art. The landscape painter, the historic artist, and the idealist in either painting or sculpture, wouldeach find themselves happily placed here, in an exception- ally pure atmosphere, in a region remarkable for its healthfulness, and in the midst of scenery unparalled for beauty. As this is a matter in which the Academy, the State University, artists of the Northwest, and the friends of Art generally, must all feel an inter- est, we are not without hope that practical results of some im- portance will follow the effort thus systematically begun. The Library of the Academy is under the management of a com- petent and zealous librarian, through whose efforts it must make steady, if not rapid growth. As was stated in my first report (for 1870-72) it has not been, and is not now, the purpose of the Academy to build up a general Jibrary, separate and distinct from that of the State Historical Society, which is fast hecoming the great general library of the State, but rather to supplement the forces therein at work by efforts to make collections especially rich in the publications of learned, scientific and other kindred socie- ties and associations of all countries, and in works generally which properly belong to the several departments embraced within the Academy, and which are not likely to be supplied otherwise. Large results in this direction have not been accomplished, but the agencies are at work, and will yield fruits more abundant as the years goon. Regarding the Academy from this standpoint, it is quite desirable that its Transactions should be published annually, instead of biennially; for such more frequent publication would render it-easier to effect exchanges with other institutions of like character, as well as with the periodical press of the world. The Museum of the Academy is making more growth than out- wardly appears. For, owing to the connection of several of the members most active in making collections, with the Geological Survey, now in progress, much of the material which would other- wise have come directly to the Museum, has very naturally and 228 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. properly gone to the State Geologist, for classification, and has not as yet reached its final destination under the law creating the sur- vey, which provides that specimens of all the material collected during its progress shall be deposited with the Academy. It may also be remarked that the officers of the Academy are yet expect- ing that large contributions will soon be made to the Museum from the considerable number of private collections heretofore formed within this State. The report of the treasurer, herewith incorporated, sets forth the financial transactions of the Academy for the years 1875 and 1876, together with the condition of its funds ut the date of the last annual meeting, just concluded: WISCONSIN ACADEMY SCIENCE, ARTS AND LETTERS, TREASURER’S OFFICE, Maopison, February 13, 1877. Hon. J. W. Hoyt, President: I haye the honor to report the financial condition of the Academy, as follows: Total amount of fees and dues received from 58 members............. $778 25 Total fees received from 10 life members........00scsececereecccreee 1,000 00 liienesrOnlipiesapdopoccasdoncqossnd 24 770g ooougdos0ecos coer. < 370 00 2,148 25 Total amount disbursed in payment of warrants to date............--- 177 97 Balancerimh treasury. aie cietei\e orelers sinker toa ioleuetei= ie eotereiers here aaa 1,370 28 GEO. P. DELAPLAINE, Treasurer. The following is a list of the papers read since the date or our last publication: ‘Views connected with the Railroad Question,” by Rey. Chas. Caverno. “On Industrial Education,” by Rev. F. M. Holland. “ \ Mastodon found in Racine County,” by Dr. P. R. Hoy. ‘* A Turtle Mound found in Beloit,” by Prof. Eaton. “The Improvement of the Mouth of the Mississippi River,” by ~ Capt. John Nader. The * Elementary Stratification of the Lower Silurian Rocks in South-Central Wisconsin,” by Prof. R. D. Irving. The ‘* Hibernation of the Striped Gopher,” by Dr. P. R. Hoy. “The Law of Embryonic Development the same in Plants as in Animals,” by Dr. I. A. Lapham. “Were the Stoics Utilitarians?” by Rev. F. M. Holiand. “On the Ancient Civilization of America,” by Prof. Nicodemus. REPORT OF THE PRESIDENT. 429 * An Account of Recent Examinations of the Ancient Earthworks in Rock county, Wis.,” by W. P. Clark, Esq. * Drift-notes,” by Prof. Eaton. *Minority or Proportional Representation,” by Rev. F. M. Hol- land. “On the Fishes best suited to stock the small lakes of Wisconsin," ley LDre, TRE Tite Lalo “ Oconomowoc Lake,” by the late Dr. I. A. Lapham. “On United States’ Sovereignty; whence derived and when vested,” by Pref. Alien. “The Barometer in Leveling.” by Capt. Nader. “On River Engineering,’ by Capt. Nader. “The instrument of Exchange,” by President G. M. Steele. “The Inter-convertible Note Scheme,” by EK. R. Leland, Esq. “ The Kaolin of Wisconsin,’ by Professor Irving. “The Revolutionary Movement Among Women,” by Dr. J. W. Hoyt. **An Account of the Aid Rendered by Various Governments to Science and Eilucation,’ by James D. Batler, LL. D. “Geological Reconnoisances in Northern Wisconsin,” E, T. Sweet, M.S. “The Encouragement of Art Culture by the State,” by Dr. J. W. Hoyt. “Some new and Remarkable Features of the Lower Magnesian Limestone, and St. Peter Sandstone in Eastern Wisconsin,” by Prof. T. C. Chamberlain. “ The Origin of the Present-Infinitive-Passive in Latin and Greek,” by Prof. Feuling. “The Significance of Faraday’s Experiment upon the Magnetic Rotatory Polarization of Light; and upon Helmholtz Paper on the Integrals of Vortex Motion; also upon the Theory of Mag- netism,” by Prof. Davies. “On Duplex Telegraphy,” by Chas. H. Haskins. In the confident belief that the Academy has before it a career of great usefulness. and that to this end it will be more and more encouraged by an intelligent public, as well as liberally fostered by the State, I have the honor to be, in its behalf, Very respectfully, TOHIN: Wa, ELON : President. Madison, February, 1876. Report ot the Sechetame SPECIAL MEETING OF THE ACADEMY. SEPTEMBER 16, 1874. The members of the Academy met in their rooms at Ty P. M. The following resolutions were passed: Resolved, That we sincerely lament the death of John Y. Smith, in whom our Society has lost an active and honored member, and the science of political economy one of its most devoted and useful followers. Resolved, That the President of the Academy be requested to appoint a member of the Academy to prepare a sketch of his lite and works Resolved, That these resolutions be published in each of the daily papers of this city, and that the General Secretary be re- quested to forward a copy of these proceedings to the family of the deceased. The President of the Academy eulogised highly the meee of the deceased member. The death of Prof. Peter Engelman, of Milwaukee, was an- nounced by Dr. I. A. Lapham, who pronounced a high elogium upon the scientific character of the deceased. The following resolutions were also passed: Resolved, That in the death of Prof. Peter Engleman the Acade- my has lost a valued member, and the cause of education one of its most active promoters. Resolved, That the President of this Academy is hereby requested to appoint some member to prepare, for the next regular meeting of the Academy, a memoir of his life and labors. Resolved, That these resolutions be published in ie Ee geese of the Academy. The Treasurer of the Academy, G. P. Delaplaine, Esq., aes the attention of members to a remarkable mound, supposed to be very ancient, in the vicinity of the city of Madison. Prof. Nicodemus, of the State University of Wisconsin, Dr. I. A. Lapham, of Milwaukee, Geo. P. Delaplaine, Esq., of Madison, REPORT OF-THE SECRETARY. 931 and Prof. Irving, of the University, were appointed a committee to investigate the mound and furnish to the Academy a report there- on, at an expense to the Academy not exceeding $25.00. JouHn EK. Davtss, General Secretary. FIFTH REGULAR ANNUAL MERTING. First Session. Acaprmy Rooms, Feb. 9, 1875, 74, Pp. u. The fifth annual meeting of the Academy was commenced in their rooms ou Tuesday evening, February 9, 1875, at 74 o'clock; there being a large attendance of members and citizens; the Presi- dent, Dr. J. W. Hoyt, in the chair; the Secretary, Prof. J. H. Davies. absent by reason of severe illness. In the absence of the secretary, Prof. James Haton, of Beloit College, was appointed secretary pro. tem. The treasurer's report was read and referred to an auditing com- mittee consisting of Prof. Nicodemus, Dr. Hoy, and Hiisha Bur- dick, Esq. The librarian’s report was read and accepted. The rules were suspended and Messrs. H. T. Sweet, R. H. Brown, J.T. Dodge, and Charles N. Gregory were elected annual mem- bers. The first paper of the meeting was read by the Rev. Charles Cav yerno, on ‘* Views connected with the Railroad Questicn.” Twenty-three members were present at this meeting of the Academy. Second Session. FEBRUARY 10, 9.45 A. w. During the absence of the President, the chair was occupied by I. A. Lapham, Vice-President of the Academy. The report of the secretary was read. The following papers were read and discussed: On “ Industrial Education,” by Rev. F. M. Holland, of Baraboo. 232 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. “A Mastodon found in Racine County,” by Dr. P. R. Hoy, of Raeine. Dr. Holland called attention to a number of bones of a Mastodon found in Baraboo thirty years ago. A paper was read on “A Turtle Mound in Beloit,” by Prof. Haton of Beloit. E. R. Leland, of Kau Claire, read a memoir upon the late Peter Engelman, of Milwaukee, a member of this Academy. Adjourned till 2:30, p. m. Third Session. Frpruary 10, 2:30, Pp. mu. The Academy met pursuant to adjournment, with a large attend- ance. Dr. I. A. Lapham, Vice-President, in the chair. Papers were read as follows: On the “Improvement of the Mouth of the Mississippi River,” by Capt. Nader. On * The Elementary Stratification of the Lower Silurian Rocks in South-Central Wisconsin,” by Prof. Irving. On “The Hibernation of the Striped Gopher,” and on “The Cato- calue of Racine County,” by Dr. Hoy, of Racine. On “The Law of Embryonic Development, the same in Plants as in Animals,’ by Dr. I. A. Lapham, of Milwaukee. The committee appointed to audit the Treasurer’s Report gave in their report, which was read and accepted. ' The meeting then adjourned till 7:30, p. o. Fourth Session. Frsrvary 10, 7:30 Pp. 1. The Academy met pursuant to adjournment; with a full attend- ance. Prof. 5S. H. Carpenter, Vice President in the chair. Papers were read as follows: * Were the Stoics Utiliturians?” by Rev. F. M. Holland of Bar- aboc. REPORT OF THE SECRETARY. 933 On “ The Ancient Civilization of America,” by Professor Nico- demus, of the University of Wisconsin. “An account of Recent Examinations of the Ancient Earthworks in Rock county, Wisconsin,” by W. B. Clark Esq. * Drift notes” by Prof. James Eaton. SIXTH ANNUAL MEETING. First Session. Acanemuy Rooms, Feb. 8, 1876, 7:30 P. mu. The sixth annual meeting of the Academy was convened in their rooms on Tuesday evening February 8th, 1876, at 74 o'clock; there being a large attendance of members and citizens of Madison; the President, Dr. J. W. Hoyt, in the chair. The minutes of the last previous meeting were read by the Sec- retury and approved. After a few remarks by the President of the Academy, on the general progress and success of the Academy during the year, the reports of the Secretary, Treasurer, and Librarian of the Academy were read, accepted and referred to appropriate committees. The President of the Academy announced that the Hon. George H. Paul, of Milwaukee, Railroad Commissioner for Wisconsin had consented to donate $100 to the Academy, and thereby become a Life Member. The following gentlemen were elected members. For Corresponding Members.—Dr. Joseph Buchanan of Louis- ville, Ky., and 8. W. Burnham Esq., Chicago, F. R. A. 8. London. For Annual Members.—K. i. Woodman, Esq., of Baraboo, Wis.; Prof. W. C. Sawyer, of Appleton, Wis.; Hon. Peter Doyle, Secre- tary of State for Wisconsin; C. H. Haskins, Esq., of Milwaukee, Gen'l. Supt. Northwestern Telegraph Co.; Right Rev. H. R. Welles of Milwaukee, Protestant Episcopal Bishop of Wisconsin; Hon. Harlow 8. Orton, of Madison; Gen. Hi. E. Bryant, of Madison; Hon. S. U. Pinney, of Madison; Hon. J. C. Gregory, of Madison; Rev. John Wilkinson, of Madiscn; Sumuel Shaw, Esq., Principal of High Schoo!, Madison; J. W. Wood, Esq., Baraboo; J. O. Culver, Esq., Madison; S. G. Lapham, Esq., of Milwaukee; E. 8. Searing, 234 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Esq.,0f Madison; Hon. I ©. Sloan, of Madison; Josiah E. Cass, Esq., of Eau Claire; HE. A. Birge, State University; T. G. Atwood, Esq., Albion, Wis; J. W. Stuart, Esq., of Madison. Dr. P. R. Hoy, of Racine, Chairman of the committee appointed to prepare a sketch of the life and character of Hon. I. A. Lapham, LL. D., late Vice President of the Academy, read an exceedingly interesting paper upon the general life and scientific labors of Dr. Lapham. Dr. Hoy feelingly referred to a friendship prolonged for Over thirty years. He summed up the important labors of Dr. Lapham by reading the following letter from Prof. Joseph Henry: SMITHSONION INSTITUTE, U Washington, feb. 3, 1876. § Dr. P. R. Hoy, Raciae, Wis.: : Dear Sir: Your letter was received during a great pressure of business, and 1 now embrace the first opportunity to give ita reply. The action of Congress in regard to the signal service was due to the immediate exertions of Mr. Lapham through the member of Congress from his district, Gen- eral Payne, in setting forth the advantages of the system to the ee inter- ests of the great lakes. Yours very truly, [ Signed. ] JOSEPH HENRY. Secretary. E. R. Leland, Hsq., of Eau Claire, spoke very eloquently of the virtues, public and private, of the deceased Vice- Been whom he had known intimately for many years. Remarks were also made by Prof. T. C. Chamberlain, of Beloit, Dr. Lapham’s successor as Director of the Geological Survey, of the State, and R. D. Irving, Professor of Geology in the University of Wisconsin. . Dr. S. H. Carpenter, Professor of Logie and English Literature im the University of Wisconsin, read an admirable review of the life, mental characteristics, and writings of the late Hon. John Y. Smith. Dr. Carpenter showed him to be a man of unusual power of mind and great clearness of thought. Prof. W. F. Allen, Pro- fessor of Latin and History in the University of Wisconsin, also added his testimony to the statements made in Dr. Carpenter’s pa- per. tes A paper upon “ Minority or Proportional Representation,” by Rev. F. M. Holland, of Baraboo, was then read by Prof. Allen. Adjourned till Wednesday morning, 9 a. m. -REPORT OF THE SECRETARY. 935 Second Session. WEDNESDAY Morninag, 94, o'clock, February 9, 1876. The Academy met pursuant to adjournment; the President Dr. J. W. Hoyt in the chair. The following papers were then read: “On the Pre-Historic Copper Implements found in Wisconsin,” by James D. Butler, LL. D., of Madison.” This paper was read by Professor W. W. Daniells, of the State University of Wisconsin. “On the Fishes best suited to stock the small lakes of Wisconsin, by Dr. P. R. Hoy, of Racine. Dr. Hoy also read a paper on the Oconomowoe Lakes,” prepared by Dr. I. A. Lapham, just before his death. “United States Sovereignty—wheunce derived and where vested,” by Professor W. F. Allen, of the State University.” “The Barometer in Leveling,” by Captain John Nader. “On River Hngineering,” a translation from the German, by Captain John Nader, of Madison. Adjourned till 25 P. M. Third Session. Wepnespay AFrrernoon, 24 P. M.—Feb. 9, 1876. The Academy met pursuant to adjournment, the President Dr. J. W. Hoyt in the chair. The following papers were then read and discussed: ‘‘On the Instrument of Exchange,” by G. M. Steele, DD., President of Lawrence University. “The Interconvertible Note Scheme,” by E. R. Leland, Esq., of Eau Claire. “On Kaolin in Wisconsin,” by Professor R. D. Irving, of the University of Wisconsin. The Academy then adjourned until 7 o’clock P. M. Fourth Session. Frsruary 7th, 74 o'clock P. M. The Academy met pursuant to adjournment, the president Dr. J. W. Hoyt in the chair. Dr. P. R. Hoy then made some popular remarks on the ‘* General Classification of Animals.” 236 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Dr. J. W. Hoyt then read a carefully prepared paper on “ The Revolutionary Movement among Women.” Adjourned 9 A. M. Fifth Session. TuurspDay, February 10, 9 A. M. The Academy met pursuant to adjournment. The President Dr. J. W. Hoyt in the chair. The tollowing papers were then read and discussed. “An Account of the aid rendered by Various Governments to Sci- ence and Education,’ by James D. Butler, LL. D. * Geological Reconnoisances in Northern Wisconsin,” by Mr. E. T. Sweet, Assistant on the Geological Survey. “The Encouragement of Art Culture by the State,” by Dr. J. W. Hoyt. ‘*On some new and remarkable features of the Lower Magnesian Limestone, and St. Peter’s Sandstone in Eastern Wisconsin, by Prof. T. C. Chamberlin, Director of the Geological Survey. Adjourned till 2 o’clock P. M. Sizth Session. Monpay, February 10, 2 o’clock P. M. Academy met pursuant to adjournment. President J. W. Hoyt in the chair. The following papers were then read and discussed. “The origin of the Present-Infinitve-Passive in Latin and Greek.” by Prof. J. B. Feuling Ph. D., of the University of Wisconsin. “The Significance of Faraday’s Experiment upon the Magnetic Rotatory Polarization of Light,” by Prof. J. EH. Davies, M. D., of the State University. “ Helmholtz’ Paper upon the Integrals of Vortex Motion; and the significance of these Integrals in the theory of Magnetism,” by Prof. Davies. “On Duplex Telegraphy,” by Charles H. Haskins, General Superintendent of the Northwestern Telegraph Company, Milwau- kee. The reading of the papers prepared for this meeting having been concluded, the Academy prepared to ballot for the election of offi- cers for the next three years. REPORT OF THE SECRETARY. 937 The following gentlemen were unanimously elected. For President, P. R. Hoy, M. D. Racine. For General Secretary, J. HE. Davies, M. D., Madison. For Vice President of Department of Speculative Philosophy, 8. H. Carpenter, LL. D., Madison. For Vice President of Department of Natural Science, Prof. T. C. Chamberlin, Beloit. For Vice President of the Department of Social and Political Sci- ences, Rev. G. M. Steele, D. D. Appleton. For Vice Presidentof the Department of the Mechanic Arts, Hon. J. I. Case Racine. For Vice President of the Department of Letters, Rev. A. L. Cha- pin, D. D. Beloit. For Vice President of the Department of the Fine Arts, Dr. J. W. Hoyt, Madison. For Treasurer Geo. P. Delaplaine, Esq., Madison. For Director of Museum E. T. Sweet, M.E., Sun Prairie. For Librarian, Charles N. Gregory, M. S., Madison. After the transaction of other minor business, the Academy ad~ journed sine die. . JouNn EK. Davirs, General Secretary. | Report of the Librarian. To the President of the Wisconsin Academy of Sciences, Arts and Letters: Srr:—I have the honor to report the receipt of the following contributions to the library of the Academy, which have been for- warded by the courtesy of the Smithsonian Institute, Washington IDB Oe Bremen Natural Science Society.—Vol. 3, parts 1 and 2, 1872. Vol. 4, part 4, 1875. Vol. 4, part 1, 1876. Supplement No. 4, 1874-5, Supplement No. 5, 1876. Amiens Linnean Society of the North of France—Monthly bul- letins from May, 1875 to June, 1876, inclusive. . Munich Royal Bavarian Academy of Science.—Transactions for 1875, parts 1 and 2. Two pamphlets on Chemistry. One pamphlet on Schelling. i Harlem Netherlands Society for the Fostering of Industry.— Transactions for 1474, transactions for 1875, and six pamphlets. Lyons Academy of Science, Belles-Letters and Arts——Memoirs Volume 16, for 1874-5. Dresden Society of Natural History.—Transactions for 1875. Vienna Imperial Royal Zoological and Botanical Society.—Trans- _ actions Volume 25, for 1876. Brunn Natural Historical Society —Proceedings Volume 13, 1875. Catalogue of Library 1874. Halle Journal of the Natural Sciences by Dr. Giebel.—Volumes 11 and 12, 1875. : Bern, Swiss Society of Natural History.—Proceedings for 1876. Menaoirs. Bern, Society of Natural Science at Bern.—Transactions 1874, 1875. London Royal Society.—Volume 23, of Proceedings. Nos. 153 to 163 inclusive. ‘On the Tides of the Arctic Seas,” from Philo- sophical Transactions of Royal Society. Neuchatel, Society of Natural Science.—Bulletin received March REPORT OF THE LIBRARIAN. 939 Natural Historical Society of Prussian Rhineland and Westpha- lia.—Transactions for 30th year 1874, aad 31st year 1875. Konigsberg. Publications of Society of Physical Heconomy.— Parts one and two, 1873 and 1874. Gottingen, Royal Society of Learning etc.—Transactions for 1875. Harlem, Archives of the, “* Musee Teyler’—Vol. 1, 2 and 3, and 1st part of vol. 4. Amsterdam, Royal Academy of Science—Publications from 1865 to 1876 iueclusive, in 2! pamphlets. Belgium, Royal Society of Botany—History of Roses, by Francis Crepin; extract from Bulletin. Danzig, Natural Historical Society; Transactions—Vol. 3, part 4. Freiburg, Society of Natural History; Transactions—V ol. 6, part 4. St. Petersburg, Physical Central Observatory—Annals for, 1874. Instructions for Meteorological stations, by H. Wilde. Andennatt, Swiss Society of Natural Philosophy—Report 1874 and 1875. Bamberg, Society of ‘Natural Philosophy—Tenth report, 1874 and 1874. Stockholm, The Royal Swedish Academy of Science—Memoir by S. Loren on ‘* Hchinoidea,”’ 1875. Transactions for 1872. t1th volume of Synopsis of Transactions, 1875 and 1876. Appendix to Transactions, volume 3, part 1. List of Swedish and Norse mem- bers May, 1876. I haye also received, by the kindness of Professor Alexander Agassiz, Cambridge, Mass., Museum of Comparative Zoology at Harvard College—Bulletin Volume 3, Nos. 11 to 16; volume 4, No. 10. Also from the State Library of New York, 87th Report of the Regents of the State of New York. Report of New York State Library for 1875. Report of New York State Museum of Natural History. Biographical sketch of Increase A. Lapham, read before the Old Settlers Club; by the kindness of Mr. Seneca Lapham, of Milwaukee. All of which is most respectfully submitted. With great respect, CHARLES N. GREGORY, Librarian. no ya List of Officers and Members OF THE ACADEMY, 1876. 16——_ was GENERAL OFFICERS § ACADEMY. PRESIDENT: Dr. P. R. HOY, Racine. VICE-PRESIDENTS: Dr. S. H. CARPENTER, - - < = = Madison. Pror. T. C. CHAMBERLIN. - - - - - - Beloit. Rey. G. M. STEELE, D. D. - - - - - Appleton. Hon. J. I. CASE, - - - - = - - Racine. REywA. Ll. CHAPIN, D. D.. - - = = - Belvit. Dr. J. W. HOYT, - - = s : - Madison. GENERAL SECRETARY: Pror. J. . DAVIES, M. D., University of Wisconsin. TREASURER: GEO. P. DELAPLAINE, Esq., Madison. DIRECTOR OF THE MUSEUM: KE. T. SWEET, Esq., Sun Prairie. LIBRARIAN: | CHARLES N. GREGORY, Madison. COUNSELORS EX-OFFICIO: HIS EXCELLENCY THE GOVERNOR OF THE STATE. THE LIEUTENANT GOVERNOR. THE SUPERINTENDENT OF PUBLIC INSTRUCTION. THE PRESIDENT OF THE STATE UNIVERSITY. THE PRESIDENT OF THE STATE AGRICULTURAL SOCIETY. THE SECRETARY OF THE STATE AGRICULTURAL SOCIETY. OF FICERSOF THE DEPART Mia DEPARTMENT OF SPECULATIVE PHILOSOPHY. President.—S. H. Carpenter, LL. D., Madison. Seeretary.—Rev. F. M. Holland, Baraboo. Counsellors.—Dr. John Bascom, President University of Wiscon- sin; President Oliver Arey, Whitewater, and Rev. A. O. Wright, Fox Lake. DEPARTMENT OF NATURAL SCIENCES. President.—Prof. T. C. Chamberlin. Beloit. Secretary.—Prot. James H. Haton. Beloit. Counsellors.—Prof. W. W. Daniells. of the University of Wis- consin; Prof. Foye, of Appleton, and Prof. Thure Kumilein, of Albion. DEPARTMENT OF SOCIAL AND POLITICAL SCIENCES. President.—Rev. G. M. Steele, D. D. Appleton. Secretary.—H. R. Leland, Esq., of Han Claire. Counsellors.—Dr. HE. B. Wolcott, Milwaukee; Rev. Charles Ca- verno, Lombard, Ill., and J. B. Parkinson, of Madison. DEPARTMENT OF THE MECHANIC ARTS. President.—Hon. J. I. Case, Racine. Secretary.—Prof. W. J. L. Nicodemus, of the University of Wis- consin. Counsellors.—Charles H. Haskins, of Milwankee; Hon. J. Mitchell, of Milwaukee, and Capt. John Nader, of Madison. DEPARTMENT Of THE FINE ARTS. President.—Dr. J. W. Hoyt, Madison. Secretary.—Hon. J. EK. Thomas, of Sheboygan. Counsellors.—Mrs. S. F. Dean, Madison; J. R. Stuart Esq., Mad- ison, and Mrs. H. M. Lewis, Madison. DEPARTMENT OF LETTERS. President.—Rev. A. L. Chapin. D. D., Beloit. Secretary.—Prof. J. B. Feuling, of the University of Wisconsin. Counsellers.—Prof. W. I*. Allen, of the University of Wisconsin: Piof. Emerson, Beloit College, and Hon. L. C. Draper, Madison. MEMBERS OF THE ACADEMY. ANNUAL MEMBERS. Allen, W. F., A. M., Professor of Latin and History in tne University of Wis- consin. Arey, Oliver, A. M., President State Normal School, Whitewater, Wis. Atwood, T. G., Esq., Albion. Wis. Bascom, John, LL. D., President of the University of Wisconsin. Bashford, R. Mo) A. M. , Madison, Wis. Ballentine, W. G. , Ripon, Wis. Butler, J. B., Die Dy. Madison, Wis. Bryant, KE. D.. Hon., Madison, Wis. Birge, EH. A., A. M., Instructor in Zoology in the University of Wisconsin. Carpenter, s. JElS5 ite D., Professor of English Literature and Logic, in the Uni- versity of Wi isconsin. Chamberlin, T. C., A. M.. Professor of Natural History Beloit College, and Di- rector of the Geological Survey of Wisconsin. Caverno, Charles, Rev.. Lombard, Ll. Chapin, A. L., D. D., President Beloit College, Beloit, Wis. Charlton, E. A., A. M., President State Normal School, Platteville, Wis. Cole, Theo. L., M. S., LaCrosse, Wis. Copeland, H. E., Whitewater. Conover, O. M., A. M., Madison, Wis. Cass, Josiah E., Eau Ch: aire, Wis. Daniells, W. W., Wile Shoe IP rof. of Chemistry in the University of Wiscousin. Davies, a Ky., A. M. M. D., Prof. of Astronomy and Physics in the University of Wisconsin. Delaplaine, Geo. P., Madison, Wis. De La Matyr, W. A., Mazomanie, Wis. Dudley, Wm, Madison, Wis., Durrie, D. S., Librarian Wisconsin State Historical Society. Doyle, Peter Hon. ., Secretary of the State of Wisconsin. Eaton, James H., Ph. D., Prof. Chemistry Beloit College, Beloit, Wis. Feuling, J. B., bh. D., Prof. Comparative Philology and Modern Languages in the University of Wisconsin. Foye, J. C., A. M., Prof. Physics, Lawrence University, Appleton, Wis. Gregory, J. C., Madison, Wis. Gregory, Chas. N. A. M., Madison, Wis. Holland, Ph. M. Reyv., A. M., Baraboo, Wis. Hauser, igs Rey., A.M. , Milwaukee, Wis. Hawley, C T., Milwaukee, Wis. Holton, E. D. ‘Hon., Milwaukee, Wis. Hoy, P. BK. MoD. President Wisconsin Academy Sciences, Arts, and Letters, Racine, Wis. Hoyt, J. W., M. D., Madison, Wis. Haskins, C. nae General Superintendent Northwestern Telegraph Company, Milwaukee, Wis. 246 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Irving, R. D., A. M.M.E., Prof. of Geology and Mining in the University of Wis- consin. Kumlein, Thure, Prof. Albion College, Albion, Wis. Kingston, J. T., Necedah, Wis. Kerr, Alex., A. M., Prof. Greek in the University of Wisconsin. Leland, 1B Late Ean Claire, Wis. Lapham, Se Milwaukee, Wis. Marks, Solon, M. D., Milwaukee, Wis. Mason, R. Z., LL. D., Appleton, Wis. Nicod emus, W.J.L.,C. i., Prof. of Civil and Mechanical Engineering in the University of Wisconsin. Nader, John, C. E., Madison, Wis. Orton, Harlow Ss Hon. ss Madison, Wis. Parkinson, J. By oA: ii tah Madison, Wis. Pradt, J. B. Rey., A. M., Madison, Wis. Preusser, Charles, President Natural History Society, Milwaukee, Wis. Pinney, 8. U, Fon. , Madison, Wis. Reed, Geo. ; Hon. ., Manitowoe, Wis. Roby, H. W., Milwaukee, Wis. Reade, E. D., C. E., Milwaukee, Wis. Steele, Rev. Geo., M., D.D., President of Lawrence University, Appleton, Wis. Shipman, S. V., Chicago, lil. Smith, Wm. E. Hon., Milwaukee, Wis. Searing, Edward, A, M., Superintendent of Public Instruction for the State of Wisconsin. Sawyer, W. C., Prof. Lawrence University, Appleton, Wis. Shaw, Samuel, "A. M., Principal of High School and City Superintendent of Pub- lie Schools ,M adison, Wis. Stuart, J. R.A. M. Madison, Wis. Sloan, iC! Hon., Madison, Wis. Whitford, Wei. AC Me, President of Milton College, Milton, Wis. Wright, A. O. Rev.. Fox Lake, Wis. Welles, E. R., Rt. Rev. S. T. D., Episcopal Bishop of Wisconsin. Wilkinson, John. Rev. A. M., Madison, Wis. Wood, J. W., Barahoo, Wis. Woodman, E. K., Bar aboo, Wis. CORRESPONDING MEMBERS. Andrews, E. B., LL. D., Prof. Marietta College, Ohio. Andrews, dmund, A.M. M. D., Prof. Chicago 1 Medical College, Chicago, 11. Biossom, T., M. E., School of Mines, Columbia College, New York. Bridge, Norman, M. D., Chicago, Ill. Brinton, JG M. 1D Philadelphia, Par Buchanan, Joseph, M_D., Louisville, Kentucky. Burnham, 8. W., F. R. A. S., Chicage, Ill. Carr, E. S., M. D., Superintendent Public Instruction, California. Ebener, F., Ph. D., Baltimore, Md. Freer, J. C., M. D., President Rush Medical College, Chicago, Ill. Gatechell, H. P., M. D., Kenosha, Wis. Gilman, D. C., President John Hopkins’ University. Gill, Theo., M D. , Smithsonian Institution, Washington, D. C. Hopkins, KF. Was M. D., Baton Rouge, La. Haldeman. 8. Se LL. D., Prof. University of Pennsylvania, Chickis, Pa. Horr, Asa, M. Da President Iowa Institute of Arts and Sciences, Dubuque, I iowa. Harris, WT, iGiUID. , st. Louis, Mo. MEMBERS OF THE ACADEMY. IAT Hubbell, H. P., Winona, Minn. Jewell, J. S., A. M. M. D., Evanston, Il. Morgan, L. H., LL. D., Rochester, Il. Marcy, Oliver, LL. D., Prof. Northwestern University, Evanston, Ill. McCabe, L. D., D. D., Prof. Wesleyan University, Delaware, Ohio. McAllister, J. H., Philadelphia, Pa. Newberry, J. S., LL. D., Prof. Columbia College, New York. Orton, E., A. M., Prestdent Antioch College, Yellow Springs, Ohio. Porter, W. B., Prof., St. Louis. Mo. Le Barron, Wm., State Entomologist, Geneva, New York. ao T. H., Director of the Astronomical Observatory of the University of nicago. Shaler, N. S., A. M., Professor Harvard University, Cambridge, Mass. Schele, De Vere M., LL. D., Prof. University of Virginia, Charlotteville, Va. Thornton, J. Wingate, Boston, Mass. Trumbull, J. H., LL. D., Hartford, Conn. Verrill, A. E., A. M., Prof. Yale College, New Haven, Conn. Van De Warker, Eli, M. D., Syracuse, N. Y. Seon: James, A. M., Director of the Astronomical Observatory at Ann Arbor, Tichigan. Whitney, W. D , Prof. Yale College, New Haven, Conn. Winchell, Alex. LL. D. Chancelor Syracuse University, Syracuse, N. Y. LIFE MEMBERS. Case, J. I., Hon., Racine, Wis. Dewey, Nelson, Ex-Governor of Wisconsin, Madison, Wis. Hagerman, J. J. Esq. Milwaukee, Wis. Hoyt, J. W., M. D., Madison Wis. * Lapham, I. A. LL. D, Milwaukee, Wis. Lawler, John, Esq , Prairie du Chien, Wis. Mitchel!, J. L., Hon., Milwaukee, Wis. Noonan, J. A. Esq., Milwaukee, Wis. Paul, G. H., Hon., Milwaukee, Wis. Thomas, J. E., Hon. Sheboygan Falls, Wis. Thorpe, J. G., Hon., Eau Claire, Wis. White, S. A., Hon., Whitewater, Wis. MEMBERS DECEASED SINCE THE ORGANIZATION OF THE ACADEMY IN 1870. Rt. Rev. Wm. E. Armitage, 8. T. D., Bishop of Wisconsin, and late Vice-Presi- dent of the Academy of Sciences, died December 7, 1873. Prof. Peter Engelmann, Milwaukee, Wisconsin. : : J. W. Foster, LL. D., late Professor in the University of Chicago, Chicago, Il. J. A. Lapham, LL. D., Milwaukee, Wisconsin, First Secretary Wisconsim Academy Science Arts and Letters. j ; t Wm. Stimpson, M. D., late Secretary Chicago Academy of Sciences, Chicago, Illinois. Hon. John Y. Smith, Madison, Wisconsin. Hon. A. S. McDill, M. D., Madison, Wisconsin. RRR aber arian Wi ea ks el * Deceased. Za CHARTER, CONSTITUTION AND BY-LAWS . OF THE Academy of Sciences, Arts and Letters, OP WISCONSIN With the Amendments thereto, up to February, 1876. CHARTER: AN ACT TO INCORPORATE THE “WISCONSIN ACADEMY OF SCIENCES ARTS AND LETTERS. The people of the State of Wisconsin, represented in Senate and Assembly, do enact as follows: Section. 1 Lucius Fairchild, Nelson Dewey, John W. Hoyt, Increase A. Lap- ham, Alexander Mitchell, Wm. Pitt Lynde, Joseph Hobbins, 4. B. Wolcott, Solon Marks, R. Z. Mason, G. M. Steele, T. C Chamberlin, James H. Eaton, A. L. Chapin, Samuel Fallows, Charles Preuser, Wm. E. Smith, J. C. Foye, Wm. Dud- ley, P. Englemann, A. 8. MeDill, John Murrish, Geo. P. Delaplaine, J. G. Knapp, 8. V. Shipman, #&dward D. Holton, P. R. Hoy, Thaddeus C. Pound, Charles E. Bross, Lyman C. Draper, John A. Byrne, O. R. Smith, J. M. Bingham, Henry Betz, Li. Breese, Thos. S. Allen, S.S. Barlow, Chas. R. Gill,C. L. Harris, George Reed, J. G. Thorp, William Wilson, Samuel D. Hastings, and D. A. Bald- win, at present being members and officers of an association known as ‘‘ The Wis- consin Academy of Sciences, Arts, and Letters,’”? located at the city of Madison, to- gether with their future associates and successors forever, are hereby created a body corporate by the name and style of the ‘- Wisconsin Academy of Sciences, Arts, and Letters,’’ and by that name shall have perpetual succession; shall be capable in law of contracting and being contracted with, of suing and being sued, of pleading and being impleaded in all courts of competent jurisdiction; and may do and perform such acts as are usually performed by like corporate bodies. SectTron 2. The general objects of the Academy shall be to encourage investiga- tion and disseminate correct views in the various departments of science, literature and the arts. Among the specific objects of the academy shall be embraced the following: 1. Researches and investigations in the various departments of the material, meta- physical, ethical, ethnological and social sciences. 2. A progressive and thorough scientific survey of the State, with a view of determ- ining its mineral, agricultural and other resources. 3. The advancement of the useful arts, through the applications of science, and by the encouragement of original invention. 4. The encouragement of the fine arts, by means of honors and prizes awarded to artists for original works of superior merit. 5. The formation of scientific, economical and art museums. 6. fhe encouragement of philological and historical research, the collection and preservation of historic records, and the formation of a general library. 7. The diffusion of knowledge by the publication of original contributions to science, literature and the arts. Suction 3, Said Academy may have 2 common seal and alter the same at pleas- ure; may ordain and enforce such constitution, regulations and by-laws as may be necessary, and alter the same at pleasure; may receive and hold real and personal property, and may use and dispose of the same at pleasuty; provided, that it shall not divert any donation or bequest from the uses and objects proposed by the donor, and that none of the property acquired hy it shall, in any manner, be alienated other than in the way of an exchange of duplicate specimens, books, and other effects, with similar institutions and in the manner specified in the next section of this act, with- out the consent of the legislature. 252 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Section 4. It shall be the duty of the said Academy, so far as the same may be done without detriment to its own collections, to furnish, at the discretion of its offi- cers, duplicate typical specimens of objects in natural history to the University of Wisconsin, and to the other schools and colleges of the State. Ssecrion 5. It shall be the duty of said Academy to keep a careful record of all its financial and other transactions, and, at the close of each fiscal year, the Presi- dent thereof shall report the same to the Governor of the State, to be by him laid before the Legislature. Sec7ion 6. The constitution and by-laws cf said Academy now in force shall govern the corporation hereby created, until regularly altered or repealed; and the present officers of said Academy shall be officers of the corporation hereby created, until their respective terms of oflico shall regularly expire, or until their places shall be otherwise vacated. “ Secrion 7. Any existing society or institution having like objects embraced by said Academy, may be constituted a departinent thereof, or be otherwise connected therewith, on terms mutually s»tisfactory to the governing bodies of the said Acade- my and such other society or institution. Section 8. For the proper preservation of such scientific specimens, books and other collections as suid Academy may make, the Governor shall prepare such apartment or apartment in the Capitol as may be so occupied without inconveni- ence to the State. : Secrion 9. This act shall take effect and be in force from and after its passage. Approved March 16, 1870. CONS TLV RIO: NAME AND LOCATION. SecTION 1. This association shall be called ‘“‘ The Wisconsin Academy of Sciences, Arts and Letters,’’ and shall be located at the city of Madison. GENERAL OBJECTS. Section 2. The general object of the Academy shall be to enconrage investiga- tions and disseminate correct views in the various departments of Science, Litera- ture and the Arts. DEPARTMENTS. Section 38. The Academy shall comprise separate Departments, not less than three in number, of which those first organized shall be: Ist. The Department of Speculative Philosophy— Embracing: Metaphysics; Ethics. 2@. The Department of the Social and Political Sciences— Embracing: Jurisprudence; Political Science; Education; Public Health; Social Economy. 3d. The Department of the Natural Sciences— Embracing: The Mathematical and Physical Sciences; Natural History; The Anthropological and Ethnological Sciences, 4th. The Department of the Arts— Embracing: The Practical Arts; The Fine Arts. - 5th. The Department of Letters— Embracing: Language; Literature; Criticism ; History. 254 WISCONSIN ACADEMY SCIENCES, ARTS, AND LEITERS. Section 4. Any branch of these Departments may be constituted a section; and any section or groupe of sections may be expanded into a full department, whenever such expansion shall be deemed important. Section 5. Any existing society or institution may be constituted a Department, on terms approved by two-thirds of the voting members present at two successive regular meetings of the Academy. SPECIAL OBJECTS OF THE DEPARTMENTS. Section 6. The specific objects of the Department of Sciences shall be: 1. General Scientific Research. 2. A progressive and thorough Scientific Survey of the State, under the direction of the Officers of the Academy. 3. The formation of a Scientific Museum. 4. The Diffusion of Knowledge by the publication of Original Contributions to Science The objects of the Department of the Arts shall be: 1. The Advancement of the Useful Arts, through the Applications of Science and the Kncouragement of Original Invention. 2. The Encouragement of the Fine Arts and the Improvement of the Public Taste, by means of Honors and Prizes awarded to Works of Superior Merit, by Original Contributions to Art, and the formation of an Art Museum. The objects of the Department of Letters, shall be: The Encouragement of Philological and Historical Research. The Improvement of the English Language. The Collection and Preservation of Historic Records. The Formation of a General Library. LCOS MEMBERSHIP. ‘ Section 7. The Academy shall embrace four classes of governing members who shall be admitted by vote ot the Academy, in the manner to be prescribed in the By-Laws: Ist. Annual Members, who shall pay an initiation fee of five dollars, and there- ° after an annual fee of two dollars. 2d. Members for Life, who shall pay a fee of one hundred dollars. 3d. Patrons, whose contributions shall not be less than five hundred dollars. Ath. Founders, whose contributions shall not be less than the sum of one thous- and dollars. Provision may also be made for the election of Honorary and Corresponding Members,*as may be directed in the By-Laws of the Academy. MANAGEMENT. Srection 8. The management of the Academy shall be entrusted to a General Council; the immediate control of each Department to a Department Council. The General Council shall consist of the officers of the Academy, the officers of the Departments, the Governor and Lieutenant Governor, the Superintendent of Public Instruction, and the President of the State University, the President and Secretary of the State Agricultural Society, the President and Secretary of the State Histori- cal Society, Counselors ez-officiis, and three Counselors to be eleccted for each De- partment. The Department Councils shall consist of the President and Secretary of the Academy, the officers of the Department, and three Counselors to be chosen by the Department. OFFICERS. Srcrion 9. The officers of the Academy shall be: a President, who shall be ez- officio President of each of the Departments; one Vice-President for each Depart- ment; a Geneial Secretary; a General Treasurer; a Director of the Museum, and a General Librarian. Srcrron 10. The officers of each Department shall be a Vice-President, who shall be ex-officio a Vice-President of the Academy; a Secretary and such other offi- cers as may be created by the General Council. CONSTITUTION AND BY-LAWS. 255 Section 11. The officers of the Academy and the Departments shall hold their respective offices for the term of three vears and until their successors are elected. Secrion 12. The first election of officers under this Constitution shall be by its members at the first meeting of the Academy. Section 13. The duties of the officers and the mode of their election, after the first election, as likewise the frequency, place and date of all meetings, shall be pre- scribed in the By-Laws of the Academy, which shall be framed and adopted by the General Council. Suction 14. No compensation shall be paid to any person whatever, and no ex- pence ocurred for any person or object whatever, except under the authority of the ouncil. RELATING TO AMENDMENTS. Srcrion 15. Every proposition to aiter or amend this constitution shall be sub- mittted in writing at a regular meeting; and if two thirds of the members present at the next regular meeting vote in the affirmative, it shall be adopted. AMENDMENTS TO THE CONSTITUTION. Amendment to Section 8: ‘‘ The Department of the Arts shall be hereafter di- vided into the Department of the Mechanic Arts and the Department of the Fine Arts.’? i Passed February 14, 1876. BY-LAWS. ELECTION OF MEMPERS. 1. Candidates for membership must be proposed in writing, by a member, to the General Council and referred to a Committee on Nominations, which Committee may nominate to the Academy. A majority vote shall elect. Honorary and cor- responding members must be persons who have rendered some marked service to Science, the Arts, or Letters, or to the Academy. ELECTION OF OFFICERS. 2. All officers of the Academy shall be elected by ballot. MEETINGS. 3. The regular meetings of the Academy shall be held as follows: On the 2d Tuesday in February, at the seat of the Academy; and in July, at such place and exact date as shall be fixed by the Council; the first named to be the Annual Meeting. The hour shall be designated by the Secretary in the notice of the meeting. At any regular meeting, ten membersshall constitute a quorum for the transaction of business. Special meetings may be called by the President at his discretion, or by request of any five members of the General Council. DUTIES OF OFFICERS. 4. The President, Vice-President, Secretaries, Treasurer, Director of the Museum and Librarian shall perform the duties usually appertaining to their respective of- fices, or such as shall be required by the Council. The Treasurer shall give such security as shall be satisfactory to the Council, and pay such rate of intere-t on finds held by him as the Council shall determine. Five members of the General Council shall constitute a quorum. 256 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. COMMITTEES. 5. There shall be the following Standing Committees, to consist of three members each, when no other nu.nber is specified: On Nominations. On Papers presented to the Academy. On Finance. On the Museum. On the Library. On the Scientific Survey of the State; which Commiitee shall consist of the Governor, the President of the State University, and the President of this Academy. On Publication; which Committee shall consist of the President of the. Academy, the Vice-Presidents, and the General Secretary. MUSEUM AND LIBRARY. 6. No books shall be taken from the Library, or works or specimens from the: Museum, except by authority of the General Council; but it shall be the duty of said Council to provide for the distribution to the State University and to the Colleges and public Schools of the State, of such duplicates of typical specimens in Natural: History as the Academy may be able to supply without detriment to its collections. ORDER OF BUSINESS. 7. The order of business at all regular meetings of the Academy or of any Depart- ment, shall be as follows: Reading minutes of previous meeting. Reception of donations. Reports of officers and cemunittees. Deferred business. New business. Reading and discussion of papers. SUSPENSION AND AMENDMENT OF BY-LAWS. 8 The By-Laws may be suspended by a unanimous vote, and in case of the order of business a majority miy snspend. They may be amended in the same manner ag. is provided for in the Constitution, for its amendment. Report of the Council. Since the last Report of the Council on February 11, 1874, the Academy has lost by death three of its most active members: Hon. I. A. Lapham, LL D., of Milwaukee, late Chief Geolegist of Wis- consin, Prof. Peter Engelman of Milwaukee, and Hon. John Y. Smith of Madison, the latter noted for his sound views and able writings in Political Economy. A short account of the life and character of Dr. Lapham, by E. R. Leland, Esq., of Hau Claire, also one by P. R. Hoy, M. D. Presi- dent elect of the Academy will be found at the end of this volume. A sketch of Prof. Peter Engelmann, by Mr. Leland will also be found in the same place. An account of the life of Hon. John Y. Smith. will be found in the Wisconsin State Historical Society’s Report for 187¢. 17———-w as IN MEMORIAM. PROF. PETER ENGELMANN. oY E. R. LELAND, EsSQ., OF EAU CLAIRE. Peter Engelmann was born on the 24th of January, 1823, and on the 17th of May, 1874, the died, before he had conipleted his fifty-second year. The object of this memoir is to give aslight sketch of this existence which was so suddenly cut short at the moment of bearing its best fruit. It is due to his memory that [should disclaim my fitness for this task, which was only undertaken upon the assurance that else it would remain undone. With- out other qualification than the admiration and respect resulting from a rather lim- ited acquaintance—with but meagre details of his life at my command, I shall at- tempt no adequate biographical sketch, but simply try to declare what the man was. Hlis birthplace was the village of Argenthal, in Rhenish-Prussia. His parents were farmers, as were his elder brothers, and of him they desired to make a farmer also; but in farm life he felt little interest even in boyhood, while, as soon as he could read, he was hungry for books, and eager in his search of knowledge. But social lines are drawn with rigor in Germany, and distinctions of caste observed al- most as scrupuously as they are in India, and it was only through the intervention of a fortunate circumstance that he was enabled to escape from the irksome pursuit ‘of the plow and follow his natural bent for learning. The Protestant clergyman of the village, and the superintendent, interested in the boy, on account of his rapid progress under inferior instruction, pursuaded his parents to send hina to a better school. To this they finally consented, in the hope to see their son gain the pulpit— than which they had for him no higher ambition—and he was sent to the ‘*Hochere Buergerschule’’ at Simmern. He went there from his ninth to his fifteenth year, walking a distance of four miles each way every day. When he reached home after his four-mile walk he had his ‘‘ chores’’ to do, and then to get his lessons. But he had energy and dilligence enough to overcome these disadvantages, and he received the highest certificates as to his proficiency. At this time he had no other aim than to gratify the piousambition of his parents; but this was not to remain the case very long. In 1838 he was—thanks to the aid of his teachers at Simmer, of whom he always spoke with tenderuess and gratitude —fitted to be received in the secunda of the gymnasium, at Kreuznach. It was wwhile here, although all his surroundings were calculated to impress his mind with PROF. PETER ENGELMANN. 259 re igious faith, that he felt constrained io give up the plan of becominz a pastor; the critical bias of his intellect constantly prompting him to question theologians and de- man | explanation of the contradictions in their teachings, until finally the old mys- tic creed of his fathers, lost every title of its influence and authority, and he ceased then, and forever after, to be swayed by its absurd hopes or childish fears. After studying at Kreuznach for the four years necessary to go through the Secunda and Prima, he passed a successful examination in 1842. The study of history and the natural sciences only served to strengthen his convictions, and, ever frank and outspoken, he found himself in antagouism to his bound-to-be-pious teachers. They could not, howeyer, help giving him in his certificate the most excellent notes in re- gard to diligence, progress, moral character and good nature. The theologian, in- serted the admonition that “he must not forget that nature and her laws are not higher than their Creator.?’ He went away to the Universities. Of his life there I know little. He joined a secret revolutionary society; but neither revolutionary zeal nor the temptations of student life diverted him from his work. There is evidence that his course was marked by the same good conduct and steadfast industry; for there, as at Kreuznach he was the object of high praise. ‘The certificate given him at Berlin where he studied three years, after one year at Heidelberg, contains twenty notes from various professors, among them Encke, Poggendorf, Dove, Ehrenberg, and Dirichlet, all unanimous in commendation. On leaving the University there were two courses open to him. One was to choose Astronomy as his calling, which he had studied theoretically and practically under Encke, but this he had not the means to pursue without aid, and he would not as he wrote in his journal “‘ beg protection.”? The other was to become a teacher at some gymnasium. He decided to apply for a State teacher’s examination and passed successfully, though he looked forward to it with apprehension, several of bis friends haying failed but a short time previously. The theologianamong the examiners, to whom he frankly confessed his unbelief, while giving him credit for his knowledge, decided that ‘‘ he could not teach religiun because he did not accept the bible as the source of truth. Royal commissioners in Prussia are very anxious to see that the youth are not misled by unbelieving teachers. Fortunately the result depended, not upon the theologian, Mr. Teressen, but mainly upon Schellbach, Rose, and Ehren- berg, and so he was granted the “ facultus docenti.’’ He then went to the Kreuznach Gymnasium, where he taught for a year anda half with marked success. Here again his frankness stood in the way of his preferment —his vutspoken declarations for republicanism preventing him from being regularly installed as a teacher. When in February 1848 the revolntion broke out in France, he hailed it with en- thusiasm, and with all the fervent zeal and energy of his nature agitated for the re- publican idea among the people of Kreuznach. Jvintly with some friends he found- ed a Turn-verein (gymnastic society) and a Buergen-verein (citizens’ society) and wrought a radical change in the public opinion. He was given to understan | that if he would “hush” he should have a desirable situation, and the Chief Director of Education of the Rhenish Provinces summoned him to an interview and advised him to desist. His answer was an increased revolutionary activity. With a few 230 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. friends of the cause he founded a democratic club and began publishing a reyolu- tionary paper. The first editor was soon compelled to flee. Engelman succeeded him in Febiuary 1849 and conducted the paper till May, when he too, had to leave his Fatherland to escape the dungeon. Another of the friends then continued the paper until it was suppressed by Prussian soldiery. In Augnst, 1849, Englemann reached New York in a destitute condition. He joined an acquaintance to try ‘Latin farming’? near Marshall, Michigan. The re- sult was as discouraging as might have been expected. One of his first acts was to take out his naturalization papers, for he burned with impatience to “renounce for- ever his allegiance to the King of Prussia,’’? and to become a citizen of the Re- public. After working for awhile as a furm-hand. he went to Milwaukee, and thence to Oshkosh. At the latter place he was taken sick, and lay prostrate for eight weeks, without friend or farthing. Returning to Milwaukee, he was again taken sick; and without money for support, or a single acquaintance, his situation and frame of mind may be more easily imagined than described. Whea partially restored, he was engaged by a farmer, three miles from Milwau- kee, to instruct two boys for his board. Soon after, he was engaged as teacher for a district school. His success as a teacher soon became manifest, so that children were sent from the city to partake of his instrnctiou. After the close of the term, although the district sought to retain him at double his former salary, he went back to Milwaukee to seck a more extended field for his educational woik. Then it was that the German and English Academy was founded. It commenced school July 1, 1851, giving its director a salary of $25 per month. Tere he reinained nntil death closed his arduous and unselfish duties. His plans were far more comprehensive than his achievements. He was not to be permitted to carry them out, but he lived to see his academy advance in mem- bers and eduzational results until it gained the reputation of being one of the best schools of its grade in the Union, a result which it is no exaggeration to say was due to his labors. Engleman was one of the pioneers in the United States cf mod- ern rational pedzgogy, as opposed to the old school routine of memorizing and recit- Ing; his aim was more to edueate and train the young mind for self-instruction, than to cram with undigested knowledge. His methods were based upon the ideas of Pestalozzie and Froebel—though he was a routine follower of no man’s lead. It had Jong been his intention to publish a number of hand-bouks for the use of sohools, among them one of Universal History, and he was about to prepare a teachers manual for mathematics. In this respect his premature death is a serious loss to the cause of education, for his metnod, based upon his rational views, have proved highly satisfactory and successful. In mora! teachings he avoided making them repugnant to the pupils by dry catechism, but taught them to love virtue by examples taken from history which were emphasized by his own excellent example. He introduced natural sciences more largely than is conimon, that his scholars might learn how t» observe—how to read and question the works of nature for themselves, and to apply the scientific methods of investigation to all things; and lastly, he ever songht to transplant his own humane sentim n‘s; his own chivalrous love for liberty and justice into the minds of the embryo citizens entruste! to his care. One of the good results of hisschool was the elevation—by a spirit of emu- PROF. PETER ENGELMANN. 261 lation—of the standard of the public schools of Milwaukee, to a much higher level than they would have otherwise attained. But the care of this Academy, absorbing as it was, by no means bounded the sphere of his activity. He and his friend Dr. A. Luning, were the principal found- ers ot the Natural History Society of Wisconsin, and he the Curator of its now very valuable museum from the beginning. He bestowed a great amount of labor upon it; zoalously collecting himself, and inciting others to follow his example. Who- ever might be lukewarm; he was not. He never wearied of the work; he shrank from no dru:lgery connected with it. Much, perhaps most of his leisure was given to the work of determining, labeling and arranging specimens. Nor was he niggardly of his precious time to either the mere curiosity gazer, the inquiring voung student, or the amateur dabbler in science. The courtesy and kindly interest with which he welcomed all comers, I have occasion to gratefully remember. Since his death, the museum bears his name. In spite of this exhausting and absorbing professional work, he found time to write many articles for liberal papers, and to give numerous lectures before radica and scientific societies, always withort pay, and often illustrated by experiments at his own expense. In short, he sought knowledge, not for the personal gratification which it affords, but to the end that he might aid in its general diffusion, or make some practical application of it for the good of his fellows, and he carried these dis- interested labors to an extreme that many of his thrifty countrymen could not un- derstand, and they were, some of them, inclined to call him visionary and a fanatic. Te was neither. Je had sterling good sense, and he rode no hobbies. His mo- tives lay upon the surface, and if men could not read them aright it was their own oblique vision that was at fault. Tis whole life was given to the advaneement of the race, to liberty of thought, of speech, of life—with a devotion that most men will admire and few have the courage to imitate. His last illness was a sharp attack of congestion of the lungs, under which hesank very rapidly, retaining consciousness to the last. He died, as he had lived, bravely and calmly; without fear or regret. With characteristic modesty he directed that his funeral should be free from formal obsequies. There were none of the conven- tional forms, but hundreds followed him to his grave and hid it with flowers as a last feeble tribute to his worth, and, few indeed are the men who havea place in the tender memories of so many hearts as this self-sacrificing teacher. The future of his beloved enterprises—concerning which he had many and ambitious hopes—is now in other hands. They may not suffer, but it will be a long search to find one man who can fill his place. This, in brief, and most imperfect outline. was the life of Peter Engelmann. It was not, as we have seen an eventful one. Jlis name never became famons, for his were not the qualities which gain fame—as the world goes. Self abnegation, honest steadfastness of purpose, devotion to principal, are prized and valued but are not loudly praised. it is the bold dogmatist, the skilled rhetorician, the sagacious trim- mer of sails to the breeze of public opinion, that wins applause. This modest pedagogue knew none of these tricks of success. With rare rectitude ‘he, in early manhood, put aside a brilliant scientific career, because he prized inde- pendence, self-respect, the approval of his conscience, more highly than place and 262 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. profit and fame; and from his devotion to principle the very nature of his religious belief, removed all taint or suspicion of selfishness, even of the most refined and spiritual sort, for he was an uncompromising materialist. Forced to the conclusion, that so far as human reason, arguing from the facts of life, can form any judgment on the subject, a self-conscious existence hereafter is an impossibility; he declined to follow these who assume that there is a higher mode of apprehending these facts than reason supplies. He would allow no attri- butes—cherish no hopes that demanded the sanction of something higher than his understanding; and whatever may be our private beliefs, it is difficult to see how the logical soundness of this position can be assailed. His belief gives the clue to his aims und his labors. Feeling that the assump- tions of the so-called, higher modes of cognition were gratuitous and mischievous, he wotked so far as he could for their downfall—but he did not stop here, he was not a mere iconoclast. He saw, what all must see, that there is a growing disposition to question these assumptions, and he was not blind to the dangers of states of trans- ition. He could use no other than the materialistic formula, but with that he did what in him Jay to revolutionize and humanize political and social life, so as to fit it toa higher creed. Ile worked tothe end that when men should no longer obey, through fear or hope, the mystical, external commands, that they should already be, through a love of goodness for itself, obedient to the higher, internal commands. Ge apprehended no danger to morality, for he well knew that morality is not the fruit of any creed, but the sum of human experience. His last work in this direc- tion, was an answer to an attempt, by one Pastor Streissguth, to prove that material- ism was error and tended to immorality. The pamphlet has been published since his death, by the Wisconsin Union of Liberal Societies; he therein refutes by unan- swerable arguments, as he had by his piure and blameless life, the silly and inecon- sequent slander, that the morality which flows from scientific materialism can be comprehended in the words, “Let us eat and drink, for to-morrow wedie.”’ Ifa man believes that his sentient existence is restricted to the three-score years on earth, will he therefore anticipate the nothingness of the future by becoming a sot in the present? or will he use his best endeavor to husband this handful of years and make them yield to him the greatest measure of spiritual life? To say nothing of the many good and able men who cannot base their theory of life upon a belief in a future individuality; there are outside the limits of Christen- dom millions of human beings who look forward to forgetfulness, and whose lives are by no means marked by a devotion to the grosser pleasures of the world. The as- sertion, or rather the inference—for it oftenest comes in that shape—that a man will be good only in proportion as he has a lively sense cf the pleasures of a coming heaven, or the pains of an inevitable hell, is a rank calumny upon our moral nature. It is safe to assert that no man of noble instincts, pure aspirations, or high moral principle will be demoralized by the contemplation of a limited existence; nor will the brute be ennobled by the prospect which the church presents to his debased im- agination. I will make no apology for thus lamely intruding these truisms. There is need of their occasional reiteration. PROF. PETER ENGELMANN. 263 No good and pure man lives without divinities—and Engleman’s were; humanity, progress, a realization of the high ideals to which his philosophy pointed. Brave an{ outspoken in uttering his convictions when need was, he was never dogmatic. He did his work in a spirit of true humanity—a humanity that was content cheer- fully to accept the place which he believed he held in nature, that of a stepping- stone—one of the myriads by which the race is to gain a glorious future. But he had none of the assumed, servile, oriental abjectures that leads man to revile him- self as a worthless worm of the dust, and in the same breath demand, with sublime egotism, why he was created, with his lofty purposes and high aspirations, if he is to have a glorious and an undying future? That leads him to deem himself defrauded if, with his matchless intellect, he is not to know a state of being far transcending anything which earth affords, more or less ineffable and gorgeous as his ideas are spiritual and his imagination vivid. The man who holds and promulgates ideas that are in opposition to the popular beliefs of his age, can scarcely live a bright and cheerful life; but it may contain much of nobleness that compensates for the loss of worldly pleasures. Engelmann was aserious but nota sad man. He bore a burden common to many, but he stood upright under it. He answered the question which man is ever asking ‘* What am 1?”) by saying ‘‘ my consciousness isa mere resultant of force acting upon matter and at the death of the fiesh it will revert to its former conditions,.as sounds revert back to the air in which they were born.’’?’ We may answer it differently, but we cannot demonstrate that he was mistaken; and we must admire his attitude when brought face to face with a great problem. Tt was with eyes open and head erect—true to his creed to the last—hugging ng delusive dreams—his highest conception of truth upon his lips. No man can meet death better! He is at peace, and if it be that the universe holds greater possibilities than were acknowledged in his philosophy, we may be sure, as has beon said of one whom in many things he resembled: ‘Wherever there is knowledge, Wherever there is virtue, Wherever there is beauty, Ife will find a home.”’ INCREASE A. LAPHAM, LL. D. BY P. R. HOY, M. D., RACINE. PRESIDENT OF THE ACADEMY. It becomes my duty, as chairman of the committee appointed for the purpose, ot - report on the life and labors of I. A. Lapham, LL. D., one of the organic members and the first Secretary of our Wisconsin Academy of Sciences, Arts, and Letters. I perform this duty with greater willingness, and, indeed, with a mournful pleasure, yemembering Dr. Lapham as a long and well-tried friend. Engaged in similar sci- entific pursuits, there sprang up between us a close friendship, cemented by sympa- thy, which lasted nearly thirty years, until his death. IT shall not attempt a complete chronological history of his life, as that has already been so well done by S. S. Sherman for the Old Settlers’ Club of Milwaukee, but shall speak principally from personal knowledge, merely introducing a short sketch of his early life by way of preface. Increase Allen Lapham, whose memory we wish to bonor. was born of Quaker parents, in Palmyra, Wayne Co., N. Y., on the 7th of March, 1811. After receiv- ing a common school training he began the study of Engineering under his father’s instructions. ; When but sixteen years of age he went to Louisville and was employed on the ship canal around the Falls of the Ohio. At this early date he began the study of Botany, Conchology, and Geology, which he prosecuted as a youthful lover of nature with the enthusiastic zeal which charac- terized his work during all the years that followed, up to the hour of his death. While in Louisville he wrote his first scientific paper entitled, ‘‘ A Notice of the Louisville and Shipping-Port Canal, and the Geology of the Vicinity,’? which was published in the American Journal of Science and Arts. This first offering contained many new facts and was highly eommended by the elder Silliman as a valuable contribution, coming as it did froma mere boy, what might not be expected from the pen of riper years, wider experience and greater knowledge? When the canal was completed, young Lapham became assistant engineer of the Ohio canal, which position he held until his appointment in 1833 as Secretary of the State Canal Board of Commissioners, when he moved to Columbns. Here he found time to devote to his specialty, Botany, and formed the acquaintance of many eminent scientific men, among them Prof. J. B. Kirtland. In the spring of I836 he landed at the straggling village of Milwaukee, in the then Territory of Michigan, where he continued to live and study for the remaining thirty-nine years of his active and useful life. INCREASE A. LAPHAM, LL. D. 265 My first acqnaintance with Dr. Lapham was in 1846, when one morning there Janded from the steamer Sultana a small man witha huge collecting box hanging at his side. {Te came from Milwaukee and intended returning on foot along the lake-shore in order to collect plants and shelis, no easy journey, encumbered, as he soon would be, with a well filled specimen box He spoke lightly of the undertaking, saying he had performed similar feats befure Truly where the heart is in the woik and the mind is fully occupied, labor becomes mere play, and what otherwise would seem drudgery is performed with ease and pleasure. In after years we were often together, studying the mounds, quarries, forest trees etc., near Racine, and my first impressions of his energy, persevorance, enthusiasm, accuracy and extent of information were all deepened by our subsequent meetings. He was a quiet unassuming gentleman, benevolent and most hospitable, as both strangers and friends can abundantly testify. He had not the advantages of com- manding presence, and was not gifted in public speaking, and being modest toa fiualt, always inclined to underrate his own abilities and labors. he often did not re- ceive that recognition which his knowledge demanded and which would have been quickly yielded had he possessed more self-assertion or a more combative temper- ament. Yet, his hight could not be hidden, though he succeeded sometimes in shadowiny it, and he soon became ¢he authority on all scientific subjects, and was eften appealed to from city, state and country for information which he alone could furnish. His politeness and patience under the infliction of ignorant question-askers who often trespassed upon his valuable time with matters of little importance, and his rule of always answering letters asking information, no matter how trifling, show his kind heartedness and unselfishness. No one could doubt his industry who saw his large, valuable, and well used li- brary, and his extensive and systematically arranged collection of minerals, fossils, shells and antiquities; or who examined his Herbarium of three thousand spect- mens—the finest in the Northwest—and thea remembered in connection with all this his work in other directions. Iis idea of rest was characteristically shown by his once cataloguing my hundreds of insects for future use in some publication, at atime when he visited me under his physicians’ orders to take a needed rest and abstain from business. He was no politician and never sought office. Such offices as he held sought him. Among the many services he has rendered to science not the least, is his work in establishing the Signal Service, which has already worked such good in saving wealth and precious lives. As his connection with this enterprise seems to have been enveloped in doubt with some, I wrote to Prof. Henry, Secretary of the Smith- sonian for information. In reply I received the following: "The action of Congress in securing the Signal Service was due to the immediate exertions of Dr. Lapham through the member of Congress from his district, Gen. Payne, in setting forth the advantage of the system in the commervial interest of the Great Lakes.” So this matter is settled as Prof. Henry is the end of the law in meteorological affairs, Was Lapham a self-made man? 266 WISCONSIN ACADEMY SCIENCES, ARTS, AND LETTERS. Yes, all men are self-made, in one sense, for there can be no unusual attainments without close and persistent study. Lapham, however, never had the advantages of a college education. But was not the book of nature ever open to impart instruction to this student who knew how to read its pages with delight and profit? To his ex- tensive reading and close observation of nature we must not omit to add as an educa- tional element in iis life, scarcely to he overestimated, his long continued correspond- ence with such men as Henry, Baird, Leidy, LeConte, Haldeman, Cassin, Hall, Morton, Kirtland, Agassiz, Gray, Eaton, Silliman, Rogers, Hitchcock, Torrey, Harris and a host of others eminent in science and arts. Another means of improvement, not neglected by Dr. Lapham, was attendance of meetings of societies devoted to the dis- cussion of his loved studies, and where mind comes in contact with mind, with mutual benefit. He was a member of most of the scientific associations of the country, and gave them many valuable written contributions. Some of his articles are published by the Wisconsin Academy, in the Wisconsin and Illinois Agricultural Reports, Agri- cultural Department of the Patent Office, Historical publications, Smithsonian Con- tributions to Knowledge, Proceedings of the American Association for the Ad- vancement of Science, American Naturalist, Geological Reports, ete., ete. Besides, he published many pamphlets and maps, both topographical and geological. His writings were brief, clear and devoid of high-sounding words used for effect—he was above such trickery. In order to judge correctly of men, we must know them under those circum- stances and in that place where nature and education have best fitted them to act. To know Dr. Lapham, we must go with him to his workshop—the great out-doors. We stroll out on the prairies. He pulls up the grass and discourses familiarly of the spikes and spikelets, the rachis and glume, inspects the roots, digs down and ex- amines the soil from which they spring. His tongue is unloosed, and: he becomes eloquent in spite of himseif. We go into the forest. He talks of the various spe- cies of trees, the vines that clamber up their trunks and nestle in their branches. He inspects the lichens that grow on the rough bark, examines the moss that ad- heres to the roots, and unearths a tiny helix that has found a home there. We go to the rapids, and he immediately interests himself in the rare ferns that festoon the rocks with their graceful fronds; or clambers among the quarries, marks the strati- fication of the Silurian rocks, and chips out rare forms of Crinoids and Trilobites— those wonderful representations of the ocean fauna of the dim past. We seek the mounds—those records of a pre-historic race—dig beneath their foundations and wrest from them their secrets. The position of the bones is carefully noted, their rude pottery restored, the curious stone implements treasured up, and 128 mounds are surveyed and mapped. We stand upon our lake shore and he discourses of the force of the waves, and describes the ingenious contrivance by which he detected the lake’s minature lunarwaves. He talks of the force of the winds and their velocity and direction and then looks up the clouds and iells their indications, and speaks of the annual rainfall and of the average temperature of the seasons for the last thirty years, during which time he had kept a faithful record of these phenom- ena. His last paper, ‘‘ Oconomowoc and the Small Lakes of Wisconsin,’’ was prepared for me. The ink was scarcely dry before his soul passed over to the ‘‘ Shining INCREASE A. LAPHAM, LL. D. 267 Shore,’ that lovely day, September 14, 1875, was the last of earth to Dr. I. A. Lap- ham. The State has Jost the service of one who knew more of her Geology, Topography and Botany than any man living, and one who contributed largely to her early pros- perity. Milwaukee has lost one of her oldest and best cltizens, an upright and hon- est man. His children have lost a luving father end his accquaintances a devoted friend. ADDITIONAL TRIBUTE TO THE MEMORY OF DR. LAPHAM. BY E. R. LELAND, ESQ., EAU CLAIRE, WIS. Mr. Presiprnt:—I cannot let this oceasion go by without trying to pay some tribute to the memory of our lamented and revered fellow-member, whom it was tong my privilege to call a friend. Known to the world as an able scientist; to the many who casually met him, as a modest, manly, cultured gentleman; by the few he was honored and beloved as it falls to the lot of few men to be, fur virtues that were not worn upon his sleeve—for # nobility that intimacy alone could reveal. I do not, however stand here as his eulogist. I should feel that to be a sort of im- pertinence in me—even if the work had not already been done far better than I could hope to do it. I desire only to make some acknowledgement of the obligation—now never to be discharged— which Dr. Lapham has laid upon me by many acts of kindness and as- sistance through all the years since I first knew him. An obligation which, I think many others must share with me, for he was ever ready with kind and helpful sym- pathy for all. The merest tyro in natural history was sure of warm welcome and encouragement at his hands, and his collection, his library, and above all his valua- ble time and experience were placed freely at the disposal of the seeker for knowl- edge. And he taught wisely; for his nature had nothing of the pedant, his spirit nothing of dogmatism. His was the open mind; ready to learn from all sources, not prone to theorizing nor swift to draw conclusions. He had learned to wait—and there was in his attitude no posturing, nor bidding for popular applause in anything which he did. He toiled for science, from a love of Science, but with a thorough and intelli- gent comprehension of the great possibilities that lie in this field of research. And it has always seemed tu me that when he came to die, the manner of his death was a serene and most fit ending of a life thus spent. No prolonged, distress- ful struggle, no whispering, crowded room; there were bending over him no beloved faces, agonized with a grief which he could do nothing to assuage. Nodoctor came, ““With phrase and fame, To shake his sapient head and give The ill he could not name; * * € * * * No brother doctor of the soul, To canvass with official breath, The future and the viewless things, Which one whofe Is death’s winnowing wings, Must needs read clearer, sure, than hel’ TRIBUTE TO DR. LAPHAM. 269 He was alone and face to face wit Nature, whose life-long lover he had been. Fanned by her softest airs, lulled by her gentlest song, his last conscious act, per- haps, a fresh effort to trace her endless clue, and he passed on, with swift and pang- less transition, to the solution of the wonderful mystery which enyelups all. TRANSACTIONS OF THE WISCONSIN ACADEMY OF SCIENCES, ARTS, AND LETTERS. Vou. IV. 1876-77. = “ MATOS Oo NE OA Po oe A ~ a S* ‘< a™ hy Le : ON \ AA A R 8 1889 : ws Nag Re ee , NY yn Soh Published by Authority of Law. MADISON, WIS.: DAVID ATWOOD, STATE PRINTER, CONTENTS. TITLES OF PAPERS PUBLISHED IN THIS VOLUME. DEPARTMENT OF SOCIAL AND PoLiTICAL SCIENCES. Page. 1. Peasant Communities in France. By Wm. F. Allen, A. M... 1-6 2. The Abolition of the Jury System. By Rev. Chas. Caverno.. 7-18 3. The Origin of the Freeholders. By Wm. F. Allen, A. M.... 19-24 4. The Duty of the State in its Treatment of the Deaf and Dumb, the Blind, the Idiotic, the Crippled and Deformed, and the Imsanes > yz kr Ze Mason Le Denies nssaccjeic tiers cists c sistcrers 25-30 DEPARTMENT OF ARTS. 1. Art as Education. By Alford Payne, S. T.D...... Saqbobood 31-43 2. The Harmonic Method in Greek Art. By J. R.Stuart, A.M. 44-49 DEPARTMENT OF LETTERS. : 1. Letters an Embarrassment to Literature. By Prof. W. C. SEMAVGEo Oca OE ooodoDOORS ofelereassett wrcrohelsieleisieveusceinye-elteeveneterores 50-55 DEPARTMENT OF SPECULATIVE PHILOSOPHY. 1. Mr. Spencer’s Social Anatomy. By Rev. H. M.Simmons.... 56-61 2. Nature and Freedom. By J.J. Elmendorf, S.T.D.......... 62-76 DEPARTMENT OF NATURAL SCIENCES. 1. Notes on Cladocera. By Edward A. Birge, Ph. D........... V7-112 2. On the Fauna of the Niagara and Upper Silurian Rocks, as Exhibited in Milwaukee county, Wisconsin, and in Counties Contiguous thereto. By Fs oH. Day, M.Di oo ay nse e ee 113-125 3. Discoveries Illustrating the Literature and Religion of the Mound Builders. By Edmund Andrews, 4. M.,M.D...... 126-131 4. How Did the Aborigines of this Country Fabricate Copper implements? By PR. Hoy, Mie Deo.) 2 cine oe Ssoa8e 132-137 5. Remarks on the Descent of Animals. By Prof. H. Oldenhage. 138-146 6. Why are there no Upper Incisors in the Ruminantia? By P. LES Lovee Mami eater atata\leia!s, wvoic'-: cial a Wetyel seevotare theisies) s\clsielt @) so) .»-. 147-150 ipoler Explosions.. By Chas..l) Kings saes kos. loess ao ces .. 151-168 8. Mind in the Lower Animals. By J.S. Jewell, M. D........ 164-187 9. The Antiquities and Platycnemism of the Mound Builders of Wasconsin) eByJIN De Hart, My Ds. s 2). 5.2 sss. ctctesse 188-200 10. On the Extent and Significance of the Wisconsin Kettle Mo- raine: By T CuChambpberliny AVM, 2.5 5. 260. 13. i " “ Antennule x 260. 14. Alonopsis media, “ Post-abdomen x 160. 15. e “fem. ac x 150. 16. Alona porrecta, male. x 150. 1%. -Graptoleberis inermis, fem. Post-abdomen x 150. 18. Crepidocercus setiger, fem. X 148. 19. Pleuroxus procurvus, fem. Front part of animal x 150. 20. oy rf fem. Hind part of valve x 150. ila ameta * denticulatus, fem. Post-abdomen x 150. - 22. a unidens, fem. Hind part of body and valves « 95. THE HELIOTYPE PRITING CO. 220 DEvoNsHIRE Sr. Boston ian wep Metctrooig EXPLANATION OF PLATE IL Fig. 1. Daphnella exspinosa, fem. Antennule x 140. 9. 66 cc male. «“ 66 3. s 6 s Post-abdomen x 140. 4, 66 (79 ce a (73 5. Daphnia levis, fem. “ a Giekipers cS ee Embryo, outline of head. 6b, b’. “ “ « Young, « 6c. S a “ Adult, ec Te ss “ male. Antennule x 140. 8. Ceriodaphnia cristata, fem. Head x 130. 9. i “ “ Post-abdomen X 180. 10. Bosmina cornuta, fem. Head, etc., x 150. 11. Plevroxus straminius, fem. Post-abdomen x 140. 12. cc insculptus, ‘“ Details of marking. 18. se hamatus, “ “ 14. € fe sf First foot « 148. 15. ec acutirostris ‘* < 1385. 16. Aloma angulata, fem. x 1385. 17. “ tuberculata, fem. x 135. 18. st male. Post-abdomen x 140. 19. Chydorus sphericus, male. x 150. Plate I. THE HELIOTYPE PRINTING CO. 220 DEVONSHIRE ST. Boston. Ihe, es TAT Haves ox t Fauna of the Magara and Upper Silurian focks. 118 ve ON THE FAUNA OF THE NIAGARA AND UPPER SILURIAN ROCKS AS EXHIBITED IN MILWAU- KEE COUNTY, WISCONSIN, AND IN COUNTIES CONTIGUOUS THERETO. BY F. H. DAY, M. D. Wauwatosa, Wis., Dec. 27, 1877. It is stated as an axiom by high paleontological authority,— that ‘‘Since rocks are identified more by their fossil contents, than by their lithological character, a name descriptive of the latter is of less importance than formerly, when fossils were the sub- ordinate characters of a mass;” and although paleozoic char- acters have assumed the supremacy over all others in distinguish- ing sedimentary strata, “still the lithological terms must not be overlooked; for if properly understood, they will be unerring cuides in tracing the condition of the surface, for more than hun- dreds of miles in extent.” Changes in the lithological features of a rock which may render observations unsatisfactory, are accompanied by greater or less variation in the nature of the fossils. It is therefore of the high- est importance in the examination of sedimentary rocks to be gov- erned by three essential facts, which are: 1st. The lithological character. 2d. The order of the superposition. 3d. The contained characteristic fossils. By an observance of such precepts geologists have been enabled to forma reliable anda systematic geological history, which is ar- ranged into natural distinctions of ages, periods, epochs, and eras, with the capability to trace from one portion of country to another, through all intricate phases, types and characters, the rocks con- taining remains, images or casts of paleozoic life. It is thus we determine the first appearance in the world’s his- tory of organized beings, as exemplified in thecommencement of 8 114 Wisconsin Academy of Sciences, Arts, and Letters. the Silurian age— usually termed the Lower Silurian, where by successive layers or strata of calcareous or siliceous sedimentary * matter, we trace each order of life through distinctive periods, and epochs, until progressive organization culminated in the era of man. : The nomenclature adopted by tacit consent of paleontologists, to be applied to rocks, is that of the locality where the exposure of a specified rock exists in its best state of preservation and can be carefully examined and studied. In this manner are the terms derived, Canadian, Trenton, Nia- gara, Salina, Lower and Upper Helderberg and Hamilton, with the subdivisions of Quebec, Galena, Waukesha, Racine and St. Claire. But it is the three principal periods: the Trenton, Niagara and Salina which particularly interest a paleontologist when making collections of paleozoic remains from the eastern portions of Wis- consin, and therefore the foregoing explanatory observations seemed to be necessary to elucidate what seemed to befog or de: ter some of our leading state geologists in arriving at definite sat- isfactory conclusions. For if you examine the strata of rocks, with their fossiliferous contents, as exhibited in various exposures by quarrying or from other causes in Milwaukee county within a radius of twenty miles, it is difficult to apply the foregoing mentioned, or geological ax- ioms. In a single quarry containing a coralline limestone near Wauwatosa I have obtained several thousand specimens within the past twenty years, and from among them I can show you repre- sentative fossils delineated and described as belonging to the com- mencement of the primordial time or Lower Silurian age, intermin- gled with many fossils characteristic of the Upper Silurian, the Guelph and the beginning of the Devonian age. However, ‘Prof. Dana asserts that there is no evidence that a species existed in the latter half of the Upper Silurian, that was alive in the latter half of the Lower Silurian.” The fossils of the Niagara fauna being mostly casts of the interior, it is more of an exception to - find the shell or testaceous covering in a perfect state of preser- vation thereby making our investigations accompanied with many Fauna of the Niagara and Upper Silurian Rocks. 115 difficulties, nevertheless Hastern Wisconsin has a fauna which in variety, beauty, perfection and numbers cannot be excelled by a similar collection, within the same extent of country on either hemisphere. : Could the distinguished Prof. L. Aggasiz have examined our corals, Hchinoderms, Brachiopoda, Lamellibranchs, Gasteropoda, Cephalopoda and Trilobita, no doubt he would have exclaimed, ‘why sir, the sight of this display would make an eastern natur- alist crazy.” On one occasion after arecent excavation by blasting at Schoon- macker’s quarry, | measured a coral disk about twenty feet in diameter, three feet in height, and more than sixty feet in circum- ference. The surface was made up of beautiful concentric layers, like the flattened whorls of a gasteropod, and were covered by very pretty Heleolites. Cruising around such coral eminences, were the “lords of the invertebrates,” the Orthoceratites, the straight variety of Cephalo- poda, measuring over twelve feet in length and twenty inches in circumference, and having siphuneles so peculiar in shape and ex- pansion, that Prof. H. A. Ward, notwithstanding his large ex- perience and observation, declared these different from any species he had seen in the old or new world, because the pyrimidal-cone- shaped siphuncle of the base, or last chamber, resembled much the contour of a Belemnite. ; Here also was the gigantic Phragmoceras having a base twenty one inches ir circumference, six inches deep, and a seven inches lat- itudinal aperture, and extremely macrochcilus or long lip, for per- fect specimens collected of five species of Phragmoceras make Prof. Hall’s description of a single specimen of our species, compara- tively a myth, and his Phragmoceras nestor is simply a descrip- tion of a mutilated specimen of a Phragmoceras macrocheilus. Prof. Hall’s Gomphoceras septoris has the curvilinear figure of a Phragmoceras, er Cyrtoceras, and in general aspect much resem- bles a Phragmoceras callistoma (Barrande), delineated in Wood- ward’s Modern and Fossil Shells. Of the four varieties of Gompho- ceras, one may prove to be G. serinvum or G. Marcyi of Winchell. The gasteropoda of the Lower and Upper Silurian and Hamilton 116 Wisconsin Academy of Sciences, Arts, and Letters. cementare found much larger and in a more perfect condition than those pictured and described in reports of previous geological sur- veys. A magnificent and perfect Plewrotomaria perlaia five inches in diameter, found in the Niagara shale, and also in the Guelph or Gault, a Zrochoceras, Gebhardit, six inches in diameter, from the cement rocks, besides many others, claim honorable mention. In no other place are such unique lamellibranchiata to be found, particularly the Moceraunas and Amphicelia, Ambonychia, and Paleocardia. Ihave quite a number of perfect specimens, retain- ing the whole or parts of their beautiful striated shells. It is in Schoonmaker’s Quarry that several distinct species of trilobites belong which are not found elsewhere—in any fossilifer- ous formation. Prof. J. Hall, in his description of the fauna of Wisconsin, was often obliged to make use of imperfect material, and in resorting to the very unsatisfactory mode of delineating restored parts, or “supposed differences,” he would naturally be much disappointed and mortified to find his opinions erroneous upon the subsequent discovery of perfect specimens, which were heretofore entirely new, or but little known. On this account it is questionable whether Hall’s synonyms for fossils like the Jdlenus, Spherexo- chus, Phragmoceras, et cetera, when perfect specimens prove them to be so radically different from Hall’s descriptions, should be ‘saddled ” with the names he intended should be applied to them, especially when his opinions are based upon a single part or frag- ment of a perfect specimen, and also when the synonym is foreign to the idea suggestive of its character. or example, the pygidium of the Jllenus cuniculus is confounded with the Bridgeport and Waukesha Jllenus armatus, which is probably an adult speci- men of Illenus insignis, or Illenus Worthmanus of Winchell, or Llloenus Springfieldensis, of Meek. There are other species of the Lllenus, or Asaphus, to which the glabella has a slight re- semblance to Hall’s description, but otherwise are totally different. The pygidium of Hall’s Sphoerexochus Romingert is simply a mutilated specimen of a pygidium of S& mirus of Beyrich. I am induced to make these assertions after a careful comparison with perfect specimens in my cabinet. Allow me, also, to state Fauna of the Niagara and Upper Silurian Rocks. 117 that I have never seen a single specimen of Jlloenus roxus, found in Schoonmaker’s Quarry, notwithstanding Prof. Hall’s mention that it is of frequent occurrence, and Prof. T. C. Chamberlaiu identifies it as belonging to this quarry. A nearly perfect head and pygidium of an Aczdaspis Danat make the specimen quite different from Winchell’s Acidaspis Jda. Extraordinary sized Ceraurus insignis are occasionally found and well marked parts of Brontews Acmas, Harpes, Lichas, Dalma- nia, wew species of Lllenus, Asaphus, besides quite a number of as yet undetermined varieties of trilobites, which are “new or but little known.” Fine specimens of //loenus ioxus are found in Waukesha and and Greenfield, but it is in the Racine quarries that the grand pa- triarchial zovus assumed his supremacy. Specimens of heads over five inches wide and three inches deep, and joined to thoracic segments, and pygidium will make full-sized specimens, more than one foot in length. The Acidaspis and several other very re- markable varieties of trilobites are also found, beautiful as well as unique, and unsurpassed. But it is in the the Wauwatosa quar- ries that the best documents are produced to illustrate the com- parative anatomy and physiology of the trilobite. A critical ex- amination of fossil specimens of this invertebrate animal reveals a bundle of contradictions on account of its possessing many at- tributes belonging to several orders, which cause the trilobite to assume as uncertain a position among the invertebrates as a Chei- roptera does among vertebrates ‘“‘ which can claim a habitation neither with birds or beasts.”’ All the parts of the trilobite, as found at Wauwatosa, béing ‘casts of the interior,’ reveal an internal mechanism which re- quires no more stretch of the imagination to localize and impute cer- tain actions to different parts, than for an anatomist to explain definitely and intelligently the properties and powers pertaining to the skeleton of a vertebrate. Precisely in similar manner do the casts of the trilobite illus- trate its organism, habits and locomotion. Like some species of Entromostracans, it was capable of being dismembered into sev- eral parts and had the attributes of Crustaceans, Mollusks and Worms. Its ambulatory movements were performed in a similar 118 Wisconsin Academy of Sciences, Arts, and Letters. manner to the larvze of insects, but its exterior covering of crusta- ceous segments, united by chitine, enabled it to move rapidly in the water similar to the molluscan Chiton. It also possessed the same natatory powers as the Crustacean Macrurans. or it could assume a spherical form like an Isopod, or lepidoptera hairy larva. By the action of its extension or flexor muscles, the trilobite was enabled to elongate or contract its size from several inches in length to one-third its longitudinal extension capacity, and did not possess a single attribute of an arachnoid. If a name were required for such an organization, it would be one suggestive of three orders of genera, combined in one, indicative of an annelid, a Mollusk, and a Crustacean. Such a proposition is the result of a careful examination of many thousand specimens of several genera and species of trilobites, and I am induced to believe that this peculiar invertebrate lived, at certain distinct periods of time, so well defined, as to indicate a sufficient reason for making a change in the ages of Geological History. For instead of classi- fying the Silurian age as one of Mollusks, and the Devonian as Fone of Fishes, substitute a Trilobite age. For Mollusks existed through all ages, and fishes first appeared in the later part of the Silurian, and assumed a prominence in subsequent ages, like the Devonian, Carboniferous, etcetera, but the Trilobite is identified at the commencement, and became extinct at the close of paleozoic life. In a paper like this, treating: of a miscellaneous fauna, I can only thus give a brief synopsis of the component parts of Trilo- _ bite, which, like the Crustacea, by aid of muscular action could be ‘sessile or stalked eyed,” and its having a chitine carapace nnited by sutures, was provided with processes, and sinuses for the attachment and action of muscles, and it could be readily dis- membered at its dissolution into cheeks, glabellz, hypostoma, thoracic segments and pygidium, that were held in proper posi- tion by a chitinous bond of union, which enabled the trilobite to perform its wormlike motions by expansion, adhesion and contrac- tions, or to fold its extremities together as the caterpillar larva, or wood louse when alarmed, or if attacked as a means of defense, or could move swiftly through the water, like the Molluscous Ohiton or Crustacean crawfish. After many years of patient research and with the aid of Fauna of the Niagara and Upper Silurian Rocks. 119 largely magnifying optical instruments, I have been unable with the single exception of the seta filaments at the extremities of the thoracic segments of Culymene — to discover any apppearance having the slightest resemblance to the strong jointed legs; char- acteristic of the limulus group. Since preparing this society paper, I have received from Mr. C. D. Walcott, Curator State Museum Natural History, Albany, N. Y., two pamphlets on the organism of the trilobite, entitled “a preliminary notice of the discovery of the natatory and branchial appendages of the trilobite,” also an explanatory letter from the author respecting the uncertanty of his discoveries, but hopeful of a final satisfactory result. A copy of the twenty-eighth Regents’ New York Report by Prof. © Hall, with reference to plate 34, fig. 14, illustrating points of at- tachment for supposed natatory organs, also fig. 13, which might be a sub-section in conjunction with other parts of a folded speci- men, could be readily construed into a semblance of strong jointed legs, resembling the limuloid species. Mr. Wélcott’s theo- ries are formed from incised specimens of ‘‘casts of the exterior,” while my conclusions are the result of examinations made of ‘‘casts of the interior.” In our investigations, Mr. Wolcott and myself may be ina chameleon sense, right or wrong, as to the opinions we may form, being largely influenced by the circumstances which govern our actions in a similar manner —as several years ago — adiver- sity of opinion existed between Professors Billings, Woodward, Verrill and Dana. - Permit me to simply state that I think I have conclusive a dence, that “ trilobites did not swim on their backs,” they did not have stout jointed legs, they did not rest with their dorsal surface downwards, and they did not belong to the higher order of entro- mostracans. But more extended and fully explanatory views concerning the trilobite, will appear in a work I am now prepar- ing for the press. But whatever the result may be of our persevering labors, nat- ural science will no doubt be benefited by our efforts to solve what have been so long problematical statements. 120 Wisconsin Academy of Sciences, Arts, and Letters. It is said to be a trite saying of the Icelander, that the “sun shines on no country equal to his own.” In like manner we may boast or as Virgil, “sing praises,” not of “men and arms,” but of the richness and variety of the “paleozoic treasures of Mil- waukee County, and other counties contiguous thereto,” fora nat- uralist will examine with ecstatic delight, the unexcelled crinoids, as found in the quarries of Raeine, Waukesha, Bridgeport and Greenville. Probably in no other fossiliferous localities are there to be found such rich collections of Silurian echinodermata. Quite a number of them are delineated and described in part 8 of Hall’s Paleontology of Wisconsin, 1871. ; But since the publication of that work, more perfect specimens and new genera and species have been added to private collec- tions, like that of our worthy president, Dr. P. R. Hoy. If I claim.to have unravelled some of the many perplexing and doubtful theories concerning the organism of the trilobite, Presi- dent Hoy can claim equal success as regards the habits and inter- nal structures of Wisconsin Niagara Echinoderms. Although a large proportion of the crinoidea may be found at Racine, a majority of the Cystidea are found in Waukesha and Milwaukee counties. For Racine, besides her unsurpassed Echinoderms, has a won- derful genera, and species of other paleozoic fossils, trilobite heads and pygidia, equal to the largest size yet published or described. Specimens are found of the very peculiar Acidaspis, Dalmanites, Bronteus, Lichas, Spheroxochus, Lilenus, Calymene and Asaphus Flarpes. Exquisitively beautiful is the internal structure of several vari- ties of Cephalopods, that of the Orthoceras abnorme, with a si- phuncle, having a central siphuncle, composed of minute cyclindri- cal ramifications which reach to the outer walls of the siphon. Also several varities of the Orthocerta, like the O. angulatum, O. columnnre, O. crebescens, O. Laphami, on account of their pecu- liarly constructed chambers, bases or siphuncles, have some re- semblance to Hndoceras. Quite a number of the Gasteropods claim our attention, as the _Pleurotomaria occidens, Trochoceras costatum, Tremanotus, Tremano- tus alphenus, Pleurotomarial Hoyt and P. Halli. Fauna of the Niagara and Upper Silurian Rocks. 121 Principal among the Brachiopods are the Osotus conradt, Spirifer nobilis, Spirifer plicatella, Strophodonta pavfunda, Pen- tamarella ventrecosus, Pentamarus oblongus. In an inspection of the fossils of Hastern Wisconsin, it is naturally expected by every votary of natural science, that an identity of fossiliferous bearing rocks should be established with some age or period. ' But it appears from the published expressed opinions of those appointed to execute the geological state surveys, that there are many complications and difficulties intervening, in localizing, in accordance with established rules and methods, definite ages and periods, for the strata of rocks as exhibited in Hastern Wisconsin. In 1862, the first plausible or rational theories were published by Wisconsin legislative enactments concerning the parallelism of New York paleontology, with the same fossiliferous bearing rocks of the northwestern states, — more particularly the eastern por- tions of Wisconsin, ——especially Milwaukee, Racine and Wauke- sha counties. Notwithstanding the conclusions reached were far from satis- factory, still some system was established, which enabled the student of Paleontology to profit by his investigations, and may have been the means of stimulating such inquiries and experi- ments, as resulted in establishing a great commercial and profita- ble branch of industry, which may give to Milwaukee a reputa- tion for hydraulic cement products, second to none in the Union, and eventually first in the world. No doubt this most gratifying success was accomplished through the suggestions and persevering investigations of the late Dr. I. A. Lapham, one of the chief pioneers of natural history. SCIENCE IN WISCONSIN. Yet, a certain amount of credit is due to the Superintendent of the Geological Survey of Wisconsin (Prof. James Hall) of 1862, for the opinions he expressed in that work, and also for the theo- ries similarly advanced in Vol. III, Paleontology of New York, and part 3d, Paleontology of Wisconsin, 171, in the introductory chapters, having reference to the hydraulic cement character, of 122 Wisconsin Academy of Sciences, Arts, and Leiters. the calciferous formations of the Upper Silurian age of rocks, as exhibited in the vicinity of Milwaukee. Prof. Hall, also in his statements in Vol. I, Geology of Wiscon- sin, represents the strata of rocks lying above the Niagara, as the equivalent of the Salina or Onondaga Salt group of New York, or the Guelph, or Gault, of Canada, and the Le Claire, of Iowa. Notwithstanding, he was unable to trace the characteristic fossil, Hurypterus remipes of the Water-Lime Group. Similar views are expressed by him in his prefatory remarks in his paleontology of Wisconsin, also see Paleontology of New York, Vol. III Like- wise what are called, on page 72, Vol. I, Geology of Wisconsin, the upper Helderberg. and Hamilton groups, have proved to be what is ‘Geolocy-of ithe- Hamilton cement, of 8 ase, in Vok-ti-ot now termed’ Wiseonsing elit, 4 otelogy 05 1200 Cane An analytical examination of the pies sentiments of the authorsin Volumes first and second of Geology of Wisconsin, con- cerning the lithological character of the rocks containing the fauna of Wisconsin, especially its eastern portion, shows no very marked distinction or discrepancy, for their final summation respecting the area, the age, and periods, embracing the characteristic epochs, as generally admitted in American Geology. To the general student of Natural History, the previous class- ification established by Hall, on 447 page, of Vol. I, of Geology of Wisconsin, comprehensively covers the synonymous terms of Mayville and Byron beds, and upper and lower coral beds, lying below the Waukesha limestone. For the Hamilton cement, the Le Claire, the Racine and Waukesha limestones, embrace all the fauna belonging to that portion of the Upper Silurian, equivalent to the Salina, Lower Helderberg and Hamilton. Such an increase of synonyms has a tendency to embarrass the student in his study of paleozoic life, notwithstanding. Prof. Chamberlin, while reiterating the ideas advanced by Prof. Hall, has invested them, in a fuller and more interesting phraseology. But some facts concerning the quarries in Milwaukee county do not sub- stantiate the correctness of Prof. Chamberlin’s views, that the three classes of limestone, Mayville, Waukesha and Racine, lying above the Trenton period of rocks, were formed simultaneously. Fauna of the Niagara and Upper Silurian Rocks. 128 If we examine the lowest depths of the sole of Schoonmaker’s quarry, we find the same characteristic rock, containing the Zere- bratulous fossil, Gypidean occidentalis, belonging to the Byron division of the Mayville bed. This formation was quarried to some extent, and formed dressed stones, for bases to grave-stones, and window caps and sills. This stratum terminated abruptly in an ancient river bed, the bot- tom of which is smooth and polished, grooved and scratched by the drift of the glacial action or era, for huge granite boulders were excavated during the process of quarrying. Above this stratum, are regular even layers of a glazed, compact, metalic ringing, cherty limestone, of several inches in thickness, which is quarried in regular rectangular forms, and is utilized as a durable pavement on the side walks, or macadamized streets of Milwaukee and Waukesha. This formation was covered with ani- mal life, similar to that, so extensively intermixed in the strata or ' groups overlying it, and is well exhibited at every exposure of this rock, in all the quarries in Milwaukee, Racine and Wauke- sha counties. But the fauna which covered the surface of the Waukesha limestone, at Cook’s, Hadfield’s and Pelton’s, in Wau- kesha county, or Trimbone’s, Swan’s, Busack’s, Schwackhart’s and Story’s in Milwaukee county; or Ives’, Horlick’s and others, in Racine county; or Cook and Mc’Henry counties in Illinois, are in an exceedingly compressed stratum, and in many instances the fossils are in such a state as to be but little better defined, than well marked outlines of the original plant or invertebrate animal. In several of the quarries, as Story’s, Schewickhart’s, Busack’s and Cook’s, the Bryozoa, Cephalopoda, Gasteropoda, Brachiopoda and Crustacea, are so intensely compressed and distorted and glaz- ened as often to give the appearance of different genera or species. In seeking an elucidation of the age and character of the dolo- mitic formations in eastern Wisconsin, and in taking into consid- eration the totality of their surroundings, a plausible, perhaps a correct theory is established from these facts. Adopting the axi- oms, that the predominating fossil contents of rocks determine their age and character, we find lying above the regular strati- fied rocks of the Niagara period, and termed the Waukesha lime- \ 124 Wisconsin Academy of Sciences, Arts, and Letters. stone, soft, porous, and in places, easily disintegrated coral form- ations, termed by Profs. Hall and Chamberlin, coral reefs, which were formed on the top of sedimentary rocks, less than one hun- dred feet deep, in an ancient sea. That these coral reefs extended from the south of Kewaunee, Wisconsin, in a southerly direction, below Bridgport, Illinois; a distance of more than two hundred miles, and westerly, to Le Claire, Towa. . | That at certain points in Milwaukee, Waukesha, and Racine, these coral reefs became more prominent and formed, as termed by Prof. J. Dana, atolls, bordering on lagoons, which upon the receding of the ancient sea, formed the fiords vallies, now occu- pied by the numerous rivers of Wisconsin. Subsequently in the vicinity or same direction of these fiord vallies, glacial vallies were formed at frequent intervals for long lines of granitic boulders, of the Archean age are found, some measuring many tons, in size and weight; they no doubt had an agency in producing the grooves, scratches and polished sur- face, exhibited on the tops and sides of the ledges of the com- pact and fine grained limestone. The compressed condition of the fossils appears to be due to an upward pressure from an upheaval at the era of Silurian eruption, from which the same cause may have changed portions of the sedimentary dolomitic strata, either by igneous action or by solution into metamorphic beauti- ful calcite, or strontianite. Such a theory would account for the extraordinary compressed condition of fossil Cephalopoda, and other genera, and calcite crystals in the Waukesha lime- stone, and at the quarries in Wauwatosa, Racine and elsewhere in the state. An equally plausible theory is, that by a grad- ual submergence, or subsidence; and also from erosion, by the waves and currents of the ancient sea upon portions of the found- ation or base of the coral reefs, certain parts were undermined, caus- ing the superior portion of the rocks to tilt over and slide down in huge blocks, which give the appearance, upon exposure by quarrying, of an upheaval of the strata. Such causes, explain somewhat, the deep vertical fissures and seams, which permeate every portion of the Wauwatosa reefs, and this situation is taken Fauna of the Niagara and Upper Silurian Rocks. 125 advantage of by workmen, in the process of quarrying, by blast- ing and excavating. ; In certain parts of the reefs are coves, or pockets, which contain remains of distinct colonies of paleozoic life. For in one cove, you will chiefly find Foraminifera and Zoophyta. In another cove, the Brachiopoda; in another the Crustacea, and so on with each class and species of fossils. A similar state exists in other of the coral reefs; for the trilobites of Wauwatosa are not found at Waukesha. ‘The magnificent and peculiar Echinoderms of Racine, are not found in other reef formations; and the trilobite species, [llenus imperator, Illenus armatus, are found in the southerly reefs of Burlington, Bridgeport and Algonquin. From the foregoing considerations, aided by geological axioms and other published opinions of accepted paleontological authority, we offer these suggestions, as an effort to supply the “ missing links” in our research, as to the age, period and epoch, wherein once lived, moved and had a being, “the fauna of Niagara and Upper Silurian rocks, as exhibited in Milwaukee county, Wiscon- sin, and ijn counties contiguous thereto.”’ 126 Wisconsin Academy of Sctences, Arts, and Letters. DISCOVERIES ILLUSTRATING THE LITERATURE AND RELIGION OF THE MOUND BUILDERS. BY EDMUND ANDREWS, A. M.. M. D., Prof. of Surgery in Chicago Medical College. Looking back into the dawn of American history, we see certain figures stalking dim and phanton-like across the horizon. So unreal do they appear, that were it not for the massive earthworks they have left behind them, we might well disbelieve their ex- istence. Little by little we have gained information respecting them. They were miners and coppersmiths of considerable skill, but apparently wrought their metal solely by hammering, yet they occasionally had molten bronze chisels, which they probably im- ported from Mexico. They possessed shells from the sea, plates of mica from the Alleghanies, and Obsidian from the Rocky Moun- tains. They probably sent copper to Mexico, and in the graves of Yucatan have been found heads of their Lake Superior chloras- tralite. They were farmers, and cultivated broad fields with hoes and spades made of flint and wood. They wove cloth, made pot- tery, and erected earthworks of such enormous size and number as to astonish even the white men who now occupy their deserted cities. Their skeletons often exceed six feet in height, their skulls, which are generally brachycephalic, are flattened at the occupit like those of the modern Indians, but enclosed a large sized brain. This comprises nearly all that we have hitherto known about the vanished races. The exploration of the interiors of their mounds has generally been conducted in a very slovenly and inefficient way. It would seem that in sacrificial mounds, the builders were accustomed to deposit sacred records inscribed on stone, but so incomplete have been our examinations, that hitherto only a few of them have been _disinterred, and these more by accident than by any real skill of the discoverers. Literature and Religion of the Mound Builder's. 127 The first one that came to my knowledge was found in a town- ship called Savannah, on the Tennessee river, in the state of Ten- nessee. A mound existed here so broad that a company of cav- alry and all their horses, in the late war, encamped on its summit. Subsequently the men removed their tents from it and systemati- cally dug away the whole structure. A small slab of stone was found with a drawing upon it representing an altar with the body of some animal upon it enveloped in flames, while the sun was depicted above. It evidently represented a sacrifice to the deity residing in that luminacy. I have not yet succeeded in securing a copy of this stone. The second was near Rockford, Illinois. A large mound was examined there, and yielded a small stone of crystalline marble containing a figure of the sun supported as if on a pedestal, with a column of hieroglyphics on either side consisting of twelve char- acters, in all. A fac similie marked No. one, is transmitted with this paper. The left hand column shows at the top a segment of acircle. Next below is a trianyle, next a snake, a lizard, and last a flower. The right hand column consists of a sigmoid line, a line like the letter U, a minute cross, head of a rabbit, two objects whose significance I am unable to make out, anda fish. The disk of the sun has a human face drawn on it, and on the fore- head of the face is the disk of a crescent moon, with as much of an imitation of a face on the latter as there was room to portray. It may be remarked here that the Aztecs, according to Prescott, (Conquest of Mexico, vol. 1, p. 122), understood the agency of the moon in producing eclipses, and portrayed these events by drawing a moon on the disk of the sun. ‘This stone, therefore, may be the record of an eclipse. It is not possible yet to translate the twelve hieroglyphic signs upon it. The third discovery of this sort also occurred near Rockford. There were hieroglyphics found on some stones excavated from a mound, but I have not yet succeeded in obtaining a copy. The fourth inscribed object was an ornament of shell found in a Mound Builder's grave, near Hast St. Louis. It contained only four characters. The fifth discovery was made last month at Davenport, Iowa, 128 Wisconsin Academy of Sciences, Arts,\and Letlers. by the Rey. Mr. Gass, a trustworthy Lutheran clergyman, with his friends. Fac similes hae been sent me by Mr. Pratt, Secre- tary of the Davenport Academy of Sciences, and copies are sent herewith, numbered two, three and four. Numbers two and three are on opposite sides of the same stone. The drawing is exces- sively rude and far inferior to the work of some modern Indians. It is a sacrificial scene, taking place on the summit of a mound. At the bottom is the mound itself, on it blazes a large fire, and near it lie the bodies of three human victims. Around it standa circle of worshipers clasping each others hands, while the smoke curls upward from the flame. Above at the right hand is the sun; at the left hand is the moon, with a human face portrayed on its disk, and between are the stars, over all arches the sky. On the upper part of the slab are about one hundred characters, which are evidently a record of something which we at present cannot read. (The irregular line from the top to the bottom represents only a fracture in the stone). The opposite side of the same slab seems to be a rude repre- sentation of a wooded country, full of game of every description, which a few lucky hunters are killing with the greatest ease. There are deer, bears, buffaloes, fish, birds, and nondescript ani- mals, possibly intended for a musk ox and a turtle. As the op- posite side was a sacred scene, this side is probably a religious delineation also, and may, perhaps, represent the famous “ happy hunting grounds” of departed souls. Two-thirds of the way up the slab, a line of hieroglyphics runs across it containing, like the Rockford stone, twelve characters, four of which are identical with those on the Rockford stone. It is to be observed, also, that the two lines of characters carried along the arch of the sky on the other side of the slab, each contain twice twelve characters, and in fac similie number four, we again find twelve hieroglyphics, so that this number seems to have some special significance in their system. Number four shows a central round spot, surrounded by four concentric circles. Between the two outer circles are ranged very regularly the twelve hieroglyphic characters just mentioned. They are very hastily drawn as if the priests had long been fa- Interature and Religion of the Mound Builders. 129 miliar with them and only felt it necessary to slightly imitate the forms. Above are two round spots, intended, perhaps, to signify the sun and the moon. It seems difficult to avoid the impression that this inscription is some sort of a calendar. The stones lay one on the top of the other at the bottom of the mound, on the original surface of the ground, and were surrounded by a circle of small rounded stones, each about four inches in diameter. No one can inspect these fac similies without the conviction that we have before us rude specimens of literature, which some future investigation may yet translate. Meantime the sacrificial mounds should be ransacked in every part, instead of being care- lessly dug into, for the only hope of being able to translate these inscriptions rests on the discovery of more of them for compari- son and study. In concluding this paper I desire to call attention to some neg- lected evidences, which seem to indicate that the Mound Builders are not extinct, as popularly supposed, but still exist among our Indian tribes. Squier, after investigating carefully the mounds of western New York, found himself driven very unexpectedly to the conclusion that ‘‘ they were erected by the Iroquois, or their western neigh- bors.” Purchens, writing two hundred and fifty vears ago, said “The Troquois have no Townes: their dwellings and Forts are three or foure stories high, as in New Mexico.”’ Greenhalgh, one hundred years ago, made a statement about the commercial houses of the Senecas, which shows them to haye been somewhat like those of New Mexico in plan. Foster is of the opinion that the mounds thirty miles south- west of Natchez, were erected, by the Natchez Indians, and states that the trees on them were younger than on the adjacent grounds. Lasalle, nearly two hundred years ago, visited the Natchez In- dians, and his companion, Touty, says their town was surrounded by a strong earthwork, defended by stakes, on which were stuck the skulls of enemies ‘sacrificed to the sun. They also kept a perpetual fire burning on a mound forty-five feet high. They, therefore, made use of mounds and earth fortifications and sacri- 9 130 Wisconsin Academy of Sciences, Arts, and Letters. ficed human victims to the sun, like the Mound Builders of Daven- port. In fact they were Mound Builders themselves. The Smithsonian Reports state that at the bottom of a mound, near Savannah, an iron sword was found with an oak handle, in- dicating communication with white men. Bartram (Antiq. Southr. Indians, p. 131), says that in his day the Choctaws erected mounds over the collected bones of their dead, and that the chief, To-mo-chi-chi, pointed out the large mound in which were the bones of a chief who had entertained a great white man with a red beard, who came into Savannah river in a ship. It is well proved that the southern Indians, like the Mound Buiiders, possessed the art of weaving cloth, which Foster erro- neously attributes to the Mound Builders alone. I have just received a letter from the Rey. A. L. Riggs, a mis- sionary among the Nebraska Indians, respecting the use of earth- works among the western tribes. He says: “ Along the Missouri river, at least from Sioux City to its head, are many remains of villages and fortifications. They are all traceable to tribes now in existence, chiefly to Poncas, Rees, and Mandans, and were built within two hundred and fifty years. The large circular dirt houses still to be seen at Fort Berthold, among the Mandans and Gros-ventres, were once built by the Poneas, also. ‘“‘T remember the site of an old fort on the Minnesota river, near the Yellow Medicine. It was on the edge of the western bluffs. Three sides had been protected by a ditch, and probably by palis- ades. It enclosed, as I remember, an acre. This fort was said to have been built by the Pawnees, or else the Omahas. This was before the Dakotas occupied the country.” It appears, therefore, that a considerable number of tribes still exist, and some of them are now well civilized, who were Mound Builders when the white men first met them. These facts may destroy some of the poetry of the mounds, but we must look at things as they are. The theories of ethnology have grown too much under blue glass, swelling to an unhealthy size, which can- not be maintained under white sunlight. We shall get on faster, if we move slower. Interature and Religion of the Mound Builders. 131 The next grand effort should be to disinter more of this buried literature, and see whether by the study of it, some genuine knowledge of the past can be made to rise from these tombs. It is also necessary to make a thorough study of the dialects of those tribes, who seem to be descended from the Mound Builders, for they will furnish a necessary stepping stone to the interpreta- tion of the inscriptions, just as the study of Coptic was an essential pre-requisite to the translation of the Egyptian hieroglyphics. No. 6, Sixteenth street, Chicago, Feb. 8, 1877. 182 Wisconsin Academy of Sciences, Arts, and Letters. HOW DID THE ABORIGINES OF THIS COUNTRY FABRICATE COPPER IMPLEMENTS. BY P. R. HOY, M.D., President Wisconsin Academy of Sciences. I propose to consider the manner in which the ancient inhabitants of this country fabricated those curious copper implements which the plow and spade turn up all over Wisconsin and the adjacent states. These copper tools are objects of great interest to the archaeologist, and it is a matter of pride that the Wisconsin His- torical Suciety has the largest and best collection to be found in any state. A few of the specimens, upon a superficial examination, seem to be cast. This point will first be considered: Did these pre- historic people possess the skill and intelligence requisite to cast articles of pure copper ? Before a cast can be made, it is necessary to have an exact copy moulded, either in sand, plaster, clay, metal, or other suitable substance. The formation of sand moulds is by no means so simple an affair as it seems at first thought. It requires long practical experience to overcome the disadvantages attendant upon the materials used. The moulds must be sufficiently strong to withstand the action of the fluid metal perfectly, and at the same time to permit the egress of the gases formed by the action of the metal on the sand. If the material is air-tight, then danger would come from pressure, arising from the rapidity of the generating of the gases, and the casting would be spoiled, and probably the operator injured. If the gases are locked up within the mould, the general result is what moulders term blown casting, that is, the surface becomes filled with bubbles of air. The preparation of sand and loam used in forming the mould must be carefully con- sidered. The greater the quantity of sand the more easily will the gases escape and the less liability is there of fracture of the casting. On the other hand, if the loam predominate, the im- pression of the pattern will be better, but a far greater liability of injury to the casting will be incurred from the impermeable na- ture of the moulding material. In moulding an accurate pattern Copper Implements. 133 must be made, generally in two or more parts. Pattern making involyes much knowledge and skill. I enumerate these difficulties in order to show that it was not likely that 2 rude people possessed that amount of knowledge and skill adequate to overcome these obstacles. I pass over all other modes of forming moulds, and speak only of those formed in stone. Almost all savage tribes possess the skill to fashion stone into various tools, and we are forced to ad- mire the workmanship displayed in working the hardest materials, such as flint, quartz, granite, greenstone, etc. In contemplating these evidences of patient toil, we are assured that they could readily work out suitable moulds in stone in which castings might be made. Copper is a refractory metal, which melts at from 2200 to 2600 degrees, a temperature that can be reached only ina furnace, as- sisted by some form of coal and an artificial blast. We must have good evidence before we assert that these dwellers by the lake possessed these indispensable auxiliaries to successful work- ing in metals. ‘Copper, when melted, is thick and pasty, and without the addition of some other metal, will not run into the cavities and sinuosities of the mould.” In consulting with an intelligent and skillful brass-founder, I was shown a hammer weighing three pounds, cast of pure copper, and was assured that this was the smallest casting he could make of this metal. The addition of one pound of zine to ten of cop- per makes an alloy that will melt at less than half the tempera- ture of copper, and will flow freely. In casting im copper it is positively necessary to put the ma- terials in a crucible, and that the surface of the melting mass be covered with a flux in order to effectually defend the melting metal from the action of the atmosphere. A word about crucibles. The manufacturing of good crucibles, such as will withstand the heat necessary to melt the more re- fractory metals, involves such a degree of knowledge, that for many generations the entire civilized world was dependent on a small section of Germany; and even now Hessian crucibles are unsurpassed. In England there are now several manufactories 184 Wisconsin Academy of Sciences, Arts, and Letters. which turn out excellent articles, one in London which makes the celebrated Plumbago crucible. It will sufficiently indieate the difficulties involved, when I state that America, to-day, is de- pendent upon Europe for the immense number of crucibles used in this country. Iam aware there is a manufactory established in Connecticut, but the quality is so inferior that they are only used for the more easily fused metals. I experimented with frag- ments of pottery taken from the ancient mounds near Racine, in order to determine the degree of heat they would stand. The result was they were melted long before the copper was — fused. A majority of copper implements found have specks or points of pure silver scattered over their services. I am prepared to prove by the best authority in America, James ©. Booth, and Thomas H. Garrett, U. S. assayers at Philadelphia, that one sin- gle speck of pure silver, visible even with the microscope, is positive evidence that the specimen was never melted. Copper unites intimately with nearly all metals, thus form- ing homogeneous alloys — with zine forming brass, with tin, bronze, and so on. The only apparent exception to this law is where large masses are fused and at rest fora long time. In these cases the heavier metals gravitate and separate more or less, but never perfectly. When large brass cannon are cast, in consequence of the great quantity of metal fused, together with the additional circumstance that the mould is made in the earth and hence re- quires days to cool, “blotches of lighter color are occasionally: found on the surface of the guns, indicating a segregation of the metals. A fibrous texture is another evidence that these imple- ments were hammered or rolled out. This (brous quality is well exhibited by the action of strong acids on the Specimens. On articles that are cast, the acid acts in a uniform manner, revealing no striae or hard bands. The absence of the slightest indication of a sprue—the opening where the metal is poured — is also, to say the least, suggestive. We certainly would expect to find in- dications of this necessary blemish in specimens so carelessly fin- ished that the mould marks remain conspicuous. If these pro- jections are the remains of the imprint of the mould, the specimen Copper Implements. Dies is of recent casting, for it is evident that these delicate marks would be the first to be corroded by the tooth of time. I make a short extract from a paper entitled “The Ancient Men of the Great Lakes,’ read by Henry Gilman at the Detroit meeting of the American Association for the Advancement of Science. Mr. Gilman isa close observer, and an accomplished archaeologist, and has made the ancient mines of Lake Superior aspecialty. He says: ‘I cannot close, however, without express- ing my wondering admiration of a relic, which, taken in connec- tion with our former discoveries, affords some of the most import- ant evidences of the character of the ancient miners, the nature of their work, and the richness of the mineral field selected for their labors, at Isle Royale. On cleaning out of the pit the ac- cumulated debris, this mass was found at the bottom, at the depth of sixteen and one-half feet. Itis of a crescent-like shape and weighs nearly three tons, or exactly 5,720 pounds. Such a huge mass was evidently beyond the ability of those ancient men to remove. They could only deal with it as best they knew how. And as to their mode of procedure, the surroundings in the pit, and the corrugated surface of the mass itself, bear ample testi- mony. The large quantities of ashes and charcoal lying round it show that the action of fire had been brought to bear onit. A | great number of the stone hammers, or mauls, were also found near by, many of them fractured from use. With these the sur- face of the mass had evidently been beaten up into projecting ridges and broken off. The entire upper face and sides of the relic present repeated instances of this; the depressions, several inches deep, and the intervening elevations with their fractured summits covering every foot of the exposed superficies. How much of the original mass was removed in the manner described, it is of course impossible to say. But from appearances, in all probability it had at least been one third larger. Innumerable fragments of copper chips lay strewn on all sides, and even the scales of fish, evidently the remnants of the meals of the miners, were recovered from the pit.” Mr. Gilman was asked if there were in or about any of these ancient mines any indications of the copper having been melted. He replied: ‘Not the least.” And now, were not these innumer- 136 Wisconsin Academy of Sciences, Arts, and Letters. able copper chips that were strewn on every side additional evi- dence that these ancient men know nothing about casting in copper? ‘Those fragments would have been the most suitable to melt, as in all metals the smaller the fragments the more easily they melt. It is evident that those chips, being too small to make any form of their implements, were abandoned as useless. Finally, How were they made if not cast? I believe that I have the key, and can fabricate any form of these ancient imple- ments so exactly as to deceive even my learned friend, Dr. Butler.* These ancient Indians, for I believe they were Indians, used fire in their mining operations. The vein-rock was made hot by building a fire on or against it; then, by dashing on water, the rock would not only be fractured, but the exposed pieces of copper be softened, so that it could be beaten into shape. Then the metal became hard, in consequence of its being pounded; it was again heated and plunged into cold water; for copper is, in this respect, the opposite of steel; the one is softened, while the other is render- ed hard. In this way copper was fashioned simply by pounding. ' In addition to the hammering process, cylindrical articles were evidently rolled between two flat rocks, which is the manner in which several of the articles in the historical collection might be made. Some of those implements that have been supposed to be cast, were, I think, swedged; that is, a matrix was excavated in stone, into which the rudely fashioned copper was placed, and then by repeated blows the article would be made to assume the exact shape of the mould. Nearly all those plano-convex arti- cles could be made in thismanner. Of twenty axes taken from mounds near Davenport nearly three-fourths were of this pattern. I will repeat a few lines of an interesting paper read at the De troit meeting of the American Association, by R. H. Farquharson, on “ Recent Explorations of Mounds near Davenport, Iowa.” “The Davenport collection of copper implements consists, at present, of twenty axes, six of which were more or less covered with cloth, four copper awls or borers, over one hundred beads, and a curiously spoon-shaped implement. The axes are all of two forms, one plano-convex, the other with flat sides. They are *Dr. Butler, who was present, has held strongly for the casting of these copper tools.— ED Copper Implements. 137 all cold-wrought by hammering. Some retaining the original scales or lamina on the surface; none of them show signs of use, and are notably harder on the edge than elsewhere.” All of these interesting implements are figured in the proceed- ings of the American Association at the Detroit meeting, page 304. We can learn more from this Davenport collection than from any other, because of the perfect condition of The specimens, be- ing unused and in some degree protected by their coverings. Besides this half swedging process, I am persuaded that, in a few instances at least, there was a complete mould worked out in halves, on the face of two flat stones, so that by placing a suitable piece of copper between them and giving it repeared heavy blows the copper was made to fill the mould accurately. Last September, while watching some workmen engaged in fill- ing the cribs of the harbor pier with stone, my attention was directed to a slight excavation on the face of a large granite boulder. On careful inspection I found that it was undoubtedly the work of man; although but a partof the excavation was left, the rock having suffered fractures, there was enough, neverthe- less, to enable me to make out the original form. We attempted to chip off the specimen with a heavy stone hammer, but failed, as the cleavage was in the wrong direction, and the mould was obliterated. I however worked out a pattern as nearly accurate as I could, representing the excavation. I took this pattera to a stone cutter, for the purpose of having a mould cut in granite. Upon consultation it was decided that the mould would have to be cut in halves in large granite boulders in order to insure suc- cess, which would be costly and incoavenient, and for the pur- pose of illustrating the subject it would be as well to havea mould cast in iron. This was done, and a beautiful ax swedged out of cold native copper was the result. This cylindrical speci- men* was made out of a piece of float copper, hammered with a stone ax into partial shape, and then finished by rolling between heavy flat stones. (The author exhibited plain convex and double convex hatchets, as well as a long cylindrical implement tapering regularly from the centre to the point, that were fabricated by him in the man- — ner stated). ©The specimens referred to was exhibited to the Academy. 188. Wisconsin Academy of Sciences, Arts, and Letters. REMARKS ON THE DESCENT OF ANIMALS. BY PROF. H. OLDENHAGE, MitwavKkezez. Whether species ‘are constant and have been created with the same specific characteristics they now possess, or whether they are variable and have desended from common ancestors, is the point at issue between the defendants of special creation and the evolu- tionists. Since Linne first introduced the idea of species into Botany and Zoology, many attempts have been made to define in an exact mauner, what we are to understand by the term species; but when a systematizer underakes to apply these definitions, it is at once seen that they are either glittering generalities, or unmean- ing phrases. Among the most recent, and no doubt the ablest of these attempts, is Agassiz’s ‘‘ Hssay on Classification,” the dogmat- ism and fulitity of which, Heckel has so thoroughly exposed in his “ Generelle Morphologie.” ‘ven before the appearance of Darwin’s work on the ‘Origin of Species,’” says Oscar Schmidt, “‘ Carpenter, in the course of his researches on the Foraminifera, arrived at the conclusion, proved in special instances, that in this group of low organisms, which secrete the most delicate calcareous shells, there could be no ques- tion of “species,” but only of “series of forms.” Forms which the systematizer, had reduced to different genera and families, he beheld developing themselves from one another” (Descent and Darwinism., p. 92). But as these Foraminifera are “‘so simple in structure, and so little is known of their individual development, the defenders of the persistency of species might claim, that Carpenter's series of forms are mere varieties, and only prove that the true ‘species’ have not yet been found.” To determine this. point, however, the researches of Oscar Schmidt and Heeckel, on sponges, have been of the greatest importance. Oscar Schmidt shows, that “ we arrive gradually at the conviction, that no rea- sonable dependence can be placed on any ‘characteristic;’ that with a certain constancy in microscopic constituents, the outward - Remarks on the Descent of Animals. 139 bodily form, with its coarser distinctive marks, varies beyond the limits of the so called species and genera; and that, with like external habits, the internal particles which we looked upon as specific, are transformed into others, as it were under our hands.” “ Any one,” thus concludes this section of Schmidt’s work on the Fauna of the Atlantic Sponges, ‘who with regard to sponges, makes his chief business the manufacture of species and genera, is reduced ad absurdum, as Heeckel has shown with exquisite irony in his Prodrome to the Monograph in the Calcareous Sponges.”’ ‘In my specific researches,’’ continues Schmidt, “I confined myself essentially to the siliceous sponges, and by thousands of microscropic observations, by measurements, by drawings, by facts and inferences, have produced evidences, which acute oppo- ~nents of the immutability of species had not brought forward before me, that in these sponges, species and genera, and conse- quently fixed systematic unities in general have no existence. The other division of the same class, the calcareous sponges, had been treated with unrivaled mastery by Haeckel in his mono- graph.” Heckel was not only able to confirm Oscar Schmidt’s state- ments, ‘‘ but, owing to the smaller compass and the greater facil- ity of observing the groups selected for study, to advance with more sequence and continuity, from the observation of details to the whole, to portray its morphology, physiology, and evolution- ary history, with the utmost completeness.’”” He sums up his. con- clusions as follows: (Preface to American Hdition of History of Creation, p, 15.) ‘ For five consecutive years I have investigated this small but highly instructive group of animals in all its forms in the most careful manner, and I venture to maintain that the monograph, which is the result of these studies, is the most com- plete and accurate morphological analysis of an entire organic group, which has up to this time been made. Provided with the whole of the material for study, as yet brought together, and as- sisted by numerous contributions from all parts of the world, I was able to work over the whole group of organic forms, known as the Calcareous Sponges, in the greatest possible degree of full- ness, which appeared indispensable for the proof of the common 140 Wisconsin Academy of Sciences, Arts, and Letters. origin of its species. This particular animal group is especially fitted for the analytical solution of the species problem, because it presents exceedingly simple conditions of organization ; because in it, the morphological conditions possess a greatly superior, and the physiological conditions are inferior, in part, and because all species of the Calcispongiz are remarkable for the fluidity and plasticity of their form. With a view to these facts, I made two journeys to the sea-coast (1869 to Norway; 1871 to Dalmatia), in order to study as large a number of individuals as possible, in their natural circumstances, and to collect specimens for compari- sons. Of many species, I compared several hundred individuals in the most careful way. I examined with the microscope, and measured in the most accurate manner, the details of form of all the species. As the final result of these exhaustive and almost end- less examinations and measurements, it appeared that ‘good species,’ in the ordinary dogmatic sense of the systematists, have no existence at all among the Calcareous Sponges; that the most different forms are connected, one with another,-by numberless gradational transition forms; and that all the different species of Calcareous Sponges are derived from a single exceedingly simple ancestral form, the Olynthus. If we take for the limitation of genera and species, an average standard, derived from the actual practice of naturalists, and apply this to the whole of the Calcare- ous Sponges at present known, we can distinguish about 21 genera with 111 species. [I have however, shown that we may draw up, in addition to this, another systematic arrangement, which gives 29 genera and 289 species. A systematist, who givesa more lim- ited extension to the ideal species, might arrange the same series of forms in 43 genera, and 381 species, or even in 113 genera and 590 species ; another systematist, on the other hand, who takes a wider limit for the abstract ‘‘ species,” would use in arranging the same series of forms, only 3 genera, with 21 species, or might even satisfy himself with 2 genera and 7 species. This appears to be so arbitrary a matter, on account of endless varieties and transi- tional forms in this group, that their number is entirely left to the subjective taste of the individual systematist.” “In point of fact,” he continues, “I haye a right to expect of Remarks on the Descent of Animals. 141 my opponents, that they shall carefully consider the exact ‘em- pirical proof’ here brought forward for them, as they have so eagerly demanded. May they, however, spare me the empty, though by even respectable naturalists the oft repeated phrase, that the monistic nature-philosophy, as expounded in the ‘Gen- eral Morphology,’ and in the‘ History of Creation,’ is wanting in actual proof. Precisely that exact form of analytical proof, which the opponents of the direct theory demand is to be found, by any- body who wishes to find it, in the ‘ Monograph of the Caleareous Sponges.’”” “This mutability of the Spongiadee”’ adds Oscar Schmidt, “affords the extremely important evidence that, so to speak, an entire class has even now, not attained a state of com- parative repose.” But to prove the variability of species satisfac- torily, ‘‘the transition of the forms succeeding one another his- torically in the strata of the earth” must be shown. The researches of Waagen, Zittel, Neumayr and Wiirtenberger have proven, in the most conclusive manner, “at least with respect to the important division of the Ammonites, the utter im- possibility of separating them into species.” ‘“ Neumayr is such a cool and cautious observer, that he allows nothing to pass current, but that which is absolutely certain.”’ It is trne he holds it to be ‘extraordinarily probable, that in al] forms these gradual trans- itious have taken place, yet in one case only does he demand un- qualified assent; namely, that he has proven ‘that Perisphinctes aurigerus of the Bathoniaus, and Perisphinctes curvirostris of the zone of the Cosmoceras Jason, are connected in such a man- ner by intermediate occurrences that it is impossible to draw a limit.’ ” Wiirtenberger’s studies were applied to thousands of specimens from the groups of the Planulate Ammonites, with ribbed shells, and of the Armate Ammonites with prickly shells. In summing up his results he says: ‘‘In groups of fossil organisms, in which, as in the present case, so many connecting links between the most extreme forms are actually before us, that the transition is regu- larly carried on, the species is far less susceptible of apprehension than in the organic forrus of the present world, which at least de- note the existing limits of the great pedigree of the organic world. 142 Wisconsin Academy of Sciences, Arts, and Letters. With respect to these fossil forms, it is fundamentally indifferent whether a very short, or a somewhat longer portion of any branch be honored by a special name, and looked upon asa species. The prickly Ammonites, classified under the name Armata, are so in- trinsically connected, that it becomes an impossibility to separate sharply, the accepted species from one another. The same obser- vation applies also to the group of which the manifold forms are distinguished by their ribbed shells, and termed Planulata. This is sufficient to show why modern inquiry “sets aside the phantom of ‘species,’ and to judge what series of observations are opposed to the assertion, that in no single case has evidence been given of the transition of one species into another.” ‘ The fact is,’ says Huxley, “that if the objections which are raised to the general doctrine of evolution were not theological objections, their utter childishness would be manifest even to the most childlike of believers.’ ” “Scarcely a single fact,” says that most careful observer Neu- mayr, ‘‘speaks more decisively in favor of the correctness of the theory of descent, than the existence of series of forms in the man- ner in which they have already been proved in many cases, and will, no doubt, be now found more frequently, since attention has been called to this point.’ ”’ But it is not only among the lower animals that these transition forms have been found. Even among vertebrates, and what is the more important, between those classes, orders and families, which at present are separated very widely from one another, these con- necting links multiply almost daily, bearing in mind, of course, the great imperfection of the geological record. “The class of birds and reptiles as now living,” says Prof. Marsh, of Yale College, to whom paleontology owes so many im- portant discoveries, “are separated by a gulf so profound, that a few years since it was cited by the opponents of evolution as the most important break in the animal series, and one which that doctrine could not bridge over. Since then, as Huxley has clearly shown, this gap has been virtually filled by the discovery of bird- like reptiles and reptilian birds.’ ”’ In 1860, shortly after the appearance of Darwin's “ Origin of Remarks on the Descent of Animals. 148 Species,” a remarkable bird was found in the lithographic slates of Solenhofen, Bavaria, the head of which was unfortunately crushed beyond recognition. Recently, however, another specimen has been found in the same formation, at Hichstadt, Bavaria, with a well preserved head. The celebrated comparative anatomist, Owen, of London, described this bird and called it Archaeopteryx. “There is this wonderful peculiarity about this creature, that so far as its feet are known, it has all the characters of a bird, all those peculiarities by which a bird is distinguished from a reptile. Nevertheless, in other respects, it is unlike a bird and like a rep- tile. There is a long series of caudal vertebrae. The wing differs in some very remarkable respects from the structure it presents in a true bird. In a true bird the wing answers to the thumb and two fingers of the hand, the metacarpal bones are pressed together into one mass, and the whole apparatus, except the thumb, is bound up in a sheath of integument, and the edge of the hand carries the principal quill feathers. It isin that way that the bird’s wing becomes the instrument of flight. In the archaeop- teryx, the upper arm bone is like that of a bird; the two forearm bones are more or less like those of a bird, but the fingers are not bound together — they are free, and they are all terminated by strong claws, not like such as are sometimes found in birds, but by such as reptiles possess; so that in the archaeopteryx we have an animal which, to a certain extent, occupies a place mid- way between a bird and areptile. It isa bird so far as its foot and sundry other parts of its skeleton are concerned ; it is essen- tially and thoroughly a bird, in the fact that it possesses feathers ; but it is much more properly a reptile, in the fact that what rep- resents the hand has separate bones resembling that which termi- nate the fore-limb of a reptile. Moreover, it had a long tail with a fringe of feathers on each side. From this description it is seen that the archaeopteryx is about three-fourths bird and one-fourth reptile.” Prof. Marsh has found during the last few years very remark- able forms of birds in the Chalk of Kansas. In the Hesperornis, ‘says Marsh,” “we have a large aquatic bird, nearly six feet in length, with a strange combination of characters. The jaws are pro- 144 Wisconsin Academy of Sciences, Arts, and Leilers. vided with teeth set in grooves; the wings were rudimentary and useless, while the legs were very similar to those of modern diy- ing birds. Ichthyornis, a small flying bird, was stranger still, as the teeth were in sockets, and the vertebrae biconcave, as in fishes and a few reptiles.” “Tt is obvious,” says Huxley, “that the contrast between the crocodile’s leg on the one hand, and the bird’s leg on the cther, is very striking. But this interval is completely filled up when you study the character of the hinder extremities of those ancient reptiles which are called the Dinosauria. In some of these, the bones of the pelvis, and those of the hind limb, became extraordi- narily similar to birds, especially to those of young or foetal birds. Furthermore, in some of these reptiles, the fore-limbs become smaller and smaller, and thus the suspicion naturally arises, that they may have assumed the erect position. That view was en- tertained by Mantel, and was also demonstrated to be probable by your own distinguished anatomist, Leidy, but the discoveries of late years show that in some of these forms the fact was actually so; that reptiles once existed which walked upon their hind-legs as birds now do. The Compsognathus longipes (Wagner) must as- suredly have walked about upon its hind-legs, bird’fashion. Add to this feathers, and the transition would be complete.” It is now generally admitted by biologists “‘ who have made a study of the vertebrates,” continues Marsh, “that birds have come down to us through the Dinosaurs, and the close affinity of the latter with recent struthious birds will hardly be questioned. The case amounts almost to a demonstration, if we compare with Di- nosaurs, their contemporaries, the Mezozoic birds. Compsognathus and Archaeopteryx of the old world, and Ichthyornis and Hes- perornis of the new, are the stepping-stones by which the evolu- tionist of to-day leads the doubting brother across the shallow remnant of the gulf, once thought impossible.” Although this kind of evidence is far weightier than that upon which men generally base their conclusions regarding important propositions, it is not that kind of evidence which might be called demonstrative. That is to say, it might be demanded “ that we should find the series of gradations between one group of animals Remarks on the Descent of Animals. 145 and another in such order as they must have followed if they had constituted a succession of stages, in time of the development of the form at which they ultimately arrive.” In short, it would have to be shown, that, with reference to birds and reptiles, for instance, ‘‘that in some ancient formation reptiles alone should be found; in some later formations birds should first be met with; and in the intermediate strata we should discover in regular suc- cession the forms which are intermediate between reptiles and birds.” . Precisely this kind of evidence has of late years been accumu- lating rapidly respecting many groups of the animal kingdom. The development of the horse offers us, perhaps, the best illustra- tion of this kind of evidence, and J give the substance of “ these thoroughly and patiently worked-out investigations of Prof. Marsh,” in his own words. Hesays: ‘I have unearthed with my own hands not less than thirty distinct species of the horse tribe, in the tertiary deposits of the west alone. “The oldest representation of the horse at present known is the diminutive Hohippus, from the lower Kocene. Several species have been found, all about the size of a fox. Like most of the early mammals, the ungulates had forty-four teeth, the molars with short crowns, and quite distinct in form from the premolars. The ulna and the fibula were entire and distinct, and there were four well-developed toes, and the rudiment of another on the fore-feet, and three toes behind. In the structure of the feet and in the teeth, the Hohippus indicates unmistakably that the direct ances- tral line to the modern horse has already separated from the other perissodactyles. In the next higher division of the Hocene, an- other genus (Orohippus) makes its appearance, replacing Hohip- pus, and showing a greater, although still distant, resemblance to the equine type. The rudimentary first digit of the fore-foot has disappeared, and the last premolar has gone over to the molar series. Orohippus was but little larger than Hohippus; in most other respects very similar. Near the base of the Miocene, we find a third: closely allied species, Mesohippus, which is about as large as a sheep, and one stage nearer the horse. There are only three toes and a rudimentary splint bone on the fore-leg, and 10 146 Wisconsin Academy of Sciences, Arts, and Letters. three toes behind. ‘Two of the premolar teeth are quite like the molars. The ulna is no longer distinct, or the fibula entire, and other characters show clearly that the transition is advancing. In the upper Miocene Mesohippus is not found, but in its place a fourth form, Miohippus, continues the line. The three toes in each foot are more nearly of a size, and a rudiment of the fifth metacarpal bone is retained. All the known species of this genus are larger than those of Mesohippus, and none pass above the Miocene.”’ “The genus Protohippus of the lower Pliocene is far more equine, and some of its species equalled the assin size. There are still three toes on each foot, but only the middle one, corre- sponding to the single toe of the horse, comes to the ground. In the Pliocene we have the last stage of the series before reaching the horse, in the genus Pliohippus, which has lost the small hoof- ‘lets, and in other respects is very equine. Only in the upper Pliocene does the true Equus (horse) appear and complete the genealogy of the horse, which in the post-tertiary roamed over the whole of South and North America, and soon after became extinct. Besides the characters I have mentioned there are many others in the skeleton, skull, teeth, and brain of the forty or more intermediate species, which show that the transition from the Kocene Eohippus to the modern horse has taken place in the order indicated, and I believe the specimens now at New Haven will demonstrate the fact to any anatomist. ‘They certainly car- ried prompt conviction to the first of anatomists (Huxley), whose genius had already indicated the later genealogy of the horse in Europe, and whose own researches so well qualified him to appre- ciate the evidence here laid before him.” Basing his conclusion on these facts, Huxley says: ‘‘ The doctrine of Evolution at the present time rests upon exactly as secure a foundation as the Copernican theory of the motion of the heavenly bodies. In fact, the whole evidence is in favor of Evolution, and there is none against it.” Another class of facts, considered equally conclusive in favor of the Theory of Descent, are the results of Embryology. Norz.— Prof. Oldenhage had only written thus far when he was seized with an illness which speedily terminated a most promising life. Why Are There No Upper Incisors in the Ruminatia? 147 WHY ARE THERE NO UPPER INCISORS IN THE RUMINANTIA ? BY P. 2. HOY, M. D., PREST. ACADEMY. In studying the anatomy and physiology of animals, we become intensely interested in the various modifications of parts, so as to exactly fit them, to perform the office assigned them. In other words, the structures are so altered as to correspond to the mode of life which the animal pursues. Perhaps no part of vertebrates is as significant as the apparatus of the mouth, for obvious reasons, as it performs an important part in nutrition, the function which strikes at the very founda- tion of life. Every vertebrate has his 67 of fure written in indelible charac- ters on his teeth. They not only indicate the food on which the animal subsists, but with few exceptions, the mode of procuring that food, as well. All those animals having no incisors in the upper jaw, and pro- vided with eight placed obliquely outward in the lower jaw, have evenly divided hoofs, complicated stomachs, and chew the cud. I am satisfied that there isa deep meaning conveyed in the absence of upper incisors in ruminantia, if the fact is correctly interpreted. In the first place, all true ruminants have a prehensile tongue. We will take one of the most familiar examples, the cow, and what is true of this domestic animal, will apply equally well, not only to the entire boss family, but with slight modification, to the entire ruminantia. The tongue is large and muscular, weighing from three to five pounds, the upper surface, dorsum, is covered with a dense, almost horny skin, especially at the point; the mucous coat, covering the tongue and lingual glands, pours out an abundance of mucus and saliva to keep the organ moist and plia- ble. itis capable of being thrust out beyond the lips to the dis- tance of from six to eight inches. In protruding the tongue it Is pressed firmly against the hardened gum of the upper jaw, then it 148 Wisconsin Academy of Sciences, Arts, and Letters. is coiled around the morsel, the tongue curves upwards bringing the food into the mouth rasping, as it were, the upper jaw. In grazing, the tongue is lapped around a wisp of grass, which is brought into the front of the mouth, and held in its grasp against the upper jaw, when by a quick motion of the head, the sharp chisel-teeth in the under jaw, clip off the herbage. In these motions we see the great advantage of the outer direction of the under incisors. In studying these movements of the tongue, we become con- vinced that upper front teeth would not only seriously interfere with its motion in protrusion by lacerating its upper surface, but would positively arrest the morsel against the upper incisors, if there were any, and thus impose a barrier against the use of the tongue in prehension. In the deer tribe, cervidae, the tongue is longer in proportion to its weight, than in the ox. Deer are mostly browsing animals, feeding on leavesand branches of shrubs and small trees; for this purpose the long flexible tongue is especially well adapted. Deer have the longest tongue of any of the ruminants, if we except the giraffe, whose tongue is simply enormous. With its extensive tongue, and long neck, this singular animal is enabled to reach branches of considerable elevation. Antelopes, for the most part, have moderately sized tongues, yet not a few have the organ largely developed ; in fact the tongues vary nearly as much as do these ill-assorted animals themselves. For the genus antelope is a kind of zoological retreat for the re- ception of those outcast hollow-horned ruminants which do not belong, either to the ox, sheep, or goat species. Goats have a moderately developed tongue, fully capable, how- ever, of procuring food in the same manner as the preceding tribes. Sheep have this organ less developed than in any other of the true ruminants. It is capable of being protruded not over three inches beyond the lips. In grazing on short pasturage, the point of the tongue is only used to fix the short grass to the upper gum, while the under teeth are made to sever the herbage. In our wild sheep of the Rocky mountains, ovis montana, the tongue is more developed than in the domestic animal. Is it not more than prob- Why Are There No Upper Incisors in the Ruminantia? 149 able that the domestic sheep, having been confined to short past- ure for a long series of generations, have lost, in length, a portion of their tongues ? In the camels, including the lamas, there is a wide departure from the typical ruminants. In fact anatomically, the camel fami- ly show a marked affinity to the pachyderms. They stand on the border line of the ruminants where they join the pachydermata, possessing characteristics of each. Their lips are large and fleshy, the upper one cleft. ‘Their dentition is peculiar, the young pos- sessing a full set of incisors in the upper jaw, which fall out as the animal approaches maturity, save the two latter ones, which are permanent. We have here perfect corresponding relations between the im- perfect set of upper front-teeth and the partly prehensile tongue which they possess. The lips and tongue are nearly equally use- ful in seizing and conveying food to the mouth. On the lowest round looking up towards the ruminants, stand the kangaroos. These herbivorous marsupials do chew the cud, though imperfectly, as they possess saculated stomachs approach- ing the multiple condition of the typical ruminants. It is inter- esting to find that these wonderful animals, of a wonderful country, do not possess a prehensile tongue, but have instead, a full, strong set of incisors in the upper jaw. Here we have then, one of the best proofs that the use of the tongue regulates the presence of incisors. Insectivorous edentata, embracing the armadillos, and ant-eaters of South America, and the Panoglins and Ard-vark of India and Africa — in these quadrupeds, the tongue is long and cylindrical, and is protruded directly forwards, so that front teeth in either jaw, would interfere with the necessary rapid motions of the tongue in feeding. Hence, the total absence of front teeth in either jaw, and in fact the ant-eaters have no teeth whatever, being strictly edentate. These animals furnish us with another proof that prehensile tongues are antagonistic to front teeth. Tf a prehensile tongue be cylindrical, then we will have a total absence of front teeth; if flat and coiled upward in using, then we will find incisors only in the under jaw. 150 Wisconsin Academy of Sciences, Arts, and Letters. § [May it not be true that the absence of upper incisors in the ru- minants, and the total want of front teeth in the edentata, are the result of long ages of disuse, accompanied with the almost con- stant friction and presure against them, which might injure and ultimately destroy the germs of the useless teeth, until their absence becomes an hereditary peculiarity, as a final result? Boiler Haplosions. 151 BOILER EXPLOSIONS. BY CHAS. I. KING, Szaperintendent University Machine Shop. In considering the subject of Boiler Explosions, I am aware that it has heretofore received the attention of many able theorists and mechanical engineers who do not agree in their conclusions. That such diversity of opinion exists, is natural from the various conditions of the matter discussed. What is here prepared may not be new, but the subject is of such vast importance, that even repetition may be pardonabie. If we fora moment consider the field, we find that its extension precludes comprehending the whole in one short paper, which covers thé subject proportionally, as the hand might cover a table. That the astonishing developments, attained by the use of steam in the various industries throughout the country, must be ascribed to its universal success as a moderately cheap prime mover none can deny; and the facility with which it can be em- ployed in any section of the land enables the manufacturer to locate his mills wherever desirable, and then transport to them the mo tive power. Without it, he must be content with the water courses wherever they may be found, and ever after transport the material of man- ufacture to and from the market. Without it many of our large cities and manufacturing centers could not exist to-day. Only while it is considered less danger- ous or less expensive than other agents, can steam maintain its now prominent position of principal motive power for nearly all branches of manufacture, transportation, ete. There are considerations in connection with the present methods of utilizing steam, which, looked upon from every point, would indicate clearly that we are justified by no means in accepting it as the most economical prime mover obtainable. Many unsuc- 152 Wisconsin Academy of Sciences, Arts, and Leiters. cessful attempts have been made to discover a substitute for steam as a source of power, there always having been found insurmount- able obstacles, inseparably connected with the use of all other agents; difficulties which science and the best mechanical skill have failed to overcome. Quite a number of years will probably yet elapse, ere these hindrances are pushed aside by the spirit of investigation and invention which pervades the age in all civilized countries. But supposing the successful employment of a more suitable and economical motor might be rendered practicable, during the coming week, month or year, the expense necessary to secure the change would preclude its rapid adoption by many using the present devices. It would in fact be so long before the present arrangements could be superseded that it must still be worth our time to strive for improvements in the manner of em- ploying the power we now have, and to gain some knowledge in which direction, further improvement in its safe and economical use may tend. Practical experience has taught us, in the past twenty-five years, that there was no economy in the “old time practice” of using steam at a low temperature and pressure for all purposes. The direct advantages accruing from its use at high pressure, securing high piston speeds, and expanding the steam to nearly zero, have been very large. This change came gradually. Many improve- ments were necessitated, but now the six to fifteen pound pres- sures of forty-five years ago, and large unsightly engines are sup- planted by pressures of fifty to two hundred pounds, and engines of half the size which give the same equivalent of work. As the economy of the higher temperatures becomes generally appreci- ated, the greater the demand will be for them. The principal impediment still existing to progress in this di- rection is due to the limited strength of the present forms of the steam generators. The boilers of the future must be improved so that safety may be insured, being either constructed in sec- tions, or of material with greater strength, also not complicated in design and of moderate cost. That the most important of these requirements have not been realized, is only too apparent from the many accidents continually occurring in different sec- Boiler Eeplosions. 158 tions of the country. That some boilers will explode is perhaps inevitable. The increase in the number of those accidents is, in a measure, owing to the increase of the number of boilers in use, and to the greater demand made of them in sustaining high pres- sure. The inference is plain, that improvements in manufacture have not kept pace with this demand. That all boiler explosions are due directly to the inability of the vessel to retain the enor- mous pressure generated just prior to the rupture, all will admit, but indirectly there are many primary causes traceable. Of the vast number of boilers in use, but comparatively few explode; for- tunately they are the exceptions. Something certainly enters into the conditions where explosions oceur different from those in which they do not. Boilers are in use under so many varying circumstances, that two explosions are seldom traceable to exactly the same causes. Instances are known where boilers have been in constant use tor twenty years, and almost without repairs, while others fail in as many weeks or months. This difference must be due to material, workmanship, quality of water, and the attention they receive. We know that certain causes produce certain effects, and that neglect and carelessness have no business in mechanical matters at all, much less should they be seen about our steam generators. It is simply astounding to know the extent to which ignorance and incapacity are placed in charge of these agents of the public service, which, in the hands of incom- petent men, are about as dangerous as a package of dynamite. That all boiler explosions are due to carelessness and ignorance we do not mean to assert, but that about nine-tenths of them are, is beyond question. People are accustomed to think i any thing constructed of iron should “‘endure forever,” merely because made of iron. Well, such an hypothesis may answer in some cases. Experience in the past year alone, however, has taught us, that it is an exceeding unsafe one in connection with steam boilers. That so many in- competent men are found in charge of so many boilers and en- gines, is principally owing to the fact that they are cheap. Cheap- ness seems to be the only required qualification. The scale bal- ances up and down like the beam of a steelyard, intelligence and 154 Wisconsin Academy of Sciences, Arts, and Letters. suitable compensation usually being found at the upper end. Pos- sibly some employers prefer this class of help lest they might learn some disagreeable truths concerning their steam generators. There is, however, one very important point in this connection which is usually lost sight of. There seems to be an inexorable law in force in these cases as in many others. There is a mini- mum cost in the management of machinery, which cannot be re- duced even by machinery. And if the steam user will employ incompetent labor because it is cheap, then the difference between its cost and that of a higher grade of intelligence must certainly be given to the boiler-maker and machinist by way of repairs, and to the coal dealer for extra fuel, as a skillful fireman will save from five to twenty per cent. over an untrained one. I call to mind a striking illustration of the case, that of a manufacturer in an eastern state, who, though a most successful business man otherwise, possessed a remarkable faculty for utilizing every piece of old iron he could obtain, and the extra work on which, in put- ting it in suitable condition, always cost him more than the new material. His annual loss from breakage and wear, making no account of time when the machinery was idle, due to the employ- ing of a one dollar man where a two dollar one was required, was at least three times the difference in cost of one or two reliable men. A very common practice, and one most reprehensible withal, is that of employers compelling their engineers and firemen (often these consist of but one man) to do their legitimate work and that of two or three others, frequently being called to distant parts of the building. No man can attend to too many duties well; it is in the nature of things that some will be forgotten, and under these circumstances it is just as likely to be the most important as any other. Boilers are constructed from a great variety of designs. Those found in more common use are of the locomotive type, and the plain cylinder with closed ends. The material usually is from 1-4 to 8-8 inches thick. As a conductor of heat, iron stands low in the scale, gold being as 1000, copper 898, and iron but 347. Now with iron but 1-4 inch in thickness, a great amount of heat is lost in boilers, owing to the inability to transfer all the heat produced Boiler Haplosions. : 155 to the water. Hence it is seen we cannot gain security by use of heavier material without a sacrifice of fuel. Small boilers, as a rule, are safer than large ones, 1f builtin proportion, as they have a less number of square inches exposed to pressure. ‘Tak- ing a hasty glance at some of the practices in vogue in the construc- tion of boilers, one of the most objectionable features in this asin many other things, is the too general tendency to obtain our goods at a price below a fair market value, and the custom of let- lng these contracts to the lowest bidder often works to the disad- vantage of both parties. In this business, of all others, the cus- tom should be discontinued. It is fair toassume that boiler mak- ers are as fallible as any other class of business men. Men do not do business for nothing, asa rule, neither for pleasure. ‘“Hach° trade has its trick,”’ and the purchasing party who obtains his boiler for less than the market rate, may seek consolation in the fact that he has been ‘“‘sold’’ somewhere in his purchase. In my own experience, I have known boilers constructed under these conditions of so poor material, that the plates did not have the manufacturers’ brand on their surface. It may not be out of place to add that the builders of those boilers have had no less than four explosions of boilers of their construction in the past five years. From the time the boiler material is placed in the hands of the workman, it is constantly growing weaker, until thrown aside as old iron. The width of the iron in common use is three feet. Along each edge and across the ends, holes are cut or punched for rivets, after which the sheets are rolled to an ap- proximation of a cylinder. When these cylinders are slipped to- gether, all of the rivet holes should coincide. That they do not is a source of much trouble. The positions of these holes are marked through a wooden templet, which will be about three inches wide by 1-2 in thickness, and of such length as each par- ticular case may require. Along theedges of this templet holes are bored, one set answering for the inside cylinder and the other for the outside. In spacing these holes, about six times the thickness of iron is allowed for difference in length, and the same number of holes must appear in each sheet, only in the short ones they are nearer together. The operation of punching the 156 Wisconsin Academy of Sciences, Arts, and Letters. holes is a rather haphazard one at best, so far as accuracy iscon- cerned. There are two chances for error by the time the plates are rolled. First. The holes will not all be made exactly where marked; if one whole is punched slightly one side of its mark, and the one which it should match the other way, the error is Fig. 1. multiplied. Moreover, it is quite impossible to produce these plates and have them perfectly homogeneous. There will be hard and soft places. The great pressure from the rolls in making the plates cylindrical will cause changes in distance between some of the holes, as the temper of the plate varies. When the cylin- ders are placed together for riveting, many holes will shut past Fig. 2. Fig. 8. Fig. 4. one another from 1-16 of an inch to 1-2 or 2-3 their diameter. This, in itself, is objectionable enough, but the case is aggravated. The overlapping metal should all be removed by the reamer and the hole filled by a suitable rivet. If the overlapping of the holes is not such as to compel the use of the reamer, a most objection- able resort is the tool known in shop parlance as a “ drift pin,” which is nothing more than a steel pin, slightly tapering, and when well oiled can be driven in with such force that the solid iron is Boiler Explosions. 157 often compressed and cracked, and pieces of the plate may be forced out. Fig. 1 is intended to illustrate the overlapping holes, and figs, 2, 3 and 4 the effects of the use of the ‘drift pin.” An- other difficulty here presents itself, arising chiefly from careless- ness and poor workmanship. Often the sheets do not come in contact, and especially at the heads or ends of the boilers, on which the flanges are turned, is this the case, and also on internal fire-box work. When the rivets are driven, the iron acts as a spring, and vibrates back and forth from the blows of the hammer. The riv- ets too, will ‘ upset” in between the plates if much apart. Rivets driven in this way can never be made tight, neither will Fig. 5. the caulking chisel remedy the defect for when the caulk. ing is done, the iron is driven back be- tween the plates forming a thin nar- row ridge under which the pressure will soon force the water or steam, Fig. 5, is a fair illustration of the case. To this defect are due, many of the mysterious leaks in new boilers, when but a short time in use. Often rivets are improp- erly supported or “ backed” when being riveted, which causes leaks; or riveted when too cold, causing crystalization to such an extent that often a slight jar will cause the heads to drop off. The outer corner of the outside cylinder must be chamfered to an angle of about fifteen degrees, thus leaving a sharp edge where the cylinders join, for caulking. In many large shops this is done by machinery before the plates are rolled, in others before the cylinders are placed together. In many, it is done after the riveting, and thus the lower sheet is more or less cut by the corner of the chisel, the greatest care cannot prevent it. With many boiler-makers, this is of minor consideration, but the fact that many exploded boilers have given way at this point should draw attention toit. The following account of an experiment made at 158 Wisconsin Academy of Sctences, Arts, and Lelters. the University machine shop shows well the effect of cutting through the outside of the iron. A piece of common five-eighths square iron was cut on the four sides with a cold chisel, so that it was well marked. A slight blow from the hammer caused it to break, the ends showing crystalization. A second piece was marked on but one side, which on being broken, was crystalized about half through, the rest showing the fibre undisturbed, and tearing out toe iron for half an inch up the bar. It has been claimed that the principal strength of iron is destroyed by cutting through the “skin,” yet, a piece of this same bar marked as in the first instance, was placed in the lathe and the marks turned out, after which it was bent to more than ninety degrees before break- ing. It is estimated that about forty-four per cent. of the original strength of the material has been destroyed by the time a boiler is ready for riveting. Theaxiom that the “strength of any struct- ure must be estimated from the weakest point,” isa good one. By these various operations, six per cent. more will be of ques- tionable value. Repeat them at every joint in a boiler twelve to twenty-four feet long, and who will tell where the weakest point may be? Imagine if you can a boiler so constructed of any flexi- ble material, it would contain more kinks and puckers and gath- ers than a fashionable dress. New boilers are often submitted to the hydraulic test, which consists of forcing in cold water to a cer- tain pressure, and then assuming it safe to carry one-third or two- thirds as much steam pressure. I believe it a questionable method and an unsafe assumption. If there are blisters or imperfect. _ welds in the plates it may develop them. A careful inspection would probably accomplish the same result. But in these tests the boiler is subjected to strains under conditions which do not occur in actual use. The water and iron are both cold, stay rods and braces are loosened which do not again come tight of their own accord. Further, most boiler iron, as demonstrated by the experiments of the Franklin Institute Committee and Fairbairn, a noted English mechanical engineer, has a greater tensile strength with an elevation of temperature, some proving stronger at 600° Fahrenheit, than at any lower point. Now it is quite certain that Boiler Explosions. 159 testing with cold water has not rendered the weakest point of the vessel much stronger. . As soon as a boiler is in use, the agents of destruction incident thereto begin their work. Probably chief among these, is the steam itself, The unit of elasticity, by which the expansive force of elastic fluids is measured, is for popular use, one pound on one square inch of surface. We glance at a steam guage and the little hand may indicate fifty. Let us ascertain what that means. If a boiler is twelve feet long and three feet in diameter (very com- mon dimensions) and contains thirty-four three inch tubes, the two heads with tube surface deducted have remaining 1,864 square inches. The cylinder of the boiler contains 16,280, equal- ing in all 18,150 square inches which, multiplied by fifty pounds pressure, give a total of nearly one million pounds, or a fraction over 450 tons, continually tending to rend the cylinder. Boilers are made round or approximately so, for two reasons. It is the cheaper form and one naturally self-supporting. I say approxi- mately round, for they are not a true circle and cannot be made so owing to the lap of the longitudinal seams. Now this enorm- ous pressure, tends to force the shell of the boiler to a true circle. The pressure is never constant. Great and unequal strains are pro- duced along the under edge of the lap, which vary from time to time according to the different degree of pressure. In effect it is similar to bending a piece of iron back and forth in the hands, only on amore minute scale. In time the same result will be effected, destruction of the fibre of the iron. Many purchasers of these steam generators commit the serious mistake of selecting boilers of insufficient capacity, simply because one or two hundred dollars cheaper. In so doing, the door is opened through which many dollars will pass in the way of fuel without an adequate return. But when a boiler has just the ca- pacity to supply the demand by forcing the fires, a nearly full opening of all passages to the engine will result. The steam flows rapidly through them, twice at every revolution of the engine, this flow is suddenly and positively checked. While so checked, there is a rapid accumulation of steam from the forced fires. The boiler expands to the greatest limit in retaining the increasing 160 Wisconsin Academy of Sciences, Arts, and Letters. pressure. The opening of the passage way again affords a tempo- rary relief. Thus the boiler dilates and contracts to such an ex- tent that the movements are sometimes visible to the eye, and they have been compared to the breathing of some large animal. With this slow and continuous change, there is no wonder that boilers eventually “give out.’’ If there is any mystery in the case, it is that they last so long and serve so well as they dv. That steam and water in pipes not properly drained have great percussive action, may be readily seen from the jumping and snapping of the pipes under these conditions, and many serious accidents have occured from pipes and fittings bursting, even loss of life resulting in some cases. With these facts before us, great care should be exercised, not to open the steam passages from the boiler, too suddenly, on account of the danger arising from re- lieving the pressure on the water. What effect might be caused by such lack of care, may be seen in the following deduction. The heat required to raise one pound of water through one de- gree of temperature is termed a unit of heat, or its equivalent, 100 pounds of water through one-tenth of a degree, or one-tenth of a pound through 100 degrees. ‘This quantity of heat possesses the same amount of power as would be required to raise 772 pounds, one foot, or one pound 772 feet. This is termed the mechanical equivalent of heat. Now if the addition of one de- gree of heat to one pound of water, be such an accession of force, the addition of 100 degrees to 500 pounds of water is an equiva- lent of a half million times that force. In practice, the combus- tion of a pound of coal imparts to the water in a good boiler about 10,000 units of heat, and evaporates eight or nine pounds of water of usual temperature. With all the losses and disad- vantages considered, a pound of coal exerts about one-fourth of a horse power per hour, fifteen horse power for a minute or 900 for one second. The heat absorbed by 5,000 pounds of water in raising it through 100 degrees, is really twelve and a half horse power for an hour, 750 for a minute or 45,000 horse power for a second. The amount of heat absorbed by 5,000 pounds of water in raising it through 100 degrees, is but a small portion of the Bowler Hxplosions. 161 quantity in any boiler in common use, yet fifty pounds of coal are required to cause it, and the imparted heat is equal to the amount expended to convert about 430 pounds of water at common temperature to steam. By a too sudden release of pressure, this latent heat might all be released in one or two seconds, and there- by cause an explosion. The idea quite generally prevails that all boiler explosions are due to low water. ‘That might cause such a disaster, but that alone I think seldom does. Often, no doubt, boilers are seriously injured by the plates being burned. Burned plates lose about one-half their strength. Repeat the operation often enough and it is only a question of time, and a rather lim- ited time, too, when the boiler will be ruined. Several years since, the United States government squandered about $100,000 at Sandy Hook and Pittsburg, trying to determine the cause of boiler explosions. ‘The experiments were under con- ditions which were almost totally different from those under which boilers are used. Hence, practically, they were nearly failures. Two things were discovered, however; one, that a boiler will not explode when you want it to, and that water, pumped in on plates red hot, would all run out through the seams, which were caused to open from the rapid contraction, or else escape through the safety valve as steam. This operation was repeated three times to produce an explosion. Boiler plates are burned oftener from incrustation than from low water. Wherever this formation is thick enough to prevent the water from coming in close contact with the iron, that must be the result, and if from this cause the plates when in use become Fig. 6. sufficiently hot to weaken the ten- sile strength in a place of any large area, a rupture will surely follow. Fig. 6 shows a section of a feed pipe filled with lime in the short space of three months. A few years since I had an opportunity to exam- ine a case of this kind. The boiler was of the locomotive type, and was not under cover. The plate over the fire had been forced 1 162 Wisconsin Academy of Sciences, Arts, and Letters. down gradually, and in shape like the bottom of a wash-bowl, becoming thinner at the lowest point until finally breaking open, it left rough, ragged edges and a hole about eight inches in diame- ter. The whole weight of three and a half tons was raised about thirty feet and thrown over back, striking the ground at an angle of about thirty degrees, and sliding along, tore off every particle of the engine. These deposits in boilers are the most difficult matters steam users have to contend with, but its formation to a dangerous thick- ness can be prevented by frequent cleaning out, also by frequently letting out a little water through the day when the boiler is under pressure. It is a bad practice, and, of course, a common one, to let the water all blow out of the boiler, after the fires are out and before sufficiently cooled. The heat retained in the metal and iS ‘vinsly) ZY a= COS FEE surrounding walls will cause the deposit to bake to the iron so that nothing less than a hammer and chisel will remove it. Gare should be exercised in setting boilers so that they may be examined at different times, and to keep them in places as dry as possible. Tron wastes away fast enough at best, and if leaks occur where the boiler is in contact with brick and mortar, corrosion goes on so rapidly that the best boilers may be rendered unsafe in a year or two. When leaks are discovered they should be considered signs of wearing out, and should receive attention at once. Usu- ally, however, because it is small or does not let out the water faster than it can be replaced, it is allowed to go. It is treading ona dangerous path. Bowler Explosions. 163 Often, when very impure water is used, boil- ers are attacked by internal corrosion. Usually it is found at the edge of the sheets, along the seams and around the rivet heads. Sometimes different plates in the boiler will be corroded, while others will be found in good condition. With all this evidence of the dangerous pro- cesses going on both without and within a boil- er, 1t seems very plainly indicated, that too much eare and attention cannot be given them. Marine boilers are of the most dangerous class, but they seldom explode. The reason is evi- dent. First-class men, and none others, are placed in charge of them. The statistics show that in the decade from 1865 to 1875, there was an average of about one explosion every i three days, and it would seem that the public ff had the right to demand some system whereby ‘i a little higher grade of intelligence could be ! placed in charge of these, now, indispensable agents of the public service. From the use of impure water results a pro- cess called “ pitting.’ Small holes quite near together are eaten into the plates, and often a pitted plate and a sound one will be found side by side. This is probabiy due to a chemical difference in the iron, and the pitting may be caused by galvanic action. Pitted plates re- semble very much the partly consumed zines from a battery. Hxperiments were made with pieces of iron cut from pitted plates, and those which were not, taken from the same boiler and placed ina bath of acidulated water, when connected with a galvanometer, the pieces excited sufficient action to sensibly deflect the needle. Fig. 7 * shows a case of pitting, and fig. 8 represents a corroded brace or stay rod, so much of which is destroyed that it became entirely useless. * Figs, 7 and 8 are taken from’ Reports of Hariford Boiler Insurance Company. e 164 Wisconsin Academy of Sctences, Arts, and Letters. MIND IN THE LOWER ANIMALS. BY J. S. JEWELL, M. D., Professor of Mental and Nervous Diseases in the Chicago Medical Coliege, and Correspond- ing Member of the Wisconsin Academy of Sciences, Arts and Letters. My subject is that of “ the evidences of mind in the lower ani- mals.” ‘The first thing to be done, in a case like the present, is to define the meaning of the leading terms. This is one of the golden rules of discussion. Then, what is mind? Before trying to answer this question, which, by the way, is not a new one, I should tell you that it was not my plan to determine, ex- cept in a superficial sort of way, what mind really is. It would require more than one lecture to deal adequately with that question. or my present purpose, it is sufficient to assume the existence of something, which may be called mind, whether mo- tional or immotional, the presence and action of which is known usually by certain signs, by which beings possessed of mind are commonly distinguished from those that do not have it. It is with these signs, rather than the mind itself, that I am to deal. But once again, what is mind? It is much easier to ask this question than it is to answer it. You all know it has been, and at this hour it would be answered very differently by various persons, who have given themselves (following different methods) to its study. . But taking all these answers together, aside from unessential particulars, they may be divided into two principal classes, which are susceptible again of division into sub-classes. But I am to call your attention to the two principal classes mentioned. They may be described as follows: In the one case, the phenomena called mental are not attributed to any other agent or source than the material organism itself. In this view there is no such being as a mind numerically differ- ent from the body of the animal, neither before nor after death. The word mind is simply a name for the aggregate of functions of the nervous system, at any rate of its higher functions. There is no actual proof of the existence of any such immaterial, immor- tal entity, as that usually designated by the terms, mind, soul, Mind in the Lower Animals. 165 spirit. Mind is simply brain action. When the brain is disor- dered, mind is disordered. When the brain is healthy, the mind is healthy. When the brain is imperfect in its development and structure, as it 1s in idiots, then the action of the mind is hope- lessly imperfect. But when, on the contrary, its development and structure are the most perfect, uniformly its action is the most perfect. Moreover, when the brain perishes as it does after death, all mental action ceases, or at least all evidences of it. In short, all that we knew as mind before the death of the individual, perishes with the brain. Any opinion that there is a being so distinct from the body, as to continue to survive after its death, is a mere creation of the fancy, at the dictates of the baseless aspirations or traditions of mankind. Mind is, hence, absolutely dependent on the body, and without it has no existence. It is simply a combination of physical forces, which return to their primitive condition after death, ready to enter into new combinations of any or all kinds. Such, in outline, is one class of opinions as to mind. ‘They are what have been called matervalistic. If this class of opinions were true, there could hardly be any difference among thinking people as to whether the lower animals are possessed of minds, as well as man. In point of fact, persons who hold to the view just described, generally admit that animals share in the possession of mind with men. By the other class, mind is regarded as something substantially different from the physical organism, or body, though closely as- sociated with it during the corporeal life of the individual, from which, however, it becomes separated in what is called death, of which this supposed separation is held to be the principal event. After this, the organization of the body indeed perishes, but not so the mind; for the latter is believed to continue to exist, as mind, in some other state. It is farther conceived, that the mind is an imperishable existence, possessed always of the same facul- ties of knowledge which distinguished it while yet connected with the body, but deprived, perhaps, of the means of mechanism furn- ished by the latter for obtaining a knowledge of the physical world, as well as for manifesting its own existence, or its invisible 166 Wisconsin Academy of Sciences, Arts, and Letters. states or acts, as depicted or represented in the changes of the body. It is also held to be not simply numerically different from the body, but radically different in substance. The body is said to be material, the mind immaterial. It cannot, therefore, possess the properties of matter. If not, then it cannot, by the terms of the case, be made cognizable by the senses, since they appear to be fitted to reach only to material impressions. Mind therefore, as mind, cannot be submitted to physical tests or examination, though the body can be. Its acts and states cannot be directly made known by such means. They can only be made known to other minds by certain signs, or in other words, certain acts and states of the body which is regarded in a certain sense as an in- strument of the mind. But these signs would be without any significance whatever, if it was not for certain modes of interpre- tation possessed by animals, and in various degrees of perfection. The only way, so far as is known, that they have for finding out the meaning of these signs, is by their own experience. They find by observation that the mutual acts and states are more or less invariably associated with certain states or acts of the body. So when they observe other animals in the same bodily states, or performing the same acts, they infer the corresponding mutual states that they have found connected therewith, in their own ex- perience. In this indirect way alone can they discover the men- tal condition of other animals. One mind cannot, so far as we know, commune directly, unless under rare circumstances, with another, during the continuance of physical life. But ordinarily, each individual mind may know directly, without the intervention of such signs, many, if not most, of its own states and acts. They take place in what is called self-con- scvousness, which is, in my opinion, the chief, if not the only kind of consciousness we have. These mutual states and acts then, though they cannot be directly reached by physical tests, and are not open to sense observations as physical objects are, may neverthe- less be submitted to the tests of immediaté self-observation. We can secretly know often what passes in our own minds, and with the utmost clearness, while the observer, who looks upon our bodies from without, cannot many times so much as suspect what Mind tn the Lower Animals. L67 is passing within us. ‘There are two ways then of studying mind. One of them is applicable to ourselves alone, and is confined to the states and acts of our own mind. This is the method of in- trospection, or of looking within our own minds, to directly ob- serve our own mental acts and states, and not the signs of them. The other method is also in a measure applicable to our own bodies. Itis the objective method. Itis from first to last di- rectly compared with the signs of mental states and acts. It is the only method by which we can study the mental states and acts of other individuals, whether man or animals. And the only way in which we can make our observations useful or intelligible is, by a recurrence to our own internal experience, our self observa- tions, which have taught us in various degrees of fullness and per- fection, that certain internal, and hence invisible, mental states and acts, are either preceded or followed by certain bodily condi- tions and signs. The key of the interpretation lies within. If this is true, then it may happen that we would be lable to be deceived by persons who in some way exhibit the signs of thought or feeling, and yet do not truly experience the states or the mental acts, which in a truthful experience the signs represent. And this is sadly too true, as nearly all can testify. Hence, it happens that a mask, a statue, a picture, may exhibit the szgns of feeling, for example, so perfectly as to excite the same state in ourselves, notwithstanding the object has only the signs, and not the fact of thought or feeling. This, I say, is the only method ap- plicable directly to the study of tne minds of other beings. It is the one that must therefore be applied to the study of animals. All we can do is to observe them, under varying conditions, and see how they act, or what they do, and then interpret their actions by appeals to our own personal experience in similar conditions. And this, as I have said, is the way in which one must study other men. But to return from this partial discussion. By persons of this second class, mind is held to be the invisible, intelligent energy, with which, in connection with the body, we truly feel, will, and think, and which permeates the body, possibly only the brain, and uses it, for sake of illustration, as the invisible magnet force, which 168 Wisconsin Academy of Sciences, Arts, and Letlers. inheres in a visible portion of magnetic ore, or of steel, causes movements of the same. In short, mind is the immaterial, imper- ishable, sensitive, intelligent being, which feels, and wills, and thinks, suffers and enjoys, within the body, which though living, would be an unintelligent, or unthinking, possibly unfeeling organism without it. Now in the sense that it is held and understood by this class, do the lower animals have minds? In relation to this question, and for various reasons, persons differ widely in opinion. Some think they have, others think they have not. And itis to the possession of mind, at any rate, or rather the signs of it in this sense, by the lower animals, that I wish to call your attention this evening. IT know as well as I can ever know, that it is a serious question with many, whether even man possesses mind in the sense just indicated. But I wish for the time, to assume without contro- versy, as a hypothesis, if you please, that they do, and my present inquiry, I repeat, is whether the lower animals show clear signs of having the same; and if this is refused, I wish to inquire what we are to include as to the mental natures of the lower animals, or how we can explain the phenomena which they present to any in- telligent observer. By the phrase “ lower animals” I should say, in passing, I mean the whole animal kingdom. I do not include simply the higher vertebrates, but the entire class. For, as we shall see perhaps, even the humbler types of the animal kingdom present us with striking exhibitions of intelligence. In dealing with this matter, it might be expected that I would lay out some division of the faculties of the mind, as a scheme under which examples from among the lower animals might be ranged. But it is deemed the best way to proceed at once to adduce suitable and well authenticated instances of phenomena, which show in fair measure whether or not animals do possess minds. In doing this, the trouble is not to find such examples, but out of the mass of such cases to make a selection. I have collected from various works under my hands many hundreds, and I might truthfully say, thousands of cases of interest. I might occupy hours detailing and discussing my own personal observa- Mind in the Lower Animals. 169 tions. But I do not have time to do either the one or the other. But to begin, take this case: A naturalist friend of mine was one day walking along a road, and saw as he walked one of those familar road beetles, rolling its ball of compost. He stopped and watched it for a few moments, and then with a pin, made the ball fast to the ground. The beetle seemed surprised at this turn in its affairs, but soon recovered itself, and endeavored as before to push its ball; but it was not able todoso. It crawled over and round it, and appeared to carefully inspect the situation, and at the same time made strenuous efforts from all points to move its ball; still it could not move it. It then climed up on its ball, and sat there for a few moments, quietly moving its antennz as if in a sort of reverie, and then rose on its wings and flew away. The gentleman much interested in what he saw, thought he would tarry a while and see what would come to pass. He had not waited many minutes, until he heard the familiar hum of two beetles. They circled about, as is their custom, and finally they both alighted near the ball. One of them was recognized as being the same beetle that had been first observed. It was known by a speck on one of its wing cases. The two immediately went to the ball and united their efforts to move it, the one pushing, and the other pulling, But after various trials, they ceased, and ht- erally putting their heads together, they seemed to be in consul- tation. During this time the gentleman quietly removed the pin and left the ball free. They at last went back to the ball, and tried to move it, and of course succeeded. Whereupon beetle number two rose up on its wings and disappeared, while beetle number one rolled its bal! along without farther interruption. Now Iam quite well aware that this is a simple story, but it is none the less interesting to one who will consent to think on it without prejudice. A hundred histories of this kind would really not be any better than one. Let us examine this case a little more closely. It might be said, with more or less propriety, that the beetle formed its ball as a nidus for its young, and then sought a proper place in which to bury it away, guided solely by instinct. But I do not think it 170 Wisconsin Academy of Sciences, Arts, and Letters. could be maintained successfully that many of the later perform- ances of the creature were in the proper sense of the word in- stinctive. It seemed as if, when it found itself unable to move its ball, —I say it seemed to stop and deliberate as to what should be done. It seemed to have found a place of securing aid from some other beetle. For, after a short absence, it returned with a companion. It seemed to have gone purposely to find it. It must have communicated in some way a knowledge of its wants, for the other beetle seemed to understand the case. They had a common purpose, as was evidenced by their united action toward the same end. They seemed to consult, when they found themselves unable to move the ball. They seemed by common consent to conclude to make another effort. When the ball was found movable again, beetle number two seemed to know that it was needed no longer, and probably returned to its own occupations. Certainly this cannot have been all due to instinct. It has the plain mark of the presence and action of mind, no less so because the signs of purposive acts were done by beetles instead of men. The signs cf mind are much the same as they would have been under simi- lar circumstances among men. As has been already intimated, one case well studied is as good asa hundred. But though this is so, I shall now proceed to ad- vance other examples from the animal kingdom, apparently in- volving mental action. For example, let us consider points in the history and doings of ants, as we have given much observation and study to these most singular little creatures. On one occasion, as I was passing along a road, my attention was attracted by a company of large, pale red ants hurrying across the way, the whole company follow- ing what seemed to be a leader, who was much in the advance. I stopped and followed them through the grass and weeds for full fifty yards, when they suddenly came to a halt, and collected in a circle in the space beneath the bending spires of grass. mmedi- ately one of the ants disappeared in a hole in the ground, only to be followed with every appearance of precipitation by one after another of the company. At this moment a smaller ant, but of a similar color, entered on the scene, and rushed for the hole in the Mind in the Lower Animals. 171 ground, but it was instantly seized by one of the marauders, and a fierce struggle ensued, which was not terminated while I watched them. But in a few seconds, as I watched the hole down which most of the company had disappeared one by one, I saw an ant come strugeling out, in a state of great excitement. It was of a smaller kind than those which I had watched cross the road. Pres- ently it was foilowed by another of the same kind, in (as I was about to say) much the same excited state, and as time passed on these two were joined by others. The place evidently belonged to them. They ran violently about the hole, and even up to the top of the blades of grass, and then jumped off to the ground ina distracted and reckless manner. At times two of them would meet and, apparently, stop fora hurried exchange of ideas, and then they would run about in the same frantic manner. Meantime all the larger ants had gone down into the hole. Ina few moments, how- ever, these latter ants began to reappear, one by one, each bearing a white ege not far from hatching, as the outline of the young ant could be seen through the cuticle. But no sooner had these latter ants reached the open day with their booty than they were fero- ciously attacked by the smaller ones, to whom the eggs properly belonged. And here began a series of struggles of the most ani- mated and interesting character— one set of ants striving, by might and main, to get away with their booty, the other set strilk- ing for their altars and fires. But aftersome time had been spent in this way, the larger and stronger got away, each one, on his own hook, traveling with great speed, on the back track, bear- ing an egg in its jaws. But now began a scene of evident distress among the smaller ants whose home had just been robbed in so miserable a manner. They ran round and round, in helpless bewilderment, meeting and consulting (apparently) and passing each other, and diving into their den, and then out again. And in this distressing condition I left them. [I fol- lowed on after the marauders, and found most of them already across the road. At last, fully sixty yards from the scene of the robbery, they came to their own den, and carried the eggs down into a special chamber, as I afterwards found. After the eggs had been deposited below, the ants of the expedition came 172 Wisconsin Academy of Sciences, Arts, and Letters. up, and with a seeming air of satisfaction at their exploit, passed their time in rubbing off their bodies, cleaning and polishing their limbs and mandibles. ‘This was an instance of the doings of slave- making ants. In this case, there can be no reasonable doubt but that one of the party which composed the expedition had made a discovery of the colony that was to be raided. The ant returned to its com- panions, reported its discovery, a party was organized, led by the discoverer, the colony was robbed, a conflict ensued, and finally the spoils were carried home. This whole performance looks very like what men have done in all ages. But when done by men such actions are not ascribed to instinct, but to mind. But let them be done by even one of the higher animals, not to say an ant, and they are loosely at- tributed to instinct. But why so, where the signs are essentially the same ? But I have not done with the history of the singular doings of ants, which seem to indicate the presence of mind. ‘To do this fully would require several lectures. I have watched ants on the hunt for colonies of aphides or plant lice. I have watched them after discovering such a colony. They station guards over them, to dispute the entrance of any other ants, on theirdomain. They carefully tend the aphides, as a shepherd would his flock. If one of the clumsy creatures of their charge gets off its plumb, and is in danger of falling, a guardian ant takes and tenderly places it in position. The ants step around, among and over the mem- bers of their flock with every sign of care. But why? Let any one see. They do not do that to feed on them, but they use them in a sense asmen usecows. An ant will stand astride of, or behind the plant louse, and with its pointed feet will seize the little aphid underneath tbe abdomen, and by a motion of combined pressure and tickling, induces it to issue amethystine drops from its back, from a little bag. The ant watches for this, and when it appears, stoops and drinks it with apparent gusto, and then goes his way. The only ants that have this privilege are those which belong to the colony — they alone have the passport. Ants have armies, commanded, it seems, by officers who seem- Mind tin the Lower Animals. 173 ingly issue their orders, insist upon obedience, and will not permit any of the privates to stray from the ranks. There are some ants which till the ground, plant the particular grain on which they feed, cut it when ripe, and store it away in subterranean granaries. ‘I'here are ants which bury their dead. There are ants who have slaves, as already intimated, and compel them to labor while their masters live on its proceeds, just as we have known of man. How can we attribute all these things to instinct? If so, let us call the whole thing instinct, and so end it. Take the case of the bee. It has required a small volume in which to record the doings of these little creatures, which, to say the least, are curious. Take the case of weak hives, which on that account are hable to the incursions of more powerful neigh- bors, who are ever ready to appropriate the works of the thrift of their less powerful neighbors. In such cases, it has been fre- quently observed that the weaker colony casts up a cross within the entrance or hallyport to their hive, a wall of wax, etc., called, I believe, a traverse, in engineering parlance. Upon entering, the bee is at once confronted by this traverse, and is obliged to turn either to the right or left to enter the hive proper. But in so doing it must pass a very narrow way at either end of the traverse. By this means a few bees can defend a hive against the assault of a very large number of marauding bees. Butall hives donot have this traverse, and why not? Is it made in obedience to a blind tendency, such as an instinct is ordinarily held to be? If so, why do not all hives have the traverse? It seems to me, the only natural way is to admit that such doings are an evidence of the possession of mind. Sometime since a gentleman was struck by a happy thought, viz.: one in which he could utilize bees. He formed the design of exporting a number of hives to the island of Hawaii, where there are flowers all the year round. His thought appears to have been that, as bees gather honey guided solely by a blind tendency or an instinct, that they would work all the year round, and hence make honey all the year, and if so, become a source of no small profit. If they gathered honey wholly from a mere blind im- pulse, his expectations would have been fulfilled. But in the 174 Wisconsin Academy of Sciences, Arts, and Leilers. course of a few years the bees learned somehow that it was un- necessary to lay up honey as in climates where flowering plants exist only a part of the year, and they became valueless from an economical point of view. Was this due to instinct, or to educa- tion? If to the latter, is mind involved in the case? I must confess, it seems so to me. Take the following anecdote from many hundreds of others of various kinds, in respect to dogs : ‘There is a water mill on the Tweed in Scotland called Max- wellhaugh, by the road between Kelso and Trovist. It is driven by a sluice of water from the Trovist, just before it joins the Tweed, and consists of two flats. The upper flat, or story, is on a level with the public road, and is called the “ upper mill,” while entrance to the lower story was reached by a lath road descending from the highway. The first thing the miller did in the morning was to unchain the dog. The dog immediately placed himself across the upper doorway, while the miller proceeded with his work in the lower mill. As soon asthe miller had finished his work there, and removed to the upper mill, the dog, without being told, set off to the milier’s house, and in two journeys brought his master’s breakfast, — namely, milk in a pitcher and porridge in a ‘bicker,’ tied up in a towel. ‘On one occasion, when the Trovist and the Tweed were in a flood, a little dog ventured incautiously into the Tweed, and was carried rapidly down the stream, struggling and yelping as it was hurried along. It so happened that the miller’s dog, while carry- ing his master’s breakfast to him, saw the little dog in distress. He immediately put down his burden, and set off at full gallop down the stream. When he had got well below the drowning dog, he sprung into the river, swam across, and so exactly had he calculated the rapidity of the river and his own speed, that he in. tercepted the little dog as it was being helplessly swept down the current, and brought it safely to land. ‘‘ When he got his burden safely on shore, the dog, instead of displaying the least affection for it, cuffed it, first with one paw and then with the other, and returned to the spot where he had deposited his master’s breakfast and carried it to him, as usual. Mind in the Lower Animals. 175 “ How is it possible,” says the author of the anecdote, to ‘ re- fer the proceedings of this animal to mere instinct? Had anegro slave performed them, we should have used them (and with per- fect justice) as arguments, that so intellectual and trustworthy a man ought not to be the property of an irresponsible master.’ “The whole behavior of the dog is exactly like that of a burly, kindly and rugged barger, possessed of cool judgment and rapid action, willing to risk his life for another, and then to make light of the whole business. ‘The process of reasoning that took place in the dog’s mind is as evident as if the brain had been that of a man and not a dog. The animal exhibited self-denial, presence of mind, and fore- thought. Had he jumped into the water at once, he could not have caught the little dog; but by galloping down the stream, getting ahead of the drowning animal, and then stemming the cur- rent until it was swept within his reach, he made sure of his ob- ject; and no man could have done better if he had tried to save a drowning child ?” There are hundreds of cases, from among not only the almost innumerable species of lower animals, but also, so to speak, of the higher, such as birds of many kinds, cats, dogs, horses, elephants, and monkeys. But, manifestly, I cannot refer to them to-night; nor, indeed, is it necessary to do so after what has been said, and when it is remembered that it is probably true that there is not one person present but has had opportunities for making interest- ing personal observations bearing on this question. Contenting myself, therefore, I will pass at once to a discussion of the subject in various of its aspects. Tor my own part, I am led to hold to the position provisionally, that the lower animals are possessed of minds, the same in kind as those of men. I haye said, this is my provisional opinion, for it has become, after much endeavor, a habit of mine to adopt opinions with care, and if not well founded, to try and remember that they are not well founded. Such opinions I try to be ready to drop at the first occasion which seems truly to require me to do so, even if I am left without opinions, as, indeed, I have come to be, in relation to many things. I will now proceed to give you some of the rea- 176 Wisconsin Academy of Sciences, Arts, and Letters. sons which seem to me to justify me in adopting the opinion to which I have here given expression. i, One strong proof of this position is to be gained from such facts as I have been relating in your hearing. An unprejudiced and attentive examination of the mental phenomena of lower animals, shows them to have in some measure most, if not all, the mental capacities or faculties which distinguish men. But let us for a moment go even back of this. The nervous system, the ad- mitted instrument of mind, in its intimate structure, is essentially the same ; even the drain of man and the lower animals agree so closely as to render all but futile the elaborate attempt of Prof. Owen to establish a separate class, the archencephale, of which man is held to be the sole member. The agreements in general, and even in details, are surprisingly close, whether in gross form or in minute texture, between the brains of men and the anthropoid apes. Then the lower animals have the same extrinsic means for acquiring a knowledge of the outer world that man has. But why have they the sense apparatuses of vision, hearing, touch, taste, smell, the muscular sense, etc., unless for the same purposes that they subserve in men? But to come nearer. The lower animals experience sensations both agreeable and the contrary, they enjoy sense-perception, and in many cases far beyond what is true for man. They have frequently as perfect, and often a more elaborate muscular system than man, which is exercised and controlled by means of the same kind of nervous mechanism, and is devoted to similar purposes. They have often well marked and very tenacious memories, so far as we can tell, the same as that which belongs to man. They can reason also, or compare the perceptions they have or have had, and many times in a surpris- ing degree. They have most certainly a will, and hence power to choose from among alternatives, the story of Buridan’s ass to the contrary notwithstanding. They display all the principal quali- ties and passions which belong to man, such as parental affection, jealousy, anger, fear, courage, constancy, fidelity, friendship, ill- temper, hope, despair (for animals have been known to commit suicide), pride, self-importance, caution, trickery, maliciousness, ete. examples of all of which it would be easy to give and of many Mind in the Lower Animals. aber of them to multiply. They can certainly learn and improve, even in many such actions as have been called instructive. They even show abuse of humor and fun, some appreciation of the beautiful, and would appear in some instances to have a knowledge of right and wrong. It is admitted that the moral sense, if developed at all in the lower animals, is very rudimentary. But the same may be said with some degree of seriousness of many human beings, especially of young children and idiots. A young child, if arrest- ed in its moral development at an early period, would, so far as signs can show, be a mere human animal, not equal perhaps to an intelligent monkey. It might be expected a prior, that if the lower animals should fail anywhere in a comparison with man, it would be in respect to the higher faculties. And this is found to be actually true. Butif the lower animals show but little, if any evidence of possessing a moral and especially a religious sense and capacity, let it be remembered, as already said, that some time elapses in the human being before the conscience is developed so as to beget what is called accountability. A young child is not held to be accountable for its acts, when they lead to bad conse- quences, any more than isa mere animal. So after all, it would seem from the confessedly superficial view of the case, we cannot refuse to admit that the lower animals have minds similar to men, at least in kind, on the score of radical difference in their mental phenomena. 2. Then to what shall we ascribe the mental phenomena ex- hibited by the lower animals, if not to mind? It has been the custom to refer them to what has been called mstinct. But what is instinct? When an act is performed by an animal without hav- ing learned to perform it, as when a bird builds a nest without ever having learned to do it, or when a bee builds its cell of a cer- tain geometrical figure without any previous instruction or de- monstrable plan to follow, or when a pig will begin twenty-four hours before an approaching storm to gather materials for a bed, and in making which, it will heap them up on the side from which the storm is to approach, etc., such actions are called enstinctive or automatic. The animal does them without purpose or design. Many such actions are performed like the leaping of a headless 12 178 Wisconsin Academy of Sciences, Arts, and Letters. frog, when, according to ordinary experience, the mind would seem to have been removed. But take the case of a bird build- ing its nest. This is said to be instinctive. If this means any- thing, it means that the animal is fitted prior to experience, and independently of all knowledge, to build its nest. It is created from the start with a nest-building tendency, which is the soul so to speak, of a nest-building mechanism, which at some peculiar conjunction in its affairs impels and guides the bird, it knows not how or why, to build the nest, which it is under the necessity of building on account of the fixed conditions and modes of action of its nest-building apparatus, and in a certain way and none other. Hence the individual members of the same species will build their nests after a peculiar pattern or of peculiar materials, so much so, that it is enough for the observant naturalist simply to see the nest, in many cases, to name the bird. But the case is, or seems to be different, with the architect who plans and builds a house, as every one knows. But let us look more closely at this instinctive act of nest building. One thing is certain, there must be a plan somewhere, consciously or unconsciously followed, for the nests of the same species are made alike, or after a common type or plan. The only possible places (so to speak) in which the plan can inhere, are either just in the mechanism or organism of the bird itself, in which case it would have to be assumed that it was constructed to work of itself, in the absence of a mind. It would work then, for example, like a watch, or better yet, if you please, like a pin or match machine, which is fitted to take the raw material at one end, and give out at the other the finished product. It cannot in the nature of its case make anything but tacks. Any power which can set it in motion, no matter from what source, may, through the agency of the mechanism, bring about the result; or the plan may inhere in the mind of the ani- mal, as well asthe apparatus to which the mechanism corresponds. Why should wz deny the presence of mind, in a given case, be- cause it works through an apparatus, even if the latter is auto- matically perfect from the outset? Can mind not work through such mechanism as well as through one which for certain reasons is imperfect at the start, and has to be developed by purposive Mind in the Lower Animals. 179 use? In the latter case the evidence of mind may be clearer, but in the other, is it absent? Or, finally, the act called instinctive may be attributed to the immediate presence and action of the Divine mind. But in some form or other, mind must be present, and we cannot escape it, as some seem to imagine they do by call- ing certain cases in which it seems to be present, instinctive. The bird must choose a place in which to build her nest. Is this in- stinctive? Think of it a moment. How should a bird be pre- arranged to select, from thousands of places in which her nest might be securely built, the one she does select? Does she not look about, and aiter considerable search and consideration, at last fix upon the spot which, upon the whole, she likes best. Then again, is her search for and choice of materials a blind one, in which she follows, mechanically, the unvarying condi- tions of a fated or at any rate a fixed mechanism? No, it must be that however perfectly the material organism is prearranged for action, under favoring conditions, that it has within it a mind, which, it is true, has a less sphere of spontaneity than belongs to man, and which works therefore under more rigid condi- tions than in man; but still mind isthere. By the limitations of its automatic organism, it 1s made unnecessary for it to go the round of experience to learn, for it begins where man ends, or tends to end; that is, with an organism, embodying an organized experience prior to the fact. By this means, the lower animals whose lives are short, are enabled to begin their life-work at once, and from the first to avoid mistakes asa rule. But coupled with this freedom from errors in their acts, is the corresponding inabil- ity to perceive or correct them when they have been made. Just in proportion as automatic action prevails, does spontaneity and inventive capacity and adaptability disappear. Hence, these lat- ter elements are found in the greatest measure in man, and in the least in the lower animals. But this is to be remembered, that by attributing the actions of the lower animals to instinct, we do not therefore exclude the mind, though this is commonly sup- posed to have been done in such acase. LHven in view of those actions, then, which are most clearly automatic, mind is probably present, and hence by this mode of reasoning we cannot exclude the lower animals from participating in it, in common with man. 180 Wisconsin Academy of Sciences, Arts, and Leiters. Then again there is the question of the ¢mmortality of the minds of the lower animals. It has been thought if the admission is made that the lower animals have minds, that this will oblige us to concede to them immortality, equally with man. But why not do this? What harm could come of such an admission? What forbids it? Would it be contrary to scripture, to reason, to the true interests of men present or to come, or would it conflict with any well authenticated facts? Would it be degrading to men, or cheapen future existence? But if we refuse it, what shall we do with the intelligent principle, whatever it may be, which feels, and thinks, and wills, and suffers, and enjoys, and remembers, in the lower animals? What is it in them that appeals in hunger and distress, or is the spring of pride or joy, or satisfaction, or fidelity, that devises expedients, draws conclusions, etc.? If it perishes with the body, on what logical grounds can we refuse to surrender the mind of man toa similar fate? If we can do all the things done by the animals by means of a perishable combina- tion of physical and vital forces, why not join in with the so-called muterialists, and do the same for mind in man? If. not, why not? But suppose the ground is taken, that we must attribute all the phenomena bearing the marks of mind exhibited by the lower animals to the immediate presence and action of the Divine mind, how shall we reclaim the human mind from being swallowed up in the Divine mind, thus destroying all except the shadow or pre- tense of individuality ? Hence, on such grounds as these, it seems hardly possible to refuse to the lower animals the pos- session of mind in the same sense, but not necessarily in the same degree as in man. Of course there are many other reasons which may be used in support of the position that the lower animals have minds, but I cannot refer toall of them, or indeed to any, except in a brief way. But I will call your attention to two or three of the stronger reasons that may be urged against this view. I will state and briefly discuss them before I close. One of the objections which may be raised is to this effect: 1. That there is no real proof that animals possess immortal spirits, or minds. Without a revelation we could not really know, except on the grounds of a frail inference, that the mind of ani- Mind in the Lower Animals. L81 mals survives the destruction of their bodies. But we have no clear revelation on this subject. The Bible, the only pretended source of authority on such subjects, so far as revelation is con- cerned in them, makes no statement bearing on it, at least none equaling in clearness those made in respect to the future existence of the spirits of men. It would seem not unreasonable, that if the spirits or minds of the lower animals are endowed with immor- tality, that it would have been for some purpose, probably a moral one. And since men and the lower animals sustain to each other such close relations in this life, the purpose in conferring immortality on the souls of the beasts would probably have some relation to man, and hence, would naturally find some expression in the Bible, which has so much to say of the hereafter of men. But no such statements occur. Bya mere observation of animals, and a simple scientific study of the phenomena they present, it is not possible to arrive at clear and logical conclusions on this sub- ject, unless, perhaps of a kind unfavorable to the view which affirms their immortality. It is true, such modes of reasoning do not prove that animals do not have immortal souls, but it at least raises a reasonable presumption against such a view. 2. Again it is said, that the mental phenomena of lower animals do not require the agency of mind to explain them, for they have been referred almost by common consent, from the earliest times, to instinct. Men and animals differ, as regards their actions and their knowledge, chiefly in this: Animals do not as a rule learn to do, or to know what their modes of existence require them to know, or do what they need to do, and their actions there- fore are usually as well performed at first as at last. Their actions are automatic, or they are done without purpose or foresight of the animal. Itis thus with the walking of animals when first born, with their breathing or their sucking. A chicken, not yet out of its shell, will peck at, and swallow a fly; a serpent, when it first escapes from its egg, will on the instant, seek a retreat under a stone, or stick, or clod, if there is any show of violence or danger. The bee builds its cel], the bird its nest, the spider weaves its web, just as perfectly at first as at last. All these things and thousands more are done by these and other animals prior to ex- 182 Wisconsin Academy of Sciences, Arts, and Letters. perience. They were never learned. In one sense the animal does not know how to do them, viz.: in the sense of having learned to do them. It does them moved by an zmpulse, rather than de- terminate thought. It obeys a mere blind, but cogent propensity, rather than a rational conclusion, viz.: one deduced by logical processes from ascertained and definite premises. These mere propensities arise in, and then reach on, are apparatus, or mechan- ism, which is often perfect at birth, or before it. In such cases as those, in which the animal does not begin the performance of cer- tain acts or to manifest certain tendencies until late in life, the reason is to be found in the lateness of development of the ap- propriate mechanism through which the acts in question are ac- complished. The case is in nowise different from that in which the apparatus is perfect at birth. No matter how late in life it is that the animal begins to do what it does, this much is clear, that the apparatus was not developed by educative processes, as is so gen- erally the case in man. To all appearances the development is spontaneous. The animal seems to acquiesce, without purpose, and hence unconsciously its capacities to do. It does whatever it does as a rule, from the first, with automatic precision. But while this is the rule with the lower animals, the contrary is true of man. He has the smallest possible stock of instinctive or automatic acts to begin with, and those few of the lowest and simplest kind. Whatever he does or knows he has to learn to do or know as a rule, by or through slow, educative processes. The point in this case is as follows: As respects the lower ani- mals, they are provided by their Creator from the first with com- plete mechanisms, fitted to reach in a determinate way to various stimuli, external and internal, while the development and perfec- tion in structure and working of the nervous mechanisms in man are conditional on their determinate purposive use or education. If not so used, or, in other words, educated, they are never devel- oped. Hence we may have ignorant and incapable men, as com- pared with each other, but not ignorant and incapable animals, as compared with their kind. Hence arises a duty on the part of men to develop themselves, and if they do not discharge that duty we blame them, as in the scripture parable of the talents. But not Mind in the Lower Animals. 183 so in the lower animals. But why these remarkable differences between men and animals if they both have minds of the same kind? Te only way in which they may be explained is to ad- mit that in the one case there is a rational mind or spirit, which can feel and know, and can use the mechanisms with which it stands connected, so as to lead to their development in many ways and degrees, and in varying propertions to each other, while in the lower animals, the nervous and other mechanisms are developed as a rule in some other way than by their use. They are devel oped prior to or independently of use, but not so in man, as a rule. In the one case there is a mind to use the imperfect apparatus, and, according to the degree and kind of the use, to develop it in various ways and degrees; but in beasts this is not so, only ina low degree. Hence animals of the same kind are more nearly equal in their development, and men less so. Hence man is ina measure the master of his own higher development, and is, there- fore, charged with a duty in this connection; but not so the ani- mals below him. Out of such considerations, if time permitted, it would seem that quite a presumption could be raised up in favor of the view that the lower animals do not have minds as men do. But to pass on, it may be urged, 3. That any necessity which might seem to arise for admit- ting the lower animals to have mind with man, may be met, or at least justly avoided, by certain ‘distinctions which have been long recognized by many writers. It has been maintained by many, from the time of Aristotle, that in man we may discern at least two forms of mind. The one is conveyed with the objects of sense, and our relations in space and time. To it belongs the sense of perception, the capacity for comparing sense perceptions, or to think on them, and also our nerve propensities, and certain emo- tions not ordinarily classed with propensities or appetites. ‘This, it is admitted, is possessed in kind by animalsas well as men. It has been called the psyche. The other is superior to the psyche, and has relations not only to the psyche, but also to the body. It is that form of mind by which we become related to God, and which is the seat of conscience.. By it we are enabled to discern right from wrong, good from evil, the beautiful from its contrary, and by this 184 Wisconsin Academy of Sciences, Arts, and Letters. we obtain motives to action, not only for the present but the dis- tant future, not only in accordance with, but often in opposition to the mere teachings of sense, or the mere impulses of appetite or of the bodily passions, in obedience to which the lower animals act. This is the home of the reason, of even the ‘ Pure Reason” of Kant, of the moral sense, and the true seat of the religious life, to all of which the lower animals are strangers. This form or part of mind is called the pneuma. It is the possession of this part which chiefly distinguishes men from the lower animals. It is this part which it may be most truly offered is immortal, with- out contesting for the immortality of the psyche, which the lower animals possess in common with man. This latter part may perish possibly, and if so, we need not trouble ourselves about the question as to whether the mind of animals may continue to survive after the death of their bodies. But that these two forms of mind may be separable from each other would seem to be possi- ble from the fact, as they may be assumed to be, that the lower animals have what corresponds to the psyche without the pneuma in man, and from the fact, that forms of mind seem to relate to: wholly different objects, and from the further fact, as it seems to: be in the moral and religious history of mankind, that the pneuma may be either dead or alive to the proper moral and spiritual ob- jects and relations, without involving any corresponding or other change in the psyche. This is the part of a man’s nature which seems of all others the most susceptible of cultivation and ex- pansion, and which the advance of age, which seems to involve so serlously the body and the psyche, does not often affect. It is par excellence, the progressive part of man, the most human-like, nay, God-like, part of man; that it is within its domain that these aspirations take their origin, which at once imply and de- mand a life hereafter, as the only one which does not mark them, and in which alone it would seem possible for them to find satis- fying objects. By making some such distinction as has been hinted at, it would seem possible to admit a form of mind as common to man and animals, the admission of which would be perfectly compatible with a denial of its immortality, or at least with a doubt on this subject, and also with a claim for man of a Mind in the Lower Animals. 185 form of mind which, so far as the signs go, may be denied to the lower animals. 4, But finally, it may objected that it cannot be sustained on the score of utility. Of what use would a hereafter be to crea- tures who do not show any signs of needing or wanting it, and who show so little capacity for improving it, to be of any good end? Notwithstanding the acknowledged possibility of educating certain animals, yet the great fact remains, that the lives of all the lower animals are almost wholly automatic. Their lives are not spent in struggles after the practical attainments of ideals, and in an apparent sacrifice of the present for the future, in a pur- posive exercise of will, to the end of the chastening and subjection of their sensual natures, and the elevation, expansion, unlimited refinement and development of their higher faculties — faculties which, indeed, they do not have as compared with men—in the pursuit of moral and esthetic good, which often have their final object concealed, either in the immediate future or even in another state of existence, and in a rational sacrifice of self for others. I say the great fact remains, that the lives of beasts are not open to any such way, but in following out the dictates of mere pro- pensities, and these are usually, though not always, selfish. Their lives and faculties are developed for them, rather than by them. Of what use would a future life be to such creatures? It is true there may be a use for them hereafter which we do know of, but we are not permitted to go outside of our knowledge for pos- itive purposes. We should never permit ourselves to use a mere negation in a positive manner; we cannot properly use our ignor- ance as against our knowledge, however imperiect that knowledge may be. We do not know, ascompared with men, that the lower animals show no signs of desiring a future life, only at best a de- sire for a continuance of the present one, and they do not show any considerable capacities for improvement or rational enjoy- ment. But it has been and is different with men in all ages. We all have, I hope, a desire to live hereafter, that is, after death ; and as arule men have in their average estate shown capaci- ties for the acquisition and use of knowledge and for enjoyment which are too vast for the short and uncertain measure of this life. 186 Wisconsin Academy of Sciences, Arts, and Letters. But why, if there is no hereafter? This desire which men have for immortality, which is shown in so many ways, and which must have an object somewhere, has its birth in the pnewma rather than the psyche; and hence, if the distinction between these two forms of mind is admissible, and men and animals participate in the psyche, but notin the pneuma, we can see why animals should not have this desire. Such are a few among the many reasons which may be offered for refusing to admit the view that the lower animals have minds the same in kind as men, differing only in degree of development. The reasons that have been given have been selected rather than -others, because it was supposed their discussion would prove the most suggestive. I say suggestive, because my opinion is, that if what is said on such an occasion as this is said only to convey mere information, rather than to provoke and direct thought, we come together for little purpose. But it is impossible in one short discourse to adequately state, much less discuss, in a satisfactory manner, such a theme as this. As a result of my studies, which have been long turned in this ‘direction, I have been led to admit that the lower animals, even the lowest, have minds generally the same in kind as men, but with important differences. In the lower animals, the mental faculties involved in percep- ‘tion and memory, and the instincts and propensities, and the lower phases of moral sentiment, may be compared with men, in the natural state, viz.: with the savages. But in the higher prov- inces of mind, especially those which are the seats of the esthetic, moral and religious activities, the lower animals are separated from man by a vast difference in degree of development, if not of kind. It is on these latter grounds that the distinction is the most profound as between men and the lower animals when com- pared mutually. Why should we deny that animals have minds? Why deny that they are immortal? By admitting these positions no harm is done, so far as I can see, and we avoid thereby a host of un- -co mfortable questions and inferences, which we can neither an- ‘wer nor parry in a rational manner, and many of which strike at Mind in the Lower Animals. 187 the heart of the immortality of the human soul. Whether the spirits of animals, if they are immortal, will be with us hereaiter as at present, or will be somewhere else, is a question about which no one knows anything, and about which no one need concern himself. It may be thatthe old and yet living doctrine of the transmigration of the spirits of animals points to the true solution of this question. 188 Wisconsin Academy of Sciences, Arts, and Letters. THE ANTIQUITIES AND PLATYCNEMISM OF THE MOUND BUILDERS OF WISCONSIN. BY J. M. De HART, M. D. The vast difference that has been found to exist between the mounds of Wisconsin and those of other parts of the United States, both in their form and variety of structure, have led many archeologists to infer that they were constructed by a different race; but such eminent authority as the late Dr. Lapham, has dispelled these views, and finds in them sufficient evidence to prove that they are of a common origin. The animal mounds, located a few miles west of the four lakes, near Madison, were first described by Squier and Davis, in their contributions to the Smithsonian Institution, in 1848, and also by R. C. Taylor, in Siuliman’s Journal. Dr. Locke, in the Geological Report of Iowa and Wisconsin, furnished information which greatly increased our knowledge of these structures; but Dr. Lapham, in his contributions to the Smithsonian Institution and American Antiquarian Society, has done more than any other writer, in furnishing evidence of their conformation and general character. Most of these mounds consist of imitations, on a gigantic scale, of animate objects, which were characteristic of the region, such as the bear, buffalo and deer, among the mammals; of the turtle and lizard, among the reptiles, and the night hawk and eagle, among the birds; and, in a few instances, of the human form. The animal mounds seldom exceed five feet in height, while some of them were only one or two feet high, above the surrounding ground. From the fact that the mounds were nearly always located near the great rivers, and in the vicinity of the lakes, we are led to infer that the mound-builders availed themselves of the natural advantages of the country — ready access to living water, natural highways, streams abounding with fish, and the adjacent forests with game. Antiquities and Platycnemism. 189 Many of the mounds are built on high bluffs, from which an extensive view may be obtained of the surrounding country, diversified by wooded steeps and rolling prairies, with, in many instances, a broad river meandering through the landscape, or a beautiful lake, with its placid waters ever abounding with fish in great quantity. Peschel of Leipsic, in his “‘ Races of Man,” says that in North Fg. 1. | R oie It has a Fig. I represents an eagle, with a body 100 ft. long, and winga cxpanded 300 {t. on either side of it. well-defined beak, and a tail 40 ft. wide. America the aborigines made dome shaped tumuli, round, flat topped mounds and circular earth works; some of them contain graves and covered passages. ‘T'hese are very scarce in the New England states, and are rarely found west of the Mississippi, but extend from the up- per course of the Missouri and the great lakes, to the south, on both slopes of the Alleghanies, as far as Florida. Most archeologists have ascribed them to an extinct race of Mound-builders, who are supposed to have migrated from Mexico. The builders of these mounds were, there- fore, the predecessors of the Indians, and these latter were supplanted by Kuropeans. Wisconsin furnishes many evidences of the existence up- on its soil of a prehistoric race, known as the Mound-builder. Along the northern shore of Lake Mendota, many mounds may be (found. The animal mounds found in this vicinity represent a bear, deer, squirrel, and other mammals now extinct; while a few of the mounds are made in the form of birds, some of which are very large, and three of them are located in close proximity to one another, and resemble 190 Wisconsin Academy of Sciences, Arts, and Letlers. an eagle with expanded wings. The largest of these birds has a body 100 ft. long, whose expanded wings measure 300 feet on either side of his body, while the tail is 40 ft. wide. The head is quite perfectly formed, so that the outline of the beak is 15 ft. in length. [#%g. 1.] The form of a deer, about three feet high, is found near the left wing of the gigantic bird. The body of the deer measures 65 ft. Fig. 2. and the legs are 14 f} f / measures 12 ft. from Ye ft. long; the head Y, the tip of the nose Hy CA ee to the origin of the ~~ \ antlers. These lat- A ter are each 10 ft Jong, and have a ro. branch extending at BRS KY right angles from xs their center. [ Lig. BRON CORED 2.| Near the left wing of the other BS SS NN bird there is the Fig. 2. represents a deer, whose body measures 65 ft., with legs 14 ft. long. The antlers are each 10 ft. long, with branches form of a bear, with from each. a well defined body, head and legs. [ig. aes Fig. 3. Near Grand river, in Green Lake county, there is a collection of about fy one hundred mounds, mostly of a conical or circular form. One of these resembles the form of a man, S with arms of an unequal length. WON " The head points to the south, and towards a high hill, called Mt. Moriah. As these mounds are composed of a sandy soil, they do not preserve their form as well as the mounds in other localities, which are composed of adjacent soil and clay. In the vicinity of Fox river there are several mounds, some of which resemble racoons and bears, while the remainder are ob- Antiquities and Platycnemism. 194 long and circular mounds. One mound in this vicinity represents an animal whose genus and species could not be ascertained. Fig. 4. While many animal mounds. are found near Lake Mendota, there are also circular and ob- long mounds. On the follow- ing page there is a diagrara showing the location and ele- vation of eight ancient mounds. on the northern shores of this lake. Their elevation varies from 93 to 96 feet above the lake, and on some of them trees are growing, measuring” five and a half feet in circum- ference. [Mg. 5.] The larg- est circular mound of this group measures 188 feet in circumference, and 85 feet from the base to its summit’ It is the highest mound in this group, and from its elevated posi- tion, could have been used for observation, and as a means of com- munication by signal with other mounds in the adjacent country. From its summit you have an extended view of the surrounding: country for many miles in all directions. This mound was the first one of the series explored, and on the following page a diagram of the manner of exploration is given, together with the location of the skeletons and other relics found therein. [ig. 6.] In commencing the work, it was thought best to sink a perpen- dicular shaft, about six feet square, through the centre of the mound, from the apex to the bottom of the tumulus. After re- moving the surface, a black earth, similar to what is found on the: shore of the lake when muck accumulates, or on the prairie bot- tom, was removed to the depth of five feet. At this depth, and on the western side of the shaft, a group of stones, consisting of magnesia limestone, yellow und red sandstone were found. Some 192 Wisconsin Academy of Sciences, Arts, and Letters. of these stones were flat, while others were irregular in shape, and bear indications of having been obtained from the limestone quarry along the shore of the lake, where the water had worn away portions of them. Underneath this course of earth there was a layer of yellow clay, about four feet in depth, through which a similar course of stones, arranged in a semi-circular man- ~ ner, and passing off to the opposite side of the shaft, were en- countered. Another layer of black earth was found underneath this course of yellow clay, about five and a half feet in depth, after removing two feet of this deposit, ashes, charcoal, and de- cayed wood, with small pieces of flint were discovered. A few stones were removed directly below these, and the earth under- neath was so hard and dry, that it had the appearance of having been baked, another foot of earth was then removed, when the skeleton of an adult mound-builder was discovered in a sitting posture, at the southeastern corner of the shaft, several pieces of the cranium, vertebra, the body of the inferior maxillary, with the alveolar process quite complete, ribs, and bones of the extremeties were found, but none of them were wholly perfect. Where the cranium had lain, there was a perfectly formed mould, but only a few pieces of the bones were found. Had I thought to measure this mould I could have obtained some idea of the dimensions of the skull. The vertebra were very large and indicated the existence of a race larger than the Indian; of the bones of the upper extremity that were found, that of the humerus presented a feature which is regarded as characteristic of the ancient Mound-builder. There was a perforation through its inferior extremity, as shown in the accompanying illustration. In all instances where the inferior extremity of the humerus has been found in mounds, this perforation has been observed to exist, and hence it may be called a natural communication existing between the olecranon depression on the one side and the coronal and radial depression on the opposite side, in the humerus of the Mound-builder. This perforation is found to exist in the chim- panzee, ape and other animals, who go about on all four of their extremities. As shown in the accompanying illustration, the specimen found Fig. 5. a) FPA Ga Ae SHOWING THE LOCATION AND ELEVATION OF THE MOUNDS AND THEIR ELEVATION ABOVE LAKE. : No.1. The Mound first examined Xx 96 above the Lake. No. 2. The second Mound examined X 95 above the Lake. The other six Mounds have not been examined. No. 4. Represents an animal of some kind, probably a Turtle. Lf, WwW, to Represent Magnesian Limestone. Bae Rcearies Represent a bed of gravel. Rs) GS @ Represent a few trees on the Mounds and bot})m. No Mounds and Lake. ee ge These marks the elevation above the Lake. 9909 ©0999 890 90900G i Vee aa” IK OP OC 7. fp 4] Leary | ley 227 9 $$ A) or LT e rx 13 194 Wisconsin Academy of Sciences, Arts, and Letters, in this mound, presents on its anterior surface a per- foration, which is sur- HES) rounded by a gradually eH) receding margin, which is not so great as that sur- rounding the perforation on the opposite or poste- rior surface, of the same bone. In the human sub- ject, the anterior surface of the inferior extremity of the humerus presents a ridge of bones, which separates the coronal and Sie <> 255 = = are, ae = ==. as — =< raw rae; ery So —e- ——* ae, Zz as go aaa = =. Zs a, ZZ ZZ a aa Lo a ae —— — rar radial depressions. This bone is, no doubt, of great antiquity and-was very much decayed, the superior extremity having disappeared. In no case did I find any of the long bones of the extremities wholly perfect, but all of them were broken near the center of the shaft, the other extremity not being Lf = an, ZI> ZeS 7 ee hee Pare So MAE oh I to some superstitious rite or custom, connected with the sepulture of the dead, among the ancient Mound-builders, This was the only humerus found, with either extremity nearly perfect. The shafts of two tibias, found in this mound presented another characteristic of the Mound-builder. They were both remark- ably flat, and this peculiarity is termed Platycnemism. In the Smithsonian Annual Report of 1873, Mr. H. Gilman, of Michi- Antiquities and Platycnemeism. 195 gan, furnishes six comparative tables, which give the dimensions of some forty specimens of Platycnemism, and in these tables the tibias found in the mound near Rogue river, Michigan, present the greatest amount of flatness. In comparing the specimens found in this mound near Lake Mendota, with those reported by Mr. Gilman, I find that while his measure forty-eighth one hun- dredths of an inch in comparing their antero-posterior diameter with the transverse diameter, my specimens measure fifty-two one- hundredths and fifty-four one-hundredths of an inch respectively, in comparing the same diameters. This flatness of the tibia has been recognized in the skeletons found in many ancient mounds, not only in this country but also in England and Wales, and might, therefore, be justly regarded as another characteristic feature of the osteology of the Mound-builder. Prof. Buck regards Platyenemism as being characteristic of re- mote antiquity. Prof. Gilman says further, that it is impossible to give the cor- rect age of the mounds in Michigan, but from an examination of the trees growing on them, it was evident that they were either planted, or had taken root there, from 750 to 1,000 years ago. It was, therefore, beyond his observation to give anything like an aproximate age of the mounds, because they existed before the trees grew. Beneath the skeleton of this Mound-builder, there was a few inches of earth, and then a course of stones similar to those pre- viously described, resting upon a bed of yellow clay. As there were no evidences that this had ever been disturbed, and it being one and a half feet below the level of the surface, it was not thought best to sink the shaft any deeper. As shown in fig. 6, a drift was then made into the side of this mound, three feet above the level of the surface, and about eight feet wide. After the removal of several feet of earth, a similar course of stones, was found, which could be traced to the group of stones on the west side of the shaft. These were removed, and large quantities of ashes, charcoal, and pieces of flint were found near them. Qn continuing the drift towards the center of the tumulus, and near the shaft, the skeleton of a young Mound- 196 Wisconsin Academy of Sciences, Arts, and Lelters. builder, was discovered in a sitting posture. He was probably not more than six years of age, judging from the condition of the bones, a few pieces of the cranium, several vertebra, portions of the long bones of the extremities, and the superior and inferior maxillary were removed; several teeth were still in the alercolar process of the superior maxillary, several pieces of flintshell beads, two large teeth, of some animal, and small arrow heads were found in close proximity. Quite near these remains, three pieces of ancient pottery were discovered ; the largest piece measuring four and a half or five and a half inches, and about a quarter of an inch in thickness. It was smooth on its internal surface, and marked externally by raised lines running obliquely across it, such as are frequently seen upon ancient pottery found in drug. 8. mounds. I give NM = VFL Muastration CRO SS EN Rai We ; LEVER RM i Of this piece of YW, He : er sp Dp 4 =a Gj. er with a stone LL = i KOK pA, SY OY ie sen eile: WG) Ze ea 4 UM) / \ 7 YY it AGG: 4, Yf SY SAY fp Eek LESS d Gy, WUE SS implement, re- 7 => y Prez: = : SESS pe SS sembling a ham- mer, found in this mound. The drift was carried forward as far as the shaft, and then downwards to the natural bed of yellow clay. Just before striking the shaft, and near the bottom of the tumulus, the skeleton of a second adult was found, only a very few pieces of the cranium and two pieces of the femur were dis- covered. After removing some very dry and hard earth another course of stones were removed, which bore evidences of having been exposed to fire. Ashes, charcoal, and decayed wood in quite large pieces, one foot long by four inches thick, and plants were found quite near the stones. Many of the stones crumbled to pieces on handling. On removing the pillar of earth formed by the junction of the drift with the perpendicular shaft, a flat dise of stone, quarter of an inch in thickness and four inches in diam- eter was, found. Similar stone dics were found by Squier and Davis, and were called by them discoidal stones. They have been found in the other parts of the northwest, and were sup- posed by them to have been used by the Mound-builders in play- ing games, Antiquities and Platycnemism. 197 Another mound circular in form, and located a few yards from number one, and marked number two in the diagram, on page Fig. 9. 7, was that examined. This mound was about five feet high and 125 feet in circumference. A drift was made into the side of this mound on a IS level with the surround- ing ground, and six feet yin width. SS | work, the ‘“ Indigenous* Races of the IT ST Karth,”’ refer to the Mound-builders, ~UTTTITNSy : as belonging to a race far higher in civilization than the hunting tribes of America.” They call them Mound-builders, from the regular fortifications, which they have erected, in several of the Western and Southern States. The Natchez, destroyed by the French of Louisiana, in the last cen- tnry, seem, in fact, to have belonged to them. 200 Wisconsin Academy of Sciences, Arts, and Letters. Among the many relics of this ancient race, which were found by Squier, during his explorations of the valley of the Missis- sippi, was a most characteristic head, made of red pipe clay, the workmanship of these unknown builders, which exhibits the pecu- liar Indian features. He says further, “‘ that this discovery proves that these ‘ Mound- builders’ were American Indians, or type; that time has not. changed the type of this indigenous group of races; and that the ‘Mound-builders’ were probably acquainted with no other race, but themselves. In every way proving the views of author of Crania Americans.” Fig. 12 represents above overturned head, formed by squares. DIAGRAM showing Glacial Movements tre a N og & iS (ples One 1S le Bpies wees won foo m HY < SY Nn tal 4 fz] FOTHOTW tex ¥ wte p “porphyry ~ es 5 B. Aizob of Ortare ~ A.. Kn06b of Quan Tue Muwarcer Intu,.<.Exen Co, DEPARTMENT OF THE MATHEMATICAL AND PHYSICAL SCIENCES. ON. THE EXTENT AND SIGNIFICANCE OF THE WIS.- CONSIN KETTLE MORAINE. By T. C. CHAMBERLIN, A. M., State Geologist, and Professor of Geolcgy in Beloit College ! At the meeting of the Academy, three years since, I took the liberty of occupying the attention of the members by the presen- tation of some observations and conclusions in reference to a pe- culiar series of drift hills and ridges in eastern Wisconsin, known as the Kettle range, and the views then advanced afterwards found a place in my report on the geology of eastern Wisconsin.” Sim- ilar observations were subsequently made by Professor Roland D. Irving, of the Wisconsin survey, and his conclusions are in per- fect agreement with my own.® ‘In neither case, however, was any attempt made to show the full extent of the formation outside of the districts reported upon, or to point out its theoretical significance, the chapters being intended only as contributions to local geology, made under somewhat se- vere limitations as to space. It is not now possible to map, or even safely conjecture, the complete extent and limitations of the formation; but it is the purpose of this article to add such trustworthy observations as have since been made, and to gather such evidence as may justify a provisional mapping of the range, where it has not been actually 1] have taken advantage of the interval between the date of reading and the printing to introduce new matter. T.C.C. 2 Geology of Wis., Vol. II, 1877 (revised edition 1878), pp. 205-215. 3 Geology of Wis., Vol. II, 1877 (revised edition 1878), pp. 608-635. 202 Wisconsin Academy of Sciences, Arts, and Letters. traced. A portion of the paper will, therefore, relate to well as- certained facts, while other portions will be in various degrees hypothetical. If care is taken to distinguish between these por- tions, no harm can arise from their association; while the provis- ional mapping will, it is hoped, prove of service in both stimu- lating and guiding further investigation. The extent of the range is likely to prove too great for the immediate time and means of a single observer; while the broad and irregular, and sometimes obscure, character of the belt is such that it is likely to be over- looked, as a continuous range, as experience has shown, unless at- tention be called to it, or the observer be keenly alive to distinc- tions in drift topography. It is believed, therefore, that the pre- sentation of some things that are only probable, not certain, will not be without value. % It will be advisable to consider first, somewhat critically, the char- acter of the formation. The following description, which is based upon careful observation, relates more specifically to the moraine in Wisconsin, where it is usually well developed, and may require some modification in its application to the range where sub-aque- ous deposits overlap or encroach upon it, and in other special sit- uations. Surface Features.— The superficial aspect of the formation is that of an irregular, intricate series of drift ridges and hills of rapidly, but often very gracefully, undulating contour, consist- ing of rounded domes, conical peaks, winding and, occasionally, geniculated ridges, short, sharp spurs, mounds, knolls and hum- mocks, promiscuously arranged, accompanied by corresponding depressions, that are even more striking in character. These depressions, which, to casual observation, constitute the most pe- culiar and obtrusive feature of the range, and give rise to its de- seriptive name in Wisconsin, are variously known as “ Potash kettles,” ‘“ Pot holes,” ‘‘ Pots and kettles,” “Sinks,” etc. Those that have most arrested popular attention are circular in outline and symmetrical in form, not unlike the homely utensils that have given them names. But it is important to observe that the most of these depressions are not so symmetrical as to merit the application of these terms. Occasionally, they approach the Wisconsin Kettle Moraine. 203 form of a funnel, or of an inverted bell, while the shallow ones are mere saucer-like hollows, and others are rudely oval, oblong, elliptical, or are extended into trough-like, or even winding hol- lows, while irregular departures from all these forms are most common. In depth, these cavities vary from the merest indenta- tion of the surface to bowls sixty feet or more deep, while in the irregular forms the descent is not unfrequently one hundred feet or more. The slope of the sides varies greatly, but in the deeper ones it very often reaches an angle of 80° or 35° with the horizon, or, in other words, is about as steep as the material will lic. In horizontal dimensions, those that are popularly recognized as “ kettles” seldom exceed 500 feet in diameter, but, structurally considered, they cannot be limited to this dimension, and it may be difficult to assign definite limits to them. One of the peculiar- ities of the range is the large number of small lakes, without inlet or outlet, that dot its course. Some of these are mere ponds of water at the bottom of typical kettles, and, from this, they gradu- ate by imperceptible degrees into lakes of two or three miles in diameter. These are simply kettles on a large scale. Next to the depressions themselves, the most striking feature of this singular formation is their counterpart in the form of rounded hills and hillocks, that may, not inaptly, be styled invezted ket- tles. These give to the surface an irregularity sometimes fittingly designated “knobby drift.” The trough-like, winding hollows have their correlatives in sharp serpentine ridges. The combined effect of these elevations and depressions is to give to the surface an entirely distinctive character. These features may be regarded, however, as subordinate ele- ments of the main range, since these hillocks and hollows are variously distributed over its surface. They are usually most abundant upon the more abrupt face of the range, but occur, in greater or less degree, on all sides of it, and in various situations. Not unfrequently, they occur distributed over comparatively level areas, adjacent tothe range. Sometimes the kettles prevail in the valleys, the adjacent ridges being free from them; and, again, the reverse is the case, or they are promiscuously distributed over both. These facts are important in considering the question of their origin. 204 Wisconsin Academy of Sciences, Arts, and Letlers. The range itself is of composite character, being made up of a series of rudely parallel ridges, that unite, interlock, separate, appear and disappear in an eccentric and intricate manner. Several of these subordinate ridges are often clearly discernible. It is usually between the component ridges, and occupying de- pressions, evidently caused by their divergence, that most of the larger lakes associated with the rangearefound. Ridges, running acro:s the trend of the range, as well as traverse spurs extending out from it, are not uncommon features. The component ridges are themselves exceedingly irregular in height and breadth, being often much broken and interrupted. The united effect of all the foregoing features 1s to give to the formation a strikingly irregular and complicated aspect. This peculiar topography, however, finds a miniature represen- tative in the terminal moraines of certain Alpine glaciers. Most of the glaciers of Switzerland, at present, terminate in narrow valleys, on very steep slopes, and leave their debris in the form of lateral ridges, or a torrentially washed valley deposit. A portion of them, however, in their recently advanced state, descended into comparatively open valleys of gentle decline, and left typical, ter- minal moraines, formed from the ground moraines of the glaciers, and only slightly obscured by the medial and lateral morainic products, which have little or no representative in the Quaternary formations. The Rhone glacier has left three such ridges, sepa- rated by a few rods interval, that are strikingly similar in topo- graphical eccentricities to the formation under discussion, save in their diminutive size. ‘The two outer ones have been modified by the action of the elements, and covered by grass and shrubs, while the inner one remains still largely bare, and, as they have been cut across by the outflowing glacial streams, they are exceed- ingly instructive as to glacial action under these circumstances. The inner one graduates in an interesting way into the wide- spread ground moraine, which occupies the interval between it and the retreating glacier, where not swept by floods, and which pre- sents a different surface contour, illustrative of Till topography. The two Grindelwald glaciers have left similar moraines; those of the upper one, being the more massive, and being driven closer to- gether, present an almost perfect analogy to the Kettle ranges. Wisconsin Kettle Moraine. 205 The Glacier du Bois, the terminal portion of the Mer de Glace, the Argentiére, and, less obviously, the Findelen, and others, so far as their situation favored, have developed similar moraines, and indicate that this is tae usual method of deposit under these conditions. Reference is here made only to the terminal deposit of the ground moraine, eliminating, as it is quite possible to do, for the most part, the material borne on the suriace of the glacier. The Material of the Formation. —This topic, which is one of primary importance in determining the origin of the deposit, readily divides itself into three subordinate ones, all of which need discriminative attention; (1) the form of the constituents, (2) their arrangement as deposited, and (8) their sowrce. (1) Premising that the Kames, and those deposits which have been associated with them in the literature of the subject, are described as composed mainly of sand and gravel, it is to be remarked, in distinction, that a// the four forms of material com- mon to drift, viz.: clay, sand, gravel, and boulders, enter largely into the constitution of the Kettle range, in its typical develop- ment. Of these, gravel is the most conspicuous element, exposed to observation. This qualification is an important one in forming an adequate conception of the true structure of the formation. It is to be noticed that the belt, at many points, exhibits two dis- tinct formations. The uppermost —but not occupying the heights of the range — consists almost wholly of sand and gravel, and lies, like an irregular, undulating sheet, over portions of the true original deposit. This superficial formation is confined mainly to the slopes and flanks of the range, and to depressed areas between its constituent ridges ; though, when the whole belt is low, it often spreads extensively over it, so as sometimes to be quite deceptive. But, where the range is developed in force, this superficial deposit is so limited and interrupted, as to be quite insignificant, and not at all misleading; and, at some points, where it is more widely developed, excavations reveal unequivocally its relationship to the subjacent accumulations. In such cases, the lower formation shows a more uneven surface than the upper one, indicating that the effect of the latter is to mask the irregular contour of the lower and main formation. Notwithstanding this, the upper 206 Wisconsin Academy of Sciences, Arts, and Letters. sands and gravels are often undulatory, and even strongly bil- lowy, and the bowls and basins in it commonly have more than usual symmetry. A not uncommon arrangement of this stratum is found in an undulating margin on the flank of a ridge of the main formation, from which it stretches away into a sand flat or a gravel plain. Setting aside this, which is manifestly a secondary formation, it is still true that gravel forms a large constituent of the forma- tion. Some of the minor knolls and ridges are almost wholly composed of sand and gravel, the elements of which are usually very irregular in size, frequently including many boulders. But, notwithstanding these qualifications, the great core of the range, as shown by the deeper excavations, and by the prominent hills and ridges, that have not been masked by superficial modifications, consists of a confused commingling of clay, sand, gravel, and boulders, of the most pronounced type. ‘There is every gradation of material, from boulders several feet in diameter, down to the finest rock flour. The erratics present all degrees of angularity, from those that are scarcely abraded at all, to thoroughly rounded boulders. The cobble stones are spherically rounded, rather than flat, as is common with beach gravel, where the attrition is produced largely by sliding, rather than rolling. Stratification. — As indicated above, the heart of the range is essentially unstratified. There is, however, much stratified ma- terial intimately associated with it, a part of which, if my dis- criminations are correct, was formed simultaneously with the pro- duction of the unstratified portion, and the rest is due to subse- quent modification. The local overlying beds, previously men- tioned, are obviously stratified, the bedding lines being often inclined, rather than horizontal, and frequently discordant, undu- latory or irregular. The Source of the Material. — This, so far as the range in Wis- consin is concerned, admits of the most unequivocal demonstra- tion. The large amount of coarse rock present renders identifica- tion easy, and the average abrasion that has been suffered indicates, measurably, the relative distance that has been traveled. The range winds over the rock formations in a peculiar manner, so as Wisconsin Kettle Moraine. 207 to furnish fine opportunities for decisive investigation. Of the many details collected, there is room here for a single illustrative case only. The Green Bay loop of the range surrounds on all sides, save the north, several scattered knobs of quartzite, por- phyry and granite, that protrude through the prevailing lime- stones and sandstones of the region. These make their several contributions to the material of the range, but only to a limited section of wt, and that invariably in the direction of glacial striation. Any given segment of the range shows a notable proportion of material derived from the formation adjacent to it, in the direc- tion of striation; and a less proportion, generally speaking, from the succeeding formations that lie beyond it, backward along the line of glacial movement for three hundred miles or more. It is undeniable, that the agency, which produced the range, gathered its material all along its course for at lewst three hundred miles to the northward, and its largest accumulations were in the immediate vicinity of the deposit. For this reason, as the range is traced along its course, its material is found to change, both lithologically and physically, corresponding to the formation from which it was derived. These facts find ample parallel in the moraines of Switzerland. The marginal portion of the great moraine of the ancient expanded glaciers, on the flanks of the Juras, is composed, very largely, of boulder clay, derived from the limestones that lie in its vicinity, while the quantity of material derived from the more distant for- mations of the Alps is quite subordinate. Of the more recently formed moraines, those derived from the Bois, Viesch, Rhone, Aar, and other glaciers, which pass over granitic rocks, consist quite largely of sand, gravel, and boulders, clay being subordinate, while those glaciers of the Zermatt region, that pass mainly over schistose rocks, and the Grindelwald glaciers, that, in the lower part of their course, traverse limestone, give rise to a decided amount of clay. The moraines, previously referred to as minia- ture kettle ridges, are composed of commingled unstratified debris, in the main, but there are instances of assorted and strat'fied material. The inner moraine of the upper Grindelwald gl cier presents much fine assorted gravel and coarse sand, heaped up, 208 Wisconsin Academy of Sciences, Arts, and Letters. very curiously, into peaks and ridges, in various attitudes on the summit and sides of the moraine. | Relations to Drift Movements. — This is manifestly of most vital consideration. The course of drift movement may be determined, (1) by the grooving of the rock surface, (2) by the direction in which the material has been transported, (8) by the abrasion which rock prominences have suffered, (4) by the trend of elongated domes of polished rock, and, (5) less decisively, by the arrange- ment of the deposited material and the resulting topography. Recourse has been had to all these means of determination, in that portion of the range that has been carefully investigated, and their individual testimony is entirely harmonious, and their com- bined force is overwhelming. Hxceptional opportunity for positive determination is afforded by the protruding knobs of Archzean rocks before alluded to, from which trains of erratics stretch away in definite lines, continuous with the striation on the parent knobs, and parallel to that of the region, as well as concordant with the general system. The united import of all observations, in eastern Wisconsin, testifies to the following remarkable movements, which may be taken as typical, and which are here given, because they have been determined with much care. Between Lake Michigan and the adjacent Kettle range, the direction was obliquely up the slope, as now situated, southwestward, towards the range. On the opposite side, between the Green Bay valley and the range, the course was, after surmounting the cliff bordering the valley, ob- liquely down the slope, southeastward, toward the range. In the Gren Bay trough, the ice stream moved up the valley to its watershed, and then descended divergingly the Rock river valley. Between the Green Bay valley and the Kettle belt on the west, the course was up the slope, westward, or southwestward, accord- ing to position. These movements, which are imperfectly shown on the diagram, exhibit a remarkable divergence from the main channel toward the margin of the striated area, marked by the Kettle range. Much of the data relating to the movements, outside of Wis- consin, has been derived from a study of publications relating to the geology of the several states, to whose authors I am indebted, MAG BNW EMALO) VO) Aah Aq, 41 OL ASIN SAVO LVHL SALN HI OAOIW TVIOV'TO ey} JO urersetq pue ANIVYOW AlLLay 2240 AVW AYUMVNINVISN Ad Tite Mawarikne Lrrni.s Exon, Wisconsin Kettle Moraine. 209 but who should not be held responsible for the special collocation presented in the accompanying diagram, which, in some of its details, may prudently be held as somewhat tentative, until more rigorously verified. But the grand features of these movements, which may be confidently accepted, are very striking, and are very singularly related to the great basins of the lake region. The three main channels were the troughs of the great lakes, Superior, Michigan, and the couplet, Erie and Ontario, while be- tween these lay three subordinate ones in the basins of the great bays, Saginaw, Green and Keweenaw. The divergence of the striations from the main channels toward the range, in the case of the Green Bay valley, and, so far as the evidence goes, in other troughs, was an unexpected result, developed by combining individual observations; but, when the method of wasting and disappearance of a glacier is studiously considered, appears not only intelligible, but a necessary result, and one which finds partial illustration among existing glaciers. Topographical Relations and Distribution. —The topographical relations of the formation are an essential consideration, but may be best apprehended in connection with its geographical exten- sion, which now claims our attention. If westart with the north- ern extremity of the long known Potash Kettle Range, in Wis- consin, we find ourselves about midway between the southern extremity of Green Bay and Lake Michigan, and on an eastward sloping, rocky incline. The base of the range is here less than 200 feet above Lake Michigan, and is flanked on either side by the lacustrine red clays of the region; and seems, in some measure, to be obscured by them. From this point, it stretches away in a general south-southwestward direction, for about 185 miles, as- cending gradually, and obliquely, the rocky slope, until it rests directly on its crest. When within about twenty miles of the Illinois line, zt divides, one portion passing southward into that state, and the other, which we will follow, curves tothe westward, and crosses the Rock river valley. A profile of the rock surface across this valley, beneath the range, would show a downward curve of more than 300 feet. The range should not, perhaps, be regarded as sagging 14 210 Wisconsin Academy of Sciences, Arts, and Letters. more than half that amount, however, in crossing the valley, as the canon-like channel of the pre-glacial river, seems to have been filled without much affecting the surface contour of the drift. But the fact of undulation to conform to an irregular sur- face, produced by erosion, and not by flexure of the strata, is a point to be noted, as it is a serious obstacle in the way of any ex- planation that is only applicable on the supposition that the for- mation was in a horizontal position when formed, es the view that. it was produced by beach action, or the stranding of icebergs. After crossing Rock river, the range curves gradually to the northward, passing over the watershed between the Rock and Wisconsin rivers, ‘“ descends abruptly 200 feet into the low ground of the valley of the Wisconsin,”! crosses the great bend of the river, sweeping directly over the quartzite ranges, according to Prof. Irving, with a vertical undulation of over 700 feet, after which it gradually ascends the watershed between the Mississippi and St. Lawrence drainage systems, until its base reaches an esti- mated elevation of 700 to 800 feet above Lake Michigan.- From thence it has been traced across the headwaters of the Wisconsin river, by Mr. A. Clark, under my direction.” Within the Chippewa valley, it has been observed by Prof. F. H. King, of the Wisconsin Survey, and I have observed it in the vicinity of the Wisconsin Central railroad. This region is cov- ered by an immense forest, mainly unsettled and untraversed, even by foot paths, so that geological exploration is difficult and ex- pensive, and, as no industrial importance attaches to it, and the rock below is deeply concealed by it, I have not deemed it sufficiently important to trace the belt continuously to justify the large ex- penditure of time and means requisite, especially as I entertain no serious doubts as to its continuity and general position. The observations tnade, indicate that it descends obliquely the east- 1 Prof. Irving, Geol. of Wis., Vo}. II, 1877, page 616. 2To the eastward of the range, as thus traced, Col. Whittlesey describes (Smithsonian Contributions, 1866) a similar formation in Oconto county. I have observed the same at several points. Mr. EH. E. Breed informs me that it occurs on the watershed between the Wolf and Oconto rivers, but it has‘not yet been traced through the wilderness, to any connection with the main range, and it is uncertain whether it Is so connected or constitutes a later formation, as such later moraines have been observed at other points. Wisconsin Kettle Moraine. pala ern slope of the Chippewa valley, and crosses the river below the great bend (T' 32, R. Gand 7), near which the Flambeau, Jump, and several smaller streams gather themselves together, in a man- ner very similar to that of the branches of the Rock and Upper Wisconsin rivers, just above the point where they are crossed by the range. From this point the belt appears to curve rapidly to the northward, forming the western watershed of the Chippewa. It is joined in eastern Burnett county by a portion of the range coming up from the southwest, the two uniting to form a common range, analogous to that of eastern Wisconsin. The conjoint range thus formed, extends along the watershed of the Chippewa and Nemakagon rivers, to the vicinity of Long and Nemakagon lakes, on the watershed of Lake Superior. This part is given mainly on the authority of Mr. D. A. Caneday, who vis- ited a portion of the formation with me, and whose discrimina- tion can, I think, be trusted. Mr. EH. T. Sweet, of the Wisconsin Survey, describes! a kettle range as lying along the axis of the Bayfield peninsula, but it has not been ascertained that this is connected with the belt under consideration. Returning to the junction of the two ranges in eastern Burnett county, I have traced the belt thence southwestward through Polk and St. Croix counties to St. Croix lake, on the boundary of the state. The lower portion of this has also been studied by Prof. L. C. Wooster, of the Wisconsin Survey. Thesoutheastern range of the belt may be conveniently seen on the: North Wisconsin rail- road, near Deer Park, and on the Chicago, St. Paul & Minneap- olis line, to the west of the station Turner, but only in moderate force. If a good surface map of Minnesota be consulted, it will be seen that there liesalong the watershed, between the Upper Mis- sissippi and the conjoint valleys of the Minnesota and Red rivers, a remarkable curving belt of small lakes. Along this line, lies a chain of drift hills, known m its northwestern extension as the Leaf hills) Inthe Sixth Annual Report of the Geological Survey of Minnesota, received just as this article is going to the printer, 1 Manascript report on Douglas and Bayfield counties, to form a part of Vol. III, Geol. of Wis. 212 Wisconsin Academy of Sciences, Arts, and Letters. Prof. N. H. Winchell, speaking of the great moraines of the north- west, says: ‘ There are two such that cross Minnesota, the older being the Coteau and the younger, the Leaf nills. Corresponding to the latter, the Kettle Range in Wisconsin seems a parallel phe- nomenon.’ I have seen this belt, west of Minneapolis, and concur in Prof. Winchell’s opinion. I have also observed, hastily, what I regard as portions of it — dissevered by the river channels—on the peninsula formed by the bend of the Mississippi and the Min- nesota, south of St. Paul, and on the similar peninsula between the Mississippi and Lake St. Croix; and this seems to be the line of connection between the Wisconsin and Minnesota ranges. It appears to me, therefore, well nigh certain, that the Leaf hills of Minnesota are not only analogous to the Wisconsin Kettle range, but are portions of the same linear formation. The multitude of small lakes, found in Wisconsin, lie almost exclusively either along the Kettle belt itself, or in the area within, or north of it. The surface outside has a much more per- fect system of drainage, and is almost entirely free from lakelets. The Kettle range constitutes the margin of the lakedistrict. But in Minnesota, south of the Leaf hills, there is an extensive lake region stretching southward in a broad tongue, nearly to the center of Iowa, though the lakes are not very numerous in the latter state. The question naturally arises, whether this lake dis- trict is likewise bordered by similar drift accumulations, and this question, though not essential to the present discussion, has much interest in connection with it. In respect to this, I can only give some detached observations and quotations. As already stated, accumulations of this character oceur south of St. Paul. Still further to the southward, in the town of Aurora, Steel county, there is a moderate exhibition of gravelly boulder-bearing hill- ocks and ridges, accompanied by shallow basins and irregular marshes, much after the manner of the formation in question. From the descriptions of Prof. Harrington,* these features appear 1 Sixth Annual Rept. Geol. & Nat. Hist. Sur. Minn., p. 106. The R. R. profiles crossing this belt furnish valuable data. See Ann. Rept. for 1872, pp. 53 and 57, and Sixth Aun. Rept., pp. 47 and 156. ? Geol. and Nat. Hist. Sur. Minn., Ann. Rept. 1875, pp. 103 e¢ seq. Wisconsin Kettle Moraine. 213 to characterize the county somewhat widely, especially in the southern part. Near Albert Lea, in the adjoining county, on the south, and only a few miles from the Iowa line, there is a more prominent development of similar features, the ridges having a southwestward trend. Dr. C. A. White, in the Geology of Iowa,. describes a terrace in the northern part of the state, which, in its eastern extension, ‘‘ becomes broken up into a well marked strip of ‘knobby country.’ Here it consists of elevated knobs and short, ridges, wholly composed of drift, and usually containing more than an average proportion of gravel and boulders. Inter- spersed among these knobs.and ridges, are many of the peat marshes of the region.”? One knob he estimates as rising 300 feet above the stream at its base. This area lies in the line of the preceding localities, and near the Minnesota border. Between this “knobby country” and the Algoma branch of the C., M. & St. P. R. R., and stretching southwestward from the latter, there isa broad belt of low mounds and ridges, some of which show the structure and composition common to the Kettle moraine, while others present externally only a pebble clay, similar to that which characterizes the level country to the west of it. The whole presents the appearance of a low range modified by lacus- trine deposits. Near the center of the state, Dr. White describes a second range under the name of ‘“ Mineral Ridge,”*as consisting, ‘‘ to a consid- erable extent, of a collection of slightly raised ridges and knolls, sometimes interspersed with small, shallow ponds, the whole having an elevation, probably, nowhere exceeding 50 feet above the general surface, but, being in an open prairie region, it attracts attention at a considerable distance.” Both these ridges, Dr. White classes as probable moraines. This Mineral ridge lies south of the lake district, and may be regarded as forming its margin in that direction. On the western border, Dr. White describes ‘‘ knobby drift,” in Dickinson county, which, however, is ‘“‘ without perceptible order or system of ar- rangement.’’? To the northwest from this, we soon encounter the 1 Geol. of Iowa, 1870, p. 99. 2 Loc. cit. 3 Geol. of Iowa, Vol. II, p. 221. 214 Wisconsin Academy of Sciences, Arts, and Letters. morainic accumulations of the ‘‘Coteac de Prairie,” * and the “Cobble Knolls” and “ Antelope Hills.” These observations do not indicate a continuous, well defined range, but seem rather to point to a half-buried moraine, that only here and there, along its course, protrudes conspicuously, and this is the impression gained from an inspection of the formation. It is to be noted, as supporting this view, that, at least so far as’ the eastern side is concerned, this supposed moraine is flanked on the exterior by level plains, of smooth surface, often underlaid by sand and gravel, that seemingly owe their origin to broad rivers or lakes that fringed the border of the glacier, in its advanced state, when it probably discharged its waters over the moraine at numerous points, rather than at one, or a few, selected points, as would more likely be the case during its retreat, when accumula- tions of water could gather along its foot, within the moraine, and large areas be discharged at some single favorable point. But on the inner side of the moraine, the surface, although nearly level, in its general aspect, undulates in minor swells and sags, and the drainage is imperfect. The substratum, instead of being gravel, sand, or laminated clay, is generally a pebble or boulder clay. Outside of the moraine, the existing surface contour was formed in the presence, and, to some extent, under the modifying influence, of a fairly established drainage system. But on the znterior, the drainage system has not, even yet, become fully established, much less impressed itself upon the surface configuration, except in the vicinity of the main rivers. The terrace-like ridge mentioned by Dr. White, and some of the lines of hills described by Prof. Winchell in Minnesota, as running in a similar direction, may be perhaps regarded as minor morainic lines, stretching across the glacial pathway and marking oscillations in its retreat, analogous to some quite clearly made out in Wisconsin.? This southern morainic loop is, of course, presumed to be older than the Kettle range, and is here discussed because of the inter- 1 See note of Prof. Mather, Nat. Hist. Sur. 1st Dist. N. Y., p. 193. See also 2d Annual Re- port Geol. and Nat. His. Sur. Minnesota, by N. H. Winchell, pp.193 to 195; also loc cit., ante. 2 Geol. of Wis., Vol. II, 1876, p. 215 ef seg. Wisconsin Kettle Moraine. 215 esting way in which it is associated with the latter formation, and the suggestions it may contribute to the final solution of the main problem, to which the special one under discussion is only a trib- utary, viz.: the definite history of the Quatenary formations. Returning to the branching of the range in southeastern Wis- consin, we find the left arm, or that nearest Lake Michigan, strik- ing southward into Illinois. If we lay before us Prof. Worthen’s geological map of that state, and attentively observe its topo- graphical features and its drainage systems, it will be observed that nearly all the lakelets, the greater part of the marshes, and most of the region of abnormal drainage may be included in a curving line, rudely concentric with the shore of Lake Michigan, starting near the center of McHenry county, on the} Wiscon- sin line, and ending in Vermillion county, on the Indiana border. It may also be observed, on a similar inspection of Indiana, that nearly all the lake district lies north of the Wabash. In Wiseonsin, as already stated, we have found this area bor- dered by the Kettle range, which is itself notably lake-bearing. The range continues to sustain this relationship in Illinois, so far as I know it to be directly continuous. It exhibits a progressive broadening, and flattening, as it enters upon the level country that encompasses the head of Lake Michigan. The pebble clay deposit — not coarse boulder clay —that characterizes the flat couatry, and which, to the north, has been separated from the range by a belt of coarse boulder clay, here approaches, and ap- pears, to some extent, to overlap the range, and to be one cause of its less conspicuous character. From what I have seen of the region south of Lake Michigan, and from all I can find in geologi- cal reports relating to the region, I gather that the range, so far as it escaped the destructive action of the floods issuing from the Lake Michigan basin, both while occupied by ice, and subse- quently, is, to a large extent, buried beneath later deposits, or so modified as to be inconspicuous. Whatever the correct interpre- tation, it remains a fact beyond question, that the belt becomes very obscure, compared with its development to the northward. Dr. E. Andrews says: ‘As we trace it southward, the material ‘becomes finer, and the hills lower, until they shade off impercepti- 216 Wisconsin Academy of Sciences, Arts, and Letters. bly into the drift clay, of the Illinois prairies.” The members of the geological corps of Illinois did not recognize it distinctively, in the sense in which it is now considered, but Dr. Bannister, in his report on Lake county, says: “ In the western part of the county, near the Fox river, we find the ridges, in some places, to be largely composed of rolled limestone boulders. The same character has been observed further south along the same stream and remarked upon in the chapter on Cook county.”* In respect to McHenry county he says: “In the vicinity of the Fox river, the same kind of gravel ridges are met with as those which have been described as occurring in the western part of Lake county.” ® This lies in the belt identified by me, from personal observation, as belonging to the Kettle range. Concerning the district farther south, he says: ‘‘ Boulders of granite, quartzite, greenstone, and various other rocks are abund- ant in various localities on the surface of the ground, and are frequently met with in excavations for wells, etc., and large de- posits of rolled boulders, chiefly of limestone from the under- lying Niagara beds, similar to those already described in the report on Cook county, occur in the drift deposits of the adjoin- ing portions of Kane and Du Page counties.”* Concerning the topography, the same writer says: ‘ Along some of the prin- cipal streams, and especially the Fox river in Kane county, the country is more roughly broken, and can, in some parts, even be called hilly, although the more abrupt elevations seldom exceed eighty or one hundred feet above their immediate base.”° This broken country, if we may judge from what is true of the rough country along the same river to the north of this, it not due so much to the drainage erosion of the river as to the original depo- sition of the drift. The same features are said to continue into Kendall county, next south, which brings us to the vicinity of the ancient outlet of Lake Michigan, where, of course, the mo- raine is locally swept away. Still farther south, in Livingston county, Mr. H. C. Freeman mentions a ridge running southeast- * On Western Boulder Drift, Am. Jour. Sci., Sept., 1869, p. 176. peel: Sur. of Ill., Vol. IV, p. 130. 4Geol. Surv. of Ill., Part IV, p. 113. Loc. cit., p. 131. *Geol. Sury. of I., Part TV, p. 112. Wisconsin Keitle Moraine. ONG erly from a point in La Salle county, to near Chatsworth, a dis- tance of about forty miles. ‘This is gravelly and sandy, giving it a distinctive character as compared with the adjacent prairie.” * This is quite too meager to base an identification upon, but I have thought it worthy of quotation here. At Odell, which lies near this ridge, the drift is said to be 350 feet deep.” On the railroad line from Chicago to Kankakee, there is no recognizable indication of the formation under consideration. Southwestward from Kankakee, on the line to La Fayette, Ind., there are a few mounds and ridges that bear a somewhat mo- rainic aspect, but they are isolated in a generally level tract of lacustrine, rather than glacial, topography. They are, perhaps, remnants of a formation that has been largely eroded or buried. Near Fowler, in Benton county, Indiana, there isa belt of low mounds and ridges, accompanied by shallow depressions, that quite closely resemble the Kettle range in its more modified phases. Boulders appear upon the surface, and, in the more im- mediate vicinity of the village, are large and numerous. ‘This is probably a portion of the “stream of boulders two miles wide,” which Mr. F. H. Bradley mentions as extending through the eastern part of Iroquois county, Illinois, and the central part of Benton county, Indiana,? and which he attributes to floating ice. He does not, however, mention the associated topography or un- derlying drift formation. South of this low range, the country again becomeslevel, or gently undwiiting, as far as the Wabash.” The Indiana geologists have not yet critically examined the heavy drift region in the northern part of the state, through which the moraine might be supposed to pass, but in such prelim- inary inspection as has been made, they have not recognized any prominent moraine-like accumulation. The superficial expres- sion of the region is quite monotonous, and presents to view de- posits cf sand, gravel, lacustrine or pebble clays, but more rarely the coarse boulder clay or mixed material, that I regard as the unmodified ground moraine. The modifying agencies which produced this phase of the deposits, would be antagonistic to 1Geol. Surv. of Ill., Vol. IV, p. 227. 2.Geo]. Surv. of Ill., Vol. VI, p. 237. $Geol. Surv of Ill., Vol. VI, p. 236. 218 Wisconsin Acudemy of Sciences, Arts, and Letters. ridge-like morainic accumulations, and their presence, in sharp outline, is not to be expected. Inthe vicinity of Ligonier, in Noble county, there is a feeble, butsomewhat characteristic devel- opment of some of the features of the formation. So also, in the vicinity of Rome and La Grange tothe northeast. Between La Port and Otis there isa kindred, though somewhat peculiar formation, but I am in doubt as to its true character. On entering Michigan, we find the formation more unequivo- cally developed. Just north of Sturgis, which is near the south- ern line of the state, the formation appears in marked develop- ment. It does not attain a great altitude, but presents the peculiar strongly undulating and hummocky contour, and the coarse, mingled material, characteristic of the deposit. It may be seen to advantage on the line of the Grand Rapids & Indiana R. R. To the northeast in the vicinity of Albion, it may beseen from Springport on the north, to Condit on the south. It is here broad and flat, and superficially composed of gravel, for the greater part, but some of the deeper excavations reveal the char- acteristic coarser material. Onthe Michigan Central R. R., the formation may be observed between Jackson and Dexter, the most prominent portion being between the stations Francisco and Chelsea. It isnot very prominent on the immediate line of the road, which was doubtless selected to avoid it, butin the vicinity it rises into prominent hills and ridges. Some of these, on the north, are conspicuous objects at considerable distances. Still farther to the northeast, my friend, Dr. D. F. Boughton, whose identifications I have elsewhere verified, informs me that the range is well developed in Oakland county, and is finely exhib- ited near the line of the Flint & Pere Marquette R. R., between Plymouth and Holly. Still farther to the northeast, it may be seen at great convenience and advantage, along the Detroit & Milwaukee R. R. from Birmingham, below Pontiac, to Holly. On the flanks, its features are subdued, the hills and ridges being rather low, with more or less level surface between them, and the superficial sands and gravels are prevalent; but from Waterford to beyond Clarkston, the range has a fine, though irregular devel- opment. ‘The hills rise with characteristic contours, to an esti- ed Wisconsin Kettle Moraine. 219 mated altitude of 200 feet or more above the surface of the beau- tiful lakelets embosomed at their base. The deep cuts near the latter station, amply exhibit the coarse, commingled material, characteristic of the core of the range. Putting the foregoing observations together, they seem to es- tablish beyond reasonable doubt the existence of a broad, massive belt stretching northeastward on the highland between the Sagi- naw and Hrie basins. If we return again to the southwestern part of the state, we are informed by Dr. Boughton that we shall find a similar accu- mulation at, and in the vicinity of, Kalamazoo. To the north- northeast, in Barry county, the Thorn Apple river cuts across this range between Sheridan and Middleville. This belt here, though broad, presents a more prominent and ridge-like aspect, with bet- ter defined limits than elsewhere observed in Michigan. ‘To the north of this, opposite Saginaw bay, there occurs, near Farwell, broken, rough country and abundant coarse drift, that probably belongs to the belt in question, but my opportunity for observa- tion was unsatisfactory. Beyond this point, I have no definite information, but I deem it highly probable that the moraine will be found extending some distance farther, on the highlands of the Peninsula. _ The lake survey charts show that Grand Traverse bay has the remarkable depth of over 600 feet. This great depth, together with its linear character, and the form and arrangement of the associated inlets and lakes, has suggested that it may have been the channel of a separate minor glacier, analogous to that of Green Bay on the opposite side of the great lake, but I have no direct evidence that such was the fact. In the reports of the geological survey of Ohio, a formation of nearly, or quite, identical characteristics is carefully described by the several writers whose districts embraced it. In the second volume,’ Dr. Newberry gives, under the name of “ Kames,” an excellent summary of its leading features. These harmonize very nearly with those of the Kettle belt. The main points of differ- 1Pages 41-47. See also ‘“‘Surface Geology of Northwestern Ohio,” Proc. Am. Assoc. Ad. Sci., 1872, by Prof. N. H. Winchell, under heads of St. Johns and Wabash Ridges. 220 Wisconsin Academy of Sciences, Arts, and Leiters. ence are the less conspicuous character and massiveness of the Ohio range, and the greater prevalence of :ssorted and stratified material; in other words, its features are the same that the Kettle range presents in its more subdued aspects, especially where it is formed in a comparatively smooth country, and is flanked by pebble clays, with level surface, instead of coarse boulder clay, with ridged, or mammillary, contour. I cannot turn aside, here, to define, with sufficient cireumspection, the distinction between these clays, further than to indicate my belief that the former are sub-aqueous, and the latter sub-erial, or, if you please, sub- glacial, deposits." Where I have seen the Ohio formation, it presents almost pre- cisely the characteristics that are exhibited by the Kettle range in northern Illinois, where it is similarly related to plane topog- raphy and pebble clays, and it is also very similar to the same formation opposite Green Bay, where it is bordered on both sides by red lacustrine clays of later date. Dr. Newberry quite clearly recognizes the parallelism, but perhaps not the identity, of the formations. Col. C. Whittlesey, in his article on the ‘“‘ Fresh Water Glacial Drift of the Northwestern States,’? classes the formations together as identical in character, though he does not seem to have considered them members of a continuous forma- tion, and could not well do so with the prevalent view, which he somewhat emphasizes, that it is peculiarly a summzt formation. It very often does occupy the summit of a rock terrane, and it some- times forms a watershed by its own massiveness, but it likewise occupies slopes and crosses valleys, as shown in detail in the Wis- consin report. Prof. Andrews of the Ohio survey, in a personal communication, adds his conviction that the Ohio and Wisconsin deposits are parallel formations. It would seem, then, that the only question relates to the continiity of the belts. Unfortunately there intervenes the Wabash valley, the ancient drainage channel 1T have mapped these formations separately in Eastern Wisconsin. See Atlas accompa- nying Vol. II, Geol. of Wis., 1877, {Plate III, Map of Quaternary formations. See, also, p. 225 of the volume. * Geol. Surv. of Ohio, Vol. II, pp. 4. 5, and 43. Dr. Newberry’s views as to the origin of the Ohio ‘‘ Kame” belt are ct variance with those here presented. 3 Smithsonian Contributions, 1866. Wisconsin Kettle Moraine. 221 of the Erie basin. Absolute continuity undoubtedly does not exist. Jf my views are correct, this was the great —not exclu- sive — channel of discharge of the glacial floods, at the very time the moraine was being formed, where it could be formed, and, for that reason, the debris was swept away or leveled. In addition to this, the region has been subjected to the vicissitudes of erosion, of a reversal of drainage systems, and of lacustrine and fluviatile accu- mulation. Itis to be presumed, therefore, that a portion of the range, where once formed, has been lost, leveled, or buried. Some remnant indications of the range, on the upper slopes, might, however, rationally be presumed to exist. But, awaiting a criti- cal examination of the region, we must confess a want of direct evidence. The belt stretches entirely across Ohio and enters In- diana, but has not been traced farther. In the line of indirect testimony, however, some facts may be noticed. Prof. N. H. Winchell describes in the Ohio reports! six ridges running parallel to Lake Hrie, and Mr. G. K. Gilbert has described that portion of these which lie in the more immediate Maumee valley.” -T'wo of the inner ones are conceded to be lake beaches. ‘The two outer ones are members of the ‘‘ Kame,” or Ket- tle belt, according to Dr. Newberry.* The one next within, the St. Mary’s ridge, Prof. Newberry distinguishes, apparently, with justness, from both the other classes. Mr. Gilbert gives a clear and discriminating description of this, and expresses the convic- tion that it is ‘‘ the superficial representation of a terminal glacial moraine, that rests directly on the rock bed and is covered by a heavy sheet of Hrie clay, a subsequent aqueous and iceberg de- posit.”* The views of Professors Newberry and Winchell, while they each differ somewhat, agree with this in the only point essen- tial to the present discussion, viz.: that this ridge represents the mar- gin of the glacier at the time tt was formed. This shows the glacier to havebeen a tongue or lobe of ice, differentiated from the sup- posed continental glacier, and having its axis coincident with the Maumee valley, and, withal, capable of forming a morainic ac- cumulation on both sides. The St. Mary’s ridge crosses the 1 See also Proc. Am. Assoc. Ad. Sci., 1872. 2 Geol. Surv. Ohio, Yol. I, pp. 537 ef seq. 3 Geol. Sur. Ohio, Yol. II, pp. 56 and 57. * Loe. cit. 222 Wisconsin Academy of Sciences,“Arts, and Letters. Maumee - Wabash valley — the glacial trough — and, recurving upon itself, bears away to the northeast, approximately parallel to the Kettle belt already described in southeastern Michigan. This wing of the St. Mary’s ridge bears the same relation to the Kettle belt bordering the Erie basin on the Michigan side, that the opposite wing does to the “‘ Kame” belt on the south side. The force of this relationship is not easily escaped. If my viewsare correct, that this Michigan belt was formed along the right hand margin of the Erie glacier (conjointly with the Saginaw glacier), just as the “ Kame” belt was formed on the left hand margin, then its composition should give evidence of the fact. In the case of the Green Bay glacier, I have shown that the lines of striation and transportation diverge from the main axis toward the margin,’ and, so far as the paths of other glaciers lie within Wisconsin, the observations made upon them, imply the same method of movement, and this habit finds partial exemplification among the glaciers of the Alps— partial, be- cause their contracted valleys and steep slopes afford little oppor- tunity to deploy in this fashion. If this manner of movement holds true with the Hrie glacier, material from its trough will be found to have been transported westward and northwestward toward the moraine. Thirteen years ago, in an article in the American Journal of Science, entitled, ‘‘ Some Indications of a Northward Transportation of Drift Material in the Lower Penin- sular of Michigan,”’® Professor Alexander Winchell called atten- tion, with much detail and precision, to a large mass of evidence, which finds, for the first time, so farasI am aware, satisfactory explanation in the view now presented, and, in return, has the force of confirmatory evidence. It appears that immense, and often but slightly eroded masses of Corniferous limestone, have been borne in the direction indicated, and scattered over the areas of the Hamilton group, the Marshall sandstone, and the Subcarboniferous limestone; that similar blocks of Hamilton rock have been deposited over the two last named formations and even beyond ; that the Marshall sandstone has likewise been borne on to the Carboniferous limestone, and that this transportation has 1Geol. of Wis., Vol. Il, pp. 199 et seq. 2 Am. Jour. of Sci., Vol. XL, Noy., 1865, Wisconsin Kettle Moraine. 223 been from lower to higher levels, as the strata now lie, and are presumed to have lain, since the basin is one of excavation and not of flexure. These phenomena, in all their details, are pre- cisely what we should expect from the action of a glacier advane- ing through the Hrie valley, and moving in a manner analogous to that of the Green Bay glacier. That a glacier moved through this valley has been abundantly shown by the Ohio geologists. The only labor of this article is to show that it was an individual- ized stream, forming the Ohio ‘‘ Kame” beit on one side, and the Michigan on the other, simultaneously, and that they are collat- eral members of a common moraine. Eastward from Ohio, there has been, so far as I am aware, no definite attempt to trace out the extent of the belt. In western New York, Prof. Hall mentions, as one of the three general as- pects of the superficial deposits, a surface “ broken into irregular hills or ridges, with deep bow]l-shaped depressions, or long valleys, which often communicate in more extensive ones, or are enclosed on all sides by drift,” * but he does not definitely locate the forma- tion, or indicate whether it assumes the form of a belt, or other- wise. In central New York, Prof. Vanuxem says: “There is another class of deposits, well defined as to position, but irreg- ular as to composition, which ure worthy of note. They occur in the north and south valleys, which are on the south of the Mo- hawk river, or the great level.” “The whole of these deposits have a common character. They are in short hills, quite high for their base and are usually in considerable numbers.” “ They con- sist of gravel, of stones also of greater size, sand and earth.’’2 These, he says, greatly resemble the “ deluvial elevations” no- ticed in the survey of Massachusetts,’ the dezeription of which is perfectly applicable to the formation under consideration. Fur- thermore, Prof. F. H. King, of the Wisconsin survey, has exam- ined the same deposits in the vicinity of Ithaca, and recognizes their identity in kind. Neither of these observers, however, dis- cern a definite belt, although Prof. Vanuxem destroys the force of his apparent limitation of the formation to the valleys, by stat- 1 Nat. Hist. Surv. 4th Dist., Geol., Pt. LV, pp. 320, 321. 2Nat. Hist. Surv. N. Y., 3d Dist., p. 218. 5 Geol. of Mass., E. Hitchcock, 1833, p. 144, 224 Wisconsin Academy of Sciences, Arts, and Letters. ing that there are numerous points where it has formed over the hill sides, and by associating in mention with it accumulations on the “heights, apparently in no regular order.” * As these are deep, canon-like valleys, they would probably modify in some de- gree, the comparatively thin margin of the glacier, giving it a somewhat digitate outline, and the greatest accumulations would take place near the extremities of the tongues, in the valleys, so far as drainave permitted; while the connecting chains would form retreating lines, and be less conspicuous, and might, there- fore, escape observation not definitely turned to the subject. This, at least, is suggested by some observations of my own in similar situations. Such valley accumulations, however, do occur at the extremities of linear glacial lakes that are unconnected witha definite belt, as in the case of Green Lake, Wisconsin.” On the line of the Erie R. R., along the small tributary of the Delaware river that is followed up, westward, from Deposit, I have observed winding Osar-like ridges, parallel to the valley, and Kame-like hills upon the slope, up to the watershed of the Delaware and Susquehanna; likewise in the valley of the latter, at and near the village of Susquehanna, but I have no knowledge of their intimate structure, extent, or relations. In the southeastern district of New York, Prof. Mather recog- nizes the distinctive aspect of this class of accumulations.® He cites several instances of its occurrence on the east side of the Hudson, leaving the impression that they are local features. But on Long Island, it forms ‘‘an elevated ridge, called by some, ‘Green Mountains,’ and by others, the ‘ Backbone’ of theisland.” 4 This he describes in detail and maps, showing thatit branches at the east, one chain extending along the southern peninsula to Montauk Point, and the other, along the northern to its extremity, and, theoretically, to the islands beyond. Professors Cook and Smock have recently examined this, and have shown its connection with a similar moraine, that stretches across the northern part of New Jersey, from Perth Amboy to 1 Loe. cit., p. 219. 2 Geol. of Wis., 1877, Vol. IT, p. 138. 3 Nat. Hist. Surv. N, Y., Ist Dist., Pt. LV, p. 212. 4 Loc. cit., p. 161. Wisconsin Kettle Moraine. 295 the Delaware river, below Belvidere. The descriptions of this range tally quite perfectly with that of the Kettle moraine. This range, however, lies on the margin of the area of northern drift, while the western one is medial in position, and at some points is quite distant from the margin. It will be observed, nevertheless, that this distance is greatest, in general, at the west, and that in ‘Ohio it becomes very greatly reduced, so that the fact of coinci- dence on the Atlantic coast, presents no reason for supposing the ranges to be distinct. But, whether distinct or not, is a matter to be settled by observation, and it is to be hoped that it will not - long remain undecided for want of it. The extension of the New Jersey moraine westward has not, so far as I can learn, yet been traced, but the survey of Pennsylvania, in progress, will, doubt- less, soon leave nothing to be desired, so far as that State is in- volved. To the eastward, Mr. Warren Upham has recently been en- gaged in studying its probable continuation in southeastern Mas- sachusetts. In a personal communication he writes: ‘ A very clear line of terminal moraine extends along the chain of the Elizabeth islands southeast of Buzzard’s Bay ; thence it bends to the northeast and north as far as to North Sandwich, when 7 turns at a right angle to the east, and extends through Barnstable and other towns to Orleans, running along the east and west portion of Cape Cod, and terminating at its east shore.’ ‘This terminal moraine, like the ‘ Kettle moraine’, is not at the outmost limit reached ‘by the ice-sheet; for hills, in series nearly parallel to the moraine. already described, and similarly composed of glacial drift with many boulders, occur on Martha’s Vineyard and Nan- tucket islands, corresponding, perhaps, to the terminal moraine which forms the ‘backbone’ of Long Island. * * The moraine of the Elizabeth islands and Cape Cod has a length of about 65 miles.” It may be suggested that the range along the Hlizabeth islands may correspond to the northern branch of the Long Island moraine described by Prof. Mather, and that, as Mr. Upham sug- gests, that of Martha’s Vineyard and Nantucket corresponds to the southern. 1 Ann. Rept. of State Geologist, N. J., 1377, pp. 9¢t seq. 15 226 Wisconsin Academy of Sciences, Arts, and Letters. Dr. E. Hitchcock refers to these accumulations in his report on the geology of Massachusetts,’ and classes with them “diluvial elevations and depressions,” occurring at other points in that and. adjoining States. It would appear, from the geological reports of the Eastern States that analogous, though not certainly identical formations, occur locally, more frequently than in the interior, and this, from the mountainous nature of the country, is not strange; but no continuous massive range seems to have been discerned, except the southern one already described. In the interior, so far as yet ascertained, the drift limit is not marked by any such persistent ridge-like accumulation, but grad- ually dies away or is buried by later deposits, so that the precise limit of glacial advance is not easily determined. The only ap- proach to an exception to this, known to me, is the case of the Kettle moraine in Central Wisconsin, where it lies near the border of the driftless area. Elsewhere around that area, the drift thins out very gradually, so as to render the mapping of its margin a work of close inspection ; and, as the region presents no evidence of subsequent submersion, or any other special modifying agency, except the usual meteorological forces, this would seem to repre- sent approximately the original form of deposit. It is evident from the foregoing sketch that much observation remains to be made before the complete geography of this forma- tion is determined. The conjectural lines on the map are only theoretical suggestions, preliminary to observation. Summary.— It may be helpful at this point to summarize, and bring into close juxtaposition, in thought, the leading characteristics of this remarkable formation. 1. Its linear extent is very great, whatever its final limits may be found to be. 2. It has a width of from one to thirty miles. 3. Its average vertical thickness can only be very roughly esti- mated, but may, very prudently, be placed at 200 or 300 feet. 4. Its surface configuration is peculiarly irregular, and denotes an extraordinary origin. 1Geol. of Mass. 1833, pp. 144 ed seq. Wisconsin Kettle Moraine. : PAT] 5. It is a complex range, the component ridges being often ar- ranged in rude parallelism. 6. A distinction is usually to be observed between the super- ficial and lateral portions of the deposit on the one hand, and the central, underlying one on the other, the former being chiefly sand and gravel, the latter complex commingled debris. 7. The superficial sands and gravels are usually stratified in various attitudes, but the core of the range is mainly unstratified. 8. The irregularities of the range are most conspicuous where the superficial sands and gravels are least abundant. 9. The material was derived, in part, conspicuously so, from the vicinity of the range, and, in part, from the formations lying backward along the line of drift movement for at least 300 miles. 10. A portion of the material is spherically rounded, a part is scratched and polished, and some is little affected, though some- times soft or friable, the latter being usually from adjacent for- mations. 11. The range is tortuous in its course, but sustains a remark- able and significant relationship to the great lake basins. 12. It undulates over the face of the country, varying at least 800 feet in its vertical oscillations. 13. It does not sustain any uniform relation to present, or what are presumed to have been, preglacial drainage systems in their details. In some portions, it occupies water-partings; in others, lies on slopes; and in still others, stretches across valleys. 14. It crosses, in its course, all the indurated formations, from the Laurentian to the Coal measures, but exhibits no specific rela- tion to their strike or dip. 15. It sustains a definite and most important relationship to the lines of general drift movement. 16. The range is frequently flanked on its southern, or outer edge, by level areas of sand aiid gravel, of greater or less extent. These also occur between the component ridges of the belt, and on the inner flank, but less frequently. 17. The surface contour of the adjacent region within, or north of, the belt, usually, though not invariably, has a less perfect drainage system, and exhibits less noticeably the effects of super- ficial modification, than the outer side. 228 Wisconsin Academy of Sciences, Arts, and Letters. Origin.-— Waiving, for the present, some further generalizations, it is thought that the foregoing phenomena present a specific com- bination which points unequivocally to a morainic origin. ‘To the writer, familiar with the multitudinous details, that cannot here find a place, and having studied recent moraines with special refer- ence to this formation, they have a force little less then demon- strative. The range is confidently regarded as a moraine formed at the margin of a group of glaciers — which may be regarded as a single lobate one —and marking a definite stage of their history. A more vivid and graphic view of the outline and movements of these glaciers, than can be given in words, may be obtained from Ahe accompanying map, from which it will appear that through each of the great lake troughs there poured an ice stream, at- tended by minor currents through the lesser channels. Its Medial Position.— It has already been remarked that, in the interior, this moraine does not mark the extreme limit of glacial advance. Numerous striations, and other evidences of glaciation, occur on the south side of it. A line has been drawn on the inap intended to indicate the approximate limit of northern drift, based on several authorities! How nearly this shows the limit of actual glacial progress, in distinction from other means of transportation, is not, I think, as yet definitely ascertained, but the general fact of progress, to a considerable distance beyond the Kettle moraine, is sufficiently established. 'The moraine was, therefore, formed after the retreat of the glacier had commenced, and marks a certain stage of ats subsequent history. Glacial Movements before the Formation of the Moraine.—It be-— comes an interesting question to ascertain whether the glacial movements were the same before the formation of the moraine, as afterwards. Fortunately, in southern Wisconsin, we have very definite and specific evidence bearing on this question. In the towns of Portland and Waterloo, which lie within the area of the Green Bay glacier, and from twenty-five to thirty miles distant. from the moraine, there are several domes of quartzite that rise through the horizontal sandstones and limestones, which occupy the surrounding region. These domes are glacially abraded and grooved in a direction S. 80° W., and trains of quartzite boulders 1Tesiey, Newberry, Cox, and assistants, Worthen, Swallow, and Mudge. Wisconsin Kettle Moraine. 229 stretch away in that direction to the moraine, and, mingling with it, pass onward to an equal distance beyond. At the same time there is abundant evidence from the material of the drift, from the surface contour and from striation, recently observed by Mr. I. M. Buell, that the westerly movement of the Lake Michigan glacier, near the Illinois line, extended to the west side of Rock River, and that the line of junction of the two glaciers was on the west sideof thatstream. It appears then, that in this region, the move- ments were in the same general direction before and after the formation of the moraine, but that there were changes in the de- tails, and that the relative size and position of the glaciers were somewhat different, the Green Bay glacier being relatively smaller in the earlier epoch. ‘Testimony of similar general import, but less specific, may be gleamed from the reports of the other states involved. Method of Formation.— Tf, then, the glacial movements were the same, in general, before and after the formation of the moraine, and yet the minor movements and relative size of the glaciers somewhat different, how was the moraine formed? A halt in the retreat of the glaciers, by which their confluent margin should re- main stationary for a period, would doubtless cause an unusual accumulation of debris, but this would fail to aecount for the varying width or irregularities of the moraine. The structure of the range seems to indicate an alternating retreat and advance of the ice mass. During the former, debris was thrust out at the foot of the melting mass, which, when the glacier advanced, was plowed up into immense ridges. If this process be repeated several times paralled ranges will be accounted for, and the irreg- ularities incident to such advance and retreat will explain the complexity of the range. Where the later advances were equal to the earlier ones, the accumulation of drift material would be forced into a single massive ridge. Where any advance failed to equal a former one, an interval between the accumulations of the two would result, giving rise toa depression whose form would depend upon the relations of the two accumulations, but would in. general be more or less trough-like in character. Where tongues of ice were thrust into the accumulated material an irregular or 230 Wisconsin Academy of Sciences, Arts, and Letters. broken outline would be the result. If masses of the ice becama incorporated in the drift, as has been suggested, their melting would give rise to depressions, constituting one form of the kettles that characterize the range. The suggestion Just made, with ref- erence to the irregular advance of the ice mass, accounts for other forms, and, at the same time, for the irregular hills, mounds, and hillocks. Certain of the kettles may be due to underdrainage, through the action of strong underground streams that occasion- ally flow, as full brooklets, from its base. The drainage of the glacier, while it was advancing and pushing the debris betore it, was probably quite general and promiscuous over the moraine, and this would give rise to the stratified sands or gravels, and other evidences of the action of water, among which may perhaps, be reckoned some of the minor mounds, ridges and depressions. The changing attitudes, which the debris would be likely to as- sume, as it was forced along, would, perhaps, give peculiar force to torrential effects. The gaps in the range, attended by plains, or long streams of gravel and sand, appear to represent the more considerable points of discharge of the glacial floods. When the surface about the margin of the glacier permitted the accumulation of water, the moraine would doubtless be much modified by it and present a subdued aspect. The Alpine moraines, above referred to, are regarded as minia- ture exemplifications of the process by which the Kettle moraine was formed. Bet, in addition to the structure of the range, the change in the relative position of the Green Bay and Lake Michigan glaciers, already alluded to, affords evidence of an exceedingly interesting character, which has a significance much beyond what can be here indicated. It appears that the junction between the Green Bay and Lake Michigan glaciers at the last observable stage, preceding the formation of the Kettle moraine, was about twenty-five miles farther west, than at the time of the latter’s formation, or, in other words, there is an abrupt easterly shift of the line of junction. It appears, also, that the width of the ante-morainic Green Bay glacier, measured just south of the Kettle moraine, was only half Wisconsin Kettle Moraine. © 231 that of the post-morainic glacier, north of it, measured at a dis- tance just far enough to escape the terminal curvature. An in- spection of the outline of the Green Bay glacier shows that this eastward shift of the junction of the two glaciers was not due simply to encroachment on the Lake Michigan stream, nor to a common movement of both in that direction, for the opposite margin of the Green Bay glacier lay close upon the borders of the driftless region, demonstrating that there was no eastward swaying on that side. Indeed, the indenture of the outline of the driftless area strongly suggests actual encroachment on that side also, and this view is not without independent support. In harmony with these phenomena are the fiords of the Green Bay perinsula, which indicate that the Green Bay ice stream over- flowed into the basin of Lake Michigan. These facts, taken al- together, seem to warrant the belief that both glaciers retreated sufficiently far to the northward, and within their respective basins, to allow time and opportunity for the change in the rela- tive size and position of the two ice streams, and that, under slightly changed conditions that favored the Green Bay glacier, they advanced to the position of the Kettle moraine, and, after a series of oscillations, retreated permanently. This view seems also to be demanded by certain details in the distribution of the drift material that are otherwise enigmatical, but whose discussion would too much extend this article. Significance.—As forty-five years have passed since Dr. Hitch- cock called attention to some of the phenomena under consider- ation, or, at least, to some distinctly related to it, and yet, the matter has received so little consideration, that our present knowledge is limited to such a degree, that I lay myself liable to the charge of undue temerity in attempting to correlate the observations, | may be pardoned in attempting to indicate, briefly, something of the significance and importance the foregoing conclusions, if sus- tained, have in relation to the Quaternary history of the region involved. The moraine constitutes a definite historical datum line, in the midst of the glacial epoch, and becomes a basis of reference and correlation for adjacent formations. It isan historicalrampart, outlining the great dynamic agency of the period, at an important 232 Wisconsin Academy of Sciences, Arts, and Letters. stage of its activity, and separating the formations on either hand by a chronological barrier. It is manifest that the true Boulder Clay, or ground moraine, south of the belt, must have been formed earlier than that north of it, and that the two portions are not at all synchronous. In sedimentary formations synchronism is found in horizontal strata, but in glacial deposits it is to be sought in linear belts, concentric with the margin of the glacier. This fact finds illustration, and emphasis, in the demarcation introduced by this singular corrugation of the wide-spread glacial sheet. It is difficult to limit the value of such a determinate line, in the midst of the complex drift formations, if fully established, and should similar belts be found to mark other steges of glaciation, there would be opened a definite line of investigation that promises much assistance in unraveling the gnarled skein of Quaternary history. While it does not follow, necessarily, that all formations over- laying the true glacial clay, south of the Kettle moraine, are older: than those occupying similar relations to the newer Till, north of it, it is clear, that similarity of stratigraphical sequence is not, by any means, sufficient ground for assuming chronological equiva- lence. It is evident, that all endeavors at correlation between the: superficial deposits, on the opposite sides of the moraine, should be attempted with much cireumspection. These suggestions have especial application to the discussion of the vegetal deposits, so frequently found in the later Quaternary formations. By many writers, the various deposits of this kind, in the Mississippi basin, have been, very naturally, in the present. state of our knowledge, grouped together without reference to the necessary discriminations above indicated, and, as a result, beds. of diverse age are referred to a common stratum. A general dis- cussion of these deposits is not sufficiently germane to our sub- ject to be fittingly introduced here, but it is appropriate to point. out the fact that some of the vegetal strata sustain such a relation to the Kettle moraine, that they must be widely separated from others, in the date of their accumulation and burial. Some of these organic strata lie at the immediate foot of the moraine, be- neath fluviatile and lacustrine deposits that, I am confident, began Wisconsin Kettle Moraine. 233 to be accumulated during the accumulation of the moraine, and through the agency of glacial floods; while it is even more cer- tain, that other vegetal deposits accumulated much subsequently, as those found in the red clays of Wisconsin, which are lacustrine deposits of the great lakes formed after the recession of the glacier. It would be too much to assume that all plant remains, found south of the moraine, antedate its formation, but it is safe to affirm that, with only phenomenal exceptions, e. g., such as escaped glacial abrasion, all north of it are more recent. The bearing of these definite determinations of the glacial outlines and movements upon the question of the origin of the remarkable driftless area of Wisconsin, Minnesota, Iowa and Illinois (see map) was early perceived, and it was clearly foreseen that this line of investigation promised a demonstrative solution of the problem. The driftless area manifestly owes its origin to the divergence of the glaciers through the Lake Superior channel, on the one hand, and that of Green Bay and Lake Michigan, on the other, and to the obstacle presented by the highlands of northern Wisconsin and Michigan. This obstacle the glacier surmounted, and passed some distance down the southern slope, but apparently not in sufficient thickness to overcome the melting and wasting to which it was subjected, and so it terminated midway the slope. But the deep, massive ice currents of the great channels pushed far on to the south, converging toward each other; and, if they did not actually unite, at least commingled their debris south of the driftless area.’ An instance closely similar to this, considered from a dynamical point of view, may be seen, at the present termination of the Viesch glacier, and illustrations of the general principles involved in the explanation may be seen in connection with several other Alpine glaciers. If the evidence adduced to show that the Kettle moraine was due to an advance of the glaciers be trustworthy, then, to the extent of that advance, whether much or little, the moraine marks a secondary period of glaciation, with an interval of deglaciation 1Compare N. H. Winchell in An. Rep., Geol. of Minn., 1876, and R. D. Irving, Geol. of Wis., Vol. II, 1877, whose views are closely analogous to the above and each to the other but, are not strictly identical. See, alzo, J. D. Dana, Am. Jour. Sci., April, 1878. 234 Wisconsin Academy of Sciences, Arts, and Letters. between it and the epoch of extreme advance. Its great extent indicates that whatever agency caused the advance was very wide spread, if not continental in its influence. The moraine, there- fore, may be worthy of study in its bearings upon the interesting question of glacial and interglacial periods. It will also furnish definite data bearing upon the somewhat mooted question of the origin of the Great Lakes, as well as other questions involving both perglacial and postglacial topography. DEPARTMENT OF THE MATHEMATICAL AND PHYSICAL SCIENCES. ROTATION AS A FACTOR OF MOTION. By PRoFessor J. G. MCMURPHY, KEnosHa. When an elastic ball is thrown against a plane surface it re- bounds from that-surface according to certain fixed laws. Its position at any moment will depend on certain conditions. The elasticity of the ball, the angle of projection, the rotation of the ball on its own axis, the velocity, will all of them affect the re- bounding of the ball. Velocity and elasticity affect the distance to which it will rebound; the angle of projection and angular mo- tion will affect the direction of rebounding. A ball projected perpendicularly against a plane surface will re- bound in the same line, making due allowance for the attraction of gravitation, which finally comes and controls its motion. The resistance of the air is no inconsiderable factor. (In point of fact, it is the latter only which is opposed to the force with which the ball rebounds, for gravity acts at right angles to this force and is not opposed to it.) Tf the ball, without rotation, is projected against the plane sur- face at any angle, excepting ninety degrees, it will rebound so that the- angle of reflection shall be equal to the angle of inci- dence ; modified, of course, by gravitation and the resistance of the air. Let us add another factor and examine the result. Given a hori- zontal plane surface in front of the vertical plane. Let the ball 236 Wisconsin Academy of Sciences, Arts, and Letters. be placed upon it and propelled perpendicularly against the ver- trical plane by a blow, which takes effect above its center of grav- ity. Such a blow will impart to the ball a rotary motion, together with an onward motion or translation. When the ball reaches the vertical plane its rebounding force, due to translation, will tend to make it retrace its path, while the force due to its rotation will tend to make it climb the vertical plane. It is actuated by the resultant of these two forces, and rebounds through the air, in the plane of those forces following the diagonal of the rectangle of forces, The following diagram* may serve to make the explanation more apparent: Let A, B, C, D, be the vertical plane; C, D, H, F, the horizontal plane ; _ Let a be the point from which the ball d is propelled on a-b; the ball es we, having a forward DS eS a ee rotary motion; b-d del the distance the ve ball would re- One bound by virtue ® A B F of its rectilinear motion; 0-c the distance it would climb by vir- tue of its angular motion. Then will it be found somewhere on the line b-e. Being a rectangle of forces, the resultant may be expressed by the formula b-e = /(-c)+(6-d). If the ball is propelled from a point to the right of its center of gravity, and constrained to keep the same perpendicular course, it will have a negative or left-hand rotation ; when it strikes the vertical plane it will not return in the same path, but will be re- flected to the right, so that the angle of reflection is not equal to the angle of incidence. But just as before, the path of the re- turning ball is the resultant of two forces acting at right angles — to each other. If the angular velocity is very great, compared *No cuts having been furnished by the author, the printer has been obliged to construct the accompanying figures, which are necessarily very imperfect. Rotation as a Factor of Motion. 237 with the velocity of translation the deflection from a perpendicu- lar will be very great and vice versa. When the ball is propelled against the vertical plane at any other angle than a right angle with a rotary motion besides, the problem becomes somewhat more complicated. Let the ball be propelled from a Es Blau ool sens) Cah 9 aa with a positive rota- tion. By its motion of translation it ought to rebound in the path which makes it : + c the angle of reflec- ae | ~ tion, equal to the. salt is, Soo angle of incidence oa But by its rotation » a against the fixed point, 6, it would tend toward c; hence it will take the direction b-e, and be measured by the diagonal parallelogram of forces, represented by b-a@ and 6c. Here it is plain that the angle of reflection is much less than the angle of incidence. If the rotation be a negative or left-hand rotation from the same point, a, following the same path, a-d, the result- ant will be nearer a perpendicular — that is, the angle of reflec- tion will be greater than the angle of incidence. If a ball be thrown perpendicularly against a vertical plane sur- face with a positive rotation it will rebound to the left, if the rota- tion be negative it will rebound to the right, if the rotation be for- ward the ball will rise, if backward it will fall. If the ball be thrown obliquely to the left, with positive rotation, the angle of reflection will be less than that of incidence. If thrown obliquely to the right, with same rotation, the angle of reflection will be greater than that of incidence. The combinations are almost in- finite, and afford a variety of valuable observations. There are some very curious and interesting experiments in compound direct motion. If a ball lying upon a plane surface be struck by a mallet so as to produce translation with forward rota- tion on its horizontal transverse axis, and at the same time a ro- tation about a vertical axis, the ball will neither rotate upon the 238 Wisconsin Academy of Sciences, Arts, and Letters. one nor the other, but upon a new axis intermediate between the vertical and horizontal axes, pointed out by the resultant of the parallelogram of angular forces. This is the principle illustrated by the Gyroscope. The ball will describe a curve upon the plane in the same way that a truck rolled upon the ground when the axes cease to be level, begins to curveits path; of course the two cases are quite different, because the curve made by a ball is much less marked than that made by a truck or wheel. | There is something of a similar nature seen when a ball is pro- jected from a gun or cast from the hand. Since the middle of the sixteenth century, it has been known that the path of a pro- jectile is a parabola, if no account is taken of the resistance of the air. Templehoff was the first to take into consideration this ele- ment in calculating for projectiles. ‘The resistance of the air in- creases with the square of the velocity until the velocity exceeds 1,300 feet per second, when the resistance is much greater. In experimenting with smooth-bored guns, it was found that rotation had much to do with the motion of the projectile from the muzzle. The only rotation which aided in aiming the gun, and in making calculations reliable, was the axial rotation, which was attained by grooving the interior of the barrel. . In the practice of gunnery with a smooth-bored gun there was allowed enough space around the ball for free and easy motion. It was called windage. This windage allowed the ball to ballot slightly from side to side as it passed through the barrel. At each point of balloting the ball received a rotary motion by being retarded on that side next the tangent barrel. The last touch imparted the final rotation, or that which continued through the space traversed by the ball. If the last ballot was upon the right side of the barrel the ball received a right hand rotation. Italso received an impulse toward the left of the mark aimed at by the touch on the right side. But while the left side of the ball is moving forward at a much greater velocity than the center on ac- count of the right hand rotation, the right side is moving much slower than the center on account of the same rotation. The left side, therefore, encounters a greater resistance than the right side. The air in front and to the left is compressed, and accumulated Rotation as a Factor of Motion. 239 resistance finally throws the ball to the right. If the ball had balloted on the left side last, in leaving the muzzle, it would have been deflected to the right by touch and afterwards to the left by resistance and reaction of the compressed air. Thus it is possible with a smooth-bored gun to “shoot round” a nearer object in direct line and hit a more remote object behind it. I wish to give but one more instance of the effect of rotation on direct motion. It is vulgarly called ‘curved ball.” It may be witnessed in any good base-ball match. The pitcher desires to elude the strokes of the batter; after delivering a few balls in simple parabolic curves or with axial rotations, he will deliver the ball from the hand in such a way that when the ball leaves the hand the fingers touch it from below, causing the underside to be retarded while the upperside moves forward. Then the ball ro- tates upon a horizontal transverse axis, relative to its motion of translation. The greatest resistance from compressed air is in front and above the moving ball. The ball seeks a path of less resistance, preserving its plane of rotation and drops enough to form a depressed curve. By a skillful adjustment of rotation and translation, the pitcher is able to produce about such 9 curve as he wishes. ‘To the batter the ball seems coming toward a point it is destined to fall short of. Again, by delivering the ball from the hand with the fingers touching above, a backward rotation is produced on the top of the ball and a forward motion to the under side. Such a ball continues its course until accumulated resist- ance of air from ahead and below throws it upward. So the batter sees the ball coming toward a point it is destined to pass clearly above. By skillful manipulation the right side of the de- liverer the ball may be retarded, and the ball will curve to the right, and by retarding the left side it will curve to the left. The amount of curvature is variously estimated by different persons. With the rotation or twist of the best pitcher, it is no uncommon thing to make a ball curve a yard from its direct path, while many cannot effect any curve. This purports to be only the outline of a subject worthy of much greater investigation, in its relation to great scientific prob- lems. 240 Wisconsin Academy of Sciences, Arts, and Letters. Mr. President, members of the academy and others, my subject does not admit of a brilliant introduction nor of a grand perora- tion. It is the simple statement of the effect of rotation as an element of curvelinear and rectilinear motion. recent Progress in Theoretical Physics. 241 REPORT ON RECENT PROGRESS IN THEORETICAL PHYSICS. By J. EK. DAVIES, A. M., M. D., Professor of Physics in the University of Wisconsin. PART Die THE MAGNETIC ROTATORY POLARIZATION OF LIGHT. It is a well known fact that a ray of plane polarized light, vibrating in any azimuth, will, on passing through a lamina of quartz, have the azimuth of that vibration changed by an amount depending upon the thickness of the lamina, and the wave length of the particular kind of light employed. The direction, right or left, of this rotation of the plane of vibration depends upon the ——— Nore To PREvIouS PAPER On “ VoRTEX Morton.” For the production of large-sized vortex rings, the device shown in Fig. 1 is used by Prof. Tait. It isan ordinary wooden box, with a large circular hole cut out of one end, and the other covered tightly with elastic cloth. It can be filled with smoke from a @ ,. couple of retorts, @ @ one containing @) Ammonia and the other Hydrochlor- ic Acid. This will give copious clouds of chloride of Ammonium, which are driven outjin vortex rings, on striking the elastic cloth. It has been objected that the rings thus produced do not behave as Helmholtz’ mathematical results imply. It is not to be expected that they should; for Helmholtz’ investiga- tion upon vortex motion expressly assumes that the medium in which the rings are formed is a fréctdonless fluid, which air is not. The rings are truly air rings, the accompanying smoke merely serving to make them visible. This is finely shown by sending air rings from a second box against the smoke rings already formed. The invisible air rings are made manifest by the jostling of the smoke rings as they are struck by them. The suddenness of this movement is often very striking. 16 as. I DU OA Tl \ \ eww Fig. 242 Wisconsin Academy of Sciences, Arts, and Letters. quartz employed, some being right-handed and some left-handed. Certain substances such as quinine, turpentine, tartaric acid, cane —— Fig. 2, shows the direction of the motion at each point around and close to the core, or circular axis of a vortex ring. Fig. 3, shows the relation between the di- rection of motion of the entire ring and the direction of rotation around the core. It is seen to be in a direction “ per- pendicular to the plane of the ring, towards the side towards Fig. 2. which the ro- Fig. 3. tatory motion carries the znner parts of the ring.” The direction of the motion of the fluid in which the vortex ring exists, at different distances from the axis of the ring, both within the ring and without it, corresponds to the dzrec- tion of the lines of magnetic force around a circular con ductor in which an electrical current is maintained, (like the ring of a tangent galvan- ometer, for example,) and the velocities of the fluid in va- rious parts, will be in propor- tion to the ¢ntensitées of the I magnetic forces around this Ce | circular conductor, in va- rious parts of the magnetic Vie = field, which is due to the elec. M, ie tric current passing through \\| 7 || Sh the conductor, WG : SO? Wy Ly / as The directions of these WSS LIK | , SS YOSSEES Z ‘ lines of magnetic force, sur. ieee? SX. LX rounding a circular conduct. iS Seee Oe \ \ or are shown in Fig. 4, taken HH [acs \ \ " from Prof. Clerk Maxwell's cal \ \ admirable treatise upon Elec- Fig. 4. tricity and Magnetism. The small circle represents a section of the circular conductor conveying the electric current, while the oval lines represent the lines of magnetic force surrounding it. Were the conductor merely a Straight wire, the lines of magnetic force would be circles surrounding it. recent Progress in Theoretical Physics. 243 and other sugars, are also known to possess this property to a greater or less degree. Here the conductor is supposed to be bent in a ring placed vertically, and the plane of the paper, a section through it. The section and lines of one side only are shown. These lines would therefore represent the directions of the lines of flow in the fluid surrounding a vortex ring of which the small circle is a section of the core. The intensity of the magnetic force at any point of one of these lines would also be proportional to the velocity of the fluid at a corres- ponding point around the vortex. = Perhaps Figs. 5 and 6 will help to a better under standing of the relations contemplated. DirectionofE lectrie Carrent Direction of "xyz Maguctic Force, F%g. 5. Fig. 6 The behaviour of two vortex rings gyrating in the same or in opposite di- rections, in a frictionless fluid, are shown for rings gyrating in the same direction by Nos. 1, 2, 3 and 4 of Fig. 7; AWD Hod B Fig. 7. and for rings gyrating in opposite directions by Nos. 1, 2 and 3 of Fig. 8. A N03 p ! | LLt/f 244 Wisconsin Academy of Sciences, Arts, and Letters. Faraday, in 1845, showed that this rotation of the azimuth of vibration could also be produced in substances not otherwise pos- sessing it, by subjecting them to strong electro-magnetic influence, something after the manner shown in Fig. 9, where N is the polar- Fig. 9. izer which reduces the vibrations to a definite azimuth; G is the substance subjected to electro-magnetic strain; a and 0 are the “ Where the rings have equal radii and equal and opposite angular velocities, they will approach each other and widen one another; so that finally when they are very near each other, their velocity of approach becomes continually small- er and smaller, and their rates of widening faster and faster.. If they are per- fectly symmetrical, the velocity of fluid elements midway between them, parallel to the axis, is zero, and here we might imagine a rigid plane to be in- serted, which would not disturb the motion, and so obtain the case of a vortex ring which encounters a fixed obstacle. If the rings have the same direc- tion of rotation, they travel in the same direction; the foremost widens and travels more slowly, the pursuer shrinks and travels faster, till finally, if their velocities are not too different, it overtakes the first and penetrates it. So the rings pass through each other alternately.” In Fig. 7, No. 1 represents the rings rotating in the same direction at start ing; No. 2 shows the forward ring, A, slackening itsspeed and dilating; No. 3, the B ring contracting, accelerating its speed and passing through. Ring £ then slackens its speed, and dilates in turn, while A contracts. In Fig. 8, the gradual approach of the rings gyrating oppositely is not well shown. The long arrows are intended to show the direction in which the rings would move, in virtue of their respective rotations, were they not influenced by each other. The motions of the fluids at,various points surrounding a vortex filament in the shape of aring, are best traced by means of Elliptic Integrals of the Recent Progress in Theoretical Physics. 245 two poles of the electro-magnet, bored through for the reception of the substance and the passage of the light, and N, is the anal- yzer by which the position of the azimuth of the light reaching it is determined. When G is a determinate length of ‘heavy class” (a silico-borate of lead), the analyzer requires a rotation of 6° on producing the electro-magnetism, in order to be placed in the same relation to the azimuth of vibration of the light reaching it, as it was in, before the circuit was closed. That is, if the posi- tion of the analyzer is such before the electro-magnetic circuit is closed, that the field is dark, on closing the circuit, and thus plac- ing the glass in a strong field of magnetic force, the azimuth of the polarized light is so changed that a perceptible amount gets through, and the analyzer must be rotated 6° in order to again cut it off and render the field dark as before. This angle through which the light is turned, is, however, in addition to the length of the stratum of the medium through which it is compelled to pass, directly proportional to the strength of the current producing the magnetism (or rather to that resolved part of the magnetic force produced by the current, which is in the direction of the ray). The amount of the rotation also depends upon the refractive energy of the medium subjected to the magnetic strain. The rela- tion is sometimes stated thus: “ The angular rotation of the plane of polarization is numerically equal to the amount by which the magnetic potential increases from the point at which the ray enters the medium to that at which it leaves it, multiplied by a coéffi- cient, which, for diamagnetic media (like glass), is generally posi- tive.” — Maxwell. 3 first and second kind. An elementary discussion of the principal features of vortex motion, involving only the simplest Quarternion notions, is given in Prof. Clifford’s recently published ‘ Elements of Dynamics — Part I,” page 191, et seg. Sir Wm. Thompson has also published an extensive paper in the Trans. of the Royal Soc., Edin. Vol. 8 for 1869, in which many new theories are established and many illustrations of vortex motions in fluids are given, by means of real or or ideal electro-magnets variously arranged. A sum- mary of several of these theories and analogies will be found in Thompson’s “Reprint of Papers on Electro-statics, and Magnetism.’’— London, 1872. An earlier ‘paper, suggesting the idea of vortex atoms, was published in Vol. 34, p. 15, of the Phil. Mag., 1867. London, Dublin and Edinburgh. 246 Wisconsin Academy of Sciences, Arts, and Lelters. Under the same circumstances, where “heavy glass” would produce a rotation of 6°, Bisulphide of Carbon would produce a rotation of 8°; flint glass, 2° 8’; rock salt, 2° 2’; water, 1°. The behavior of a large number of substances under the simul- taneous influence of magnetism and circularly polarized light of different colors was examined by Verdet in 1863. He found the results of his experiment to agree very well with the formula: G = mer ci ( 1—A =) Moe) eee (1.) 7? where @ is the angular rotation of the plane of polarization; ma constant (the coéfficient of magnetic rotation of the medium); 7 the intensity of the magnetic force resolved in the direction of the ray; cthe length of the ray within the medium ; / the wave length in air, of the particular kind of light employed; 7 its index of refraction in the medium. / For Creosote there was considerable deviation from the formula. On account of the mixed nature of Creosote, being an aggregate of Carbolic Acid and several other substances, this might have been expected, even if the above were the true formula representing the relation between the rotation, magnetic force, wave length, and refractive index. Verdet has summed up his results as follows: Ist. ““The magnetic rotations of the planes of polarization for light of different colors are approximately as the inverse square of the wave length of the light employed. 2nd. “The exact law is that the product of the rotation of the square of the wave length, increases from the least refrangible to the most refrangible end of the spectrum.” ord. “The substances for which this increase is most sensible are also those which have the greatest dispersive power.” The formula (1) may be derived from the following more gen- eral formula 1 d 4x eae: i \=—— f) SS cal coast ES CIES ae ( paves a ) —— Iz ©: ere (OF cy & ie c / BM = l—2rCy 2 (2.) vor which Prof. Clerk Maxwell has shown to be a consequence of Sir Wm. Thompson’s assumption that the only dynamical explana- Recent Progress in Theoretical Physics. 247 tion possible for the magnetic rotation of the plane of polarized light is that, in magnetization there must be molecular electrical currents, and that the components of these currentscan bedynam- ically compounded with the angular velocity acquired by an ele- ment of the medium, during the passage through itof a ray of circularly-polarized light. :2 4 C ? and neglecting 220; —— : vo On making in formula (2), m = because it is very small, being essentially the amount of the rota- tion of the plane of polarization after passing through a thickness of the medium only equal to half a wave length of the light em- ployed, we have formula (1). Before showing the manner in which formula (2) is eaonaed by Maxwell, from Thompson's explanation of the magnetic rotation of the plane of polarized hght, it may be best to recall one or two elementary propositions relating to polarized light, and also to circular motion. In the first place, experiment shows that two rays of light circularly polarized in opposite directions, and of the same intensity, become, when united, a plane polarized ray, the plane of polarization of which will depend upon whether the periods of the component circular vibrations are the same or not. If, from any cause, the phase of one of the circularly-polar- ized rays is accelerated, then the plane of polarization of the re- sultant ray, is turned round through an angle equal to half the angle of acceleration of the phase. So also in certain cases, such as reflection from metallic sur- faces, or total reflection in glass at certain angles, as in Fresnel’s rhombs, or in the passage of light through thin laminz of double refracting crystals, as in quarter-wave laminz of mica, two plane vibrations may give rise to one circular one, right handed or left- handed, according as one or the other plane component is ad- vanced in phase by a quarter of a complete oscillation. This is only what might be expected from the well-known theorem in pure motion, that ‘two uniform circular vibrations of the same amplitude, having the same periodic time and in the same plane, but revolving in opposite directions, are equivalent, 248 Wisconsin Academy of Sciences, Arts, and Letters. when compounded together, to a rectilinear vibration. The peri- odic time of this plane vibration is equal to that of the circular vibrations, its amplitude is double, and its direction is in the line joining the points at which two particles describing the circular vibrations, in opposite directions round the same circle, would meet.” The theorem may be illustrated as follows: Tf, in any space like that represented in Fig. 10, we have a great Fig. 10. number of spins, more or less completely filling the space en- closed by the larger circle, and about axes perpendicular to the plane of the paper, the resultant will be equivalent to a spin of ' definite magnitude about some single axis likewise perpendic- ular,to the to the plane of the paper; the magnitude of this resultant spin being determined by the intensity, relative dis- tances, and number, of the component spins which go to make it up. Regarding this resultant spin only, the velocity of a particle at any distance from the axis can be decomposed into component F%g. 11. velocities, asin Fig, 11, where the uniform circular motion Y of I’, from X to Y, can be de- composed into =r. cos dand 7=r. sin #,in such a man- ner that the motion of D, to and fro on the line X, and the motion of E to and fro on on the line Y, correspond constantly in position to the motion of F around the cir- cle. In such a case, we say that the circular harmonic motion of F is compounded of two rectilinear harmonic motions along X and Y, of equal periods and amplitude, but differing by Recent Progress in Theoretical Physics. 249 a quarter of a complete oscillation. If there be two equal and op- posite tendencies operating upon F, one to carry it toward Y, and the other toward X, the result will be, that the tangential tendencies at I’ will neutralize each other, while the normal com- ponents will coincide and carry the particle towards C along r (Fig. 11), and a rectilinear motion Fig. 13. will be the result, as in Fig. 12 or Fig. 13. Thus two tend- encies to gyrate in opposite directions may result in mere rectilinear vibrations. Ifone Hig. 12. of these tenden- cies be stronger than the other, so that of it- self it would produce a more rapid rotation in zs direction, than the other component in its, then the motion will be elliptical in an orbit of which the major axis changes at each complete oscillation Hig. 15. by some angle @, the magnitude of which will depend upon the excess of velocity in one direc- tion over that in the opposite. This is easily seen by reference to Figs. 14 or 15, where the motion would be along ad, / were both cir- | Fig. 142 a cular compo- \ me nents equal, | we) Ved Loy whereas the b 'The engraver has very imperfectly copied the original drawings for this & § as for some of the other figures. *For c in the figure, read f, and for a and 6 at the extremities of one of the diameters, read a’ and 0’, respectively. 250 Wisconsin Academy of Sciences, Arts, and Letters. excess of that towards a’ carries towards a’ during the first part of the virtual motion along ab, and towards 0’ during the part from 8 to b; that is, on account of the shorter time required to complete an oscillation in the direction from a’ to U’, around the circle, than in the opposite direction, there is an acceleration of phase in that direction. Hence, aslong as the tendency to increased rapidity of one component over that of the other continues, so long will there be a change in the position of the line ab. The application of these principles to the rotation of the plane of polarization as it occurs in quartz, will be clearly shown by the following extract and diagram, taken from Prest. Barnard’s excel- lent “Lectures on the Undulatory Theory of Light,” Smithsonian Annual Report for 1862. After a general discussion of circular and elliptical polenta ta by reflection, Prest. Barnard says: ‘“‘ We are now perhaps prepared to understand the reason of the rotation of the plane of polarization of a ray transmitted along the axis of a crystal of quartz. We have seen that Fresnel, by an in- genious combination of prisms, succeeded in demonstrating the existence within the crystal of two circularly polarized rays, gyrat- rig. 16. ing in opposite directions. And we have seen that the resultant effect of two oppo- site gyrations, is to produce a movement in a plane. The gyratory movements within the crystal are then not actual but virtual —in other words, there are forces constantly tending to produce these gyra- tions, which hold each other im equilibrio, or at least nearly so. We must consider these forces as successively traversing all azimuths within the length of each un- dulation. If the wave were of the same length in both gyrations, the forces being presumed equal, the molecular move- ment would be constantly rectilinear, and the plane of polarization would not change. But, as the plane does in fact change, we are led to infer Recent Progress in Theoretical Physics. Z2o1 that the undulation lengths for the two rays are not equal. The annexed figure may serve to illustrate the mutual action of these rays. Suppose M A D B, to be the orbit in which a force P tends to urge a molecule M, to revolve around the center C, to which it is drawn by the force MC. Suppose the equal force Q to urge the same molecule to describe the same orbit in the opposite direction. These forces holding each other 7n equilibrio, the mole- cule will follow the direction of the third force, M C. Now suppose the force Q suspended, the molecule will take the direction of the circle A D B, and will continue to revolve in it so long as the force P (supposed always tangential) continues to act. But its movemehts will impart to the molecule next below it a similar motion, and that to the next, and so on; so that, as these successive molecules take up their movements later and later, there will be a series in different degrees of advancement in their several circles, forming a spiral; and when the molecule M shall have returned to its original position, the series will occupy a position like the curve MF L N’OR. If, now, P besupposed to be in turn suspended, while the force Q continues to act, the effect of Q will be to produce a contrary spiral, which may be represented by MS KTV. If{MD bea diameter of the circle M A DB, drawn from M, and DH N’ bea line parallel to the axis OC G of the cylindrical surface, which is the locus of the spirals, then, if the undulating lengths are the same for both movements, the two spirals will intersect D H in the same point, the intersection marking the completions of a half undulation for each. But if these lengths be unequal, the intersection with D H will take place at different points as N and N’. Let now a plane intersect the cylinder at any distance below M A DB, as at H, parallel to M A DB. It is conceivable that this plane may be made to pass through the point where the spirals intersect each other. Jf I mark the point of intersection, and we draw the tangents I P’ and I Q’ in the plane of the circle E HI, then there will be a molecule at the point I which wiil be in the circumstances of the molecule in [Fig. 12 at the point a] — that is to say, solicited by three forces, of which two, I P’ and I Q’ are equal and opposite, and the third is directed in the ine 1G 252 Wisconsin Acadetay of Sciences, Arts, and Letters. towards the center. The molecule will, therefore move in this line, and not in a circle; and if the plane of the circle H H I H’ be the bounding surface of the crystal, or the surface of emer- gence of the light, 1 G will mark the azimuth of the molecular movements of the emergent ray. But if the planes of EH H I H do not pass through the point of intersection of the spirals it must cut each spiral in a different point. The figure is drawn to represent this more general case, the points of intersection with the spirals being severally L and K. By joining L K and drawing the radius G I perpendicular to it, G I will bisect the angle G L K and M’, at the intersection of G JT and L K will be the position of the molecule in the plane H H LIK, which, if the tangential force P only were acting, would be at L, and if the tangential force Q only were acting, would be at K. The tangential forces acting at the moment on this molecule will not be represented by I P’ and I Q’, but will be tangents at K and L. Now, as D H, the distance between the planes AD B and EH H J, is a larger part of the length of an entire turn of the spiral MS N K than of the spiral M F L N’, the line G I will fall on the right of G H, the position it would occupy if the two undulations were equal in length. We may therefore say, as before, that if the plane EK H I were the surface of emergence of a ray from a erystal, in which it had been subject to the action of the forces supposed, its plane of polarization, G I, would be turned towards the right from its original azimuth. The plane of polarization turns, therefore, in the direction of the winding of the closest spi- ral, or of the ray of shortest undulation; but it turns in the direc tion of the gyration of the ray of longest undulation. This rotation of the plane, thus demonstrates that the two rays advance with unequal velocities in the axis of quartz —a remark- able fact which is not true of any crystal which produces plane polarization only. It also enables us to determine the relative velocities, or to ascertain the index of rotatory polarization. For since G I bisects the angle between the points K and L, which mark the relative degrees of advancement of the two rays in their respective rotations, if we take a thickness 6, which produces a Recent Progress in Theoretical Physics. 253 rotation of 90°, we know that the difference of phase is then one- halfan undulation. If A£ denote the length of the longer undula- tion, and 1, that of the shorter, then —— uns G=mi= (m+ $)X; or as = ae 2a A m 2m 6 As — = m,and 4 may be determined by experiments in refrac- ‘ tion, the value of m is known when @ is measured. By pursuing this method, Mr. Babinet found the value of 7 = 1.00008; a ‘S value which, small as it is, is the largest known for [non-magnetic] rotatory polarization.” The first mathematical explanation of rotatory polarization as it occurs in quartz, appears to have been given by MacCullagh, in 1836 (Trans. R. Irish Acad., XVII). He succeeded perfectly in explaining the phenomena as they occur in uniaxial crystals, by introducing into the ordinary equations of vibratory motion in o- fluids, terms of the form c es So that the equations become: z ae are a*y , muita Seer Rope DE ree ay may dn A OFS Gio dz dz Cauchy also appears to have furnished similar equations to M. Jamin, at the request of the latter, who compared them carefully with experiments, and found a perfect agreement so far as uniaxial crystals are concerned (Verdet—Lecons D’Optique Physique, Vol. IT, p. 323). For biaxial erystals Verdet says: ‘Za methode de MacCullagh est tres-remarquable : c'est un bel exemple de ce qu’ on peut faire quand on est réduit a de simples conjectures.” The matter has since been treated by M. Briot in an “ Mssud sur la theorie mathematique dela lumiere.” He supposes a forced distribution of the ether in rotatory crystals, so that the lines of ethereal molecules are arranged in elliptic helices. This supposi- tion introduces into the differential equations of vibratory move ment, differential coefficients of odd orders, the presence of which indicates the rotatory power. Airy has suggested similar equations for the rotation produced } 254. Wisconsin Academy of Sciences, Arts, and Letters. by magnetism, “not as giving a mechanical explanation of the phe- nomena, but as showing that the phenomena may be explained by equations, which equations appear to be such as might possi- bly be deduced frem some plausible mechanical assumption, although no such assumption has been made.” This explanation of what rotatory polarization is, as it occurs in bodies which of themselves rotate the plane of polarization, may Fig. 16. help to an understanding of Fig. it. the manner in which an | electric current, circulating the around a medium through which circularly polarized light is passing, may possi- bly affect the velocity of either circular component of the polarized light, and thus, accord- ing as the direction of the current is with a circular component, as in Fig. 16, or against it, as in Fig. 17, produce a right-handed or a left-handed rotation, according to the direction in which the current circulates around the medium. Of this latter, Sir Wm. Thompson, in 1856, made the important observation,’ which Prof. Clerk Maxwell has elaborated into the “The magnetic influence on light, discovered by Faraday, depends on the direction of motion of moving particles. For instance, in a medium possess- ing it, particles in a straight line parallel to the lines of magnetic force, dis- placed to a helix round this line ag axis, and then projected tangentially with such velocities as to describe circles, will have different velocities, according as their motions are round in one direction (the same as the nominal direc- tion of the galvanic current in the magnetizing coil) or in the contrary direc- tion. But the elastic reaction of the medium must be the same for the same displacements, whatever be the velocities and directions of the particles; that is to say, the forces which are balanced by centrifugal force of the cireular motions are equal, while the luminiferous motions are unequal. The absolute circular motions being therefore either equal or such as to transmit equal cen. trifugal forces to the particles initially considered, it follows that the lumi- niferous motions are only components of the whole motion; and that a less luminiferous component in one direction, compounded with a motion ex- isting in the medium when transmitting no light, gives an equal resultant to that of a greater luminiferous motion in the contrary direction compounded With the same non-luminous motion. I think it is not only impossible to conceive any other than this dynamical explanation of the fact that circularly- \ Recent Progress in Theoretical Physics. _ 250 fundamental equation with which we began this article, and which the experiments of Verdet so remarkably corroborate. “he disturbance which constitutes ght, whatever its physical nature may be, is of the nature of a vector, perpendicular to the direction of the ray. This is proved from the fact of the interfer- ence of two rays of light, which, under certain conditions, pro- duces darkness, combined with the fact of the non-interference of two rays polarized in planes perpendicular to to each other. For, since the interference depends on the angular position of the planes of polarization, the disturbance must be a directed quantity or vector, and since the interference ceases when the planes of polar- ization are at right angles, the vector representing the disturbance must be perpendicular to the line of intersection of these planes, that is, to the direction of the ray. The disturbance, being a vector, can be resolved into compo- nents parallel to x and y, the axis of z being parallel to the direc- tion of theray. Let and 7 be these components; then, in the case of a ray of homogeneous circularly-polarized light, € =7rcos G, f= ew (1) where @=nt —qz +a. (2) In these expressions, 7 denotes the magnitude of the vector, and @ the angle which it makes with the direction of the axis of x. The periodic time, t, of the disturbance is such that (Ne = 2s: (3) The wave-length, A, of the disturbance is such that Mh eg. (4) The velocity of propagation is ~ The phase of the disturbance when ¢ and z are both zero is a. The circularly-polarized light is right-handed or left-handed according as q is negative or positive. polarized light transmitted through magnetized glass, parallel to the lines of magnetizing force, with the same quality, right-handed always or left- handed always, is propagated at different rates, according as its course is in the direction or is contrary to the direction in which a north magnetic pole is drawn; but I believe it can be demonstrated that no other explanation of that fact is possible. Hence it appears that Faraday’s optical discovery affords a demonstration of the reality of Ampere’s explanation of the ulti- mate nature of magnetism.” — Srr Wa. THOMPSON. 256 Wisconsin Academy of Sciences, Arts, and Letters. Its vibrations are in the positive or the negative direction of rota- tion in the plane of (a, y), according as n is positive or negative. The light is propagated in the positive or the negative direction of the axis of z, according as n and g are of the same or of oppo- site signs. In all media n varies when qg varies, and i is always of the . . n same sign with —. Hence, if for a given numerical value of n, the value of — is greater when 7 is positive than when 7 is negative, it rollers that for a given value of g, given both in magnitude and sign, the positive value of m will be greater than the negative value. Now this is what is observed in a diamagnetic medium, acted on by a magnetic force, 7, in the direction of z. Of the two cir- cularly-polarized rays of a given period, that is accelerated of which the direction of rotation in the plane of (a, y) is positive. Hence, of two circularly polarized rays, both left-handed, whose wave-length within the medium is the same, that has the shortest period whose direction of rotation in the plane of (a, y) is positive, that is, the ray which is propagated in the positive direction of z from south to north. We have, therefore, to account for the fact that when in the equations of the system g and r are given, two - values of 2 will satisfy the equations, one positive and the other negative, the positive value being numerically greater than the negative. We may obtain the equations of motion from a consideration of the potential and kinetic energies of the medium. The potential energy, V, of the system, depends on its configuration, that is, on the relative position of its parts. In so far as it depends on the disturbance due to circularly-polarized light, it must be a a func- tion of 7, the amplitude, and gq, the coefficient of torsion, only. It may be different for positive and negative values of qg of equal numerical value, and it probably is so in the case of media, which of themselves rotate the plane of polarization. The kinetic energy, Z, of the system, is a homogeneous function of the second degree of the velocities of thesystem, the coefficients of the different terms being functions of the coordinates. Recent Progress in Theoretical Physics. 257 Let us consider the dynamical condition that the ray may be of constant intensity, that is, that 7 may be constant. Lagrange’s equation for the force in r becomes Oh GHE CLT OV Gi INO nat Cp Since 7 is constant the first term vanishes. We have therefore the equation 0. (5) ie Pa 9) (6) dr dr in which g is supposed to be given, and we are to determine the value of the angular velocity 0, which we may denote by its actual value, n. The kinetic energy, 7, contains one term involving n*; other terms may contain products of n with other velocities, and the rest of the terms are independent of n. The potential energy, V, is entirely independent of n. ‘The equation is, therefore of the form Alig ae Jey se (GSU) (7) This being a quadratic equation, gives two values of x. It ap- pears from experiment that both values are real, that one is posi- tive and the other negative, and that the positive value is numeri- cally the greater. Hence, if A is positive, both Band C are neg- ative ; for, if n, and m, are the roots of the equation, A(n, + m) + B= 0. (8) The coefficient B, therefore, is not zero, at least when magnetic force acts on the medium. We have, therefore, to consider the expression Bn, which is the part of the kinetic energy involving the first power of n, the angular velocity of the disturbance. Every term of 7’ is of two dimensions as regards velocity. Hence the terms involving n must involve some other velocity. This velocity cannot be r or g, because, in the case we consider, y and g are constant. Hence it is a velocity which exists in the medium independently of that motion which constitutes light. It must also be a velocity related to n in such way that when it is multiplied by » the result is a scalar quantity, for only scalar quantities can occur as terms in the value of 7, which is itself 1” 258 Wisconsin Academy of Sciences, Arts, and Letters. scalar. Hence this velocity must be in the same direction as n, or in the opposite direction, that is, it must be an angular velocity about the axis of z. Again, this velocity cannot be independent of the magnetic force, for if it were related to a direction fixed in the medium, the phenomenon would be different if we turned the medium end for end, which is not the case. We are therefore led to the conclusion that this velocity is an invariable accompaniment of the magnetic force in those media which exhibit the magnetic rotation of the plane of polarization. We have been hitherto obliged to use language which is, per- haps, too suggestive of the ordinary hypothesis of motion in the undulatory theory. It is easy, however, to state our result ina form free from this hypothesis. Whatever light is, at each point of space there is something going on, whether displacement or rotation, or something not yet. imagined, which is certainly of the nature of a vector or directed quantity, the direction of which is normal to the direction of the ray. This is completely proved by the phenomenon of inter- ference. In the case of circuilarly-polarized light, the magnitude of this vector remains always the same, but its direction rotates round the direction of the ray so as to complete a revolution in the peri- odic time of the wave. The uncertainty which exists as to whether this vector is in the plane of polarization or perpendicular to it, does not extend to our knowledge of the direction in which it rotates in right handed and left: handed circularly-polarized light respee- tively. The direction and the angular velocity of this vector are perfectly known, though the physical nature of the vector and its absolute direction at a given instant are uncertain. When a ray of cireularly-polarized light falls on a medium un- der the action of magnetic force, its propagation within the me- dium is affected by the relation of the direction of rotation of the light to the direction of the magnetic force. From this we conclude that in the medium, when under the action of magnetic force, some rotatory motion is going on, the axis of rotation being in the direc- tion of the magnetic forces; and that the rate of propagation of cir- Recent Progress in Theoretical Physics. 259 cularly-polarized light, when the direction of its vibratory rotation and the direction of the magnetic rotation of the medium are the same, is different from the rate of propagation when these direc tions are opposite. The only resemblance which we can trace between a medium through which circularly-polarized light is propagated, and a me- dium through which lines of magnetic force pass, is that in both there is a motion of rotation about an axis. But here the resemblance stops, for the rotation in the optical phenomenon is that of the vector which represents the disturbance. This vector is always perpendicular to the direction of the ray, and rotates about ita known number of times in a second. In the magnetic phenome- non, that which rotates has no properties by which its sides can be distinguished, so that we cannot determine how many times it rotates in a second. There is nothing, therefore, in the magnetic phenomenon which corresponds to the wave-lensth and the wave-propagation in the optical phenomenon. A medium in which a constant magnetic force is acting, is not, in consequence of that force, filled with waves traveling in one direction, as when light is propagated through it. The only resemblance between the optical and the magnetic phenomenon is, that at each point of the medium something exists of the nature of an angular velocity about an axis in the direction of the magnetic force. ON THE HYPOTHESIS OF MOLECULAR VORTICES. The consideration of the action of magnetism upon polarized light leads, as we have seen, to the conclusion that in a medium under the action of magnetic force something belonging to the same mathematical class as an angular velocity, whose axis is in the direction of the magnetic force, forms a part of the phenomenon. This angular velocity cannot be that of any portion of the me- dium of sensible dimensions rotating as a whole. We must, therefore, conceive the rotation to be that of very small portions of the medium, each rotating on its own axis. This is the hypoth- esis of molecular vortices. CS A i 260 Wisconsin Academy of Sciences, Arts, and Letters. The motion of these vortices, though, as we have shown, it does not sensibly affect the visible motions of large bodies, may be such as to affect that vibratory motion on which the propagation of light, according to the undulatory theory, depends. The dis- placements of the medium, during the propagation of leht, will produce a disturbance of the vortices, and the vortices, when so disturbed, may re-act on the medium so as to affect the mode of propagation of the ray. It is impossible, in our present state of ignorance as to the na- ture of the vortices, to assign the form of the law which connects the displacement of the medium with the variation of the vortices. We shall therefore assume that the variation of the vortices, caused by the displacement of the medium, is subject to the same conditions which Helmholtz, in his great memoir on Vortex-mo- tion, has shown to regulate the variation of the vortices of a per- fect liquid. Helmholtz’s law may be stated as , follows: — Let P and @ be two neigh- i boring particles in the axis of a vortex, EG then, if in consequence of the motion of the fluid these particles arrive at the points P’ Y, the line P’ Y will rep- resent the new direction of the axis of the vortex, and its streneth will be altered in the ratio of P’ Y to P Q. Hence if a, 8, 7 denote the components of the strength of the vortex, and if €, 7, € denote the displacements of the medium, the value of a will become a=a4 pes | ie 7 a& da: dy dz dy d: di (me ( aynaeedl es eel ed ene aie da dy USE (1) , dt ag de =rtaS 4 pte 4,7 aes! ” des ; dy de We now assume that the same condition is satisfied during the small displacements of a medium in which a, f, 7 represent, not Recent Progress of Theoretical Physics. 261 the components of the strength of an ordinary vortex, but the components of magnetic force. The components of the angular velocity of an element of the medium are (2) dt \ dz dc mn d i sui dé } ae \ ag dy The next step in our hypothesis is the assumption that the kinetic energy of the medium contains a term of the form: 2 C(aw, + Bo, + 703). (38) This is equivalent to supposing that the angular velocity ac- quired by the element of the medium during the propagation of light is a quantity which may enter into combination with that motion by which magnetic phenomena are explained. In order to form the equations of motion of the medium, we must express its kinetic energy in terms of the velocity of its parts, the components of which are = - = We therefore integrate by parts, and find 2 0 J. We - (Gah Ae Clas ck any) Oe Gh ee =0f f(r; ABS) dy e+ Off (a8 —7E) dea ae of] (8 oa ae dy + CLL, : — =) dy a dy — fi) in de ( me da th ay ob (4) dt \ dz da aD Neier SCO) ' The double integrals refer to the bounding surface, which may be supposed at an infinite distance. We may, therefore, while investigating what takes p'ace in the interior of the medium, con- fine our attention to the triple integral. 262 Wisconsin Academy of Sciences, Arts, und Letters. The part of the kinetic energy in unit of volume, expressed by this triple integral, may be written 4x0 (& eae 6) dt where u, v, w are the components of the Be current. It appears from this that our hypothesis is equivalent to the as- sumption that the velocity of the particle of the ‘medium whose dé oy dé di? dt’ dt’ combination with the electric current whose components are w, © components are , is a quantity which may enter into v, W. Returning to the expression under the sign of triple integration in (4), substituting for the value of a, 8,7, those of a’, f, 7’, as given by equation (1), and writing d d d d see SHORE (= a en 6 a eR ce (6) the expression under the sign of integration becomes Ges (a a) + dt - =) (dt dh\dy — dz didh\dz dz dt dh \dx In the case of waves in planes normal to the axis of z the dis- placements are functions of 2 and ¢ only so that & = _ and Z this expression is reduced to US dn in Oy as C | Py Oe) "leu ea 8) The kinetic energy per unit of volume, so far as it depends on the velocities of displacement, may now be written at dé Ge dnl Gane T= = +t A C i eae fo hee e TAO Cr | a eae ae where p is the density of the medium. The components, X and Y, of the impressed force, referred to unit of volume, may be deduced from this by Lagrange’s equations aE a? xe Ley ae p dt r dz2-dt u a? ae V = 92 Oe lim au FREE a) Recent Progress in Theoretical Physics. 263 These forces arise from the action of the remainder of the medium on the element under consideration, and must in the case of an isotropic medium be of the form indicated by Cauchy, X A, So + AS 1 Bie (12) Viz ye coe cic (13) If we now take the case of a circularly-polarized ray for which E = reos (nt — qz), 7 =r sin (nt—qz), (14) we find for the kinetic energy in unit of volume hi 5) Onn CO rieg 7. (15) and for the potential energy in unit of volume VS PAW = 4uG 2 aie) =a (16) where @ is a function of q’. The condition of free propagation of the ray given in equation (6), is ian Ve xesins gy —— eI lf dr dr ae which gives on? — 2Cr7n = Q, (18) whence the value of n may be found in terms of ¢. But in the case of a ray of given wave-period, acted on by mag- ene de netic force, what we want to determine is the value of oe when n is constant, in terms of — when; is constant. Differentiating (18) {20n — 2Cyrq") dn — ee + 4Crqn op Gornene == 0), «(AIG q d Cyn d e thus fin e is Chae Gl (20) If 2 is the wave-length in air, and 7 the corresponding index of refraction in the medium Gh = Diet nA = Div: The change in the value of g, due to magnetic action is in every case an exceedingly small fraction of its own value, so that we may write dq Y= + ay” 264 Wisconsin Academy of Sciences, Arts, and Letters. where g, is the value of g when the magetic force is zero. The angle, 0, through which the plane of polarization is turned in pass- ing through a thickness, c, of the medium, is half the sum of the positive and negative values of q c, the sign of the result being changed, because the sign of ¢ is negative in equations (14). We thus obtain 1 2 Tame gee ole) ART 1 — any which is the complete form of the equation for determining the angle, through which the plane of polarization has been turned by the magnetic force while passing through a thickness of the medium equal to ¢, and is, in its modified form the one with which Verdet’s results have been compared. From this comparison of the consequences of assuming the motions of light to be capable of composition with the motions caused by electric currents, with what experiment shows to be true of bodies conveying circularly polarized light when also placed under magnetic strain, we have probably good evidence for the opinion that some phenomenon of rotation is going on in the magnetic field, that this rotation is per- formed by a great number of very small portions of matter each rotating on its own axis, this axis being parallel to the direction of the magnetic force, and that the rotations of these different. vortices are made to depend on one another by means of some kind of mechanism connecting them. The problem of determining the mechanism required to establish a given species of connection between the motions of the parts of a system always admits of an infinite number of solutions. Of these some may be more clumsy than others, but all must satisfy the conditions of mechan- ism in general.” — MAxweLL — Electricity and Magnetism, Chap. >O-dh clip EO i) Norr.— On page 246 the radical sign (¥v) should be the Greek letter gamma Ga in formula No. (2). PROCEEDINGS OF THE ACADEMY SINCE FEBRUARY, 1876. REPORI OF THE PRESIDENT. To His Excellency, WILLIAM KH. SMITH, Governor of the State of Wisconsin: Sir :—It affords me great pleasure to be able to report that the Wisconsin Academy of Sciences, Arts, and Letters is in a flourish- ing condition, steadily gaining in membership and usefulness. | Every college and educational institution of high grade in the state is now represented in the Academy; thus bringing together many of the ablest men in science, literature and art. The sum- mer meetings held ia Racine and Milwaukee were well attended and were instrumental in exciting a lively interest in the society and its aims. We are satisfied that in inaugurating this summer migratory meeting, the society acted wisely, and that these ses- sions will be productive of good. At the Milwaukee meeting, a number of ladies were elected members, several of whom are not unknown to science and litera- ture. In electing these ladies, tae Academy has gained valuable working members and hasadded nota little to its well-being, intel- . lectually as well as socially. The society acted on the broad prin- ciple that science and letters, have neither country, color or sex: The straight-jacket of superstition and bigotry no longer cramps and cripples investigation in any department of kaowledge. The report of the librarian shows the extent and value of our exchanges from this and foreign countries. We have already formed the nucleus of a valuable library. The finances are in a healthy condition, the funds are not large, but sufficient for the workings of the society, aside from the publish- ing of the proceedings, which is justly done by the state. 268 Wisconsin Academy of Sciences, Arts, and Letters. We are in need of suitable rooms to accommodate the society, We want space sufficient to display and securely keep a cabinet such as will certainly come into our possession as soon as we have permanent accommodations. ; The usefulness of the Academy will be greatly enhanced by the possession of suitable rooms for cabinet and library. Very respectfully, P. BR. HOY, Presedent. PROCEEDINGS OF THE ACADEMY. [Since February, 1876.] REPORT OF THE SECRETARY. Rooms oF WIsconsIN ACADEMY OF SCIENCE, ARTS AND LETTERS, CaPiToL, Maptson, WISCONSIN. SEVENTH ANNUAL MEETING. Held at Madison, Wisconsin. FIRST SESSION. February 13, 1877. Academy met at 7:30 P. M. Usual routine of business. Prof. Davies, General Secretary, called attention to the many valuable exchanges received from foreign and American societies, and the urgent necessity of providing proper rooms and cases for them. Prof. Allen, Prof. Chamberlin and Gen. Delaplaine were appointed a committee for such purpose. Remarks were made by Prof. Carpenter upon the death of Prof. J. H. Eaton, of Beloit, and a committee consisting of Dr. Chapin, Prof. Chamberlin, of Beloit and Dr. 8. H. Carpenter, of Madison, were appointed to draw up an account of the life and work of Prof. Eaton. A very interesting paper on a wmode of illustrating Phylotaxis, by means of a model, was read by E. A. Birge, Hsq., of the University of Wisconsin. Dr. P. R. Hoy, President of the Academy, read a paper upon an elephant’s tooth containing an iron bullet. He explained how the bullet sank into the pulp and appeared in another part of the tooth three feet off. Profs. Chamberlin and Allen, and Gen. Delaplaine were appointed a com- mittee to memorialize the Governor in regard to more ample room for the accommodation of the books and specimens of the Academy. SECOND SESSION. February 14, 1877. Academy met at 9:30 A. M., President Hoy in the chair. On account of the unavoidable absence of the secretary, Hon. E, E. Woodman, of Baraboo, was chosen Secretary pro tem. | 270 Wisconsin Academy of Sciences, Arts, and Leiters. On motion of Prof. Davies, the following gentlemen were chosen annual members: Dr. Clark Gapen, of Madison, Wis. Mr. W. A. P. Morris, of Madison, Wis. Dr. BE. W. Bartlett, of Milwaukee, Wis. W. F. Bundy, Esq., of Sauk City, read a paper on the “ Crustacea of Wis- consin.” Mr. James R. Stuart, of Madison, read a paper on “ Art Instruc- tion.”’ Prof. Davies showed the ‘‘ Application of Fourier’s Theorem to the Phe- nomena of Composite Sounds.” Adjournment, to meet at 2:30 P. M. THIRD SESSION. February 14, 2:30 P. M. Gen. Ed. E. Bryant read a paper on the “ Cost of Government.” Dr. Clark Gapen read one on “Hereditary Insanity,” which was discussed at great length by President Bascom, Prof. S. H. Carpenter and Dr. Gapen. Prof. Wright, of Fox Lake, read a paper on “ The Philosophy of History.” FOURTH SESSION. 300s Me Mr. E. A. Birge read a finely illustrated paper upon the the habits and structure of the ‘Cladocera, a minute crustacean of our fresh water lakes.’” Many points of its structure were shown to be exceedingly curious. Hon. E. E. Woodman, of Baraboo, read a valuable paper on “The Pipe- stone of Devil’s Juake.” Dr. E. Andrews being detained at Chicago by important surgical cases, his paper was read by Prof. Davies. It gave a history of the present descendants of the mound-builders, considering the latter as still not entirely extinct. The paper elicited a great deal of discussion by Dr. Hoy, Prof. Butler, Mr. Wood_ man éf al. FIFTH SESSION. February 15, 9:30 A. M. Mr. E. T. Sweet read a valuable paper containing results of analysis of the Milwaukee brick clay. The following business was then transacted: First, the summer meeting for July, 1877, was appointed to be held at Racine on the third Tuesday of July; the autumn meeting being entirely set aside for the future. F. H. Day, M. D., of Wauwatosa, Wis. Prof. George W. Peckham, of Milwaukee, Prof. W. Bundy, of Sauk City, Hon. W.C. Allen, of Racine, Rey. H. M. Simmons, of Kenosha, were elected as annual members. : John W. Barrow, of No. 313 E. Seventeenth street New York city was elected a corresponding member. The following amendments to the By-laws were offered for one year’s con- sideration, according to the provisions of the constitution. By-law No. II to be amended so as to read as follows: “The regular annual meeting to take Proceedings of the Academy. 271 place herexfter on the last Wednesday and Thursday of December, at Madison and the summer annual meeting to be held on the third Tuesday in July, at such place as shall be fixed upon at the regular annual meeting in De- cember. Special meetings may be called by the President at his discretion, or by request of any five members of the council. By-law, Art. I, sec. 7, to be amended to make the fee of annual members three dollars in place of two. ' The resignation of the Librarian was accepted, and the Secretary was re- quested to act as Librarian until the next election of officers. The Department of Fine Arts was regularly organized. Hon. Joseph Hamilton, of Milwaukee, was elected an Honorary member of the Academy. Hon. J.C. Ford, of Madison, an annual member. The report of the treasurer was then read as follows: WIsconsIN ACADEMY OF SCIENCE, ARTS AND LETTERS, TREASURER’S OFFICE, Madison, Dec. 18, 1877. Hon. P. R. Hoy, President : I have the honor to report the financial condition of the Academy as fol- lows: Total amount of fees and dues received from 58 members........ $778 25 Total fees received from 10 life members....... MN atePaloparwistotersts; serene 1,000 00 MT ERES TOM OI secret Sete Tiere ei cre hale & eicmmiea tele eae aieie sala oa ea eyichees 370 00 Total amoant disbursed in payment of warrants, to date.......... ae OF a DIeuU CMEC AGU: efotaseinisieycieve sis orefaninfetnfsteieiniets\cie nfeesla/elnyalere laren teiars 1,370 28 Signed, GEORGE P. DELAPLAINE, Treasurer. The Academy then adjourned. to meet at Racine upon the 10th of July following. FIRST SUMMER MEETING. Held at Racine, Wisconsin. First Semi-ANNUAL MEETING. July 10, 11 and 12, 1877. W. A. Germain, Acting Secretary. FIRST SESSION. Racine, July 10, 7:30 P. M. The Academy met at 7: 30, P M., President Hoy in the chair. Dr. Meachem, mayor of the city, delivered an address of welcome. Rev Dr. Steele, of Appleton, responded. Prof. Chamberlin then read a Eulozy on the late Prof. James Eaton, of Beloit, which was ordered printed in the transactions. Rev. Dr. James DeKoven, Pres’t Racine Coilege, then read a paper on “ Re- ligion as an Element in Education.” The Academy adjourned to meet next morning at nine o’clock. 272 Wisconsin Academy of Sciences, Arts, and Letters. SECOND SESSION. July 11,9:00 A. M. Academy met pursuant to adjournment. Minutes of the last annual meet- ing read. Prof. Butler called attention to the fact that notice of Prof. Wright’s paper on “ Philosophy of History,” had been omitted. Correction was made by the Acting Secretary. Attention was called by President Hoy to the amendments offered at the last regular meeting. -To amend sec. 3 of the by-laws so as to read: 1. The regular annual meeting to take place on the last Wednesday and Thursday of December, at Madison, and the summer annual meeting to be held on the third Tuesday of July at such place as shall be fixed at the reg- ular annual meeting in December. 2. Special meetings may be called by the President at his discretion, or by the request of any five members of the council. 3. Article I of sec. 7 of the constitution to be amended to make the fee of annual members three dollars in place of two dollars. Prof. Allen moved the adoption of the amendments. Dr. Steele moved to amend so as to read, in place of “the regular annual meeting shall take place, etc.,” the following: “The reguiar annual meeting shall take place during the last week of De- cember, the days to be appointed by the council.” Amendment carried. The resolutions were then adopted unanimously as amendments to the by-laws. The following persons were then elected as annual members: Rev. J. L. Jones, Janesville, Wis. Rev. 8. A. Griffith, Milwaukee. Rev. A. P. Meade, Racine. Rey. Dr. James DeKoven, Racine. Prof. J. J. Elmendorf, Racine. Prof. H. F. Oldenbage, Milwaukee. Prof. F. W. Falk, Ph. D., Racine. Dr. E. H. Merrell, Ripon. Rev. G. E. Gordon, Milwaukee. Hon. Edward Martin, Kenosha. Prof. G. D. Swezey, A. M., Beloit. Prof. Peter Henrickson, Beloit. Prof. G. R. Kleeberger, Whitewater. R. W. Reynolds, La Crosse W. A. Germain, Delafield. Prof. C. A. Kenaston, Ripon. Prof. W. M. Hailman, Milwaukee. Prof. G. W. Gerry, Ripon. Prof. J. McMurphy, Kenosha. Frank Head, Esq., Kenosha. Prof. J. P. Marriett, Kenosha. Hon. J. H. Howe, Kenosha. Dr. J. G@. Meachem, Racine. Dr. J. G. Meachem, Jr., Racine. Proceedings of the Academy. 273 As Corresponding members: Dr. C. C. Abbott, Trenton, New Jersey. Alford Paine, 8. T. D., of Hinsdale, I11. As Honorary member, Prof. Spencer Baird, M. D., LL. D., of Washington, D. C. Prof. Alien, chairman of the committee appointed to see about securing rooms for the Academy, reported that the rooms of the Railroad Commis- sioners could be secured in December. The report accepted, and the com- mittee continued. Prof. Allen then read a paper on “Early Form of Land Tenure.” Dr. Falk made extended remarks on Prof. Allen’s paper, and gave a review ef the feudal relations in Germany. Prof. McMurphy read a paper on “ Rotation as a Factor of Motion.” The President then read the following communication from Captain Nader, C. E., on “The Balloon in Meteorology.” Mapison, Wis., June 20, 1877. Dr. P. R. Hoy, Racine, Wis.: DEAR AND ReEspEcTED Str: Your very kind note of invitation of the 7th instant was duly received, and while I regret very much that I shall be unable to partake of the proffered hospitality of the people of Racine, I feel very thankful for your kind remembrance. My duties here render my time uncertain, and occupy my atten- tion so much that I shall not be able to attend the meeting, which no doubt will be pleasant and instructive. I shall be unable to produce anything in time. I was preparing a letter to you, when I received your note, on a subject which may be interesting, and which I will now give you as briefly as possible. It is but a short time since an idea occurred to me which I be- lieve to be novel, and perhaps of scientific import, and should you consider it of sufficient importance, I beg you would please present the same for discussion at the meeting. The object is to explore the atmosphere, so far as may be prac- ticable, without the risk of life and limb. This I propose to do in the following manner: In the first place, I resort to a gas balloon to carry up my apparatus, and since there is no danger of any irre- parable damage, the same may be constructed as light as possible, even frail, | may say; and since the charge is not required to endure very long, small ieaks need not be noticed, and I believe such a balloon may be constructed at a nominal cost. Kach cubic foot of gas of specific gravity, say 0.6, will displace about 530 grains of air, and deducting its weight, 32 grains, will 18 274 Wisconsin Academy of Sciences, Arts, and Letters. support a weight of 498 grains, so that 1,000 cubic feet will carry about 70 pounds weight, which is the displacement of a balloon of less than 13 feet diameter. The balloon is allowed to rise at pleasure by means of a cord of sufficient strength to support considerable more than its own weight, of the desired length or height. The lateral motion, while rising, will indicate the direction of the currents; the height is computed at any time by its position. The principal apparatus will be that for recording the tempera- ture and barometrical changes. This is done by a clock-work ar- rangement carrying a strip of highly sensitised paper, with a regular motion, so that. the condition of both instruments is photographed at each instant of time. The observation having commenced, it is only necessary to note the time and corresponding altitude, and ob- tain the corresponding phenomena when the apparatus is recovered. Under favorable circumstances, the balloon may be brought to rest at different altitudes, in order to give the instruments time to as- sume local conditions. To the apparatus is attached a parachute, so that the same may be recovered in case of collapse or other acci- dent. I have thought some of adding a magnetic apparatus, but have not had time to develop the idea. This might possibly throw some light on the possibility of aerial navigation, and also be worthy of consideration in other respects. Hoping you will have an interesting and pleasant meeting, I remain, most respectfully, your obedient servant, JOHN NADER. THIRD SESSION. July 11, 2.30 P. M. Rev. H. M. Simmons read a paper on “ The Social Organism.” Prof. Hailman delivered a lecture on “The Kindergartens.” Judge Allen then read a paper prepared by Dr. Mason, on the “ Duty of the State to its Unfortunate Classes.” Prof. Butler read a paper on “ American Pre-Revolutionary Bibliography.”’ FOURTH SESSION. 7.30 P. M. Prof. Jewell, of Chicago, read a paper on “ Mind in the Inferior Animals.” Academy adjourned to attend a reception given by Mayor Meacham in honor of the members. Proceedings of the Academy. 275 FIFTH SESSION. 9:30 A. M. The Academy met pursuant to adjournment. Prof. Luther, of Racine, was elected an annual member. Dr. Hoy, President of the Academy, delivered a lecture on the “ Disappear ance of Large Animals in Wisconsin.’ Rev. C. Caverno read a paper on “ Abolition of the Jury System.” Dr. Elmendorf read a paper on “ Nature and Freedom.’’ SIXTH SESSION. 2:30 P. M. Prof. Stuart read a paper on “ Harmonic Method in Greek Art.” Prof. Butler then read a paper on “ The Mosque of Omar at Jerusalem.” Mr. A. Paine, read a paper on “ Art as Education.” The following resolutions were then proposed by Prof. Butler, and seconded by Prof. Caverno, and unanimously adopted: “ Resolved, That the Wisconsin Academy of Sciences, Arts and Letters begs to tender its grateful acknowledgments te the mayor of Racine for his cor- dial greeting in the Court House, and reception at his mansion, as well as to the citizens of the city for their generous huspitalities, and for their attendance on the sessions. “Resolved, That the Wisconsin Central,and Western Union railroads, which have facilitated our convening in the ,interest of science, are hereby thanked for their kind courtesies. “ Resolved, That the sheriff and county commissioners, by placing at our disposal their new and noble court house, have done a service to science and shall be remembered by us with gratitude. “ Resolved, That the hearty thanks of the Academy are hereby presented to Dr. DeKoven, as well as the Professors of Racine College and other gen- tlemen for their able lectures, with which they have honored, entertained and instructed our Association. “ Resolved, That these resolutions be presented to the newspapers of this city for publication.” Prof. Perkins, in behalf of the Association, expressed the sincere thanks of the Academy to Dr. Hoy, President, for his earnest efforts to promote its interests. The Academy then adjourned to meet in Madison on the 26th of December following, according to the change in the by-law regulating the time of the Regular Annual Meetings. 276 Wisconsin Academy of Sciences, Arts, and Letters. EIGHTH REGULAR ANNUAL MEETING, Held at Madison, Wisconsin, December 26th, 27th and 28th, 1877. WEDNESDAY, Dec. 16, 1877. The Eighth Regular Annual Meeting was opened at 2:30 P. M., there being a Jarge attendance. Dr. Hoy, President of the Academy, in the chair. The minutes of the Racine Semi-annual Meeting were read, and the amend- ments to the Constitution and the By-laws then made, commented upon and formally ratified. The Secretary gave notice that a complete catalogue of all books and pamphlets thus far received by the Academy was completed, and would be published in the forthcoming Vol. IV of the Transactions. The Treasurer made the following report: TREASURER’S OFFICH, Wisconsin Academy of Sciencies, Arts and Letters, . Mapison, Dec. 26, 1877. P. R. Hoy, M. D., President of the Wisconsin Academy of Scionces, Arts and Letters: I have the honor to report the financial condition of the Academy, as fol- lows: Total amount of fees and dues from 62 members................. $817 25 Total feesttromil. OlifetmMennib ersey crap selslcietiefetelaleeteleie hehe lot eletle nate 1,000 00 Total interest on loan ....-..... ialopeldicaiets decraleve a eee more RS ct, 440 00 $2,259 25 Total amount disbursed in payment of warrants to date.......... $855 17 Balan Cemimitneasumiyye rr) oie rereieret eetelots) tel elelerel etic) eiette elie r ieee $1, 402 08 (Signed) G.P. DELAPLAINHE, Treasurer. The Treasurer urged greater promptitude on the part of members in the payment of their dues. Only 62 members out of about 200 have paid any dues whatsoever thus far. The following papers were read and dicussed during the session: How Did the Aborigines of this Country Fabricate the Copper Implements ? By P. R. Hoy, M. D., President of the Academy. Some Remarks on the Descent of Animals. By Prof. Oldenhage, of Mil- waukee. Why Have the Ruminants no Upper Incisors. By P. R. Hoy, M. D., Pres- ident of the Academy. Boiler Explosions. By Chas. I. King, Superintendent University Machine Shop. Proceedings of the Academy. 277 Antiquities and Platycnemism of the Mound Builders. By J. N. De Hart M. D. Extent and Significance of the Wisconsin Kettle Moraine. By T. C. Cham- berlin, A. M., State Geologist. The German, French, English and American Press. By Hon. Joseph Hamilton, of Milwaukee, Honorary Member of the Academy. The Ethical Bearings of the Doctrine of Evolution. By Rev. Jenk. Ll. Jones. Mr. C. H. Haskins, of Milwaukee, gave a very interesting description of the Bell Speaking Telephone, illustrating his remarks by experimental dem- onstrations. A paper on the Fauna of the Niagara and Upper Silurian rocks in Milwau- kee county, by F. H. Day, M. D., was read by title only, not being received in time to be read in full. The death of Prof. Oldenhage of Milwaukee was announced and his paper read by Prof. Peckham. Profs. Peckham, Rogers and McAllister, of Milwaukee, were appointed a committee to presenta memoir of Prof. Oldenhage, for publication in Vol. IV of the Transactions of the Academy. The following gentlemen and ladies were elected annual members of the Academy: J. 8. Westcott, Superintendent of City Schools, Racine. J.T. Lovewell, Female College, Milwaukee. Albert Hardy, Principal High School, Milwaukee. Rufus B. Smith, Madison. Willett S. Main, Madison. Geo. B. Smith, Madison. P. B. Parsons, Madison. B. EH. Hutchinson, Madison. Mrs. 8. F. Dean, Madison. Mrs. H. M. Lewis, Madison. Miss Ella Giles, Madison. J. N. DeHart, M. D., Madison. J.J. Saylor of Cleveland, Ohio, was elected a corresponding member of the Academy. Academy adjourned to meet in Milwaukee, at a time to be specified by the President of the Academy after consultation with the officers of the Scientific Club. SECOND SEMI-ANNUAL MEETING, Held at Milwaukee, Wisconsin. FEMALE COLLEGE, MILWAUKEE, July 23, 1878. Pursuant to a notice given by the Milwaukee Scientific Club, the second semi-annual (or summer) meeting of the Wisconsin Academy of Science, Arts and Letters was convened in the Female College, Milwaukee, at 7:30 o’clock, P.M. President P. R. Hoy, of Racine, in the chair. Hon. Har- 978 Wisconsin Academy of Sciences, Arts, and Letters. rison ©. Hobart, acting mayor of the city of Milwaukee, delivered an address of welcome. P.R. Hoy responded. Prof. J.J. Elmendorf, 8. T. D., of Racine, then read a paper on the “ Popular Epics of the Middle Ages as Aids to Historic Study.” TuurspDay, July 24, 1878. Academy met at9o’clock A. M. President P. R. Hoy in the chair, Prof. J..E. Davies, acting as Recording Secretary. The following persons were elected annual members of the Academy. The president of the academy prefacing the ballot with the remark that “ science knows no distinction of race, color, or sex: ”’ Mrs. Laura J. Wolcott, M. D., 471 Milwaukee St., Milwaukee, Wis. Mrs. Charles Farrar, 614 Milwaukee St., Milwaukee, Wis. Miss Brooks, 614 Milwaukee St., Milwaukee, Wis. Miss Marion Stewart, 469 Marshall St., Milwaukee, Wis. Mrs. Emery McClintock, 507 Astor St., Milwaukee, Wis. Mrs. George Gordon, Humboldt Av., Milwaukee, Wis. Miss Frank Whitnall, Humbolt Av., Milwaukee, Wis. Mrs. A. M. Thomson, 459 Cass St., Milwaukee, Wis. Mrs. A. W. Bate, 320 Terrace Av., Milwaukee, Wis. Mrs. Celia C. Wooley, Sec. Philosophical Society, Chicago, Ill. Mrs. P. Abboit, cor. Jackson and Division Sts., Milwaukee, Wis. Mrs. Lewis Sherman, 171 Wisconsin St., Milwaukee, Wis. Mrs. Dr. Marks, Prospect Av., Milwaukee, Wis. Mrs. Carl Deerflinger, 707 Jefferson St., Milwaukee, Wis. Mrs. Matilda F. Anneke, 269 Ninth St., Milwaukee, Wis. Mrs. Julia Ford, 375 Greenbush St., Milwaukee, Wis. Mrs. N. H. Adsit, 268 Knapp St., Milwaukee, Wis. Mrs. R. C. Spencer, 275 Prospect Av., Milwaukee, Wis. Mrs. Edward P. Allis, 381 Prospect Av., Milwaukee, Wis. Mrs. D. A. Olin, Racine, Wis. Mrs. Frackleton, 469 Marshall St., Milwaukee, Wis. Mrs. Olympia Brown Willis, Racine, Wis. Mrs. J.G. McMurphy, Racine, Wis. Mi s Jeuny Hoy, Racine, Wis. Miss Mary J. Lapham, Summit, Wis. Prof. Robert C. Hindley, Racine College, Wis. Mr. Eugene B. Winship, Racine College, Wis. Mr. Charles Mann, Milwaukee, Wis. Mr. Wm. P. Merrill, Milwaukee, Wis. Dr. G. A. Stark, Milwaukee, Wis. Mr. James S. Buck, Milwaukee, Wis. Mr. George Gordon, Milwaukee, Wis. Dr. Thomas A. Green, 146 Martin St., Milwaukee, Wis. Prof. Charles A. Farrar, Milwaukee College, Wis. Mr. H.S. Durand, Racine, Wis. Mrs. H. 8. Durand, Racine, Wis. Miss Frankie Durand, Racine, Wis. Rev. F. 8. Luther, Racine Ccllege, Wis. Dr. R. M. Byraness, Cincinnati, O., was elected corresponding member. At the suggestion of Prof. J. J. Elmendorf, a resolution was framed and adopted to the effect, that all books that are now in the possession of the Aca- demy, may be loaned, for one year, to any of the members desiring them. A request was a'so made by Prof, J. E: Davies, that all members contem- Proceedings of the Academy. 279 piating readiny papers notify him of the same, for the purpose of facilitating the arrangement for the annual meeting. An invitation was received from Dr. Day, soliciting the members to visit his cabinet at Wauwatosa. A committee, consisting of Prof. S. H. Carpenter, Prof. Ailen, and Prof. J. E. Davies, was appointed, to report, at the next meeting, a suitable memoir of the late Dr. Feuling. Judge W.C. Allen, of Racine, then read a paper entitled, “ The Accounta- bility of Public Officials.” President Chapin, of Beloit College, read a paper on the “Nature and Functions of Credit.” This was followed by an extempore history of credit in Wisconsin, by Mr. Chapman. At the afternoon session, the following papers were read: “ Drinking Water,” by Dr J. G. Meacham, of Racine. ‘‘ Mental Hospitality,’ by Miss Ella Giles, of Madison. “Scientific Housekeeping,” by Mrs. A. W. Bate, of Milwaukee. “The Origin of Certain Constellations,” by the Rev. H. M. Simmons, of Kenosha. The Academy then adjourned to attendat the invitation of the resident members and committee of arrangements, a banquet given in the evening at the Plankington House. ‘ The following account of the banquet is taken from the Milwaukee News, of Thursday, July 25th, 1878: “ By invitation of the committee of arrangements, W. P. McLaren acted as President of the evening. At his right, sat President Chapin, of Beloit Col- lege, and at his left Dr. Hoy, president of the Academy. President Chapin asked Divine blessing on the gathering, after which an unusually long time was spent in disposing of the long and palatable list of dishes on the bill of fare. Mr. McLaren finally called the gathering to order and, in a neat and well-timed speech, introduced the first sentiment on the programme, “The State of Wisconsin.” It was expected that the Hon. George H. Paul would respond to this, but,in Mr. Paul’s absence, Judge Allen, of Racine, was called. The Judge gave a highly interesting account of the growth and pro- gress of the state from the small beginnings of forty years ago, when he first came into this section of the country. To the second toast, “The City of Milwaukee,” the Hon. E. D. Holton re- sponded, drawing parallels from history and from the present condition of cities in other parts of the world, to show the great advantages which Milwau- kee possesses and the magnificent promises of the future. Dr. Hoy responded for “The Wisconsin Academy of Sciences, Art and Letters,’? very briefly sketching the objects and work of the society. To the fifth sentiment, ““Amer- ican Science,” it was expected that Dr. Kempster would respond. But that gentleman was not present, and Prof. Davies, of our State University was called upon. Prof. Davies’ speech was short, but full of the most interesting matter, and clothed in well-chosen words. 280 Wisconsin Academy of Sciences, Arts, and Leiters. One of the best speeches of the evening was that of ex-Superintendent MacAllister, who answered for ‘Our Public Schoals.” President Chapin responded in an eloquent and logical manner to the seventh toast, ‘‘ Arts and Letters.” M.Almy Aldrich spoke for “The Press,” and the regular senti- ments closed with “‘Our New Associate Members,” to which Mrs. Amelia Bate responded in a manner that elicited the heartiest applause and warmest commendations on all sides. Brief speeches followed by the Rey. Messrs. Gordon and Livermore, Dr. Wight, Dr. Elmendorf, Mr. Buck and others; and the gathering broke up about 11 o’clock. Fourth Session, Jory 25, 1878. Academy met at 9 o’clock A. M. President P. R. Hoy in the chair, Dr. J. E. Davies acting as recording secretary. : A resolution offered by Prof. Elmendorf, that in the appendix of the trans- actions shall be printed a list of the public and private collections of books within the state, as available for the use of members, to aid in the work of the society, was referred to Prof. Elmendorf and Prof. W. C. Allen, for further consideration. A motion made by Mr. Peckham, that the secretary of the society be allowed to expend one hundred dollars ($100) for binding pamphlets belonging to the academy, was unanimously carried. Dr. J. N. De Hart, of Madison insane asylum, then read a paper on the ” Microscope and its Benefits to Science.” Rev. C. Caverno, of Lombard, Ill., read a paper entitled ‘“ Savings Banks and the Industrial Classes.”’ A paper entitled “ The Relics of a Prehistoric Race,” prepared by Dr. De Hart, was read by Rey. G. E. Gordon, as Dr. De Hart was suffering from a severe cold. Mr. A. R. Sprague, of Evansville, Wisconsin. Mr. W. P. McLaren, Milwaukee, Wisconsin. Dr. D. W. Perkins, Milwaukee, Wisconsin, Were elected annual members of the Academy. After the morning session the members adjourned to meet at the Planking- ton House at 3 o’clock P. M., where the resident members of the Academy and citizens of Milwaukee nad provided carriages for a drive around the city. The members were taken through the handsomest residence streets of Milwaukee, were shown the elegant grounds and conservatory of Mr. Alex. Mitchell, and then taken to the National Soldier’s Home near the city, where they were introduced to Genl. E. W. Hincks, commandant of the Home, who gave them a most cordial welcome. They were then returned to the Plank- ington House, having spent a most enjoyable afternoon. Academy adjourned, to meet in Madison on the 26th and 27th of December, 1878, J. E. DAVIES, General Secretary- REPORT OF THE LIBRARIAN. To the President of the Wisconsin Academy of Sciences, Arts and Letters: Sir: At the suggestion of the General Secretary, Dr. Davies, I have made a complete revision of the library of the Academy. This work has been of considerable difficulty, owing to the fact that the bulk of the library consists of pamphlets, and the unbound publications of the various scientific associ- ations in our own and foreign countries. Many of these are exceedingly valuable. Many of them contain the summation of the life-long investiga- tions of specialists in their particular department of the vast field of science. Owing to their not being sufficiently well bound, few of these are at present available to the members of the Academy —a thing to be deeply regretted, since these publications are to be found in no other library of the State, that of the Academy filling a distinct and separate purpose, being, to a large extent, supplementary to the State Historical Library. Taking these things into consideration, it seems advisable that a certain sum should be set aside annually for the purpose of preserving these various publications in a more substantial binding, The library of the Academy contains seven hundred and forty-four volumes, including pamphlets. Under the present system of exchange, it is rapidly growing. I herewith transmit a complete catalogue, embracing all publica- tions received up to the present time (June 15th, 1878). The greater part of those from foreign societies have been forwarded by the courtesy of the Smith- sonian Institute, at Washington, D. C. W. A. GERMAIN, Acting Librarian. . PUBLICATIONS OF LEARNED SOCIETIES. Now inthe library of the Wisconsin Academy of Sciences, Arts and Letters. EUROPEAN. BELGIUM, Musee Teyler — Archives — Vol. I, Pts. 1, 2,38 and 4. Vol IT, Pts. 1, 2, 3 and 4. Vol. III, Pts. 1,2, 3 and 4. Vol. IV, Pts. 1 and 2. Hainaut Academy of Science, Arts and Letters — Memoirs for 1871, 1872, 1873, 1874, 1875, 1876 and 1877. 282 Wisconsin Academy of Sciences, Arts, and Letters. FRANCE. National Academy of Caen ,— Memoirs, Vols. I, II, III, IV, V, VI and VII — 1871-6. Academy of Bordeaux — Acts de L’Academie, 8d Series, 1872-3. Acts de L’Academie, 3d Series, i872. Academy of Lyons — Memoirs, Vols. XV, XVI, XVIII, XIX — 1870-75. Academy of Metz — Memoirs — 1871-2, 1872-3, 1874-5, 1875-6. Tables Generales de |’ Academie, 1819-71. Montpellier Academy of Science, Arts and Letters — Transactions, Vols. IV, V, VI, VII and VIII — 1868-76. Agricultural and Scientific Society of the Sarthe — Bulletins, Vol. XIII, Parts 1,2 and 3, 18%1—2; “ Se SVE Ape oss So) EXERT Sa: ie ee OGL SIGE Amiens Linnean Society of the North of France — Monthly Bulletins, from May, 1875, to December, 1877, ITALY. Royal Instetute of Lombardy — Transactions for 1873, Vol. VI; 1874, Vol. VII; 1875, Vol. VII; Memoirs | Vols. XIII, XIV and Xy. Academy of Modena — Memoirs, Vol. XVI. Royal Geological Commission of I taly — Bulletines, Nos. 1 to 12, 1874. Publication of 1875. NETHERLANDS, Nederlandsch Meteorologroca. id Jaarboeck, 1868. id Jaarboeck, 1871. Royal Academy of Amsterdam — Transactions, Vol. I, P’ts 1, 2,3 and 4, 1865-7; Vol. II, P’ts 1, 2 and 3 1867-8; Vol. III, P’ts 1, 2 and 3, 1868-9; Vol. EV Pts 1 2 eand 2 1869-70; Vol. V, 1871: Vol. VI, 1871-2; Vol. VII, 1873; Vol. VIII, 1874; Vol. IX, 1875: Vol. XIII, 1874; Vol. XIV, 1875; Vol. XV, 1875. Year Book, 1873 and 1874. Catalogue of the library of the Academy, 1877. Proceedings of the Academy. 288 Netherland Society for the Encouragement of Industry — Records, 1873, 1874, 1875 and 1876. Proceedings, 1874, 1875 and 1876. Amsterdam Royal Society of Physical Science — Transactions, Vols. I, II, III, IV, V, VI, VII, VII, IX, 1868-76. Holland Society of Scvence — Transactions, 1873, 1874, 1875, 1876 and 1877. Catalogue of members, 1877. Provincial Society of Arts and Scvences — Publications, 1872, 1878, 1874, 1875 and 1876. Royal Netherland Meteorological Institute — Meteorological Observations, 1873. Year Books for 1868, 1871 and 1874. RUSSIA. Royal Academy of Sciences of St. Petersburgh — Repertorium of Meteorology, 1874, 1875 and 1876. Royal Academy of Finland — Natur och Folk, 1871, 1872, 1878, 1874 and 1875. Imperial Physical Observatory — Dorput Publications, Vols. I, II and III. Annalen, 1875 and 1876. SWEDEN AND NORWAY. Kongliga Swenska Vetanschaps Academensis. The Royal Swedish Academy — Transactions, Vol. III, 1874. Memoirs, 1875, 1876 and 1877. University of Upsala — Meteorological Observations, Vols. IV, V and VI. Royal Society of Upsala — Transactions for 1874, 1875 and 1876. Royal Academy of Science of Christiana — Enumeratio Insectorium Norvyicorum, 1874, 1875, 1876 and 1877. University of Christiana — Publications for 1873, 1874, 1875 and 1876. Physiological Studies, by J. W. Muller. Researches in Egyptian Chronology. Official Statistics of Norway, 1870, 1871, 1872. 284 Wisconsin Academy of Sciences, Arts, and Letters. GERMANY. Academy of Natural Sctences of Munich — Transactions for 1871, 1872, 1873, 1874, 1875 and 1876. Gottingen Royal Society — Transactions for 1875, 1876 and 1877. Royal Observatory, near Munich — Annals, XX. Vol. Mannheim Academy of Natural Sciences — Transactions for 1870, 1871, 1872, 1873 and 1874. Academy of Sciences of Heidelberg — Transactions for 1874, 1875, 1876 and 1877. Silesian Society, Breslau — Transactions for 1873 and 1874. dist Annual Report, 1873. o2d Annual Report, 1874. 53d Annual Report, 1875. o4th Annual Report, 1876. Academy of Natural Science— Bremen — Transactions for 1872-1873 and 1874, Tables, etc., 1873, Parts I and II ; 1874, Parts I and II, Vol. IV. ings, Part I, 1876. Supplement to same, 1876. Rhenish Prussia and Westphalia Soctety of Sciences — Transactions — 9th year, 1872. a 10th “ Part I, 1873; Part II, 1878. “ Part I, 1874; Part II, 1874, sh Part I, 1875; Part IT, 1875. - Part I, 1876. Giessen Society of Science, Arts and Letters — Transactions for 1876 and 1877. Halle Journal of Natural Science — Berlin— Transactions — Vols. IX to XIV, 1874-5 and 6. Natural History Society of Dresden — Transactions for 1876, Isis Academy of Natural Science — Dresden — Transactions for 1874, 1875, 1876 and 1877. Polytechnic School at Hi anover — Programme for 1874, 1875, 1876 and 1877. Natural Science Society of Freiburg — Transactions, 1874, 1875 and 1876. . Proceed- Proceedings of the Academy. 285 Academy of Eldena — Transactions for 1870. Royal Phys.-Heon. Society of Konigsberg — Publications for 1878, 1874, 1875 and 1876. Natural Science Society of Gorlitz — Transactions, XV. Vol., 1875. Society of Naturalists, Dantzig— Publications for 1872, 1873, 1874, 1875 and 1876. Munich Royal Bavarian Academy of Science — Transactions for 1875, Parts I and II.; 1876, Part I. SWITZERLAND. Zurich Academy of Natural Science — Transactions for 1873-1874, and 1875. St. Galle Natural Science Society — Transactions for 1874 and 1875. Natural Science Society of Buasel— Transactions for 1874, 1875, 1876, 1877 and 1878. Natural Science Society, Neuchatel — Transactions for 1875, 1876 and 1877. Natural Science Society of Berne — Transactions for 1873, 1874, 1875, 1876 and 1877. Natural Science Society of Schaffenhausen — Transactions for 1872 and 1873. Natural Science Society of Chur — Transactions for 1873 and 1874. Natural Science Society of Luzerne — Transactions for 1576. Academy of Vaudoise — Transactions, Vols. XIV and XV, 1877-8. Bulletin for 1877. ENGLAND. Philosophical Society of Manchester — ' Memoirs, Vols. XII, XIII, XIN, XV — 1872-6. Catalogue, 1875. London Royal Society — Proceedings — Vol. XXII, Nos. 158-155; Vol. XXIII, Nos. 156-163; Vol. XXIV, Nos- 164-170; Vol. XXV, Nos. 171-179; Vol. XXVI, Nos. 179-183. 286 Wisconsin Academy of Sciences, Arts, and Letters. DENMARK. Royal Society of Denmark — Transactions for 1874, 1875, 1876 and 1877. Bulletin for 1877, No. I. Royal Academy of Copenhagen — Bulletins for 1876, Nos. I and II. AUSTRALIA. Public Library of Melbourne — Mines and Min. Statistics of New South Wales. Treatise on New South Wales. Nat. Industrial Resources of New South Wales. Ann. Rept. of the Dept. of Mines. MEXICO. Natural Museum of Mexico — Annals, Vol. I, 1877. SPAIN 4 ND PORTUGAL. Royal Academy of Lisbon — Transactions for 1875. SOUTH AMERICA. Venezuela Monthly Gazette for 1877 and 1878. ISLAND OF MAURITIUS. Academy of Mauritius — Transactions, Vol. IX, 1876. IRELAND. Royal Dublin Society — Journal for 1870-1875. AUSTRIA. Academy of Natural Sciences of Vienna— Transactions, 1872, 1878, 1874, 1875 and 1876. Royal Zoological and Botanical Society of Vienna— Publications, 1872, 1873, 1874, 1875, 1876 and 1877. Hmden Natural-Philosophy Society — Transactions for 1872, 1878, 1874, 1875, 1876 and 1877. Society of Natural History, Brunn— Transactions, Vols. XII and XIII, 1873. Catalogue of the Library, 1874. Proceedings of the Academy. 287 AMERICAN SOCIETIES. Boston Society of Natural History — Proceedings — Vol. 17, Parts II, III and IV, 1874. Vol. 18, Parts I, II, III and IV, 1875-6. Vol. 19, Parts I and II, 1877. Buffalo Academy of Natural Science— Bulletin — Vol. I, No. I, 1873. Vol. I, Nos. II, III and IV, 1874. Vol. II, Nos. I, II and ITI, 1874. Huseum of Comparative Zodlogy — Harvard University — Bulletin— Vol. II, Nos. 1-10, 1876. Vol. III, Nos. 11-14, 1876. Vol. III, Nos. 15-16, 1876. Annual Report of Trustees, 1874. Annual Report of Trustees, 1874. St. Louis Academy of Science — Vol. III. Nos. I, If, I1f, LV, 1873-1875-1876-1878. Quarterly Journal of Conchology — For 1874, 1875 and 1876. Philadelphia Academy of Natural Science — Proceedings. Parts I and [I, 1877. New York State Museum of Natural History —- Twenty-fifth Annual Report of Regents. American Academy of Science — Proceedings — Vol. IV, from May, 1876, to May, 1877. Kansas Academy of Science— Vol. IV, 1875. Vol. V, 1876, Birds of Kansas (Snow), 1875. American Association for the Advancement of Scieace — Proceedings — Buffalo, 1876. Cleveland Academy of Science — Proceeedings, 1845-1859. 288 Wisconsin Academy of Sciences, Arts, and Letters. BOUND VOLUMES AND MISCELLANEOUS PAMPHLETS. Wells, Walter, Water Power of Maine. Durrie, D. §., Cat. State Hist. Society, Vol. I, 1873. Durrie, D. S., Cat. State Hist. Society, Vol. II, 1873. Driunellette, P. S., Epistola. Museum of Natural History of New York. Munsel, J., Chronology of Paper Making, Dudley Observatory, Annals of, Vol. II . Cabinet of Natural History, New York. Munsel, J. Manual of the Lutheran Church. University of the State of New York, 85th Rep’t, 1872. Noye, W. Maxims of the Laws of England. Ill. R. R. Commissioner’s Rep’t, 1871. Department of Agriculture, Washington, Report, 1871. Smithsonian Report, 1871. Land Office Report, 1870. DeCosta, B. F., Hudson’s Sailing Directions. Tophographic Survey of Adriondic Wilderness. Natural History and Geology of Maine for 1863. University of State of New York, 1873. R. R. Commissioner’s Report, Ill., 1872. Same for 1873. Transactions of the Wisconsin Agricu'tural Society, 1869. Transactions of the Wisconsin Agricultural Society, 1870. Transactions of the Wisconsin Agricultural Society, 1871. Transactions of the Wisconsin Agricultural Society, 1872-3. Transactions of the Wisconsin Agricultural Society, 1873-4. Transactions of the Wisconsin Agricultural Society, 1874-5. Transactions of the Wisconsin Agricultural Society, 1875-6. Public Libraries of the United States, Part I, 1876. Report Speciale Sur Immigration, 1872. : Raymond — Min. Resources West of the Rocky Mountains, 1872. Raymoad — Min. Resources West of the Rocky Mountains, 1878. Finance Report of 1876. - Compendium of the United States Census, 1870. Memoirs Manchester Phil. Society, Vol. V. Mines and River Resources of New South Wales, 1875. Report of the Chief of Statistics, Washington, 1876. Commerce and Navigation, Washington, 1876. Proceedings of the Academy, 289 Wisconsin Agriculture, 1876-7. Hayden — U. 8. Geological Survey, Washington, 1877. Birds of the Northwest — Qoues. Museum of Natural History, New York, 1872. New York State Library, 57th Report. Patent Office Report, Vol. I, 1869. Patent Office Report, Vol. II, 1869. Patent Office Report, Vol III, 1869. Report of Commissioner of Education, Washington, 1871. Explorations in Nevada and Arizona. Ninth Census of the U. S. Hayden, F. V., Geological Survey, Vol. II, 1875. Hayden, F. V., Geological Survey, 1867-8-9. Hayden, F. V., Geological Survey, 1870. Hayden, F. V., Geological Survey, 1871. Hayden, F. V., Geological Survey, 1872. Hayden, F. V., Geological Survey, 1873. Hayden, F. V., Geological Survey, 1874. International Exhibition, London, 1862 Powell. B. P., Geology of the Uinta Mts. Hayden., U.S. Geol. Survey, 1874. Hayden, U.S Geol. Survey, 1876. Hayden, U.S. Geol. Survey, 1876. Powell, B. P., Colorado River Exploraitions, 1873. Memoriam — Increase A. Lapham. New England and the English Commowealth. Fur-bearing Animals of the Northwest — Cowes. Powell, J. W., American Ethnology. Hayden, F. V., U.S. Geol. Survey, ,Vol. XI. Hayden, F. V., U.S. Geol. Survey of 1875. Memoirs, Vol. I, 1875. Memoirs, Vol. II, 1875. U.S. Geol. Exploration of 9th Par., C. King, 1875. Department of Agriculture, 1875. Department of Agriculture, 1876. Commercial Relations, 1875. Messages and Documen's U. S., 1871. Commerce and Navigation, Part I, 1876. Commerce and Navigation, Part II, 1876. The Electoral Count of 1876. Leading Cases in International Law (Digest). Western Review of Science and Industry. Theo. 8. Case, Kansas City, Mo. Vols. I and II. Medical Investigator, 1878 to 1878. 19 290 Wisconsin Academy of Sciences, Aris, and Letters. REPORT OF THE COUNCIL. Since the last report of the Council, on February 138, 1876, the Academy has lost by death the following members: James H. Eaton, Ph. D.,,for many years Professor of Chemistry in Beloit College, and one of the most valuable contributors to the Transactions of the Wisconsin Academy of Sciences, Arts and Letters. A memoir of Professor Eaton, contributed by his colleague, Professor T. C. Chamberlin, will be found at the end of this volume. H. E. Copeland, A. M., Professor of Natural Sciences in the Whitewater State Normal School. No memoir of Professor Copeland has yet been pre- sented. John B. Feuling, Ph. D., Professor of Comparative Philology and Modern Languages in the University of Wisconsin, a memoir of whom, by his col- league, Professor 8. H. Carpenter, will be found at the end of this volume. Stephen H. Carpenter, LL. D., Professor of Logic and English Literature in the University of Wisconsin, whose sudden death has taken place while the last pages of this volume were in press. A brief sketch of his life, taken from the Wisconsin State Journal, will be found at the end of this volume. J. E. DAVIES, General Secretary. LIST OF OFFICERS AND MEMBERS OF THE ACADEMY, 1878, GENERAL OFFICERS OF THE ACADEMY, (Term expires Dec. 27, 1878.) PRESIDENT: Dr. P. R. HOY, Racine. VICE-PRESIDENTS : Dr. 5S. H. CARPENTER, - : - - - MAnDISoN. Pror. T.C. CHAMBERLIN, - - - - BELOIT. Rey. G. M. STEELE, D. D., - - - - APPLETON. How. J. I. CASE, = - = - - RACINE. Rey. A. L. CHAPIN, D. D., - - - - BEnorr. Dr. J. W. HOYT, - - - - - MADISON. GENERAL SECRETARY: Pror. J. E. DAVIES, M. D., Untversity or WISCONSIN. TREASURER: GEO. P. DELAPLAINE, Esq., Mapison. DIRECTOR OF THE MUSEUM: LIBRARIAN: MEMBERS OF THE COMMITTEE EX-OFFICIO: HIS EXCELLENCY THE GOVERNOR OF THE STATE. THE LIEUTENANT GOVERNOR. THE SUPERINTENDENT OF PUBLIC INSTRUCTION. THE PRESIDENT OF THE STATH UNIVERSITY. THE PRESIDENT OF THE STATE AGRICULTURAL SOCIETY. THE SECRETARY OF THE STATE AGRICULTURAL SOCIETY. THE PRESIDENT OF THE STATE HISTORICAL SOCIETY. THE SECRETARY OF THE STATE HISTORICAL SOCIETY. 294 Wisconsin Academy of Sciences, Arts, and Letters. GENERAL OFFICERS OF THE ACADEMY. * Term expires Dec. 27, 1881. PRESIDENT: A. L. CHAPIN, Benorr. VICE PRESIDENTS: Pror. R. D. IRVING, A. M., M. E., = - Mapison. Hon. G. H. PAUL, - = - - MILWAUKEE. G. M. STEELE, D. D.,_ - 2 - - APPLETON. GENERAL SECRETARY: Pror. J. E. DAVIES, A. M., M. D., University otf Wisconsin. TREASURER: Hon. 8. D. HASTINGS, Manison. DIRECTOR OF THE MUSEUM: Pror. G. W. PECKHAM, M. D., MinwavuKeEr. LIBRARIAN: E. A. BIRGE, Pu. D., Manison. * Owing to the unusual delay in the publication of the present yolume of Transactions, it was thought advisable to print the above list ot General Officers of the Academy, who were elected at the Regular Annual Meeting, held at Madison, Dec. 27, 1878. Officers of the Departments. 295 OFFICERS OF THE DEPARTMENTS. Department of Speculative Philosophy. President Ex-Oficio—THE PRESIDENT OF THE ACADEMY. Vice-President —S. H. CARPENTER, LL. D., State University. Secretary — REY. F. M. HOLLAND, Baraboo Counselors — PRESIDENT BASCOM, State University, PROF. O. AREY, Whitewater, and REV. A. O. WRIGHT, Hox Lake. Depariment of the Natural Sciences. President Hx-Oficio— THE PRESIDENT OF THE ACADEMY. Vice-President — PROF. T. C. CHAMBERLIN, Belozt. Secretary — PROF. J. H. EATON, Beloit. Counselors —PROF. W. W. DANIELLS, State University, PROF. J. C.. FOYE, Appleton, and PROF. THURE KUMLEIN, Albion College. Department of the Social and Political Sciences. President Hx-Oficio —THE PRESIDENT OF THE ACADEMY. Vice-President — REV. G. M. STEELE, Appleton. re — a LELAND, Hau Claire. ounselors — DR. E. B. WOLCOTT, Milwaukee, REV. CHAS. CA Lombard, Ili., and PROF. J. B. PARKINSON, Madison. Mes Department of the Mechanic Arts, President Hz-Oficio —THE PRESIDENT OF THE ACADEMY Vice-President — J. 1. CASE, Racine. 3 Secretary — PROF. W. J. L. NICODEMUS, State University. Counselors — CHAS. H. HASKINS, Milhoaukee, HON. J. L. MITCHELL Milwaukee, and CAPT. JOHN NADER, Madison. Department of Letters. President Ex-Officio —THE PRESIDENT OF THE ACADEMY. Vice-President — REY. A. L. CHAPIN, D. D., Belozt. Bee — eee FUNG: State University. ounselors — . W. F. ALLEN, Madison, PROF. EMER‘ } PLO. LC! DRAPHR aici veo) mie ee Department of the Fine Arts. President Hz-Oficio—THE PRESIDENT OF THE ACADEMY. Vice-President — DR. J. W. HOYT, Madison. Secretary — HON. J. E. THOMAS, Sheboygan. POU a R. STUART, MRS. 8S. F. DEAN, and MRS. H. M. LEWIS adison. ; 296 Wisconsin Academy of Sciences, Arts, and Letters. MEMBERS OF THE ACADEMY. LIFE MEMBERS. Case, J. I., Hon., Racine, Wis. Dewey, Nelson, Ex-Governor of Wisconsin, Madison, Wis. Hagerman, J. J., Esq., Milwaukee, Wis. Hoyt, J. W., M. D., Governor of Wyoming Territory. Lawler, John, Esq., Prairie du Chien, Wis. Mitchell, J. L., Hon., Milwaukee, Wis. Noonan, J. A., Esq., Milwaukee, Wis. _ Paul, G. H., Hon., Milwaukee, Wis. Thomas, J. E., Hon., Sheboygan Falls, Wis. Thorpe, J. G., Hon., Hau Claire, Wis. White, 8. A., Hon., Whitewater, Wis. ANNUAL MEMBERS. Adsit, N. H., Mrs., Milwaukee, Wis. Allen, W. C., Hon., Racine, Wis. Alien, W. F., A. M., Professor of Latin and History in the University of Wis- consin. Bartlett, E. W., M. D., Milwaukee, Wis. ' Bascom, John, LL. D., President of the University of Wisconsin. Bashford, R. M., A. M., Madison, Wis. Bate, A. W., Mrs., Milwaukee, Wis. Birge, E. A., Ph. D., Instructor in Zoology in the University of Wisconsin. Bryant, Ed. H., Hon., Madison, Wis. Buck, James 8., Milwaukee, Wis. Bundy, W. F., A. M., Sauk City, Wis. Butler, J. D., LL. D., Madison, Wis. Cass, Josiah E., Eau Claire, Wis. Caverno, Chas., Rev., Lombard, III. Chamberlin, T. C., A. M., Professor of Natural History in Beloit College, and Director of the Geological Survey of Wisconsin. Chapin, A. L., D. D., President of Beloit College, Beloit, Wis. Conover, O. M., A. M., Madison Wis. Daniells, W. W., M. S., Professor of Chemistry in the University of Wis- consin. Members of the Academy. 297 Davies, J. E., A. M., M. D., Professor of Physics in the University of Wisconsin. Day, F. H., M. D., Wauwatosa, Wis. Dean, 8. F., Mrs., Madison. Wis. DeHart, J.N., M D., Madison, Wis. De Koven, James, Rev. Dr., Racine, Wis. De La Matyr, W. A., Spring Green, Wis. Delaplaine, Geo. P., Madison, Wis. Doerflinger, Carl, Mrs., Milwaukee, Wis. Doyle, Peter, Hon., Secretary of State of Wisconsin. Draper, L. C., Hon., Madison, Wis. Dudley, Wm., Madison, Wis. Durand, H.S8., Racine, Wis. Durand, H.S8., Mrs., Racine, Wis. 6 Durand, Frankie, Miss, Racine, Wis. Durrie, D. 8., Librarian Wisconsin State Histurical Society, Madison, Wis. Elmendorf, J. J., 8. T. D., Professor in Racine College. Emerson, Prof., Beloit College, ‘Wis. Falk, F. W., Ph. D., Professor in Racine College, Racine, Wis. Farrar, Chas. A., Prest. Milwaukee College, Milwaukee Wis. Farrar, Chas., Mrs., Milwaukee, Wis. Ford, J. C., Hon., Madison, Wis. Ford, Julia, Mrs., Milwaukee, Wis. Foye, J. C., A. M., Professor of Physics in Lawrence University, Appleton, Wis. Frackleton, Mrs., Milwaukee, Wis. Gapen, Clark, M. D., Madison, Wis. Germain, W. A., Delafield, Wis. Giles, Elia, Miss, Madison, Wis. Gordon, Geo., Milwaukee, Wis. Gordon, Geo., Mrs., Milwaukee, Wis. Gordon, G. E., Rev., Milwaukee, Wis. Gregory, Chas. N., A. M., Madison, Wis. Hailman, W. M., Milwaukee, Wis. Hardy, Albert, Principal High School, Milwaukee, Wis. Haskins, C. H., General Superintendent Northwestern Telegraph Company, Milwaukee, Wis. Hastings, 8. D., Hen., Madison, Wis. Hawley, C. T., Milwaukee, Wis. Henrickson, Peter, Prof., Beloit College, Beloit, Wis. Holland, F. M., Rev., A. M., Baraboo, Wis. Holton, HE. D., Hon., Milwaukee, Wis. Hoy, P. R., M. D., Racine, Wis. Hoy, Jenny, Miss, Racine, Wis. Hutchinson, B. E., Hon., Madison, Wis. Irving, R. D., A. M., M. E., Professor of Geology and Mining Engineering . in the University ef Wisconsin. 298 Wisconsin Academy of Sciences, Arts, and Letters. Jones, Jenk. Ll., Rev., Janesville, Wis. Kenaston, C. A., Ripon, Wis. Kerr, Alex., A. M., Professor of Greek in the University of Wisconsin. King, Chas. I., Superintendent Machine Shop, University of Wisconsin. Kingston, J. P., Necedah, Wis. Kleeberger, G. R., Whitewater, Wis. Kumlein, Thure, Prof., Albion College, Albany, Wis. Lapham, Mary J., Miss, Summit, Wis. Lapham, 8. G., Milwaukee, Wis. Leland, E. R., Eau Claire, Wis. Lewis, H. M., Mrs., Madison, Wis. Lovewell, J. T., Professor in Female College, Milwaukee, Wis. Luther, F.S., Rev., Racine College, Racine, Wis. Mann, Chas., Milwaukee, Wis. Marks, Solon, M. D., Milwaukee, Wis. Mason, R. Z., LL. D., Appleton, Wis. McLaren, W. P., Milwaukee, Wis. McMurphy, J. G., Prof., Racine, Wis. Meacham, J. G., M. D., Racine, Wis. Meacham, J. G., Jr., M. D., Racine, Wis. Merrill, Wm. P., Hon., Milwaukee, Wis. Morris, W. A. P., Hon., Madison, Wis. Nader, John, C. E., Madison, Wis. Nicodemus, W. J. L., A. M., C. E., Professor of Civil and Mechanical Engin-. eering in the University of Wisconsin. Olin, D. A., Mrs., Racine, Wis. Orton, Harlow S., Hon., Judge of Supreme Court of Wisconsin, Madison, Wis. Parkinson, J. B., A. M., Professor of Civil Polity and Political Economy in the University of Wisconsin. Parsons, P. B,, Madison, Wis. Peckham, Geo. W., Professor of Natural Science in the Milwaukee High School, Milwaukee, Wis. Perkins, D. W., M. D., Milwaukee, Wis. Pinney, S. U., Hon., Madison, Wis. Pradt, J. B., Rev., A. M., Madison, Wis. Preusser, Chas., President of Natural History Society, Milwaukee, Wis. Sawyer, W. C., Professor, in Lawrence University, Appleton, Wis. Shaw, Samuel, A. M., Principal High School, and City Superintendent of Public Schools, Madison, Wis. Shipman, 8. V., Chicago, Il. Simmons, H. M., Rev., Kenosha, Wis. Sloan, I. C., Hon., Madison, Wis. Smith, R. B., Attorney at Law, Madison, Wis. Smith, Wm. E., Governor of Wisconsin. Sprague, A. R., Evansville, Wis. Stark, G. A., M. D., Milwaukee, Wis. Members of the Academy. 299 Steele, Geo. M., Rev., D. D., President of Lawrence University, Appleton, Wis. Stuart, J. R., A. M., Madison, Wis. Swezey, G. D., A. M., Professor in Beloit College, Beloit, Wis. Whitford, W. C., A. M., Superintendent of Public Instruction of the State_of Wisconsin. Wilkinson, John, Rev., A. M., Madison, Wis. Willis, Olympia Brown, Mrs., Racine, Wis. Winship, Eugene B., Racine College, Racine, Wis. Wolcott, E. B., M. D., Milwaukee, Wis. Wolcott, Laura J., Mrs., Milwaukee, Wis. Wood, J. W., Baraboo, Wis. Woodman, E. E., Baraboo, Wis. Wright, A. O., Rev., Fox Lake, Wis. CORRESPONDING MEMBERS. Abbett, C. C., M. D., Trenton, New Jersey. Andrews, Edmund, A. M., M. D., Professor in Chicago Medical College, Chicago, I11. Barrow, John W., No. 313 East Seventeenth street, New York city. Bridge, Norman, M. D., Chicago, Ill. Brinton, J. G., M. D., Philadelphia, Pa. Buchanan, Joseph, M. D., Louisville, Ky. Burnham, S. W., F. R. A. S., Chicago, Ill. Byrness, R. M., M. D., Cincinnati, Ohio. Carr, E. 8., M. D., Superintendent Public Instruction, California. Ebener, F., Ph. D., Baltimore, Md. Gatchell, H. P., M. D., Kenosha, Wis. Gill, Theo., M. D., Smithsonian Institute, Washington, 1D. Ce Gilman, D. C., President John Hopkins’ University. Haldeman, 8. 8., LL. D., Professor in University of Pennsylvania, Chickis, Penn. Harris, W. T., LL. D., St. Louis, Mo. Hopkins, F. V., M. D., Baton Rouge, La. ‘Horr, Asa, M. D., President Iowa Institute of Arts and Sciences, Dubuque, Towa. Hubbell, H. P., Winona, Minn. Jewell, J.S.,A. M., M. D., Professor in Chicago Medical College, Chicago, Ill. Le Barron, Wm., State Entomologist, Geneva, New York. Marcy, Oliver, LL. D., Prof., Northwestern University, Evanston, Ill. Morgan, L. H., LL. D., Rochester, Ill. Newberry, J. S., LL. D., Prof., Columbia College, New York. Orton, E., A. M,, President Antioch College, Yellow Springs, Ohio. Paine, Alford, 8. T. D., Hinsdale, Ill. 800 Wisconsin Academy of Sciences, Arts, and Letters. Porter, W. B., Prof., St. Louis,Mo. Safford, T. H., Director of the Astronomical Observatory of Williams College, Williamstown, Mass. Schele, De Vere M., L. L. D., Prof. University of Viriginia, Charlotteville, Va. Shaler, N.S., A. M., Prof. Harvard University, Cambridge, Mass. Trumbull, J. H., LL. D., Hartford, Conn. Verrill, A. E., A. M., Prof. Yale College, New Haven, Conn. Van DeWarker, Eli, M. D., Syracuse, New York. Watson, James C., A. M., Director of the Washburn Astronomical Observa- tory at Madison, Wis. Whitney, W. D., Prof. Yale College, New Haven, Conn. Winchell, Alex., LL. D., Chancelor of Syracuse University, Syracuse, N. Y. HONORARY MEMBERS. Baird, Spencer, F. M. D., LL. D., Washington, D. C. Hamilton, Joseph, Hon., Milwaukee, Wis. NotE— Members of the Academy will confer a favor upon the secretary by communicating to him their full postoffice address, and by giving him timely notice of any permanent change of residence on their part; also by pointing out any corrections needed in the fore- going listz of members. a Members Deceased. 3801 MEMBERS DECEASED Since the Organization of the Academy in 1870. Wm. Stimpson, M. D., Late Secretary Chicago Academy of Sciences, Chi- cago, Ill. J. W. Foster, LL. D., late Professor in the University of Chicago, Chicago il. Died June 29, 1878. Rt. Rev. Wm. E. Armitage, 8. T. D., Bishop of Wisconsin, and for a term Vice President of the Academy of Sciences. Died Dec. %, 1873. Hon. John Y. Smith, Madison, Wis. Died May 5, 1874. Prof. Peter Englemann, Milwaukee, Wis. Died May 17, 1874. I. A. Lapham, LL. D., Milwaukee, Wis. First Secretary of the Wisconsin Academy of Sciences, Arts and Letters. Died Sept. 14, 1875. Hon. A. 8. McDill, M. D., Madison, Wis. Died Nov. 12, 1875. Prof. H. E. Copeland, Whitewater State Normal School, Whitewater, Wis. James H. Eaton, late Professor of Chemistry in Beloit College, Beloit, Wis. Died Jan. 5, 1877. J. C. Freer, late President Rush Medical College, Chicago, Ill. Died April 12, 1877. Thos. Blossom, M. E., School of Mines, Columbia College, New York. Cor- responding member of the Academy. Prof. H. F. Oldenhage, Milwaukee High School, Milwaukee, Wis. J. B. Feuling, Ph. D., late Professor of Modern Languages and Comparatiye Philology in the University of Wisconsin. Died March 10, 1878. J. Wingate Thornton, Boston, Mass. Corresponding member of the Acad- emy. Died June 6, 1878. 8. H. Carpenter, LL. D., late Professor of Logic and English Literature in the University of Wisconsin. Died Dec. 7, 1878. 302 = Wisconsin Academy of Sciences, Arts, and Letters. COMMITTEES OF THE ACADEMY. By-law No. 5, states that there shall be the following Standing Commit. tees, to consist of three members each, when ne other number is specified: 1. On Nominations. 2. On Papers presented to the Academy. 3. On Finance. 4. On the Museum. 5. On the Library. 6. On the Scientific Survey of the State; which committee shall consist of the Governor, the President of the State University, and the President of this Academy. 7. On Publication; which committee shall consist of the President of the Academy, the Vice-Presidents, and the Genera] Secretary. Under this by-law it has been customary to appoint, on the first committee, three members of the Academy present at the beginning of the regular meet- ing, at which the nominations are made. The President and General Secretary of the Academy constitute the second. The committee on Finance, to whom is referred the report of the Treasurer, Consists of three members of the Academy, appointed by the President at the regular annual meeting in February or December. The committee on the Museum at present consists of Professors T. C. Chamberlin, R. D. Irving and J. OC. Foye. The committee on the Library consists of Prof. W. F. Allen, Gen. Geo. B. Delaplaine and Gen. Ed. E. Bryant. CHARTER, CONSTITUTION AND BY-LAWS OF THE ACADEMY OF SCIENCES, ARTS, AND LETTERS, OF WISCONSIN With the Amendments thereto, up to February, 1878. CHARTER. AN ACT TO INCORPORATE THE “WISCONSIN ACADEMY OF SCIENCKHS, ARTS AND LETTERS, The people of the State of Wisconsin, represented in Senate and Assembly, do enact as foliows : Section 1. Lucius Fairchild, Nelson Dewey, Jchn W. Hoyt, Increase A. Lapham, Alexander Mitchell, Wm. Pitt Lynde, Joseph Hobbins, E. B. Wol- cott, Solon Marks, R. Z. Mason, G. M. Steele, T. C. Chamberlin, James H. Eaton, A. L. Chapin, Samuel Fallows, Charles Preuser, Wm. KE. Smith, J. C. Foye, Wm. Dudley, P. Englemann, A. 8S. McDill, John Murrish, Geo. P. Del- aplaine, J. G. Knapp, 8. V. Shipman, Edward D. Holton, P. R. Hoy, Thaddeus C. Pound, Charles E. Bross, Lyman C. Draper, John A. Byrne, O. R. Smith, J.M. Bingham, Henry Betz, Ll. Breese, Thos. 8. Allen, 8. S. Barlow, Chas. R. Gill, C. L. Harris, George Reed, J. G. Thorp, William Wilson, Samuel D. Ilastings, and D. A. Baldwin, at present being members and officers of an association known as “The Wlsconsin Academy of Sciences, Arts and Let- ters,” located at the city of Madison, together with their future associates and successors forever, are hereby created a body corporate by the name and style ot “The Wisconsin Academy of Sciences, Arts and Letters,” and by that name shall have perpetual succession; shall be capable in law of contracting and being contracted with, of suing and being sued, of pleading and being impleaded in all courts of competent jurisdiction; and may do and perform such acts as are usually performed by like corporate bodies. SEcTION 2. The general objects of the Academy shall be to encourage investigation and disseminate correct views in the various departments of science, literature and the arts. Among the specific objects of the academy shall be embraced the following: ~ 1. Researches and investigations in the various departments of the material, metaphysical, ethical, ethnological and social science. 2. A progressive and thorough scientific survey of the state, with a view of determining its mineral, agricultural and other resources. 3. The advancement of the useful arts, through the applications of science, and by the encouragement of original invention. 4. The encouragement of the fine arts, by means of honors and prizes awarded to artists for original works of superior merit 5. The formation of scientific, economical and art museums. 6. The encouragement of philological and historical research, the collec- tion and preservation of historic records, and the formation of a general library. SECON 3. Said Academy may have acommon seal and alter the same at pleasure; may ordain and euforce such constitution, regulations and by-laws as may be necessary, and alter the same at pleasure; may receive and hold real and personal property, and may use and dispose of the same at pleasure ; provided, that it shall not divert any donation or bequest from the uses and objects proposed by the donor, and that none of the property acquired by it shall, in any manner, be alienated other than in the way of an exchange of duplicate specimens, books, and other effects, with similar institutions and in the manner specified in the next section of this act, without the consent ot the legislature. 20 806 Wisconsin Academy of Sciences, Arts, and Letters. Section 4. It shall be the duty of said Academy, so far as the same may be done without detriment to its own collections, to furnish, at the discretion of its officers, duplicate typical specimens of its objects in natural history to the University of Wisconsin, and to the other schools and colleges of the state. : Sxctron 5. It shall be the duty of said Academy to keep a careful record of allits financial and other transactions, and, at the close of each fiscal. year, the president thereof shall report the same to the governor of the state, to be by him laid before the legislature. Sxcrion 6. The constitution and by-laws of said Academy now in force shall govern the corporation hereby created, until regularly altered or re- pealed; and the present officers of said Academy shall be officers of the cor- poration hereby created until their respective terms of office shall regularly expire, or until their places shall be otherwise vacated. Section 7. Any existing society or institution having like objects em- braced by said Academy, may be constituted a department thereof, or be otherwise connected therewith, on terms mutually satisfactory to the govern- ing bodies of the said Academy and such other society or institution. Section 8. For the proper preservation of such scientific specimens, books and other collections as said Academy may make, the governor shall prepare such apartment or apartments in the capitol as may be so occupied without inconvenience to the state. SEcTIon 9. This act shall take effect and be in force from and after its passage. Approved March 16, 1870. Constitution. 307 CONSTITUTION. NAME AND LOCATION. Snorron 1. This association shall be called “The Wisconsin Academy of Sciences, Arts and Letters,” and shall be located at the city of Madison. GENERAL OBJECTS, Section 2. The general object of the Academy shall be to encourage in-. vestigations and disseminate correct views in the various departments of Sci-. ence, Literature and the Arts. DEPARTMENTS. Section 8. The Academy shall comprise separate Departments, not less; than three in number, of which those first organized shall be: 1st. The Department of Speculative Philosphy — Embracing: Metaphysics; Ethics. 2d. The Department of the Social and Political Sciences — Embracing: Jurisprudence; Political Science; Education ; Public Health; Social Economy. - 3d. The Department of Natural Sciences — Embracing: The Mathematical and Physical Sciences: Natural History ; The Anthropological and Ethnological Sciences. 4th. The Department of Arts — Embracing: The Practical Arts; The Fine Arts. oth. The Department of Letters — Embracing: Language; Literature ; Criticism; History. Srction 4. Any branch of these Departments may be consti ‘ y ) ituted a sec- tion; and any section or group of sections may be deennded into a full De partment, whenever such expansion shall be deemed important. 308 Wisconsin Academy of Sciences, Arts, and Letters. Section 6. Any existing society or institution mey be constituted a De- partment, on terms approved by two-thirds of the voting members present at two successive regular meetings of the Academy. SPECIAL OBJECTS OF THE DEPARTMENTS. Sxction 6. The specific objects of the Department of Sciences shall be: 1. General Scientific Research. 2. A progressive and thorough Scientific Survey of the State, under the di- rection of the Officers of the Academy. 3. The formation of.a Scientific Museum. 4, The Diffusion of Knowledge by the publication of Original Contribu- tions to Science. The object of the Department of the Arts shall be: 1. The Advancement of the Useful Arts, through the Application of Sci- ence and the Encouragement of Original Invention. 2. The Encouragement of the Fine Arts and the Iinprovement of the Public Taste, by means of Honors and Prizes awarded to Works of Superior Merit, by Original Contributions to Art, and the Formation of an Art Museum. The objects of the Department of Letters, shall be: 1, The Encouragement of Philological and Historical Research. 2. The Improvement of the English Language. 3. The Collection and Preservation of Historic Records. 4, The Formation of a General Library. MEMBERSHIP. Srctron 7. The Academy shall embrace four classes of governing mem- ‘pers who shall be admitted by vote of the Academy, in the manner to be prescribed in the By-Laws: 1st. Annual Members, who shall pay an initiation fee of five dollars, and thereafter'an annual fee of two dollars. 2d. Members for Life, who shall pay a fee of one hundred dollars. 3d. Patrons, whose contributions shall not be less than five hundred dollars. 4th. Founders, whose contributions shall not be less than the sum of one thousand dollars. Provisions may also be made for the election of honorary and correspond- ing members, as may be directed by the by-laws of the Academy. MANAGEMENT. Srcrion 8. The management of the Academy shall be intrusted to a gen- eral council; the immediate control of each Department to a Department Council. The General Council shall cons'st of the officers of the Academy, the officers of the Departments, the Governor and Lieutenant Governor, the Superintendent of Public Instruction, and the President of the State Univer- sity, the President and Secretary of the State Agricultural Society, the Presi- dent and Secretary of the State Historical Society. Counselors ew-officids, and three Counselors to be elected for each Department. The Department Coun- cils shall consist of the President and Secretary of the Academy, the officers of the Department, and three Counselors to be chosen by the Department. OFFICERS. Section 9. The officers of the Academy shall be: a President, who shall be ew-officto President of each of the Departments; one Vice-President for each Department; a General Secretary; a General Treasurer; a Director of the Museum, and a Genera] Librarian. Section 10. The officers of each Department shall be a Vice-President, who shall be ev-officio a Vice-President of the Academy; a Secretary and such other officers as may be created by the General Council. Constitution. 3809 SEcTION 11. The officers of the Academy and the Departments shall hold their respective offices for the term of three years and until their successors are elected. SecTion 12. The first election of officers under this Constitution shall be by its members at the first meeting of the Academy. Section 13. The duties of the officers and the mode of their election, after the first election, as likewise the frequency, place and date of all meet- ings, shall be prescribed in the By-Laws of the Academy, which shall be framed and adopted by the General Council. SEcTION 14. No compensation shall be paid to any person whatever, and no expenses incurred for any person or object whatever, except under the authority of the Council. RELATING TO AMENDMENTS. Section 15. Every proposition to alter or amend this constitution shall be submitted in writing at a regular meeting; and if two-thirds of the mem- bers present at the next regular meeting vote in the affirmative, it shall be adopted. AMENDMENTS TO THE CONSTITUTION. Amendment to Section 3: “ The Department of the Arts shall be hereafter divided into the Department of the Mechanic Arts and the Department of the Fine Arts,” Passed February 14, 1876. 810 Wrsconsin Academy of Sciences, Arts, and Letters. DB WSEAN iS: ELECTION OF MEMBERS. 1. Candidates for membership must be proposed in writing, by a member, to the General Council and referred to the committee on Nominations, which committee may nominate to the Academy. A majority vote shall elect. Hon- orary and corresponding members must be persons who have rendered some marked service to Science, the Arts, or Letters, or to the Academy. ELECTION OF OFFICERS. 2. All officers of the Academy shall be elected by ballot. MEETINGS. 3. The regular meetings of the Academy shall be as follows: On the 2d Tuesday in February, at the seat of the Academy; and in July, at such place and exact date as shall be fixed by the Council; the first named to be the Annual Meeting. The hour shall be designated by the Secretary in’ the notice of the meeting.- At any regular meeting, ten members shall con- stitute a quorum for the transaction of business. Special meetings may be called by the President at his discretion, or by request of any five members of the General Council. Amended at Racine, July 10, 1878, as follows: The regular Annual Meeting of the Academy, shall be held as follows: On the last Wednesday and Thursday in December, at the seat of the Acad- emy; and the regular Semd-annual Meeting shall be held in July, at such time and place as shall be determined upon at the previous regular Annual Meet- ing in December. The hour shall be designated by the Secretary in the no- tice of the meeting. Special meetings may be called by the President or the General Secretary, at their discretion or by request of any five members of the General Council. DUTIES OF OFFICERS. 4. The President, Vice-President, Secretaries, Treasurer, Director of the M useum and Librarian shall perform the duties usually appertaining to their respective offices, or such as shal? be required by the Council. The Treas. urer shall give such security as shall be satisfactory to the Council, and pay such rete of interest on funds held by him as the Council shall determine. Five members of the General Council shall constitute a quorum. COMMITTERS. 5, There shall be the following Standing Committees, to consist of three members each, when no other number is specified: On Nominations. On Papers presented to the Academy. On Finance. By-Laws. 311 On the Museum. On the Library. On the Scientific Survey of the State; which Committee shall consist of the Governor, the President of the State University and the President of this Academy. On Publication; which Committee shall consist of the President of the Academy, the Vice-Presidents, and the General Sec- _ retary. MUSEUM AND LIBRARY. 6. No books shall be taken from the Library, or works or specimens from the Museum, except by authority of the General Council; but it shall be the duty of said Council, to provide for the distribution to the State University and to the Colleges and public Schools of the State, of such duplicates of typical specimens in Natural History as the Academy may be able to supply without detriment to its collections. ORDER OF BUSINESS. %. The order of business at all regular meetings of the Academy or of any Department, shall be as follows: Reading minutes of previous meeting. Reception of conations. Reports of officers and committees. Deferred business. New business. Reading and discussion of papers. SUSPENSION AND AMENDMENT OF BY-LAWS. 8. The By-Laws may be suspended by a unanimous vote, and in case of the order of business a majority may suspend. They may be amended in the same manner as is provided for in the Constitution, for its amendment. ° . pa i 4