74 A f= eA Ss Ges] 4 P REW, id TY Neer omrs7) i] AEF aren Oy PSY ER WeGibsonelovit Ss a ia “7 ele > ~ =i ie j Vs Z Wee Hert ATU uh Vit. / ch} AYA! A) a LOU i‘ i ri 4 1H yma Hed Daan L i AMAR Bt, Ki BOON Bs Wo) pt ‘ iin ti i mah My eal 5 7 oe » i ae ee 7 = = , Ser oe en en ae fe Se : Bae en rn Ns Ii A Bila ih 5 ee ee gl) ml a a Redline aa - — ‘ ee } Hydrographic Map of /TURKEY LAKE, XE WAWASEE, KOSCIUSKO CO.,INDIANA. BY CHANCEY .JUDAY, From overnmenf surveys and Surveys and gS,made during the summer of 1895, by _ ’JubaAy,D.C.RipGLEY and THomaAs LarRGce = Be, ahr peel cS | UNIVERSITY BIOLOGIGAL STATION. 4 | T INDIANA UNIVERSITY BIOLOGIGAL STATION, Hydrographic Map of” TURKEY LAKE, OR LAKE WAWASEE, KOSCIUSKO CO.,INDIANA. BY CHANCE .JUDAY, From The Government surveys and surveys and teat 18) 7 5 soundings,made during the summer of 1895, by CHANCEY Jupay, D.C.RinGLeEY and THOMAS LaRGE Contributions from the Zoblogica/ Laboratory of the Indiana University under the direction of CARL H EIGENMANN,No /5¢ SYRACUSE Stara STATION) |ao\ Sg 4 8 Senle 110560 Vertical Senile ___ GROSS SECTIONS re) 10-60, BorToM coxrours Scale of Depths OP RLEVaTION Lixe | omen SSA cr tA swore % sPRIXG i —— now 3-69, KET OC DEETH fa OCEEDINGS OF TH Indiana Academy of Science “~~ Pat ca re BRA R ~~ oe 9 } | 895 P4 NEW YORK e ate ROTANI e 6 7 » 2 MH 2. "ARES EMTPOR, = 94) . A. WALDO. ASSOCIATE EDITORS: J. C. ARTHUR, W. A. NOYES, C. H. EIGENMANN, A. W. DUFF, V. F. MARSTERS, A. W. BUTLER, W. S. BLATCHLEY. INDIANAPOLIS, IND., FEBRUARY, 1896. > ie INDIANAPOLIS: ‘Wo. B. BURFORD, PRINTER, 1806. SPAS me wp TAbeeee eONTENTS. AGHioOtiie bublicatonsOn MeO.) shemales s+ =< +), Act for the Protection of Birds, Their Nests and Eggs .. « - Indiana Academy of Science—Its Work and Its Purposes .« . Officarsiand: Committees 1895-6. 9. ..-. we Ue elt Complete List of Officers of the Indiana Academy of Science EOUMITUTULOM Re © awe Ses en Oke Rees lh Ss, ssc eo 6) es wee ele) LCST DES Sa Ue Ge ne en eS Gee a SS. ye nn nr Proceedings of the Eleventh Annual Meeting ........ IBFERIGONtAStFAOGOTOSS oss cco) us ae see ots og CROPS coo aat EERIE LESEU LEC SM Tee ee ears os. kp she se we taieiten ee fe te iw, kp eth er ave ve ie a) ie weed wegen a AN ACT TO PROVIDE FOR THE PUBLICATION OF THE REPORTS AND PAPERS OF THE INDIANA ACADEMY OF SCIENCE. [Approved March 11, 1895.] WHEREAS, The Indiana Academy of Science, a chartered scien- Preamble. tific association, has embodied in its constitution a provision that it will, upon the request of the Governor, or of the several depart- ments of the State government, through the Governor, and through its council as an advisory body, assist in the direction and execution of any investigation within its province, without pecuniary gain to the Academy, provided only that the necessary expenses of such investigation are borne by the State, and, Wuereas, The reports of the meetings of said Academy, with the several papers read before it, have very great educational, industrial and economic value, and should be preserved in permanent form, and, Wuereas, The Constitution of the State makes it the duty of the General Assembly to encourage by all suitable means intellectual, scientific and agricul- tural improvement, therefore, Section 1. Be it enacted by the General Assembly of the State of penton of the re- ; ; raat Sat sO r ports ofthe Ldiana, That hereafter the annual reports of the meetings of the naiana = - ° - = E . 1 ry > va , . meedciiy Indiana Academy of Science, beginning with the report for the year of Science. 1394, including all papers of scientific or economic value, presented at such meetings, after they shall have been edited and prepared for publication as hereinafter provided, shall be published by and under the direction of the Commissioners of Public Printing and Binding. Src. 2. Said reports shall be edited and prepared for publica- Editing oaats tion without expense to the State, by a corps of editors to be selected and appointed by the Indiana Academy of Science, who shall not, by reason of such services, have any claim against the State for compensation. The form, style of binding, paper, typography and manner and extent of illus- tration of such reports, shall be determined by the editors, subject to the approval : of the Commissioners of Public Printing and Stationery. Not less aaa than 1,500 nor more than 3,060 copies of each of said reports shall mean be published, the size of the edition within said limits, to be deter- mined by the concurrent action of the editors and the Commissioners of Public Printing and Stationery: Provided, That not to exceed six hundred dollars ($600) shall be expended for such publication in any one year, and ; not to extend beyond 1896: Provided, That nosums shall be deemed pie to be appropriated for the year 1894. Sec. 3. All except three hundred copies of each volume of said reparts shall be placed in the custody of the State Librarian, who sie pcan shall furnish one copy thereof to each public library in the State, one copy to each university, college or normal school in the State, one copy to each high school in the State having a library, which shall make ap- plication therefor, and one copy to such other institutions, societies or persons as may be designated by the Academy through its editors or its council. The re- maining three hundred copies shall be turned over to the Academy to be disposed of as it may determine. In order to provide for the preservation of the same it shall be the duty of the Custodian of the State House to provide and place at the disposal of the Academy one of the unoccupied rooms of the State House, to be designated as the office of the Indiana Academy of Science, wherein said copies of said reports belonging to the Academy, together with the original manuscripts, drawings, etc., thereof can be safely kept, and he shall also equip the same with the necessary shelving and furniture. Sec. 4. An emergency is hereby declared to exist for the imme- diate taking effect of this act, and it shall therefore take effect and insane tr) be in force from and after its passage. An ACT FOR THE PROTECTION OF BIRDS, THEIR NESTS AND EGGS. [Approved March 5, 1891.] Section 1. Be it enacted by the General Assembly of the State of _. Indiana, That it shall be unlawful for any person to kill any wild mee bird other than a game bird or purchase, offer for sale any such wild bird after it has been killed, or to destroy the nests or the eggs of any wild bird. Src. 2. For the purpose of this act the following shall be con- , sidered game birds: the Anatide, commonly called swans, geese, art 2 brant, and river and sea ducks; the Rallide, commonly known as rails, coots, mudhens, and gallinules; the Limicolz, commonly known as shore birds, plovers. surf birds, snipe, woodcock and sandpipers, tattlers and curlews; the Gallin, commonly known as wild turkeys, grouse, prairie chickens, quail, and pheasants, all of which are not intended to be affected by this act. 6 Src. 3. Any person violating the provisions of Section 1 of this aes act shall, upon conviction, be fined in a sum not less than ten nor more than fifty dollars, to which may be added imprisonment for not less than five days nor more than thirty days. ; Sec. 4. Sections 1 and 2 of this act shall not apply to any per- ee son holding a permit giving the right to take birds or their nests and eggs for scientific purposes, as provided in Section 5 of this act. Penite ko Sec. 5. Permits may be granted by the Executive Board of the Science. Indiana Academy of Science to any properly accredited person, per- mitting the holder thereof to collect birds, their nests or eggs for strictly scientific purposes. In order to obtain such permit the applicant for the same must pre- sent to said Board written testimonials from two well known scientific men certi- fying to the good character and fitness of said applicant to be entrusted with such privilege, and pay to said Board one dollar to defray the necessary expenses attending the granting of such permit, and must file with said Board ae a properly executed bond in the sum of two hundred dollars, signed by at least two responsible citizens of the State as sureties. The bond shall be Rona oe forfeited to the State and the permit become void upon proof that feited. the holder of such permit has killed any bird or taken the nests or eggs of any bird for any other purpose than that named in this section, and shall further be subject for each offense to the penalties provided in this act. Sec. 6. The permits authorized by this act shall be in force for Two years. 3 5s two years only from the date of their issue, and shall not be trans- ferable. Birds of Sec. 7. The English or European house sparrow (passer domes- prey. ticus), crows, hawks, and other birds of prey are not included among the birds protected by this act. Sec. 8 ace arts . Ss > For ass 7 . 7 Mckee Src. 8. All acts or parts of acts heretofore passed in conflict pealed: with the provisions of this act are hereby repealed. Src. 9. An emergency is declared to exist for the immediate Emergency. aes! ; : ee ; oe taking effect of this act, therefore the same shall be in force and. effect from and after its passage. INDIANA ACADEMY OF SCIENCE. (A Statement Made to the General Assembly, in 1895, of Its Work and Purposes.) The Indiana Academy of Science has published during the last three years three volumes of proceedings. The first volume appeared in ’92. It included many of the papers in full or in abstract that were presented at the previous Christmas meeting of the Society, together with titles and authors of all other papers presented before the Academy since its organization in 1885. Of all the titles appearing in this volume, many of them upon topics of vital importance, not over five per cent. were discussed in full in the publication. All the rest of this valuable literature has been scattered and lost or rendered practicably inac- cessible. The volumes appearing in ’93 and ’94 give in full or in abstract most of the important papers presented in each case at the previous holiday meeting, while the volume appearing in the summer of ’94 is enriched by the reports of a large corps of voluntary and unpaid but thoroughly trained workers, who have under- taken and are energetically pushing a systematic biological survey of the State. But the expense attending these publications has been too great for private enter- prise and the treasury of the Academy. Unless the State now takes hold of the matter they must cease for a time, at least, and a serious break in the proceedings must occur. This would be a lamentable check upon the progress of science in the State. At this crisis the State is asked to join hands with the Academy only in so far as to establish and preserve the work to which the latter is dedicated. It is our purpose here to set forth in detail, but briefly, some of the reasons why the State should make this compact. These reasons fall under two general heads: The Workers and Their Work. By publishing the proceedings of the Academy the State secures, without fur- ther compensation, the services of over a hundred trained experts working in fields specially chosen and agreeable, spending a large portion of their time upon new problems whose solution is of vital importance to the development of our Com- monwealth. These workers have been trained in the best schools, home and 8 foreign, and bring to their investigations zeal, enthusiasm, skill, patience and common sense. For the results of their work they seek no other remuneration than the honor that comes from the willing and loving recognition of their labors by their friends, neighbors and fellow-citizens, to whose highest and best interests their lives are consecrated. These trained experts, who constitute the best au- thority in the State upon their several subjects, will act without compensation with the legislative body of Indiana just as the National Academy acts in con- junction with Congress; will freely advise with the legislators when asked upon scientific subjects, and give proper direction to scientific investigations undertaken by the Legislature as a basis for wholesome and logical laws. To the work already done the publications of the Academy give but an im- perfect witness. Certain it is that interest in these proceedings, incomplete as they are, has gone out far beyond the confines of our own States and has been ex- tensively awakened even in transatlantic countries. The Academy has helped to train some of the foremost scientists of our day. When it expresses an opinion upon a scientific subject it is listened to with respect, even by such distinguished scientists as have been drawn in large numbers to our nation’s capital. It will be here attempted to set forth the scope and aims of the Indiana Academy in the barest outlines. The outline itself must be imperfect at best, but we hope this synopsis will show how closely it is identified in all of its ramifica- tions with public progress. Without pretending to exhaust the subject, we will arrange under six heads what we have to say upon the character of the work un- dertaken by the Academy and the reasons why this work should be fostered by the State to the extent of proper publication and dissemination of its results. The six heads are: Educational Services, Development of Natural Resources, Industrial Assistance, Economical Effects, Contributions to the Reputation of the State and Recognition Accorded to This Kind of Work in Other States. We may mention six ways in which the work of the Academy strengthens the educational forces of the State: 1. Through its meetings and publications the Academy gives direction and enthusiasm to the study of the sciences throughout Indiana. Scientific instruction is no longer taken up in a half-hearted, perfunc- tory way, but is instinct with life and energy. 2. It transforms teachers into life-long investigators. The best science teachers are those most under its influ- ence. 3. It fosters and develops workers apart from and outside of the schools. All have observed the tonic effects on a community of a single bright, active mind. With every person thus endowed the Academy joins hands and helps him make a general uplift of his own locality in just such a way as university exten- sion operates. 4. It brings together for conference teachers who are opening up 9 lines of work in their several localities and enables them to plan and distribute original work in the wisest manner. 5. It fosters a spirit of home effort which makes the student of science everywhere practically familiar with home surround- ings and alive to the possibilities of home fields and forests. 6. It classifies and arranges in a systematic way the whole plant and animal life of the State, making accessible at small expense to everybody the most important information other- wise scattered through an expensive library. Without going into details, it is only necessary to call attention to the fact that everywhere the Academy is a powerful auxillary in developing the mineral, vegetable and animal resources of the State. We may consider the industrial activity of the Academy under three heads : Its efforts in behalf of agriculture, of mines and minerals, of manufactures. It aids agriculture by studying and eradicating injurious weeds; by investigating insect life and showing what insects are beneficial, which injurious, and devising means for fostering the former and exterminating the latter; by studying para- sitic fungi, their habits, effects, control; by the investigation and adaptation of soils; by studying birds and animals in their relation to agriculture. It aids mines and mineral industries—by the study of coal, gas, oil, clays, sands, road materials, gravels, building stones, etc.; by application of physics, chemistry and mechanics to mine work; by the application of scientific knowledge of existing conditions, to the end that money should not be wasted in wild-cat- ting and other useless operations. It aids manufacturing industries—by investigating the physical and chemical properties of wood and iron, by perfecting accurate and economical methods of manufacture and testing; by stimulating and laying the foundations for the devel- opment of inventions which shall convert a given amount of power into the maxi- mum amount of useful product; by investigating and devising economical methods of developing and distributing power; by preventing the expenditure of money upon unscientific and useless inventions. We may group the general economical services of the Academy under three ‘heads: 1. It strives to increase the possibilities of existing properties—by improving the soils; by the study and culture of fish; by developing new soil products, such as the sugar beet, or by investigating the conditions under which they flourish; by utilizing neglected food materials, such as mushrooms, ete.; by discovering prac- tical and beneficial uses for waste products; by studying the uses of woods, clays, etc. in the arts and manufactures; by studying the medicinal properties of 10 plants; by studying the properties of plants injurious or fatal to man or beast, as the stagger-weed. 2. It strives to increase the happiness, safety and productive capacity of society by investigating food adulteration, drainage, water supply, sanitary ques- tions; by investigating the effects of mineral and vegetable poisons upon man and. animals; by studying the diseases of animals; by investigating general econom- ical and social problems. 3. It studies the question of the protection of forms of life beneficial to man, such as forests, native birds, game and fishes. In general, we may remark, the reputation of a State is a matter of pecuniary as well as sentimental importance. While it is true that the work of the Academy is widely known and its worth acknowledged, while the same is true for other edu- cational forces in the State, yet when all is said, we must confess that we occupy too low a position in the estimation of the scientific world, lower we believe, than our merit as a State deserves. On the other hand, if the State Legislature should cordially recognize the work being done, should encourage investigation along all lines by the method here suggested, as it can at so slight an expense, that act alone of enlightened and far-seeing policy would greatly improve our reputation; it would tend to give tone and character to the State; it would make the strong workers within its borders more patriotic; they would not be so ready when oppor- tunity offers to change their residence to some more appreciative community; it would do much to attract from without first-class ability to assist in making Indi- ana in every respect what her fertility and natural resources intended she should be—a leader among the States of the Union. New York, Connecticut, Wisconsin, Illinois, Minnesota, Iowa, Kansas and the National Government, together with the foremost foreign States and nations, are more or less committed to the policy advocated. Its results in Indiana can not be different from those achieved elsewhere. Its adoption can only inure to the great and lasting benefit of Indiana and all her people. The amount annually needed to publish in a proper manner, illustrate and distribute the proceedings of the Society will not exceed $2,000. The Academy: does not ask a direct appropriation of money, but an annual publication of its proceedings. As shown by its constitution, the objects of the Academy “‘shall be scientific research and the diffusion of knowledge concerning the various_departments of science.” El The membership is limited only by the following clause: ‘Any person engaged in any department of scientific work, or in original re- search in any department of science, shall be eligible to active membership.” The membership now numbers 146, of whom 25, known as Fellows, are supposed in a special manner to represent the Academy in its relations to the general public. In order that the general character of the Academy may be clearly under- stood, the list of Fellows with their addresses is appended : Daniel Kirkwood, Riverside, Cal.; J. C. Arthur, Lafayette; P. S. Baker, Greencastle; W. 8. Blatchley, Indianapolis; J. C. Branner, Palo Alto, Cal.; A. W. Butler, Brookville; J. L. Campbell, Crawfordsville; John M. Coulter, Lake Forest, Ill.; Stanley Coulter, Lafayette; H. T. Eddy, Minneapolis, Minn.; C. H. Eigenmann, Bloomington; W. F. M. Goss, Lafayette; Thomas Gray, Terre Haute; O. P. Hay, Chicago, Il].; H. A. Huston, Lafayette; J. P. D. John, Greencastle; D. 8. Jordon, Palo Alto, Cal.; V. F. Marsters, Bloomington; T. C. Mendenhall, Worcester, Mass.; D. M. Mottier, Bloomington; W. W. Norman, Austin, Texas; W. A. Noyes, Terre Haute; W. P. Shannon, Greensburg; Alex. Smith, Chicago, Ill.; W. E. Stone, Lafayette; M. B. Thomas, Crawfordsville; L. M. Underwood, Greencastle; T. C. Van Nuys, Bloomington; C. A. Waldo, Greencastle. OFFICERS, 1895-96. PRESIDENT, STANLEY COULTER. VICE-PRESIDENT, THOMAS GRAY. SECRETARY, JOHN S. WRIGHT. AssISTANT SECRETARY, A. J. BIGNEY: TREASURER, W. P. SHANNON. EXECUTIVE COMMITTEE. STANLEY COULTER, Amos W. BUTLER, T. C. MENDENHALL, THOMAS GRAY, WA; Noyes, JOHN C. BRANNER, JoHN S. WRIGHT, J. C, ARTHUR, Ji 2: Di vionn A. J. BIGNEY, J. L. CAMPBELL, JoHn M. CovuntTEr, W. P. SHANNON, OS SP: Ebay, Davin S. JoRDAN. CURATORS. OMVAUN ast s bicge since ic aie Cee Es he ah EEN parte J. C. ARTHUR. TORREY © OG Nesey se ata near eer ae ee ele C. H. EIGENMANN. HERPETOLOGY i MAMMALOGY ..Amos W. BuTuLer. ORNITHOLOGY . I BIN ROMO WO GING wr oe, Peak Ee eee eee W. S. BLATCHLEY. COMMITTEES, 1895-96. PROGRAM. C. A. WALDO, A. J. BIGNEY, MEMBERSHIP. C..H. E1GENMANN, GEORGE A. TALBERT, G. W. Brenton. NOMINATIONS. W. A, Noyes, W.. E.. Stone, W. S. BLatTcHLEY. AUDITING. W. E. STone. STATE LIBRARY. W. A. Noyes, A. W. BurLer, A. W. DvFr, J. S. WRIGHT. C. A. WALDO, LEGISLATION FOR THE RESTRICTION OF WEEDS. J. C. ARTHUR, J. M. Courter, J. S. WRIGHT. PROPAGATION AND PROTECTION OF GAME AND FISH. C..H. EIGENMANN, A. W. Burier, Pu. KrIrscu. EDITOR. C. A. Waxpo. DIRECTORS OF BIOLOGICAL SURVEY. C. H. EIGENMANN, VY. F. MARstTERS, RELATIONS OF THE C. A. WALDo, J. C. ARTHUR. ACADEMY TO THE STATE. A. W. BUTLER, C. H. EIGENMANN. GRANTING PERMITS FOR COLLECTING BIRDS. A. W. BurLer, C. H. EIGENMANN, Wie eR: DISTRIBUTION OF THE PROCEEDINGS. A. W. BuTLer, W. A. NOYEs, C. H. Ercenmann, V. F. MARSTERs, SHANNON. C. A. WALDO. J. S. WRIGHT. 14 ‘uouUvYS ‘dq “AA ‘uouuRYys “dM ‘MoUURYg “d “AN ‘OPIEM. “V “OD ‘OPIEM “V ‘0D ‘suIyuar ‘A ‘O ‘suryuay “gf “O ‘suryuay “gq ‘OQ ‘suIyUua “d ‘O ‘suryuar’ “q ‘O SUIUAL “TO “Aaa OSVAYT “Lousiq aie “V7 ‘Aausig *f °V “URTUION “AA “AA “UBTUION “MM | ‘Taypnoy Aopurqg f ‘AUVLAMOAG “LSSV VYSL MA “SG uyor qUSlIAy “GS ugor BC BUPA evi) ‘lepng ‘AQ soury ‘apn “AA soury ‘TapNg “AA soury ‘raping ‘AQ soury “apn “AQ soury ‘Lopng *A\ soury ‘raping “A, soury ‘lapng “A\ soury “RY V LAOS “Taypnoy Aapurqyg TON “MV ‘S@A0N “V "M qnyiaty “OD £ ‘Teqdmey "T '¢ ‘ABH ‘d ‘O ‘[[eyuepuey “fy “L ‘ouuBag “) uyOs TUNTROVE AGE al TE ‘Taq NOY "Ww uyor ‘URpdOLr "g prAaeg 9-G68T CTH68T P-68T &-G68L G-1681 I-068T 06-6881 6-888T S-Z88T Z-988T 9-C881 “ING CISad “AONATIOS JO AWAAVOV VNVIGNI AHL AO SHAOIMAO CONSTITUTION. ARTICLE I. Section 1. This association shall be called the Indiana Academy of Science. Src. 2. The objects of this Academy shall be scientific research and the diffusion of knowledge concerning the various departments of science; to promote intercourse between men engaged in scientific work, especially in Indiana; to assist by investigation and discussion in developing and making known the material, educational and other resources and riches of the State; to arrange and prepare for publication such reports of investigation and discussions as may fur- ther the aims and objects of the Academy as set forth in these articles. Whereas, the State has undertaken the publication of such proceedings, the Academy will, upon request of the Governor, or of one of the several depart- ments of the State, through the Governor, act through its council as an advisory body in the direction and execution of any investigation within its province as stated. The necessary expenses incurred in the prosecution of such investigation are to be borne by the State; no pecuniary gain is to come to the Academy for its advice or direction of such investigation. The regular proceedings of the Academy as published by the State shall become a public document. ARTICLE II. Section 1. Members of this Academy shall be honorary fellows, fellows, non-resident members or active members. Sec. 2. Any person engaged in any department of scientific work, or in original research in any department of science, shall be eligible to active mem- bership. Active members may be annual or life members. Annual members may be elected at any meeting of the Academy; they shall sign the constitution, pay an admission fee of two dollars, and thereafter an annual fee of one dollar. Any person who shall at one time contribute fifty dollars to the funds of this Academy, may be elected a life member of the Academy, free of assessment. Non-resident members may be elected from those who have been active members 16 but who have removed from the State. In any case, a three-fourths vote of the members present shall elect to membership. Applications for membership in any of the foregoing classes shall be referred to a committee on application for mem- bership, who shali consider such application and report to the Academy before the election. Sec. 3. The members who are actively engaged in scientific work, who have recognized standing asscientific men and who have been members of the Academy at least one year, may be recommended for nomination for election as fellows by three fellows or members personally acquainted with their work and character. Of members so nominated a number not exceeding five in one year may, on recommendation of the Executive Committee, be elected as fellows. At the meet- ing at which this is adopted the members of the Executive Committee for 1894 and fifteen others shall be elected fellows, and those now honorary members shall become honorary fellows. Honorary fellows may be elected on account of special prominence in science, on the written recommendation of two members of the Academy. In any case a three-fourths vote of the members present shall elect. ARTICLE III. Section 1. The officers of this Academy shall be chosen by ballot at the annual meeting, and shall hold office one year. They shall consist of a president, vice-president, secretary, assistant secretary, and treasurer, who shall perform the duties usually pertaining to their respective offices, and in addition, with the ex-presidents of the Academy, shall constitute an executive committee. The president shall, at each annual meeting, appoint two members to be a committee which shall prepare the programmes and have charge of the arrangements for all meetings for one year. Sec. 2. The annual meeting of this Academy shall be held in the city of Indianapolis within the week following Christmas of each year, unless otherwise ordered by the executive committee. There shall also be a summer meeting at such time and place as may be decided upon by the executive committee. Other meetings may be called at the discretion of the executive committee. The past presidents, together with the officers and executive committee, shall constitute the Council of the Academy, and represent it in the transaction of any necessary business not specially provided for in this constitution, in the interim between general meetings. - Sec. 3. This constitution may be altered or amended at any annual meeting by a three-fourths majority of attending members of at least one year’s standing. No question of amendment shall be decided on the day of its presentation. 17 BY-LAWS. 1. On motion, any special department of science shall be assigned to a cura- tor whose duty it shall be, with the assistance of the other members interested in the same departmient, to endeavor to advance knowledge in that particular de- partment. Each curator shall report at such time and place as the Academy shall direct. These reports shall include a brief summary of the progress of the department during the year preceding the presentation of the report. 2. The president shall deliver a public address on the evening of one of the days of the meeting at the expiration of his term of office. 3. No special meeting of the Academy shall be held without a notice of the same having been sent to the address of each member at least fifteen days before such meeting. 4. No bill against the Academy shall be paid without an order signed by the president and countersigned by the secretary. 5. Members who shall allow their dues to remain unpaid for two years, hay- ing been annually notified of their arrearage by the treasurer, shall have their names stricken from the roll. 6. Ten members shall constitute a quorum for the transaction of business. MEMBERS. FELLOWS. Jig Co Amur. 5-00 ss Soe epee AO tee chee eet meee ee Lafayette. PSS DH aer> 2. Sc anigt ote heels deme e clo Seas ae hele Greencastle. eho aie LEY sata. top eck, tae ko. ae Smee Indianapolis. BER EDS ATIMOL ache. cq fees, Pe ey as oe oa aa Se eS Palo Alto, Cal. Wino welBryanyke tenet rate tee aekie ce eee Bloomington. INGA Wy (BUG ns heat. cccs a, Bae e oe oO «eee tite ae eiaee Brookville. Rab. Callies Ss s-ck! jarenGh rer bre remicseueeaer Snr ..Cincinnati, O. Spit. Carn belli cSt eine one & ett eine shoe Crawtordsville. John M. Coulter..... eS Pte Orth ema 3, 2 Lake Forest, Ill. StanleysCowlter-iccck att): cre erie bas or Oke as Lafayette. DS WreDennis een. oer eee eee cc ae eerie io iter Richmond. OES Bugeniaamite * . cos eee te ee ns eee ele ee Bloomington. Katherme BinGoldenersse ate te eee eee ieee: Lafayette. A Voce ded Ra G10; eck ae a re ae ee st ts his cot Lafayette. JUICER G ath ee Read ode chic Gaagr asm Aaa oe 4 ons Sarecri.< Terre Haute. AGE Se EM ait ln Wet VR ae Sole ss cians Tee ae lte) hoteles rere Terre Haute. 0 Yo) 2A & Ey eee cn dP ree A ere tos paar rb Si soles Chicago, Ill. EAS EMISuOn se tee oe oe eras ote Sere eee neat Lafayette. ips) Ben) DS EE IG) teers ke lop ety ek eke Beaigso Ae can lead) ESIC Greencastle. Dyas Shedd Roirae 2) chet che tehet t es aretha die Ak a Deca bee kaha Stanford University, Cal. Wer oe Miarsterssertet co ste ce tinqss siete a el oie oie tore eter Bloomington. Oia) Wiig dN) [eC is S acas st lo clene BIS IG RIAE Port Graemed SS So comic Terre Haute. TSO“ Mendenhall ety tare eee a ein oe eee Hoboken, N. J. DMMaMotlion. <2 teas Gece cee cee aes oe ee eer Bloomington. eas oan SO See On ae ne Ian eo ais. acai. sie Seapine via ed ysis ws dace: Tufts College, Mass. ERNE ee Sea a8 i RY ate Oicon,s. co's, sa ois ow Cincinnati, O. ROUEN LEISCR 8 oc co ran ING eyes Sg: nicrei's sn 3 a's Sa ww a Washington, D. C. 2 Devas Geo 20 Bloomington Ee Crown Point. MiemPee SMM AT ES Per AA e SRS of RSS oY Foul Saie es wide Terre Haute. on he TEESE ae ee 2 Oe oR a Fae Indianapolis. EOC MVD ELTON WA LPNS borne) oayora clais eto oo eel oa Indianapolis. PN AANL SW ited ae ESTILO ete Re Sei) aihch p05) oran isl/e siwiers/ «sieves MOOKe’S Hall, SNe EEO EHELOTIS I PEt NESS oo ose ogres ee wis Sed cee we Bloomington, iit WN PEMIABTAES SSI A SEO Bae not ayifeh e owe nies gj v ohesater ciarat aerate Lafayette. PS SRANTEL CERES TAC Mere tc, St Maar Tae cial oan cierno hah shale fate charade eh athe Greencastle. IPAS PE CARN OD MeL Ae AEN Nace BS oct or sth a eee Ae Ft. Wayne. OLE SCI S tic. oe aro Oe aa Indianapolis. Be, Braver ”. See: I Ha ANN oD kt Kee SYS oe Irvington. Seem UPVC ts SS el. oo ee TDs es + se Lafayette, 20 el 38h Sipe Cee cin eae bind o BSS ioe elo. Cloverdale. iINoble(G: Butler’. Sos ee cr k etek eens pce ett Wier nore Indianapolis. Jock, Campbell & gol Micke ete Ge orn asctelesemten et ete Rockville. Bae Ghianslerts ee see 0. (hess terete th ny. castor erorte Bicknell. Bred. iM. ‘Chamberlainw -..ceee hee ceriee cere teeter Bloomington. Ji bred. Clearwaterseae. s-ee reece bil iia ler leleter eter Indianola, Il. Fd. -Clamentsy iy ee ae he oho Genrer bint Washington. LUPO Clb. Gi APES Heinle Soka IOM MOS OA AR a Acchc atc Mankato, Min. MP SO ro wells ne ae Ch as ko ee cle ore eens ee Indianapolis. Gilera, Gin oncoim obo botis cou po mBe + cedap ero no nods sod Hanover. NOV Gramibacks <8 keer uit a aon ts aes Beer Sak Greensburg. indaghie Gunminc ham) ee eter eke tos teaser tet Kirkpatrick. EIS Comming hams. 608 yeas © ee Chicago. Vi DER LE 8 [By Grea rs SRC a Irvington. SeAIBARLIM NORA AY Sarid a5 wana Sa nnd! miciysaneani Indianapolis. RCL CET SA! Cerra) o 6) ris sm when nope ns Se eased Bloomington. RIEU ONeT, Smead oh tas 365s Sgn 4 ee aes eens Logansport. Jo LS 15 TE TOS OR Se eee eee Indianapolis. NEARS EN pierce LIS ris ia, See, Ci TA osds eissenra a ceases Bloomington. (Tos) INOIG Co Sieg a2 ee a Irvington. Pte ANCOR Et anieratd oak oy ss nossa sah Sse se cd ou ae Indianapolis. FARMER RES LESS UP) oP PRU Ohio e acl Seok Adee Sajetnswanes Carmel. SUMUVEHEGE MODAN Say Shere oa 6 oy inv =) 2s eden seb eee Irvington. “TEESE 6 CNN) 2 a Franklin. (CLR ANEEN ISITE aan has odie ONE Ae Bloomington. re ATLe: crypt Jays MAL Sen cosine ores kw so amore wives Bloomington. Dio, \Gac LSHG OTA Swag Oeste) Cae Sener ee Irvington. 12h. TST Cale eats chan +o caret Rage nko OR eae ew Columbia City. LEC ES, RS Owe See Oe ee Bloomington. SEESETALES or teats ets 4 oe Aksoy SSA ps ses oes ose Rensselaer. eine Ie Me -iy MAAR OLS aie pas cand wiles 9 Se oe ad ences Indianapolis. eee MCW eit os wa das eae ote s aj nnens cane Indianapolis. Beene SV OUN ocho MV A505 —o. 2 Eliminating @ by (4) and (5), and inserting the value of ¢, w& lo7 ie 64 2p Np 8 Naty When ¢ is small, a near approximation is xed alae : MeN oe (7) . Supplying this value of y in (6), and solving for 7, An w pl?t? = lt a aa ates 2 aV p7l?t? + 4w l—t)p. (8) Table II gives the value of T calculated by the above formula for mica frames varying in thickness from 0.0013 em. to 0.02067 cm. Mr. Hall in his investigation used glass frames (made of cylindrical glass rods) of the shape indicated in Fig. 3. He deduced for them equations correspond- F085 ing to (6), (7) and (8). He admits, however, that these equations are so compli- cated as to be almost unmanageable, and that the correction is obtained more easily by determining the constants of a frame by using frames of different length and of the same diameter, and again of the same length but of different diame- ters. It is very difficult indeed to make such frames, and to use them after they are made. The chief objections to glass frames may be summed up as follows: The value of y, and hence the correction that must be applied to the maximum weight in order to obtain the true film weight which measures the tension, depends in a very complicated way upon the diameters of the rods of the frame. This correction forms a considerable part of the total maximum weight (see Table I.). Frames can not be made sufficiently rigid and less than 0.03 em. in diameter. Hence the correction is at least ten per cent. of the whole. The frames are difficult to make and they require delicate handling at every stage. With cylindrical end rods the actual length of the film surface is uncer- tain. It occurred to me that these troublesome corrections and inaccuracies might be partially avoided by using a different kind of frame. After experimenting with frames of various materials, among which I may mention thin sheet glass, platinum, aluminum and mica, I found that the latter offered decided advantages over glass. The general shape of the mica frame is given in Fig. 4. The frame is supported by a forked glass stem, and the method of using is exactly as with a 7a (pol glass frame. 71 My first frames were made by cutting the mica sheet as it lay under a steel rule upon a piece of plate glass. I afterwards had made two heavy steel plates of the exact shape of the frame desired. The inner surface of each plate was ground plane with emery dust upon plate glass. A sheet of mica was clamped between them and cut to their dimensions. The advantages of frames made in this way are: The steel plates are accurately ground; the frames are correspondingly regular. The mica does not split along the cut edge. The edge is of the same thickness as the plate itself; there is no bur. Very thin frames are easily made, but it is difficult to work with them when they are much less than 0.002 cm. thick. A difficulty experienced with the mica frame, as also with those of platinum and aluminum, is that the fluid does not readily and equally wet all portions of the surface. It has a tendency to collect in drops, rendering the after-weighing uncertain. This difficulty was entirely overcome by roughing the surface (dark- ened in Fig. 4) of the plate near the edge by rubbing very lightly with the finest French emery paper. Both weights could then be taken again and again with a variation of only a few hundredths of a milligram. The advantages claimed for the mica frame are as follows: 1. They are easily made, and do not require careful handling. 2. They are of even thickness, with straight edges and square corners. Hence the film length is not so uncertain as with glass frames. 3. They can be made less than one-tenth of the thickness of a glass frame, reducing the correction correspondingly. Table I gives the relative corrections for glass and mica frames, obtained by determining the maximum weight for a soap solution, and then weighing the film itself. The film weight divided by twice the length of the frame gives the surface-tension. But with many liquids it is impossible to obtain the film weight, as the film breaks immediately after it is formed. The maximum weight can be determined in almost every case, and the film weight by correction. It is evident that a slight error in the value of this correction will he lessened by reducing the total correction, as is done by using the mica frame. TABLE I. Kind of / t i Film Per cent. Frame. Weight. Difference. Glass 2250: 6.346 0.0405 0.39226 0.34100 15 GLE ot eet eee 7.584 0.0510 0.48283 0.40302 19 CE rec fae alee 10.163 0.0620 0.65420 0.53700 21 (GILSES rss Si 7.475 0.0920 0.52480 0.39660 32 MiCav ects. 2: 6.012 0.0030 0.31202 0.30697 1.6 Mica: jets 5.301 0.0051 0.27776 0.27092 2.5 MG GAH! $as 5.140 0.0079 0.27222 0.26260 3.7 4 A fresh solution was used in the last three measurements. 4, The correction varies directly as the thickness of the frame, Fig. 5. Ob- servations with two frames of varying thickness are sufficient to determine the actual film weight and hence the tension. 1 1.0202 fe ae [ou a fie i es a be WE ma — MAXIMUM WEIGHT IN GRAMS = THICKNESS OF MICA FRAME IN CENTIMETERS. es bo i ae we ae 3 a ' ’ 73 5. In the case of thin frames the tension can be determined at once from the maximum weight uncorrected, with results that vary less than do those obtained by the method of capillary tubes. For example, compare Table II with Table III, the latter giving selected results obtained by Quincke by the capillary tube method. ? TABLE II. T by formula. Temperature t w _ we T by equation (8) of Water 21 0.00130 em. 0.98260 g. 0.07396 0.07365 20°.7 C. 0.00190 ~ 0.98420 0.07408 0.07374 20°.7 0.00352 0.98791 0.07437 0.07372 20°.7 0.00516 0.99094 0.07458 0.07365 20°.7 0.00928 0.99991 0.07527 0.07352 20°.8 0.01206 » 1.00592 0.07572 0.07355 20°.8 0.01536 1.01358 0.07630 0.07345 20°.9 0.01828 1.01973 0.07676 0.07339 21°.0 0.02067 1.02468 0.07713 0.07332 21°.0 TABLE IIL. (TEMPERATURE 18°.) Kind of glass. ' eo KN of Age of tube. a ube. Common Jena glass ............. 0.5832 0 hr. 0.07528 Common Jena glass............. 0.5851 24 hrs. 0.07336 Wanlisn tint glass. eS. 0.6390 2 mos. 0.07490 English flint glass. ............... 0.5740 -Ohr. 0.07411 Fusible (soft) Jena glass......... 0.6440 0 hr. 0.07258 Fusible (soft) Jena glass......... 0.9106 12 hrs. 0.07480 6. As yandf?#are small, a small error in the assumed value of / will not appreciably affect the calculated value of T, Eq. (6). y being small, the film is much narrower than with a glass frame. There- fore there is less temperature change due to evaporation from the film surface and less absorption of gases and impurities from the air. 1 Weidemann’s Annalen, No. 5, 1894, p. 14. 74 7. The equations for w and y are not so complex that they can not be used. In Table II are given the values of Z7’deduced by formula (8). It will be noted that the last frame is about sixteen times as thick as the first, yet the greatest difference in these values is but a little more than one part in two hundred. Of the results for the first four frames, the greatest difference is one part in seven thousand. The thicker frames can not be expected to give such consistent results, as the water tends to creep in between the thin layers of which the mica sheet is made up. THE TEMPERATURE COEFFICIENT. Previous determinations of the temperature coefficient of surface tension give results not more consistent than the values obtained for the tension itself. Brunner gives the coefficient as .14 dynes per degree, and Merian as .253 dynes. The latter result is almost double the former. Other observers give intermediate values. In view of these differences, I concluded to make a determination of the temperature coefficient by the mica frame maximum weight method. This investigation is not yet completed, so I shall not go into detail. I am using a Troemner balance, No. 5, easily sensitive to one one-hundredth milligram. The arrangement of the balance and box or closet is very much the same as in Hall’s experiment. Inside the wooden box I have a double-walled tin box, open on the side next the glass door. The space between the walls of the tin vessel (the walls being about two inches apart) may be filled with a bath to regulate the temperature of the enclosure. This temperature is obtained by read- ing three thermometers, placed in different positions. A rotary fan is used to equalize the temperature throughout the enclosure. It is arranged so that the water whose coefficient is to be determined is siphoned in and out of the vessel inside, without opening the door or disturbing the balance. I have tried four methods of regulating the temperature of the enclosure. I “ t ~ Lino 2 sin | wt — tam, =i nS R + R, (6) V oR +R) 24 B? we? and its virtual value — = = : ce (7) V (BR + B,) 2? + Lu? : , s > . =a Lu i which we can represent by the vector OB, lagging tan a degrees behind Biase OA. This armature current will react upon the magnetizing forces due to the constant field excitation, and by virtue of the inductance of the armature will produce an M. M. F. in phase with itself which is represented by the vector NN,, drawn parallel to the current vector from the positive extremity of ON. This armature M. M. F. sets up a cyclic magnetization developing a counter E. M. F. OD, lagging 90° degrees behind the current, and there is a loss of effective FE. M. F. due to the armature resistance that is shown by the short E. M. F. vee- tor in phase with OB,, therefore the total loss of EK. M. F. in the armature will be the resultant of these two vectors or OA,. The effective E. M. F. that over- comes the resistance of the non-inductive external circuit will be the vector A,A, since it completes the E. M. F. triangle on OA and is in phase with the current =3\ + if el. he w i Feng d anne Sita! wt ee ¥ f f at. i = J] ite = ie ; y 1 t \ - ‘- 4 f H o 4 1 ra an ed aa * In consequence of this change the current vector wil! assume the position OB, and the other variable vectors will move to their corresponding positions shown by the subscript letter (c). The current in its new position is not only in advance of the E. M. F. (A-O) at the brushes, but is also in advance of the E. M. F. OA, since it has moved from B, to a maximum value when passing OA, and then de- creased in value.+ 1. See Bedell and Crehore’s Alternating Currents, p. 297. ~~ ae 83 The collector E. M. F., on the other hand, steadily increases as the ‘capacity decreases till it reaches a value AeA much greater than the open circuit E. M. F. of the machine. A resonant effect comes into play here after the capacity of the line neutralizes the inductance of the armature that is very well illustrated by the figure: the line A-A will be a maximum when it passes from A through the center of the circle OAcA,A,O, and will represent the greatest difference of potential that can possibly exist between the brushes so long as R and R, remain un- changed in value. This rise in potential is due to the current being in advance of the vector OA, for the position of the armature M. M. F. vector is also advanced, and NN, increases the total flux in the air-gap instead of diminishing it. The cross-magnetizing action of the armature, however, remains approximately the same. The introduction of capacity into the line causes the inductance E. M. F. of the armature to move to the position D:, and the reactance E. M. F. of the external circuit to decrease through zero and then increasing, assume a position Q-O, considerably in advance of the coilector E. M. F., and 90° in advance of the current OBe. The arrows indicate the relative direction of motion of the vectors as the re- sistance is varied from infinity to zero, or as the reactance is carried from zero capacity to an infinite inductance. By following out a similar line of constructions the effects produced by vari- ations of the armature inductance can be studied, and by successfully varying the resistance, inductance, capacity and freqnency constants, and constructing corresponding diagrams, a large variety of problems involving the simultaneous variation of several terms can be successfully treated. A MetHop or MEAsuRING PERMEABILITY. By A. Wi~MER DUFF. [ABSTRACT.] The most common method of measuring the permeability of iron, or the ratio in which the presence of iron strengthens the magnetic field, is to make a ring of the specimen, cover it with two layers of wire, one connected with a source of current to magnetize the ring, the other with a ballistic galvanometer to measure the quantity of electricity induced in this secondary coil by making or breaking the primary current. The galvanometer is calibrated by means of a straight calibrating coil consisting of a non-magnetic core similarly wound with a primary 84 . and secondary. Then from the various dimensions of the ring and the ealibrat- ing coil as regards number of turns of the primary and secondary, cross-section and length of core, intensity of primary currents and throws of the galvanometer, the permeability of the specimen can be calculated. The objections to the above method are the tediousness of observing the con- stants (about a dozen in all) and making the calculation therefrom, and, further, the inaccuracies involved in assuming the areas of windings and core to be the same, in neglecting the difference in closeness of winding between the inside and outside of the ring, ete. For the last two years the author has recommended the following method to his students. An exact non-magnetic copy of the ring specimen is made in the form of a plaster of Paris cast therefrom. This cast is wound precisely similarly to the iron ring. The permeability is then simply the ratio of the throws given by the iron ring and the plaster of Paris ring on making or breaking equal currents in the primaries. The calculations are thus greatly simplified and the « inaccuracies involved in the above mentioned assumptions are greatly reduced and can be completely eliminated by winding the primaries and secondaries in alternate turns on the core. It is not claimed that by this method the galvano- meter is more exactly calibrated, but it is calibrated under the exact conditions under which the actual measurements on the specimen of iron are made. It is calibrated, in fact, by the actual windings on the ring specimen, the iron core being replaced by a non-magnetic core. With a view to testing the sum total of the errors inherent in the ordinary ring method, simultaneous determinations of the permeability of the same speci- men were made by the two methods. It was found that the total error involved in the use of the ordinary calibrating coil was often large, amounting in some cases to as much as thirty-eight per cent. EMPIRICAL FORMULA FOR THE TEMPERATURE VARIATION OF Viscosity. By A. WILMER DUFF. [ABsTRACT.] A careful determination was made of the viscosity of glycerine between zero and thirty degrees. The method employed depended on Stokes’ formula for the rate of descent of a sphere through a viscous liquid. Several different forms of formula have been proposed for the representation of this temperature varia- tion. It was shown that none of these would apply throughout a wide range of 85. temperature variation. By plotting a curve of the sub-tangent of the viscosity- temperature curve against the temperature, a subsidiary curve was formed which should, in all the types of formula proposed, be a straight line, but which turned out to be a parabola. On determining tHe constants of the parabolic equation and integrating this to obtain the equation of the viscosity-temperature curve, a formula was deduced which represented the experimental results to within the limits of experimental accuracy. This formula was an exponential one, the exponent being the inverse tangent of a linear function of the temperature. Reasons were given for believing that this would represent the temperature variation of the viscosity of any liquid. THe EFrect oF GRAPE-SUGAR UPoN THE CoMPposITION OF CERTAIN FAtT- Propucine BacrerrA. By Ropert E. Lyons. It has been observed by Dr. E. Cramer* and others? in studies upon the com- position of bacteria, that the same micro-organism grown upon Peptom and Grape-sugar Agar-Agar produces in each case different quantities of nitrogenous substances and matter which is soluble in alcohol and ether. In this same direction Ducleaux{ demonstrated that yeast cells grown upon a material containing grape-sugar produced fat, while the same yeast grown upon pure nitrogenous material did not produce fat. To study how grape-sugar affects the quantities formed of nitrogen, ash, fat and matter to be extracted by nieans of alcohol and ether, three varieties of cap- sule bacilli were selected : Pfeiffers’ Capsule Bacillus. | Fadenziehender Capsule Bacillus. | No. 28 Capsule Bacillus. *Dr. E. Cramer—‘‘ Zusammensetzung der Bacterien in ihrer Abhiingigkeit von dem Nihrmaterial.’’ Arch. fiir Hygiene—1é6, 151-191. + Tayosaka-Nishimura—‘ Zusammensetzung eines Wasserbacillus.’’ Arch. fiir Hygiene 18, 318-333. tDucleaux—“ Sur la nutrition interacellulaive.’’ Ann. de l’Institute Pasteur—1889 No. 8, p. 413. | Fadenziehender and No. 28 are forms from the water of the River Lahn, near Mos- bourg. 86 The culture medium employed was a neutral 1 per cent. meat extract, agar agar, with the addition of varying quantities of grape-sugar, 1, 5 and 10 per cent., respectively. The agar was prepared in an autoclave after the method of v. Meyer & Buchner and every care taken in each preparation to obtain as uniform a material as possible. To control the uniformity of the various preparations, estimations were made from time to time of the solids (105° C.) in the nutrient media, for example: 10 ce. 1 % grape-sugar agar = 0.369 grm. Residue. LOvce: \* te aso oe oh LO Ces is i ie tC eg , To grow the organisms agar agar plates were inoculated with a fresh bouillon culture, by means of a roll of thin platinum foil and within a moist chamber placed in the thermostat at 37.°5 C. At the expiration of 48 hours the purity of the culture was controlled and the bacteria-mass carefully removed with a scalpel and dried in a yacuum over sulphuric acid. Dr. F. Smith (1) maintains that the presence of grape-sugar in the culture medium causes an increased production of gas and acids. However, when the drying operation was conducted in the apparatus of Arz- berger & Zulkowsky, connected with a condenser, the presence of acid in the dis- tillate could not be demonstrated. The gas production varied, as the amount of sugar, and the odor of ethylic alcohol was always present, but the odor of the fatty acids was never encountered. That volatile acids are formed during the growth of the cultures, under the conditions given, could not be demonstrated. The material dried finally at 105° C. was subjected to analysis. Estimation of ash: rs ‘* Nitrogen (Kjeldahl N>6.25=nitrogenous substances, cas ‘¢ Ether extract (Soxhelet’s app., 48 hours. ) me ‘¢ Alcohol extract (Soxhelet’s app., 90 hours.) (1) Dr. F. Smith—‘ Bedeutung des Zuckers, in Kultur Medien.” Centralblatt fiir Bact. u. Parait 18, 1-s. 1. 87 1 per cent. 5 per ecnt. 10 per cent. Grape-sugar Grape-sugar Grape-sugar Agar Agar. Agar Agar. Agar Agar. [ X. Sibstess. 22-1: 62.75 58.88 45.88 Ether Extr..... 1.68 3.50 2.67 : Aleohol Extr... 12.17 17.30 29.60 Pfeiffer ........ ; en ey hat 7.16 2.97 3.09 | OMeTotalean vas 83.76 82.65 81.24 fit. Sabsb.. 22. .: 71.51 59.12 46.25 | Ether Extr..... eae 3.84 2.84 No. 28 , Aleohol Extr... 11.39 15.91 22.78 GT ee | Aone: = So 6.51 3.66 4.18 vee (Ss Uc 1 re 93.03 82.53 76.05 eli subst 2.0: - 61.05 44.31 33.25 | Ether Extr..... 1.75 2.24 1.87 : ! Aleohol Extr... 18.40 21.80 27.50 Fadenziehender. 1 Meta ai Sas. 8.09 4.50 3.02 As CG Oba nc. eae 89.29 72.85 65.64 On examination of the table it is seen that a constant decrease in nitrogenous substances of the bacteria-mass accompanies the increasing percent. of sugar in the culture medium. Whether or not the total nitrogen consists in part of albumen-nitrogen, or in part of extract-nitrogen; and, further, if the extracted nitrogenous sub- stances contain a lower per cent. of nitrogen than the albumen of the bacteria, can not as yet be determined owing to the very small amount of material. The increase in the quantity of extract matter goes hand in hand with the increasing per cent. of sugar in the agar agar. For the matter soluble in ether this is true only to five per cent. grape-sugar ; at ten per cent. sugar the maximum production of fat seems to have been attained. In this connection it is interesting to observe the relationship between the ether extract and the ash. A decrease in the ash and an increase of fat corresponds to five per cent. sugar and to ten per cent., vice versa. It might seem that the apparent increase in fat was due wholly or in part to the relative decrease in the ash. It is readily seen that this is not the case by calculating the per cent., exclud- ing the ash; on the contrary, the three forms studied produce more matter soluble in ether and alcohol when they are grown upon media with a high per cent. sugar than when they are grown upon such containing a lower per cent. sugar. 88 Briefly stated the results of the investigation are: 1. The quantity of nitrogenous material is inversely proportioned to the quantity of sugar present. 2. To a certain limit the increase of sugar is accompanied by a decided in- crease in the quantity of fat. At ten percent. sugar the most favorable conditions for fat production ap- pear to be overstepped. 3. Matter soluble in alcohol increases constantly with the increasing per cent. of sugar. A New MernHop FoR THE PREPARATION OF PHENYL-CompouNDs WITH SUL- PHUR, SELENIUM AND TELLURIUM. By Ropert FE. Lyons. The very great similarity between the compounds of sulphur, selenium and tellurium was observed by Frederick Woehler and other chemists of his time. To trace this similarity further I was led to attempt preparing certain bodies to fill up the gaps between the known compounds of the organic radicals, methyl, ethyl and phenyl, with sulphur, selenium and tellurium, C. Chabrie* gives the results of several years’ study of aromatic compounds of selenium prepared after the Friedel-Crafts’ reaction, but this method in my hands did not lead to satisfactory results. On the other hand, the method proposed by Drs. F. Krafft and W. Vorster,t i. e., the replacement of the SO, group in the sulfone by sulphur or selenium : C,H;. SO,. C,H; +S=C,H,. 8. C,H; + SO,. Diphenylsulfone. Diphenylsulfid. was easily carried out and afforded 60-70 per cent. of the theoretical amount. As excellent as this method is for the preparation of sulphur and seleninm compounds, it was nevertheless found, that the sulfohenzid, even after prolonged heating with powdered tellurium, remained unchanged. Tellurium dichloride, Te Cl,, was next prepared in the hope that through its action upon mercury diphenyl, Hg (C,H;)., the diphenyltelluride would be ob- tained according to the following reaction : O,H;. Hg. C,H; +Te Cl, =C,H;. Te. C,H; + Hg€l,. *Ann.de Chemie et de Physique, WI sirie t. XX. p. 202-286 (1890); also, Compt. rend. 109, 182 et 568 (1889). + Berichte der Deutschen Chem. Gesell. 26, 2813. 89 However, the reaction did not take place according to the above equation, but the tellurium and the mercury combined in the final reaction, with the formation of monochlorbenzene. ; (C, H;). Hg+Te Cl,—2C, H,; Cl+ Hg Te. From this change I was led to expect the formation of the desired body, Di- phenyltellurid, by the double decomposition of Diphenyl-mercury, by means of metallic tellurium alone—and the expectation was happily confirmed by experi- ment. (C, H;) Hg+Te,—C, H, Te C, H;+He Te. If tellurium and mercury-dipheny] in the proportions by weight indicated by the equation be heated together in a sealed tube filled with CO, gas, 4-5 hours, at a temperature of 200° Cent., there results a grayish black crystalline mass, sat- urated with a thick, heavy oil. This oil, by extraction with ether and purification by rectification, was found to be Diphenyltellurid, 78 per cent. of the theoretical quantity. Thus I succeeded in preparing the, till then unknown, diphenyltellurid. The method is a general one. Dreher and Otto* studied the action of sulphur upon mercury-diphenyl and were of the opinion that diphenyl-sulphide was formed only at a red heat. However, the corresponding sulphides and telsurides may be obtained with the greatest ease by heating mercury-diphenyl with sulphur or selenium to 200° C. under the conditions given. CampuHoric Acitp. By W. A. Noyes. In a paper presented to the Academy last year two acids, which were called cis-campholytic acid and cis-transcampholytic acid were described. The cis- campholytic acid has now been reduced and a dihydro acid obtained from which thea-brom derivative has been prepared. This, on treatment with alcohclic potash yields the cis-campholytic acid again, thus proving conclusively that the double union in the latter is in the 3 position. CH at; Xylyllic acid, C, H, | CH, 3. has been reduced by means of amyl alcohol CO, H 4. and sodium and the a-brom derivative of the hexahydro acid obtained, was pre- pared. The latter, on treatment with alcoholic potash, does not give either of the * Berichte der Deutschen Chems., Gesell, 2. 543. 90 campholytie acids. This furnishes quite conclusive proof that the formula for camphor proposed by Armstrong* is not correct. CH 15 The preparation of the acid, Cb H, 1 So: H 2. has been undertaken and CH: 3.7 by a study of its derivatives it is hoped to secure proof of the truth or falsity of ‘Collie’st formula for camphorie acid. Note on Mix Inspection. By Gro. W. BENTON. The milk supply of cities is becoming a matter of scientific interest. Formerly milk sophistication consisted of skimming or watering or both. More recently various well authenticated rumors of the employment of chemists in the prepara- tion of adulterants, and the marketing of preparations which enables the creamery to substitute foreign fats for milk fats have caused increased attention and greater care in their examination. The inspector, devoid of scientific skill, relies upon the lactoscope, the lactometer, the hydrometer and the Babcock machine, instru- ments sufficiently accurate and reliable for the cases of skimming and watering for which they were made, but entirely unreliable when taken alone in the detec- tion of the preparations made by chemists for the express purpose of deceiving those using the instruments. In my two years’ experience in the work of milk analysis, abundant evidence ot the untrustworthiness of ordinary inspection came to my notice. Besides the watered and skimmed milk, samples of pure cream, common herd and Jersey milk, were passed upon and pronounced suspicious by the ordinary methods in the hands of the inspector. And, finally, it became necessary, in view of the fab- rications employed, to do away with such tests, and subject everything to a more searching examination, as the only sure way to get at the truth. A cise in point came under my observation in December, 1892, as follows: An inspector brought in a sample of milk which, by his testing instruments, gave evidence of being rich, but the appearance, on close examination, was not in strict conformity with the other indications, and he submitted it for analysis. Results attained were as follows, the data taken from my notes made at the time: A careful physical examination showed the milk to be abnormally thick for milk, but not for cream. 5 "UMOLO Oroeatods yalep furgy 4awoyg -Moppox fury * {ks ym aoring ‘Ulq) ‘[[RuIg BRU EO tate j ee | aot OU a tonS YStystl ‘uryy ncoue ‘ayepnp ‘ayepupun “yuo ‘oyRpnpun ‘oyR[np ‘yusUTMVId OyQRY| “quouruOAd oyIIT WY] -Un A[[BoLued uovd A[[BOLIyUe0TO)-qns “qUdUTMOId A[YYSTIG A[[BVOlL}U90M09 $ J|-uUN A] [RoOLIQVUBDTIOD ‘uouturoid 9]941, y|‘yueutmoid aqyey “AIOJAG LIYoOryy ‘Yoryy PeyMeTI, -Imord ATAQSsITS: “a10Jaq 190 orgy yorgy Oaty V “ “poyeyUr yey “poyeyUr yee *poayepul -9U10S ‘[RO1YAI[[)-9 W OS ‘[BoOTZdTT[ A IY MOULOS [BO1IZAIT [A ‘\yuoutrmoad A[YYSIS \uoututoid A[} GSTS “puryog “aL0jaq 1ayoryy “aLoJoq “aLO0F *a10goq IIUUIg) ory! ‘“pauayoryy APYSUG ioyoryy ‘uryy roy eY|-oq Aoyoryy ‘urgy so9yyRY|Ioyoryy ‘Yory ePIT V *poyeyur *posseidur0o “payey “possoid eo a hace eee woyyed ‘pRoudrT TT Rerearces qRondi[ [Hy -at AYSIS ‘TRoydypA| — -Woo-qns ‘prod TT peyepar onan “MONT “TV1Vaad “SANVIGUIYS *SISNASVXHL “SIUVINOISHA “SOATTIOd "SN TNONDAYND “SINYNNYS “dNOUuy SHAUVd AHL AO SYUMLOVUVHAD) OLAIONdS HHL HO SISTONAS 119 ADDITIONAL NOTE. Since the work on this group of Unios was completed I have had the oppor- tunity to re-examine a carefully prepared paper by Mr. Chas. T. Simpson on the “‘Unionide of Florida.” I must dissent from some of the conclusions Mr. Simpson reaches, though in the main he is, beyond question, correct. That author places Unio lepidus Gould and Unio trossulus Lea in the parvus group. Both these shells are here out of place. Unio trossulus has the fine concentric undulations on the umbones which are so characteristic of many Unios typified by Unio fallax, Unio lienosus et cetera. Both Lea’s figure and his description do not permit that this form go into the present group. The character of the radiation, as given by Mr. Simpson in his very poor outline figure of Unio lepidus places it elsewhere, for if there is any such thing as a characteristic in the parvus group its radiation, when present, is very remarkable and quite uniform. There is no doubt that Unio trossulus and Unio lepidus are synonyms. The paper of Mr. Simpson is to be com- mended as marking a distinct advance in the study of the southern representatives of this great family. It appeared in volume XV of the Proceedings of the United States National Museum, 1892, and should be in the hands of every student of Unio. The proofs of this article reached me when consultation of my library on one or two points suggested by careful re-reading was impossible. The synonymy of Unio parvus should have included the following: Unio singleyanus Marsh. Ephemerally described in the Joliet Weekly, a newspaper of Illinois, May, 1891. See also the ‘‘ Nautilus,” Vol. V, p. 29; Simp- son, ‘‘Notes on Florida Unionide,” Proc. U. S. Nat. Mus., Vol. XV, pp. 426, 497. pl. LX VIII, figs. 4, 5 (1892). Without doubt a synonym for Lea’s Unio marginis, itself a southeastern representative of Unio parvus. Plate lL. SEVELC: del. ex Gonvad e& Lea CALL, ON PARVUS GROUP OF UNIO. Plate II. Sree ial ey. Vien. CALL, ON PARVUS GROUP OF UNIO. Plate HL. OREERG: ae\. ex NSE CALL, ON PARVUS GROUP OF UNIO. Plate IV. foe oe eee CALL, ON PARVUS GROUP OF UNIO. Plate V. Gir 3 Y REC. deicer Lana et CALL, ON PARVUS GROUP OF UNIO. Plate VI. REC. Le\ oc ex, CALL, ON PARVUS GROUP OF UNIO. 126 THE FISHES OF THE MissourrI River Basin. By Barron W. EVERMANN AND J. T. ScoveEtu. In 1892 and again in 1893 Dr. Evermann made extended investigations in Iowa, South Dakota, Nebraska and Wyoming for the purpose of selecting a site for a fish-cultural station somewhere in that region. In 1891 he had made similar investigations in Montana and Wyoming and primarily for the same purpose. While engaged in this work we examined a great many streams and made large collections of fishes representing a great many localities. Studying these collections very naturally led to a consideration of the entire fish-fauna of the Missouri basin, and it is with some of the interesting features of this fauna that the present paper deals. That we may understand more clearly the distribution of the fishes a few words concerning the characteristic features of the basin may not be out of place. The Missouri River Basin. ‘The Missouri is the longest river in North America. Its headwaters are among the Rocky Mountains of Montana, Wyoming and Colorado. At numerous places its sources are but a few miles from those of the Saskatchewan, the Columbia and the Colorado. In northwestern Montana are the sources of Milk River which are said to be connected directly with those of the Saskatchewan, while only a few miles to the westward the drainage is into Flathead River and thence into the Columbia. In southwestern Montana the headwaters of the Big Hole, Beaverhead, Red Rock and Madison on one hand closely approach those of the Bitter Root, Salmon and Snake on the other, In northwestern Wyoming, just south of the Yellowstone National Park, the head- waters of the Columbia and Missouri actually unite in Two-Ocean Pass, forming a continuous waterway from the mouth of the Columbia to that of the Mississippi.* In Wyoming the Sweetwater, a tributary of the North Platte, and in Col- orado the South Platte, rise within a few miles of streams which are tributary to the Colorado of the west. The headwaters of these various tributary streams are 8,000 to 14,000 feet above sea level. (allatin, Montana, where the Jefferson, Madison and Gallatin rivers unite to from the Missouri proper is 4,132 feet altitude, the sources of Madison River are over 8,300 feet above the sea, while Two-Ocean Pass is about 8,200 feet. *Fora full description of this phenomenon and its bearing upon the distribution of fishes see Evermann, in Popular Science Monthly, for June, 1895. 127 The mouth of the Missouri. River is about 400 feet above sea level; the total .all of this river is over 7,000 feet, or 3,732 feet between Gallatin and the Mississippi. The length of the Missouri proper is given as 3,000 miles; add to this the length of Madison River and we have 3,230 miles, which may properly be regarded as the total length of the Missouri. Among the important tributaries may be named Milk River; Jefferson Fork, 140 miles; Gallatin Fork, 170 miles; Yellow- stone River, 1,100 miles; Platte River, 1,250 miles (including the North Platte); and the Kansas River, 900 miles (including the Smoky Hill Fork). The area drained by this great river is given as 518,000 square miles. This includes the entire State of Nebraska, all of South Dakota, except a few square miles in the northeast corner; nearly all of Montana, North Dakota and Wyoming, about half of Kansas, more than half of Missouri, and large parts of Iowa and Colorado. The Missouri basin may very properly be divided into three parts, viz., the western or mountainous, the middle or plains portion, and the eastern or region of deciduous trees. The mountainous belt includes western Montana, northwestern and central Wyoming, and a small portion of central Colorado. This includes the portion with an altitude of about 4,000 feet or over, and is the region uf coniferous for- ests and swift, clear and cold mountain streams. The middle belt includes most of northern and eastern Montana, a part of eastern Wyoming and Colorado, and, excepting a narrow strip along their east- ern edge, all of the Dakotas, Nebraska and Kansas. This is, in its general features, a broad, level plain, with slight irregularities here and there. It is a region without forests, and over much of its surface not much vegetation of any kind is found. The only timber of any importance is the narrow strip of cotton- woods and willows covering the bottom lands along the streams. The western and central portions of this belt are very barren, in places even desolate, particu- larly in the Bad Lands, or Mauvais Terre of South Dakota, and parts of North Dakota, Wyoming, Montana and Nebraska. These tertiary beds are of great thickness, usually full of alkali, and very easily eroded. The Black Hills constitute a mountainous island of evergreen forests and beautiful, clear, cold streams in this desert plain, but need not concern us in the consideration of the basin as a whole. The eastern part of this belt receives more moisture and is a typical prairie region, but its streams are slow, shallow and shifting, still carrying much solid matter in suspension from the region to the westward. ' The third or eastern belt embraces a narrow strip along the eastern border of South Dakota, Nebraska and Kansas, and the portions of Iowa and Missouri lying 128 within the Missouri basin. This is essentially a region covered with forests of deciduous trees. It is true that some parts of it are prairie, but the soil contains little or no alkali, and the small streams having their rise in it are fairly clear and pure. In the mountains at the headwaters of the various tributary streams there is an abundance of rainfall in summer and snow in winter; as a rule the mountains were originally heavily timbered and the moisture was therefore conserved and fed out slowly during the season of drought. This is still true in general, but the reckless destruction of the forests in many places is having its effect upon the streams. After leaving the mountains the tributaries of the Missouri, with scarcely an exception, enter the broad treeless plain of the middle belt. Here the alkali soil erodes easily, the current becomes slower, the bed broadens, the channel shifts from year to year, and the water becomes warmer and often of the consistency of thin soup. This is the character of all the larger streams as they pass through this middle belt, and the character of the water is the same in all the smaller streams which start in this belt. The Missouri Basin as a whole, however, is a country whose soils erode with unusual ease and, after getting out of the mountains and upon the plain, few of the streams are ever really clear The Missouri River is always carrying vast amounts of solid matter in suspension and justly deserves the name ‘‘ Big Muddy.” The channels of the Missouri and all the larger tributaries are constantly chang- ing and shifting the beds of the streams. THE FISHES OF THE MISSOURI RIVER BASIN. All this, of course, has its effects upon the fish fauna of this river system. Each of the three belts possesses a fish fauna differing very materially in the aggregate from that of each of the other belts. The total number of species and subspecies of fishes now recognized from the entire Missouri basin is 143. These are distributed among 24 families and 68 genera. The families with large numbers of species are: The Cyprinidae, with 50 species. The Percidx, with 20 species. The Catostomidae, with 16 species. The Centrarchide, with 12 species. The Siluride, with 10 species. 2 129 Only 10 species are characteristic of the western belt, the most characteristic ones being the cut-throat trout, Williamson’s whitefish, the blob, the grayling, the long-nosed sucker, Jordan’s sucker, and the western dace. Only 45 species are known from North Dakota, Montana, Wyoming and Colorado. On the other hand, Missouri and the small part of Iowa drained by the Missouri, furnishes 94 species, or, if we include the narrow timbered and abundantly watered strip of eastern Kansas, Nebraska and South Dakota, we have about 100 species occurring in this eastern or lower belt of the Missouri Basin. The middle belt has such characteristic species as Platy,obio gracilis, .Hybopsis gelidus, Hybognathus nuchalis evansi, and the like. Few if any of these are confined to this belt, but they probably all extend more or less into the lower and upper belts. In the lower portion of the middle belt is found the limit in the western extension of spiny-rayed fishes. West of the 96th meridian, which is approxi- mately the eastern boundary of Nebraska and the Dakotas, not over a dozen species of spiny-rayed fishes are known to occur. This fact becomes interesting when we recall that a single small creek in Indiana (Bean Blossom Creek, Monroe County*!, is known to contain not fewer than thirty-five species of spiny- rayed fishes, and from the streams of Indiana alone we know at least fifty-one species of that group—nearly as many as’the total number of species found in the entire fish-fauna of the Missouri basin west of the 98th meridian. In the Missouri itself and in its larger tributaries are found such large river species as Polyodon spathula, Scaphirhynchus platorynchus, Leptops olivaris, Ictalurus punctatus, species of Ictiobus, and the like; but in the smaller streams Catostomus, Hybognathus and Notropis are the principal genera represented. Micropterus, Perca, Lepomis, and Etheostoma are not rare on the eastern edge of this region, but they become more and more rare as we go westward and very soon disappear altogether. Perca has not yet been found west of Mitchell, S. D., 98° west; Micropteus has not been found west of Ravenna, Neb., 98° 30’ W., and it is not likely that it occurs naturally even that far west. Of the four darters whose range extends farthest west in this basin, Boleosoma nigrum reaches only to Mitchell, S. D., Hadropterus aspro to Ewing, Neb., 98° 20/ W.. Etheostoma iowae extends still further west, having been found by us at Valentine, Neb., 100° 30’ W., while Boleichthys exis, a somewhat doubtful species, was found even a little farther west in North Dakota. The Flat-headed Chub is pre-eminently the characteristic fish of the shallow, alkali streams of the middle Missouri basin, and shows better than any other the “ Bigenmann and Fordice, Proc Phil. Acad. Sei. 1885. G 130 peculiar bleaching effect of the alkaline waters of that region. The fishes are all reduced to a nearly uniform pale or faded appearance. Except those found in the headwaters above the alkali, they seem to be almost wholly without pigment cells of any kind. Perhaps the most extreme case of bleaching is that of Platygobio gracilis, which, of all American fishes, seems to be the one most perfectly adapted to life in these alkaline streams. An examination of the literature shows that seventy-four nominal species have been described as new from Missouri basin localities. These seventy-four names represent fifty-one species as now understood, but all but twenty-eight of the seventy-four nominal species had already been described, so only twenty- eight of them were really new. Indeed, we are inclined to think that a little closer investigation will show at least eleven of these twenty-eight to have been not new, so that of the seventy-four fishes which have been described as new from the Missouri basin only seventeen, or about 23 per cent., were really so. TABLE GIVING NAMES OF DESCRIBERS OF MISSOURI BASIN FISHES, THE NUMBER DESCRIBED BY EACH, AND THE NUMBER OF EACH WHICH STILL HOLD. No. of No. AUTHORS. Species Which Described.) Still Hold. NCES VAN a eRe NG TEN Ae Tees Oey ORAS SNe Hee Ryan clea cl ANC 3 1 AUT OL oy ys tee oa aes ea TC ER RAIS oe ee 4 0) Cope ised Oe Sabl eee ee CE RE CER Cte Oem aati 21 8 LD OTer 1 ll Dai ee et Sin eR Piet MARAE Siero? 70 be oe arate autre rte, hens 3 0 TO RSSV ETOAC 01 Re AL Soe a aN eats ot eh ek alt) 35S oe ee eRe Fe 1 1 Everman sand © Omers eee ees Soe ees, cae ae ee 2 2 Gilbert 43.0. & ee ie ee Serene ene AP aes 2 1 (GATT rs Sere ore su hckeeRe SRO RAT AEE ee eR Oe eee 2 1 Seat LI ee oY eA SO SS ar ART Pe SR NRE Pld CAO an ree oan 5 1 Garand eon) Aces Peete eget cee Ren eer Sa a ee Oc 20 8 Vaya econeseyis eke sates: ie Maines cll aah ROT Re CCE Us LR as 3 0 Jordans... Save Se ee eee oT ene te eters 4 1 Jordanvand: Wyermanns, i. feo Eee eo eiee cine one ] 1 Mee ee crits oes suerte cesta e roots vcs oh Suey Neen oR ae es OPEN oma ed 2 2 Mialliner 5.2.00 Jaye Pee BA SNE tae One 1 1 Tr Galle ec Wanctn evoke Ga ee ote eae eich tte eee e 74 28 131 REcENT INVESTIGATIONS CONCERNING THE REDFISH, ONCORHYNCHUS NERKA, AT ITs SPAWNING GROUNDS IN IDAHO. By Barton W. EVERMANN AND Jie8: SCOVELL. _, Of the 130 or more families of fishes now recognized as constituting the fish- fauna of North America, the one of greatest and most general interest is the Sal- monidae, the family to which belong the whitefish, the salmon, and the trout. Whether we consider beauty of form and color, activity, gaminess, quality as food, or abundance and size of individuals, the different members of this family stand easily with the first among fishes. Confined to the north temperate and arctic regions, they abound wherever suitable waters are found. In North America alone no fewer than sixty-two species are found. Some of these species are confined to the smaller rivers and running brooks, entering lakes or the sea as occasion serves, but not habitually doing so. Such are some of the species of trout of the genera Salvelinus and Salmo. Others again are lake fishes, approaching the shores or entering the trib- utary streams only at spawning time and then retiring again to deeper waters. These are the whitefishes and lake herrings. Then there is another gronp made up of species that are marine and anadro- mous, living and growing in the sea, but entering fresh waters at spawning time. Such are the five species of salmon of our west cvast. From California to northern Alaska and across to Kamchatka are found five species of true salmon of the genus Oncorhynchus, viz.: 1. The Hump-back salmon, O. gorbuscha, 2. The Dog salmon, O. keta, 3. The Silver salmon, O. kisutch, 4. The Blue-back salmon, O. nerka, and 5. The Chinook salmon, O. tschawytscha. The most interesting and by far the most important of the five are the Chinook and the Blue-back; and it is to the last of those two species that this paper is devoted. In Kamchatka and Alaska this species is known as the Red salmon and is commercially worth more than all the other salmon of Alaska combined. It here ranges in weight from five to eight pounds, and in late summer and early fall they enter the rivers and lakes of Alaska in myriads at spawning time. In the Columbia River it is called the Blue-back salmon and, next to the Chinook, is the most valuable fish of that river. 132 The Blue-backs enter the Columbia along with the Chinooks early in the spring, the height of the run being in the month of June; and the catch in the lower Columbia amounts to several hundred thousand fish annually. Such as escape the labyrinth of nets, traps and wheels which for miles literally fill the lower Columbia, pass on to their spawning grounds. We do not yet know just where all their spawning grounds in the Columbia basin are located, but we do know that there are important ones in the inlets of Wallowa Lake in Oregon, and Payette Lake and the Redfish Lakes in Idaho. It was not, however, until 1894 that any naturalist visited these lakes at the spawning time and made any study of the spawning habits. In September of that year we made a brief visit to Alturas and Pettit lakes and Big Payette Lake, where we found this salmon spawning. Big Payette Lake is situated near the head of Payette River about 120 miles northeast from Weiser, Idaho. Alturas and Pettit lakes are two of a group known as the Redfish Lakes, lying among the eastern spurs of the Sawtooth Mountains, forty-five to seventy-five miles northwest from Ketchum, Idaho, the nearest railroad station. These Redfish lakes are really the headwaters of Salmon River, the principal tributary of the Snake, und their distance by water from the sea is more than a thousand miles. The investigations of 1894 showed that the vicinity of those lakes afforded excellent facilities for studying the habits of the salmon which spawn there, and it was decided to visit them again in 1895. It should be here stated that the Blue-back salmon which enter the Columbia River are no longer known by that name when they reach their spawning grounds, but are known as Redfish. When they enter the river from the sea they are a clear, bright blue above and silvery on the sides, but when they reach their spawning grounds they have become more or less red, especially the males, which are often a bright scarlet red on the back and sides, the head being a light olive- green. At these Idaho lakes two forms of the Redfish have long been known to occur, a large form weighing four to eight pounds and corresponding to the regular Blue-backs taken in the mouth of the Columbia; the other is a small form weighing almost invariably a half pound each and not corresponding to any salmon ever taken in the lower Columbia. Structurally it does not appear to differ from the large form in anything except size, and the two forms are regarded as being specifically identical. But a number of questions concerning this fish were veiled in more or less obscurity, among which may be mentioned the following : 135 1. Do the Redfish which spawn in the inlets of the Idaho lakes really come up from the sea, and when do they first arrive ? 2. During the spawning season the Redfish are observed to have their fins more or less worn or frayed-out and to have sores upon the body. Are these mutilations received on the spawning grounds, or are they injuries incident to the long and perilous journey from the sea? 3. What are the habits of the Redfish during spawning time ? 4. What becomes of them after done spawning? Do they return to the sea, to the lakes, or do they all die? In order to answer as many of these questions as possible, it became at once evident that an extended series of observations at one of the lakes would be necessary. A camp was therefore established at Alturas Lake last summer on July 20, and the observations begun then were carried on continuously until September 24. Alturas Lake is situated at an altitude of 7,200 feet, between two immense glacial moraines extending downward from the eastern spurs of the Sawtooth Mountains. It is about two miles long, four-fifths of a mile wide, and has a maximum depth of 158 feet. Its inlet is a small mountain stream about eight miles long, and thirty feet wide at the mouth. The outlet of Alturas Lake is somewhat larger, and after flowing through Perkins Lake (a small lake about a half mile below) enters Salmon River Valley. After a course of about five miles to the northeast, Alturas outlet joins Salmon River. Just above the lake on either side of the inlet tower extremely rugged mountains whose peaks are 9,000 to 11,000 feet above the sea, and the scenery is as wild as any to be found in America. In order to study the Redfish effectually, we set gill nets in the outlet and in the inlet and examined them from day to day. The nets in the outlet would tell us when the fish arrive from below on their way to the spawning grounds. The nets in the inlet would tell us when the fish run up out of the lake to their spawning beds, and also whether they return to the lake after done spawning. Without going too much into detail, it will suffice to say that daily observa- tions of the lake, outlet and inlet, were made, and the nets, though not kept continuously set, were so regulated as to assist in solving as many as possible of the problems involved. Not a single Redfish was ever caught in any of the nets in the outlet. If they come up from the sea, they had reached Alturas Lake before July 20, when our nets were set. 134 On July 24 four small Redfish were caught on the net in Alturas inlet, and in a day or two they were abundant in this stream. Evidently, therefore, they had entered the lake at some date prior to July 20, and had remained in it until the evening of July 23 when they first entered the inlet. Beginning with July 23 the fish continued to enter the inlet until early in September. During this time at least 2,000 Redfish, only about a dozen of which were of the large form, entered this small creek. Hundreds of these were ex- amined as they were running up into the inlet from the lake, and not one of them showed any sores, frayed-out fins, or mutilations of any kind. Toward the close of the spawning season there was scarcely a fish whose fins were not more or less worn out (frequently the caudal was entirely gone) and whose back or sides were not sore. And we were able to see how these mutilations were received. : During the spawning period there is a rather definite pairing off of the sexes. The spawning beds are usually in very shallow water on a bottom of fine gravel and sand. While spawning, this gravel and sand is moved about a good deal and made up into so-called nests, both sexes taking part in the work. The gravel is moved about by the fish striking it with the tail, or by pushing against it with the lower fins, or sometimes even with the dorsal fin and the back. The gravel is moved by a rapid, quivering movement of the body as the fish swims over the nest; then she circles around down stream a few feet and approaches the nest to repeat the act again. The male follows closely behind the female, and frequently moves the gravel in the same way. The fish move about to some extent in the inlet, but there is no evidence that they ever try to return to the lake. Our nets caught a good many from the upper side, but they were nearly all dead or dying fish which had been carried down by the current, and were only slightly gilled or simply lodged against the upper side of the net. We saw no evidence whatever indicating any tendency to return down stream, and it is not easy to believe that any fish, so seriously mutilated as these all are at the end of the spawning season, could suryive. On September 5 we counted about 1,000 fish in Alturas inlet; two weeks later all had died but about 150, and a week later practically all had died. We consider it, therefore, absolutely proved that the Redfish which spawn in the inlets of the Idaho lakes spawn only once and then die, and that the mutila- tions are received on the spawning beds. 135 A New Habitat FoR GASTROPHILUS. By A. W. BittTinc. The genus Gastrophilus contains two well known species, Gastrophilus equi and Gastrophilus haemorrhoidalis. These parasites are commonly known as bots and inhabit the stomach and duodenum of the horse. The life cycle is as follows: The female deposits her eggs upon the ends of the hairs upon the fore limbs or some other part of the body that the horse is likely to touch with his mouth in fighting flies. The eggs hatch and the lid breaks open to permit their escape in from five to fifteen days. They attach themselves to the lips or tongue when the host is fighting flies and soon find their way into the stomach or interior part of the duodenum. Here they pass a period of development lasting about seven months. Their food consists of the nutri- ment found in solution in the juices of the stomach. They escape from the body with the excrement, pass a pupa state in the ground to emerge in a short time as adult. The particular observation to be recorded here is the finding of this parasite in the alveoli of the horse’s teeth. Last September there were an unusual number of cases of caries of the teeth at the clinics. While extracting teeth six larvae were obtained attached to the tissues of the teeth or alveolar cavity. They were alive and active. They were about three centimeters from the surface of the gums and there was no visible point for entrance. The question remains how did they get to their destination and how did they accommodate themselves to take nutriment from the blood when it is believed that they are dependent upon the juices of the stomach? Are they a factor in producing caries of the teeth? SEcoND CONTRIBUTION TO A KNOWLEDGE OF INDIANA Motuusca. By R. ELLs- WORTH CALL. The sources of information on which the facts stated in this brief paper are based are various. No single source has availed largely in determining the locality references that are given, though the collection in the Geological Museum, in the State Capitol, has furnished the greater number. All the rest have been contributed by specimens submitted through several gentlemen practically inter- ested in the work of the biological survey of the State. For this aid thanks are 136 due W. S. Blatchley, State Geologist; Dr. J. T. Scoville, Terre Haute High School; Dr. C. H. Eigenmann, State University, Bloomington; Mr. Harry Dodge, Charleston, Indiana, and Mr. Charles Dunn, Chicago. The specimens which have been seen are mainly the most common forms. In some few cases they have been found to be widely distributed over the State; others are, apparently, confined to the Ohio and its principal tributary stream, the Wabash. North of the divide that separates the Ohio and lake drainages fewer forms of Unionide occur, but the limnwid fauna appears to represent both an increased number of individuals and of species. The land shells of the Ohio drainage are both more abundant and varied. But no really final generalizations can yet be ventured in the absence of extended collecting and large numbers of shells—a condition which the present activity of members in this branch of the State’s biological survey indicates to be very remote. The facts collected for the year past are the following: LAND Monuusca. Mesodon albolabris Say. Charleston, Terre Haute, Indianapolis, New Albany. Mesodon clausus Say. Vigo County, Indianapolis, Peru. Mesodon: elevatus Say. Terre Haute, Indianapolis, Corydon. Mesodon exoletus Binney. Vigo County, Indianapolis. Mesodon multilineatus Say. ; Terre Haute, Indianapolis. Mesodon profundus Say. Charleston, Indianapolis, Terre Haute. Mesodon thynoides Say. Vigo County, Indianapolis, Charleston. Patula alternata Say. Vigo County, Charleston. Patula solitaria Say. Vigo County, Charleston. Patula perspectiva Say. Vigo County. Patula striatella Anthony. Vigo County. 137 Zonites arboreus Say. Vigo County, Bloomington, Charleston. Zonites ligerus Say. Vigo County. Zonites guiaris Say. Charleston. Zonites fuliginosus Griffith. Gibson County. Triodopsis fallax Say. Vigo County, Indianapolis. Triodopsis inflecta Say. Charleston, Vigo County. Triodopsis appressu Say. Vigo County, Indianapolis. Triodopsis palliata Say. Vigo County. Triodopsis tridentata Say. Charleston, Vigo County. Tebenophorus dorsalis Binney. Vigo County. Limax campestris Binney. Vigo County, Turkey Lake. The ‘‘slugs” or shell-less terrestrial mollusks of Indiana are hardly known. Very few collections contain any representatives. Inasmuch as they do not ap- peal to the conchologist and are rather difficult of preservation, requiring alcoholic methods, they have been neglected. They promise useful facts if particular at- tention is directed to their systematic collection. They are to be sought under chips, boards, logs, flat rocks, bark, sidewalks, in cellars and about barns and other outhouses in damp situations. A track of dried mucus will often lead one to their hiding place, if carefully traced. They should receive especial attention from the collectors of the survey. Stenotrema monodon Rackett. Vigo County. Stenotrema hirsutum Say. Vigo County. Macroeylis concava Say. Charleston, Indianapolis, Terre Haute. 138 Suceinea avara Say. Vigo County. Suceinea obliqua Say. Vigo County. FRESH WATER UNIVALVES. Bulinus hypnorum Linneus. Coffee Chute, Gibson County. Limnea caperata Say. Vigo County. Limnophysa humilis Say. Very abundant on marshy banks of the Ohio, in springs at New Albany ; found in 1894 in myriads. Limnophysa reflera Say. Ponds, Vigo County. Physa gyrina Say. Marion County; probably found everywhere in the State; exceedingly abund- ant in pools on the Falls of the Ohio. Helisoma trivolvs Say. Vigo County. Planorbella campanulata Say. Ponds, Vigo County; Lake Maxinkuckee. Pleurocera subulare Lea. Wabash River, Vigo County. Plurocera canaliculatum Say. Very abundant on the Falls of the Ohio; on muddy banks of the Wabash River, at Terre Haute, occurs in myriads. A large number of specimens were collected in October, 1895, at the last named locality, which present a wide range of variation, both in the characteristic grooving of the body-whorl and in coloration. Many specimens occurred without any indication of a groove; in others the angle, which is found along the lower border of the body-whorl, may be sharp, or obtuse, and is fre- quently thickened at intervals, constituting a character that makes a number of specimens approximate Pleurocera moniliferum Lea. Any one of a half dozen species belonging to the pleurocerid group, of which cana- liculatum is a type, might be separated from the material before me. Many thousands of this shell have been taken at the Falls of the Ohio | 139 opposite Louisville. They present a still wider range of variation, per- haps from the character of their habitat. The very wide range of vari- ation suggests some interesting synonymic conclusions that it is hoped will be elaborated during the coming year. Goniobasis pulchella Anthony. : Wabash River, Ohio River at the Falls, Turkey Creek. Widely distributed over the State, and with Goniobasis livescens Menke, ranges farthest north. Goniobasis livescens Menke. Turkey Creek, St. Joseph River. Goniobasis sp. A very great quantity of these small shells were collected by me at the Falls of the Ohio during the past three years, but opportunity to work it up has not yet been afforded. As in the pleuroceroid section, this material promises an abundant synonymy. Lioplax subcarinata Say. Wabash River, Ohio River. Vivipara interterta Say. Wabash River, Gibson County, Lake Maxinkuckee. Vivipara contectoides Binney. Lake Maxinkuckee, ponds along Wabash River. Campeloma decisum Say. St. Joseph River, Lake Maxinkuckee. Campeloma ponderosum Say. Ohio River, Wabash River, ponds in Vigo County. Campeloma rufum Haldeman. St. Joseph River. Campeloma subsolidum Anthony. Peru, Lake Maxinkuckee, White River. The very interesting and very difficult group of shells comprised in Campeloma is probably the least understood and the most abused of any in the North American fauna. At brief intervals some tyro arises to declare his ‘‘ discovery that after all there is but one species,” etc., etc., the latest of these being a writer in the ‘‘ Proceedings of the Iowa Academy of Sciences.” * In this paper the remarkable suggestion is confidently made that ‘‘Mr. Binney’s disposition of these forms is still the best.” Now, Mr. Binney wrote on these mollusks thirty * Proc. lowa Acad. of Sciences, 1893 [1894], p.108. Shimek, “ Additional Notes on Iowa Mollusea.’’ 140 years ago, with poor and scanty materials at his command. He succeeded in involving the group in almost inextricable confusion for nearly a quarter of a century, a result hardly to be wondered at with paucity of material and want of familiarity with fresh water forms. So far from the truth is it that Mr. Binney’s disposition of these forms was wise that, without detracting a whit from his well earned reputation as a student of our terrestrial mollusca, it may be fairly stated that had he left the group severely alone its limitations would sooner and better be reached. As species go, every form listed from Indiana is distinct and is easily separable, no matter how mixed the material may be. The embryonic forms differ; the mature shells differ; their character is obvious to any who will carefully study extensive series. What the specific value of certain forms may eventually prove to be does not in the least affect the general proposition that the group is composed of a number of forms which must be recognized as species. It would, indeed, be a striking commentary on the acumen of American conchologists if, after thirty years, no advance had been made in this group. And this same writer accepts several undoubted synonyms of the cireumpolar Vallonia pulchella Miiller, as good species! CoRBICULAD®. Spherium suleatum Lamarck. Ponds, Vigo County. Spherium striatinun Lamarck. Turkey Creek; Ohio River; Ponds, Vigo County. Spherium transversum Say. Abundant in the Ohio at Charleston. UNIONID.®. * Anodonta edentula Say. Ponds, Vigo County ; Bennett’s Creek ; Wabash River; Cedar Creek ; St. Joseph River. * Anodonta ferussaciana Lea. Bennett’s and Coal creeks, Vigo County; Five Mile Pond, Vigo County; St. Joseph River. Anodonta footiana Lea. : Lake Hamilton; Lake Maxinkuckee. * All names thus marked have Indiana representatives in the State Museum. ut Indian- apolis. —- 141 = Anodonta grandis Say. Fourteen Mile Creek, Charleston; Lake Hamilton; Five Mile Pond, Vigo County; Raccoon Creek. Anodonta imbecillis Say. Bennett’s Creek, Vigo County. Anodonta pavonia Lea. Pond, near Terre Haute; Bennett’s and Coal creeks, Vigo County. Anodonta salmonia Lea. Yellow River; Cedar Creek; St. Joseph River. = Anodonta suborbiculata Say. Wabash River. * Anodonta subcylindracea Lea. Wabash River; Cedar Creek. Anodonta undulata Say. Lake Maxinkuckee. Anodonta wardiana Lea. Fourteen Mile Creek, Charleston. * Margaritana calceola Lea. Wabash River, White River, Turkey Lake. * Margaritana complanata Barnes. Wabash River, White River, Ohio River, Bruiett’s Creek. * Margaritana confragosa Say. Wabash River. * Margaritana dehiscens Say. Wabash River, Ohio River. * Margaritana deltoidea Lea. Lake Maxinkuckee, St. Joseph River. This form is a synonym of Margaritana ca:ceoia Lea. * Margaritana hildrethiana Lea. Wabash River. * Margaritana margmata Say. Wabash River, White River, Ohio River, St. Mary’s River. * Margaritana monodonta Say. | Ohio River, Wabash River. This shell was described, in 1830, from the Falls of the Ohio, by Mr. Say, but was by him regarded as a Unio. Mr. Lea described it the same year as Unio soleniformis. Mr. Lea’s shell is given the indefinite locality ‘‘Ohio,” and the shell probably came from the Ohio River, near Cincinnati. Mr. Say’s name has 142 priority, even though it is now recognized that the species falls in Margaritana rather than in Unio. In habit the species resembles Margaritana dehiscens in that it is often deeply buried in the gravelly banks it affects, in rather swiftly flowing water. Most commonly, however, it may be found buried deeply under large flat rocks, and between clefts in rocky bottoms. It is a rather rare shell in collections. * Margaritana rugosa Barnes. Wabash River, White River, Blue River, Fourteen Mile Creek. * Unio wsopus Green. Wabash River, Ohio River. * Unio alatus Say. White River, Ohio River, Wabash River. * Unio anodontoides Lea. Wabash River, Ohio River, Bruisett’s Creek, Vigo County. * Unio asperrimus Lea. Wabash River, Ohio River, at the Falls; this form is equivalent to Unio lachrymosus Lea. * Unio camelus Lea. Ohio River; this is an old and heavy Unio phaseolus, of which it is a synomym, * Unio camptodon Say. Wabash River, Ohio River. * Unio capax Green. Wabash River, Ohio River. * Unio cicatricosus Say. Wabash River, Ohio River. * Unio circulus Lea. St. Mary’s River, Ohio River, Wabash River, Peru. * Unio clavus Lamarck. Wabash River, very abundant; St. Joseph River. * Unio coceineus Hildreth. Wabash River, Ohio River. * Unio cooperianus Lea. Wabash River, Ohio River. * Unio cornutus Barnes. Ohio River, Wabash River. 143 * Unio crassidens Lamarck. Wabash River, Falls of the Ohio, abundant. * Unio cylindricus Say. Ohio River, Wabash River, White River. These shells, as are indeed most others from the Wabash River, are singularly beautiful and perfect. Even the largest and oldest examples present perfect um- bones, with epidermis and apical crenulations entire. It is rare indeed to find these forms so perfect. Both this species and Unio metanervus, which are charac- terized by peculiar arrow-shaped green color-markings over the whole disk, pre- sent this feature in singular beauty. The State Collection, at Indianapolis, con- tains several well-marked and beautiful specimens. * Unio donaciformis Lea. Wabash River, Ohio River at Falls of the Ohio; found, also, in collections under the name of Unio zigzag Lea. ‘The latter name was given two years after Unio donaciformis was characterized. = Unio ebenus Lea. Wabash River, Ohio River, Falls of the Ohio. * Unio elegans Lea. Wabash River. Ohio River, Falls of the Ohio. * Unio ellipsis Lea. Wabash River, Ohio River, Falls of the Ohio, common. * Unio fabalis Lea. Wabash River. Unio lapillus Say, is a synonym of this form. * Unio fragosus, Conrad. Wabash River, Ohio River, White River. = Unio gibbosus Barnes. Wabash River, Sand Creek, Ohio River, Turkey Lake, Lake Tippecanoe, St. Joseph River, Lake Maxinkuckee, Falls of the Ohio, St. Mary’s River. The white and heavy variety of this shell, called by Dr. Lea, Unio aretior, occurs somewhat commonly in both the Ohio and Wabash rivers. *= Unio glans Lea. Wabash River, White River, Lake Maxinkuckee. * Unio gracilis Barnes. Wabash River, Ohio River on Falls of the Ohio, Muscatatuck Creek, Jen- nings County. 144 * Unio graniferus Lea. Wabash River, Ohio River. * Unio iris Lea. Wabash River, Delaware River, Lake Maxinkuckee. * Unio irrorratus Lea. Wabash River, Ohio River. Very abundant, perfect and beautiful in the Wabash. * Unio lens Lea. See Unio circulus, of which it is a synonym. * Unio ligamentinus Lamarck. Wabash River, Ohio River, Yellow River, Turkey Creek, Delaware River, St. Joseph River. Widely distributed over the State. The most com- mon Unio of our waters, with the possible exception of Unio luteolus. * Unio luteolus Lamarck. i Whitewater River, White River, Wabash River, Ohio River, St. Mary’s River, Turkey Creek, Cedar Creek, Fourteen Mile Creek, Charleston ; Lake Maxinkuckee. * Unio metanevrus Rafinesque. Wabash River, Ohio River. * Unio multiplicatus Lea. Wabash River, Ohio River; a mud-loving form which reaches gigantic size in both these streams. Very large and fine specimens are in the State collection. * Unio multiradiatus Lea. Wabash River, White River, St. Joseph River. * Umno mytiloides Ratinesque. Wabash River, Ohio River. * Unio nigerrumus Lea. Wabash River; a single specimen is in the State collection, labelled correctly as above—though the locality can not be vouched for. Mr. Lea described the form from Alexandria, Louisiana. The collection contains many southern shells and I am inclined to regard this locality reference as an error and to think the shell should not be reckoned as an Indiana form. * Unie obliquus Lamarck. Wabash River, Ohio River; probably the same form Rafinesque called mytiloides. 145 * Unio occidens Lea. Decatur County, Ohio River, Wabash River, Falls of the Ohio, Bennett’s Creek, Vigo County. * Unio orbiculatus Hildreth. Wabash River; Mr. Lea later described the female of this species under the name of Unio higginsii. * Unio parvus Barnes. Wabash River, Ohio River, Creek at Greencastle (Underwood), Lake Maxin- kuckee. Very large specimens of this usually small shell are obtained in the Wabash. So marked is their development that they are commonly known as ‘‘ the big parrus of the Wabash.” * Unio perplerus Lea. Wabash River, White River. Mr. Lea later twice described again this fotm, once as Unio rangianus and then as Unio sampsonii, both the latter from Indiana waters. It has other synonynis, by the same writer, in Tennessee waters. * Unio phaseolus Barnes. Wabash River, Ohio River, St. Joseph River, Lake Maxinkuckee, Fourteen Mile Creek, near Charleston. * Unio plenus Lea. Wabash River. * Unio plicatus Le Sueur. Ohio River, Wabash River. This shell, widely distributed, has a number of synonyms which I have else- where indicated.*+ It is also often confounded with Unio undulatus Barnes, which is, however, a markedly different shell, very much more compressed. * Unio pressus Lea. Sand Creek, Decatur County; Bruiett’s Creek, Vigo County; St. Joseph River, Lake Maxinkuckee. * Unio pustuiatus Lea. Ohio River, Wabash River, White River. *Unio pustulosus Lea. Wabash River, Ohio River. 7 See Trans. St. Louis Acad. Sci., Vol. VII, No.1, pp. 36, 37; 1895. 10 146 * Unio rectus Lamarck. Wabash River, Ohio River; White River, St. Joseph River. * Unio retusus Lamarck. Wabash River. * Unio ridibundus Say. White River, Wabash River. * Unio rubiginosus Lea. Ohio River, Wabash River, Lake Maxinkuckee. * Unio securrs Lea. Wabash River, Ohio River. * Unio solidus Lea. Wabash River. * Unio subovatus Say. Wabash River, Ohio River, White River. * Unio subrostratus Say. Wabash River, Lake Maxinkuckee, Bruiett’s Creek, Vigo County. Wrongly labelled Unio nasutus in the State collection. * Unio sulcatus Lea. White River, Marion County. * Unio tenuissimus Lea. Wabash River, Ohio River. A specimen in the State collection is labelled Unio vellum Say. * Unio triangularis Barnes. Wabash River, White River. * Unio trigonus Lea. Wabash River, Ohio River. * Unio tuberculatus Barnes. Ohio River, Falls of the Ohio. Wabash River. *Unio undulatus Barnes. White River, Ohio River, Wabash River, Bruiett’s Creek, Vigo County. * Unio varicosus Lea. Ohio River. * Unio ventricosus Barnes. Lake Maxinkuckee, St. Joseph River. * Unio verrucosus Barnes. Wabash River, Ohio River, White River. CINCINNATI, OHIO, December 23, 1895. 147 CONTRIBUTIONS TO THE BIioLoGICAL SURVEY OF WABASH County. By ALBERT B. ULReEy. The present paper is intended (1) to indicate the progress made during tke year in listing the fauna and flora of Wabash County, and (2) to give a sum- ‘marized statement of the work already done, thus placing the material collected within access of those interested in special lines. I have included in these lists, with but a few exceptions, only those forms of which specimens were preserved : . J. Tae Fauna: hes - oO. The list of fishes includes forty-two species, seven of which were not noted in the last published report. I have included in the list the Brook Lamprey (Ammocetes branchialis). Several specimens were taken in a creek near North Manchester, about May 15, 1895. Batrachians, 19. a. Salamanders and Water Dog ( Urodela and Proteida), 10. b. Tailless Batrachians (Salentia), 9. Reptiles, 18. a. Snakes (Ophidi), 11. b. Lizards (Lacertilia), 1. ce. Turtles ( Testudinata), 6. Birds. The list of birds includes 186 species. Twospecimens of the Horned Grebe (Colymbus auritus L.) were taken along the roadside November 27, 1895, after a severe storm. This is the first record of the bird in the county. Mr. W. O. Wallace has taken another specimen of the rare Kirtland’s Warbler (Dendroica kirtlandi) at Wabash. It was taken some time in May, 1895. The mammals listed include about twenty species. Il THe Fora: Among Phanerogams the list comprises about 750 species represent- ing eighty-nine families. Only a few of the forest trees are included, 116 species of grasses and twenty-three sedges. About 400 species have been added during the year. The Cryptogams have not been listed, but some valuable material has been collected in certain groups, such as the ferns and some forms of fungi. 148 In the collection of Dr. A. Miller, of North Manchester, Ind., there q are probably 175 species of parasitic fungi and perhaps twenty-five species of the Slime Moulds, if I may, for convenience, still place them among the fungi. Nearly a complete list of the Phanerogams may be found in the herbarium of Mr. John N. Jenkins, North Manchester, Ind., who has done valuable work in collecting these forms. Brrps oF WABASH County. By ALBERT B. ULREY AND WILLIAM O. WALLACE. The present list enumerates 188 species of the birds of Wabash County. Under each species are given notes concerning its abundance and in some in- stances we have incorporated other observations which pertain to the life-history of the species. Most of the work was done at intervals during the years 1890 to 1893. Part of the observations were made in the extreme northern portion of the county in the Eel River valley, near North Manchester. About an equal amount of work was done in the Wabash valley near Wabash, and some observations were made nine miles north of Lagro by Mr. Orrin Ridgley. We have included in the list only those species identified by us, and with only a few exceptions skins of each species have been preserved. We have noted the breeding habits of those species only which came under our own observation. We may expect to find two hundred or more birds within the county. The list is quite complete in warblers, containing 314 species, one of them the very rare Dendroica kirtland:. Perhaps three more would complete the list to be found in the county. We shall probably find Protonotaria citrea, H:lmitherus vermivorous and Geothlypis formosa. The deficiencies in our list are mainly among the water birds. Our only large stream, the Wabash, flows nearly eastward here and is not rich in migrating water birds. The region in the northwestern part of the county, con- taining numerous small lakes, has not contributed many species to our list, be- cause only a few of the rarer birds taken there by the hunters have been iden- tified by us. The Wabash River flows in a northerly direction to Logansport, where it bends abruptly to the east and continues in this direction. through the county. Near Wabash one of the tributaries of the Wabash River flows nearly due south- ward. A heavy growth of timber extends along the stream northward some dis- tance from the Wabash and ends abruptly at a large tract of land under cultiva- tion. During the spring migrations the birds collect in the north edge of this 149 woodland in great numbers. It seems that in their northward migrations along the Wabash River the birds attempt to follow the wooded region of the smaller stream instead of pursuing the eastward course of the Wabash, and on reaching the open fields find themselves in a sort of trap. It was at this place that a large per cent. of the birds inhabiting the woodland were taken. 1. Podylimbus podiceps Linneus. Pied-billed Grebe. Rather common migrant. 2. Colymbus auritus L. Horned Grebe. Two specimens were taken No- vember 27, 1895, after a severe storm. 3. Urinator imber Gunner. Loon. Great Northern Diver. Not infre- quently taken on the lakes. Five or six were taken on the Wabash River near Wabash. 4. Larus argentatus smithsonianus Coues. American Herring Gull. One specimen taken as it flew over the house four miles west of Wabash. The speci- men was taken by Mr. E. Wright and is now in his possession. 5. Larus philadelphie Ord. Bonaparte’s Gull. One specimen taken on Lake Maxinkuckee. It will probably be taken here. 6. Sterna forsteri Nutt. Forster’s Tern. Several specimens were taken on Lake Maxinkuckee. 7. Hydrochelidon nigra surinamensis Gmel. Black Tern. Probably taken here. We have aspecimen from the same place as the last. 8. Phalacrocorax dilophus Sw. and Rich. Double-crested Cormorant. A male and female were taken on Long Lake, November 15, 1890. 9. Merganser americanus Cassin. American Merganser. Not uncommon migrant and winter resident. 10. Lophodytes cucullatus Linneus. Hooded Marganser. Rare. Three specimens taken. 11. Anas boschas Linneus. Mallard. Abundant migrant; sometimes taken in midwinter, and three were killed July 3, 1892, by Mr. E. Wright. Hunters report its breeding, but we have not observed it. lla. Anas obseura Gmelin. Black Duck. One specimen taken at Wabash. 12. Anas discors Linneus. Blue-winged Teal. Only one specimen. It was taken April 15, 1891. 13. Atr sponsa Linneus. Wood Duck. Abundant summer resident. I have taken the young when still unable to fly. Wallace. 13a. Spatula clypeata L. Spoon Bill. Only one specimen taken. Wabash. 14. Aythya afinis Eyt. Lesser Scaup Duck. A specimen was taken on Long Lake, November 15, 1890. 150 15. Charitonetta albeola Linneus. Butter Ball. One specimen from Long Lake. Occasionally killed on Eel River by hunters. 16. Branta canadensis Linneus. Canada Goose. One specimen taken; frequently seen migrating. . 17. Olor columbianus Ord. Whistling Swan. One specimen taken No- vember 15, 1894, on Long Lake. 18. Botaurus lentiginosus Montag. American Bittern. Several specimens known to have been taken. 19. Botawrus evilis Gmelin. Least Bittern. Two specimens taken, April 19 and May 1, 1894. 20. Ardea herodius Linneus. Great Blue Heron. Common summer resident. 21. Ardea egretta Linneus. American Egret. A specimen taken just be- yond the north line of Wabash County, in Kosciusko County. ; 22. Ardea virescens Linneus. Green Heron. Abundant summer resident. Breeds. 23. Nycticorax nycticorax nevius Bodd. Black-crowned Night Heron. Two specimens taken. One at North Manchester and one at Wabash. 24, Rallus virginianus Linneus. Virginia Rail... One specimen taken at Rock Lake, in Fulton County just across the line, September 1, 1894. 25. Porzana carolina Linneus. Carolina Rail. Not infrequently taken by hunters. 26. Fulica americana Gmel. American Coot. Abundant migrant. 27. Philohela minor Gmel. American Woodcock. Not very common. 28. Gallinago delicata Ord. Wilson’s Snipe. I took a specimen January 1, 1892, and the same winter two were killed between December 25th and January 1 by a friend of mine. I have seen them in midsummer. Wallace. 29. Tringa maculata Vieillot. Jack Snipe. Very common during migra- tions, especially in September. It may be found at this time in great abundance along the Wabash River in company with the Solitary Tattler and Killdeer. 30. Tringa minutilla Vieillot. Least Sandpiper. Rare. One specimen taken from a flock of Solitary Tattlers, August 29, 1893. 31. Tringa bairdii Coues. Baird’s Sandpiper. Rare. Only one specimen taken. This is apparently the only record of the bird in the State. [Proc. Ind. Acad. Sci. 1893, p. 118]. r 32. Totanus melanoleucus Gmelin. Greater Yellow-legs. I have never seen this bird except on September 24 and 25, 1893, when I observed a number along the river, three of which I shot. Wallace. 151 33. Totanus solitarius Wilson. Solitary Tattler. Very,common summer resident. Breeds. ; 34. Bartramia longicauda Bechst. Upland Plover. One specimen taken from a flock of three. 35. Aetitis macularia Linneus. Spotted Sandpiper. Very common summer resident. Breeds. 36. -digialites vocifera Linneus. Killdeer. Abundant summer resident. Breeds. 37. Colinus virginianus Linneus. Bob-white. Formerly very abundant, but much less so since the winter of 1892-3, when they were destroyed in great numbers by the severe cold and snow. 38. Bonasa umbellus Linneus. Pheasant. Formerly common, now becoming rare. 39. Tympanuchus americanus Reich. Prairie Hen. Occasionally taken on the prairie region near Wabash. 40. Meleagris gallopavo Linneus. Wild Turkey. Formerly common, now probably extinct. The last one known to have been taken was in 1880. 41. LEctopistes migratorius Linneus. Wild Pigeon. Formerly abundant, but none have been seen recently. 42. Zenaidura macroura Linneus. Turtle Dove. Very common resident. Breeds. 43. Cathartes aura Linneus. Turkey Buzzard. Abundant summer resi- dent. Breeds in hollow logs, trees, ete. 44. Cireus hudsonius Linneus. Marsh Hawk. Rather common about prairie regions. Extremely variable in color. Breeds. 45. Accipiter cooperi Bonaparte. Cooper’s Hawk. Common. Probably our most common injurious hawk. 46. Buteoborealis Gmelin. Red-tailed Hawk. Abundant resident. Breeds. 47. Buteolineatus Gmelin. Red-shouldered Hawk. One specimen taken. 48. Buteolatissimus Wilson. Broad-winged Hawk. Two specimens taken. 49, Falcosparverius Linneus. American Sparrow Hawk. Quite abundant resident. Breeds. 50. Strix pratincola Bonaparte. American Barn Owl. A single specimen taken by Mr. Frank Bell at North Manchester. 51. Asio wilsonianus Less. American Long-eared Owl. A specimen was taken near the north county line. It is in the collection of Mr. M. L. Galbreath. 52. Asio accipitrinis Pallas. Short-eared Owl. Four specimens taken at Wabash and one just north of the county line in Whitley County. 152 53. Syrnium nebulosum Forst. Barred Owl. Quite abundant resident. 54. Nyctala acadica Gmelin. Saw-whet Owl. One specimen taken No- vember 20, 1894. 55. Megascops asio Linneus. Screech Owl. Abundant, both red and gray phases. 56. Bubo virginianus Gmelin. Great Horned Ow]. Abundant resident. Breeds. 57. Nyctea nyctea Linnweus. Snowy Owl. A specimen of this owl was taken near Roann, probably during the winter of 1891-2, another near North Manchester during the winter of 1893 and one in 1894. 58. Coecyzus americanus Linneus. Yellow-billed Cuckoo. Abundant sum- mer resident. Breeds. 59. Coceyzus erythrophthalmus Wilson. Black-billed Cuckoo. One or two specimens taken. Perhaps rather common. 60. Ceryle aleyon Linneus. Belted Kingfisher. Abundant summer resi- dent. Breeds. 61. Dryobates villosus Linneus. Hairy Woodpecker. Abundant resident. 62. Dryobates pubescens Linneus. Downy Woodpecker. Abundant resi- dent. Breeds. 63. Sphyrapicus varius Linneus. Yellow-bellied Woodpecker. Common migrant. a 64, Ceophleus pileatus Linneus. Pileated Woodpecker. Formerly com- mon, but none have been seen recently. 65. Melanerpes erythrocephalus Linneus. Red-headed Woodpecker. Abun- dant, some years resident. Breeds. 66. Melanerpes carolinus Linnzeus. Red-bellied Woodpecker. Abundant resident, more common in winter. 67. Colaptes auratus Linneus. Flicker. Abundant resident. Breeds. 68. Antrostomus vociferus Wilson. Whip-poor-will. Abundant summer resident. 69. Chordeiles virginianus Gmelin. Night Hawk. Common summer resi- dent, more common in late summer. 70. Chetura pelagica Linneus. Chimney Swift. Abundant summer resi- dent. Breeds. 71. Trochilus colubris Linneus. Ruby-throated Humming-bird. Common summer resident. Breeds. On May 19, 1894, two were found dead after a few days cold weather. : 153 72. Tyrannus tyrannus Linneeus. Kingbird. Very common summer resi- dent. Breeds. 73. Myiarchus crinitus Linneus. Crested Fly-catcher. Common summer -resident. Breeds. 74. Sayornis phebe Latham. Pheebe. Abundant summer resident. Breeds. 75. Contopus virens Linneus. Wood Pewee. Very common summer resi- dent. Breeds. ; 76. Empidonax flaviventris Baird. Yellow-bellied Fly-catcher. Not very common migrant. 77. Empidonax acadicus Gmelin. Acadian Fly-catcher. A common mi- grant. ri 78. Empidonax minimus Baird. Least Fly-cateher. Not very common mi- grant. 79. Otocorys alpestris praticola Hensh. Prairie Horned Lark. Resident. Breeds. More abundant during severe cold in winter. 80. Cyanocitta cristata Linneus. Blue Jay. Abundant resident. Very destructive to young birds and eggs. 81. Corvus americanus Aud. American Crow. Abundant resident. Breeds. 82. Dolichonyx oryzivorus Linneus. Bob-o-link. Summer resident. Breeds. Formerly rare or wanting. Becoming more common every summer. 83. Molothrus ater Bodd. Cow bird. Abundant summer resident. 84. Ag-laius pheniceus Linneus. Red-winged Blackbird. Abundant sum- mer resident breeding in swamps. 85. Sturnella magna Linneus. Meadow Lark. Common summer resident and often seen in mid-winter. Breeds. 86. Icterus spurius Linneus. Orchard Oriole. Cormmon summer resident. Breeds. 87. Icterus galbula Linneus. Baltimore Oriole. Probably more abun- dant than the last species. Breeds. 88. Scolecophagus carolinus Mill. Rusty Blackbird. Rather common mi- grant. 89. Quiscalus quiscula wneus Ridgway. Crow Blackbird. Abundant sum- mer resident, sometimes seen in mid-winter. 90. Coccothraustes vespertina Coop. Evening Grosbeak. Two pair were taken just beyond the north county line in Whitley County, one pair of which is in the collection of Mr. M. L. Galbreath, Collamer, Ind. 154 ek 91. Carpodacus purpureus Gmel. Purple Finch. Migrant, not very com- mon. 92. Loria eurvirostra minor Brehm. American Crossbill. Two specimens seen September 11, 1894, in the cemetery at Wabash. 93. Acanthus tinaria Linneus. Redpoll Linnet. Several flocks were seen during the winter of 1889-90. This is the only time they have been noted in the county except a record of the same date by Mr. D. C. Ridgley, nine miles north of Lagro. 94. Spinis tristis Linneus. American Goldfinch. Abundant resident. Breeds. 95. Spinus pinus Wils. Pine Siskin. One shot from a flock of goidfinches which came to feed on the mulleins in our yard January 10, 1892. ( Wallace.) 96. Calearius lapponicus Linneus. Lapland Longspur. This bird was first taken by Mr. Orrin Ridgley in the fall of 1891. At Wabash one was taken in 1892, and during the winter of 1893-94 they were common, coming in September and remaining until March 15. All were in company with Horned Larks. 97. Poocetes gramineus Gmel. Bay-winged Bunting. Very abundant summer resident. 98. Passer domestica Linneus. European House Sparrow. ‘English ’ Very abundant resident. Not so abundant as in 1892. A great many Sparrow.’ were destroyed during the winter of 1892-95. 99. Ammodramus sandwichensis savanna Wils. Savanna Sparrow. Mi- grant, not common. 100. Ammodramus savannarum passerinus Wils. Grasshopper Sparrow. Abun- dant summer resident. Breeds. 101. Chondestes grammacus Say. Lark Sparrow. Not very common sum-, mer resident. Breeds. More common during migrations. 102. Zonotrichia leucophrys Forst. White-crowned Sparrow. Abundant mi- grant, occasionally seen as late as June 10. 103. Zonotrichia albicollis Gmel. White-throated Sparrow. Much more. abundant than the last species. Its peculiar note, once heard, is not readily for- gotten. 104. Spizella monticola Gmel. Tree Sparrow. Abundant winter resident. 105. Spizella socialis Wils. Chipping Sparrow. Very common summer resi- dent. Breeds. : 106. Spizella pusilla Wils. Field Sparrow. Abundant summer resident. Breeds. 155 107. Juneo hyemalis Linneus. Slate-colored Junco. Snowbird. Common winter resident, but more abundant in fall and spring. 108. Melospiza fasciata Gmel.. Song Sparrow. Abundant resident. Breeds. 109. Melospiza georgiana Lath. Swamp Sparrow. Migrant, not common. 110. Passerella iliaca Merr. Fox Sparrow. Common early migrant. - 111. Pipilo erythrophthalmus Linneus. Towhee. Chewink. Common sum- mer resident. Breeds. A few remain over winter. 112. Cardinalis cardinalis Linneus. Cardinal Grosbeak. A common resi- dent, less so than formerly. Breeds. 113. Habia ludvoiciana Linneus. Rose-breasted Grosbeak. Summer resi- dent, sometimes abundant and sometimes wanting. Breeds. 114. Passerina eyinea Linneus. Indigo Bunting. Very common summer resident. Breeds. 115. Spiza americana Gme]. Black-throated Bunting. Very abundant sum- mer resident. Breeds. 116. Piranga erythromelas Vieill. Scarlet Tanager. Common summer resi- dent. Breeds. 117. Progne subis Linneus. Purple Martin. Summer resident, abundant in cities. Breeds. 118. Petrochelidon lunifrons Say. Cliff Swallow. Summer resident, breeds, but is not so common as formerly. It has been driven out by the English Sparrow. 119. - Chelidon erythrogaster Bodd. Barn Swallow. Adundant summer resi- dent. Breeds. 120. Tachycineta bicolor Vieillot. Tree Swallow. Not often seen. They were observed in some abundance in the fall of ’93. 121. Clivicola riparia Linuenus. Bank Swallow. Common along the Wabash River. Breeds. 122. Stelgidopteryxr serripennis Aud. Rough-winged Swallow. Only two specimens taken. 123. Ampelis garrulus Linneus. Bohemian Waxwing. A specimen was taken near the Wabash County line and is now in the collection of Mr. M. L Galbreath. 124. Ampelis cedrorum Vieill.. Cedar Bird. Common resident. Breeds late in summer. » 125. Lanius borealis Vieill. Northern Shrike. Butcher Bird. Winter resident, not abundant. 156 126. Lanius ludoncianus excubitorides Swainson. White-rumped Shrike. Common summer resident. Breeds. The typical species may also be found here. 127. Vireo olivaceous Linneus. Red-eyed Vireo. Abundant summer resi- dent. Breeds. — 128. Vireo philadelphieus Cassin. Philadelphia Vireo. Rather rare mi- grant. 129. Vireo gilvus Vieill. Warbling Vireo. Common summer resident. Breeds. 130. Vireo flavifrons Vieill. Yellow-throated Vireo. Abundant migrant. 131. Vireo solitarius Wils. Blue-headed Vireo. Migrant; not common. 132. Mniotilta varia Linneus. Black and White Warbler. Abundant in woodland during migrations. 133. Helminthophila pinus Linneus. Blue-winged Warbler. Summer resi- dent, never very common. Breeds. 134. Helminthophila chrysoptera Linneus. (Golden-winged Warbler. Mi- grant; not so common as the last. 135. Helminthophila ruficapilla Wils. Nashville Warbler. An abundant migrant. 136. Helminthophila celeta Say. Orange-crowned Warbler. Rare. One specimen taken May 15, 1892. 137. Heiminthophila perigrina Wils. Tennessee Warbler. Abundant mi- grant; most common in fall, when they may be found in great abundance along the rivers. . 138. Compsothlypis americana Linneus. Parula Warbler. A rare migrant; two specimens taken. 139. Dendroica tigrina Gmel. Cape May Warbler. Migrant; not common. 140. Dendroica wstiva Gmel. Yellow Warbler. Very common summer resident. Breeds. 141. Dendroica evrulescens Gmel. Black-throated Blue Warbler. Migrant ; common. In the fall of 1893 it was probably our commonest warbler. It is fond of the dense woodland. 142. Dendroica coronata Linneus. Yellow-rumped Warbler. The earliest of the warblers to arrive and the last to go in the fall. It is probably our most abundant warbler. , 143. Dendroica maculosa Gmel. Magnolia Warbler. Not very common, Its habits of seclusion make it seem Jess common than others of equal abundance, 144. Dendroica cerulea Wils. Cxrulean Warbler. Rather common. So far it has been found only during the migrating season. 157 145. Dendroica pennsylvanica Linneus. Chestnut-sided Warbler. Common migrant. 146. Dendroica castanea Wils. Bay-breasted Warbler. Not common; most most frequently seen in the fall. 147. Dendroica striata Forst. Black-poll Warbler. Rather rare migrant. 148. Dendroica blackburnie Gmel. Blackburnian Warbler. Abundant mi- grant. 149. Dendroica dominica albilora Baird. Sycamore Warbler. Rather rare migrant. 150. Dendroica virens. Gmel. Black-throated Green Warbler. Very abundant migrant. 151. Dendroica vigorsii Aud. Pine-creeping Warbler. Only two specimens taken in the county. 152. Dendroica kirtlandi Baird. Kirtland’s Warbler. The only specimen known in the State was taken May 4, 1892. This is the twenty-second specimen reported from North America. Little is known of its life history. I took it ina thicket. It was alone, there being no other birds in the near vicinity of it. It seemed to be an active fly catcher, not having the motions of the other Dendroicr, being less active. It would dart off after an insect and then return to the same perch. Another specimen was taken May 7, 1895. Early in the morning I heard a bird singing in the thicket of plum trees near the house. The song was strange to me, and consisted of a loud ringing note repeated three times in quick succession, suggesting that of the Wrens or Maryland Yellow Throat. I did not go to look for it at once, but as it continued singing for some time I finally got my gun and went to look for it. It had flown over into the orchard then, but soon returned to the plum thicket and was constantly uttering that peculiar note. I finally caught sight of it and watched it for some time, not thinking of its being the rare kirtandi. It moved with the grace and ease of a vireo or fly-catcher. Wallace. [Proc. Ind. Academy of Science, 1893, pp. 11, 120]. 153. Dendroica discolor Vieill. Prairie Warbler. One specimen was taken May 2, 1892. 154. Dendroica palmarum Gmel. Red-poll Warbler. Abundant migrant. 155. Seiurus aurocapillis Linneus. Oven-bird. Very common summer resident, 156. Seiurus noveboracensis Gmel. Short-billed Water Thrush. Rather rare migrant. 157. Seiurus motacilla Vieill. Large-billed Water Thrush. Summer resi- dent; more common than the last. Arrives as early as April 3. 158 158. Geothlypis agilis Wils. Connecticut Warbler. Only one specimem taken. 159. Geothlypis philadelphia Wils. Mourning Warbler. Found in dense thickets. It was rather common in the spring of 1892, but has not been seen since. 160. Geothlypis trichas Linneus. Maryland Yellow-throat. Abundant sum- mer resident. 161. Icteria virens Linn. Yellow-breasted Chat. Summer resident, not common. 162. Sylvania mitrata Gmel. Hooded Warbler. One specimen was taken September 13, 1893. . 163. Sylvania pusilla Wils. Black-capped Yellow Warbler. Three speci- mens were seen during the spring of 1892, but it has not been noted since. 164. Sylvania canidensis Linneus. Canadian Fly-catching Warbler. A common migrant. 165. Setophiga ruticilla Linneus. American Redstart. Summer resident, but much more common during migrations. 166. Anthus pennsylvanicus Lath. American Titlark. A migrant of irregu- lar occurrence, but in some seasons very abundant. 167. Galeoscoptes carolinensis Linneus. Cat-bird. Abundant summer resi- dent. Breeds. 168. Harporhynchus rufus Linneus. Brown Thrusher, Brown Thrush. Abundant summer resident. 169. Thryothorus ludovicianus Lath. Carolina Wren. Rather rare resident. Some seasons none are seen. 170. Thryothurus bewickii Aud. Bewick’s Wren. Rather common summer resident. y 171. Troglodytes aedon Vieill. House Wren. Common summer resident. sreeds. 172. Troglodytes hyemalis Vieill. Winter Wreii. Common migrant. Prob- ably some remain throughout the winter. 173. Certhia familiaris americana Bonap. Brown Creeper. Common mi- grant. Occasionally seen in midwinter. 174. Sitta carolinensis Lath. White-breasted Nuthatch. Common resident. 175. Sitta canadensis Linneus. Red-breasted Nuthatch. One specimen taken Sept. 15th, 1891. 176. Parus bicolor Linneus. Tufted Titmouse. Very common resident. 159 177. Parus atrocapillis Linneus. Black-capped Chickadee. Abundant winter resident. 178. Regulus satrapa Licht. Golden-crowned Kinglet. Common winter resident. 179. Regulus calendula Linneus. Ruby-crowned Kinglet. Common mi- grant. 180. Polioptila cerulea Linneus. Blue-gray Gnateatcher. Common summer resident. 181. Turdus mustelinus Gmel. Wood Thrush. Common summer resident. 182. Turdus fuscescens Steph. Wilson’s Thrush. Migrant. Not so common ‘as the preceding. ‘183. Turdus ustulatus swainsonii Cab. Olive-backed Thrush. Rather com- mou migrant. 184. Turdus aonalaschke pallasit Cab. Hermit Thrush. .Common migrant. ‘Our most abundant Thrush. 185. Merula migratoria Linneeus. American Robin. Very abundant sum- mer resident. Breeds. 186. Sialia sialis Linneus. Blue Bird. Abundant summer resident. Breeds. Nores oN A COLLECTION oF FisHEes oF DPusors Country, Inprana. W. J. MoENKHAUS. The following list of fishes is offered as a slight addition to our knowledge of the fishes of Indiana. The list is based on a collection made during the second week in September, 1893, in Patoka River and Short Creek near Huntingburg, Dubois County, Indiana. It has been withheld from publication thus long be- cause I have hoped that further work might be done in the same streams, but as each year makes this more improbable, it is perhaps best to publish the list as it is. Very little is known of the fishes of the Patoka River, investigations having been made only near its mouth, at the city of Patoka, by Jordan and Evermann, some years ago. (Jordan, Bull. U. S. Fish Com. VIII, 1890). The Patoka River flows from east to west across about one-half the width of the State. In its course it passes through the southern part of Orange County and through the middle of Dubois, Pike and Gibson counties, emptying into the Wabash a few miles south of the mouth of the White River. In the vicinity of Huntingburg where it was fished, the channel is from 75 to 100 yards in width. The stream is everywhere obstructed along the banks and ofttimes entirely across 160 by fallen timbers, The water is always more or less muddy, except in the fall, when very low, it approaches clearness. The river was fished for three-quarters of a mile where Hunley Creek empties into it. The water was very low and the fish were mostly collected in the deeper places in the channel. The ripples were repeatedly seined, but were found to be poor in fish. These places seemed ideal for darters, but not a single one was taken here. All that were caught were living together and had collected in the apparently stagnant holes, Short Creek is a narrow muddy stream about seven miles in length, emptying into Hunley Creek three miles above its mouth. During dry seasons it dries up at many places and presents only pools of yellow, muddy, stagnant water. It was in some of these pools from its mouth to about a mile above that our fishing was done. : Patoka River will be indicated by (2) in the descriptions, and Short Creek by (S). All of this collection is in the Indiana University Museum. The common names given are those by which they are known in this locality: 1. Ictalurus punetalus Rafinesque. Channel cat. (P.) Two specimens. 2. Amimrus melas Rafinesque. Black cat. (P.) One specimen. 3. Leptops olivaris Rafinesque. Flat-head. Mud cat. (P.) One specimen. 4, Schilbeodes minrus Jordan. (P.) Sixteen specimens. 5. Morostoma aureolum Le Sueur. Red horse. White sucker. Four specimens from Short Creek and fourteen from the Patoka River. 6. Hybognathus nuchalis Agassiz. Thirty-seven specimens from Short Creek and fifty-nine from Patoka River. 7. Pincephales notatus Rafinesque. (P.) Seven specimens. 8. Cliola vigilax Baird & Girard. (P.) Many specimens. 9, Notropis microstomus Rafinesque. (P.) Nineteen specimens. 10. Notropis whipplei Girard, (P.) Sixty specimens. 11. Notropis avaens Cope. (P.) Twenty specimens. 12. Notropis wm bratilis Girard. (S.) Fifty-eight specimens. 13. Notroprs atherinoides Rafinesque. (P.) Thirty-eight specimens. 14. Opsopoeodus emiliae Hay. (S.) Two specimens. 15. Notemigoneus chryscleneus Mitchell. Golden shiner. (S.) Five specimens. 16. Dorosoma cepedianum Le Sueur. Mud shad. Hickory shad. (P.) One specimen. : 17. Tygonectes notatus Rafinesque. Top minnow. (P. S.) Sixty-one speci- mens from Patoka River and five from Short Creek. 18. Lucius vermiculatus Le Sueur. Pike. Pickerel. (P.) Four specimens. 19. Labidesthes sieculus Cope. Silver side. (P.) 20. Aphredoterus sayanus Gilliams. (S.) Five speci 21. Pomoris annularis Rafinesque. Calico bass. ( All ages. Six specimens show the following characters VI-14, VI-15, VI-14; anal fin, VI-19, VI-19, VI-18, VI-17, VI-19, VI-17. 22. 23. Thirteen specimens. Chaenobryttus gulosus Cuv. & Val. (S.) Mieropterus salmoides Lacépéde. All ages. 24. Lepomis nugalotis Rafinesque. 25. Lepomis pallidus Mitchell. and fifteen from Patoka River. (P. S.) mens. S.) Five specimens. 161 Twenty specimens. : Length, 85, 96, 108, 123, 124, 145; lat. 1, 43, 44, 43, 46, 45, 47; dorsal fin, V-15, VI-15, VI-15, (S.) One specimen. Four specimens. Large-mouthed black bass. (P:) Six specimens from Short Creek 26. Etheostoma aspro Cope & Jordan. Blacksided darter. (P.) Forty-nine specimens. The Table X contains details of counts and measurements of these specimens: heer eulicrS = gece Use A Dore 3 | Soe} | 5 Weal2 jz | 8 | eo); q = Wso}mq ie = a2 4 = 26 i fa] 3 elvore |S S J = el ace = Sele BS 2 a = a Sorin ohio. “2p ls Sn |Shl/=se| 22 a S on |e se| se Pent ge Ba loga |] as 3 S K me | oe s¢ SRE Sie | s Bier) Se | Ss en =| ° BO} or om om a .] = o = a M2 a 1738 CONVOLVULACE#, Ipomea purpurea Lam, (289.) Gardens, etc. September 28, 1894. SOLANACE®, Solanum nigrum L. (140.) Common about yards. July 29, 1895. Solanum Carolinense L. (276.) Waste places. September 28, 1895. Physalis Philadelphica Lam. (91.) Along B. & O. Railroad and in woods south of Oak Grove. Physalis pubescens L. (139.) About yards. July 29, 1895, Datura Stramonium 1. (230.) Near Washington. September 28, 1895, Datura Tatula L. (229.) Near Swan Pond. Not so common as No. 230. August 5, 1895. As Mr. Clements confused the two species the inference is that Tatula is the abundant form. SCROPHULARIACE®. Verbascum Blattaria L. (134.) Common in waste places. July 10, 1895. Linaria vulgaris Mill. (244.) Common weed, lots and streets, September 10, 1895. Scrophularia nodosa L., var. Marilandica Gray. (70.) Oak Grove on railroad track. May 18, 1895. Pentstemon pubescens Solander. (189.) Railroad track south of Oak Grove. Pentstemon levigatus Solander, var. Digitalis Gray. (216.) Hyatt’s. Wet places. June 6, 1895. Mimulus alatus Ait. (164.) Prairie Creek bridge, Swan Pond road. August 5, 1895. ; Veronica Virginica L. (95.) Along B. & O, railroad, two miles west of Wash- ington. July 4, 1895. Veronica peregrina L. (22.) Bretz’s pasture. April 14, 1894. Gerardia quercifolia Pursh. (171.) Woods south of B. & O., and Oak Grove. Flowers, lemon-color. Plant, six to eight feet high. August 10, 1895. Gerardia purpurea L. (193). Woods south of Oak Grove. September 28, 1894. BIGNONIA CE. Tecoma radicans Juss. (96.) Along B. & O. tracks, west of Washington. July 4, 1895. 179 ACANTHACE®. Ruellia strepens L. (303.) Abundant along Prairie Creek at Hyatt’s. May 18, 1899. VERBENACES. Verbena urticefolia L. (285.) Common weed in waste places. September 28, 1894. Verbena angustifolia Michx. (119.) Along railroad track east of Washington. July 16, 1894. Verbena hastata L. (270.) Yard of B. & O. shops. August, 1895. (132.) Wilson’s woods; wet places. Verbena stricta Vent. (133.) Common plant along railroad and in vacant lots. July 10, 1895. Verbena bracteosa Michx. (125.) Growing along sidewalks, ete. July 31, 1895. Lippia lanceolata Michx. (122.) Common, growing along grassy fences and in pastures. July and August. Phryma Leptostachya L. (131.) Sanford’s woods. July 10, 1895. LABIAT. Teucrium Canadense L. (106.) South of B. & O, Railroad and Oak Grove. July 4, 1895. Mentha piperita L. (150.) Along railroad tracks. July 29, 1895. Lycopus rubellus Moench. (277 and 291.) Field west of B. & O shops. Sep- tember 28, 1894. Pyecnanthemum lanceolatum Pursh. (173.) Abundant in waste lands two miles east of Washington. July 16, 1895. Monarda fistulosa L. (105.) Woods south of Oak Grove. July 4, 1895, Blephilia hirsuta Benth. (129.) Wilson’s woods, along branch east of Wash- ington. July 10, 1895. Nepeta Glechoma Benth. (64.) West Eighth Street and B. & O. track. May 11, 1894. Scutellaria laterifora L. (169) Near Swan Pond. August 5, 1895, Scutellaria canescens Nutt. (107.) Woods south of Oak Grove. July 4, 1895. Scutellaria nervosa Pursh. (68.) Woods south of Oak Grove. May 11, 1895. Brunella vulgaris L. (153.) South of B. & O. at Oak Grove. July 29, 1895. Marrubiwm vulgare L. (168.) Swan Pond. August 5, 1895. Lamium amplericaule L. (248.) Side of northeast Sixth Street, near Walnut. May 11, 1895. 180 ILLECEBRACEX. Anychia dichotoma Michx. (121.) South of B. & O. railroad at Oak Grove, in edge of woods. Anychia capillacea DC. (264.) South of Oak Grove, near railroad. AMARANTACE®. Amarantus retroflecus L. (234.) Gardens, yards, etc. July. Amarantus albus L. (211.) Weed about gardens. September 28, 1894. ‘ Amarantus spinosus L. (209.) Weed in all gardens, ete. September 28, 1894. CHENOPODIACE®. Chenopodium album L. (290.) Common weed. September 28, 1894. PHYTOLACCACER. Phytolacea decandra L. (147.) Common, roadsides, ete. July 29, 1895. POLYGONACE®. Rumex Britannica L. (238.) Waste places. August 16, 1895. Rumex Acetosella L. (69.) Common everywhere in waste places. May 18, 1894. Polygonum Pennsylvanicum L, (286.) Yards, etc. September 28, 1894. Polygonum orientale L. (235.) Escaped from yards. August 16, 1895. Polygonum Virginianum L. (146.) Woods south of Oak Grove and B. & O. Railroad. July 29, 1895. Polygonum dumetorum L., var. scandens Gray. (117.) John Hyatt’s woods and E. & I. Railroad. July 13, 1894. ARISTOLOCHIACE. Asarum Canadense L. (85.) South of B. & O. tracks at Hyatt’s. Not com- mon. May 18, 1895. ; SANTALACES. Comandra umbellata Nutt. (249 and 306. ) Woods south of Oak Grove, where woods run into a low, grassy place. May 1], 1895. EUPHORBIACE2. Euphorbia Preslii Guss. (280.) Weed in waste places. September 28, 1894. Euphorbia corollata L. (154.) Common along banks of B. & O. Railroad and woods south of Oak Grove. July 29, 1895. = = 181 URTICACER. Laportea Canadensis Gaudichaud. (116.) John Hyatt’s woods. July 13, 1:95. Behmeria cylindrica Willd. (267.) John Hyatt’s woods. July 18, 1895. Parietaria Pennsyvlanica Muhl. (267a/) John Hyatt’s woods. July 13, 1895. IRIDACE®. Tris versicolor L. (72.) First pond beyond Oak Grove, south of B. & O. tracks. May 18, 1894. Belameanda Chinensis Adans. (127.) In pasture on Sanford’s farm. July 10, 1895. Sisyrinchium angustifolium Mill. (90.) Prairie Creek, west of Washington. May 18, 1895. AMARYLLIDACEX. | Agave Virginica L. (233.) Near B. & O. Railroad, two miles east of Wash- ington. Six to seven feet high. July 16, 1895. DIOSCOREACE®. Dioscorea villosa L. (59.) Woods south of B. & O. Railroad and Oak Grove. May 11, 1894. LILIACE. Smilax herbacea L. (45.) Sanford’s woods. Common in all woods. May 4, 1894. Smilax Pseudo-China L. (78.) A vine covering a small tree. Bank of White River, north of B. & O. track. May 18, 1894. Allium Canadense Kalm. (75.) Prairie Creek, south of B. & O. Railroad. May 18, 1894. Camassia Fraseri Torr. (76.) Prairie Creek, south of Oak Grove. May 18, 1894. Polygonatum biflorum Ell. (61.) Woods south of Oak Grove. May 11, 1894. Polygonatum giganteum Dietrich. (253.) Beside railroad track near Oak Grove. May 18, 1895. Asparagus officinalis L. (160.) About one mile north of West Washington. August 5, 1895. Smilacina racemosa Desf. (46.) Sanford’s woods. May 4, 1894. Uvularia grandiflora J. E. Smith. (23.) Woods south of Oak Grove. April 21, 1894. Erythronium Americanum Ker. (19a.) Hyatt’s woods, south of B. & O. shops. April 14, 1895. 182 Erythronium albidum Nutt. (16.) Woods south of B. & ©. shops. April 13, 1894. ’ Trillium sessile L. (74.) Hyatt’s, south of B. & O. Railroad. Not common in this vicinity. May 18, 1894. Trulium recurvatum Beck. (21.) Common in most woods. April 20, 1894. Trillium erectum L. (30.) East of Washington. April 26, 1894. COMMELINACE2. ae Tradescantia Virginica L. (62.) Common. Railroad bank and woods south of Oak Grove. May 11, 1894. | ARACES. Arisema triphyllum 'Yorr. (38.) Hyatt’s woods, south of B. & O. shops. April 27, 1894. Arisema Dracontium Schott. (73.) Prairie Creek, south of B. & O. Railroad. May 18, 1895. ALISMACEZ. Sagittaria variabilis Engelm, (245.) Ditch, south of B. & O. shops. Sep- tember 10, 1895. CYPERACE. Cyperus strigosus L. (202.) Along ditch, west of shops. September 28, 1895. Carex Grayii Carey. (300.) Wet places near B. & O. Railroad at Hyatt’s. May 18, 1895. Carer Shortiana Dewey. (301.) Hyatt’s, near B. & O. Railroad. May 18, 1895. Carex crinita Lam. (217.) Hyatt’s. June 6, 1895. Carex teretiuscula Gooden. (302.) Wet places near Hyatt’s. May 18, 1895. GRAMINE. Panicum mierocarpon Muhl. (308.) Two miles east of Washington. July 4, 1895. Cenchrus tribuloides L. (201.) Along railroad tracks. September 28, 1895. 183. NoTEWORTHY INDIANA PHANEROGAMS. By STANLEY COULTER. The ruling of the directors of the Survey that no form should be admitted to. the catalogue of the flora of the State unless verified by actual specimens has led me as far as possible to secure first exceptional forms of limited range, in the hope that by a publication of the data concerning them the attention of collectors might be directed to them, and our knowledge of their distribution within the State be- increased. ‘The most notable collection of these exceptional forms that has come into the possession of the Survey was that received from Rey. E. J. Hill, of Engle- wood, Ill., embracing 163 species. All of the specimens were of extreme interest, and many of them represented the sole record for the State. The following notes. are based very largely upon this collection, and most of the forms represent a southern extension of northern forms. It should be remembered, however, that, until we have a full knowledge of the isotherms of our country, statements as to. **southern limit” and ‘‘ northern limit” are merely terms of convenience, and do. not necessarily involve any real extension of range. A fuller knowledge of natural drainage systems, of prevailing winds at vary- ing seasons and of numerous other physical conditions is necessary before we can properly undertake a definite limitation of the range of any plantform. Ina limited area, in which there is a definite organization of work, it is possible to- determine many of these conditions and by their record add much to the ease with which some of the problems of geographical distribution may be solved. Another feature emphasized by this paper is the extreme importance of long- continued collections in the same region. The work of Mr. Hill in Lake County covers a period of twenty years and has resulted not only in the addition of many new forms to the State flora but in a thorough botanical knowledge of that portion of the State. The work of Mr. Van Gorder in Noble County, extending through ten years, has shown similar results. Many problems which present themselves. ean only be solved by work of this kind. The tendency of collectors in the past work of the State has been to cover large areas, rather than to study closely some definite regions. Closer attention should be given by all collectors throughout the State to mass distribution, as distinguished from the station at which the collec- tion is made, and also to the collection of fruiting specimens. A somewhat careful study of our State flora leads me to believe that many forms may be added if a more careful study is made of our marsh and lake forms and of those groups which are of difficult discrimination. Special studies should also be made during the coming season of definitely characterized regions, as, for 184 example, of the flora of lime stone cliffs, of clay soils, of sand hills, ete. The work needed is not so much a collection of plants as a collection of facts verified by plants. In the following notes I have not in all cases referred to Mr. Bradner’s list of the plants of Steuben County, because I have had no opportunity to examine his collections. The references, save as indicated in the notes, are to material in the possession of the Survey. A large number of interesting forms of Cyperacee and Graminee have been omitted, because our knowledge of the distribution of these forms in the State is too scant to justify any conclusions concerning them. Cardamine pratensis L. This rare Northern plant, which was included in the State catalogue, but of which no specimen had been preserved, is now definitely reported with verifying specimens from two localities. Wet banks of Calumet River, Miller’s, Lake Co., June 6, 1893 (E. J. Hill); Section 5, York Tp., Noble Co., May 28, 1894 (W. B. Van Gorder). Mr. Van Gorder sent me specimens of this plant last June, at which time I determined it to be C. pratensis L., a deter- mination which was later confirmed by a careful comparison with the material in the Gray Herbarium at Harvard University. Under date of November 6, 1895, Mr. Van Gorder writes as follows: ‘“OCardamine pratensis L. grows plentifully on a tract of wet land, three or four acres, in section 5, York Tp., Noble Co. This tract is a part of the Elkhart River flat. I had seen the plant for several years, and at a distance thought it C. rhomboidea DC. This last spring it was dry enough, and passing the place I determined to know for sure. It flowers from May 15 to June 10. The specimen sent you was collected May 28.” The manual range of the plant is, ‘*Wet places and bogs, Vt. to N. J., Wis., and northward; rare.” The following local references which I was able to collate while at the Gray Herbarium during the past summer may serve to show the interest which attaches to this plant as a member of the Indiana flora: State (Indiana) Catalogue, ete. Lake Co. P. 3. Flora of Michigan. Wheeler, C. F., and Smith, E. F. “Bogs.” Rare &., frequent in C. and common N. P. 14. Flora of Minnesota. Warren Upham. Lake Superior to sources of Missis- sippi. North. (Houghton.) P. 24. i Flora of Nebraska. Samuel Aughey. Includes without note. P. 6. Flora of Iowa. J.C. Arthur. Does not include. ae Preliminary Catalogue of Anthophyta and Pteridophyta, etc. Torrey Botanical Club.—Includes without note. 185 Catalogue of Plants of New Jersey. N. L. Britton.—Cedar swamp at New Dur- ham. Rare. P. 8. Catalogue of Native and Naturalized Plants of the City of Buffalo and Its Vicinity. David F. Day.—Rare. S. E. portion of Buffalo, near West Seneca. P. 18. Flora of Cook Co., Iil., and Part of Lake Co., Ind. Higley, Wm. K., and Rad- din, Chas. S.—Calumet River, near Miller’s, Ind.—Rare. April. (Bastin and Hill.) P.9. This reference is evidently based upon the collection of Mr. Hill cited supra. Plants of Illinois. HH. N. Patterson.—Does not include. Flora Peoriana (Ill.). Frederick Brendel.— Does not include. Higher Seed Plants of Minnesota Valley.. Conway Macmillan.—Does not in- clude. Catalogue of Canadian Plants. John Macoun.—‘‘ Wet, swampy meadows, Labrador; St. Patrick, Charlotte Co., N. B.; vicinity of Prescott Junction, three miles south of Ottawa; wet meadows and swamps, Hastings Co., Ont.; Whiskey Island; Georgian Bay; Hudson’s Bay; throughout Arctic America and Green- land.” Manual and Instructions for Arctic Expedition, 1895. Hooker, on arctic plants, p. 203, says: ‘‘The most arctic plants of general distribution that are found fur north in all the arctic areas are the following; all inhabit the Parry Islands or Spitzbergen or both.” A list of fifty-three plants is given, including Cardamine pratensis L. 2 On page 226, the range of this form is given as ‘‘from Mackenzie’s River to Baftin’s Bay. Throughout Arctic Greenland.” In same volume, page 244, the following note concerning this form is given by James Taylor: ‘‘ Cardamine pratensis L. Flowers June-July. East side Disco Island. Altitude, 200 feet. North lat., 69° 10’; W. long., 54° 307.” In the various catalogues of the New England States it is usually included with the statement, ‘‘chiefly found in the northern part.” From these citations it will be seen that the Indiana stations mark the south- ern-central limit of this true arctic form, which in all probability found its way southward during the glacial period. Arabis lyrata L. ‘Dry, sandy ground, Miller’s, Ind., June 6, 1893.” (E. J. Hill.) Reported also from Laporte County, presumably upon authority of Dr. Barnes, and included in Bradner’s flora of Steuben County. The form in general is a northern one in its mass distribution, although extending south along the mountains as far as Kentucky. Its local distribution will probably be found to 186 be limited to the northern portions of the State, and its occurrence there can only be expected in exceptionally favorable localities. Hudsonia tomentosa Nutt. ‘‘Sand hills, Miller’s, Ind., June 20, 1893.” (E. J. Hill.) This striking form has as yet its only station as indicated. It is so unlike the ordinary phanerogam of Indiana that it could scarcely have escaped notice if it was of any wide distribution. The range of the plant is ‘‘sandy shores, Maine to Md., and along the Great Lakes to Minn., rarely on streams inland.” It is therefore probable that its distribution in Indiana is extremely restricted. Lechea thymifolia Michx. “Sandy ground, Tolleston, Ind. Flowers collected Sept. 16, 1882; fruit, Oct. 1, 1881.” This is the only record for the species, and if the determination holds good, is a rather peculiar extension of range. The assigned range is ‘“‘dry grounds near the coast, E. Mass. to Fla.” The retfer- ence is apparently accurate, but on account of the well-known difficulty of dis- crimination between the species of this genus, I am unable to feel absolutely cer- tain in the absence of authenticated specimens for comparison. The authority of Mr. Hill, however, is sufficient to retain the plant in the State list until oppor- tunity oceurs for comparison with forms from the east. Arenaria Wichauxii Hook. f. ‘Dry sands, Clark, Ind., June 13, 18938.” (EK. J. Hill.) There seems to be no special reason why this species should not be found generally distributed throughout the State, although as yet this is the only station recorded. The known range of the plant easily includes Indiana, and it should be looked for throughout the State. Arenaria lateriflora 1. ‘‘ Dry woods, Miller’s, Ind., June 20, 1893.” (E. J. Hill.) This species was reported by Dr. A. J. Phinney in his list of plants of the region covering Jay, Delaware, Randolph and Wayne counties. He, how- ever, secured no verifying specimen. The Lake County collection, however, seryes under the rules of the State to give the species a place in the flora of Indi- ana. It is probable that the plant will be found to occur only in the eastern and northern counties of the State, its general range being northward. Hypericum Kalmianum L. “‘ Wettish sands, Tolleston, Ind. Flowers col- lected June 29, 1880; fruit, September 3, 1880.” (KE. J. Hill.) Also collected at Laporte by Dr. C. R. Barnes. This species is evidently limited to the northwest- ern counties of the State and will probabiy not be found much beyond the lake region. The assigned range is Niagara Falls and northern lakes. Linum su'catum Riddell. ‘‘Dry, sandy soil, Pine Station, Ind., July 28, 1875.” (E. J. Hill.) So far as I am able to determine, this is the only station 187 in the State for this species. Its general range, ‘‘ E. Mass. to Minn., and south- westward,” would indicate, perhaps, a more general distribution since it has made its appearance within our boundaries. Nemopanthes fascicularis Rat. ‘* Wet ground, Miller’s, Ind. Flowers collected April 29 and May 11, 1882; leaves and fruit July 4, 1882.” (E. J. Hill); Steu- ben County (E. Bradner). Although not ineluded in the lists of Mr. Van Gorder, I have received from him this summer material of this species collected in Noble County. The manual range of the plant was extended upon the collection of Mr. Hill, and from the later reports it is fair to infer that its occurrence is limited to perhaps the northern tier of counties Lathyrus maritimus Bigel. ‘‘Shores of Lake Michigan, Whiting, Ind., July 15, 1875.” (E. J. Hill.) A species inhabiting the seashore from Oregon and New Jersey to the Arctic Ocean, and also found on the Great Lakes. The range in Indiana can evidently be but slightly extended, if at all. Rosa Englemanni Watson. ‘‘Flowers collected, East Chicago, Ind., June 5, 1890; fruit collected in damp thickets at Pine Station, Ind., Aug. 25,1891. Four feet to eight feet high.” (E. J. Hill). The specimen furnished the survey seems clearly referable to this species, though showing a decided increase in size. The plant is normally from ‘‘three to four feet high, or less.” Its range is given as ‘“Whisky Island, Lake Huron, shores of Lake Superior, and west to the Red River valley, and in the mountains from N. Montana and N. Idaho to Colorado.” Its appearance in Indiana is of extreme interest and adds a new station for the species. Heuchera hispida Pursh. ‘‘Sandy, open grounds, Tolleston, Ind., June 20, 1893.” (KE. J. Hill.) This is an additional station for this species which was formerly reported only from Vigo County by W.S. Blatchley. It may be assumed that the form will be found in favored localities throughout the State. (Saxifra- gacez in Indiana, Proc. Ind. Acad. of Sci. 1894, p. 105.) Sambucus racemosa L. ‘‘Open woods, Porter, Ind., May 17, 1890; fruit, Otis, Ind., May 21, 1881” (E. J. Hill); ‘‘common at least in eastern part of Noble County” (Van Gorder) ; Steuben County (Bradner); Putnam County (MacDougal) ; Jefferson County (J. M. Coulter); Clarke County (Baird and Taylor). This species is northern in its mass distribution and is more rarely found southward. In leaf, fruit and bark characters, it at times runs perilously close to S. Canadensis L. I have found the color of the pith to be by far the most satisfactory means of dis- crimination between the two forms. Although the assigned range includes Indi- ana, my own experience leads me, in the absence of verifying specimens from 188 other localities, to limit the distribution of the species to the northern portion of the State. Linnaea borealis Gronoy. ‘‘Moist, pine woods, Pine Station, Ind., June 7} 1884.” (E. J. Hill.) This is the recorded southern limit for this definitely northern form. Its occurrence so far south is worthy of note. It must be remem- bered, however, in this extension of ranges that limits are marked by parallels of latitude, when the proper method would be a consideration of isothermal lines. Galium boreale L. ‘‘Sandy prairies, Sheffield, Ind., July 6, 1875” (E. J. Hill); ‘“‘rather common, Noble County” (W. B. Van Gorder). The distribution of this species seems fairly well made out for Indiana, being confined to the northern counties which represent in a general way its southern limits. It is a form that can not be readily mistaken for any other members of the genus, being definitely marked by its bright white flowers. Liatris cylindracea Michx. ‘‘Dry sands. Lake County, Ind., September 4, 1893. (E. J. Hill.) The Indiana stations for this plant, so far as reported, in addition to that in Lake County, are St. Joseph County (C. R. Barnes); Gibson and Posey counties (J. Schneck). These widely separated stations indicate at least the probability of its occurrence throughout the State in favorable localities. The manual range reads: ‘‘ Dry, open places, Niagara Falls to Minn. and Mo.” The St. Joseph County record is verified by specimens in the Purdue Herbarium. The inclusion of the Gibson and Posey County station is upon the authority of Dr. J. Schneck, of Mt. Carmel, II]. Solidago humilis Pursh. ‘‘Sand hills, near Lake Michigan, Miller’s, Ind., September 12, 1893. Sometimes 3 feet high.” (E. J. Hill.) This is a distinctly northern form, and one which shows in its very considerable increase in size the effect of its new range. In its normal range, ‘‘Rocky banks, W. Vt., along the Great Lakes, and northward,” it is a low plant from 6 to 12 inches high. At the base of the White Mountains a form is reported, by Gray, as occurring, having a ‘“stout stem, 1-2 feet high.” Variety Gillmanni Gray, is larger (2 feet high), but in addition to differences in inflorescence, is sharply separated from the species by its ‘‘laciniately toothed leaves.” The species is undoubtedly a member of the State flora, and the Lake County station is to be added to the other exceptional stations recorded, ‘“‘islands in the Susquehanna, near Lancaster, and at the Falls of the Potomac.” 3 Solidago uliginosa Nutt. ‘‘Peat bogs. Pine Station, Ind., Sept. 11, 1890.” (FE. J. Hill.) This plant, which is northern in its mass distribution, has its southern limit, so far as reported, in the northern tier of counties of Indiana. Additional stations are, St. Joseph County (C. R. Barnes) and Noble County (W. | 189 B. Van Gorder). Specimens have been examined from all three localities. The recorded range of the plant is ‘‘ Peat bogs, Maine to Penn., Minn., and north- ward.” Brachycheta cordata Torr. and Gray., Among the forms that have come into the Indiana flora from the South the above is one of the most interesting. Its station is in Jefferson County, especially at Clifty Falls. The station is one of the remarkable ones in the State, because of the number of rare forms there found, Sullivantia Ohionis Torr. and Gray, being perhaps the most noteworthy if we except Brachycheta. The manual range of the plant is as follows: ‘‘ Wooded hills, S. Ind. and E. Ky. to N. Ga.” In the Synoptical Flora, p. 161, the range is given as follows: **Open woods, etc., W. North Car. and E. Ky. to upper part of Ga.” The plant was apparently first collected by Rafinesque, by whom it was described as Solidago sphacelata, Raf. Ann. Nat. (1820), p. 14. In Short’s Supplement to the Catalogue of the Plants of Kentucky it is de- scribed as Solidago cordata Short. In DeCandolle’s Prodromus, V. 318, it appears as Brachyris ovatifolia DC., with the range ‘“‘in agro Kentuckensi ad ripas fuminum legit, cl. Rafinesque. * * Species, distinctissima.”’ Additional localities are as follows: Flora of West Virginia C.F. Millspaugh. P. 382.—‘‘Fayette County, near Nuttalsburg, plentiful.” Flora of Southern United States. A. W. Chapman, 2d edition. P. 213, entered as Solidago cordata Short. ‘‘ Mountains of Georgia and North Carolina and north- ward.” Botany of Southern States. John Darby. P.370—‘‘ North Carolina and North- ern Georgia.” A Sketch of Botany of South Carolina and Georgia. Stephen Elliott. Vol. I (1824), which includes Solidago, does not distinguish the form. Tennessee Flora. August Gattinger (1887). P. 51—Records as occurring over the whole State. The specimens in the Gray Herbarium only include four sheets, all being from the South. They are as follows: Solidago cordata (n. sp.) Short. Cliffs of Kentucky River. C. W. Short, M. D., Lexington, Ky. This is the type specimen of Brachychwta cordata Torr. and Gray. 190 Solidago cordata Short, Wilkes County, North Carolina, M. A. Curtis; Table Mountain, North Carolina, M. A. Curtis. Both of these have received the label Brachycheta cordata in the handwriting of Dr. Gray. Solidago cordata Short. French Broad River, 1843. No collector’s name. Brachycheta cordata Torr. and Gray. Curtiss, North American Plants, No. 1298; Bluffs of Cumberland River, near Nashville, Tenn. Legit A. Gattinger. An examination of the above data shows that this form can be reasonably expected in the southwestern counties of the State. It is easily mistaken for a Solidago, which genus it resembles closely in head and flower, except in the pap- pus. It perhaps should be looked for in collections among the Solidagos. Aster polyphyllus Willd. ‘‘ Grassy borders of low thickets, Whiting, Ind. September 29, 1892.” (E. J. Hill.) The range of this species being ‘‘ northern Vermont to Wisconsin, and southward,” it is a little remarkable that this is its only record for the State. It is possible that it has been mistaken for A. erveoides L., which it resembles in many particulars. The extreme variability of this lat- ter form renders such an error a natural one. It is probable that A. polyphyllus is more widely distributed throughout the State than the single recorded station would indicate. Aster umbellatus Mill. ‘‘ Moist grounds, Pine Station, Ind. September 4, 1893.” (E. J. Hill.) This form, ‘‘common, especially northward,” is only recorded from four counties of the State. Additional stations are as follows: Jefferson County (C. R. Barnes); Clark County (Baird and Taylor); Jay County (Dr. Phinney). The Jefferson County reference has its authentication in speci- mens in the Purdue Herbarium; the Clark and Jay County stations rest upon the authority of the collectors. The plant may be confidently looked for in the northern counties of the State, and many new stations should be added as a result ot the work of the ensuing season. Aster ptarmicoides Torr. and Gray. ‘‘ Dry sands, Pine Station, Ind.” (E. J. Hill.) This form, oceurring on ‘‘dry rocks, western New England to Min- nesota, along the Great Lakes, and northward,” is another species that has entered the State from the north. The Lake County station is the natural one for the State. In the fall of 1894, Messrs. Conner and Laben collected this species at Happy Hollow, Tippecanoe County. I withheld judgment upon the determina- tion, until I was able to examine the type specimens in the Gray Herbarium. There is no question that A. ptarmicoides occurs in Tippecanoe. The station in which it is found is so secluded as to preclude the probability of its recent intro- duction. The range of the species must therefore be extended somewhat. 191 Echinacea angustifolia DC. ‘‘ By Michigan Southern and Lake Shore Rail- road, Durham, Ind. Ina prairie. July 4, 1892.” (E. J. Hill.) So far as I am able to find, this is the only record for this species in the State. The form has evidently entered our flora from the west, its recorded range being ‘‘ Plains from Ill. and Wisc. southwestward.” It is easily distinguishable from FE. pur- purea Moench. and should be looked for carefully in the western counties of the State. Artemisia Canadensis Michx. ‘‘Shores of Lake Michigan, Lake Co., Sept. 4, 1893.” (E. J. Hill.) This northern form has its only recorded station for Indiana in the above reference. Its range is ‘‘ Northern New Eng. to the great lakes, Minn., and northward.” It is closely allied to A. caudata Michx., which also has its sole Indiana station in Lake Co. No specimen of this latter form, however, has as yet been obtained by the Survey. A. caudata having a range ‘‘ Mich. to Minn., and southward,” should be found, at least, in the northern counties of the State. Both species are separated from the other Artemisias by their dissected leaves and should be readily recognized. Cnicus Pitcheri Torr. ‘‘Sandy shores of Lake Michigan, Pine Station, Ind., June 21, 1891.” (E. J. Hill.) This well-marked species has this as its only sta- tion in the State, so far as the records indicate. Its range, ‘‘ Sandy shores of Lakes Michigan, Huron and Superior,” would indicate but a slight probability of any material increase in its distribution. It would probably be found in Laporte County in the region of Michigan City, if careful search were made. With its cream-colored flowers and white woolly covering it is an extremely attractive form and could scarcely be mistaken for any other species of the genus. Cnicus pumilus Torr. ‘Pine barrens. Lake County, Ind., July 4, 1891.” (E. J. Hill.) This form is labeled Cnicus Hillii W. M. Canby. Iam unable, however, to see any reason why the form should not be referred to C. pumilus Torr., and in the absence of Mr. Canby’s original description I have so referred the specimen sent to the Survey. Certain variations from the type seem to me easily referable to geographical causes, and not of sufficient importance to neces- sitate the establishment of a new species. The range of the plant, ‘‘ Dry fields, N. Eng., near the coast, to Penn.”, seems to me to furnish the only argument against the reference. It is possible that more abundant material may lead to a different conclusion. The reported occurrence of Cnicus pumilus in Dearborn County (S. H. Collins) is not authenticated by specimens, and is in all probabil- ity an error in determination. The extension of the range of a coast plant to the Great Lakes could be easily accounted for, but its extension to Dearborn County without intervening stations would be difficult of explanation. 192 Prenanthes racemosa Michx. ‘‘Open, grassy land, East Chicago, Ind., Oct. 5, 1892.” (E. J. Hill.) Noble County (W. B. Van Gorder). The range of this species in Indiana seems to be limited to the northern tier of counties. The form is found in ‘‘plains, N. Maine to N. J. and northward,” though extending also into Missouri. It is easily distinguished from the other species of the genus found in the State by its heads being in crowded clusters, and could scarcely have escaped the attention of collectors had it been of any general distribution. Pyrola chlorantha Swartz. ‘‘Sandy woods, Whiting, Ind., May 25, 1878.” (E. J. Hill.) A northern form, ranging from Labrador to Minnesota, northward and westward, with the single record from Indiana as indicated. The specimens in the possession of the Survey are, so far as known, the only ones from the In- diana station in the herbaria of the State. Trientalis Americana Pursh. ‘‘Damp woods, Miller’s, Ind., May 11, 1878.” (E. J. Hill.) ‘‘In tamarack marshes in moss near the roots of trees. Very com- mon in some places. Noble County.” (W. B. Van Gorder.) The mass distribu- tion of this species is decidedly northern, its southern limit being the northern tier of counties in Indiana, save where it extends southward along the mountains. It will probably be found in all of the northern counties, but need scarcely be ex- pected farther south. Menyanthes trifoliata L. ‘‘ Bogs and peat marshes, Pine Station, Ind. May 13, 1876.” (E. J. Hill.) ‘‘ Moist shores of lakes—very common at Pleasant Lake, Noble Tp., Noble Co.” (W. B. Van Gorder.) Whiie the sixth edition of Gray’s Manual includes Indiana in the range of this species, its authenticated distribu- tion is confined to the stations mentioned. It probably occurs throughout the northern portion of the State in favorable localities. Convolvulus arvensis L. ‘‘ By railroad, Pine Station, Ind. July 28, 1875. Rare.” (E. J. Hill.) Also reported from Jay, Delaware, Wayne and Randolph Counties (Phinney), and Dearborn Co. (Collins). This adventive species, hereto- fore restricted to North Atlantic States, has evidently made lodgment in Indiana. I am inclined to think the Dearborn County reference somewhat doubtful, judg- ing from the general range of the plant and taking into consideration the means of distribution to which the presence of this intruder is evidently due. I believe its range in the State will be found limited to the northern and central counties. Stachys hyssopifolia Michx. ‘‘ Wet, sandy banks, Laporte, Ind. July 22, 1875.” (E. J. Hill.) Also collected at Laporte by C. R. Barnes. The State cata- logue notes the plant as occurring from ‘‘ Marion Co. and northward.” The Ma- rion County reference was doubtless based upon the authority of the late Dr. H. E. Copeland, who was an exceedingly keen observer, but who, unfortunately, left 193 no verifying specimens. It is scarcely possible that this can be the only station for the plant, since its range fairly covers the State. Utricularia resupinata B. D. Greene. ‘Sandy margins of ponds, Whiting, Lake County, Ind., Aug. 16, 1883.” (E. J. Hill.) This collection, upon which is based the extension of the range of this form in the 6th Edition of Gray’s Man- ual (p. 725 c¢.), is only one of the many evidences of the critical work done by Rey. E. J. Hill and proof of the value of a long continued study of a single area. This same form was sent me last summer by W. B. Van Gorder from north shore of Bear Lake, Noble County, thus extending its local distribution. Utricularia purpurea Walt. ‘Shallow ponds, Pine Station, Lake County, Sept. 13, 1879.” (E. J. Hill.) This is another form shown by Mr. Hill to be a member of the State flora. This station for the plant is somewhat remarkable be- cause it is so far inland. While the range is ‘‘ponds, Maine to Florida,” it is limited by the additional statement, usually near the coast. Utricularia gibba L. ‘‘Sandy, wet margins of ponds, Pine Station, Lake County, Sept. 13, 1879.” (E. J. Hill.) While this plant would be naturally ex- pected within our range, it has been but rarely collected in the State. The speci- mens furnished by Mr. Hill being the only ones I have seen from Indiana. It is especially desirable that close observations should be made in favorable localities in order that the distribution of these forms within the State may be determined. Corispermum hyssopifolium L. ‘‘Dry, sandy ground, Pine Station, Ind., Sept. 4, 1893” (E. J. Hill.) The only reported station for this species. No great extension of its range throughout the State need be expected, since in our range it seems confined to the beaches of the Great Lakes, although farther west and south it is not so restricted. The form is presumably from the west, judging from available data. Salsola Kali L., var. Tragus. This plant has undoubtedly obtained a sufficient foothold in the State to be included in its flora. It is, however, very doubtful if its spread will be sufficiently rapid to give it rank among our worst weeds. The plant is definitely reported from Clarke, Lake County, by E. J. Hill, and from Avilla, Noble County, by W. B. Van Gorder. Both collections are labelled “along railroad,” indicating very clearly the method of introduction into our State flora. An examination of both specimens leads me to question the reference of the Lake County specimen. It does not agree in many particulars with the Noble County specimen, which latter is very plainly the typical variety Tragus, and so far as I am able to judge agrees more nearly with Sa/sola Kali. The exten- sion of the range—‘‘ sandy seashore, New England to Georgia”—by the addition of ‘‘and along shores of Great Lakes” is a very natural one, but is apparently (13) 194 incorrect because of the label, ‘‘ along railroad.” So far as I am able to learn, the plant has not spread with the rapidity to be expected from the variety Tragus. In view of the accuracy of Mr. Hill in all of his determinations, the Lake County station is admitted, with the suggestion that the plant in that particular locality needs a much closer study. The Noble County plant is unmistakable, not only in its characters, but in its habits of growth. From facts ascertained through the work of Supt. Van Gorder, it is safe to say that if the Russian thistle spreads throughout Indiana it will be from the Noble County station as a center. The plant has been carefully watched since its first appearance in 1893, and efforts made to prevent its spread, though with no very great success, as the following letter indicates : BRIMFIELD, INnp., Nov. 3, 1895. Mr. W. B. Van Gorder, Knightstown, Ind.: DEAR Str—In reply to yours of some time ago, will say that the Russian thistle came up again this year worse than last year. It was not cut soon enough, which, of course, scattered the seeds. I have not heard of it any place else Vietoae ors or J. EK. NiswANDER. In the last map issued by the United States Department of Agriculture, showing the distribution of the Russian Thistle, a location is given in south-cen- tral Indiana. The map is, however, so small that I have not been able to locate the station, nor have I been able to discover upon what authority it was added. In my opinion there are not more than two stations for the Russian Thistle in the State. Of these, that in Noble County alone seems to threaten any great spread of the pest. While the plant should be carefully watched, its general character as to periods of flowering and maturation of seed, taken in connection with the fact that though known to exist in Indiana since 1892, it has yet made no marked advance, would indicate that the danger from its introduction has been overestimated. Polygonum tenue Michx. ‘‘Sand hills, Pine Station, Ind., July 28, 1875.” (E. J. Hill.) Tippecanoe County, 1893. (Stanley Coulter.) This species has perhaps a more general distribution throughout the State than the references would indicate. Its normal range easily includes our territory, yet so far as I know no other stations are recorded. In a study of the genus Polygonum made re- cently I examined all of the collections in the State, and it is certainly not found in them from any other localities. The species is sufficiently characteristic to be easily separated from the more common forms, and could scarcely be confused with any other species, if we except P. ramosissimum Michx., from which it is readily distinguished by the character of the achenes. — 195 Polygonelia artieulata Meissn. ‘‘Sand hills, Miller’s, Ind, October 1, 1881. Flowers white or rose-colored.” (E. J. Hill.) This seems to be the only authen- ticated station for this species. Mr. Van Gorder includes it in his list of plants of Noble County, published in pamphlet form in 1884, but excludes it from list published in 1887 in Eighteenth Report of the State Geologist. I infer from this that its inclusion in the first list was an error. Baird and Taylor also include it in their ‘‘ Flora of Clark County,” but as they made no collections the record is necessarily a doubtful one, with the probability against the accuracy of the de- termination. The assigned range is: ‘‘ Dry,sandy soil; on the coast from Maine to New Jersey, and along the Great Lakes.” It can be readily seen that its distri- butiou in Indiana is in all probability limited to the northwestern counties. Shepherdia Canadensis Nutt. ‘‘Sand ridges, usually near sloughs. Pine Station, Lake County, May 13 and 27, 1876.” (E. J. Hill.) This attractive shrub has perhaps its southern station in this record. Its reported range is from ‘‘ Ver- mont and New York to Michigan, Minnesota and north and westward.” It is worthy of notice, perhaps, that in Indiana it occurs ‘‘near sloughs,” while in other regions it is found chiefly on rocky or gravelly banks. Euphorbia polygonifolia L. ‘‘Sandy shores of Lake Michigan, Lake County, Indiana, September 4, 1893.” (E. J. Hill.) The range of this species is probably limited to the shores of Lake Michigan, at least so far as Indiana is concerned. While in general appearance it might be easily confused with other species, it is characterized by having seeds larger than those of any other species in section Anisophylium. Myrica asplenifolia Endl. ‘‘Sand hills, Miller’s, Indiana. Flowers collected April 29 and May 30, 1882; fruit, July 4.” (E. J. Hill.) This is the only lo- cality for the State and it was upon this collection that the range of the species was extended in the sixth edition of Gray’s Manual to include Indiana. Betula papyrifera Marshall. ‘‘Sandy soil, Pine Station, Ind. Flowers col- lected May 13, 1876; fruit, September 3, 1876. Trees ten to thirty feet high.” (E. J. Hill.) The material furnished the Survey was somewhat scant, but seemed sufficient to verify the determination. The petioles were shorter, perhaps, than in the normal form, but this seemed the only deviation from type in the leaf characters. The reduction in size from a tree fifty to seventy-five feet high in the normal range, to that indicated above, is the most marked feature in this extension of range. The form also occurs in northern Illinois, but I have no data at hand which indicate whether or not a similar reduction in size occurs. The species, as is well known, is northern in its general range. 196 Pinus Banksiana Lambert. ‘‘Sand barrens, Lake County, Ind., May 13, 1876.” (E.J. Hill.) This is the only record for the gray or northern scrub pine in the State. The specimens sent the Survey establish the species as a member of the State flora beyond question. The inclusion is an extension of the reported range from Southern Michigan to Northern Indiana. It is a fact that in all prob- ability more new forms will be added to the State flora by a careful study of our forest trees than from any other group of plants, if we except, perhaps, the water plants. For various reasons forest forms have received less attention and are more poorly represented in existing herbaria than any other. It is especially urged that during the ensuing season specimens of all forest trees be furnished the Survey by those interested in the work. Orchidacee. Our knowledge of the occurrence and distribution of the various orchids of the State has been very greatly increased during the past year, a fact due largely to the labors of Messrs. Hill and Van Gorder. Both of these gentle- men have studied definite regions for years and have placed the Survey under many obligations for their careful and courteous responses to the many requests for information. I have asked Miss Alida M. Cunningham to collate the facts at hand, which she has done under the title ‘‘ Distribution of Orchidacee in Indiana,” and reference is hereby made to that article (These Proc., p. —). I wish also, in this connection, to express the thanks of the botanical division of the Biological Survey to Miss Cunningham for the patient and efficient work she has done in the study and comparison of critical forms, which has done much to expedite the work of the division and has added greatly to the value of its final report. Tofieldia glutinosa Willd. ‘‘ Moist sands. Pine Station, Ind., July 28, 1875. (E. J. Hill.) The State Catalogue refers this species to the ‘northern tier of counties.” This, however, is the only station in the state from which I have been able to secure herbarium specimens. It is included in the Flora of Noble County by W. B. Van Gorder (18th report of State Geologist, p. 66,) as growing in ‘“moist grounds along the Elkhart river in Orange township, and is represented in Mr. Van Gorder’s private herbarium. I know of no other stations in which the species occurs. The recorded range of the plant is ‘‘moist grounds, Maine to Minnesota, and northward ; also south in the Alleghanies. Triglochin maritima L. ‘‘ Wet sands, border of slough, East Chicago, June 13, 1893.” (E. J. Hill.) This species has been added to the state flora through the close work of Mr. Hill, who has recorded the only station for Indiana. The species is easily distinguished from the other members of the genus by its fruit of six carpels. The assigned range of the plant is, ‘salt marshes along the coast, : : : - Labrador to N. J., and in saline, boggy or wet places across the continent. 197 Potamogeton. Any systematist who has undertaken a study of this genus, will at once appreciate the fact that the value of specific determinations is largely in- creased if they have received the sanction of a specialist inthe group. Mr. Hill’s forms of tliis genus have undergone the scrutiny of the late Dr. Thomas Morong and may be added with confidence to the state flora. It is therefore with very great diffidence that I venture to question the determination of one or two of the sheets sent the Survey. The question is not of the original determination, but the suggestion is made that in the distribution there has been a confusion of forms. The most noteworthy species of this genus are the following: P. puleher Tuckerm. ‘‘Shallow ponds, Pine Station, Lake Co., June 21, 1884.” (E. J. Hill.) From an examination of many specimens, I am led to be- lieve that this form as received by the Survey should be referred to P. amplifolius Tuckerm, because of leaf and fruit characters. The range of the two forms is practically the same and it is possible that they may be found associated, and be- come mixed in distribution. The size of the fruit is perhaps the most apparent distinction between the two forms. In addition to P. pulcher Tuckerm, P. ampli- folius Tuckerm is also without doubt a member of the state flora. P. prelongus Wulf. Cedar Lake, Lake Co., Ind., Feb. 27, 1882. (KE. J. Hill.) This well marked form should be more generally found in the northern counties of the State. The region is fairly within the range of the plant and the ‘conditions for its occurrence are good. It has, however, been reported from no other locality, so far as I have knowledge. P. Robbinsii Oakes. ‘‘ Cedar Lake, Lake Co., Ind., June 30, 1886.” (E. J. Hill.) This is another interesting northern form added to the Indiana flora as a result of Mr. Hill’s indefatigable work. (Man. 6th edn. 735c.) In the specimen sent the Survey by Mr. Hill, both fruit and flowers are absent. From this specimen standing alone, I would refer the form to P. marinus L., since the leaf and stem characters do not conform to the description of P. Robbinsti. My very high appreciation, however, of the skill and acuteness of Mr. Hili lead me to include the form P. Robbinsii Oakes, and also to add the species P. marinus L. I am inclined to believe that a more careful study of the plants of our marsh and lake regions would result in the extension of the range of many forms in this and allied groups. Eriocaulon septangulare Withering. ‘‘Sandy borders of ponds, Laporte, Ind., July 22, 1875. Scapes 6-8 striate.” (E. J. Hill.) The addition of Indiana to the assigned range of this plant in the 6th edition of Gray’s Manual was based 198 upon the collection of Mr. Hill. During the last summer Mr. Van Gorder col- lected it in Noble County, and Mr. Bradner includes in catalogue of the Flora of Steuben County (17th Report of State Geologist, p. 156), with the statement, ‘“badly named, as the scape frequently has eight striae.” The Hill collection is of the normal size from 2-6 inches high, while that of Van Gorder shows speci- mens from 1-2 feet high, having been submersed. DISTRIBUTION OF THE ORCHIDACE® IN InpIANA. By Alida M. Cunningham. The family of Orchidacez, as shown by the reports and specimens examined, is represented in the State by twelve genera and thirty-seven species. Miecrostylis monophyllos Lindl., according to the 6th edition of Gray’s Manual, s found growing in cold swamps in northern Indiana. It is also reported from the ‘‘ Knob” region by Dr. J. M. Coulter. No specimen was examined. Microstylis ophioglossoides Nutt., has been reported from Monroe by W. S. Blatchley, whose determination is verified by specimens in the DePauw Herba- rium. One specimen of this species has been reported from Noble by W. B. Van Gorder and has been examined. Liparis liliifolia Richard, occurs in the southern and central portions of the State. It is reported as rare in Franklin by O. M. Meyncke, but common in rich, shady woods in Gibson and Posey by Dr. Schneck. No specimens of this form have been examined. Liparis Leeselii Richard, grows in extreme northern counties. Specimens from Lake by E. J. Hill and from Noble by W. B. Van Gorder were studied. Mr. Van Gorder states that it is very rare in that region and grows in tamarack marshes. Aplectrum hiemale Nutt., is reported from the following counties: Clark, Jef- ferson and Franklin in the southeast; Gibson and Posey in the southwest; Put- nam in the central; Noble and Steuben in the north. The State catalogue includes the species, referring it to Tippecanoe, but gives no authority for its in- clusion. Specimens from Clark and Noble were the only ones studied. Corallorhiza is represented in the State by three species—innata, odontorhiza and multiflora. C. innata R. Brown. No Indiana specimen of this species was examined. It is reported, however, from the “knob” region by Dr. Clapp. 199 C. odontorhiza Nutt., is reported from Gibson and Posey by Dr. Schneck as rare, and found growing in shady woods in rich soil; from Franklin, by O. M. © Meyncke; from Steuben, by E. Bradner, and from Noble, by W. B. Van Gorder, whose specimens were examined. C. multiflora Nutt., is reported from Union by W.S. Blatchley, whose determi- nation is verified by specimens in the DePauw Herbarium. From Noble, by W. B. Van Gorder, who states that it is rare in that county and grows in dry woods; and also from Steuben, by E. Bradner. The State catalogue includes this species, referring it to Jefferson, but gives no authority for its inclusion. No specimens were examined. Spiranthes is said to be represented by four species: latifolia, cernua, preecor and gracilis. S. latifolia Torr., is very limited in its range, at least as far as we have knowl- edge of its distribution. It is reported from Noble by Mr. Van Gorder, who states that only a few specimens were found. It is reported also from Tippecanoe by John Hussey, and his determination is verified by a specimen in the Purdue Herbarium. S. cernua Richard, occurs chiefly in southern and western counties. It is re- ported also from Noble, where it grows with cranberry vines on the low shores of lakes. S. precox Watson, has been reported from Clark by Messrs. Baird and Taylor, and from Steuben by E. Bradner. The 6th edition of the Manual does not in- clude Indiana in the range of this species, which reads: ‘‘ Wet, grassy places, Mass. to N. J. and Fla.” S. gracilis Bigelow, is fairly well distributed, being reported from southeast- ern, northern and central counties, but is not found abundantly. Specimens from Noble, Lake and Jefferson were examined. Goodyera repens R. Br., is reported from Steuben by E. Bradner. No speci- mens were studied, but the habit and range of the plant renders the determina- tion doubtful. Goodyera pubescens R. Br., has been collected in Noble by Mr. Van Gorder, whose specimen was examined. It is also reported from Warren and Vigo Coun- ties. Arethusa bulbosa L., is referred, in the State catalogue, to Lake Co. Dr. J. M. Coulter also reports it in the region of “‘Barrens.” This would make it a true northern form and indicate that it grew in a cool climate and in both dry, sandy soil and low ground. No specimens were examined. - 200 Calopogon pulchellus R. Br., is a northern species, being reported from St. Jo- ‘seph by Dr. Barnes, whose specimen is in the Purdue Herbarium; from Steuben by E. Bradner, and from Noble by Mr. Van Gorder, who states that it is very abundant in that county and found growing in the same locality with Pogonia ophioglossoides. Pogonia is represented by three species: ophioglossoides, pendula and verticillata. P. ophioglossoides Nutt., is another true northern form. It is reported from Lake by E. J. Hill, from Noble by W. B. Van Gorder, who reports it to be very abundant and growing in cranberry marshes and low ground along the Elkhart River, and from Steuben by E. Bradner. P. pendula Lindl., is reported from the extreme northern and extreme southern portions of the State. From Lake, by E. J. Hill, as very rare; Noble, by W. B. Van Gorder, as rare and growing in rich woods; Steuben, by E. Bradner; Gibson -and Posey, by Dr. Schneck, as rare, growing in damp, rich woods, and from Jetf- ferson, by Dr. J. M. Coulter. P. verticillata Nutt., has been reported from three counties. From Monroe by W.S. Blatchley, Jefferson by Dr. Barnes, and from Noble by W. B. Van Gorder. Specimens from Noble and Jefferson were examined. Orchis spectabile L., is the most widely distributed species in the family, being represented in twelve counties. It has been reported from the following: Jay, Delaware, Randolph and Wayne in the east; Jefferson, Clark and Monroe in the south; Noble and Steuben in the north; Putnam in the central; Franklin and Dearborn in the southeast. ; Huabenaria is represented by twelve species. H. tridentata Hook., is reported from Lake by E. J. Hill whose specimen was examined. H. virescens Spreng., is reported from Steuben by E. Bradner. No specimen of this species was examined, but its range would include it in the State list. H. bracteata R. Br. Mr. Van Gorder reports three specimens of this species from Noble. Dr. Stanley Coulter says that it is fairly abundant in Tippecanoe, being reported by almost every class. Specimens from both counties were studied. H. hyperborea R. Br., is referred to Lake in the State Catalogue, but no authority is given for its inclusion. It is probably, however, based upon the col- lection of E. J. Hill. H. Hookeri Torr., is a northern form. Mr. Van Gorder reports it from Noble. A specimen from Lake by E. J. Hill was the only one studied. Fe 201 H, orlveulata Torr., is also a northern species, being reported only from Noble, where it is very rare ani grows in rich woods. A specimen from this county was examined. H. ciliaris R. Br., is reported from St. Joseph by Dr. Barnes, from Noble by W. B. Van Gorder and from Steuben by E. Bradner. H. leucophea Gray, is reported from Noble by W. B. Van Gorder, from Steu- ben by E. Bradner and from White by J. Hussey. HI, lacera R. Br., is reported from Noble, where it grows in tamarack marshes, Hi. psycodes Gray, is limited to the eastern half of the State, being reported from Jay, Delaware and Randolph by Dr. Phinney; Clark by Baird and Taylor; Jefferson by Dr. J. M. Coulter; Noble by W. B. Van Gorder and Steuben by E. Bradner. A H. jimbriata R. Br., has been reported only from Clark by Messrs. Baird and Taylor. H. peramena Gray, is a southern and western species. A specimen from Jef- ferson was the only one studied. Cypripedium is represented by five species. C. candidum Muhl, has been reported from Steuben by E. Bradner, and also from Gibson and Posey by Dr. Schneck, who states that it was at one time very common in that locality, but is rapidly disappearing. C, parviflorum Salisb., is reported from Lake and Noble in the north; Dearborn in the southeast; Gibson and Posey in the southwest. In Noble it is rare and grows in birch marshes. It was at one time common in Gibson and Posey, but is becoming rare. C. pubescens Willd., grows in northern and central counties. It was, at one time, common in Franklin, but is becoming rare. Mr. Van Gorder states that it is very common in dry woods in Noble C. spectabile Salisb., is another extreme northern species. It is found in Noble growing in moist, shady places of tamarack swamps and bogs. It is re- ported also from Steuben by E. Bradner. C. acaule Ait., has been collected in Noble by W. B. Van Gorder whose speci- men was examined. It is also reported from Lake. Out of the thirty-seven species named in this paper twenty-seven have been verified by herbarium specimens. Most of the others doubtless occur in the State, as they have been reported by good authorities. From these facts we find that the following species are found only in the region north of an imaginary line drawn east and west through Indianapolis: 202 Liparis Leeselii, Spiranthes latifolia, GGoodyera repens, Arethusa bulbosa, Calopo- gon pulchellus, Pogonia ophioglossoides, Habenaria tridentata, H. virescens, ‘H. bracteata, H. Hookeri, H. orbiculata, H. ciliaris, H. leucophea, H. lacera, Cypripedium spectabile and C. acaule. Of these the following are confined ex- clusively to the northern tier of counties: Goodyera repens, Arethusa bulbosa, Habenaria tridentata, H. virescens and H. hyperborea. . The following are reported only in the region south of the above named line: Microstylis ophioglossoides, Liparis liliifolia, Corallorhiza innata, Habenaria fim- briata and H. peramcena. Habenaria fimbriata is confined exclusively to counties bordering on the Ohio river. Habenaria virescens and Goodyera repens are reported only from Steuben County, and need verifying specimens to support the reference. Three species, viz., Arethusa bulbosa, Habenaria tridentata and H. hyper- borea, are reported exclusively from the western portion of the State, yet it isa noteworthy fact that all three come from Lake County, and are doubtless ex- clusively northern species. In all probability a careful study of the flora of the northeastern counties would show no division between the eastern and western species. FIRST REPORT OF THE BIOLOGICAL STATION. ConNTENTsS.—Drrectors’ First REPORT oF BIOLOGICAL STATION. Part PART PART Introductory. Acknowledgments. Equipment. Plankton net. Sounding apparatus. Additional equipment. Plan of work. J.—Turkey Lake as A Unit oF ENVIRONMENT. Introductory. Orientation. General features. Size. Relation of water to outflow and evaporation. Constancy of Turkey Lake as a unit of environment. 203 A Preliminary Report on the Physical Features of Turkey Lake—D. C. Ridgley. Hydrographic map of Turkey Lake—C. Juday. Temperature of Turkey Lake—J. P. Dolan. IJ.—TueE INHABITANTS OF TURKEY JAKE. Note on Plankton—C. H. Eigenmann. General Fauna—C. H. Eigenmann. Leeches—Mrs. B. C. Ridgley. Rotifera—D. S. Kellicott. Cladocera—E. A. Birge. Decapoda—W. P. Hay. Mollusca —R. E. Call. Fishes—C. H. Eigenmann. Batrachia—C. Atkinson. Snakes—G. Reddick. Turtles—C. H. Eigenmann. Water Birds—F. M. Chamberlain. TI].—VaRIaATION. The study of Variation—C. H. Eigenmann. Variation of Etheostoma caprodes—W. J. Moenkhaus. 204 TURKEY LAKE* AS A UNIT OF ENVIRONMENT, AND THE VARIATION OF ITS INHABITANTS. Frrst Report oF THE INDIANA University BroLocican Station. By C. H. EIGENMANN. 1 Inrropuctory.—At the last meeting of the Academy I outlined a plan for the future work of the zodlogical section of the biological survey of Indiana. It was, in brief, to study some lake as a unit of environment and the variation of its inhabitants. This plan has materialized, and I present this as the Biological Sta- tion’s first report. To select a suitable site I visited, in February, 1895, lakes Maxinkuckee, Eagle and Turkey. The lakes were frozen over, and I had a good long walk over Max- inkuckee and a sleigh ride over Turkey Lake. Turkey Lake seemed well suited for a starting point for the work in hand. In March I again visited this lake to look for a suitable laboratory and quarters. A laboratory was found in a large boat-house belonging to Mr. T. J. Vawter, the owner of Vawter Park. The boat- house is directly on the water’s edge, in about 86° 18’ east longitude and 41° 23.57 north latitude. In March the lake was still frozen over with but a narrow rim of free water near the shore. When I again visited the lake, to make the final ar- rangements, on the 30th of May, and captured snakes, turtles, frogs, and two spe- cies of spawning fishes, all within a hundred feet of the laboratory door, I was convinced that no mistake had been made in the selection of a locality. Deep water near the laboratory, a spring at the laboratory door, the situation of the laboratory nearly eyuidistant from either end of the lake, high land all about the laboratory, the nearness of such large bodies of water as Lake Tippecanoe of an- other river system, and a large number of smaller lakelets within a mile of Turkey Lake, all contributed to make the location selected as near perfect as could be ex- pected. “The only recorded name of this lake seem: to be Turkey. It appears so in the govern- ment surveys of 1838, and on all the maps published since that time. I am told that it re- ceived that name from the fancied resemblance of the general outline of the lake to a Thanksgiving turkey. During the last few years the lake has been known to those person- ally acquainted with it as Lake Wawasee, and there seems to be a laudable ambition that this latter name should supplant the homlier, but more significant, name of Turkey. The lower lake is locally known as Syracuse Lake. : The following letter was received from the Director of the Bureau of American Ethnology: In response to your letter of December 6th last, I beg leave to inform you that the word “‘ wa-wi-see,”’ ‘‘ wa-wi-si”’ or ‘‘ wa-wa-sing,’’ signifies ‘ at the bend of a river.’ Yours with respect, J.W. PowELL. +Contributions from the Zoilogical Laboratory of the Indiana University, No. 14. 205 A twelve-room cottage was rented, in which fifteen of the members of the Station besides my family were quartered. While a summer cottage, thus peopled, is not a good place for consecutive thinking, this experience will also be remem- bered with pleasure. Most of the students rented a large dining tent and hired a cook. Others tented and boarded themselves. Their expenses ranged from $1.25 to $3 per week. The laboratory was open from June 25 to September 1. ACKNOWLEDGMENTS.—Mr. T. J. Vawter, besides placing the boat house at our disposal, gave us camping ground just back of the laboratory, and assisted us in various ways, both in fitting up the Station and during the entire summer. I am under many obligations to the officers of the Baltimore & Ohio, the Vandalia and the Michigan Division of the Big Four for transportation over their lines leading to Vawter Park, and for other favors. During our stay at Tippecanoe Mr. W. S. Standish assisted us very materially. He took the whole party on a tour of general inspection about the lake from end to end, and placed himself and his steamer at our disposal during our entire stay. The Pottawatomie Club granted us the use of their reception room, where some of the lectures were delivered. Professors Birge, Kellicott and Call have prepared accounts of material col- lected during the summer. I must especially thank Dr. J. C. Arthur, Dr. G. Baur and Geologist Willis Blatehley, who visited the Station to deliver lectures before the members. Lastly, | am indebted to Mr. J. P. Dolan, superintendent of the Syracuse schools. He first directly, and through Mr. Eli Lilly, of Indianapolis, called my attention to Turkey Lake, met me at Warsaw, and guided me to the lake and over and around it on my first visit. During the summer he furnished the Station with a splendid row-boat, and by his knowledge of the lake and its surroundings and personal acquaintance with the natives contributed much to the success of the undertaking. EquipMENT.—The equipment of the Station consisted of a room 18x30 feet, with six windows on a side. In this space the twenty-two members of the Station were provided with tables. Continuous with this available laboratory space was a space 18x20, opening by very wide doors to the lake front. This space was util- ized for storing apparatus. The apparatus, nearly all furnished by the Indiana University, was as follows: Compound microscopes (Zeiss), 21 ; dissecting micro- scopes, 3; microtome, 1; dredge, 1; plankton net, 1; Birge net, 1; dipnets; re- agents, about 200 bottles; working library, about 200 volumes; Wilder’s protected thermometer, 1; lamps, glassware, etc., the usual equipment of a laboratory 206 table; two boats; one sounding machine. The plankton net and sounding appa- ratus and the method of using them may be described here. PLANKTON Net.—An idea of our plankton apparatus and its modus operandi can be gathered from one of the illustrations. The sounding boat was fitted in the stern with a swinging derrick. Through the end of this was attached a pulley, through which the rope supporting the net passed. The derrick was high enough to allow the net to swing clear of the sides of the boat, so that when a haul had been made, the net could be swung forward over a tray of tubes, ready to receive the condensed plankton. The depth through which hauls were made could be ascertained either by means of the sounding apparatus or by the direct measurement of the plankton rope. The plankton net was built essentially as devised by Hensen and Apstein, except that the straining net of No. 20 silk bolt- ing cloth, Dufour’s, was permanently attached to the truncated cone of canvas. The bucket which receives the plankton was from necessity greatly simplified, but as no measurements were made with it, and further improvement, both in effi- ciency and simplicity, have heen devised, I will describe this instrument as it will be made for next summer. The diameter of the bucket will be made one and one-half inches. Its bot- tom will be of a sheet of brass or copper, hammered so that it will be slightly concave or cup-shaped. A hole will be punched from the inside and provided with a nipple soldered on the outside. The sides of the bucket will be made of one piece of wire net of the same caliber as the No. 20 bolting cloth of Dufour.* The upper part of the bucket will consist of a flat brass or copper ring soldered to the wire sides, and provided with openings through which the binding screws, fastening the whole bucket to the net, may pass. Three legs of narrow strips of cop- per passing from the upper ring along the sides of the bucket, being also fastened to the bottom, will give rigidity to the sides and form a support for the bucket when it is being emptied. To the nipple at the bottom of the bucket will be attached a short rubber tube. The opening in the bottom will be closed with a tight-fitting rubber stopper, manipulated from aboye by a glass rod passing through its mid- dle. The whole cost of the bucket need not exceed $3.50. The estimate received on one of Hensen’s pattern was $25. * Only part of the sides were made of the wire netting during the past summer. A piece of new bolting cloth was found to have 83 per cent. of its surface solid, 17 per cent. being open for the passage of water. The wire cloth used during the past summer had 77 per cent. of its surface solid, 23 per cent. being open for the passage of water. Repeated trials of forcing water thick with plankton through the bolting cloth and through the wire showed that the wire was under such conditions a more effective strainer than the cloth. 207 SounpInG APPARATUS AND METHOD oF UsinG 1T.—A flat-bottomed boat capable of running into shore at all points was manned by three persons. One who was an expert and steady oarsman at the oars, one in the stern to take notes and steer, and one in the bow to make the soundings. The sounding apparatus consisted of a wheel two inches wide with a circumference at the bottom of a flat marginal groove of one foot ten inches. (It had been ordered with a circumference of two feet.) On the drum was wound 175 feet of fine annealed wire. This, when wound, formed less than two layers over all parts of the drum. The weight con- sisted of a round pebble as large as a fist and was tied in a piece of cheese cloth. This was a very simple and efficient piece of apparatus. The weight, if lost, could easily be replaced by one of several others carried along, and the wire was found sufficient for the whole summer’s work. The original cost plus the cost incident to its operation did not exceed $1.50. The wheel was provided with a crank and being of a definite circumference the depth was measured by the number of turns it took to raise the weight from the bottom to the surface. This apparatus would be efficient in any lake of moderate depth. To run a line of soandings the bear- ing to the objective point on the distant shore were taken from the starting point with a compass. The oarsman pulled thirty strokes, backed water and held the boat. A sounding was made in the bow and the depth recorded by the man in the stern. It was found that with the boat always used for the purpose, manned as above in calm weather, when all the sounding was done, 30 strokes moved the boat 300 feet. This method proved entirely satisfactory in short lines a mile and a half in length. In long lines it proved unsatisfactory. ADDITIONS TO THE EQuipMENT. A new laboratory 18x55 feet, two stories high, will be ready for occupation by June 1 of 1896. A partial description of new apparatus devised for next summer’s work may be given. One flat-bottomed boat similar to sounding boat, 12 feet, 2 oars. One flat-bottomed boat 15 feet, four oars. Plankton apparatus. Three glass-bottomed galvanized iron boats about 12 inches in diameter to explore bottom. One galvanized iron tube 2 inches by 20 feet, glass ends and funnels for fill- ing or emptying, to determine color of water. \ Automatic recording apparatus to observe seiches. PLAN oF WorK.—It must be understood that the undertaking was quite expensive both in time and in money. The Indiana University endorsed the plans and lent apparatus from the zodlogical laboratory with the provision that 208 the Station be of no expense to the University. At the end of the season the Uni- versity paid for some of the apparatus specially designed for the Station, which thus became the permanent property of the University. In order to defray ex- penses, a series of courses in elementary and advanced instruction were offered and given. Each one of the advanced students and the instructors took charge of some particular work of the survey. The preliminary reports of some of these, form part of this first report. The work was distributed as follows: C. H. Eigenmann, Director. W. J. Moenkhaus, Variations in Etheostoma. F. M. Chamberlain, Variations in Lepomis. J. H. Voris, Variations in Pimephales. D. C. Ridgley, Physical Survey and Variations in Micropterus. Bessie C. Ridgley, Variations in Labidesthes. Thom. Large, Physical Suryey and Variations in Fundulus. Chancy Juday, Physical Survey and Planktonist. Curtis Atkinson, Variations in Batrachians. H. G. Reddick, Variations in Reptiles. O. M. Meincke, Botanist. J. P. Dolan, Meteorologist. The work of but few has progressed far enough to justify even ‘‘forlaiufige” notices. We have but just begun our work, and the Station will remain at least three years longer at the same place. Excursions were made to lakes Tippecanoe, Webster, and Shoe in the Mississippi basins. While much of this report is taken up with the physical features of the lake, and the enumeration of the inhabitants, it must be borne in mind that the phy- sical studies are merely a means to an end. That however interesting in them- selves, to us they are only interesting as far as they form part of the environment of the highest creatures making the lake their permanent home. It may even be that some of the things considered or to be considered, form in reality no part of the environment of the vertebrates, 7. e., that they in no way affect them, but this is a matter that must be determined, and for the present we must”consider as many things as may influence them. The things probably most directly influenc- ing the higher forms to be found in a lake are light, temperature and food. The last item is again conditioned as the highest forms are, so that nothing short of a complete understanding of the conditions will be sufficient. A lake seemed to me the ideal place because here the changes due to light, temperature, change of water or surface are reduced to the minimum to be found in this latitude. A 209 small lake is better than a large lake, because the unknown elements can be re- duced to a smaller number. We have attempted to collect specimens of the higher creatures in such numbers and sizes, that had we collected all the specimens in the lake, our results would not be different. How far we have succeeded in this remains to be seen. _ The main object of the Station is the study of the variation of the non-migra- tory inhabitants. I may be permitted to quote here the plan as stated in the circular issued by the Station last spring. The main object of the Station will be the study of variation. For this pur- pose a small lake will present a limited, well circumscribed locality, within which the difference of environmental influences will be reducedtoa minimum. Thestudy will consist in the determination of the extent of variation in the non-migratory ver- tebrates, the kind of variation, whether continuous or discontinuous, the quantita- tive variation, and the direction of variation. In this way it is hoped to survey a base line which can be utilized in studying the variation of the same species throughout their distribution. This study should be carried on for a series of years, or at least be repeated at definite intervals to determine the annual or periodic variation from the mean. A comparison of this variation in the same animals in other similarly limited and well circumscribed areas, and the correla- tion of the variation of a number of species in these areas will demonstrate the influence of the changed environment, and will be a simple, inexpensive substi- tute for much expensive experimental work. For this work the situation of Lake Wawasee, surrounded as it is by other lakes, some of them belonging to other river basins will be admirably adapted. In connection with this study of the developed forms, the variation in the de- velopment itself will receive attention. For instance the variation in segmenta- tion, the frequency of such variation, and the relation of such variation in the development to the variation in the adult, and the mechanical causes affecting variation. This plan will be moditied as our knowledge grows and our experiences dictate. PART I. THE LAKE AS A UNIT OF ENVIRONMENT. Intropuctory.—A lake is a depression in the ground filled with water more or less stagnant. A glance at a good map of North America will show the following peculiar- ities in the distribution of lakes: I. A large number of lakes are found in Florida. (14) 210 II. A host of them are distributed in northern United States and Canada, including the greatest collection of fresh waters on the globe. If. A good number in the Sierra Nevada and the Rocky Mountains. The remainder of the country from the southern boundary of Georgia to the northern boundary of Pennsylvania west to the Rockies is practically free from lakes, except IV. along either side of the lower Mississippi and Red Rivers. These four groups of lakes are due to four different methods of lake forma- tion. but all four are indicative of the fact that the lake-rich areas have under- gone recent change. The first series is due to the comparatively recent elevation of an irregular ocean floor. The second series is due to the action of ice in the irregular gouging and irregular dumping of debris. These are all of recent date, probably none of them being over 10,000 years old. The third series is due to the exigencies of mountain formations, including in this plication and plication hollows, craters and lava flows and the settling of small areas. The fourth is due to the change of channel on the part of the Mississippi and to the debris brought down by the Red River which it has deposited at the mouths of its tributaries.* Of course the lakes of one of these regions need not be all of the same origin. Small lakelets around Lake Tahoe in the Sierra Nevada are certainly due to the gouging action of glaciers coming from a steep incline onto a comparatively level plain. Generally speaking, mountain regions, unless, as in the case of the Appalachian, they have outgrown their lake stage, contain lakes of the greatest diversity of origin. . Lakes are of interest to the geologist to determine the particular way in which a general cause has been modified to produce a particular effect at any particular lake; to the physicist to account for the various colors, temperatures, pressures, reflections, refractions, etc.; to the chemist to determine the degree of concentration of minerals and gases in solution; they are of interest to the naturalist to determine the organic inhabitants, their quantity and kind and their life histories; to the cecologist and evolutionist to determine the geological, physical and chemical characters in their effect on the organic inhabitants and these on each other. Lakes may therefore be studied for other than purely economic interests, such as water supplies and highways for commerce or location of summer resorts. * The facts for the foregoing have largely been drawn from Russell’s American Lakes. Ginn & Co., 1895. 211 ORIENTATION.—A hight of land (morain) extends from the northeastern corner ot Indiana directly southwest to south of Albion in Noble County, and from here westward between Turkey Lake and Tippecanoe Lake, then northwest through Nappanee in Elkhart County to near South Bend. In its range from the north- eastern corner to south of Albion this ridge separates the Lake Michigan from the Lake Erie basin. West of this it separates Lake Michigan basin from the Ohio basin, and still farther west from the Mississippi basin proper. In the eastern half of Indiana this ridge is exceedingly rich in lakes. Most of these lie on the northern side of the divide, but about the headwaters of the Tippecanoe and Blue rivers many are also found on the south side of the divide. A glance at the map leaves the impression that this region is low and swampy, while in reality this whole region forms one of the highlands of Indiana, a considerable part being over 1,000 feet high. Turkey Lake is the most western lake of this series lying north of the divide. It lies in Turkey Creek Township, in the northeastern corner of Kosciusko ’ County. South of the ridge separating the Mississippi and St. Lawrence basins at this point lie Webster and Tippecanoe lakes, and south of these the Barber lakes and Shoe Lake. Between the crest of the ridge aud Turkey Lake the country is pitted and grooved. Many of the pits are filled with water, forming ponds of various sizes. One.of these has recently been drained. Many more lakelets are found about the head of Turkey Lake, but the topography of this region will be dealt with in one of the following reports. This whole region gives one the im- pression that it has changed but little since the ice left it. GENERAL FEATURES.—The lake has a general trend from southeast to north- west. It is divided by a wide stretch of very shallow water, which is fast being reclaimed by various water plants. A deeper channel extends through this swampy region, connecting the upper and lower portions. The greatest length from the head of Turkey Lake to the end of Syracuse Lake is tive and one-half miles. The width, measured at right angles to such a line, rarely exceeds a mile. The greatest width is just east of Ogden Point, where it measures one and a half miles. The length of Turkey Lake from Mineral Point to Conkling Hill is about four miles. The total shore line is between twenty and twenty-one miles. The excellent map prepared by Messrs. Juday and Ridgley, based as it is on numerous soundings, shows the lake bottom to be of the same rolling character as the surrounding region. A lowering of the surface of the lake ten feet would make the long stretch of territory between Syracuse and Turkey lakes dry land, and make the lake entirely landlocked. 212 The similarity of the lake bottom to the surrounding country, which seems to have been little changed by erosion, makes it quite certain that the lake basin is due to the irregular dumping in a terminal moraine, parts of it containing deeper kettle holes. The lake was never much more extensive than now. There are evidences that the surface was a few feet higher. These will be considered in a later report. The lake is surrounded by extensive swamps on the east, north, and west; these would practically all be covered by water should the surface of the lake be raised five feet. The hydrographic basin is so small that at present but seven inches of water are removed from the surface by outflow, while thirty are removed by evap~ oration. The lake having a surface of 5.6 square miles, an increase of this sur- face by =, or about one and a third square miles, would be sufficient to allow all the water coming into the lake to be lost by evaporation except in wet seasons- The surface of the lake, therefore, can not have been very much higher than at present if the present precipitation and evaporation have been constant since the ice left this region. The lake has been about six or seven feet lower, having been raised to its present height by the building of a dam across its outlet. The changes due to this dam and to the encroachment of plants will be considered in another report. Size.—The total area now under water is 5.659722 square miles. This area was obtained by weighing a sheet of paper of uniform thickness and of the shape of the whole area to be calculated, and comparing this weight with the weight of a square of the same paper covering a square mile. This method is much more expeditious than calculating such an irregular body as these lakes in the absence of a planimeter, and quite as exact. ‘The same method was used in determining the areas below which there is a certain depth of water, with the following results: Depth of Area in Amount of Water Water. Square Miles. in Cubic Miles. TETAS ee aa singe ane moe ome dae corso sr achO or B20 .00310395 OHO. Eeiiae wicks Seo toe eeroat Dantes apna Hane Pot -59027 .00167690 DAT SSY a ets oe eae yentosean clo cher a icheite eo auto Cac RIOR c .62500 .00314867 CYjEU (nian Sa enn 5 oS edmeo boe.c Gab ome S ocbo ot .45833 .00303817 ZN VR Oi AO Rel eee orn MOI OG Dano oda codd od .39583, .00337165 ILCs By oop elom oo oe pd ms ooms ecmomeo oto aot .22918 .00231162 GO LOGO Ais ait ache cies eke seria chee) era lee Mane 0694 .00082026 5.64576 .0174712 Brror tobe. distributed® . 24). 245-262 2-e- .1396 5.65972 oe 213 Forel (Faune profonde des lacs Suisses, p. 5) proposed to estimate the volume of a lake by comparing it with a cone whose height is the maximum depth, and whose base is the surface of the lake. Estimated in this way he found the cone gave but .67 of the actual volume of Lake Geneva. A similar estimate for Tur- key Lake will give us .024654 cubic miles, or considerably more than the actual value. The average depth obtained by dividing the cubic contents by the surface gives us 16.6 feet. All these measurements were made during the summer of 1895 when the lake was below the average height, so that 17 feet will probably be nearer the average depth. It will be found that by another method Mr. Ridgley obtained 21 feet as the average depth. Over half the area contains water less than 10 feet deep. A reduction of thirty feet below the present level would reduce the lake to a Y-shaped figure ex- tending nearly from end to end of the present lake. One of the horns of the Y would extend to Crow’s Bay, the other to Mineral Point. The base of the figure would lie to the west of Black Stump Point. Between the horns of the Y we should have a peninsula continuous with Morrison’s Island, which is the last of a series of islands left in the lake. During the ancient history of the lake the land about Buttermilk Point was an island, and ridges of land east and west of this formed the islands. One of these is seen in the illustration. The detailed descrip- tion of the hydrography of the lake will be given in the map and Mr. R:dgley’s report. RELATION OF WATER TO OUTFLOW AND EvAporation.—Without any addi- tion to the water of the lake the quantity now in the lake would be sufficient to supply the present outlet for 26 years.* In other words, every cubic foot of water entering the lake will remain in it on an average of twenty-six years, unless removed by evaporation. Ridgley esti- mates that the inflow from springs equals the outflow, yet the lake was observed to fall on an average of one-quarter inch per day, rising of course during rains. That the outflow will not account for the fall of the lake is sufficiently shown by the fact that the calculated fall due to the outflow is but .0016 inches per day. (See Ridgley’s report). The remainder of the fall must be due to evaporation and seepage, very largely to the former. Attempts were made to estimate the amount of evaporation from the surface, but they proved failures. It is self-evi- dent that simply exposing water in an open dish will not answer the purpose of estimating the amount of evaporation in the lake for the reason that water in a shallow dish is heated to very different degrees from the water of the lake. An “Based on Ridgley’s and Juday’s estimate of the outflow, and my estimate of the lake’s contents. 214 apparatus which promised to measure the evaporation accurately and at the same time do several other things was devised, but it proved a failure because it could not be well protected in rough weather and still maintain natural conditions. The apparatus which we hope we shall be able to perfect is as follows: A glass jar 9 inches in diameter and 12 inches high with a small hole near the bottom and open at the top is sunk into the lake to within two inches of its top. When the water in the jar has reached the level of the lake water a tight rubber stopper is inserted in the small opening from without. The column of water in such a jar would be as near as possible under the same conditions as the surround- - ing water, and the fall of the water in the jar, plus the amount of rainfall for the period, would very closely approximate the amount of evaporation. This appa- ratus would also enable one to get at the amount of water received from springs and other sources aside from rain falling directly into the lake. The amount of reduction due to outflow from the lake can readily be calculated by observing the outlet. Mr. Ridgley has estimated it at .0017 inches per day. If at the end of thirty days there was a difference between the water in the jar and the water in the lake, less the calculated reduction of the lake due to outflow, the difference would represent the inflow from springs and other tributaries during thirty days. The lake is frozen over about four months in a year. During the remaining eight months evaporation is going on at a maximum rate of one-fourth inch per day and a minimun of 0. Taking one-eighth inch per day as the average, we obtain about thirty inches as the amount of the annual evaporation. At this rate the lake, if without income, would become dry in twenty-eight years. Four years would reduce the lake to half its present size. Outflow and evaporation operating together would reduce the level at the fol- lowing rate: BONN ear rae Reduction by Reduction by : Time in Years. Guilaw: Evaporation. Total Reduction. 3 Tees eShaite dotte loins 9 ft. Some 3 4 7 6 ia! 6 2 2 2 5 8 2 2 4 8 5 9 8 2 6 8 5 11 8 1 5 2 2 6 Uta 6 1 about 17 a 2 6 10 1 14 33 2 35 68 215 These figures do not claim any great degree of accuracy; they simply help to form an estimate of the length of time it would take both the outflow and evaporation together to empty the lake. But while it would take both the out- flow and the evaporation fourteen years to empty the lake, one-fourteenth does not express the per cent. of the water of the lake changed annually under present conditions. Since the vertical reduction is the same whether the surface is large or small, it is evident that a much larger amount would be evaporated while the surface is large. In reality, if a bulk were to be taken from the lake equal to the outflow, plus the evaporation over the present area, about six years would be suf- ficient to empty the lake, or, to put it in other words, during average years every cubic foot of water entering the lake remains on an average six years. During very wet seasons the amount of loss may reach a much larger proportion of the whole contents. Constancy oF TurRKEY LAKE as A Unit OF ENVIRONMENT.—From the preceding chapter it must be evident that the conditions in the lake, from month to month and from year to year are but little changed, that the conditions, as far as the water is concerned, are remarkably constant, especially if we compare these conditions to those obtaining in the lower courses of such rivers as the Wabash or the Lllinois. In the early part of this century a dam was built across the mouth of the outlet forming an effective barrier to the ingress of fishes from below. The lakes being at the headwaters, nothing has entered it from above. A few forms were planted in recent years by Col. Lilly of Indianapolis. The level of the lake was changed by the building of the dam, and as late as 1840 trees were standing in water six to seven feet deep. Many of the stumps still remain. Their location and the effect of the dam upon the lake will be dis- cussed elsewhere. - WORKS CONSULTED. Agassiz, A. Hydrographic Sketch of Lake Titicaca. Proc. Am. Acad. Art and Sci, XI, 11, 283-292; 1876. Agassiz, L. Lake Superior. Belloc, M. BE. Les lacs de Caillaouas et ceux de la region des Gourgs-Blanes et de Cladabide. Assoc. Francaise 9 Aout, 1893. Belloc, M. E. Nouvelles recherches lacustres feites au Port de Venasque dans le haut Aragon et dans la haute Catalogne. Assoc. Francaise 9 Aout, 1893. Comstoc, C. B. Professional papers corps of engineers U. S. A., No. 24, Primary triangulations U. S. lake survey. Washington, 1882. 216 Davis, W. M. The classification of lakes.. Supplement in Russell, 1895. Evermann, B. W. The investigation of Rivers and Lakes with Reference to the Fish Environment. Bull. U. S. Fish. Comm., 69-73, 1893. Forbes, S. A. Biennial Report Illinois State Laboratory, 1893-94. Forel, F. A. Algemeine Biologie eines Siisswassersees, in Zacharias die Thier und Pflanzenwelt des Siisswassers. Leipzig, 1891. Forel, F. A. Le Leman, Tome premier, 1892; Tome second, 1895. Lau- sanne. Le Conte, John. Physical studies of Lake Tahoe. Overland Monthly, 1883, 1884. Levette, G. M. Observations on the depth and temperature of some of the lakes of Northern Indiana. Geological Survey of Indiana, 1875. Reighard, J. E. A biological examination of Lake St. Claire. Bull. Mich. Fish Comm. Russel, I. C. Lakes of North America. Ginn & Co., Boston, 1895. Seligo, A. Hydrobiologische Untersuchungen I. Schrifte der naturf., Ges. Danzig, N. F. Bd. VII, 1143-89, 1890. Tarr. Ralph S. Lake Cayuga a rock basin. Geol. Soc. Am.,.Bull., Vol. 5, 1894, pp. 339-356. Whipple, G. C. Some observations of the temperature of surface waters, and the effect of temperature on the growth of micro-organisms. J. New Engl. Water Works Assoc. LX, No. 4. é A PRELIMINARY REPORT ON THE PHysicAL FEATURES OF TURKEY LAKE. By DC eRinGEny.— ACKNOWLEDGMENTS. Most of the data on which this preliminary report is based were collected during the summer of 1895 at the Indiana University Biological Station at Vawter Park, Kosciusko County, Indiana, under the direction of Dr. Carl H. Eigenmann. I wish to acknowledge the aid of his valuable suggestions, both in the collection of the data and the preparation of the report. I wish to acknowledge also the * Contributions from the Zodlogical Laboratory of the Indiana University, No. l5a. PEATE I: , Inp1ana UNIVERSITY BioLoGic4sL STATION. No. 2. INTERIOR OF THE LABORATORY. PLATE Il. No. 3. No 4. Buack Stump Point FROM THE LABORATURY. PLANKTON Boar. PLATE lil. No. 5. Looxinc TowarpD OGDEN PornT FROM THE LasoraTORY. PLANKTONIBOaT IN. FOREWATER. No. 6. OcGpEN Pornt rrom NEAR THE PoTTawaToMIEe CLus-HovwsE. PLATE IV. StupDENTS’ Camp IN VAWTER PARK. PLATE V. “IL ‘AMV S,1TAZLUVH ‘1 ‘ONVT 8. 1TAZLUVH “Il ‘av S ULAZLUVH “aGNVISI G10 “H4VT S UHdOOH “AMVT AMMAN “UNV SXVO 8. No. “HNV'T AUMUAT, 1O GVAF{ LY ANIVUOP, HOUT MALA TVUANAY PLATE VI. No. 9. West Beacu oF Morrison’s ISLAnpD. No. 10. Crow’s Bay SHowine Ice BEACHES. PLATE VII. No. 11. CEDAR Porn. No. 12. Beacu West oF CEDAR POINT. PLATE VIII. No. 13. In THE CHANNEL BETWEEN TURKEY AND Syracuse LaAkEs. No, 14. Av THE HEAD oF Syracusk Lakr. 217 assistance of Mr. Chauncey Juday, Mr. Thomas Large and others in taking the soundings of the lake; of Mr. Juday, in making a survey of the shore and for copies of the accompanying map with which he has furnished me and from which the report on the topography of the bottom is largely drawn; of Mr. J. P. Dolan for records of daily observations of lake phenomena and for the history of the ‘lake in years past; of the officials of the Baltimore & Ohio Railroad who fur- ‘nished data with reference to elevations and whose generosity has made it possible for me to make frequent visits to the lake during the winter. GENERAL FEATURES OF THE LAKE. Turkey Lake is made up of two parts, connected by a channel. The channel is three-quarters of a mile in length and from one hundred feet to a half mile in width. Its depth varies from one to five feet. The part of the Lake north of the channel is known as Syracuse Lake. It includes an area,of three-quarters of a square mile, which is approximately one-eighth of the area of the entire Lake. The larger part of the Lake, to the south and east of the channel, may be known as the main lake. The general direction of the lake is from southeast to northwest. Its greatest length is five and a half miles, and its greatest width at a right angle to its length is one and a half miles. The entire shore line is between twenty and twenty-one miles in length, and the area of the lake is a little more than five and a half square miles. No very prominent irregularities occur around Syracuse Lake, while in the main lake a number of evident indentations are to be found. The east end of the main-lake is made up of three bays. Johnson’s Bay, extending to the north, is one mile long and three-eighths of a mile wide. Ogden Point lies to the west of the entrance of this bay and Cedar Point to the east. The east end of the main lake is Crow’s Bay, with Cedar Point on its north and Morrison’s Island on its south. Jarrett’s Bay extends to the southeast, with Morrison’s Island to the east of its entrance and Clark’s Point to the west. In the west end of the main lake is Conkling Bay, circular in form and with the surrounding marsh a half mile in diameter. It lies south of Conkling Hill. These are the most prom- inent indentations. Between the channel and Ogden Point, which are two and a quarter miles apart, the shore line curves gently northward three-quarters of a mile, forming Sunset Bay. Between Clark’s Point and Black Stump Point, one and three-quarters miles to the northwest, the shore line bends southward one- third of a mile. 218 a The following places are located for convenience in referring to different parts of the shore line and lake: The town of Syracuse lies on the west side of Syracuse Lake near Turkey Creek, the outlet of the lake. Pickwick Park is on the north shore of the main lake a half mile east of the channel. Eppert’s is 1,000 feet east of Pickwick Park, and nearly a half mile further east is Jones’ Landing. Three-fourths of a mile east of Jones’ Landing is Wawasee. Jarrett’s — Landing is at the middle of the southern extremity of Jarrett’s Bay. Vawter® Park is a half mile west of Clark’s Point and directly south of Wawasee. The laboratory of the Indiana University Biological Station is located on the shore of the lake near the west end of Vawter Park. TOPOGRAPHY OF THE BOTTOM. The data from which the topography of the bottom has been determined con- sist of numerous soundings taken throughout the lake between June 29 and Au- - gust 21, 1895. The water was very low during this period. For our purpose we may consider all soundings taken when the lake had the level of July 6, 1895. This level has been marked and is used for a bench line from which to read the fluctuations in level On August 21 the lake had receded 5 inches from this level. Soundings were taken along 28 lines in the main lake and 4 lines in Syracuse Lake. These soundings were taken about 300 feet apart along all lines. Where water deeper than 60 feet was found, numerous soundings were made to determine the extent of such areas. Below is given the number and location of each line along which soundings were taken, except No. 3 and No. 9 in the main lake, neither of which was used in drawing contour lines or in computing average depth. No. of Line. DWrID Ore De He wre IN MAIN LAKE. LocaTION. 7 From Biological Station to Ogden Point, North 37° East. From Ogden Point to east end of Crow’s Bay, South 53° East. From Biological Station to Wawasee, North. _ From Wawasee to Black Stump Point, South 52° West. From Biological Station to Cedar Point, North 64° East. From Cedar Point to Morrison’s Island, South. From Morrison’s Island to northeast corner of Crow’s Bay, North 8° East. From south end of Jarrett’s Bay to mouth of Bay, North 7° West. From east margin of Ogden Point to north end of Johnson’s Bay, North 1° West. From north end of Johnson’s Bay to mouth of Bay, South 10° East. From east side of Ogden Point across Johnson’s Bay, North 60° East. From middle of east side of Johnson’s Bay, across the Bay, North 79° West. From Clark’s Point to Morrison’s Island, East. From mouth of Turkey Creek across Jarrett’s Bay, West. From a point 3 of a mile west of Biological Station across the lake, North. From Clark’s Point to east side of Ogden Point, North 53° East. From point a half mile east of Biological Station, North. From Ogden Point to Black Stump Point, North 83° West. Fiom west side of Jarrett’s Bay to Mineral Point, East. From Clark’s Point to east side of Johnson’s Bay, North 30° East. From north end of No. 22 to Ogden Point, South 85° West, From point one-half mile west of Wawasee across lake, South. From Black Stump Point, North. From Eppert’s South. One-quarter of a mile west of No. 26 and parallel with it. One-quarter of a mile west of No. 27 and parallel with it. IN SYRACUSE LAKE. LocaTION. From middle of east end of Syracuse Lake, South 80° West. From point 700 feet southeast of west extremity of Lake, North 70° East. From a point on north shore one-half mile east of west extremity of lake, South 10° West. me From west extremity of lake, South 80° East. In the accompanying map, constructed by Mr. Juday, the hypothetical con- tour lines of the bottom of the lake were drawn from the soundings along the above mentioned lines, and numerous other soundings taken to determine the ex- tent of certain depths of water. The contour lines indicate intervals of ten feet 220 in depth. From the same data were constructed ten vertical sections of the bottom. In constructing the vertical sections a base line was drawn from Pick- wick Park to Mineral Point, and seven of the vertical sections, from ‘‘A” to ‘“G” inclusive, were made at right angles to this line at intervals varying from one-quarter of a mile to two-thirds of a mile. Vertical section ‘“‘H” is a short distance east of No. 18, ‘‘I” is along No. 4, and “‘J” along No. 25 of the lines of soundings in the main lake. The remarks on the topography of the bottom are drawn largely from a study of these contour lines and vertical sections. The average depth of the lake, found by taking the average for the soundings at regular intervals of 300 feet along the lines of soundings is 21 feet 6 inches in the main lake, 13 feet 6 inches in Syracuse Lake, and 20 feet 5 inches for the entire lake. By a different method, as explained in his report, Dr. Eigenmann has computed the average depth at a little more than 17 feet. The maximum depth found in the main lake is 68 feet 7 inches, one-quarter of a mile from the southern extremity of Jarrett’s Bay; 1,000 feet northeast of the Biological Station a depth of 66 feet 5 inches was found; three-quarters of a mile north and one- quarter of a mile west of the Station the water is 60 feet deep; and a half mile northwest of Black Stump Point it is 63 feet 3 inches deep. The deepest water found by us in Syracuse Lake is 28 feet 10 inches. A depth of 35 feet is recorded for this lake in the State Geologist’s Report for 1875. An examination of the contour lines of the map shows that if we consider water having a depth of 30 feet or more as deep water, we have in the main lake four areas of deep water varying greatly in size, and connected with each other by channels. In Crow’s Bay the greatest depth found was 49 feet 9 inches. These waters enter the main body of the lake through a channel deeper than 30 feet, and 200 feet wide at its narrowest point. This channel flows across the mouth of John- son’s Bay, meeting a short arm deeper than 30 feet from that bay, and comes within 600 feet of the southeast extremity of Ogden Point. ‘This channel con- tinues less than 400 feet wide to a point two-thirds of a mile west of Ogden Point where it joins the channel deeper than 30 feet from Jarrett’s Bay. The deepest water in Jarrett’s Bay is 68 feet 7 inches, and the area deeper than 30 feet is one- fourth of a mile wide, extending north beyond the mouth of the bay and to within 700 feet of its southern shore. This 30-foot depth joins the main body of the lake a half mile north of Clark’s Point where the channel 30 feet deep is only 100 feet wide. Turning to the west, 1,000 feet northeast of the Biological Station this channel deepens to 66 feet 5 inches, and widens to a half mile directly north of the Station. Here it meets the narrow channel 30 feet deep from Crow’s Bay. 221 ‘The two channels merge into one and form an area of water from 30 feet to 66 feet in depth, one mile in length and with a maximum width of three-quarters of amile. This area of deep water lies nearer the south shore, its center being one- third the distance from the south shore to the north shore. Near Black Stump Point the deep water narrows abruptly from the north, and 500 feet out from Black Stump Point its width is but 200 feet. West of Black Stump Point the deep water widens abruptly to the north to a width of one-quarter of a mile and deepens to 63 feet 3 inches. West of this the area of deep water narrows again and the water having a depth of 30 feet ends one-quarter of a mile southeast of the entrance to the channel between the main lake and Syracuse Lake. Between the deep channels from Crow’s Bay and Jarrett’s Bay the area having a depth less than 30 feet is one and one-quarter miles long, 1,300 feet wide, and contains an area one mile long and 500 feet wide over which the water is less than 10 feet deep. If the level of the lake were lowered 30 feet there would remain four bodies of water connected by channels from 100 feet to 200 feet wide and less than 10 feet deep. These four bodies of water would be: (1) a small area in Crow’s Bay with a maximum depth of 19 feet; (2) about one-half of Jarrett’s Bay with a maxi- mum depth of 38 feet: (3) the main body of the lake, its width decreased almost one-half, and its maximum depth being 36 feet; (4) a small area northwest of Black Stump Point with a maximum depth of 33 feet. Lower the level of the lake 10 feet more, that is, 40 feet below its present level and these four bodies of water would remain as separate lakes, the connecting channels now being dry. Great changes in the shore line will take place if the level of the lake be lowered to a much less extent. By observing the map it will be seen that a low- ering of the level of the lake to the amount of 10 feet would move the shore line to the first contour line. This would leave one-half the bottom of Johnson’s Bay dry land; it would move the shore line along Crow’s and Jarrett’s Bays from 400 feet to 1,000 feet into the lake. Clark’s Point would extend 2,000 feet further north, and the distance between Clark’s Point and Ogden Point would be reduced from 4,000 feet to 1,800 feet. The south shore line from Clark’s to Conkling Bay would be moved northward distances varying from 250 feet at Iron Spring Point to 1,000 feet along the shore west of Black Stump Point. The north shore line from Ogden Point to the Channel would be moved southward from 900 feet to 2,000 feet, and at one place—between Jones’ Landing and Black Stump Point— 4,000 feet, reducing the width of the lake at this place from 1 mile to 500 feet. The Channel between the main lake and Syracuse Lake would be drained, and the greater part of Syracuse Lake would become dry land. 222 Judging from the contour of the land, the level of the lake has probably never been more than 5 feet below its present level. TOPOGRAPHY OF THE SHORE. The shore of 20 miles is about equally divided between dry shores and marshy shores. The shores of Syracuse Lake and of the west end of the main lake were. not carefully surveyed, but accurate measurements and notes were taken of the shore line of the east end of the main lake from a point on the north shore three- eighths of a mile to the northwest of Wawasee, around the east end of the lake to a point directly south of the starting-point. These data were used in mapping a ten-foot elevation line around this part of the lake. For this reason the shores of the east end of the lake are treated more in detail than the others. The dry shores are composed of sand and gravel. Some are less than 5 feet high, but more often they are abrupt bluffs from 10 to 30 feet high, or hills which ascend rapidly to a height of 40 feet. The west, north and northeast shores of Syracuse Lake are bluffs or hills. The east shore is marshy. The shore south of Turkey Creek, the outlet, is also marshy, and these marshes extend along both sides of the Channel between Syracuse Lake and the main lake. Pickwick Park is located on a gravelly shore less than 10 feet above the level of the lake. Be- tween Pickwick Park and Eppert’s is the Gordoniere Marsh extending north- west to the Channel. Pickwick Park and the land to the west of it is sur- rounded by the main lake, the Channel and the Gordoniere Marsh and is known as British Island. The shore between Eppert’s and Jones’ is mainly marsh. From Jones’ one-quarter of a mile east the shore is a bluff from 10 feet to 15 feet high. From this point almost to Wawasee the land near the shore is at present a dry marsh. The blutf at Wawasee is 15 feet high and extends along the shore 1,700 feet. This bluff extends back from shore 500 feet where it joins the marsh which stretches along the shore to Ogden Island, and also to the east to Johnson’s Bay. Ogden Island, which is surrounded by the lake only on the southwest side and on all other sides by marshes, extends a half mile to the noithwest of Ogden Point and is from 300 feet to 1,000 feet wide. Its greater part is from 3 feet to 6 feet above the level of the lake. About one-half of that part of the island which touches the lake is a bluff from 10 feet to 18 feet high. The area higher than 10 feet is 1,100 feet long and from 175 feet to 400 feet wide. The marsh around Johnson’s Bay is known asthe Johnson Marsh. It skirts the southeast and east sides of Ogden Island, surrounds a piece of timbered land 700 feet in diameter 223 north of Ogden Island known as Oak Island, borders the bay on the north, send- ing off a broad marsh across the country to the northeast, and continuing along the east side of the bay with a width of a half mile, joins a narrow marsh ex- tending to the southeast. On the east side of Johnson’s Bay are two bluffs, one reaching a height of 23 feet and extending from Cedar Point northwest one- quarter of a mile along the shore and having 500 feet for its greatest width; the other is 1,000 feet further to the northwest, and is between 10 feet and 15 feet high, 700 feet long and 150 feet wide. Lying to the northeast of these bluffs and extending between them is an arm of the Johnson Marsh from 50 feet to 800 feet in width, which joins Crow’s Bay just east of Cedar Point. From the northeast cor- ner of Crow’s Bay the bluffs extend south along the east end of the lake for a half mile. They are from 10 feet to 27 feet in height. The 10-foot elevation line then leaves the shore and extends almost south to Turkey Creek, leaving an area of well timbered dry land along the lake with an elevation of from 3 feet to 10 feet and attaining a width of 1,000 feet. The land on both sides of Turkey Creek, the inlet of the lake, is marshy. Lying to the north of the mouth of the creek this marsh is 400 feet wide and ex- tends one-quarter of a mile north along the lake. This marsh is separated from the marsh along the east margin of Morrison’s Island by a shallow channel of water. The west side of Morrison’s Island is a bluff reaching a height of 21 feet. From Turkey Creek to Buttermilk Point the shore is skirted with marsh from 200 feet to 400 feet wide. Mineral Point is 200 feet from the lake and ascends abruptly from the marsh to a height of 25 feet. A half mile south of Turkey Creek the lake is entered by Jarrett’s Creek which is the outlet of a chain of small lakes lying southeast of Jarrett’s Bay. This stream flows through a marsh 400 feet wide, and all the small lakes are bordered by marsh land. The marsh along the lake ends at Buttermilk Point, and for a quarter of a mile the shore is dry and sandy. The land along this shore is not a perpendicular bluff, but rises rapidly from the lake to the south and reaches a height of 40 feet at a distance of 400 feet from the shore. The west side of Jarrett’s Bay is skirted by a marsh from 140 feet to 1,000 feet wide. West of the marsh is a bluff from 10 feet to 15 feet high cqn- tinuous with the land south of the bluffs of Vawter Park. West from Clark’s the south shore of the lake is a perpendicular bluff reaching a height of 29 feet in Vawter Park and extending west beyond the point where our survey of the sum- merended. This bluff is cut by a ravine 50 feet wide at the Biological Labora- tory and by a small stream entering the lake a quarter of a mile west of Vawter Park. The shore extending west to and around Black Stump Point is from 5 feet to 15 feet above the level of the lake. The high bluffs from Clark’s Point to Black 224 Stump Point is by far the longest stretch of highland along the shore, being nearly two miles in length. Conkling Bay during the summer months contained an area of water about 300 feet in diameter and 20 feet deep, bordered by wide stretches of marsh containing a few small pools of very shallow water. To the north of Conkling Bay, Conkling Hill ascends rapidly to a height of 40 feet or more. This hill is conical in shape and slopes to the water on the south and east, and to marsh and lowland on the north and west. It will be noticed that the perpendicular bluffs of the main lake face to the south at Jones’ Landing; to the southwest at Wawasee, Ogden Island and Cedar Point; to the west along Crow’s Bay and Morrison’s Island; and to the north along Vawter Park. The high hills at Jarrett’s and Conkling’s are without pre- cipitous shores. Al] of these bluffs are bordered by wide areas of shallow water, and it wiil be noticed that the 10-foot contour line of the bottom does not approach the shore much nearer than 400 feet, and is usually much further from shore. As a rule, the bluffs facing to the south and southwest have a much wider margin of shallow water than those facing to the west or north. Wherever there is a long stretch of shore, bordered by marsh, there is no beach formed, but the muddy bottom of the lake merges into the mud of the marsh along the shore line. Along all the dry shores, and along the marshes of small extent lying between bluffs, the beach is composed of gravel aud sand. This gives a gravelly or sandy beach around Syracuse Lake} except on the east and southwest; along the north shore of the main lake, from the Channel to Ogden Point; along the east shore of Johnson’s Bay, from Cedar Point northwest to the extremity of the dry shores; from the northeast corner of Crow’s Bay to a point east of the north end of Morrison’s Island; along the south end of Jarrett’s Bay; from Clark’s Point along the south shore for a short distance beyond Black Stump Point. These beaches along the bluffs are formed by erosion and deposit along the base of the bluffs. The sandy and gravelly beaches along marshes are found where the adjoining bottom of the lake is composed of sand and gravel. These beaches have most probably been formed by the action of ice. Around the main lake a number of beach formations of this kind are found. From Wawasee a half mile west the beach is composed of sand and gravel. It is about three feet above the water’s level, and is higher than the land back of it. From the east end of the bluffs of Wawasee to the dry land of Ogden Island is a distance of a half mile, and the marsh along the shore is very little, if any, higher than the level of the lake. Between the marsh and lake is a beach com- posed of sand and gravel. This beach is two feet or more above the level of the water, and 30 feet wide. The beach along the bluff of Ogden Island is of the a 225 usual formation, but this beach continues along the shore for one-fourth of a mile beyond the bluff as a very sandy beach a foot or more above the water’s level and 50 feet wide; then the beach grows narrower and is on the Jevel of the water, the sand becomes less plentiful, and the beach is composed of a small amount of coarse gravel and then merges into the marsh, where the shore line of Ogden Point turns north. The same formation is found running a short distance north of the bluffs on the east side of Johnson’s Bay. Between the two bluffs on the east side of Johnson’s Bay is a beach 1,000 feet in length, with the lake on one side and a marsh containing pond lilies on the other. This beach is from 20 feet to 80 feet wide, 3 feet above the water’s level, and composed of sand and coarse gravel. The margin of the beach further from the lake is the higher, and is covered with a growth of willows, cedar and other small trees. Along the lowlands of Crow’s Bay is a broad beach composed of coarse gravel about three feet high and on a level with the land back of it. Along the south end of the west side of Morrison’s Island, which is lowland, the beach is from 15 feet to 25 feet wide, three feet high, and composed of coarse gravel. The beaches along marshes and lowland are broader and higher, and contain much more material than those along bluffs. The action of the ice is an important factor in the formation of these beaches. For the explanation of the action of ice on beaches as well as the formation of ice cracks, I am indebted to I. C. Rursell’s excellent book, ‘‘Lakes of North America.” The lake freezes over and by expansion the ice is pushed up along the shore carrying sand, gravel and stones with it. Numerous ice cracks form during the winter and fill with water. This water freezes and pushes the ice still further up the shore carrying the beach forming material still higher. These ice cracks are very numerous and may be as much as three inches wide. The amount of lateral pressure brought to bear on the shores by this means is very great, and beach ridges are begun and added to each year. The action of the ice in forming beaches along marshes is very great, while along bluffs it is smal]. In the first case no great resistance is met with in expansion, and the material for building the beach will be carried up to the full extent of the expansion of the ice, while along the bluffs the ice crowds against the shore and is itself broken at every ex- pansion. A recent ice formation is evident at the northwest end of the Gordo- niere Marsh, between the marsh and the Channel. In 1891 this marsh was under water, but since that time the water of the lake has receded and left the marsh dry. Separating the marsh from the Channel is a ridge of earth more than one foot high running parallel with the water’s edge. This ridge can be accounted (15) 226 for by the action of the ice subsequent to the time when the marsh was left with- out water. Some of the most striking examples of ice action in the formation of beaches are found along the east side of Johnson’s Bay; along Crow’s Bay; at Morrison’s Island, where two ice beaches, separated by a few feet, are now coy- ered by trees; at Clark’s Point, where an old beach extending as much as 200 feet from shore is found, and at Black Stump Point. CHARACTER OF BOTTOM. In the shallower parts of the lake the bottom is composed of sand, gravel, and small boulders, except along the low marshy shores, where it is composed of mud. At several places, both in Syracuse Lake and in the main lake, dredgings were taken at depths from 25 feet to 60 feet. Here the bottom was covered with a deposit of marl in which were found many diatoms and shells. Further investigations will be carried on to determine more fully the charac- ter of bottom at different depths. ICE. For information concerning the freezing of the lake I am indebted to Mr. J. P. Dolan, who has given me the history of ice formations as he has observed them during years past, and he has furnished me with records of careful observations made since the first formation of ice in October, 1895. These observations, unless otherwise indicated, are for Syracuse Lake. Ice forms on the main lake at the same time, but it does not freeze entirely over so soon as Syracuse Lake. The lake begins to freeze along the edge, except where strong springs enter near the margin. Information has been obtained concerning the influence of springs only at Crow’s Bay and Vawter Park. Springs are numerous along Crow’s Bay for a half mile and the water along the edge is kept open after the lake is frozen over, but I have not yet learned to what extent these springs in- fluence the freezing of the edge of the lake in this locality. From Mr. Smith Vawter, who has observed the springs at Vawter Park for a number of years, I learned that the spring, which is near the margin of the lake and 2(0 feet east of the Biological Laboratory, keeps the edge of the lake open throughout the winter. If the weather is not severe, ice does not form for 25 feet along the shore, and from 12 feet to 15 feet from shore. In the severest weather the lake is kept open for 2 or 3 feet from the margin. The ice spreads rapidly from the shore towards the center. The lake freezes over quite rapidly when the general temperature remains below 32° Fahrenheit : 7 7 | 227 and there is no accompanying wind. All parts of the lake freeze, except where it is kept open by springs, but the last place to freeze is a narrow strip from 20 feet to 30 feet wide, extending from the north end of the Channel to Turkey Creek, the outlet of the lake. Ice sometimes forms to a thickness of 6 or 8 inches along the margins of this channel before it freezes over. This is due to a current along this narrow channel towards the outlet. The ice is always thinner here than elsewhere. Accurate information could not be obtained concerning the exact date of freezing in 1894, but from Mr. Dolan’s observations we can give an accurate account of ice-formation during the fall and winter of 1895. The first ice of the season was observed on October 20. The temperature of the air at 7 A. M. was 28°. A thin layer of ice 4 or 4 feet wide had formed along the edge of the lake. It melted during the day. At 7 A.M. October 30, the temperature of the air was 26°, and about one-fourth of Syracuse, Lake was frozen over. Not quite all the ice melted, but it all disappeared on the fol- lowing day. At 7 a. m. November 2, the temperature of the air was 22°. The mill race was covered with ice three-eighths of an inch thick. Only the edge of the lake was frozen, as the wind blew during the night. On November 21, the temperature of the air at 7 A. M. was 13°, and ice had formed from shore to shore on Syracuse Lake; at 12 M. the ice was nearly all melted, and at 5 p. M. the lake was free of ice. This was the first date on which the ice ex- tended entirely across the lake. On November 23, at 7 A. M., the temperature of the air was 30°. Ice had formed on the mill race, but no ice formed on the lake, owing to a slight wind. On November 27, the temperature of the air at 7 A. M. was 16°, and a wide belt of ice had formed around the lake, but it disappeared on the following day. On December 2, the night was clear and calm. There was no ice at 4 P. M., but at 7:30 P. M. a thin sheet of ice had formed and extended apparently from shore to shore. On December 3, Syracuse Lake was completely covered with ice. The temperature of the air during the day was 6° at 7 A. M., 16° at 12 mM. and 12° at5 p. m. On December 5, the ice was 2 inches thick nearshore. On December 7, the ice near shore was 3 inches thick, and 500 feet out from shore 1} inches thick. I visited the main lake on Decem- ber 7, and the ice appeared to extend over the entire lake. Warren Colwell had skated over the lake during the forenoon as far east as Ogden Point. The only place where he found the lake open was a space about 20 feet square, half way between Ogden Point and Black Stump Point. Three dozen ducks and mud-hens had congregated in this open space. 228 The increase and decrease in the thickness of the ice from December 9, to De- ~ cember 20, are shown in the following table. The measurements were taken 50 feet or more from shore. Tak THICKNEss | TEMPERATURE ratte oF Ick oF AIR AT ConDITION OF WEATHER. * | in INCHES. 5 P. M. 9 4 18° North wind; cloudy. 10 43 26° Wind, southwest to south. - a 36° Snow and rain. 2 54 20° Clear. 13 D3 24° East wind; clear. - bt 36° Wind, south to southwest. 61 26° Clear. 16 53 39° East wind. 17 5 46° Southwest wind; rain. 18 4} 52° South wind; rain. iG) 24 54° South wind; rain. 20 0 52° South wind. On December 13, ice cutting for commercial purposes was begun, with the ice 53 inches thick. Last winter no ice was cut until January 1, 1895, when the ice had reached a thickness of 6 inches. On December 15, the ice had reached a thickness of 6} inches, after which it grew thinner, owing to the rise in temperature and the heavy rains. By December 20, the ice had melted so that only slush ice remained. On the morning of December 21, this ice had drifted to the north and northeast parts of the lake and at 5 p. M. of the same day the ice had all melted. Mr. Dolan has given me accurate information concerning the ice on the lake from January 1, 1895, to March 25, when the ice left the lake. OnJanuary 1 the ice was 6 inches thick and kept increasing in thickness for more than a month. The maximum thickness, observed by persons engaged in fishing through the ice, was noted in the early part of February and found to be from 24 inches to 28 inches. The greatest thickness is found where the ice has been kept clear of snow by the wind. In January and February the snow lay about nine inches on the level, but it was drifted in many places on the lake while other areas were without snow. In the spring the ice sometimes wears into holes out in the open lake, and breaks up in the center of the lake first, the last ice to break being along the shores. This is the case when the ice goes off in cloudy weather and with heavy rains. Usually the ice begins to melt along the shore, with some holes further out. A heavy wind then breaks the ice and carries it ashore. For the past ten years the 229 ice has gone off with a west or southwest wind and has been piled up on the east or northeast shores. In the spring of 1895, the ice went off the lake in an unusually short time. The lake had remained completely frozen over until March 24. During this day the ice began to melt along the shores. On the morning of March 235, the ice had melted to a distance of 20 feet from shore. At noon the ice had receded 400 feet from shore. A heavy west wind was blowing all day, and the cracking of the ice could be heard. At 3p. m. the noise caused by the crushing of the ice became very loud and could be heard for a quarter of a mile. The ice was broken into huge cakes. The wind now began to lift the ice and drive it eastward. At4p. M. all the ice was piled along the east shore. The height to which the ice is piled depends on the character of the shore and the strength of the wind. The piles are not so high along a low marshy shore as along an inclined or abrupt shore. Occasionally a great sheet of ice is pushed up a smooth inclined surface 6 or 7 feet without breaking the ice to any great extent. An instance of this kind was observed by Mr. Dolan on the northeast shore of Syracuse Lake last March. No ice formed on the lake after March 25. Ice cracks are very numerous from the time the ice forms entirely across the laké and has attained sufficient stability. They form before the ice has reached the thickness of one inch. When the first cracks formed in December the ice was so thin that it sagged slightly along the crack. The water came through the crack and spread over the surface of the ice sufficiently to melt the small amount of snow covering the ice, to a distance of 5 or 6 feet on each side of the crack. The explanation of ice cracks as quoted from Gilbert by Russell in his “Lakes of North America” is so applicable to the case in hand that I reproduce the quotation here: ‘““The ice on the surface of a lake expands while forming, so as to crowd its edge against the shore. A further lowering of the temperature produces contrac- tion, and this ordinarily results in the opening of vertical fissures. These admit the water from below, and, by the freezing of that water, are filled, so that when expansion follows a subsequent rise of temperature the ice can not assume its original position. It consequently increases its total area, and exerts a second thrust upon the shore. When the shore is abrupt, the ice itself yields, either by crushing at the margin or by the formation of anticlinals (upward folds) else- where; but if the shore is gently shelving, the margin of the ice is forced up the acclivity and carries with it any boulders or other loose material about which it may have frozen. A second lowering of temperature does not withdraw the pro- truded ice margin, but initiates other cracks and leads to a repetition of the 230 shoreward thrust. The process is repeated from time to time during the winter, but ceases with the melting of the ice in the spring.” The formation of these cracks is accompanied with noise, and, when the ice has reached the thickness of four or five inches, the noise resembles the distant booming of cannon. These cracks may be mere seams in the ice, or they may be several inches wide. On December 7, I measured a crack three-eighths of an inch wide in ice one and three-fourths inches thick. On December 9, Mr. Dolan meas- ured one two and three-fourths inches wide in ice four inches thick. On the same day he counted eleven loud reports caused by the formation of ice cracks in five minutes. They form during all parts of the day and night. They cross the lake in every direction, and, while the cracks are slightly zig-zag, their general courses - are in straight lines. The ice is very clear and pure, especially out from the shore, where there is no vegetation near the surface. Is is used very largely for commercial purposes, the ice being cut from about one-fourth of the surface of Syracuse Lake each year. INLET. The only stream flowing into the lake and containing water throughout the year is Upper Turkey Creek, which enters the lake on the east side of Jarrett’s Bay. During the summer months it was filled with an abundant growth of water vegetation, and was without any perceptible current. When the water is high the chain of small lakes lying to the southeast is drained into the large lake through Jarrett’s Creek, entering Jarrett’s Bay a half mile south of Turkey Creek. During the past summer no water entered the lake from this source. A small stream one-fourth of a mile west of Vawter Park, and another from the east side of Johnson’s Bay, contribute water to the lake when the water is high, but not during the dry summer months. There are no springs around Syracuse Lake, but springs are found along the margin of the main lake wherever the shore rises fifteen feet or more and extends across the country as elevated territory. These springs usually enter the lake near high water mark. This gives springs along Crow’s Bay, Mineral Point, the south and west sides of Jarrett’s Bay, and along the south shore from Vawter Park one mile west. No springs are found along the bluffs at Jones’, Wawasee, Cedar Point, Morrison’s Island, or Conkling Hill, but in each case these highlands are narrow and surrounded by marsh or lowland. For a half mile along Crow’s Bay the bluff is more than twenty feet high. All along the foo of the bluff the water percolates from the gravel, and at places it flows from quite strong springs. At Mineral Point there are a number a. > 231 of strong springs. At Buttermilk Point and along the base of the bluffs west of Jarrett’s Bay are a number of springs. The margin of the lake from Vawter Park one mile west is very springy, but the flow of water is not so strong as along Crow’s Bay. The waters from all these springs show traces of iron more or less strongly. OUTLET. The waters of the lake flow into Lower Turkey Creek through which they enter the Elkhart River near Goshen, Indiana; then through the Elkhart and St. Joseph rivers they reach Lake Michigan. Near the outlet of the lake the creek, during the summer, was about 20 feet wide and had an average depth of less than 6 inches. The volume of water dis- charged through the outlet was computed from measurements taken in the creek and the overflow of the mill race July 18, 1895. The outflow through the creek was 103 cubic feet, or 7723 gallons, per minute; through the mill race, 41 cubic feet, or 3073 gallons, per minute, making a total of 144 cubic feet, or 1,080 gal- lons, per minute. At the same time the volume of the creek a half mile below was computed at 1374 cubic feet, or 1,031 galions, per minute. By taking the outflow of the lake at 144 cubic feet per minute, finding the amount discharged in twenty-four hours, and computing the amount the level of the lake, with an area of 53 square miles, would be lowered by such an outflow with no inflow, we find it to be .016 of aninch. At this rate it would require 623 days to lower the lake one inch. In one year of 365 days, at the same rate, the level would be lowered 5.84 inches. The inflow, during the summer months, is almost entirely due to springs, and probably equals the outflow. The lowering of the level of the lake, during the summer months, seems to be due almost en- tirely to evaporation. ELEVATION. The elevation of the lake above the sea and above Lake Michigan is shown in the following list of stations and their respective elevations. The list of sta- tions with their respective elevations above mean tide at Sandy Hook, New York, was furnished by the General Superintendent of the Baltimore & Ohio Railroad. The elevation of each station above Lake Michigan was found by subtracting 582 feet, the elevation of the surface of Lake Michigan above the sea, from the ele- vation of the station above the sea: 232 ELEVATIONS OF STATIONS ON BALTIMORE & OHIO RAILROAD FROM SOUTH CHICAGO. ILL., TO PATTON SIDING, IND., THE MOST EASTERN STATION IN INDIANA. Ss.4 oes powens E25 |828.2 [833 Te. Sees |soe NAME OF STATION. 20g |e] 4 lee S23 5/8 iopslae - SES S52 593/5'¢ S Zr Mos i DM I as ao STATIONS IN ILLINOIS. Somth Chicago ¢ cic. outs teers: a Mew ie Se teh hetigniaes sis 19 593.0 11.0 Rock Island Jinction tos ke ree ee ee caine 593.5 11.5 STATIONS IN INDIANA. NUN Energi 95) 22S ee sg cree ents, Se ee eee ee 598.5 16.5 Bd semoGOt es cbr oe ceo sede, cole riieke G ieee ee ical oe 596.5 14.5 WitlSomse.4). Saati ect lediae SR etal nets, Seite WNP ACTS once 604.5 22.5 Mrs: a acer es sac ee akc Carbon, a see Sees 37 617.0 35.0 Woe kasd pci. s xtc stn wet his 86 ec nae sees ais ical ieee eis oe 621.5 39.5 Wallow-Creek: ... 2: ¢ SIO SS 255 Boe eee ee eee ee 640.3 58.3 Mie Coo les earn %, srss ct a Sa eee yee oe ee ie | (eae ee 640.5 58.5 Bab COGKaRy cy cere e rie ie oe oe ose ee ee eee ect eee 652.0 70.0 Woodville spe et 255. Be OPES, co trae es bre teenl were tere 687.8 105.8 Syma So 7s, Sia sR ae Oe Bahk aN eee ae 748.6 - 166.6 WODURE on. oe Sina a0 oie citi oa os oahe linen Wumios Matin ae Goer s een aeiens 786.0 204.0 PO arer ET eae IE BE TA Se a Te et eta ee 57 788.8 206.8 Wiellsborot h:.95 3 ae eee vot 2 See eer nee 64 760.0 178.0 Winton" Oentre so. hace enero ea aaoa ronnie kc ree eee 71 718.5 136.5 Wialikertontee en Sao cee Sek ae ae tie oie. Soe Oates 79 716.0 134.0 MEG eARGEN’ ccs Merks ores S. P coe ashe ete Gee teas 85 800.7 218.7 1k yl ESA etal et gegen lad aie ARN wr SOE inl ag ale See 859.0 277.0 earPaz.unetion 2. 0.2 ieeee Oo ae ba ee See 88 856.0 re IBremeng seed 2 cain eo ee Ore oa ee 96 819.0 237.0 IBerlintons ssc. © aces cibe le eee ee ce te LE Ee 853.0 271.0 INANE eR oso oe SAO ne ee ee nee nee eee 104 880.0 298.0 Milford Junctioniy «ies see sos TPE AS ARES. 112 840.2 258.2 Sy PACUSES ret tis ian ceio ct atte el eeree eciee das aoe 116 869.2 287.2 WikwWasee tect. Mine teen aro, 6 Sehs, oe Clee onnete es opal 120 882.2 3! 0.2 Groniwelly cs Cows Gore Ree ee Be eee EE 125 935.2 303.2 Gre yey) I RED Sees ieee a le ea Oe Re bebe pe br noel Pain Sten de 923.2 341.2 BYCUST Kester ances ee ee Se Ion i RL sae ei ol ocelot 901.6 319.6 PAN ION eis eh cee ae oC Re Sine senate 135 926.2 344.2 Riley: 2: SA 6 Sot Bere ce ce Ee ee ee Fe eee 970.2 388.2 Avilla Fe i eI RO Cn on ote ons Sale ae 145 961.2 379.2 ES (21) a, Se Meth oe nies Co Os a OT SES 150 890.0 308.0 Auburn JaNnetion Ve. eae cee ee eee ee 153 871.7 289.7 VENTER. Joys s,s s ideas Cas RRS Sh one Eee | teehee 864.2 282.2 StGOh = sc ect. Rina = RR RIS See Ree ee eee 163 812.2 230.2 LEP rays hel Kt (0 6y aoe Anions ARR e ao ss olicoe a easol snes ee - 849.7 267.7 —oSeqs=sanmnaeanananansnqnsnmnmmSmSESESSsSsSsSsSsSmSmSmSsSS 5 Oe - : 233 Syracuse is the station having most nearly the elevation of the surface of Turkey Lake. The mean level of the lake is about 5 feet below the station at Syracuse. This gives the lake an elevation of 864 feet above the sea, and 282 feet above the surface of Lake Michigan. CHANGES IN LEVEL. Changes in the level of the lake have been due to three causes: erosion, the dam which is built across Turkey Creek just below the outlet of the lake, and climatic conditions. Old beach formations give evidence that the level of the lake was formerly 5 or 6 feet higher than at present. By erosion the channel at the outlet was cut 10 feet below this ancient level, and the dam has raised the level of the lake 5 feet to its present level. The history of the dam as given by an old settler is as follows: A small dam was built in 1828, to which additions were made in 1831. This dam washed out in 1833, and the present dam and mill race were begun in the same year. This raised the level of the lake so that timber stood in water 5 feet deep. Much of this timber remained uncut in 1840, and some was still standing as late as 1865. The vertical distance between the level of the water in the creek below the dam and the top of the waste gate, December 7, 1895, was five feet. This would be the amount the dam, when in working order, would raise the level of the lake. The dam is not in use at present and a small portion has been removed, which allows the water to pass into the creek at a level 16 inches below the top of the waste gate. This present condition of the dam holds the water of the lake ‘3 feet 8 inches above the level of the water in the creek below. The submerged stumps in many parts of the margin of the lake is the best evidence that the dam had the effect of increasing the area of the lake. These stumps stand at present in water from a few inches to two feet or three feet deep. Along the margin of Syracuse Lake the stumps are most abundant at the point of the lake extending furthest west, and on the east shore along the edge of the marsh. Turkey Creek, from the lake to the dam, is sixty feet wide, and only twenty feet along the middle is clear of stumps. This was the channel of the creek before the dam was built, and the stumps now standing in water are the remains of the timber which grew along the banks of the creek. On the north and south sides of Buck Island, at the south end of Syracuse Lake, areas of sub- merged stumps indicate that this island was formerly one hundred feet wider in 234 each direction. On the east side of the entrance of the main lake to the channel are many submerged stumps. Along Johnson’s Bay much timber stood in water, especially on the east side of Ogden Point and on the east side of the bay just north of the bluffs. In these localities the stumps are very numerous, and among the largest in the lake. There are afew stumps along the marsh just east of Cedar Point. Others are found in the vicinity of Morrison’s Island and go to indicate that this island, before the building of the dam, was a part of the mainland. It is so represented in the government survey of 1838. On the west side of Jarrett’s Bay submerged stumps are numerous, especially along the southeast corner, where much small timber is still lying in the marsh at the margin of the lake, and at Clark’s Point where many large stumps are found in the water. Submerged stumps are also found west of Black Stump Point. The elevation of the lake by the dam, not only increased its area but must have rendered much of the low level land in the vicinity of the lake marshy, which would have been tillable. It is claimed by persons living in the vicinity of the lake that the dam rendered four thousand acres of land untillable. The fluctuations in the level of the lake are caused by climatic conditions, and vary with the inflow and outflow, rainfall and evaporation. In Mr. J. P. Dolan’s report will be found the record of changes of level as observed during the past few months. Annual fluctuations are estimated to be about two and one-half feet. The level of the lake is usually highest about May 1, after the heavy spring rains, and lowest in August, although this year it kept lowering until November 2, owing to the very light rains up to that time. It was then ten and one-half inches lower than on July 6. The lake was lower on November 2, than at any time since 1871, when the marshes around the lake were drier than in 1895. Since November 2, the lake has been rising until, on December 25, it was fifteen and three-quarters inches higher than on November 2. In May, 1891, the lake was higher than at any time during the past twenty years. The difference between well-remembered high water marks of that time and the level of November 2, 1895, is four and one-half feet, which is the maxi- mum fluctuation during recent years. Each spring since 1891, has found the level of the lake lower than during the preceding spring. This gradual lowering of the level of the lake has decreased its area and has shown marked schanges in the marsh land along the margin of the lake. Four years ago the water in Conk- ling Bay covered an area a half-mile in diameter, now it is reduced to three hun- dred feet in diameter; a small shallow lake just west of Conkling Bay contained. water throughout the year, now it is dry and growing good crops; fields lying west of the channel were almost marsh land, the crops being greatly damaged by 235 water, but during the past two years no difficulty has been experienced in tilling them; two or three feet of water flowed over the Gordoniere Marsh, which is now dry with beach lines forming along its margin; and boats were rowed over all parts of the Johnson Marsh, while at present hardly any of its surface is snh- merged. ConsuLt HyprocrapHic Map Next To Front Cover. TEMPERATURE OF TURKEY LAKE. By J. P. Douan.* In making these observations a Charles Wilder standard, protected, thermom- eter was employed. They were begun the 13th of July, during which month four soundings were taken in the deepest parts of the lake from the surface to the bottom at every five feet. Then on October 5 two records were made at about the same points, and again on November 2. September 17 a rain guage was set up and from that day to the present a regular record of temperature, precipitation, direction of wind and rise and fall of lake has been kept, but the observations have been confined to the northwest part of the lake; properly, Syracuse Lake. I. TEMPERATURES OF TURKEY LAKE, 1595. | Suny. Ocr.5. | Noy.2.|Dxc.14.|Dre.24. i es 3 I.U.. | Jan- | L.U. | Baacx Ispraxa Unrvensity Broroc- | 0. | gert’s| Bro. | Stump ~ pe Stat’n.| Bay. |Srat’n.| Port. Tr | 16th, | 17th, | 234 : | 1sth, | (th. | L7th, | 23d, 1:45 | 11:10 (10 A.M. ee. bien bce WAM.) po ye | alu, | 104M] | | Deg. / Deg. | Deg. | Deg Deg Deg Deg. | Deg 814 | 8334] 78%] 72 ie a eee 50 a eee 74 75 75 76%. 60% 61% 43 34% |- PW iscccausas saaces sweets | vesand— cease oteeny cee s|eseees creas | sees ne oteess 60 60% sc aspanewexe 5 AN See 73 7+ ia al 60 | 59 45 | 24% sinkeawawealen 72%} TA 74k 70 59 : Cie | nec EE Orel [ec Sema ASP ma | 7 Te) erg | pate) sang [age 68 65 68% 61% eb, Ee. ASEZS |< Siw on eaten > Q | weeeee sense 0072 DOJQ | -nccccseesee| coeees cecene| eeneeccueces 60 | 62 Jones wre 58% | 58i¢ | 588 -| 35% bebalada: &8% 58 bsfacdsees eo Pek sense Se ae ae Ee 58 58341 58 ee. <| eee Fe pl ae 58 7A ae name | eas a Epa ties terre ads 28 cane Tart el al s| | 38 oe l. 5 58% | Fy eA Re Re |e eee ee 58 58 58 3a? Seapwae eee ee = *Contributions from the Zodlogical Laboratory of the Indiana University, No. 15. 236 VI. SUMMARY OF SOUNDINGS OF TURKEY LAKE. grees Kirst 20 ft. i 2 a = = ° 7 = o o = = Lo | Bio. Station..| 3 i WE Deg| Deg Bee Deg} Deg 3 3 2 | 2 Eng. ‘|e: Sh (ee . . - | . . =| a ge C=: tel S Ss 1D &2|/s8/)/8|\|S] So =) S ° ° — pe ~ | + — i=) 3 =) i=) N oD oD = 45 to 50 ft. 50 to 55 ft. 55 to 60 ft. 60 to 65 ft. Aol 2 | 2 eee 0 ee ee = eS = ° > e|=a|2|s|4 Deg} Deg| Deg} Deg| Deg 16 | 74 | 58 | 66 (719 9a ee ee 183 | 763 | 58 | 673 |65.06 23 | 603 | 58 | 592 |58.84 vi imercemt Il, TURKEY LAKE TEMPERATURES, 1895. 6° 7 ; Precipitation be UTE eee 1.40 08] 09) |'eamee Totialin ches 1.53 | | | October ........- a Be | 3 | 4 5 6 7 8 | 9.) 10 jem | a2 | 18) 14 aes | u J | WAM Se9 ok Rese ccees: 561 58] 68| 68| 6} 62| 64] 45] 38] 45] 49| 45 | 40] 54] 48] 46 Surface ......... Ft ees 63 | 603 Bale atid beocenae BGI 5a Wide: [ssee- Ae SH B-8 | oeneee 53] 52 Bottom ......... 55) | eocec= 58" 5601) 582) DOli|i---c- 563] 56: || 534) ---.: 522 | eee |eeeeee 53 | 52% Near shore -..| ---.-- sasepall casoesa| evases| weesece |iemesscs EA cena lleceres| heeeeor AB PAT, I) eee ee 50 Precipitation] ..---.| -..e0.| ---12-| seeeee| cose =| eeeee| seeee See (copa cel ecb ere leceecap bsecol lessee | acccs. paneee October -..------ 17 | 18 | 19 | 20 a1 | 22 | 23 | 24 | 25 | 26 | 27 | 28 | 29 | 30] 31 | | | ! | | | ATi fc a) ae all Le | | : ! AG coos tes noe] 945 1A | 596] OR Besa alt ee: 60 | 60| 48] 40] 38| 34] 34 Gunkace sees leolaleore eae BG LAGU eral cm oie aa 5 4A || (43 A cee ees 39 Bottom ...--...| 51} ee Asi eairal ere: heaseecs esl |e | 463' 46 | 44 Janey 39 Near shore -..| ----- | .-----| .---. EUs | 92 Es) | See ee Pee eases Reece 2. Ci Rese aoe! [boon ccel bee eee Precipitation] -.... | .-....| ---.-- : | Beni | iat ed ce eee | chet | eae Tenge cso ueal needa | Scecoe | ace | | | November..... ik | 2 3 4 D6 7 8 Oe M02) ae 2a 13a) aa 15 | 16 L | Air.. «| 30°) 22 | 54 | 60] 62 | 60] 60.| 45° )) 32) )) See) 285) 26°) ~ | as) cee oe Surface, 25, ft | 38 | 43| 43 AVL AZ |) 43") 43a AS 42 eee AOE) seesec| acensol eee eee Bottom, 2 9 ft| 43| 48 | 43 | 42) 41] 45 | 43] 43) 44) 43] -..... 7: BI Wecered| | Reese | choc ose Surface near RINGTG a cccerss || «code UE A icwraselirateee BP kone eres UW Reker } BB | wceccc] cesses, |] scuces |! Seekers | eeeesn ees ee Precipitation |: scsc:|lse--2<| cere |i ceece- || ences. 02) 78 [1.10 | wees] wns | ereeee] seen O2/ ates iyi esse | Er 43 | 42 Surface near REOPEN cocececes|i vcsene AE Nae. Weed Wicwancel mccaas|| eauee PEHEIPIEALION) 2525 ||\p<55-2| ‘ceszasl) seocen| Acas<=]) | Surface, 25 ft} 30 56 31 39 30 34 7, 8, 9, 10 33 S | Bottom, 2 ft} 30 | 57 al ae 26 | 36 | 6,8, 9,15, 17,18,19| 35 | = . | eso ke roel Peers | _ Strid ls Gel peered eee Sp as eee eae > =< N.B.—Water general average for three months higher than air. 238 | AIR. | Sunract. Bottom. Grand average for four months mnt 42.94 | 48.37 | 48.87 From December 3 to noon of the 20th the lake was covered with ice. During this period the surface temperature varied from 33° to 343° and the bottom from 35° to 36°. At 5:00 p. M. of the 20th, ten hours after the ice started to move in a body from the lake, the surface showed 354°, a gain of 25°; the bottom 373°, another gain of 23°, and in the shallow water, fifty feet from south shore, where it had been 32°, 33°. 33° on the 7, 8 and 9th respectively, it was now 43°, a gain of 10°. The next day surface and bottom both registered 37° degrees at the twenty- five-foot station. The results of these observations are embodied in the accompanying profile chart, in which it has been attempted to show the absolute and relative move- ments of the air, surface, and bottom of lake at a depth of twenty-five feet. od a) wor al i el 4 x a Tala Temperatures from September 23 to December 23. Broken line, temperature of air; dotted line, temperature of water 25 feet below surface on the bottom; continuous line, tem- perature of water at the surface at the same place. 239 (a) A few well-known facts are emphasized, the variableness of the atmos- phere and the persistence of the water; that water is a poor (b) radiator and an indifferent conductor of heat, and responds slowly to atmospheric changes. (d) It shows also that the great volume of Syracuse lake at no time has been stagnant, but that a condition of activity has obtained throughout theentire period of observation. (c) For the four months in which a large number of observations were made the general average of the water, both surface and bottom, is higher than that of the air. . A difference of 10° between the water one foot deep near the shore and the surface mid-lake during a rain the day the ice left the lake, shows that the surface drainage is no small factor in winter and spring in raising the temperature of the whole body. PART IJ. THE INHABITANTS OF TURKEY LAKE.* PLANETON. By plankton, Hensen, the author of the word, means everything floating in the sea and passively driven about by the waves and currents. Haeckel in- cludes under plankton all organisms swimming in the sea. Haeckel says: “The totality of the swimming and floating population of the fresh water may be called limnoplankton.” Limnoplanktonic studies have been made when- ever a collector scooped for protozoa, diatoms or other minute organisms. Planktonic studies of this sort have been carried on for a long time. Recently plankton has been studied in a new way, first in the ocean and more recently in fresh water. This more recent study has been the quantitative and qualitative estimation of the plankton in a given volume of water. There seem to have developed in a remarkably short time two schools of planktonists, the one headed by Hensen asserting that planktonic organisms are uniformly distributed, the other, headed by Haeckel, being equally sure that planktonic creatures are to be found in clouds or schools. We are interested in plankton only in so far as it is part of the environment of the vertebrates inhabiting the lake. That it is not an unimportant element of the environment is due to the fact that it forms the primitive food of most of the fishes and that at the most plastic period in the life of the individual. The amount of plankton, as well as its composition from year *Contributions from the Zodlogical Laboratory of the Indiana University, No. 16. 240 to year, is therefore of prime importance in the search for the causes of the differences in the same fish in two contiguous lakes or in two successive years in the same lake. Our plankton apparatus was completed too late to enable us to make any systematic measurements, especially as our planktonist was actively engaged in the physical survey of the lake. But plankton was collected and some of its different constituents will be reported upon. A good historical account of planktonic studies, as well as exact definitions, are to be found in the Planktonic Studies of Haeckel, translated by G. W. Field, and published in Commissioners’ Report, 1889-91, U. S. Com. Fish and Fisheries, pp. 565-641. In the following sketch several groups of animals are not at all considereds and others but briefly. The only groups found in the lake of which we approxi- mate a complete list are the fishes, batrachians and reptiles. Deficiencies will be removed in subsequent reports when a classification of the material into littoral, bathybial and pelagic will also be attempted. PROTOZOA. The Protozoa were not represented by a large array of species during the summer. No detailed work has been done on them as yet, but I want to mention two characteristic forms. The most striking Protozoan is Ophridium. It is found in clumps varying from microscopic minuteness to the size of walnuts, and in different parts of the lake the pebbles and exposed parts of clam shells are covered with these colonies to such an extent as to suggest young lettuce beds. Ceratium hirudinella is as striking and abundant in the pelagic regions as Ophridium is in the littoral. In this connection two plants may also be noticed. Rivularia is very abundant during the whole summer. It is conspicuous in calm weather, when it rises to the surface. Toward the end of August and in early September it collects in such numbers as to form large patches and streaks, forming a true Wasserbliithe. ‘Various forms of Palmella are abundant during the whole summer, and in October, when Rivularia has disappeared, it torms large patches on the surface forming the Wasserbliithe of the late fall. 241 PORIFERA. Sponges are not abundant in the lake. They are found in small: patches on boards, sticks and other things near the margins of the lake. They grow much more Juxuriantly in the outlet of the lake where they sometimes form patches several square feet in extent. CNIDARIA. Hydra viridis L. Specimens of hydra were exceedingly rare. On one occasion a few were taken on a submerged stick near Black Stump Point. PLATHELMINTHES. Flat worms were not systematically collected and none of these collections have been identified. Of Turbellarians there were several species. Aiia calva is infested by a tape worm and by a Distomum. NEMATHELMIA. No attempt was made to collect thread worms. Gordius is exceedingly abundant on the margins during the latter part of summer. I counted as many as twelve in the area of one foot square. ANNELIDA. BY BESSIE C. RIDGLY. No Chaetopoda were collected. No systematic attempt was made to get large numbers of leeches, but speci- mens were preserved whenever found. In the classification I have followed Verrill. Nephelis quadristriata Grube. Thirteen specimens from Turkey Lake. Nephelis fervida Verrill. Fourteen specimens. Clepsine parasitica Diesing. Three specimens. Clepsine ornata stellata Verrill. This species was not found in Turkey Lake. Two specimens were taken iu Tippecanoe Lake. Clepsine ornata rugosa Verrill. Four specimens. Clepsine ornata variety d Verrill. Ten large specimens corresponding with the second specimen described by Verrill were found, most of them on turtles. Clepsine papillifera Verrill. One specimen. Clepsine papillifera carinata Verrill. Three specimens. One of these, one- half inch long, was found under a stone in front of the laboratory. A number of young were attached to it. Clepsine pallida Verrill. One specimen. Clepsine pallida variety b Verrill. One specimen. Clepsine elegans Verrill. Five specimens. (16) 242 Rotrrera. D. S. KEetuicorr. I received in September three vials of plankton, from Mr. Chancey Juday with the request to report upon the Rotifera found therein. The vials were marked and described as follows: ‘‘I. Contains plankton caught at the surface of the water of Wawasee Lake, Indiana, by using a plankton net; taken August 28, 1895; killed in picro-sulphuric acid; washed in 35 per cent. and 50 per cent. alcohol and preserved in 85 per cent. alcohol.” ‘II. Depth of haul, 60 feet (Wawasee) ; depth of water, 65 feet; taken July 20, 1895; killed in Flemming’s Fluid; washed in 35 per cent. and 50 per cent. alcohol, and preserved in 85 per cent. alcohol.” ‘III. From Tippecanoe Lake; depth of haul, 110 feet; depth of water, 117 feet; taken August 7, 1895; killed in Flemmings’s Fluid; washed in 35 per cent. and 50 per cent. alcohol, and preserved in 85 per cent. alcohol.” I find that the Rotifera were much better preserved in II and III than in the first. The illoricate species in I were scarcely recognizable ; in fact three species found in this vial I have not been able to place more nearly than the probable © genus. Those in II and III have all been satisfactorily identified. While the whole number recognized in these collections is not large some interesting facts are brought to light. Three species not hitherto reported from this country are among the number, and others rarely. It is certain that the rotiferal fauna of these lakes is rich and will yield many unique forms as a reward to any student who may be able to work in the region, to take and study them in the fresh state, and in all their varied relations and situations of residence. I shall enumerate, with remarks, the species found in each haul separately, although it will cause some repetition, and in the order of Hudson and Gosse’s Rotifera, without citing the bibliography farther than a description where the par- tial bibliography, however, will usually be found. iF 1. Floseularia mutabilis Bolton. Not infrequent. It is quite unexpected that a floscule should occur among pelagic species, and yet there are four known species of these Rhizota that cut loose and become sailors. Mr. H. 8. Jennings has found three of them in St. Clair and lakes of Michigan. Of this one he says: ‘‘ Very common in towings from Lake St. Clair, either at the surface or near the bottom. Hudson and Gosse, I, 56. , 2. (cistes brachiatus Hudson. A large number were found, but it was im- possible to identify them surely. The tube conforms to the figures and descrip- tions of that of Brachiatus ; it is cylindrical, smooth, compact, perfectly hyaline, — 243 often containing a slight amount of adhering matter, often containing several eggs, which, however, are not so elongate as the figures represent those of Brachiatus; the long narrow foot and the long non-retractile antenne agree well with the type. I am pretty confident that it is Brachiatus, yet 1 am surprised to find so many of them, or any of them, in a surface tow, as it is evidently norm- ally anchored ; perhaps they were attached to floating alge which apparently are not uncommon in the lake. H. and G.,, I, 83. 3. Philodina megalotrocha Ehrenberg. Numerous. I have often taken it at a distance from land, particularly in shallow lakes or among floating alge. ea, eG. ,, J, 101. More than one species of Rotifer which could not by any means be identified were present. 4. Sacculus viridis Gosse. Rare. H. and G., I, 124. 5. Polyarthra platyptera Ehrenberg. ‘Many seen. The serrations on the edges of the broad plates are coarse and more distant than in the type. H. and t., U1). 3. 6. Dinocharis pociilum Ehrenberg. One individual. It is a bottom feeding species and rarely occurs in a surface tow. H. andG., II, 71. 7. Dinocharis collinsii Gosse. One. Bottom feeding species. It has not been observed in this country before. No species exceeds it in beauty. I could not make out the pair of spines on the foot and the edge of the lorica appears to be set with a row of small spines, rather than being serrate as described and figured. H. and G., II, 72. 8. see eae wae oat nae hone eer ae ae ec: eae Ks er a ee ey eres 1 Green River, Greensburg, Ky ........... Beeclf; tee | sell yk ert AS ee Little Barren River, Osceola, Ky...........| 4 1 5 Pin rare desl Me a 2 1 Little South Fork Cumberland River, Wayne Oormntys Keys Ce cence oa Rakes Maicantrcie Deda ae Jal eee Toe Eagle Creek, Olympus, Tenn .............. Dict) JelG a liesaye ere ae! | ee lal Obeys River, Elizabethtown, Tenn.......... Peat SED (een oe eae PA STOP cis: Watauga River, Elizabethtown, Tenn ...... oe I ea eaten il 1 North Fork Holsten River, Saltville, Va....| 1 16 SS ean eee il mekacdsprings. vAwk oa tee ee eile oe Dit 1G al ersce| © chet tomer 1 @hocola Greek wOxtord, Adaceer .> 4) see oa: 4 LSS eee Vag 7 San Marcos Springs, dex s250.. 6.0200. see yaa oy a hd a i fos oc | fn =~ The color-pattern varies from a probably primitive, simple pattern consisting of alternate whole and half cross-bars distributed along the entire length of the body through the pattern consisting of whole, half and quarter bars, having an incomplete longitudinal series of lateral spots to a pattern haying a very promi- nent longitudinal series of dark lateral blotches with fine reticulations on the back. Between these different patterns all stages exist, so that they can be connected by regular steps. Those specimens inhabiting the lakes were found to possess a pecu- liar color-pattern. This was derived from the primitive, simple pattern by sup- posing the lower part of the whole bars to have become much broader than the upper part, and then to have shifted backwards slightly. ra 281 This lake variety (manitou, Jordan) is one of the most abundant of the fishes in Turkey and Tippecanoe Lakes, and upon it the results given in the following pages are based. Six hundred specimens, all that were collected irom Turkey Lake, and three hundred of those collected from Tippecanoe Lake, have been examined with a view, first, of making a comparison of this species in the two lakes, and second, of determining the range and character of its variation within Turkey Lake itself. The number of species collected from Tippecanoe Lake is much greater than 300, but this number was thought sufficient to give fairly good results. The effect of natural selection will be taken up at a later time. Etheostoma caprodes has two dorsal fins, the first, a spinous one, well separated from the second, which is composed of soft rays. The anal fin is composed of two rather strong spines followed by a number of soft rays. The scales are very reg- ularly arranged, so that they can be definitely counted along the complete lateral lines. The number of spines and rays in these fins, and the number of scales in the lateral line of both sides of the body have been determined. Besides these characters the presence or absence of scales on the nape has been determined. These structures have been taken because, with the exception of the last, they present definite, countable elements, so that in the results the personal factor is entirely eliminated. Curves have been constructed to represent the variation in these structures. In all the curves the horizontal distances represent the countable elements, and the vertical distances the per cent. of specimens possessing these varying elements. COMPARISON OF TURKEY LAKE AND TIPPECANUE SPECIMENS. CoLorAtion.—The coloration of these fishes in the two lakes will be taken up in detail later. The color-pattern of Turkey Lake specimens is, on the whole, of a more blotched character than that of Tippecanoe Lake specimens, and shows a slighter affinity to the simple, primitive coloration characteristic of the Wabash River forms. The connection of Tippecanoe Lake with the Wabash River may account for this greater affinity. SQquUAMATION OF NapE.—In Turkey Lake the nape is as a rule naked, while in Tippecanoe Lake it is usually scaled. Table I will bring out the difference. 282 TABLE I. v = : |! sees o 2) sae D se | 328 Sea | aaa Per cent. of specimens having no scales on nape ............. 88.00 | 19.32 Per cent. of specimens having few scales on nape............. 8.00 23.87 Per cent. of specimens having several scales on nape ......... 4.00 28.32 Per cent. of specimens having nape thinly scaled............. 0.20 16.67 Per cent. of specimens having nape closely scaled ............ 0.00 11.74 LATERAL Lrne.—The specimens of Turkey Lake have on an average two more scales in the lateral line. The average number for Turkey Lake is 89.46 for the left side, 89.74 for the right side; for Tippecanoe Lake, 87.69 for the left side, 87.45 for the right side. Fig. 1 represents the curves for the scales of the right side. The continuous line represents the conditions in Turkey Lake, and the broken line those of Tippecanoe Lake. It should be noticed that the entire curve for Turkey Lake is two units to the right of that of Tippecanoe Lake, showing that practically all the Turkey Lake specimens have a greater number of scales. Table II contains the summary of the counts for the scales in the lateral line. 20 BR EREREEE ERE PBR E ERE eee aH SSSR Sees beeeeseeae fen eto 5} BE CRMeE Bre SReaeE EEC ENE ai (Eee oe =SSanse Sst ied apaeta we HERD Sr HEE DiBE SERS aes soeeees ator ti pestansatae S BeAWEREERELO SOA EEA Oe EE RRERGteEGee f= 4b Cee eee Te OSeS or 80 85 90 35 100 Fie. 1. 7 TABLE I. TuRKEY LAKE. |/Trpp’CANOE LAKE Leit Right Left Right Side. Side. Side. Side. Per cent. of specimens having 78 scales.... LETS oes Hersecte = Sih wos eee eee Pemecns..al specimens havisit, 79 SCRIEN. oo lone ocafe sos ceo [fivaes eas] aces wens Per cent. of specimens having 80 scales.... 0.17 NS. Ah Spee | emerges 37 Per cent. of specimens having 81 scales....|........ 0.34 as Se ae ae ae Per cent. of specimens having 82 scales.... 0.17 0.34 1.00 2.00: Per cent. of specimens having 83 scales.... 1.37 1.55 | 2.50 3.50 Per cent. of specimens having 84 scuales.... 3.44 1.89 | 7.00 4.50 Per cent. of specimens having 85 scales.... 3.78 5.17 | 8.50 11.50 Per cent. of specimens having 86 scales.... 6.88 9.3) 11.50 13.00 Per cent. of specimens having 87 scales....| 11.02 | 10.68 || 15.00 16,50 Per cent. of specimens having 88 seales....| 12.56 | 11.55 15.00 13.50 Per cent. of specimens having 89scales....}| 17.72 14.82 16.00 16.00: Per cent. of specimens having 90scales....| 12.39 12.93 |}, 11.50 10.50 Per cent. of specimens having 91 scales.... 8.08 11.03 | 7.50 4.00 Per cent. of specimens having 92 scales.... 6.53 | 5.67 | 1.50 | 1.50 Per cent. of specimens having 93 scales.... 5.16 | 3.62 || 1.00 2.50 Per cent. of specimens having 94 scales.... 3.61 | 3.78 0.50 0.50 Per cent. of specimens having 95 scales.... 2.08¢|- 2%] An UN eae ets Per cent. of specimens haying 96 scales.... 1.37 2.41 0.50 0.50: Per cent. of specimens having 97 scales.... 1.03 Abo AU xen, wedi nts 2 are Per cent. of specimens having 98 scales: .*:.|- 0.17 |........|).... -..-[eceeeeee Per cent. of specimens having 99 scales.... | 0.34 1 | aie ee (eee Per cent. of specimens having 100 scales....|........ Ceo opt ol | Reape aed hens perso Per cent. of specimens haying 101 scales... | QE LOREF Meese esta pecal erste oaeeeot Per cent. of specimens having 102 scales.... 0 ge OE RS | Ce OY 5 Pee Per cent. of specimens having 103 scales... ’ 0.17 | OE | SO aa 9 ee ANAL Fin.—The number of spines in the anal fin varies from the normal in only nine specimens from Turkey Lake and in six from Tippecanoe Lake. This variation is always toward. a lower number, and extends only through one spine. Turkey Lake specimens have on an average fewer rays in the anal than Tippecanoe Lake specimens. The averages are 10.87 for the former, 11.15 for the latter. Fig. 2 represents the curves for the anal rays. Here again, and also in the succeeding curves for the comparison of the two lakes, the continuous line represents Turkey Lake and the broken line Tippecanoe Lake. Table III gives the summary of the anal rays for both lakes. 284 The prevailing number of rays in both lakes is 11; 53 per cent. from Turkey lake, and 56 per cent. from Tippecanoe Lake having that number. The number : of rays in the next highest per cent. is 10 for Turkey Lake and 12 for Tippe- canoe Lake, about 27 per cent. in each case. . The range of variation is two greater in Turkey Lake. This may be due t the greater number of specimens from this lake. | = 4 saea diate SURAT EHH Hea | SEE SS5Snar H Fic. 2 TABLE III. | e) Ss b 5 40 | gueae Se | 5 Si a5 3 | Sone BaeHe BaH4 Per cent. of specimens having 7 anal rays................-- 0.16; |code Per cent. of specimens having 8 anal rays ..... ...........- 0:16) |\seeeeee Per cent. of specimens having 9 anal rays .................- 1.48 0.77 Per cent. of specimens having 10 anal rays .................- 26.80 15.50 Per cent. of specimens having 11 anal rays .................- 53.43 56.21 Per cent. of specimens having 12 anal rays .................- 14.13 27.13 Per cent. of specimens having 13 anal rays .................- 0.49 0.35 Dorsat Sprnes.—Turkey Lake has on an average more dorsal spines, the average being 14.52 for Turkey Lake and 14.23 for Tippecanoe Lakes. Fig. 3 represents the curves for this structure. The range of variation is the same, from 12to 17. Although the average number of spines differs but slightly in the two . 285 lakes, the preferences shown for a given number of spines are quite different. In the Tippecanoe Lake specimens the preference is decidedly for 14. In the ‘Turkey Lake specimens the preference is for 15, although not so decided. From Table IV and the curves, it will be seen that the number of individuals in Tur- key Lake having 14 spines and 15 spines are about the same, 41 per cent. having 14 and 44 per cent., 15, while in Tippecanoe Lake this is not the case, 60 per cent. having 14, and only 25 per cent. having 15. 2 ish IEC 1F. Fig. 3. TABLE IV. | » Sg © suo | gic gf | 228 Bae | Bae Per cent. of specimens having 12 dorsal spines............... 0.32 0.38 Per cent. of specimens having 13 dorsal spines............... 5.09 11.24 Per cent. of specimens having 14 dorsal spines............... 41.26 60.85 Per cent. of specimens having 15 dorsal spines..............- 44,22 25.96 Per cent. of specimens having 16 dorsal spines............... 6.90 1.16 Per cent. of specimens having 17 dorsal spines............... 0.65 0.38 Dorsat Rays.—The average number of dorsal rays for Turkey Lake is 14.87, for Tippecanoe Lake, 16.40, the latter having on an average almost two more. The curves are given in Fig. 4. From this and Table V it will be seen that Tur- key Lake specimens show a decided preference for 15 rays, while the Tippecanoe Lake specimens show just as decided a preference for 16 rays, 52 per cent. of the 286 specimens having these numbers in both lakes. The range of variation is two greater in Turkey Lake, from 12 to 18 as compared from 14 to 18 in Tippecanoe Lake. This again may be due to the greater number of specimens. ae BEEBE RBS x rt Soe fiat ECC ss a 12 1S 165. t7- 18 Fie. 4. TABLE V. ' o ‘ Sa |e - S| Hag = aes =I Hos me = a4 = | & Per cent. of specimens having 12 dorsal rays................. O32. |||) eee Per cent. of specimens having US dorsalirayse.. os st ces uae eee LA8) | oe Per cent. of specimens having WAC CorsallraySiac. petite ietenes 28.77 3.48 Per cent. of specimens having 16 dorsal rays................- 52.26 31.78 Per cent. of specimens having IG dorsal ways cs ee. se5 = eee 12.16 52.32 Per cent. of specimens having U@sdorsalerays: sae rise 1.64 15.11 Per cent. of specimens having 18 dorsal rays................. 0.16 Ori Table VI presents all the combinations of dorsal spines and dorsal rays from both lakes. The spines are represented by Roman numbers and the rays by Arabic numbers. The commonest combination in Turkey Lake is XIV—-15 and XV-15; XIV, XV, occurring most frequently in the spinous dorsal, and 15 most frequently in the soft dorsal. The per cent. of specimens having these combina- tions is 22.46 and 24.49 respectively. In Tippecanoe Lake, XI V—16 is the com- monest combination, XIV being the prevailing number in the spinous dorsal and 16 in the soft dorsal. 32.11 per cent. of the specimens have this combination. 4 TABLE VI. 7 | 4 ay) | 4. Sc gud bse ke my alae Sete : =a aac oats ee ce & Per cent. of specimens having the combination XII-14..... O26 eases Per cent. of specimens having the combination XII-15..... O.1G5 > es Per cent. of specimens having the combination XII~16.....|........ 0.37 Per cent. of specimens having the combination MXIII-14..... 0.84 0.37 Per cent. of specimens having the combination XIII-15..... 3.71 2.22 Per cent. of specimens having the combination XIII-16..... 0.67 5.92 Per cent. of specimens haying the combination MXIII-I7.....|........ 2.59 Per cent. of specimens having the combination XIV-12..... Ged Go ha genoer Per cent. of specimens having the combination XIV-13..... A ee ee Per cent. of specimens haying the combination XIV-l4.....) 11.99 1.48 Per cent. of specimens having the combination XIV-15..... 22.46 20.37 Per cent. of specimens having the combination XIV-16..... 5.74 | 32.11 Per cent. of specimens haying the combination XIV-I7..... 0.33 6.66 Per cent. of specimens having the combination XIV-I8..... ae Lat Per cent. of specimens having the combination a ee OT ls am eee Per cent. of specimens having the combination VAISS 3 43 13.51 1.85 Per cent. of specimens having the combination XV-15.....| 24.49 8.14 Per cent. of specimens having the combination XV-16..... 5.40 14.44 Per cent. of specimens having the combination D0" Ey Carnes 0.84 1.48 Per cent. of specimens having the combination XV-18..... UG six cae eres Per cent. of specimens having the combination XVI-12..... CG ee Per cent. of specimens having the combination XVI-13.....| O1G? Revo Per cent. of specimens having the combination XVI-14..... POO in a atcha ote Per cent. of specimens having the combination XVI-15..... 3.04 cab Per cent. of specimens having the combination XVI-16..... 0.84 0.37 Per cent. of specimens having the combination XVI-17..... UES el | anes Per cent. of specimens having the combination XVII-14..... DSO! ess are Per cent. of specimens having the combination XVII-15.....)........ 0.37 Per cent. of specimens having the combination XVII-16..... QONGr Pe. 35 ee ee Per cent. of specimens having the combination XVIII-14..... U.1Gares STs In Table VIL is given the variation in the two dorsal fins taken together. The average number for the two fins is 29.21 for Turkey Lake and 30 for Tippecanoe Lake. In Turkey Lake 36.82 per cent. have the average number; in Tippecanoe Lake, 41.8 per cent. spinous dorsal and five for the soft dorsal in Tippecanve Lake, and seven in each dorsal fin in Turkey Lake. Lake the range of variation is, in each case, one greater for the two fins taken The range oi variation in the fins separately is six for the With an exception in the spinous dorsal in Tippecanoe together, than for the fins separately. Although the extent of variation is only one greater for the two fins together, the per cent. of specimens having the aver- age number is much smaller than the per cent. of specimens having the average 288 number in the fins separately. In Turkey Lake nearly 37 per cent. have the average number of the fins taken together, while 44 per cent. and 52 per cent. have the average number in the spinous and soft dorsal respectively. In Tippe- canoe Lake 41 per cent. have the average number for both fins, while 52 per cent. and 61 per cent. have the average number in the spinous and soft dorsals Per cent. of specimens having 29 rays in the dorsals .......... Per cent. of specimens having 30 rays in the dorsals.......... respectively. TABLE VII. i bs: Ba |e & s a =) ef | $83 = = Per cent. of specimens having 26 rays in the dorsals .......... 0:33: pauee eee Per cent. of specimens having 27 rays in the dorsals .......... 2.02 0.37 Per cent. of specimens having 28 rays in the dorsals.......... 16.38 4.07 Per cent. of specimens having 31 rays in the dorsals .......... 9.28 22.22 Per cent. of specimens having 32 rays in the dorsals .......... 1.85 3.33 Per cent. of specimens having 33 rays in the dorsals.......... 0.67 |... SUMMARY. 1. This species is equally abundant in the two lakes. 2. The color pattern of Tippecanoe Lake specimens shows a greater affinity for the primitive, simple Wabash River pattern than does that of Turkey Lake specimens. 3. In Turkey Lake the nape is usually naked; in Tippecanoe Lake the nape is usually scaled. 4, Tippecanoe Lake specimens have a smaller number of seales in the lat- eral line. 5. Thejanal spines vary but little, and show the same variation in the two. lakes. 6. The anal fin is somewhat larger in the Tippecanoe Lake specimens. 7. Turkey Lake specimens have one more dorsal spine. 8. Tippecanoe Lake specimens have one more dorsal ray, 16 rays is the mean in Tippecanoe Lake and 15 in Turkey Lake. 9, The combinations of the dorsa] spines and rays are determined by the. numbers that prevail in the fins separately. 289 a 10. The range of variation in the total number of dorsal spines and rays combined is one greater than the variation in the fins separately. 11. The number occurring most frequently is 29 in Turkey Lake and 30 in Tippecanoe Lake. 12. The preference shown for a given number is less decided for the two dorsal fins taken together than for the dorsal fins taken separately. 13. The variation is in all cases continuous. THE VARIATION IN TURKEY LAKE. Many of the facts on the extent and character of the variation of the 600 specimens from Turkey Lake, taken as a whole, have been given in the pre- ceeding. The lengths of the 660 specimens from Turkey Lake were measured and upon comparison were found to fall into three quite distinct groups. Fig. 5 represents the curve for al]. Each of the smaller horizontal distances represents one mm, and each of the larger verticle distances one per cent. The sizes ranged from 27 mm. tol02mm. The first group ranges from 27 mm. to 60 mm.; the second from 60 mm. to 80 mm., and the third from 79 mm. to 103 mm. The three curves of Fig. 5 represent these three groups. I have watched the growth during the first summer, and know the first curve to represent the first summer’s fish. The second curve in all probability represents the second year’s fish, and the third curve, those three years old and over. The growth, thus, is most rapid during the first sum- mer, the rate of growth decreasing each year after. The fish reaches practically its full size the third year, though the more gradual slope to the right of the last curve shows that it does not cease growing entirely. am \ cH 0 35 40 45 50 55 60 65 70 75 90 $5 90 $5 (00 RIG wos (19) 290 Having grouped them into three definite ages, a summary of the characters for each was made, and curves constructed. Figs. 6, 7, 8 and 9 represent the curves for these characters. In all the curves constructed for these ages, the contin- uous line is for the third year specimens, the broken line for the second year specimens and the dotted line for the first year specimens. LATERAL Lixe.— Below is the table of the average number of scales in the lateral line of the three ages. 1st year. 2d year. 8d year. Wiehtwside mci mnie. sae save eee Seater re etree ree 87.84 90.80 88.39 Weise BA. & kat iais: neler CORE ER ARE, Stee Soa aoe 88.00 89.80 88.78 From this it is seen that the first and third year specimens are most nearly alike. The second year specimens have about two scales more. By reference to the curves, Fig. 6, and Table VIII below, it will be seen that the great bulk of the specimens of all three ages have from 85 to 92 scales. The increased average in the second year is due to a larger per cent. having 93, 94, 95 and 96 scales than in the first and second years. ae | | | SERED TOOSS He Ht tt tf | iy | Hoe Gee fiast ettete BAI Se ; ' | | “sopeog [OT sulavy : : Ss suameds jo “quay I9g : : * “SaTBIG OOL SULAR A : - susUIIpadg Jo “yuay 19g : : “SOTBIS G6 SULABHL ; : = suampedg Jo “yuep log 5 : * "S8TBIY gH SulAtH = 5 = suetmtaedg jo -yuap log : : = “saTBag 16 SULABA = S = sueultvedg jo “quay 13d = a “SO[TBIS 96 SULARH Rg = = suemitdedg Jo-yue) Jog | 4 =i 7 “SOTBIG CG SUIABA = S <2 susuliadg jo yueD 139g = oS Bal *SO[BIG FH FUIABH = = = suamiidedsg jo jyusg Jeg = ‘ ‘ 1 ‘ é ch rar q ‘ h ‘ , TABLE “OF CONTENTS. AGE. An act to provide for the publication of the reports and papers of the ae Indian agAcad eniy OL SCLONCE feria ns aja ache since nies fase terns toins ae 4 An act for the protection of birds, their nests and eggs................--. 5 DEE At FO OS BNC: ine ao om oa epee Cnet otis eet ee ee eMac aS a WOMMMATECCR PLO GO—T ate sister wiep-aire Saks sie = srepeerance sc si pets Oe alte emmerveeeercl.s yee % 8 Pemeipak OlICers SINCE OFPATIZALLON:. <. . sc. eps isa sajciene we saaies 4 qn e,8 on 9 OHISHULITLOT gas bernie, orev era) eects Hie cata epi tte ee Gre ewes preter Sl caskci oie) 10 MMCMDEES COWS. Acie nibs w C8 5 dsp oes ny borden 5, ater Heies ehe ee Ie oe miele es 13 Mb rtiinrs “ianistenideninn foc oat ee oleic = dune Beira cea hea eng. cs ee SSN 14 MEIER S CROLL UG oe oe rans YN os ate sia aie re a alee na See 8 = lle nee rece 14 Haine tie PORCID COFFERNOROCIUN ¢ cs. ss kets | calsyr sen: vic Rep ak a> a aetenrs Sey 19 Propramo. Let hrannia li meetin shite oeeretes LOGOmiituem ase ae Terre Haute. Mirae. HOLES ERS 5 oe oul sais akinesia eee PSIG ee ee culate Terre Haute. Je Re Scovelllesihicis saat ectteies ee 1AOde aes hot sie: Terre Haute. WB; Shannon Voi. o-28 ts tent REDS Mees. tier Greensburg. Mex OMIUM Sitch coteoletw cc sto LGGoN meme ote. Chicago, Ill. \iel DS RiGiGhs eames Onn siod hegb baa. BOSE eee Sos oe ae Lafayette. MeCBaithonias;-ccmerie sete sero Ito BSS ON ne ee Ae cA Crawfordsville. Tie Ni i uderwoodis. ws%.cn.8 dese: LOS PoE eee New York City. TAO WVianU Ny Bits epee een ele ier oi LSOS Sasser set Bloomington. CPAry Wiall dO. agstier atin casts selaeener 1895) eevee Lafayette. eM sWebsterees sccberacciocs sts oe SOAS ee crate etic Wooster, O. ELON s: DWilleyicietocis s Biracty Bice ae 1S0DE See ie etna Washington, D. C. A Icy ets emf oh «1 ee Oey AB Od es eatane a oe Indianapolis. NON-RESIDENT MEMBERS. Ds Canip elles s0 of alchore- So. net snie, ke a area tote ae ake Stanford University, Cal. ey MERIVELMMA TIM aoa’ fc nice ee eee ree eyee Washington, D. C. Charlesse Gilbert, ss satincls «visto: a-cirsa eae en ee Stanford University, Cal. Ga WietGreen Sari egNa fae ¢ osc ecewie eee ee eeerag Stanford University, Cal. CE iY lS ei deat nes Sp bc eee Oe didabedna sors .oc cabddaoade Syracuse, N. Y. Rid ward Selig heap gets sitet -\6 o's: seumyaraie Re a teleyeyes eto ee Stockton, Cal. Og (ea oalihiepeans boos too moose odentS oo accec Canar Stanford University, Cal. Jers kun esley <.c aero G a ee aga es ee mies Tuits College, Mass. Alired Sprinvets ie | bra setacel iit eis ele inte wine = Cincinnati, O. Robert lbs) WV angele erie yen cierto ariel Washington, D. C. Hredenick aw. And rewsters aeiciterstieriorieeacictensey teeter: Bloomington. ete dle) PNG fetoeitacincio ao AO NAS Gio on iahieniOe S oOES Bloomington. Creare Jal, Morb esoo o gacesuee Ahead erates Indianapolis. Mamotiyel. Ball ct. 5 oe alee aie cel occ eisai ene erate Crown Point. HIGGER Ballard asec ca oneneeiare aie sess cuales screenees a eters Terre Haute. *Date of election. MEM MNES od ss Meri ia ayais elds 2's 4 Gs ode e Se Indianapolis. LTP nah ne | Pa CES Ae BRP ee ke Ser a Sa ae Moore’s Hill. a ie: Bergstrom Ie oe a ee Bloomington. PERCU 2 een ate Rte e Vitae cote d eer asin selene 28 Lafayette. PRP UNGEE gS ad dels waste raase sas cab ss ces Sans Greencastle. il feaiet WOMEN hee ly RE ey Lafayette. Mepsildsane Bogants 2. con". . nd pats eee o caw e sa see Crawfordsville. VIM Aey ESE AH OF ene 2 Sopris 2. MI wy RCN oleae 2/6 cicis bar MM Ayes Charles, C> Brown’... 3-.<.:-- eRe) ER es es Indianapolis. Tem eRE SUM OR aan ye hoes tose) acct tie Sere a raosic ia Slee Irvington. PEVCLAN CCD LU REAN CS Dae clang twas 5 siaeteoini<| sin iat sears 2 Lafayette. Pere RECN Sey oi ei Riniciere «i Wak addi eons ways Cloverdale. Noble/C. Butler... 3... 2.0.2 Oey a ee OIE Indianapolis. PRED AAIS ELLIE R Soe nn iia in ee ass ih Be sy et fares Sere South Bend. per ae ARIE e 5 So on ees sion Se < haw saree dbs ale tates Rockville. 1D. 1d et OLAS Ss Ee ne Ar Se eg ein ra Bicknell. io We RMAC TIRE «nee o.uic soe ens wid sa weer eas Bloomington. PRCT O HERINATE wer. treed | aise oni wate nee asia Warsaw. ep Bred Glearw aters ro. e aye 2 ade sole sie eaves pciee Seis Indianola, Ill. eee OC EIMOTIH GIS ats ie os nis wis clea Ges oes ene ee Crawfordsville. Mr PUTO os ed 19g oiled a ames s fo aha Poke eee See Washington. MMe e MEKEN EES ers yelee of the State in which he works, and that he is as jealous of her honor, as careful for her prosperity, as watchful over her interests as the man who edits a news- paper, who practices law or runs for office. But where the monastic idea prevails, where the laboratory so absorbs that he loses sight of his citizenship, he is derelict in duty and discredits science. On the other hand, the State, through her legislators, may be said to owe cer-- tain duties to science. One of the most patent of these’ is official recognition of the value of scientific work to the State. From the days of the New Harmony Settlement, when Indiana was the Mecca of all the Scientists of the land, when: the Owens and Say and Lesquereux and others were not only revealing the: natural wealth of the virgin State, but were adding lustre to her intellectual! record, down to the present time has science and the scientist done much for the State. The exploitation of our coals, of our stone quarries, of our clays, of our forest resources, with the development of the industries dependent upon them, has been based directly upon the work of the scientist. As the result of the study of farm products, of plant and animal diseases and their remedies, of soils and fertilizers, thousands of dollars annually have either been saved to the State or added directly to its wealth. In manifold ways, without withholding, has science given largely and liberally to the State. It would seem but a natural thing in view of such a record for the State to assume that science still had something in store for her; to assume that when she spoke her utterances would have value. It would seem but a just thing when the scientists of the State are associated to- gether and have organized definitely for an increase of knowledge of the resources- of the State to at least provide for the publication of this knowledge. It would seem to be the high-water mark of practicality as well as economy to secure some- thing for nothing. The worker has the satisfaction of work well done, the State all the results oi his labor. 40 Points of view vary, however, and what may seem just and generous to the scientist, may not have such a fair seeming to the legislator. But I believe that an honest and intelligent study of the contributions of science to the material wealth and intellectual development of the State will furnish a sufficient warrant for the views advanced. The obvious way in which this official recognition could be given objective form is in a permanent appropriation for the publication of the proceedings of this Acad- emy—an appropriation sufficiently liberal to insure the proper presentation of its work. The expense would be most trivial compared with the results such action would secure. Results which would extend beyond the material and would powerfully upbuild and support the educational system of the State. It seems to me that a failure to utilize such an agency is inexcusable. I believe that if there were no material interests involved, the proper encouragement of scientific inves- tigation, regarded from a purely intellectual standpoint and because of its reflex influence upon the character of the instruction in the secondary schools, is within the province of the State and may fairly be classed as one of its duties. The history of such action and its results in other States serves to emphasize this view. I am not, however, so much interested in the duty of the State to science as in the converse, and feel in nowise moyed to instruct legislators in their duties. If, however, there is a full recognition of the mutual obligations existing between science and the State, then the organization of this Academy opens wide the gate of opportunity. Before suggesting these opportunities, allow me to say that I believe that, perfect as is our organization, it can be made far more productive of results by a proper co-ordination and distribution of work. There are certain investigations which can not be made by individual workers which can easily be carried on in the laboratories of the colleges. There are other investigations which can only: be carried to a successful conclusion by the co-operation of many persons or in some cases of several colleges. It is one of the most difficult things in the world to recognize the limitations our environment imposes upon us, but a failure to recognize such limitations leads often to a sad waste of energy. To properly utilize the energy of the Academy there should be a co-ordination of the scientific work of the State of such a character as would at least prevent overlapping and valueless repetition, as would give the individual worker his proper field, thus freeing the larger laboratories for the broader problems demanding for their so- lution large equipments and libraries. Apparently, the only thing that stands in the way of such co-operation and such a practical distribution of work is the de- sire most of us have to pose as past masters of science. Is it too much to say a 41 feeling of jealously, a fear lest some other worker will gain more of reputation or popular favor? I much fear me that were we fully truthful with ourselves some slight leaven of professional jealousy might be found working in our actions. It seems clear to me—very clear indeed—that before we can properly seize the op- portunities offered, there must be some practical, though not necessarily formal co-ordination of work. Take the opportunities for concerted, co-ordinated work in a single science and notice how great their practical as well as theoretical value. There are cer- tain natural resources of the State which may be materially developed in some instances, or have their utility greatly increased in others, by full and complete chemical studies. Perhaps that of the greatest importance from a commercial standpoint is the thorough and complete investigation of the clay deposits of the State. I will be pardoned for saying that I think that the last vol- ume of the Geological Reports fully justifies all the grants ever made to the survey by the preliminary investigation of the clay deposits of the coal bear- ing counties. The certain outcome of the work is the rapid development of new industries, based upon this formerly unutilized resource, which will annually produce thousands of dollars in excess of all appropriations ever made for the survey. But this investigation has but begun, and a full knowledge of the clay deposits will only be possible after many years, unless there be in the various laboratories of the State full and complete studies made of the possibilities of these clays in various directions. Some are fitted specially for tile, some for paving brick, some for building brick, some for pottery, special uses which can only be determined by studies in the chemical laboratory or by the costly experi- ments of actual manufacture. From work of this character would naturally fol- low monographic work upon the chemical problems involved in the successive steps in the manufacture of each of these various products. Such work would give almost immediate return and would appeal to a much larger constituency than the scientist can usually hope to reach. In the line of increasing the utility of resources already developed, it is evi- dent that chemical investigations would reveal many ways in which our coal and gas and oil might be made to yield even richer returns than at present. That an intimate relationship exists between public prosperity and public health is no longer questioned. It is a matter of popular knowledge, which is taking form in the various voluntary and legalized organizations for the improve- ment of sanitary conditions in homes and municipalities. This movement sug- gests another opportunity for concerted chemical work bearing upon these grave problems. No more valuable work for the State could be carried out than that of 42 a chlorine survey of the natural waters of the streams and springs of the State. A knowledge of the local normal chlorine in the natural waters of the State is almost a necessity, if outbreaks of disease are to be anticipated. Any sudden in- crease in the amount of chlorine in a given locality, would give warning of possible danger and serve to give direction to the efforts of health officers in averting disease from their districts. A chlorine map of the State is a necessity for its proper sanitary control and this work can only be done satisfactorily and rapidly by the concerted work of an organization, such as this Academy. After the establish- ment of this chlorine base line there would still be necessary the regular examina- tion of water supplies for purposes of comparison, which could be done in almost every case by the local health officer. Without this base line chemical analyses of water lose much of their meaning. Correlated naturally with this would be the general examination of water in epidemic districts, the immediate benefits of which are self-evident. The mineral waters of the State open another field of chemical research work, attractive and of evident value. It is manifest that in the working out of prob- lems, such as these, covering the whole area of the State, there should be the most careful co-ordination, the most perfect division of labor. It does not seem to me that such work is beyond the province of the Academy, indeed it seems to. be its supreme province so far as its relation to the State is concerned. Since I am speaking of chemical research, allow me to suggest that much yet remains to be known of the chemistry of the soils and rocks of the State, much that must be known if in the near future we reach the apotheosis of usefulness, which some one says consists of making two blades of grass grow where one had grown before. The plant world also offers to chemistry opportunities for investigation in lines not merely of theoretical interest, but of high practical value. The exami- nation of vegetable products—for example, of plants producing sugar, tannin, medicinal properties, ete. How much of unutilized wealth is at our feet, bound up in plants, only waiting the word of science for its release. It is said that one of our smart weeds (Polygonum amphibirem), a common plant in marsh regions, contains 18 percent., by weight, of tannin’, an amount sufficient, if the statement is true, to justify at least an attempt to utilize it for commercial purposes. This is but an illustration of scores of cases which might be cited to show the possibili- ties of this form of work. It is strange when we consider the length of time scientists have been at work in the state, that there is so little of actual knowledge concerning its topographical 1 Bot. Gaz., vol. i, p. 20. 43 features, and, stranger still, of its drainage systems. In a general way we recog- nize the lowlands of the State are located in the southwestern counties, while the highland regions, if they can be dignified, are in the eastern-central counties; we know there are chains of hills in the south and prairies in the north, but beyond these facts we know very little. We are familiar with the two great drainage systems of the State, but of the minor details essential in the working out of local problems we have absolutety no data—at least none that are at all available. In an attempt last year, in the sanitary laboratories at Purdue, to make a contour map of the State, the paucity of data was strikingly apparent. Had it not been for the railroad levels, not eyen an approximation could have been reached. It is not necessary to say more than that amoment’s reflection will suggest the far-reaching application and value of this work. It is also manifest that the accomplishment of such work is only possible through the intelligent co-operation of the members of a body such as this. I have purposely omitted thus far any mention of the opportunities that open to biologists. From my point of view they are so numerous and of such impor- tance that they are almost self-evident. Fields that have already been entered show themselves broadening as the work advances. And the work already done sug- gests yet further worlds for conquest. The biologist still has much to do in the line of plant and animal diseases, infinitely more in the line of sanitation. The accomplishment of yesterday in these lines serves merely as the incentive for the work of to-day. There is little danger that work of this character will be neg- lected. There are, however, other problems, the solution of which depends upon a patient gathering of facts almost innumerable, and an equally patient study of these facts in their true relations—problems which by their mere statement carry little idea of their real importance. Systematic botany has, I presume, in the opinion of most people, about as little to do in the realm of practical affairs as any branch of knowledge. Such an opinion is doubtless true if systematic botany consists, as is the popular conception, in the mere cataloguing and naming of plants. The systematic botany of to-day is, however, far more than this; it involves studies of plants in their relations to soil and rainfall, to heat and light, to air and mechanique, to each other, to animal life. More and more clearly out of the great masses of facts being collected in ecological studies is the truth be- coming apparent that plants stand as the sure sign of the natural agricultural capacity of the soil upon which they grow. Allow me to quote from Mr. Corille’s ‘“‘ Botany of the Death Valley Expedition,” a report, which is a model in every way. After showing that trees and shrubs +4 are most reliable as zonal guides, he says: ‘‘Shrubs and trees, being com- monly larger than herbaceous plants, reach higher into the air and penetrate more deeply into the soil, thereby subjecting themselves to a wider range of con- ditions than do these smaller plants. They also, by continuing throughout the year exposed to successive, varying seasonal conditions, complete the full round of their possibilities in environment. They therefore stand as the most complete summation that can be attained of the natural light, heat, moisture, food, air and mechanique of any area; in other words, a sure index of the natural agricultural capacity of the soil upon which they grow. From a utilitarian point of view, too- much stress can scarcely be laid upon this fact. It has been the practice of agri- culturists to gauge the capacity of soils, in regions new to the plow, by observa- tions on rainfall, temperature, cloudiness, chemical composition of the soil, drainage, and many other phenomena, or by the even more laborious process of experimenting on every farm with each kind of cultivated product; ignoring the fact that this determination can be greatly hastened, cheapened, and authenticated by correlating the natural vegetation, especially that made up of the trees and shrubs, with that of other regions, whose agricultural capacities are known.”! A careful gathering of facts of the character indicated regarding our native flora would not only give results of the highest practical value, but would also- serve in a great measure to relieve chemists and agriculturists of irksome work, the results of which at best could be of but local value. In this broader view even systematic botany has opened before it a splendid opportunity, for I know to my sorrow how few facts of this kind are available. Here, also, it is evident that data sufficiently extended can only be secured through intelligent co-opera- tion of botanists throughout the State. No more attractive field offers; none in which the prospect of valuable returns is more promising. A recent article in Nature, by M. T. Masters, abstracted in the Popular Science Monthly for October, 1896, on ‘‘ Plant Breeding,” is also suggestive of work of great practical value along botanical lines. Quoting briefly: ‘‘The natural capacity for variation of the plant furnishes the basis on which the breeder has to work, and this capacity varies greatly in degree in different plants, so that some are more amenable and pliant than others. The trial grounds of our great seedsmen furnish object lessons of this kind on a vast scale. The two processes (selection and cross-breeding) are antagonistic. On the one hand, every care is taken to preserve the breed and to neutralize variation as far as possible, so that ) the seed may ‘‘come true,” on the other hand, when the variation does occur the observation of the grower marks the change, and he either rejects the plant, 1 Botany of the Death Valley Expedition. 18 45 manifesting it as a ‘“‘rogue” if the change is undesirable, or takes care of it for further trial if the variation holds out promise of novelty or improvement. Where the flowers lend themselves readily to cross-fertilization by means of insects, it is essential, in order to maintain the purity of the offspring, to grow, the several varieties at a very wide distance apart. Some apparently slight variations, which, even to the trained botanist, are hardly noticeable, may be of great value commer- cially —as, for instance, of two apparently almost identical varieties of wheat, one may be much better able to resist mildew and diseases generally than another ; some again prove to be better adapted to certain soils, or for some climates, than others; some are less liable to injury from predatory birds, and so on. So far we have been alluding to variations in the plant as grown from the seed, but similar changes are observable in the ordinary buds, and gardeners.are not slow to take advantage of these variations. The field is one of great scientific as well as commercial interest, and a thoroughly equipped biologist would probably ‘soon distance the ordinary gardener who works by rule of hand in producing and perpetuating valuable variations.” This audience will carry the thought of opportunity into other lines of scien- tific work without additional detail. The zodlogists are hard at work, under care- ful organization, and will at this meeting show something of the scope of their work, with the results already reached. The engineers, with all their energies, have as yet been unable to fully occupy their territories, so manifold are their fields for investigation. All that I have suggested involves no neglect of pure science. Neither does it necessarily involve the abandoning of work which, with our present knowl- edge, seems purely theoretical. It dves not suggest the introduction of the mercenary or utilitarian idea into scientific work. It is only an intimation of how, by a judicious and well-ordered treatment of what may be called the by- products of our activity much good may be accomplished for science, much for the State. As the manufacturer often finds that the careful utilization of the by-products conditions success, so the scientist may find that his success depends upon his contributions to the general good. Every truth will, of course, at some time take its appointed place and be assigned its true value; but many truths of science as yet stand isolated—unrelated, marvelous products, often, of skill and patience, but, until they find their true place, of little general interest. Through facts such as these scientist may appeal to scientist, but it is through simpler facts of readier application that science appeals to the State. 2 Pop. Sci. Monthly, Oct., 1896, pp. 859-860. 46 I have thus in the broadest lines indicated what seemed to me some of the evident duties of the Academy to the State, and what seemed to be opportunities for increasing its value to the State. All are dependent upon the combined work of many individuals. Few, if any, can be accomplished save through an organ- ization such as this. I look over the secondary schools of the State and find that the teachers of science, with few exceptions, are poorly paid; that science courses are, almost without exception, arranged with reference to recitation schedules rather than to logieal sequence of subjects or intellectual capacity of pupils. That science is assigned a value in the curriculum far less than language, or number, or form. I find in our colleges, again, with few exceptions, that while it is not expected that one man can teach both Latin and Greek, it is expected often that one man can teach Botany, and Zodlogy, and Physiology, and Chemistry, and Physics, with other incidental subjects to fill his schedule. I find a prevailing belief that the scientific specialist is a narrow man, when, by the very nature of things, he must be, if a true specialist, one of the broadest of men; a belief, in general, that science is impractical, theoretical, visionary. All this in spite of the fact that far more than any other force has science directed—yes, dominated—the progress of the past decades. I believe the cause of all this to be that science has not been fairly dealt with by her devotees. That the scientist, absorbed in the work of the laboratory, has too often forgotten his citizenship and neglected to transfer to the State the truth which science had placed in his hands. Prima- rily the objects of the Academy are inspirational, but secondarily, at least, and certainly in its relations to the State, its objects should be eminently practical. If we fully grasp the idea of this relationship, which I have but imperfectly outlined, the possibilities of science in Indiana are almost limitless. Its influence will be increased, its constituency broadened, its achievements more splendid, and the prophecy of a high place in science, born in the New Harmony days, will have its realization in the effective and beneficent work of this Academy. THE Evonurion or THE Map oF MAammotH Cave, Kentucky. By R. E.ts- WORTH CALL. There probably does not exist elsewhere on earth so famous a natural feature concerning which so little is definitely known as the Mammoth Cave of Kentucky. Its scientific exploration has been so hampered and guarded by a jealous fear of rival interests that no one has been permitted to survey the great cavern and to 47 project it on the surface in order to determine its relations to the topography of the region in which it is located. There have been but few attempts to so de- lineate its hundreds of ramifications that the visitor may know his whereabouts by reference to surface features. These are commonly conjectural; the guides profess to have, and for the most part are honest, but little knowledge of the rela- tions of the outdoor topography to that of the avenues and chambers of the cave. The liberal management of the present Superintendent, Mr. Henry C. Ganter, extended to the writer in a hundred different ways the most complete opportuni- ties to examine and study the cave in the usually inaccessible localities as well as those commonly visited. Measurements and compass work was permitted within the cave but the line was drawn when surface work was planned or attempted. Courtesy freely extended must be regarded, and while the results attained are not of the most exact kind, nearly four years of exploration have given a better idea of its surface relations and internal ramifications than could otherwise have been possible. The interests of the present owners are as jealously guarded as ever, and in this communication, therefore, I shall not violate any confidence which has been vouched to me. Nevertheless, I can not refrain from placing on record, in this manner, my firm belief that a survey which has been made ought to be projected in map form and given to the world of science. Only good could result to all the interests involved should an accurate knowledge of the cavern’s relations to the surface be made public. Such information would be invaluable to one who wishes to know the great cavern as a geological entity. Perhaps, as the years roll by, wiser counsels will prevail and the world will eventually know Mammoth Cave in all its ramifications and will see them represented on a map which will also show their relations to the surface. For the present it is my purpose to give a history of the several published maps, and the manner in which they have been prepared, to show how difficult has been the process of evolving the map and to emphasize the present need of a cartograph which shall exhibit the cave as it is, Mammoth Cave was discovered through an accident of the chase in the year 1809 by one Hutchins, a hunter who, tradition says, traced a wounded bear to the entrance, then quite hidden in a dense growth of underbrush and fallen trees. It would be difficult to imagine a more rough and wild region than is the country in which this greatest of caverns is situated. Facing north, on the side of the Green River Canyon, far away from the traveled routes of the olden time, accident only could have brought it to view. If Hutchins ever really lived there now remains no trace of him beyond the tradition of discovery; none of his kith or kin have been discovered in the region. Perhaps with this single act to make him forever 48 known he was content to pass from human view. In those good old Kentucky days, when firearms were as much in vogue as they are in these later days, and with worthier ends be it remarked in passing, gunpowder was a scarce article and pom was husbanded beyond comparison. A roving Philadelphia chemist, Dr. Samuel : Brown by name, first taught the earlier settlers the methods of manufacture of gunpowder, with probably as great acceptability as Latinus first taught the Latins. agriculture. But the nitre-bearing sheltered cliffs and caves of the Blue Grass region could not alone furnish all the needed nitrate, originally obtained in the form of calcium nitrate, from which the needed saltpetre, or potassium nitrate, was procured through the medium of wood ashes in the clumsy chemistry of nearly a century ago. Recourse was therefore had to other caverns, which were assiduously sought after and many found. From these the needed nitrate was obtained in abundance and a great industry was built up in Kentucky. Rumors of the great cave in Warren County, for we may be sure that coupled with the growth and size of that famous bear each time the story was recounted, Hutchins did not fail to tell of the cave he had found, reached the ears of the middle Ken- tucky folk and business enterprise soon made Mammoth Cave a fact of history. Mammoth Cave appears to have attracted great attention from the very first, though its chief value seems to have been connected with the manufacture of saltpetre. When the war of 1812 came and the resources of the United States: were taxed to the utmost in securing materials for the making of powder because the foreign supply was rendered uncertain through the exigencies of war, the caverns of Kentucky furnished nearly all the saltpetre used in that memorable conflict. With central Kentucky, and notably with Lexington, the great eastern city of Philadelphia had intimate commercial relations. It resulted that the caverns of this portion of the State soon were exhausted of their precious nitrate and the new, stupendous Green River cave came prominently into view. A Phil- adelphian of Hebrew descent, and a patriot, by name Hyman Gratz, associated with one Charles Wilkins, of Lexington, leased Mammoth Cave from its earliest owner and carried on in extensive scale the manufacture of saltpetre. Many tons of ‘‘petre-dirt,” as the miners called it, were brought from far within the cave, the places where they last dug and the vats in which they leached the earth still attesting the magnitude of their operations. With the development of this industry came visitors, and with the visitors went wonderful stories of the great cave. It thus happened that in August of 1814 a gentleman unknown to later days wrote an extended account to ‘‘a respectable gentleman of New York,” which was published in the Medical Repository, then under the editorial control of the eminent Dr. Samuel Latham Mitchill, accompanied by a map. The account 49 and map appeared in the seventeenth volume of that journal. It is presented herewith, not because it has value as being an accurate map of the cave, but because it possesses a certain archaic value as being the first map to have appeared in print. A previous map, essentially the same, is known to have been made, but there is no record of its having found a way into literature. The author of our map is unknown, so far as any fact connected with its publication goes, but in a later number of the same journal another map is mentioned as accompany- ing a description of a mummy from a cave near by and on deposit for exhibition purposes in the Mammoth Cave, and is said to be the same, substantially, ‘‘ as: that which we had received before from Mr. Bogert;” from which fact it appears: that such was the name of the man who presented the original map. But noth- ing more is known of him. This map is not drawn to scale, nor was the compass employed in determining the relations and directions of the several halls. With the exception of a very few localities near the entrance, which are fairly correctly located, it is impossible to identify any of these avenues with those now known. But the map is important as being the beginning of the published cartography of the cave. The second map of Mammoth Cave was the one prepared by Dr. Nahunt Ward, a photographic copy of which is presented herewith, its original, the only copy now known to be extant, being in my own library. This map first appeared in the Worcester Spy, a newspaper of Massachusetts, in June or July, 1816. My copy is a facsimile, printed on one-half of a newspaper sheet, with blank reverse. As presented herewith it is reduced one-half. As in the case of Bogert’s map, so in this one, it is impossible to identify very many ot the localities mentioned. The descriptions of Doctor Ward are quite full but are by no means exact. He appears to have been thoroughly impressed by the great magnitude of the cavern, and the terms selected to convey his ideas of the cave comport well with its greatness. But the map is drawn to no scale and, as may be noted from the map itself, its horizontal distances are grossly inaccurate. In addition this writer makes the cavern to pass under the Green River in three separate places. As a matter of fact it is impossible for such an extensiom to’ happen; the area of the cave is limited by the configuration of the country around it; while its depth is determined by the level of Green River, into whieh, by several separate channels, breaking out as large or small springs, the waters of the cavern eventually find their way. The drainage levels of the subterranean streams are all determined by that of the Green. While Ward employed the compass at places and determined thus the directions of the longest diameters of the great halls, he did not employ it constantly or systematically and nowhere did 50 he run long lines or have points for ‘‘tying” those he did run. His published account is the first extensive one in literature, though it, like all the earlier ones, abounds in exaggerations.* The next map, in order of publication, bears the date of 1835, the year of its copyright, and was prepared by Edmund F. Lee, a civil engineer of Cincinnati, Ohio. It is based upon the first instrumental survey ever made of the cave, and is *both complete and accurate for that portion which may be called the cisriparian eave. The rivers and all that vast area of the cavern which lies beyond, were then unknown and undreamed of. : The rivers were discovered by Stephen Bishop, the guide, in the year 1840, -for the way to them, over what is now the Bottomless Pit, had not been known; »the Pit itself was not crossed until 1840, the crossing being almost immediately followed by the discovery of River Hall and all its wonders. Consequently none of this portion of the cavern appears in Lee’s map, a copy of which is herewith given, from a faded copy in my library, which, like the others mentioned, is the only copy now known to be in existence. Lee’s map is further characterized by sections of the several known avenues and chambers, and is the result of many month’s of underground work. As laid down in his map the relations of the -avenues and chambers are absolutely accurate; the nomenclature has since very .greatly changed, as the fancy of visitors or the caprice of the several managers chave dictated. It will be at once recognized that this map has extraordinary value when it is stated that it forms the basis of several other maps which have appeared from time to time; further, it is the first map to have been profession- ally made. Complete surveys of most of the newer or transriparian avenues have never been made. Some of these avenues and passages, like that which leads te Mystic River, leaving El Ghor just below Martha’s Vineyard, have been entirely closed up by the management and never will be surveyed. A complete .map of the cave will, therefore, always be impossible, and some avenues will only * Since this article was completed, chance has thrown in my way an old volume pub- jished by Lee & Shepard, Boston, in 1873, ‘‘ The Wonders of the World,’ which reproduces Ward’s account of Mammoth Cave, together with his original map; the map appears as page 327 and has a cut of the ‘‘ mummy, now in the American Museum, New York.’’ It is interesting to note that this old map is useless in suchabook. It is further interest- ing to note that the mummy was not then in the American Museum, nor ever had been, be- yond a few days for exhibition purposes, but was deposited in the museum of the American Antiquarian Society, at Worcester, Massachusetts. A short time since, following the World’s Fair, where it was on exhibition, it was removed to the National Museum, at Wash- ington, where it may now be seen. A most excellent photograph of this famous mummy was recently made for me and forwarded by the courtesy of the late Dr. G@. Brown Goode. The account of the cave, which this volume gives, in 1873, is a verbatim reproduction of Nahum Ward's original description, made in 1816. In this way do great publishing houses sive us new and iresh knowledge of the world’s wonders, 51 have historic names. They will never be visited by future explorers. But Lee alone has surveyed the intricate and devious windings which make up the Laby- rinth, together with its associated chambers. Use was made of his work by the maps which followed. The parts of the cavern which are beyond the pass known as El Ghor, includ ing a considerable portion of explored but unmapped cave, have had several names bestowed on them by the earlier visitors. Of the parts which it will now be impossible to visit, owing to the artificial occlusion of the small passage under Martha’s Vineyard, are the following; Byrd’s Avenue, Miriam’s Avenue, Har-- lan’s Avenue and Hebe’s Spring. The Mystic River itself rivals the famous Echo: River, but is less in size. It has probably some connection with Roaring River; a great stream at times, reached from Stephenson’s Avenue at the Cascades, but as yet unexplored fully. Several attempts made by the writer to reach its end were defeated by lack of boats, the only means by which the deeper and unfa- miliar places can be passed. Lee’s map was followed by one prepared from accounts and free-hand sketches: of Stephen Bishop, in 1845, and is found in a little volume called ‘‘Mammoth Cave, by a Visitor,” and published by Morton & Griswold, of Louisville, Ken- tucky. This map appears to have Lee’s map as its basis for the older portion of the cave; the newer portion, which had not then been surveyed, is laid down by Bishop and from his notes. In common with all the published maps of later date’ than Lee’s, the distances are grossly exaggerated, and the relations of some of the avenues are certainly hypothetical. But this map stands to-day as the best that has been published, and while inaccurate for any scientific purpose is certainly~ exact enough for the visitor. It names and shows the points of departure of the side avenues from the larger and better known or more traveled portions and” gives a sketch of their turnings and ramifications. It is to be constantly remem- bered that none of the maps, except Lee’s, have been based upon compass-bear- ings, even, to say nothing of determining their relations by exact methods:. No other map appeared until 1875, when Forwood’s ‘‘ The Mammotli Gave of © Kentucky,” Fourth Edition, appeared from the Lippincott press, of Philadelphia. His map gives only the two traveled routes, called the ‘‘ long” and the ‘‘short” ’ routes, and is grossly inaccurate even for these. No dependence can be placed‘ upon any of the details of this map. It is noticed here simply because it is one of the few which have ever been published. Hovey’s map, which appeared in his ‘‘Celebrated American Caverns,” im 1882, is the next in order of time. It is probably the best known map of the cave having been reproduced in a number of other publications and been sent abroad. 52 in numerous copies of his guide book, itself a separately bound excerpt from the larger volume, with slight changes in the later editions. This map is chiefly that of Bishop; all the main features of Bishop’s map appear and few additional facts. For the older portion of the cave, like Bishop’s map, this one follows very closely the original work of Lee. No mention is made of these sources, and Doctor Hovey did not himself map any part of this great cave except Ganter’s Avenue. Some measurements of separate localities were made by him, but beyond this his map has ~very little original matter or matter not already known. It is, however, a useful one, for more names to localities appear on this map than on any other, many of which have been happily bestowed by Hovey who, in these matters, has appreciated the “eternal fitness of things.” In his names record is often made of the pioneers of discovery in the cave; in other cases he has happily made allusions to mythologie ‘characters to which is added the uncanny suggestiveness of the gloom of the un- derground world. The latest map of the cave is still unpublished, but will appear within a few months. In it the attempt will be made to correct the errors of the older maps and to add to them as wholes the newly discovered portions or those portions of which little has hitherto been known. But when this map shall have appeared it will demonstrate the need of accurate surveys, which are never likely to be made, rather than add very greatly to our knowledge of the cave. Still, errors of others ‘being corrected, the golden goal of exact knowledge will be brought a very little nearer. Jt is well known that the main avenues of the cave have been ‘ ‘run” by com- ‘petent engineers, and they have been platted on the surface, in part at least. This was done in the attempt to learn whether any of the more valuable parts of the cave extended beyond the limits of the present ‘‘cave estate.”” No one has been al- lowed to see these plats except those who are directly interested. The closeness with which this information is kept argues for the fact that without doubt the cavern extends beyond the estate. Numerous attempts have been made to find other entrances than the one on the estate; that they exist is proven by the free circulation of the air and the presence, in places miles from the well-known mouth, of seeds and leaves, sticks and bark, from the surface, and oftentimes in a fairly fresh condition. But these entrances are small and not likely to ever prove valuable to others if found. It is this fear of attempts to enter the property of the present estate that operates to make impossible, at present, a cartograph which exhibits Mammoth Cave in its true relations to the region in which it is situated. 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( t ¢ ; J 5 MAP OF THE MAMMOTH CAVE, ACCOMPANIED WITH NOTES, BY EDMUND F. LEE, CIVIL ENGINEER, os CINCINNATI. 54 Fauna oF MammotH Cave, Kentucky. By R. E. Catt. Published in the American Naturalist, May 1, 1897. Notes oN INDIANA CAVES AND THEIR Fauna. By W. S. BLATCHLEY. Published in the State Geological Report for 1896. A PosstBLE RELATION OF THE ACADEMY OF ScIENCE TO THE TEACHERS OF BroLoay In Our SEconDARY ScHoots. By L. J. RETTGER. [Abstract.] The purpose of the Academy of Science, as I understand it, is in the main two-fold. It aims to encourage original research work among its members, and so enhances the amount of scientific knowledge by valuable contributions. It also encourages younger observers to attempt more critical work and so prepare to continue the regular research work. By its organization and its meetings it is able to accomplish this to a very satisfactory degree. The second purpose is probably the dissemination of scientific knowledge among the people. It is this second purpose that makes the first one peculiarly valuable to the State, and in the fullest way repays the favors which the State officially grants the Academy. But the dissemination need not be limited to the actual research work of the Academy. It may legitimately include that basal scientific information which any advanced work presupposes. It will in this way create a more general and a more intelligent appreciation of true scientific work and may result in bringing out scientific talent that would otherwise have been missed. The avenue along which the Academy may most efficiently exert its influence: in this way is in the secondary schools of the State. By persistent efforts biologi- cal studies in some form or other are included in almost every high school curric- ulum and so the way is open as far as the subject matter is concerned. In many instances, too, there are teachers who have had a high grade laboratory training and who teach the subject in the high school in a most commendable way. But the fact remains that possibly in the majority of instances biological work in our high schools is still deeply mired in text book work. The utter worthlessness of biological work which does not bring the student into a direct contact with at least a reasonable number of actual things need not be restated. It is a maxim that such work is laboratory work or it is nothing. —— 55 In many instances this kind of work done is due to the lack of training of the teacher himself and for such a place there is no hope until by some good fortune the teacher gives way to a better. But there is a second class where biological work is handicapped in spite of a well trained teacher, and it is this class for which a possible remedy is here suggested. In few high schools indeed does the work in biology fall to a single teacher and occupy all his time. In practically al! our secondary schools the teacher of biology has in addition to his zéology or botany classes, three or four other classes that may range from Greek through English Literature to mathematics. Usually his entire school day is occupied in ‘‘ hear- ing” recitations. Timespent in laboratory work is usually ‘“‘offtime.” Thereseems often but one thing left and that is to devote the recitation period in botany or zéology to an exposition of some text, and the actual study of things is very infrequent. Ii it be asked why the recitation period itself is not devoted to actual laboratory work, one needs but to be reminded that laboratory work requires material, good material, and a fairly large amount of it. And to continue this day after day -with new forms means an amount of time spent in preparing this materiah which is not available to the high school teacher with his multiplicity of other duties. The teacher is further often quite unacquainted with the resources of his neighbor- hood, and is frequently not assigned to his place of duty until after the opportunities for collecting are gone. The writer has had the opportunity of visiting numbers of High Schools, and in almost all instances the apology for doing a low grade of work in botany or zodlogy was the one that specimens were, in spite of best efforts, not accessible. Sometimes the neighborhood would yield in abundance two or three different forms for study, and these would be studied as the material warranted, and yield all those desirable results which flow from the study of actual things. But these forms are soon exhausted, and the interest of the class is lost in attempts to put in the remaining time in this line of work which the program calls for. y For this difficulty it seems to me the Academy could offera remedy. It could establish a central station of supplies from which all secondary schools could draw their material. Being controlled by the Academy, the following things wouid be assured in this matter: (1) Material well adapted for school work would be se- lected. This material could so be hardened, dried or otherwise preserved as to be in available form during any time of the school year. (2) Exchanges could be made subject to the approval of the station, and so a variety of forms secured for a collection of one or two forms which the teacher’s own neighborhood easily af- forded. A possibility to get a good assortment of forms without the direct outlay 56 of money is thus opened. As nearly every neighborhood has semething in abund- ance which is more or less rare in others, this plan can not be wholly impracti- cable. (3) Along with this high grade material the station could send carefully prepared directions for study in order to insure the proper use of the material. (4) This central station, being under the immediate control of the Academy, would preclude the suspicion that there was a mercenary element back of the af- fair, and would come to the teachers or school authorities with the force and in- fluence of the Academy itself. (5) It would furnish all material to schools at actual cost, which would make the expense to equip a botany or zodlogy class through the winter a very slight one. (6) It would be a central station to which regular collectors could send the surplus of their collections for free distribution, and so materially widen the value of their work. [Upon motion, the Chair appointed a committee to investigate the desirability of such a plan; the committee consisting of L. J. Rettger, Dr. C. H. Eigenmann and W. P. Shannon. | Tur OCCURRENCE OF UROGLENA IN THE LAFaAyYErre (INp.) Crry WaTER. By SEVERANCE BURRAGE. It not infrequently happens, even with the best public water supplies, that the attention of the consumer is attracted by some peculiar taste or oder in the water. This is particularly apt to be the case when the supply is derived from a lake or pond, or if it has to be stored for any length of time in a reservoir. In such instances the superintendent or water commissioners receive complaints to the effect that the water has a very disagreeable taste and smell, and that there must be dead fish or eels in the pipes. Just such complaints were heard in Lafayette in the early part of October, and vigorous attempts were immediately made to get rid of the trouble by flushing the pipes at different points in the city. But there was not much improvement. The city water supply is derived from driven wells in the vicinity of the Wabash River, and is a remarkably pure water, both from the chemical and bio- logical standpoints. This water is pumped directly into the pipes. There is a reservoir situated on a hill some two miles from the pumping station, and it has been generally understood that the water stored there was only used in case of an emergency, such as a large fire. But upon inquiry it was learned that the pumps were not kept working all night. Thus, as the supply from the pumps was stopped, the reservoir water must work back gradually into the pipes, replacing 57 that used in the town after the pumping had ceased. Now if the trouble was in the reservoir water, we would expect to have the complaints made in the early morning, which would be the only time, as we have seen, that this water had access to the service pipes. And such was the case. AJ] the complaints were made in the morning, and when the superintendent would go to investigate at this or that place late in the forenoon he could detect nothing wrong in the water. The pumps had started and forced the reservoir water back to a certain extent, fresh water from the wells taking its place. All of this evidence, together with our knowledge of the natural history or biology of bodies of water exposed to the sunlight would point to the reservoir as the source of the trouble. A microscopical examination of this water was made, and it showed the presence, among other things, of the colony-building infusorial organism Uroglena in small numbers. This Uroglena is well known in Massachusetts and Connecticut as having caused strong fishy tastes and disagreeable oily smells in many large water sup- plies, and in some cases in the very best ones. So that knowing the history of this organism, and finding it in the water of the reservoir, it was unnecessary to search further for the trouble. This organism itself has been described by Ehrenberg!, Biitschli?, Stein’, Kent*, and Calkins’. It was first recognized in this country by Conn’, who found it in the reservoir of the Middletown (Connecticut) waterworks. Since then it has been known to cause trouble in a large number of prominent Eastern water supplies. ; The colonies in the LaFayette water were just visible to the naked eye, being considerably less than ;}5 (one one-hundredth) of an inch in diameter, and spheroidal in shape. Each colony is made up of a delicate gelatinous matrix, in the periphery of which are imbedded two hundred or more individual monads, these monads having two flagella each, chromatphores, and, quite important to us in connection with water supplies, many oil: globules variously distributed throughout the cell. It is supposed, and with good reason, that these are the direct source of the oily taste and smell in the water. When the colony is intact, in its normal condition in the water, very little if any odor can be detected; but let that water be disturbed in such a way as to rupture or disintegrate the colonies 1Die Infusionsthiere als vollkomna Organismen. Leipzig, 1838. *Zeitschrift fiir Wissenschaftliche Zodlogie. 1878. Bd. XXX, p. 265. °Organismus der Infusionsthere, III. 1878. 4Manual of the Infusoria, I. London, 1881. (W. Saville Kent.) On Uroglena. G.N. Calkins, in Annual Report Mass. State Board Health, 1891. ®Report of Water Commissioners for 1889, Middletown, Ct. 58 and the odor becomes quite strong. This, of course, is what occurs when the water runs into the service pipes. The change of conditions causes the disrup- tion of the colonies, and so we get the smell and taste in the hydrant water, but almost none in the water examined fresh from the reservoir. This matter of the cause of such odors and tastes in drinking waters has been the subject of much study by the Massachusetts State Board of Health’, and I had the privilege of doing some work in that line in 1894, while connected with that Board. Most of the experiments were conducted on this Uroglena because it had such a strong and characteristic odor. Large quantities of water contain- ing an abundance of Uroglena were filtered through cotton, and this cotton was immersed in ether and several other solvents of oil, particularly the volatile ones. Then the ether was allowed to evaporate, leaving an oily residue on the watch glasses which in some cases gave the characteristic odor, somewhat intensified. But in nearly all of the experiments trouble was caused by the ether itself leay- ing a noticeable residuary odor after evaporation, which was in some instances quite misleading. The Uroglena oil, however, was collected, and did to a certain extent have the sought for odor. Among the other solvents tried were carbon bisulphide and chloroform, with the same difficulty of the residuary odor. The ordinary method of microscopical analysis (Sedgwick-Rafter) is practi- eally useless in determining the numbers of Uroglena colonies in a given quantity of water, because of the readiness with which the organisms break up. The esti- mates consequently in such cases would be far too low. In the analysis of the water supply of Lafayette made last October the water was examined without making any attempt to concentrate the organisms. Cubic centimeter after cubic centimeter was examined directly with a small hand lens, and in no case were there more than twenty colonies per 100 cubic centimeters. The average was six per 100 c. c., but this was sufficient to give the offensive odor to the water when drawn from the faucet. As was found in other cities, and as we might expect to find in Lafayette, the water drawn from the housetops in the morning, while giving the odor, showed absolutely no Uroglena colonies. The question naturally suggests itself, how did the reservoir get planted with this troublesome organism? Of course we can make no definite statement in re- gard to this, but an examination of the reservoir overflow, which forms a more or less stagnant pond just below the reservoir itself, showed a larger number of these Uroglena colonies per 100 cubic centimeters than the reservoir water, and it 10dors in Drinking Waters. G. N. Calkins. Mass. State Board of Health, Ann. Re- port, 1892, p. 355. 59 would not be very difficult to imagine that birds flying directly from the overflow to the reservoir might carry the organisms there. — To get rid of the trouble in this case was comparatively easy, because the reservoir was small and it was not a difficult matter to entirely change the water in the reservoir by keeping the pumps going full force day and night for a few days. In three weeks from the time my attention was first called to the matter, I was unable to find any Uroglena in the reservoir water, and I have heard no com- plaints since. Ii is not known that the Uroglena, even in very great abundance inthe water, causes any disturbance or inconvenience to our bodies. It is most important, how- ever, that the city engineers and waterworks superintendents should know this, in order to so inform the people when they make their complaints. The suffering public under such circumstances are apt to imagine that all sorts of ills are caused directly by this to them unseen pest, and they are too prone to find fault with the water supply. While we can not prophecy when Uroglena may appear in or disappear from a water supply, we can state with much certainty that it is perfectly harmless, and that it does not necessarily indicate a bad condition of the water. The Lafayette water, for the past two years at any rate, has been abso- lutely free from all dangerous contamination, and the recent appearance there of Uroglena does not mean that the water supply is at all degenerating. THE ENGINEERING RESEARCH LABORATORY IN Its RELATION TO THE PUBLIC. By W. F. M. Goss. In the present era of the world’s progress we hear much of our ‘‘ material prosperity ” and of the ‘‘development of our resources.” Feeling sure that the earth was made for man, man is anxious to make his possession yield him its best. Nor is he contented with what his own immediate neighborhood can furnish. If there is anything in the ends of the earth, or in the air, or in the sea which is capable of making for his advancement, he rests not until he has secured it. The business of the world, therefore, increases with every hour, and its problems multiply. In the midst of its hum and hurry, the engineer is a prominent figure. It is his province to study the properties of matter and to make them useful to man in structures and machines. He deals with the mining and reduction of ores, the chemical and physical properties of metals, and all the great variety of processes by which iron and steel are shaped for purposes of construction; with earth-work 60 dams, with systems of municipal piping, with steam engines and pumping ma- chinery, with locomotives and other railway equipment, with bridges and build- ings, with ships and harbor improvements—in fact, with structures and machines of every conceivable type. : The engineer is the servant of the people. His ingenuity and skill are the starting point which leads to the employment of all the artisans who fill our shops and factories; his work makes possible the peace and comfort of household life, the success of social affairs and the perfection of business methods, and it often serves to furnish inspiration for modern thought and to give direction to its tendencies. The basis of the whole science of engineering, extensive as it is, is to be found in facts which have either been deduced from practical experience or derived from especially conducted experiments. The early engineer could neither lean upon accepted theories nor look to precedent for guidance. It was not what Brindley, and Telford, and Watt, and the two Stephensons knew, but what they did, that helped to inaugurate our present era of engineering. Since their day, every important structure has served a double purpose: first, that for which it was especially designed, and, secondly, that which regards it as a sub- ject for observation and study. Where such structures have been a complete success, information concerning them has become a matter of record, and the essential facts have been given a place in the annals of good engineering practice; and where structures have failed, the causes have been carefully studied, that the fault might be understood and consequently avoided in future work. Successes, therefore, have inspired imitators, and failures have warned all followers. But while it is in this manner that a large part of our present fund of engi- neering data has been brought into existence, and while the process still goes on, it is admitted to have its limitations. The attempt to build a house and at the same time determine the subsequent behavior of certain details entering into its construction, is illogical and expensive. For example, it is poor economy to ascertain the strength of an iron column by finally seeing it fall under the load of a wall. A crack in an arch or a fragment from an exploded boiler may testify to faults in construction,.and may even serve as a basis for theories leading to better practice, but the information obtained is dearly paid for in the damage suffered by the collapse of the arch or the explosion of the boiler. Again, great as are the losses occasioned by failures, they do not equal those which occur through fear of failure. The fear that workmanship may be bad or materials defective leads to lavishness which could not be justified if our informa- tion were more definite. It is indeed true that ‘‘factors of safety are factors of 61 ignorance.” When it is doubtful just how great a resistance can be withstood by a given bulk of material, we make success certain by building many times stronger than is really necessary. If we could know at the outset the exact value of the stresses involved and the actual strength of the materials to be employed, it would become obvious that such a practice as this could give no additional security, and its result would be wastefulness. In the domain of machine construction the same general principle applies. The demand is everywhere made for machines that will act with a higher degree of efficiency; that is, do their work with less wear and tear and at a lower run- ning expense. There is no lasting market for inferior gocds, and success in competition is to be obtained as the result of merit. Thus it is that designing engineers who give their thought and skill to planning great bridges, buildings and machines are successful in proportion to their ability to simplify and cheapen and at the same time perfect, while all unite upon the general principle that a bridge must not only stand, but it must also involve 4 minimum of material, and a machine must not only run, but must do its work with the highest degree of efficiency. It is clear, therefore, that what is needed in engineering work is a more perfect knowledge of the materials and forces involved. This is not a reflection upon the knowledge of the past, but a suggestion that its fund is insufficient for the future. The engineering of the last quarter century has done much to make definite matters which were before but little understood. Facts have been gath- ered and compared, and from them theories have been deduced. Failures are fewer and the efliciency of structural work, and of machines of every sort, has been increased. But the end is not yet. To-day, more than ever before, the attention of the whole engineering world is directed to methods of improving and saving. Its efforts are put forth in response to the demands of a more exacting clientage, and this clientage is the public. It is evident that everything which contributes to the perfection of engineering methods must benefit the people and must arouse their interest, for it is the people who finally reap the advantages, as well as pay the price. Hence public interest in the work of the engineer is keen and critical, and will always sustain any serious movement which promises té advance true practice. Such a movement presents itself in the establishment of laboratories devoted to engineering research. When all forms of mechanical construction were crude it was possible to im- prove by the mere application of experience, but as construction became more refined it was necessary to examine with greater accuracy and to proceed with greater care. The crude stage in engineering is now a thing of the past, and 62 every day increases the degree of refinement which characterizes the work. The research laboratory stands as a response to these conditions. It is its function to investigate, in a scientific manner, problems which arise in practice or which may be suggested by practical experience. The tields of science and the field of engineering combined make up its proper domain. Its equipment, therefore, em- braces the delicate apparatus of the scientist and the ponderous machinery of the engineer, and its lines of investigation may be chemical, metallurgical, structural, pneumatic, hydraulic, or thermodynamic. Its methods eliminate the complicating conditions of service and allow effects to be traced singly to their causes. For example, efforts to determine the power and efficiency of locomotives while in service upon the road extend back through more than three decades, with no general result that is satisfactory. But the difficulties and inaccuracies which appear in the process of road testing entirely disappear when tests are made in the laboratory, for here it is possible to maintain for an indefinite period an unvarying condition of speed and load, and to employ sensitive apparatus in observing the performance of the machine. There have been many instances where locomotives on the road have left bent rails in the track behind them, but it required the laboratory to demonstrate that under conditions not uncommon in practice, the drive-wheels of a locomotive leave the track at every revolution. This being proved, the matter of the bent rails was easily explained. Again, it has been assumed for years that the draft produced by the exhaust steam in a locomotive was the result of an action similar to that of a pump; that each puff from the cylinders supplied a ball of steam which filled the stack as a pump piston fills its barrel, and pushed before it a certain volume of the smoke- box gases until it passed out at the top of the stack. Believing this view to be the true one, designers have shaped the details of locomotive draft appliances accordingly, and the value of proposed improvements has been measured by the completeness with which they have satisfied the conditions of the accepted theory. But the processes of the laboratory have disproved this whole assumption. They have shown that the steam does not fill the stack except at its very top, and that the action of the jet is clearly one of induction. In accordance with these results a new theory has been formulated, and although it is but a few months old, the laboratory facts which sustain it are so conclusive that it has already been generally accepted. These illustrations, drawn from a single field of inves- tigation, will serve to show something of the character of the work done by the research laboratory. They might, with equal justice, have been selected from any one of the many different departments into which engineering research may 63 be divided. But they have served their purpose if they have emphasized the fact that the laboratory process gives results which can not be obtained in any other way, and that these results may be relied upon to guide and direct practice in engineering affairs. English technical papers admit that the painstaking processes of German laboratories have so well guided German manufacturers that Germany not only competes with England in many lines of manufactured goods, but in some has driven her from her markets. We have a new country, in which large engineer- ing enterprises, both public and private, are always being pushed and are calling for economy in expenditures; and there is a strong national desire for an outlet of manufactured goods through exportation, which can only be secured on merit, in competition with the world. With these facts in mind the conclusion is obvious that there is room and need in this country for research laboratories. All such laboratories are but means to ends. They are not only contributors to the public fund of information, but they infuse into every branch of construction and of operation a spirit of accuracy and a desire for excellence. LovuIsvILLE FILTRATION EXPERIMENTS. By Gro. W. BEntToN. The lst of August, 1896, completed the routine work of one of the most unique series of experiments the scientific world has had the privilege of wit- nessing. The question under investigation was the chemical and bacterial con- dition of the Ohio River water, as furnished the City of Louisville, Ky., and the relative merits of the several systems of filtration seeking establisament there, and proposing to do away with the mud and its accompanying bacterial impuri- ties, so familiar to the citizens of and visitors in the great cities adjacent to the Ohio, the Missouri and the Mississippi rivers. The peculiar yellow clay suspended in the Ohio water will not subside even on standing, and ordinary schemes of filtration utterly fail in its treatment, even in times of low water. In view of the conditions, Mr. Charles Hermany, Chief Engineer, and Mr. Charles R. Long, President, of the Louisville Water Company, decided that the only sure way to treat the question was by means of an experimental plant erected on the ground and operated for a term of months, which should give them definite knowledge of the water in every stage. In accordance with this 64 plan, Mr. Long issued an invitation to all the large concerns engaged in the filtration of water on an extensive scale to establish experimental plants at the pumping station. The terms of the arrangement were as follows: Each company entering the competition to establish its own plant and operate it with its own representatives in charge; the Water Company to provide tem- porary buildings for the housing of these plants, the necessary steam power, and the unfiltered water to be used in the experiments. The entire operation of the plants to be under the supervision and control of a competent staff of engineers and scientific experts in the employ of the Water Company, who were to have access at all times to the several plants, keep accurate records of metre readings, both of filtered and unfiltered water, to take samples at any time and at any stage, to examine the chemicals used as to quality and quantity, and to note the expense of the power required for operating the machinery. Four companies entered the competitive test, namely: (1) The O. H. Jewell Filter Co., of Chicago, presenting the Jewell Filter; (2) The Cumberland Manu- facturing Co., of Boston, presenting the Warren Filter; (3) The Western Filter Co., of St. Louis, presenting two filters, the Western Gravity and the Western Pressure; (4) The John T. Harris Magneto-Electric Purifying Co., of New York, presenting a process based on electrolysis. These filters are doubtless well known to those interested in water examina- tion, as they are extensively advertised, and time will not be taken to consider the details of their operation. Work began October 1, 1895, with a laboratory force of three, including Mr. George W. Fuller, Chief Chemist and Bacteriologist, in charge; Mr. R. S. Wes- ton, Chemist, and Mr. C. L. Parmelee, Engineer. This force was gradually increased until, at the close of the period of work, there had been added to those already mentioned Mr. J. W. Ellms, Chemist; Mr. G. A. Johnson, Clerk; Mr. H. C. Stevens and Mr. R. E. Bakenhus, Engineers; Mr. Hibbert Hill, Bacteriol- ogist, and myself. I can not refrain from expressing at this time my high appre- ciation of the enthusiasm and untiring energy, the skill and scientific value, of the experts named. The volume of work was enormous, and during the month of July, when I had the privilege of ranking as one of the force in the bacterial laboratory, our chemical thermometers frequently ranged (expressed in Fahren- heit degrees) 98 to 100. The excessive heat had no effect upon the work. Every man seemed infested by the work bacillus, and spread contagion throughout the whole plant. During July, not counting specie work, which constantly went on, over fifteen hundred bacterial samples were plated and counted; in many cases, recounted the second time. The chemists were equally busy. 65 Ethical as well as business reasons prevent the announcement of even approximate results, the complete elaboration of which will appear over Mr. Fuller’s name early in 1897, whether in public form or as a private report to the Louisville Water Company I am not informed. In any case, the matter which it will contain concerns not Louisville aloe: but the world as well. It is to be hoped that water experts will have access to it. I believe that I am entitled to say, however, that Ohio River water has been successfully filtered in quantity, under the most extreme conditions, during the course of these experiwents. It has come from the filters clear and sparkling, on days when the chemists found in the neighborhood of 3,500 parts of solids per million, and when the river showed 12,000 to 25,000 bacteria to the cubic centimeter, I have counted six to ten indi- vidual colonies in the filtered water. The equipment of both chemical and bacterial laboratories was complete and thoroughly up to date. The methods for bacterial work, preparation of media, classification, etc., were mostly taken from unpublished manuscripts. The steam sterilizer was largely replaced by the autoclave, at a pressure of 20 pounds and a registered temperature of 126 degrees Celsius. Color tests were a feature of the chemical work. the method being that of the Massachusetts State Board of Health. Chemists and bacteriologists can not praise too highly those members of the Louisville Water Company, who, in the face of much criticism, and at such great expense, have not only made possible the solution of the question of their own water supply, but that of the great cities of the Mississippi basin, and at the same time placed in Mr. Fuller’s hands the means of enriching our experience in the handling of refractory sources of potable waters for cities. Indianapolis, December 30, 1896. Gro. W. BEnTON. A ‘“TorNADO” In RusH County, Inprana, Avucust 1, 1896. By W. P. SHANNON. On the first day of last August there was a destructive storm along the south- ern line of Rush County. Approximately, we may say, it began near Milroy in Rush County, and ended near Metamora in Franklin County, running from west to east on a line bearing but little to the south. It was not continuous. The most destructive part of its course was shortly after the beginning, on my old home farm. I visited the place two days after the storm. My brother, H. F. 66 Shannon, who was in the storm, described it as a cannonading from the clouds, and, as the evidence shows, this figure is a good one. What seemed to be an ordinary rain cloud rose from the north. In a short time the cloud showed that it was bordered behind with a straight line, and the blue sky appeared beneath. It seemed that in a few minutes the cloud would be over and all would be bright again, when suddenly from the rear edge of the cloud in the northwest vapor began to puff downward; in a moment a broad bind of buff-colored cloud reached from the main cloud to the ground, not straight down but obliquely to the south, and curving more southward near the ground. This. band was a half or a mile wide, the width of the storm as it was approaching; then parallel bands began to float southward from the main band. Then the real nature of the band began to show itself—it seemed that shots were being fired fast and thick in front of the main band from the upper cloud to the ground. Imagine the smoke from a cannon to continue to boil from the ball as it progresses, and you have a picture of one of these shots as it went from the cloud to the ground. The buff color, or the dust-like appearance, may have been due to electricity. The storm ran from west to east along the well defined rear edge of the main cloud. c While the storm was passing, my brother was in a barn near the south doors, which were open. (The roof of the barn slopes to the east and west). While the- storm was approaching it gave a rumbling sound, while it was passing it made a hissing sound, and the air was so full of vapor that the house, a few steps from the barn, couldn’t be seen. Suddenly there was a dead thud on the west side of the barn, then a deluge of water poured from the hay above, and all who had taken shelter in the barn had to gape for breath. Then he saw passing obliquely before the open door what he took to be the head end of one of the shots. It was like frost particles moving among one another, as bees while swarming. The thud west of the barn was another one of those shots. Those who were in the house had retreated to the cellar, when they were deluged with water. They noted the hiss- ing sound and a glare of lightning over the ground, and had the same difficulty to get their breath. A woodhouse and the porch connecting it with the house were- knocked into pieces, and large trees about the house and barn were broken off or uprooted; but no one heard any crashing of timber or buildings, the only noise was the hissing sound. A hundred acres of corn west and northwest of the barn was laid flat. In a. piece of timber, beyond the corn, three-fourths of the trees were knocked down. In another piece of timber, southwest of the barn, nearly all of the trees were down. About forty rods east of the barn is another tract of timber. In a hundred 67 acres of this more than half the trees were down. A map of the 2,000 acres of land covering the most destructive part of the storm’s course, with lines showing the directions in which trees were thrown, should have the lines arranged fan- shaped, running from north to south on the western border of the map, and from west to east on the northern border. These lines may be evidence that the storm was not a tornado. My brother took me over the ground and showed me the records of the work. They were not so striking as immediately after the storm, but they were still plain. In a piece of bottom land, covered with horse weeds, a large sycamore tree had been turned out of root, and in a circle of fifty feet or more in diameter about the root of this tree the horse weeds were flat, almost beaten into the ground. It looked as if a great ball of water, or something, had struck the ground there and turned the tree out of root. It was no trouble in the patch of horse weeds, or in the corn field, or in the grassy woodland, to pick out where every shot had struck the ground. In every case where a shot struck the ground in front of or at the base of a tree, the tree, if green, was turned out of root, if dead, was broken off even with the ground. In most cases where the shot struck a tree above the base, the tree was broken off. In one case, while standing at the base of an upturned tree in the center of the spot of fattened grass, we could tell by looking upward and westward, the course of the shot by another tree that had been topped in its path. In another ase we were standing in the center of a spot of flattened horse weeds, wondering why the shot didn’t hit one or the other of two ash trees on the west side of the spot; soon we observed by limbs broken away that the shot had passed between the two trees. In nearly every case where a tree had been topped, we could find the spot of flattened grass a little distance east or southeast of the base of the tree, the direction depending upon our position in the deyastated area. In this way we could, in nearly every case, make out the path of the shot through the air. Near the central part of the devastated area the shots moved from the northwest downward at an angle of 45°. In the eastern part of this area they moved nearly eastward at an angle of 30° with the horizon. In some cases a dead tree was un- harmed, while a green tree near by was turned out of root, or had its top cut off. ‘There was evidence that, on the south margin of the devastated area, trees were blown down by the wind; but in the central part they must have been knocked down by globe lightning, or something’ else, shot from the cloud. The evidence is that each shot was accompanied by electricity, rarified air, and a deluge of water. The appearance resembling particles of frost flying among one another, as swarming bees, suggests electrified snow. Such a suggestion may dJead to experiment. What kind of a storm was this? 68 CoMPARATIVE CRUSHING STRENGTH OF CUBES AND PRISMS OF BEDFORD LIME-. stone. By W. K. Harr. [ABSTRACT.] An examination of the curve representing Baushinger’s experiments on the crushing strength of stone cubes as compared with the strength of stone prisms, will show that the law of variation of strength is such that the strength of a prism whose height is 1}, the length of its base will be only 92 per cent. the strength of a cube of equal section. It is a matter of doubt whether such a difference will occur between tests of any given specimens of the variation in height mentioned under the ordinary condition of testing. Tests of 31 specimens of Bedford Limestone (of rather soft variety) made at Purdue University, show that 17 cubical specimens (4x4x4) were slightly weaker than 14 prisms (4x4x6) of the same material, subjected to the same conditions throughout. Specimens were bedded in plaster of paris. The average angle of failure in shearing was 64.5 degrees. Some Mounps oF VANDERBURGH County, InpIANA. By A. H. PURDUE. Exactly in the southeast corner of Vanderburgh County, Indiana, is a collec- tion of mounds and earthworks, which, so far as I am aware, have never been fully described,* and which are doubtless among the most interesting of the State. They are locally known as the Angel Mounds, taking their name from the owner of the land on which they occur. As the ground upon which they are situated is nearly all under cultivation and the mounds are rapidly disappearing, it is desirable that a description of them be placed in permanent form. The remains are situated upon the alluvial soil of the Ohio River, north of Three Mile Island, and lie between two bayous, one on the south separating Three Mile Island from the main land, and an older one on the north. When in a perfect state there was probably an inclosure, formed by the bank of the bayou on the south and an irregularly curved wall, presumably a rampart, either end of which was terminated by the embankment. At present there are about 1,400 yards of this wall remaining. As it now stands it is from 5 to 10 feet wide at the base, and from 1 to 2 feet high. At intervals, usually of from 37 to *An imperfect description of these mounds will be found in the Smithsonian Report, 1881, p. 591. 69 40 yards, there are semicircular mounds with radii of from 5-to 8 feet, joined to the outer side of the wall. On the supposition that the wall was a rampart, these semicircular projections from it were probably lookouts from which the guards could easily flank the outer face of the wall. It will be seen by reference to the map that there is within the outer wall a similar inner one, which terminates in Mound No. 2. There is evidence, though very slight, that this wall formerly ex- tended from Mound No. 2 southward. It is possible that it marks the border of the original inclosure which was afterward extended to the outer wall. The area included between the outer wall and the embankment north of the present bayou is a little more than 5 acres. The most striking object among the collection is the large mound within the inclusure. Its longest diameter is 500 feet. Its width varies from 175 feet to 225 feet. With reference to altitude it is divided into three parts. The southern part, which is 160 feét long and which has been under cultivation for years, varies in height from 6 to 9 feet. The east border of this part is somewhat ob- secured, from cultivation and erosion, but the south and west borders are distinct. The second part of the mound rises about 17 feet above the first part, and is 26 feet above the base. The top is flat and is 240 feet long by 112 feet wide, and has been utilized until recently for an apple orchard. The third part is a dome 13 feet high and stands on the southeast corner of the second part. The base of this dome is about 48 feet in diameter, and the highest point is 39 feet above the ground on which the mound rests. If the trees along the Ohio River were re- moved, the top of this dome would afford a commanding view for several miles up and down the river. I shall not even venture a conjecture as to the purpose of this remarkable mound. Besides this, there are six other mounds within the inclosure, denoted by Arabic numerals. These mounds are all circular at the base and have rounded tops, except No. 3, which is a truncated cone. It has a diameter of 160 feet and is 10 feet high. Trees of walnut, oak and maple are growing upon it. The largest tree is an oak, which is 23 feet in diameter. This mound has for a long time been used by the people of the vicinity as a burying place. Mound No. 1 is 115 feet in diameter and 12 feet high; No. 2, 90 feet in diameter and 6 feet high; No. 4, 100 feet in diameter and 5 feet high; No. 5, 60 feet in diameter and 4 feet high; No. 6 is a small indistinct mound. All of the small mounds, except No. 3, are being cultivated. In Mound No. 5, Mr. Charles F. Artes, of Evansville, reports having found 13 human skulls, 12 of which formed the circumference of a circle, the thirteenth 6 a «“ 70 being in the center. All were well protected by slabs of shale. No human re- mains are reported from any of the other mounds. In the southeast part of the inclosure the plow frequently brings to the sur- face bones of birds, small and large mammals, and human beings. This is for that reason designated on the map “ Burying Ground.” Pieces of pottery, such as is now made by the western Indians, are common within the inclosure. On the north side of the old bayou, beyond the area shown in the map, is an old excavation, from which a portion of the earth in the mounds was doubtless obtained. In this excavation are stumps of oak trees, two feet or more in diameter. A striking feature of these mounds is their perfect state of preservation. True, the rampart, if it were such, has been greatly reduced in height; but this is probably due to the fact that most of it overflows during the Ohio floods. The east end of the natural embankment north of the bayou and south of the Burying Ground was improved, and, with the exception of a few small washes, now stands as it was left by the aboriginal men who did the work. The large central mound, except where cultivated, is apparently in a perfect state of preservation. The ap- parent recency of the work certainly indicates that it is none other than that of the American Indians. Why these mounds were located here on this alluvial soil, most of which over- flows, and which is productive of malaria, while the highlands are only a mile north, and three miles to the northeast, at the town of Newburgh, is one of the most commanding views along the entire course of the Ohio River, is a question. About a mile northeast of the large mound is a single conical mound, 150 feet in diameter and 25 feet high. There are several small mounds along the alluvial deposits of the Ohio in Warrick County. Angel Mound (1894) _ pie 1 Agha tal = é z = = 2 G = é = é Burying- Ground THATS WENA WINE yy . — wif E, ft ait n (4 ny EE 1\ 3 ALR TT 1) CTU GT DH ME ryt BY A.H. PURDUE 1894. 11417) Ot Ahn Vanderburg County, Ind, ANGEL MOUNDS Wt PHO cyt ~] bo THE LAKE MICHIGAN AND MISSISSIPPI VALLEY WATER SHED. By T. H. BALL. Commencing near the headwaters of the Des Plaines River in Wisconsin, but a few miles from the shore of Lake Michigan, then passing southward, winding slightly, passing within eight miles of Lake Michigan, and then, just west of the city of Chicago, passing the south arm of the peculiar Chicago River, still going southward, this line passes west of Blue Island, eight miles west of the Indiana State line. It then passes southwest around the headwaters of Rock Creek, and then, southeastward, around Thorn Creek, which is its most southern point in Illinois, and is near Eagle Lake, two miles west of the Indiana line and directly west of the Lake County village of Brunswick and twenty three miles south of the State line monument on the shore of Lake Michigan. This line then passes northward and enters Indiana and Lake County in section 36, township 35, range 10 west of the second principal meridian. It then bears southeastwardly around the headwaters of West Creek, to a high, wooded ridge about a quarter of a mile north of Red Cedar Lake, and then passes along a low, curving ridge on which was once a wagon road, the most beautiful and best marked portion of the line in Lake County. It passes eastward three miles over a timbered table-land, and running south of the center of Crown Point about two miles, it passes across sec- tion 17, on which was laid an ‘‘Indian float,” and the south part ‘of section 16, township 34, range 8 west, and then south on the east side of the old Stoney Creek, and east across sections 35 and 36, in township 34, range 8, and into sec- tion 31, range 7 west, where is now the village of Le Roy, and where it turns northward, having reached its extreme southern limit in Indiana. Here it winds around the head of the south branch of Deep River, passing between that and Eagle Creek, and bearing eastward, south of Deer Creek, it leaves Lake County almost due east of the center of Crown Point, distant from that town seven miles and a mile and a half, nearly, south of its point of entrance into the county. It then passes north of a little lake, and then east, and then ina northeasterly direc- tion across Porter County, running barely south of Valparaiso and north into Liberty Township in township 36, range 6, then east across Jackson Township into Laporte County. Passing the city of Laporte and running eastward near the line of the Lake Shore Railroad, distant a few miles oniy from the north line of Indiana, it turns again southward till it comes into Portage Township in St. Joseph County, a little west of South Bend. And here on this noted portage be- tween the St. Joseph and Kankakee Rivers, this notice of this watershed line will close. 73 It may prove a matter of interest to some, in another generation, to have this line traced with even this much definiteness, although, of course, it has not been given with the entire accuracy of a surveyor’s field notes; for the drying up of water courses and the drainage by means of large ditches have already almost consigned to oblivion the names and the winding beds of some of the small streams that were well known to the Illinois and Indiana pioneers. Some Norice oF STREAMS, SPRINGS, WELLS AND SAND RIDGES IN LAKE County, Inpriana. By T. H. Batt. Some of the natural features of Lake County, Indiana, are rather peculiar, and are quite surely of interest to students of physical geography. Bounded on the north by Lake Michigan, on the west by Illinois, on the south by the Kankakee River, if the waters of Lake Michigan ever passed southward into the Mississippi and the Mexican Gulf, as some suppose, the outflow was quite surely over a part of what is now Lake County. Of the two most southern points of the Lake Michigan basin, as stated in a former paper, one is in Lake County, eighteen miles south of Lake Michigan, and the other is distant about fifteen miles, almost exactly west, not far from the IIli- nois line. North of the water shed the beds of the streams have an easterly and westerly direction mainly, or northwesterly and northeasterly, while south of this line the streams flow mainly southward. The Calumet, the largest northern stream, is quite peculiar in this respect, that it flows across the county nearly twice, one stream known as the Little, the other as the Grand Calumet. The windings of the bed of Deep River, the second in size, are quite remarkable, and this stream, for some two miles of its course, flows due north. While not a region of brooks, there are, nevertheless, in this county, some in- teresting and remarkable springs, about twenty in number, that are quite well known. Three of these are near Crown Point, and in the Deep River Valley. One has excellent, healthful, mineral properties, and one will furnish water suf- ficient, so its owner believed, to supply the wants of a thousand head of cattle each day. A fourth of these springs is near Creston, in the Cedar Creek Valley, affording a large amount of water, and covering several square yards of surface. A fifth one, furnishing quite a flow of water, is on the west side of Red Cedar Lake, north of Paisley, at the base of the low bluff. The sixth is on the east side 74 of the lake, south of the Sigler hotel, some rods out from the bluff, and once coy- ered with the lake water, and the seventh is still covered by the lake water, in the northeast part of the lake, its existence ascertained by bathers, or divers, on ac- count of the change in temperature of the water. Others like it doubtless feed the lake. The eighth to be mentioned here is in the east part of the town of Lowell, in the Cedar Creek Valley, the feeder of a beautiful little fish pond. The ninth, and last, to be specially mentioned, and surely not the least, was known in the early settlement of the county as the Mound Spring, or Springs. These springs, forming quite a stream called Spring Run, are in the prairie, two miles east of the Lowell mill pond, and a mile east of Pleasant Grove. From these springs water was hauled in barrels for three or four years to supply many fami- lies of early settlers. Other fine springs are in Cedar Creek and Eagle Creek townships and along the West Creek Valley, nearly all being lowland springs.and furnishing excellent water. At LeRoy, near the water-shed, there is a well called artesian, sixty-two feet in depth, which is an artificial spring. The water is excellent. There is another like it a mile east of Crown Point in the Deep River Valley, near the river bed, eighty-five feet in depth. At Hammond, in the Grand Calumet lowland, are three true artesian wells eighteen hundred feet in depth. An effort was made to obtain one on the public square at Crown Point, but after going through 16 feet of earth and clay, 100 of quicksand, 25 of blue clay, 112 of slate and shale, 667 of blue limestone streaked with pure white sand rock, brown sand rock and fine gravel of different colors, and into so-called Trenton rock, in all 3,100 feet, the effort was abandoned. No rising water found. The sand layers and ridges of the county form an interesting study. The shore of Lake Michigan is all sand, and this sand, generally in ridges, some mas- sive, some low, running about parallel with the shore line, with marshes and swales intervening and some swamps extend to the Little Calumet, with an average width of seven miles. Some of this sand is quite white, some yellowish. South of the Calumet a ridge of sand extends across the county passing out into Illinois for several miles at Lansing, and leaving the county on the east near Hobart. This ridge varies in width, being twenty rods and then less and then more. The crest is in some places thirty or more feet high. Its direction is nearly east and west. South of it, on the west side of the county, is yet another ridge with a base about as broad and a crest as high, commencing at Dyer on the State 7d - line fifteen miles south of the Illinois and Indiana corner-stone, and passing east- ward five miles and three-quarters, then turning northward, taking in the town of Griffith and becoming much broader, it bears northeast and connects with the ether ridge near Ross, half way across ‘the county. This ridge seems to have been once washed by Lake Michigan’s ‘‘ proud waves.” South of these main ridges and large sand barriers are four special sand banks or small ridges that are worth inspection. One is three miles west of the north end of Red Cedar Lake, a large bank on the West Creek Bluff out of which a few years ago a number of human skeletons were taken. The second is on the northeast shore of that lake, where, also, human skeletons, some twenty in number, were taken out in 1880, and where is now a known, undisturbed Indian burial ground. The third is one mile and a half west of Crown Point, near one of the head branches of Deep River. It is known as the Beaver Dam and isnear.a large marsh. The fourth is three miles and a half east of Crown Point, near one branch of Deep River. In the north part of Crown Point sand comes within a few feet of the surface, but some prairie soil now lies over it. The immense bed of sand over the Kankakee marsh region, some five miles in width, is covered by several feet of muck. Unlike the deep white and yellow- ish sand of Lake Michigan, this marsh sand makes excellent roadbeds, five, north and south, marsh roads having been made with it. No time now remains for noticing what these few facts indicate in regard to the physical conditions here somewhere back in the mighty past. Account OF A MoRAINAL STONE QUARRY OF UPPER SILURIAN LIMESTONE NEAR RICHMOND. That bowlders, or rock fragments in some form are to be found in the track of a glacier, is one of the most familiar of phenomena. From Maine to Minnesota, and beyond, these fragments are in a direction southerly, with greater or less deviation, from the rock masses to which they previously belonged. Lines of boulders, pebbles, sand and rock-paste are strung along or spread in the course of the ice sheet; granite from granite quarries, gneiss from gneiss beds, quartz from quartz veins, conglomerate from conglomerates, copper from copper deposits, and so on from wherever they were formed in place. But that an acre, more or less, of stratified rock should be grasped, en masse in the great ice palm and dragged or shoved for miles is not so common. Professor Orton, in the Geological Report of Ohio, Vol. III, page 385, men- - tions a mass of Clinton Limestone sixteen feet thick and covering three-quarters of an acre, quite below its geological horizon and resting on glacial clays and gravels which separate it from the blue limestone of the Cincinnati rock beneath. The subject of this paper is a mass of upper silurian rock, Niagara limestone, or more likely, Niagara and Clinton. It is clearly a drift deposit and was originally the greater part of an acre in extent. It is difficult to say just what is its area as it extends back from the hill-slope, where it is exposed, under a heavy deposit of later, modified drift. The Evansville & Richmond Railroad, which was never finished further than the road bed, cut through it a few years since to its full depth, or very nearly. Portions of the border of this rock moraine had been ex- posed for time unknown by erosion. A mixture of clay, sand and a variety of small boulders separates this deposit from the Hudson River rock of the Lower Silurian. Fig. 1 gives a view for near 70 yards east and west. It has been five years since the rocks were cut through, and as a consequence the superposed loose ina- terial has drifted over the ledges and into the crevices, partially obscuring the promiscuous jumble of the separate masses. Still it can be seen that the coarse chunks of various sizes and forms are jammed together at all angles. Fig. 2 represents an instance of a large block glaciated on the under side. The use of a glass will aid in discerning the well-marked strie. One or more observers who have examined the deposit are of the opinion that the rock was glaciated from above while in place, and subsequently inverted, but the repeated occurrence of such under-polishing and the finding of it nowhere but at the bottom, would seem to indicate that it was caused by sliding over the surface below. Furthermore, some of the blocks, while being shoved along, appear to have tilted upward in front, and as a result were rounded off at the heel. Much of the rock is thick-bedded and very compact. Other portions are softer, disin- tegrate very easily, are stained brown by iron oxide, and are composed mainly of crinoid fragments. The harder rock contains various species of corals and brachiopods, and occasionally the trilobites Calymene niagarensis and Illenus day- tonensis. Large bowlders of this limestone are found for a mile and more south and southwest from the main moraine. All must have been removed from a point eight, ten or twelve miles north. The fine exposure of striated bed-rock at Thistlethwaite’s pond, two miles to the north, has the striew pointing south 26° west, which is very nearly in line with this morainal deposit. Bia Merrago- Thick es Ain Fig.1. North Side of Cut—East and West. Extent near 70 yards. Shows how the rock masses tip atallangles. G. The ledge that is polished on under side, as in Fig. 2. Fig. 2. Nearer view of a mass, marked M in Fig. 1, showing glaciated surface on under side—W. W to BH,six feet. Sy H gee 3 S. 1 Ps 2 ae ; ; s B , es as shown by erosion in creek bank below point W in Fig. 1. M, M, M, masses buried in talus. P, pit from which rock has been quarried. West end of moraine 79 ForMULAS FOR SHAFT Friction. By J. J. FLATHER. Among the various methods employed for the long distance transmission of power shafting has been used to a limited extent. In many of the earlier applications the motion was one of translation. Thus in the transmission of power from the large overshot wheel at Laxey, on the Isle of Man, trussed rods are used to transmit about 150 h. p. several hundred feet ; the rods are continuously connected and are supported on wheel carriers running on iron ways. This method was adopted, on a very large scale, in the mines of Devonshire for the transmission of power from large overshot water wheels to pumps fixed in the shaft of the mine at a considerable distance higher up the valley. In one case the water wheel was 52 feet diameter, 12 feet breast, and its or- dinary working speed was 5 revolutions per minute. The length of stroke given by the crank to the horizontal or ‘‘ flat” rods was 8 feet; the rods were 33-inch round iron, and were carried on cast-iron pulleys. At Devon Great Consols, near Tavistock, there are altogether very nearly three miles of 3-inch wrought-iron rods, carried on bobs, pulleys and stands, whereby power for pumping and winding is conveyed along the surface to differ- ent parts of these extensive mines from 11 large water wheels ranging up to 50 feet in diameter. In the transmission of power by rotating shafting supported in bearings throughout its length, the friction of the journals is a very important considera- tion, and effectually debars its use for long-distance transmission. This can be seen in the following formule, which show the relation between the horse-power required to overcome the friction of the shaft due to its weight and velocity, and the horse-power transmitted by the shaft for a given diameter and length corresponding to an angular distortion of ;'; degree per foot of length. If the contact between shaft and its bearing be a line contact only, the initial load which produces friction will be P; on the other hand, if the shaft exactly fits the bearing the friction load will be = P; midway between these lies a - value, PXI.28, or ka P, which will be here assumed as closely approaching con- ditions of actual practice when the journal is well worn to its bearing. Under these conditions the friction horse-power will be: Pao a : Way 33000 _ = 33000 (1) 13 OM peor — 80 In which F = load due to friction ; vy = velocity of surface of shaft; o = coefficient of friction for factory shafting ; W = weight of shaft. While @ varies from 0.03 to 0.08 under different conditions, we have assumed it to equal 0.06 for ordinary factory shafting, with more or less imperfect lubrica- tion and alignment. If there are no pulleys on the shaft, W will equal T ‘ = d? L & 3.36 pounds, where L = length of shaft in feet, and d = diameter of shaft in inches. The horse-power exerted to overcome friction will then be: Fy PS opis Die Gio 83 1 ae tay 5 ees F 1B El 33000 ~~? * 4 33000, — = 0:000006 d? Lv. (2) The horse-power transmitted by the shaft will be: ~~ da°?ix<2aN H. P. = 7§ 72 x 33000 * (3) If we assume the angle of torsion not to exceed ;; degree per foot length of shaft, there is obtained __ 360 X12) 360 ta = é = - Fane Gt ie ie Ci ae as (4) hence: ee OnLO Mei S< 12’ hence the ratio of power absorbed by friction to the horse-power which the shaft is capable of safely transmitting will be j HPS. | (0:0% Sa ar aonie ee = =— per cent. HP.) OUOLds Ne d2 ie _— — 85 From this expression the following table has been computed for a 3-inch shaft running at 100 and 250 revolutions per minute: | . ) Percentage of loss when length in feet. | / Diameter of shaft Revolutions per / wets f in inches. minute. - £ 100 200 400 800 =~ 1600 3 100 51 | 99 19.6 38.7 7 3 250 58 10.6 20 39° 2 aig It is worthy of remark that in long lines of shafting the influence of belt pull on the bearings is very slight compared to the weight of shaft and pulleys, so that the loss in friction is but little more than that due to weight alone. _ With better alignment and better lubrication the loss will be less than that here given; in long continuous lines of shafting the bearings are always more or less out of line, and for this reason the loss will be less if short lengths be employed. ORTHOGONAL SURFACES. By A. S. HATHAWAY. It is well known that a given system of surfaces f (x, y, 2) = c has in general no pair of orthogonal conjugate systems, i. e., such that the surfaces of the three sys- tems through any point are mutually orthogonal at that point. It has been shown by Cayley [Salmon’s Three Dimensions, p. 447] that f(z, y, 2) must satisfy a dii- ferential equation of third order if it possess a pair of orthogonal conjugates. In the course of some recent investigations on fluid motion I was led to observe that a given system of surfaces might have two pairs of orthogonal conjugates, in which ease it would have an infinite number of such pairs. In order that such may be the case f(z, y, z) must satisfy a differential equation of second order which is a particular integral of Cayley’s equation of third order. This differential equation is, in Cayley’s notation, . [(a, 6, c.f, g, h) (L, M, N)?—(a+b+e) (127+ M?+ N*))}? =4(77+ M?*+ N?) (A, B, GF, G, A) (L, M, NYP where L, M, N, a, b, c, f, 9, h, ave the first and second differential coefficients of f(z, y, 2), and A, B, C, etc., are the minors of a, 6, ¢, efe., in the matrix “J 86 A very general solution of this equation comes from a=h=e, f=yg=h =o, which are the differential equations of the series of spheres that pass through a given fixed circle, including, as particular cases, concentric spheres, planes inter- secting in a fixed line, and parallel planes. It may be shown that the above equation factors into four factors of the form Vb—e Ds Ve—d MW) = Va'—b! NM where a’, b', c, are the roots of the cubic found by replacing a, b, ¢ in the above matrix by a—xz, b—a, c—x. The differential equation may also, by the usual reciprocal transformation X— L, Y= M, Z=N, U+u=—La+M y+ Nz, be reduced to a simpler form. The preceding differential equation and the resulting theory of orthogonal surfaces were obtained by quaternion analysis. Briefly, if 7,76, are two perpen- diculars to the surface normal 6, that are also surface normals, then we have, (1) 8S Aa=—as (2) SAV Ao; (3) SAcyvAc=o. We may replace (3) by (3!) SAoy,Ao,=0, or SA¢ Vor=o, where 6A=}3 (y,SA0,+ 0, SAy;). Thus @ is the self conjugate linear vector function, whose matrix is given above. From (1) and (3!) we find VA Voce Voy=o This determines 4 as one (and 4c as the other) of the two latent directions of the plane self-conjugate vector function Voo Vo7. There is therefore in general but one pair of normals that may satisfy the conditions of which (2) becomes a condition upon o, or the differential equation satisfied by f(x, y, z) in order that it may possess a pair of orthogonal conjugates. If, however, the above plane vector function have equal latent roots, then its latent directions become indeterminate. This means that (1) becomes a factor of (3!) so that the only equations to be satisfied are (1), (2). These may be satisfied without other condition upon ¢ than the above equality of latent roots which is the differential equation that we have given at the be- ginning of the paper. NoTEe.—Since presenting the above I have noticed that the latent roots of the plane strain mentioned are proportionals to the principal radii of curvature of normal sections of the surface f (x, y, 2) =e. The above differential equation of second order therefore expresses that every point of each of these surfaces isan umbilic. Hence the general solution consists of a system of spheres (or planes) with one variable parameter, (w= Ax, y, z). The above quaternion method gives also the conditions that a system of lines may be the intersection of one pair of orthogonal systems of surfaces, or of an infinite number of such pairs. THE CALENDAR Group. By C. A. WALDO. 87 Linear EvuruHymorpHic FuNcCTIONS OF THE First ORDER. ) By E. M. Buaxer. (ABSTRACT.) Euthymorphie functions are those monogenic functions which satisfy an equa- tion of the form ¢ (2) + pi(z) ¢(fil2)) +. ~ . + :pn(2)-¢(fn(2)) +p(z)=0 Wwitererf;, <9 5 fy fas Pi < -) («Pay p ane given functions of which p,; :~ i>, Pn, p are algebraic. The order of 9 (2) is n and it is linear if alloff,,. . ., az+ fn are of the form 2. é f The paper gives a systematic compilation of the investigations of Babbage, Rausenberger, Koenigs and others upon functions defined by an equation of the _faz2z+B 6(2) =pi2)- o( art, (1) yz+ 6 (where p(z) is algebraic) in so far as relates to their existence and analytical ex- form pression. The theorems of Koenigs relate to more general functions but they are only defined within a limited circle of convergence. _The application of these theorems to euthymorphic functions and their continuation over the entire z-plane are believed to be new. A tabulation of the results contained in the paper is as follows: ; Every equation (1) can be reduced by a linear transformation to one of the three forms: 9 (2) =p (z)¢(z+1) I. shea) jb ¢ (z) =p(z)¢(az),| «|< |. III. Sub-forms and their solutions, (/ is any function), 9% (z) =p (2) ole Ia. ¢(z) = ¢ (2+ 1); f(e?™**) Ib. ¢ (2) =b¢(e1+1; b=. f(e?**) ie Lees 22 (2 Ge) rhe) B= Een _V(e—6,).... Te—ba) (Tea)... Le ey Id. ¢(z) =p(z)¢(z2+1); p(z) irrational is unsolved. Ila. ¢(z)=¢ (e292); f (2) f (e2™*2) IIb. 9 (2) = bo (ez); z—". F (222) IIc. ¢ (2) =p(z)¢(—2); (p(2). p(—2) =1); (1+ p(2)). f(2F) 88 For p(z) not a constant IIc. is the only solved form. emt Ula. (2) =9 (22); fle 54) log b 2mt IIIb. $ (z) =b¢(az); é el 2 Tog ;) ew SG" ts n 2mt Ile. $(2)=29 (a2); fmj(L+e™2). [nf U+S)- f (ia) Illd. ¢(z)=p(z)¢ (ez); (p(o)=1); 7 (z).f tae The 7(z) has the same number of branches as p(z). It may be algebraic, When transcendental » is its only essential singular point. The solution of any equation of form III. consists of a product of solutions of the four types given. New MEcHANICAL CompuTeR. By FRED MORLEY. A New APPARATUS FOR PHOTOGRAPHIC SURVEYING. By FRED MORLEY. CRUSHING STRENGTH OF WrRoUGHT IRON CyLINDERS. By W. K. Harr anp L. FLETEMEYER. TrESTs oF A WrRouGHT IRON CaR AxLE. By W. F. M. Goss. While much has been written concerning the variety and intensity of the stresses which service conditions impose upon car axles, there have been presented but few descriptions of the behavior of such axles when under stresses that are simple and definite in character. Interesting material of the latter class is sup- plied by a recent test of a 60,000-pound axle made in the Engineering Laboratory ot Purdue University. The axle tested was supplied by the Bass Foundry and Machine Works, of Fort Wayne. It is said to have been made of No. 1 wrought railroad scrap, and to have been selected at random from a lot of 100 which were being shipped to a railroad company, and with it there was delivered to the laboratory a small test specimen which had been drawn down from the crop end of the axle. As prepared for the tests the axle carried two 33-inch cast wheels, and it was tested under transverse stresses, while the small specimen was subjected to tensional tests. The work was executed by Mr. J. H. Klepinger, who perfected details in the general plan and was painstaking in the manipulation of the apparatus. 89 The tests were made on a 300,000-pound Riehle testing machine, a general view of which, with the axle in place for testing, is shown by Fig. 1. Fig. 2 gives the dimensions of the axle and the details of the arrangements for applying loads. The axle was supported by cast iron blocks, AA, four inches in breadth, shaped to the form of a bearing, and extending from the center to the outer end of the journal. The actual points of support were located in the center of these blocks. Load was applied to the wheel treads through steel rollers, BB, which, at the beginning of the test, were located 4 feet 10 inches apart; that is, at a point corresponding to a position three-fourths of an inch outside of the inner or ‘‘gauge face” of the rail upon which it may be supposed the wheels were set to run. In this manner stresses were imposed upon the axle which were in every way similar to those which might have been imposed by a car, if the axle had been in service, but to give greater facility in testing, the usual order was re- versed, the rails being assumed to be above the axle and the car below. Fig. 2 shows also the means employed in determining the deflections corre- sponding to different loads. At each end of the axle there was attached a light arm (bb), extending at right angles both to the axle and to the plane of the stresses to which it was subjected. Over these was stretched a fine wire parallel to the axis of the axle. The wire passed through the web of the wheels, in holes which were drilled for the purpose, and made sufficiently large to give ample clearance. The whole length of wire between the arms (bb) was at all times perfectly free, and the arrangement was such that although the axle might be bent by loads applied to it, the wire would remain straight. Three micrometers attached to blocks clamped about the axle served to locate the latter with reference to the wire, and thus to determine the deflection. A fourth micrometer was used to measure distances between the wheeis’ flanges in a line parallel with the axle and 163 inches distant from its center. Loads were applied at C in 5,000 pound increments, and all micrometers were read before each change of load. In this way a maximum load of 85,000 pounds was applied, under which the axle showed unmistakable signs of failure, the elastic limit having been reached with a load of 55,000 pounds. The results are presented graphically by Fig. 3, in which the curve marked “center” repre- sents the deflections of the center of the axle as determined by the middle microm- eter, Fig. 2; the curves marked ‘‘right” and ‘‘left” represent corresponding deflections for points 18 inches either side of the center. Deflections of the axle involved changes in the gauge of the wheels as measured above or below the axle, the extent of which is indicated by Fig. 4. 90 The actual readings of all micrometers are given in the tabulated statement below: | Micrometer Rerapines at Dirrerent Loaps. ToraL DEFLECTION. LOAD. m Pad 3 . o Ba core ane : ava © Sey SH Pa ° © og i on = Ot 7) es © é 3 7) = o| : a | 8 SI] <= BS a ql a PROPS a Sl ae) Bo) Oo /}A A 1A — |A me |A o 4 s FY The dimensions of the axle were such (Fig. 2) that when loaded to its elastic limit, the maximum fiber stress at its center was 29,730; at 18 inches from the center 22,100 pounds, and at the neck of the journal 20,600 pounds. The axle tested was designed for use under a freight car of 60,000 pounds capacity, the car itself weighing about 20,000 pounds. Each of the four axles under such a loaded car, therefore, must withstand a static load of 20,000 pounds, which load would develop a maximum fiber stress in the center of the axle tested of 10,810 pounds. In comparing these values with those obtained in the tests as given in the preceding paragraph, it is important to remember that the stresses to which car axles are subjected when in service arise from complicated condi- tions, and that their value can not be determined from static conditions alone. The test specimen which was forged down from the crop end of the axle was turned down in the center for a distance of 8.5 inches and tested under tension. The results are as follows: Didmeter iniin chess a tystthed. oehse Stacie rae eee cee beeierete ot 1.875 Axvea sol: cross Section j4/, sn ua msresgeees x oe eRe ee ee ae 3 2.755 Motalitoad;, pounds escola seh Seca eiene PRR Oe eieae fs acneiens 140,700. Ultimate strength, pounds, per square inch..................... 51,070. Mas tre wma oo. fc a iecd ts ce ead Chace ore ee eenTitede Aare ete a en ete 30,000. Modulustofvelasticityn ean ne toe oe meee ers re 29,671,000. 91 Area at point of fracture— : Peecre OC bariginal aves... 002. seus oe ca ee ee ete 61.6 © Ee AGLON BG SPER UGS,. POP CONG. ci ec ies sd sas oa aioisare ins a een si 27.3 Finally one end of the test specimen was exposed to the action of acids, and the etching thus produced used in printing Fig. 5. This figure, therefore, shows the disposition and relative density of the various layers of iron composing the specimen. Thesymmetrical arrangement of curved lines, which is so noticeable, is due evidently to the hammering of the round section of the axle to a square section in the process of forging the end of the axle down to the size of the test specimen. While the tests show the iron of the axle to have been of excellent quality, the most significant fact developed is that concerning the amount of distortion which such an axle will withstand without taking a permanent set. It would at first sight appear impossible that by loads applied at the journals a common car axle could be deflected at its center as much as a third of an inch without exceeding its elastic limit, but an analysis of the data given will fully justify such a conclusion. The results show also that a deflection of the axle well within the elastic limit of the material may be sufficient to produce a tem- porary change of gauge in the wheels mounted upon it of quite three-tenths (0.3) of an inch. Fig. 1. Tests of a Wrought Iron Car Axle. \ MM’ Aw Taaie. ‘GF “TESTING ? Fig. 2. Fig.2. Tests of a Wrought Iron Car Axle. eee P48 «ceene PAP ie 90000 80000 70000 ce) 40000 LOAD IN POUND Sar 30000 WT aa FLECTION IN|INCHES. ae Lae as ee ie GL de tC nec. 1.0 20000 10000 Fig. 3. Tests of a Wrought Iron Car Axle. (92) 93 Fig. 4. Fig. 4. Tests of a Wrought Iron Car Axle. Fig. 5. Car Axle. SUBDIVISION OF PoweER. By J. J. #LATHER. While economy in the use of power should be secondary to increased output, yet careful attention to details will often greatly reduce the useless waste of power. Tt is well known among engineers that there is a very great percentage of loss - due to shaft friction, which, in shops where the buildings are more or less scat- tered, is probably not far from 75 per cent. of the total power used. In two cases known to the writer these losses are 80 and 93 per cent. respectively. No matter how well a long line of shafting may have been erected, it soon loses its alignment, and the power necessary to rotate it is increased. In machine shops with a line of main shafting running down the center of a room, connected by short belts with innumerable countershafts on either side, often by more than one belt, and, as frequently happens, also connected to one or more auxiliary shafts which drive other countershaits, we can see why the power required to drive this shafting should be so large. o4 There is no doubt, however, that a large percentage of the power now spent in overcoming the friction of shafting in ordinary practice could be made avail- able for useful work if much of the present cumbrous lines of shafting were removed. Manufacturers are realizing the enormous loss of power which ensues from the present system of transmission, and we find a general tendency to introduce different methods by which a part of this loss will be obviated. Among these are the introduction of hollow and lighter shafting; higher speeds and lighter pulleys; roller bearings in shaft hangers; and the total or partial elimination of the shafting. Independent motors are often employed to drive sections of shafting and isolated machines, and among these we find steam engines, electric motors, gas engines and compressed air motors, although the latter have not been used for this purpose to any extent in this country. For the average machine shop, short lengths of light shafting may be em- ployed to good advantage, and the various machines, arranged in groups, may be driven from one motor. By this method fewer motors are required and each may be so proportioned to the average load that it may be run most of the time at its maximum efficiency. When short lengths of shatting are employed the alignment of any section is very little affected by local settling of beams or columns, and since a relatively small amount of power is transmitted by each section, the shaft may be reduced in size, thus decreasing the friction loss. Moreover, with this arrangement, as also with the independent motor, the machinery may often be placed to better advantage, in order to suit a given process of manufacture; shaits may be placed at any angle without the usual complicated and often un- satisfactory devices; setting-up room may be provided in any suitable location as required without carrying long lines of shafting through space. This is an im- portant consideration, for not only is the running expense reduced thereby but the clear head room thus obtained free from all shafting, belts, ropes, pulleys and other transmitting devices, can be more easily utilized for hoists and cranes, which have so largely come to be recognized as essential to economical manufacture. There is also less liability of interruption to manufacture on account of the subdivision of power, and, in case of overtime, it is not necessary to operate the whole works with its usual heavy load of transmitting machinery. _ Another advantage is the adaptability of the system to changes and exten- sion; new motors may always be added without affecting any already in opera- tion, and the ease with which this system lends itself to varying the speed of different unit groups is a very potent factor in its favor. 95 In the choice of motors for this work the steam engine has heretofore been used, especially where the units are relatively large. An interesting example of this is noted in the sugar refinery of Claus Spreckles, in Philadelphia, in which there are some seventy-five Westinghouse engines about the works, many of them being of 75 and 100 horse-power. A similar subdivided plant involving forty-two engines was erected several years ago at the print works of the Dunnell Company, Pawtucket, R. I. More recently, however, the electric motor has superseded the steam engine for this work, as its economy and convenience over the latter is now thoroughly recognized. For isolated machines and for heavy machines that may be in occasional use the electric motor is particularly well adapted as a source of power, for such a means of transmission consumes power only when the machine is in operation. This is true also of compressed air, and we find numerous instances where it has entirely replaced steam even in large work. Thus, at the steel works at Terni, Italy, a 100-ton hammer is worked by compressed air, and also two large cranes, one having a capacity of 100-tons and the other 150 tons. Compressed air in some cases is also superseding steam for operating pumping machinery. In Paris, according to Prof. Unwin, compressed air motors are even used to drive dynamos for electric lighting. At some of the newspaper offices there are motors of 50 and 100 horse-power driving presses, and in shops and factories these motors are used to run lathes, saws and various other machines. In the transmission of air, within reasonable limits, the loss in transmission need not be considered, for although there is a slight loss in pressure due to the frictional resistances of the pipes, yet there is a corresponding increase in vol- ume due to fall in temperature, so that the loss is practically inappreciable. In the compression of air, with steam actuated compressors, there are various sources of loss, which, in the aggregate, will vary from 25 to 45 per cent. of the total power of the machine. The greatest loss of efficiency is that inthe air motor. It is usually imprac- ticable to reheat the air with any degree of economy when employed intermit- tently, and we find very generally that the air is used at normal temperature for the various purposes to which it is applied. Insmall motors (1 to 2 horse-power) the loss may be as much as 65 per cent. when the air is used without expansion. With larger motors (75 horse-power), using a reheater and hot air jackets, the motor loss has been kept within 20 per cent. at full load. These results and others would indicate that compressed air as now used is not at all efficient as a source of motive power, since the combined efficiency of compressor and motor, even under favorable conditions, is not more than 50 per 96 cent. of the available energy put into the compressor. In other cases the effici- ency is as low as 20 per cent. There should be no comparison between the cost of the transmission of power by compressed air and its so-called rival, electricity, since each has its own field of usefulness, yet it may be interesting to note for our present purposes the effici- ency of electric transmission. A modern generator, belted from an engine, will have an efficiency of about 90 per cent. when working under favorable conditions, but as the average load is ordinarily not more than two-thirds full load, and often much less, the efficiency will not usually be more than 85 per cent. Since the engine friction was added to the losses in compression, so also it should be considered here, in which case the efficiency of generation will lie between 75 and 80 per cent. With a pressure of 220 volts, which is very suitable for ordinary shop transmissions when both light and power are to be taken off the same line, the loss in transmission need not be more than 5 per cent. so that the efficiency at the motor terminals will not be far from 75 per cent. With motors running under a nearly constant full load the efficiency of motor may be 90 per cent., but with fluctuating loads this may fall to 60 per cent. at quarter load. In numerous tests made by the writer the average load on several motors in machine shops was only about one-third of the rated capacity of the motor. It is interesting to note that in recent tests made at the Baldwin Locomotive Works it was found that with a total motor capacity aggregating 200 horse-power, a generator of only 100 horse-power was sufficient to furnish the current, and ordinarily only 80 horse-power was required. Under these conditions when the driven machines are not greatly over- motored we may assume a motor efficiency of 80 per cent., which may be less or greater in individual cases. The combined efficiency, then, of generator and motor working intermittently with fluctuating loads will be about 75 x 80=60 per cent. of the power delivered to the engine. For greater distances than those which obtain in plants of this character the loss in transmission will be greater, and higher voltage must be employed in order to keep down the line loss; while it is possible to put in conductors suffi- ciently large to carry the current with any assumed loss, yet the cost of the line soon becomes prohibitive with low voltage. In work of this kind it is well to remember that while the efficiency may be very high the economy may be very poor, and good engineering is primarily a question of good economy, all things considered. It is not the most efficient plant which produces the greatest economy. While it is interesting to know that a certain amount of power may , 97 be transmitted a given distance with a high efficiency, it is more important to know that the same amount of power could be obtained at the objective point for one-fourth the cost of the former. Lafayette, Ind., Dec. 30, 1896. EconoMyY IN THE DESIGN OF ELEcTRO-MaGneEts. By W. E. GoLpsBorouGH. Published in the Electrical World, Vol. XXIX, p. 196, Feb. 6, 1897. An EFFICIENCY SURFACE FOR THE PELTON Motor. By W. K. Harr. Published in the Journal of the Franklin Institute, June, 1897. On SeEicues. By A. W. DurFr. Some EXPERIMENTS ON THE PHENOMENA OF THE ELEVATION OF THE ELASTIC Limit. By W. K. Hart. Viscosity AS A FUNCTION OF TEMPERATURE. By A. W. DUFF. [Abstract.] The author shows the insufficiency of the formule proposed by Poisenille, Slotte, Koch, Griitz and others, and finds generalized formule. tta\n pO Sa \ — Ca “8 ra(3+t) J which are in agreement with all data hitherto obtained, the former applying to water and most substances of slow variation of viscosity, and the latter to glycer- ine, mercury and most substances of rapid variation of viscosity. 98 COMPARISON OF CLARK AND Weston CELis. By S. N. Tayuor. A great deal of work of very excellent character has been done upon the Latimer Clark Standard Cell by Prof. Glazebrook, Prof. Carhart, Prof. Kahle, Lord Rayleigh and others, and by them the merit of the cell has been well estab- lished. It has been shown by them that the cell can be made so that, under favorable conditions, it will vary in E. M. F. less than one part in a thousand, even when made by different persons and of materials obtained from various sources. It has also been shown that with proper care the cell maintains its potential indefinitely, and forms a very excellent standard of electro-motive force, which is both moder- ately portable and cheap. It is well known, however, that this standard of potential has at least one very serious drawback, namely, it has a very large temperature coefficient, and the E. M. F. of the cell varies considerably for slight changes in temperature. Moreover the coefficient may not be the same for different cells, or may be differ- ent at different temperatures eyen in the same cell, if the temperatures considered are not near together. Therefore the coefficient for any cell can be exactly de- termined only by experiment on that particular cell, and must be ascertained for all ranges of temperature to which the cell is likely to be exposed. It is also true that changes in temperature in the cell can not be detected easily and accurately, and hence arises some doubt as to the actual E. M. F. of a Clark cell at any particular instant. Methods have been proposed for obviating this difficulty, but for want of space we must omit them here. It goes withont saying, however, that if we could find another cell having the same excellencies as the Clark in all respects, and not having this defect in temperature coefficient, it would be a decided advantage. The Cadmium cell, recently invented by Mr. Edward Weston, has attracted considerable attention, and so far as our observations go, it possesses these very qualifications. For the past three years we have spent considerable time in test- ing the merits of this cell as compared with the Clark Standard Cell. To do this we made a number of Clark cells according to the latest instruc- tions given by the English Board of Trade, as found in the Philosophical Trans- actions for 1892. We also made a number of Weston cells similar to the Clark, except that in the Cadmium or Weston cells Cadmium and Cadmium-Sulphate took the place of the Zine and Zinc-Sulphate of the Clark. 99 Groups of cells were made at various times, and tests made upon them. We mention the group set up during March, 1895, as typical of all the Cadmium cells. They were of the H form (see Fig. 1) and constructed as follows: ae ORs eee Pit ach Baer Teper eee Ho ATOM At A there is a quantity of Cadmium Amalgam about one centimeter deep, and covering the platinum wire, the negative terminal. Above this, at B, there is a concentrated solution of Cadmium Sulphate (CdSO,) containing crystals of Cadmium Sulphate. At E there is pure mercury covering the platinum wire which serves as a positive terminal. Above the mercury, at D, there is a thick paste of Mercurous Sulphate (Hg,SO,), reaching as high as the cross tube. The remainder of the space, CC up to the corks FF, is filled with a solution of Cad- mium Sulphate. The tubes are then sealed above the corks in the usual manner by marine glue or some other form of cement. I can not describe here the manner in which these materials were prepared, but can only refer those interested in the subject to a dissertation which I am about to publish concerning my investigations at Clark University. Suffice it to say that the mercury used was some which I had purified a short time before by means of chemicals and distillation in vacuo; 100 and the other materials were bought of Eimer & Amend as being chemically pure. The cells are easily made, and can be set up by anyone without much trouble. The method adopted for comparing these cells one with another was a modi- fication of the potentiometer method used by Professor Kahle, and was as follows: Fig. 2. The current from a single storage cell 4 { Fig. 2) passes through an ordinary resistance box B! and through a wire resistance R made of German silver, with sliding contact capable of continuous variation for fine adjustment. At the mer- cury commutator J the circuit is divided. The first branch passes through B, then through the wire ¢ back through d and M to the storage cell A. The second branch of the circuit passes successively from M through the transfer switch S, the variable resistance R!, the sensitive galvanometer G, back again to S, and thence through Wto M. The resistance box B was made especially for this pur- pose and consists of seven coils of wire, having the resistances of 10, 15, 50, 100, 300 and 500 ohms approximately. These dip into a dish of kerosene, so that their temperature can be measured more readily. C is a German silver wire 1,122 mms. long, stretched tightly over a boxwood meter bar. The resistances of both 101 B and ¢ have been very accurately measured in international ohms and their tem- perature coefficients determined. JW is a standard cell, either a Clark or a Weston, and is connected in opposition to the storage cell A. As the current then passes from A, if the resistance in B is properly adjusted, the E. M. F. of W will just counterbalance the potential around the B-branch and there will be no de- flection of the galvanometer G when the key K is closed. But increasing the re- sistance in B, if A is constant, has the same effect upon the potential around the B-branch as decreasing the resistance in R would have. Hence we may choose any resistance in the B branch that we may wish, and yet regulate the potential about that branch by properly adjusting the resistance in R. This being true, let B denote the total resistance of the B-branch, including c and d; let ¢ denote the resistance of the wire a 6b; let Ey denote the E. M. F. of the standard cell W and E. the potential about the wire a, orc. Then, when the resistance in B' and R are so adjusted that we get no deflection of the galvanometer G when K is closed, we have the proportion: B:C:: Ew: Ee Knowing the resistance ¢ of ab and that of the total B-branch, of course we know the potential about c. ‘Again, since the potential between any two points p gq be- tween a 6 increases directly as the resistance included between them, and since the resistance increases directly as the distance between the points, we can find any portion of the potential E. by measuring off on the meter bar the appropriate length along the wire ad. Another portion of the potentiometer consists of a third branch circuit including two standard cells W, and W, which are to be compared. For short we shall call this branch the N-branch. It starts from a movable contact p on the wire ab and leads to the reversing commutator N, thence through W, and W, to S through the galvanometer G back again through N to q, another movable contact onab. p and q are knife-edged contacts and can be placed at any position along the wire a b and the distance between them measured by means of the meter rod. The two cells W, and W,, which are to be compared, are now placed in this branch in opposition to each other. If, then, the E. M. F. of W, is exactly equal to that of W,, that is if E, — E., and if p and ¢ are placed close together upon C, then there will be no deflection of the galvanometer G when K is closed. If, however, E, is greater than E, we can find two points upon C such that the difference in potential between p and q shall exactly equal the difference between E, and E, and in opposite directions. The potentials in the N-branch will then be at equilibrium, and there will be no deflection of the galvanometer. In other 8 102 words, we thus measure the difference between E, and E, in terms of the stand- ard cell W. This is expressed by the formula 8, —nP© at Where Ey = E. M. F. of the cell W; E, = E. M. F. of the cell W,; E, = the E. M. F. of the cell W, n= number of millimeters between p and q ] = total length of the wire ad in millimeters c = resistance of the wire ab B = total resistance of the B-branch Bet = IB or the constant of the wire ab. The resistance of 2! consists of a few coils of wire varying in resistance from zero to fifty thousand ohms, but their actual resistance need not be known. Neither is it necessary to know the resistance at B' and R, nor that of the galva- nometer G, since the method of no deflection is used. Care was always taken, however, never to close the circuit through the galvanometer without including a high resistance at R', unless it was first known that the system was almost ex- actly at equilibrium. For it is important that as little current as possible shall be allowed to pass through the cells. But when the system has been carefully ad- justed, the resistance of R' can be gradually cut out, so as to utilize the full sensi- tiveness of the galvanometer. Measurements made by means of this apparatus were limited in accuracy only by the galvanometer’s sensitiveness. For by taking the resistance in B large enough we can make & as small as we please. Thus we found that we were able to detect differences in E. M. F. as small as three one- millionths (,59é500) of a volt with a considerable degree of certainty. One difficulty which we had to overcome was the change in position of the galvanometer’s zero, caused by the passing of electric street cars some four hun- dred feet distant. It was found necessary to make the final measurements be- tween 12:30 and 5:30 a. M., when the cars were not running. Measurements made at various times upon a number of Clark and Weston cells are given in the following table: 108 g°¢ + 8M jie + 3M PST + PM Pees ROM GHEE A) NGO Gale eae eel lnnatterslniasvenll csc vicniareeaiell sletiars + atiesaeell| dates sat peter a "9 TOGO), OpRUL sTToD A, Fea eae seu Saueen e DL Aa Slaw ePepel Beh LON | Gat ak Alene ener eed shit es ces Pecado a *00°0Z "90°61 eGo 00°02 Zo’ 0% "00°61 "000% "8.6L "080'8I “dN, “9681 “C681 “C6SI “H68I “68I “G68I “C68I “C681 “C6gI aieva : = -AYNSVa “6B ABW | “CZ"900 | ‘zDeUNe | ‘gttady | “Tudy | ‘opady | ‘eg -aeyy ‘SE IRW | ‘OL AVW || ao ea “SLTOA °29°0% NT SITHO NOLSUM ANV WUYVTO 10° "WA AO SNOILVIAVA ‘TON ATA Vi 104 From this table it will be noticed that-when the Cadmium cells are first set up they differ somewhat in KE. M. F. But after about a month they come to have a normal value which is common to all. Moreover, this value is not affected by any moderate change in temperature, and so far as our experience goes, these cells are more easily made, and there is less variation in E. M. F. between them than there is between the Clark cells. It will be noticed that the values given in Table No. | are simply relative, but we have made absolute determination of their E. M. F., and find for the Wes- ton cell the value 1 0185! volts when the resistance is measured in Legal ohms; or 1.015633 volts when the resistance is measured in International ohms. The result of our investigations lead to the following conclusions : First. That the Cadmium cell is more easily constructed than the Clark cell. Second. That it has practically no temperature coefficient. Third. That the E. M. F. of the Cadmium cell is even less variable than that of the Latimer Clark. | Sor SoLvENTS FoR AVAILABLE PoTASH AND PHospHoRIC AciIpD. By H. A. Huston AND J. M. BArReErr. It seems to be accepted that in the case of worn soils solution in strong min- eral acid gives little insight into the availability of their potash and phosphoric acid. More recently the use of dilute organic acids, such as the one per cent. cit- ric acid used br Dr. Bernard Dyer! and the acid ammonium oxalate used by Dr. A. M. Peter’, has been tried with more promising results. The theory of the use of dilute organic acid solutions seems to rest on the idea that plant roots give off fluids containing organic acids which act on the soil in a degree comparable with the effect of the dilute acids employed in the laboratory experiments. While I do not question that plant roots in contact with polished marble, or even granite, may make appreciable markings on the carbonate of lime and on the feldspar of the granite, the conditions of the experiment, as usually conducted, differ radically from those found in the field, for in the experiment the plants are not supplied with normal soil water. So far as I have obseryed, normal soil waters give an alkaline reaction. No inconsiderable part of the food of the plants comes to it dissolved in the soil waters. The work of Dr. H. J. Wheeler* shows what marked difficulty is encountered in growing plants on a well-drained soil haying an acid reaction. 105 Soil waters rising from a subsoil are charged with more or less of mineral salts; and if the upper layers of the soil have a different composition from the lower layers in which the soil waters have been charged, we may expect chemical changes to take place according to the well established facts of soil absorption. In view of these considerations some work was undertaken with alkaline solvents. The first solution used contained the same amount of ammonium oxa- late as the solution used by Dr. Peter; but instead of the acid an amount of ammonia equivalent to the acid was added. All work is based on the same rela- tive quantities of soil and solution as used by Dr. Peter—200 grams soil and 1,000 ce solution. In working with Dyer’s solution the digestions continued at room temperature for seven days, with shaking at frequent intervals. All the other digestions were continued for five hours, with constant shaking in the apparatus described in Indiana Agricultural Experiment Station Bulletin 55, and Wiley’s Principles and Practice of Agricultural Analysis, Volume II, page 142. The flasks were inverted every thirty seconds. The utmost care was used to secure clean precipitates of potassium platinic chlorid. THE SOILS USED. The Kentucky soils are those used for work by the Association of Official Agricultural Chemists for the past two years, and are described on page 31 of Bulletin 47, Chemical Division United States Department of Agriculture. Briefly stated, the soil requires the addition of potash to produce satisfactory crops of corn, potatoes and tobacco, but seems to contain enough available potash for a good wheat crop. The field tests indicate abundance of available phosphoric acid. Soil No. 1 has received phosphoric acid and nitrogen, and Soil No. 2 has received potash and nitrogen. Of the Indiana soils the one marked ‘‘ Turley” is from Orange County. It is a medium clay resting on a red clay, which in turn rests on the limestone rock of the region. The land has been under cultivation for some seventy years, and at one time was so badly worn as to be considered of very little value. The sample was drawn after plowing for corn in the spring of 1896. In 1895 wheat had been so poor on this land that hogs were turned in to eat the standing crop. In the spring of 1896 the clover was so uneven that the land was put in corn, of which it pro- duced in this very favorable year for corn, thirty-seven bushels per acre on the unfertilized plats. The owner does not believe that it can produce a profitable crop of wheat without the use of some commercial fertilizer or manure. The usual application has been one hundred pounds ground bone per acre. The field tests this year showed marked gain in corn from the use of acid phosphate and 106 potash, but increasing the amount of potash from thirty to sixty pounds per acre gave no increased yield. Original timber, oak. The soil marked ‘‘Campbell” is from Monroe County, and represents a cold, badly drained clay, resembling the so-called ‘‘crawfish” clay. Commercial fertil- izers are considered necessary for wheat. Field tests this year showed marked gains on corn from the use of acid phosphate and potash, but increasing the amount of potash from thirty to sixty pounds per acre gave no increased yield. Original timber, poplar and mixed hard woods. The station land is a second-bottom soil, resting on gravel. It is a dark, pro- ductive loam. In favorable seasons the land will produce fifty bushels of corn and thirty bushels of wheat per acre without the use of fertilizers or manure. While commercial fertilizers have some effect in increasing the crops, the use of them on this land has not been profitable. Original timber: Black walnut, oak, maple, wild cherry and some hickory. The plats from which the samples were drawn have been in wheat since 1888. Plats 3 E. 1 and 3 E. 4 have received no fertilizers; plat 3 E. 2 has ‘received ‘‘complete”’ chemical fertilization, and plat 3 E. 5 has received applications of barnyard manure. In five years (1890 to 1894), 3 E. 1 lost to crop 8.1 pounds phosporic acid, 11.3 pounds potash, and 17.8 pounds nitrogen; plat 3 E. 4 lost 7.2 pounds phosphoric acid, 10.1 pounds potash, and 15.9 pounds nitrogen; plat 3 E. 2 lost net 0.8 pounds phosphoric acid, 3.2 pounds potash, and 7.9 pounds nitrogen; plat 3 E. 5 gained 4.2 pounds phosporic acid, 6.9 pounds potash, and 0.3 pounds nitrogen. The plats contain one-tenth acre each. Plat 3 E. 4, a blank plat, contains humus (by Huston’s method) *5.3 per cent., and nitrogen in this humus 4.52 per cent. Plat 3 E. 5, which has received barnyard manure, contains humus 5.6 per cent., and nitrogen in this humus 5.71 per cent. The mechanical analyses of the Indiana soils are shown in Table I. TABLE I. Z| | 2 a SOURCE. Babee | Og | ix 3 Sl S jee Sauls 1 Sai Go. te PSG a ae % | % % Air eyiie tet a He) oa Se een he ciate 0.25 | 0.16 7.05 | 39.82 | 47.64 | 5.31 160.23 Campbell --ee.: --- oe 1.57 | 67 | 12.23 | 45.02 | 35.21 | 5.68 | 99.78 Station 3 E.4......................-] 156 | 256 | 13.95 | 35.42 | 36.54 9.94 99.97 107 Since Peter’s solution and the alkaline ammonium oxalate contain a salt of ammonia, it was thought that the phenomena of soil absorption might come into play. To test this, a solution of the same alkalinity, but containing the samé amount of ammonia as chloride as was contained in the other solutions in the form of oxalate, was used. To test the question of soil absorption pure and simple, a neutral solution of ammonium chlorid, 17.2 grams to the liter, the same amount of ammonium chlorid as in the previous solution was used. The soils were also digested with ammonium hydrate, sp. gr. 0.96, containing 17.2 grams ammonium chlorid per liter, and with ammonium hydrate, sp. gr. 0.96 alone. Ammonium hydrate was tried, because, as I have previously shown’, phosphates of iron and alumina are dissolved by ammonium hydrate. At first we hoped to utilize the ammonia and ammonium chlorid mixture, but in the presence of the ammonium chlorid not a trace of phosphoric acid was dissolved. On the Kentucky soils a number of solvents were tried at a higher tempera- ture. This modification seemed no improvement—rather the reverse ; and it was decided to use room temperature. Table II contains the results of the work. The total potash in each soil, and the amount of potash and phosphoric acid removed by hydrochloric acid, sp. gr. 1,115, are also added for the purpose of comparison : 108 ILF | Se0°%} 0080 | 0 F600" | PELO” 7A UY lhe eel Laat) ¢gs0" | 8S80" | 0 LtF | SS6T| 9810" | 0 OOLO’ | GLLO" WAG 0 GPEO" | 6EE0" | 0 OLF | 918°T) 6S20° | 0 F600" | POLO ee celle 0 P9EO | SZFO" | O OS | 896'T| 9410" | 0 GROO | SBTO" 1G ecoinaig 0 8rd" | 0640" | 0 €8G | 868°T} 8810" | 0 9800° | OSLO" Ne al GLO’ | SclO" | 0 pGe" | LEG) 820" | 0 GELO" | TOTO" QSOieeege 0 [S10 | 4200° | 0 zor |etoo" | gr00" |p fee Too" |e Dore fereees[ereres PLS | PAS ZW AS] MU Pe Ne oI mop [oon 0 fo ten ie ore | ogetl onto [oo ba one edttid Teh [oe QO [ce feee|oce p 3 > > = | ip Ne, ae 5 5 are Bs i=} ~ eh = 5 ee Pon idplet, | eis Wy CME ISS, WEE, NW Sitey s°|eO| se | 5/75/82 BEB | SS! 4 ref fe pe oe =. = ou | IR | ror | on | Se wi} SF) eB | os) mst | ge ee |eris5| Fo | d-|sa Pigatlesney eel Se Ey ee | Seliger Pee S | one eo |e bre fe & £ ar | ¢ | | | | | | O9L0" 6920" 6110" GOZO" S810" Z8L0" 8600" 6 FBO" 8ST0" GLL0 g viluoumMy | 19 *d e (SIZ 0g ‘*durey, mooy ) (‘say ¢ !*dmey, wOOY ) “TH HI LWT T Uy eplyoTyy "MY suRID ZT 1680" 1S00° 8180" 9100" 8630" 6E00" 1620" £100" 6920" COLO OORO" 9600" PSE0" | SIZ" 0 0 6180" | 98TO" 0 0 6080" | S810" 0 0 Tgs0" | LLT0" 0 0 LG60° | GSTO" 0 0 8660" | 220° 0 0 0200" | $z00" 0 0 8120" | LEO" ) 0 | | | i! (say ¢ :‘duey, ULOOY ) 19}JV AA OWT] T Poly “Wy smBLy ZL VE AMAL I os 1uo0urm ploy yy ‘uly sure. (s1y{ ¢ :*duey, mooy ) 960) ul 9 “Ig ‘dg & ul 9 L3G0" 1900" 8660" £100" POEO" 8500" 100" €800° S600" 8000" S100° SPLO’ ¥ (‘siy{ ¢ ‘dures, BIdow UL | mooy) 96°0 "1 "dS Tg00" 0 SOTO" 0 9610" 0 (SIH St 9 HO]G “Wy eUlTeyTy || 0G9) ep 800° LZ00° CE LO" C610" E410" G20" | (say ¢ $9 099) OFBTBXQ “UY oUlTEXTY | Il WIaViL S100" €100° 0020" G90’ S810" Z6PRO" (SIAL 0 .¢9) WoIyNTOY s,1939g be ¢ PLEO" 6LEO" CCIO’ | SL60" OFLO’ | LERO OSLO" | PSZ0" 9S10° | 08S" OSLO” | FPZO" LSLO’ | &SS0° 1910" | 320" 9100" | £080" 6920" | OLEO" SZ00" | Leo G800° | STOO" Lc00° | $F L0" PRO’ | S810" GOTO" | 9LL0° 9220" | GSTO" SELO" | 8z90" > ae) eet lat oe ee | BS Be | en Be | oe BF He. Ko] (=) 7 =) ee (al ian) S = = Es) ®}| 8 i=} (SIH ¢ 8920" 6 100° 920" B00" 890)" €S00" L960" LEOO PRG $100" *(sAuq dwey, wooy) ploy 8 1dA(T dT %T worynyoy Se ) sara ies ‘Om ered LOZ tay aie ‘ & : "O%d J CN Eas sOLULOYO | “OT ie seehye ees rand YUR[q [oT & :NOILYLG LNANINAAX GY 20: oe bcishae! Sas aa gerne 9 5 BL age Sotelo er chee Aegan Aotany, Oty [ON-€ ‘ON sQtq cs e°ON-T ON OP cecereeyte eee Fok “O%d | -O.41U pus plow ssoyd TON OM \ UOSOAVIU puw Ysujzod eon > AMONGNYY “ATdANVS AO HOUNOS 109 It will be seen that Dyer’s solution and Peter’s solution resemble each other in a general way in their action on the phosphates of the Kentucky soil (rich in phosphates) and on the Turley soil (poor in phosphates); while on the Campbell land (poor in phosphates), and on the station land (fairly good in phosphates) they differ radically. In their action on potash the two solutions differ widely in the case of the Kentucky soils containing too little available potash for corn, while they resemble each other in their action on the other soils, which seem from field tests with corn to contain considerably higher available potash than the Kentucky soils. Dyer’s solution extracts more phosphoric acid from the Kentucky soil that had received phosphoric acid than from the one receiving none. From the station soil it extracts the highest phosphoric acid from the soil that had received superphos- phate; but it failed to extract as much phosphoric acid from the soil receiving its phosphoric acid in the form of manure as it extracted from either of the plats that had received no fertilizers. On the average, Dyer’s solution extracts no more phosphoric acid from the station soils known to contain a fair supply of available phosphoric acid than from the clay soils known to be very deficient in phosphoric acid. Dyer’s solution dissolves more potash from the Kentucky soil that had re- ceived potash than from the one not receiving any. From the clay soils, which seem from field tests with corn to be somewhat deficient in available potash, it dissolves relatively high amounts of potash. From the station soils it dissolved no more potash from the soil that had received full applications of muriate of potash than from the soils that had received no potash. Peter’s solution would indicate that there was a good supply of available phosphoric acid in the Campbell soil, where it is known to be deficient. It would also indicate that the Turley land was higher in available potash than the station soil, although the field tests indicate to the contrary. The acid solutions of Dyer and Peter seem to fail when applied to soils of different types, although their indications are in the right direction when applied to soils of exactly the same type, such as the Kentucky soils. The alkaline ammonium oxalate dissolves practically as much potash from the Kentucky soil as from the station soil, although the available potash is much higher in the latter, as shown by field tests. tO = it dissolves about the same amount of phosphoric acid from the Kentucky soil as from the station soil, both of which have a fair amount of available phos- phoric acid, although the former has a much higher total phosphoric acid con- tent. It distinguishes these soils very sharply from the clay soils known to be deficient in phosphoric acid. The alkaline ammonium chlorid distinguishes the fertilized from the unfertil- ized plats very sharply on the station soil and to a fair extent on the Kentucky soil. Its action on the clay lands is in accord with what knowledge we have in regard to the potash in these soils. The ammonium chlorid dissolved in ammonia, sp. gr. 0.96, gives results on potash in the same general direction as the mildly alkaline ammonium chlorid, but the differences are less sharply defined. As this solution is rather troublesome to work with, I would prefer to use the mildly alkaline one. The neutral ammonium chlorid distinguishes very well the Kentucky soil from the station soil, gives fair indications on the clay soils, but fails to show the effect of the potash salts applied to the station soil. Ammonium hydrate, sp. gr. 0.96, gives results on potash that are quite at variance with what is known about these soils, but on phosphoric acid it gives promising results. The character of the individual results indicates that the digestion was not continued long enough to complete the reaction. Yet the results clearly distinguished the lands poor in phosphoric acid from those known to be ‘well supplied with available phosphoric acid. The only case where it seems at fault is on plat 1 of the station soil. But every other solvent acts in the same way, indicating that the sample from this plat is really higher in phosphoric acid than the sample from the other blank plat, No. 4. Crop tests covering five years show that plat 1 has a crop-producing capacity about 15 per cent. greater than plat 4. Ammonium chlorid in neutral and alkaline solution removes notable quan- tities of lime from soils. The quantities were determined and are given in Table III. 111 TABLE III. PER CENT. OF CALCIUM OXID REMOVED BY VARIOUS SOLVENTS. Z aS oe eee ‘) | (>) | was fee (eee) oe ot ee ee Cs mo | ice wi “OSs SOURCE OF SAMPLE. A Be | Sg ees Safa) sg28a| Ovs aHod | Pod | Me =——“_—~_ =—~_—-~ S= ~ | a | a | | | | 6 ESS CSS a Oe ee her 0: b445 ib. © ONS / 0.51 | 6 BRB AN Or Bditin 7 fk vuniote baat eens Gah Ses 5 122 196 ol BRE Le Vt iaraiays Dtiags IONS Ae etal oa the Se enchal oie eee .066 By A eae yer PENCNE, ect ero ha we Foes weaken ak day .114 a Lo ae Berea te PbAOTN SRT: Les ce Sproat Miels kre. aca = «ee aE .096 oSLGT4 | Sasetacee SOI IESS a a ieee eee Par ie | .089 | a aoe ees ort SURRMNEM SENT Era Forage eas banal mame d Po ge eae 113 | .226 447 CIS AS SS Dole name ee eee ey ae | 105 227 A472 It will be seen that the alkaline ammonium chlorid removes about one-fourth and neutral ammonium chlorid about one-half as much lime as the hydrochloric acid used in the customary method of soil analysis. The station soils are prac- tically free from carbonates, containing an average of only 0.015 per cent. of carbon dioxid. Of the solvents used we consider alkaline ammonium chlorid and neutral ammonium chlorid promising for available potash, and ammonium hydrate prom- ising for available phosphoric acid. Alkaline ammonium oxalate seems to do very well for available phosphoric acid in some cases, but the material is rather troublesome to work with on account of the large amount of organic matter that goes into solution. Where ammonium chlorid is present the solutions are nearly free from organic matter, filter very rapidly, and the ignition is readily made, leaving only a small amount of bases to be removed before determining the potash. Tatlock’s method was tried for potash, but proved unsatisfactory. We have tried chlorids of calcium, magnesium, and sodium, but prefer to use the ammonium salt, since it introduces no involatile base which would interfere with the potash determination. We are now at work with ammonium hydrate, continuing the digestion for a longer time and changing the strength of the solution. We are also testing am- monium chlorid dissolved in 1 per cent. hydrochloric acid. We shall also test 112 the question of the relative quantities of the soil and solvents used as the present amcunts—200 grams soil to 1 liter of solvent—seems to involve too small a vol- ume of solvent. While we feel encouraged by the outcome of the work reported above, it must be borne in mind that before any method of soil testing can be con- sidered satisfactory, it must give reliable indications on soils of different types that have been subjected to investigation by field tests; and these tests must not be confined to one crop, but must relate to all the crops likely to be produced on the land under investigation. From data now at hand it seems probable that certain soils may have ample potash in an available form to produce good crops of cereals, while not having enough to produce profitable crops of corn, potatoes, or tobacco. This phase of the matter must be kept in mind in deciding upon any definite amount of soluble ingredients which shall be used as a minimum in judg- ing of the fertilizer needs of a soil. Purdue Agricultural Experiment Station, November, 1896. (1) Jour. Chem. Soc., London, March, 1894. This paper contains a resume of suggestions by various authors and special investigations by Dr. Dyer. (2) Chem. Div. U. S. Dept. Agr., Bull. 47, p. 32. (3) Rhode Island Agr. Exp. Sta., 7th Ann. Rpt., p. 152. (4) Chem. Div. U.S. Dept. Agr., Bull. 38, p. 84; Wiley’s Agr. Analysis, vol. 1, p- 326. (5) Chem. Div. U.S. Dept. Agr., Bull. 31, p. 99. (6) Determined by Harry Snyder. See Bull. 47, U. S. Dept. Agr., Chem. Div., p- 49. ACTION OF AMMONIUM CITRATE AND Citric Acrip on Basic Sitac. By H. A. Huston anp W. J. JONES, JR. [ ABSTRACT. | This is a continuation of the work carried on for several years by the authors under the general head of the availability of commercial phosphates. This paper deals with the two most prominent materials proposed for determining the ayail- ability of the phosphoric acid in the slag. The factors controlling the action of the reagents are discussed under the following heads: I. Influence of time of digestion. II. Influence of temperature. IlJ. Influence of acid (citric) ard alkali (ammonia). IV. Influence of quantity of slag used. 113 V. Action of citric acid on slag. Amount of acid neutralized in times ranging from one-half to five hours, at 25° C and at 65° C. Amount of phosphoric acid remain- ing in solution at the end of these periods. The phosphoric acid in solution decreases with a rise in temperature and with an increase in time. VI. Comparison of the U. S. official method with the method proposed by Dr. Paul Wagner, including special molybdate and magnesia solu- tions. The paper will be found in complete form in Bul. 49, Chem. Div. U.S. Dept. Agr., p. 68-72. Laboratory State Chemist of Indiana, Purdue Univ., Nov., 1896. THE CHARACTER OF THE VOLATILE Matrer Lost spy Birumrnous Coals AT 100° C. By W. E. Burk. The conditions accompanying the common method of determining moisture in coal suggested a study of the nature and amount of volatile matter given off at the temperature of determination. The work was done on two classes of Indiana coals, one high in moisture, the other considerably lower, the operation consisting in passing the volatile products from the coal heated approximately to 100° C, together with a current of dry air over copper oxide in a combustion furnace, absorbing the moisture coming over with calcium chloride, and carbon dioxide arising from combustion of any vola~ tile hydrocarbons in a caustic potash solution. A hard glass combustion tube was used, which extended some 20 c. m. froni the forward end of the furnace. This portion of the tube was jacketed with a glass sleeve with rubber plugs, and arranged with entrance and exit openings through which a continuous current of steam was passed. By this means a tem- perature approximating 100° C was maintained through the forward-part of the tube in which a weighed quantity of powdered coal was placed in an aluminum boat. A slow current of dry air was passed, and the heating of coal and com- bustion of volatile products maintained for one hour. The boat was then removed and the absorption bulbs weighed, after which they were attached again and the tube heated for a further twenty to thirty minutes. The boat containing coal was weighed in a glass enclosing tube, and after the operation was allowed to cool in 114 same tube and under similar conditions, thereby preventing any reabsorption of moisture while cooling. Determinations were made on from one to three grams of coal, giving reste of which the following are fair examples: ‘ - Wei revere . | Carbon Found ee tageR. of Coal at 100°C. | ofEachTabe, | Moisture, | From 0H | 1.4217 gr. | 1994 | 2014 14.00% 048% 1.1195 “ 1596 1625 14.25% 058% 3.1079 2111 | 2113 6.78% 022% 3.2356 “ 2152 2142 6.65% 025% 2.9408 * 1967 1967 6.65% 037% The gain in weight of the calcium chloride tube corresponds with a slight difference to the loss in weight of the coal, giving per cent. of moisture, which agreed very well with separate determination of moisture in the same coals by the ordinary method of heating for one hour in a toluene bath, results being slightly higher, due perhaps to current of air passing over coal, removing moisture more completely. The gain in weight of the caleium chloride tube exceeded the loss in weight of the coal more than what would arise from the combustion 6f any volatile hydrocarbons present, as indicated by carbon found and calculated as methane. This excess of water found may indicate presence of free hydrogen, but a correct explanation of its presence, as well as of the source of carbon found, can not be made without an accompanying analysis of the gases given off from the coal at 100° C, as the small percentage of carbonic oxide, carbon dioxide and hydro- carbon volatilized at 100° varies widely with different coals. The per cent. of volatile hydrocarbons given off in these experiments —.0299% to .077%—calculat- ing as methane, is probably higher than occurs in the regular determination of moisture because of the air current, while on the other hand the somewhat lower temperature of these experiments would tend to modify the difference. As in no case, however, does the loss of volatile matter other than water nearly reach one- tenth of one per cent., the error in calculating the same as moisture is of no prac- tical importance. Notres ON DIPHENYLSELENON AND SELENTHREN. By Ropert Lyon. Notes on L— anp B— Lupanin. By SHERMAN .DAVIS. THE PuHysioLoGicAL ACTION OF CoMPOUNDS CONTAINING BIVALENT CARBON, By Jie Ua NER: THE CALCULATION OF THE HEATING EFFECT OF COALS FROM THE PROXIMATE ANALYsis. By W. A. Noyes. So far as I am aware, no satisfactory formula has ever been given for the cal- culation of the heating effect of coals from the amounts of fixed carbon, volatile combustible matter and sulphur present. It has been generally assumed that the amount of oxygen in coals varies so greatly that no rational basis for such a cal- culation could exist. During the spring of 1895, Mr. J. R. McTaggart and Mr. H. W. Caver made careful analyses and determined the heating effect with Hem- pel’s calorimetre, for six Indiana coals. Recently I have had the opportunity of examining similar analyses and calorimetric tests of fifteen Pittsburgh coals, made under the direction of Prof. N. W. Ford, of the University of Ohio, In the analyses as given, the amount of oxygen in these coals appears to vary between quite wide limits. On subtracting from the total oxygen the oxygen present in the form of water, however, it was found that the average amount of oxygen of combustiWe matter was 7.72 per cent. for the Indiana coals and 8.05* for the Pittsburgh coals, or a general average of 7.96 per cent. and a maximum devi- ation from that average of 1.23 per cent. In only one coal is the difference from the mean more than one per cent. Since the per cent. of hydrogen in these coals is subject to only a slight variation, it follows that the combustible matters present in all of these coals so far as they consist of carbon, hydrogen and oxygen, have a nearly constant com- position. There should, therefore, be a nearly constant factor for this total com- bustible matter. In order to calculate this factor for the coals in question it hag been assumed that one-half of the sulphur is found in the volatile combustible matter as calculated from the difference between total volatile matter and water, and that the fixed carbon is given with sufficient accuracy by subtracting the ash from the coke. In other words, the combustible matter was formed for the pur- poses of this calculation by subtracting from 100 the per cents. of water and ash *In calculating this result Professor Ford’s figures for oxygen were corrected by adding three-eighths of the weight of sulphurs, on the supposition that iron pyrites in the coal ig burned to ferric oxide in the ash. See Jour. Am. Ch. Soc. XVII. 116 and one-half of the per cent. of sulphur. When the heating effect, as found in the calorimetre (calculated on the basis of the fuel burned and vapors of water at 100° C.) was divided by this per cent. of combustible matter it was found that one gram of combustible matter gives, on the average, for the Indiana coals 8073 calories and for the Pittsburgh coals 8078 calories. We may, therefore, give the following empirical rule for the calculation of the heating effect of coals: Find the combustible matter by subtracting from 100 the per cents. of water and ash and one-half of the per cent. of sulphur, and multiply this re- mainder by 80.7. The result will give the heating effect of the fuel burned to liquid water. For the twenty-one coals referred to, the heating effect calculated by this rule shows a maximum deviation from the calorimetre test of two and one-fourth per cent., while the agreement is in most cases, much closer than that. It would not be safe to apply this rule to coals known to be of very different origin or character, until a similar comparison of calorimetre results with the analysis has heen made for such coals. NOTES ON THE Fiora oF LAKE Cicott AND LAKE MAXINKucKEE. By Rospert HEsSLER. ‘The following notes on the flora of the region surrounding Lakes Cicott and “Maxinkuckee are offered as a contribution toward a complete flora of Indiana; they are based on personal observations made during the period beginning with August, 1894, and ending with December, 1896. Longcliff, just west of Logansport, has been the basis of operation, so to speak, and this locality has been examined most fully. 1 thought it best, therefore, to make mention of the noteworthy plants found here, although the flora does not differ materially from that common to the central part of the State. It is the usual glacial drift flora, with beech as the most common forest tree. The region about the lakes is in marked contrast. The upland soil is made up of a fine sand which contains only the merest trace of lime, and with oak as the prevailing tree. The lowlands in places are wet or swampy. Tamarack swamps and peat bogs occur here and there, but are nowhere of great extent. It is, perhaps, unnecessary to state that the wet northern portion of Indiana is being drained more and more every year, and the land, exceedingly fertile, brought under cultivation. The completion of the Kankakee drainage system will, in time. be followed by numerous minor systems, and in the course of a few years the 117 ‘Marsh Flora,” if we may so call it, will have disappeared from Indiana. A\l- ready many of the plants, once common, are rare and restricted to isolated areas ; the natural habitat being destroyed, the extermination of plants naturally follows. In my own numerous excursions [ have, in many instances, been unable to find more than one or two specimens of certain species after three seasons of close search. The reports of other observers in different parts of the State show a sim- ilar result. Even now the swamps and bogs mentioned in this paper are being ditched and drained, and in a very short time the last vestiges of a once common flora will have disappeared. The flora of the uplands, with, perhaps, a few exceptions, is in no immediate danger of extinction. It will be many years before the comparatively barren oak flats and oak ridges will be brought under cultivation, and even then species will continue to lead a more or less precarious existence in waste places and along fence rows. Species with showy flowers, or those that are useful, are among the first to disappear; this being especially true of the flora of lakes visited by sum- mer tourists. A few remarks on the location and general surroundings of the chief localities embraced in this paper will render unnecessary in the notes extended references to localities, which would otherwise be frequent. For instance, ‘‘Swamp east of Lake Cicott” refers to one definite locality, as described below. Lake Crcorr is located near the western border of Cass County, about eight miles west of Logansport. At present it is an oval body of water less than half a mile in length, east to west. Formerly it was much larger, with an irregular shore line. The north and south banks are high, even bluffy; those on the east and west low and flat. There is no outlet, but in the event of high water the ex- cess would drain into Crooked Creek, a mile to the east. The recession of the water has been in the west, and this portion is now dry and covered by a dense growth of weeds, chiefly ragweed and smartweeds. The water is very clear and contains few aquatics. The soil of the neighborhood is sandy, a fine-grained eolian sand with little lime, and with a vegetation characteristic to such soils, chiefly oak, with an entire absence cf beech. The country is gently rolling, be- coming level to the west and north. The railroad station at the lake is Cicott, also spelled Ciecott. Swamp East oF Lake Crcort is situated about one mile due east of the lake, and marks approximately the boundary between the sandy lands on the west and the glacial drift soils on the east. At present it is reduced to a few acres, and is being rapidly encroached upon by drainage, and will soon cease to be. The number of rare species found in it is remarkable; some were seen nowhere else. 9 118 LAKE MAXINKUCKEE. This well-known lake, several miles in length, is located in the southwest corner of Marshall County, about thirty-five miles north of Logansport. The soil in the vicinity is sandy, especially in the uplands. The most interesting butanical localities are along the low marshy southern extremity, and, unless otherwise indicated, my references are to this part. TAMARACK Swamp, SoutH OF DELONG, is located in the extreme northwest corner of Fulton County, within half a mile of the station on the Michigan Divi- sion of the Vandalia Railroad, and a few miles south of Lake Maxinkuckee. It has an irregular outline, is narrow in places and contains several hundred acres. In the center is the remains of an old lake, now almost covered over by a mass of ericads and peat moss. The whole region has recently been ditched, the ditch in places passing through peat four feet in thickness. This drainage is an example of what is going on all over northern Indiana. TAMARACK Swamp, East oF MONTERAY, is several miles west of the last named swamp, and just east of the little town of Monteray, in Pulaski County, It covers less than fifty acres, but is very dense, and also contains the remains of a lake. Sanpy Lanp, West oF LOGANSPORT, is interesting, botanically. It begins abruptly at Kenneth, three miles west of Logansport, in the form of a triangle, widening from a narrow point to a mile or more, and gradually fading or disap- pearing at Logansport. Geologically it is a limestone ridge covered with wind- blown sand in a glacial region. At the western extremity it rises abruptly, as already indicated, and is more or less bluffy on the sides, especially on the south, fronting the Wabash River. From a height of about forty feet at the angle, it gradually declines to the east and finally merges into the ordinary ‘second bottom’ soil of the valley. The sandy covering, that is, the soil, is deep on the north and very thin on the south, the underlying rock being bare in places. The Western portion is covered with a thin oak wood; the remainder is in cultivation. Cer- tain species occurring here plentifully are either absent in the other localities or oceur sparingly. THE WasaAsH River at Logansport, and for many miles below, has its bed eroded in the limestone; the bluffs in places are perpendicular and often twenty- five feet high . the bottom is of solid rock, sandbars being few and small. The periodical high water washes out everything before it, and, therefore, plants usually found on the sandy banks of rivers are notably absent. Localities other than the above are referred to b¥ name or descriptively under the proper species. Where no locality is given the species is general. 119 In regard to species included and excluded, the list is limited as follows: (a.) To phanerograms or flowering plants. (b.) Plants new to Indiana, /. e., plants not given in Coulter’s Catalogue of the Plants of Indiana. ‘e.) Plants rare in Indiana, or locally distributed, according to the above catalogue. (d.) Plants noteworthy for some particular reason. (e.) Excluded species are those common throughout the State and which may be seen at any time. At the suggestion of Prof. Stanley Coulter, however, some species have been mentioned on account of their rarity or absence, an ab- sence well marked to one accustomed to note the plants about him. The nomenclature is that of the sixth edition of Gray’s Manual, as at present used by the State Biological Survey. For the benefit of the reader not familiar with the botanical names the common English names have been added. Specimens of species mentioned, unless common in other parts of the State, are in my herbarium. A set comprising those new to the State, and a number of the rarer ones, has been presented to the Biological Survey. In case of doubt as to the identity of a species, critical comparisons were made with the specimens in the herbarium of Purdue University. My thanks are due to Prof. Stanley Coulter for his kind assistance in making comparisons and in determining several species which were in leaf only. Anemone Pennsylvanica L. General but nowhere abundant. Anemonella thalictroides Spach. Rue Anemone. Common in sandy soils west and north, rare in drift soils. Thalictrum polygamum Muhl. Tall Meadow Rue. Seen occasionally in wet soils about the lakes. Ranunculus multyidus, var. terrestris, G. Two plants only found in a dried-up pool on the western border of Lake Maxinkuckee. None of the leaves were fili- form. Ranunculus sceleratus L. Cursed Crowfoot. Frequent in the brooks about Logansport; not seen at the lakes. Isopyrum biternatum T. and G, Plentiful in- beech woods, rare in sandy soil woods. Caltha palustris L. Marsh Marigold. Frequent in wet places. Coptis trifolia Salisb. Goldthread. Common in one small locality, tamarack swamp at DeLong; does not occur at Lake Cicott. No other notes. Caulophyllum thalictroides Michx. Blue Cohosh. Rare in drift. 120 Jeffersonia diphylla Pers. Twin-leaf. Not seen; absent. Brasenia peltata Pursh. Water-shield. Common in Lake Cicott; no notes on other localities. Nelumbo lutea Pers. Water Chinguapin. Absent. Nymphea reniformis 1D). C. White Water Lily. Lakes, ponds and slow streams; common. Nuphar advena Ait. Yellow Pond Lily. With the last, plentiful. Sarracenia purpurea L. Pitcher Plant. Common in tamarack swamps around Lake Maxinkuckee. Not seen at Lake Cicott. Corydalis flavula D.C. Plentiful about Logansport in all soils. Arabis hirsuta Scop. Frequent along the banks of the Wabash. Plants smoothish; stems clustered. Not given in Coulter’s catalogue. | Arabis dentata T. & G. Frequent on dry limestone cliffs and in hilly drift. Erysimum asperum D, C. Western Wall Flower. Common on a few lime- stone cliffs west of Logansport. Sisymbrium eanescens Nutt. Tansy Mustard. Very common in the sandy lands west of Logansport, not seen in other localities. Polanisva graveolens Raf. Noticeably absent irom the banks of the Wabash River, and not seen anywhere. Helianthemum Conadense Michx. Frost-weed. Frequent in dry, sandy soils about the lakes. Lechea major Michx. Pinweed. Seen in two localities only, and here plenti- ful; one at Lake Cicott, in moist, sandy ground; the other east of Monterey. Lechea minor L. A few plants seen near Lake Cicott; one locality. Viola pedata L. , Bird-foot Violet. Plentiful on sand ridges at Lake Cicott. Solea concolor Ging. Green Violet. Rare, on limestone, west of Logansport. Cerastium arvense Var. oblongifolium H. & B. Common in the Wabash Valley. Hypericum prolificum L. Shrubby St. John’s Wort. Rarely seen; east of Lake Cicott only. Hypericum cistifolium Lam. In several places; wet limestone ledges on the Wabash; plentiful where it does occur. Geranium Carolinianum L. A weed along the railroads. Xanthoxylum Americanum Mill. Prickly Ash. Frequent in drift. Tlex verticillata G. Winter Berry. Frequent about the lakes. Nemopanthes fascicularis Raf. Frequent in tamarack swamps at DeLong; not seen anywhere else. Rhamnus lanceolata Pursh. A few bushes on the limestone outcrops west of Logansport. 121 Ceanothus Americanus L. New Jersey Tea. Common everywhere in dry, up- land, sandy soils; not seen in drift. Vitis Labrusea L. Fox Grape. Rare; about the lakes. Negundo aceroidesM. Box Elder. In drift soils, rare. Rhus venenata D. C. Poison Tree. Poisin Dog-wood. Excessively common about DeLong in tamarack swamps and peat bogs. Not seen at Lake Cicott. Its presence in a swamp acts as an effectual barrier to the entrance of many persons, especially those readily susceptible to its noxious influence. Many persons proof against the common Poison Ivy readily succumb to this species. Rhus Canadensis Marsh. Fragrant Sumach. Very common and forming thickets in the thin, sandy soils west of Logansport and in the limestone ledges. Rarely seen in other localities. Polygala Senega L. Seneca Snakeroot. Common in sandy soils east of Lake Cicott; more or less general in sand soils, but nowhere common. Polygala sanguinea L. Rarely seen, in moist alluvial soils at lakes. Polygala cruciata L. A few plants in one locality only, a moist place south- east of Lake Cicott. Lupinus perennis L. Wild Lupine. Common about the lakes. Psoralea onobrychis Nutt. Rare, in sandy soils. Amorpha canescens Nutt. Lead Plant. Seen occasionally at Lake Cicott. No notes on its occurrence in other localities. Petalostemon violaceus M. Rare; in sandy soils. Petalostemon candidus M. With the last and rare. Tephrosia Virginiana Pers. Goat’s Rue. Lake regions; rare. Astragalus Canadensis L. Along the west shore of Lake Maxinkuckee; not rare. Desmodium canescens D. C. In sandy soils. Lespedeza violacea Pers. Common in sandy soils west of Logansport; also oc- casional in other places. Lespedeza reticulata Pers. Sandy woods of lake regions; frequent. Lespedeza capitata M. With the last and common. Lespedeza angustifolia Ell. A single large, bushy plant was found along the railroad east of Lake Cicott; perhaps a migrant. Vicia Caroliniana Walt. Sandy soils about the lakes; frequent. Several other species, belonging apparently to the Viciew group, were found in leaf only, and on account of their uncertain identity are here excluded. Apios tuberosa M. Absent. 122 Gymnocladus Canadensis Lam. Coffeenut Tree. Seen occasionally in drift soils at Logansport: trees often large. Prunus Americava Mar. Wild Plum. Rare. Prunus Virginiana L. Choke Cherry. Limestone bluffs; rare. Spiraea salicifolia L. Common Meadow Sweet. Common in wet situations about the lakes. Spireae tomentosa L. Hardhack. Steeple-bush. With the last, but rare. Spiraea lobata Jacq. Queen of the Prairie. With the preceding. Physocarpus opulifolius Maxim. Nine-bark. Rare; along Crooked Creek. Potentilla Norvegica L. A weed in cultivated ground; common in drift. Potentilla fruticosa L. Shrubby Cinquefoil. In a few places near the lakes, and here common. Pyrus arbutifolia Var. melanocarpa Hook. Choke-berry. Frequent in low lands at the lakes. Amelanchier Canadensis T. & G. Service-berry. Generally distributed, but rare. Amelanchier Canadensis Var. oblongifolia T. & G. Dwarf June-berry. On limestone cliffs of the Wabash; not rare. Sazifraga Pennsylvanica L. Meadow Saxifrage. Frequent in wet places. Parnassia Caroliniana Michx. Abundant in many wet places. Ribes floridum L’Her. Wild Black Currant. Seen occasionally in wet woods near Logansport. Drosera species. Although a very close search was made for species of Dros- era, not a single plant was found. Hamamelis Virginiana L. Witch-hazel. None seen. Liquidamber Styraciflua L. Sweet Gum. Seems to be absent. Myriophylium. No notes. Lythrum alatum Pursh. Loosestrife. Common near the water’s edge Lake Cicott; less common at Lake Maxinkuckee; moist places along the Wabash. Decodon verticillatus Ell. Swamp Loosestrife. I have no specimens and no notes on its occurrence, but at this writing (December, 1896) believe it occurs in at least one wet place near Lake Cicott. I may add, parenthetically, that it oc- curs plentifully at Turkey Lake, in the northeast portion of Kosciusko County. Epilobium angustifolium L. Great Willow Herb. A single large specimen of this handsome plant was found on the edge of the Tamarack Swamp at DeLong. Not in Coulter’s Catalogue. Heracleum lanatum Michx. Cow-Parsnip. Moist places about Lake Cicott ; not rare. 123 Eryngium yuecaefolium Michx. Rattlesnake Master. Frequent about the lakes, especially Lake Cicott. Aralia racemosa L. Spikenard. In drift soils; rare. Viburnum acerifolium L. Dockmackie. Common in sandy soils. Triosteum perfoliatum L. Horse Gentian. Rare. Triosteum angustifolium L. Common in sandy soils. (Besides these well-marked forms there occur, especially in the sandy soils west of Logansport, specimens that partake of the characters of both. Ina large collection all stages of transition of one to the other may be seen. Are possibly hybrids. ) ; Houstonia caerulea L. Bluets. Only two plants were found, one of which was in bloom, on the grassy edge of a thin sandy woods, about one mile south of Lake Cicott. The leaves are very hairy. i Houstonia purpurea L. A narrow-leaved form is common in the sandy lands west of Logansport; also seen about the lakes. Galium boreale L. Northern Bedstraw. - Noticed in three localities. Common in the swamp east of Lake Cicott and also common on the southern edge of Lake Maxinkuckee; rare on the wet limestone ledges just west of Logansport, on the Wabash. The occurrence in Cass County greatly extends its southern range in Indiana, according to Prof. S. Coulter. Valeriana edulis Nutt. Common in a wet meadow on the southeast edge of Lake Maxinkuckee and inthe swamp east of Lake Cicott, seen nowhere else. This species is not reported in Coulter’s Catalogue. Valerianeila radiata Dufr. According to my notes, occurs along the railroad east of Cicott, but I can not vouch for its identity ; no specimens preserved. Eupatorium sesilifolium L. Upland Boneset. Occasional in sandy lands west of Logansport. Liatris scariosa Willd. Frequent in dry sandy soil. Liatris spicata Willd. Common in wet situations. Grindelia squarrosa Dunal. Appearing along the railroads. Solidago latifolia L. Broad-leaved Goldenrod. Rare. Solidago uliginosa Nutt. Wet places. Solidago speciosa Nutt. Rare; in sandy lands west of Logansport and in the neighborhood of Lake Cicott; not seen elsewhere. This showy species is not re- ported in Coulter’s Catalogue of the Plants of Indiana. Solidago patula Muh!. Common in wet places. Solidago rugosa Mill. Collected at Lake Maxinkuckee in the fall of 1894, No notes. 124 Solidago ulmifolia Muh]. Common in thin woods, sandy lands west of Logans- port. Solidago arguta Ait. With the last, rare. Solidago serotina Ait. Collected at Lake Maxinkuckee. No notes. Solidago nemoralis Ait. Frequent in dry places at Lake Cicott. Solidago radula Nutt. Collected at Lake Maxinkuckee. Sohdago rigida L. Some large plants at Cicott; frequent. Solidago Ridellii Fr. Common in wet places. Solidago lanceolata L. Common. Solidago tenuifolia Pursh. At Lake Cicott; rare. (Besides the above several Solidagos of doubtful identity were collected in different localities. Where no locality is given in the list the species occurs gen- erally. These remarks also apply to the Asters. Asters are not represented as well as the Solidagos. ) Aster Nove-Anglie L. Common in wet places. Aster azureus Lindl. Wet meadow east of Cicott. Aster cordifolius L. Frequent. Aster laevis L. Frequent. Aster umbellatus Mill. Very tall and common in a wet place east of the Ken- neth Stone Quarries, west of Logansport; rare at Lake Maxinkuckee. Aster linariifolius L. Occurs sparingly on the southern high, dry, sandy bank of Lake Cicott; not found elsewhere. Silphium terebinthinaceum L. Frequent; open, sandy soils. Silphium laciniatum L. The Rosin-weed was not seen by me, but a friend brought me some leaves from the extreme northwest corner of Cass County; is re- ported common on the prairies to the northwest. Silphium int-grifolium Michx. Frequent about Lake Cicott. Parthenium integrifolium L. Very rare; a few plants south of Cicott. Ambrosia psilostachya D.C. Seen in leaf only; along the Vandalia Railroad at Marmont; evidently a migrant. Not in Coulter’s Catalogue. Echinacea purpurea Moench. Purple Cone-Flower. Generally distributed, but not common. Rudbeckia subtomentosa Pursh. About Lake Cicott; rare. Lepachys pinnata T. & G. General, but rare. Helianthus occidentalis Rid. In dry places, Lake Cicott ; rare. Helianthus divaricatus L. Sandy woods west of Logansport; rare. Coreopsis palmata Nutt. High south bank, Lake Cicott; rare. Coreopsis tripteris L. Sandy woods; common. 125 Dysodia chrysanthemoides Lag. Along the railroad at Cicott; evidently a migrant. Not seen elsewhere. Artemisia caudata Michx. High, sandy bank, Lake Cicott; rare; a few plants only. Not seen elsewhere. Cacalia atriplicifolia L. Dry, sandy soil, along the railroad, east of Lake Cicott ; possibly a migrant. Cacalia tuberosa Nutt. Tuberous Indian Plantain. Swamp east of Lake Cicott only, and here common. Cnicus arvensis Hoffm. Canada Thistle. Noticed a small patch at Logans- port by the side of the railroads; is a migrant. Prenanthes racemosa Michx. East of Cicott; rare. Not in Coulter’s Cata- logue, but reported since then. Lactuea scariola L. Prickly Lettuce. This rank weed is excessively common along the railroads, and is rapidly spreading. Lobelia cardinalis L. Not seen; if present at all, is certainly rare. (Common at Turkey Lake, in Kosciusko County.) Lobelia spicata Lam. Frequent in dry, sandy soils. Lobelia Kalmvi L. Not rare in wet places. Campanula rotundifolia L. Var. Arctica. Harebell. Common in crevices in limestone bluffs on the Wabash; frequent on high banks of Lake Maxinkuckee. Not seen at Lake Cicott. Gaylussacia resinosa T. & G. Black Huckleberry. Common in open, sandy woods about the lakes. Vaccinium Pennsylvanicum Lam. Dwarf Blueberry. Seen in one locality, a thin, sandy woods south of Lake Cicott. Doubtless occurs in other localities. Vaceinium corymbosum L. Common or Swamp Blueberry. Common in swamps in sandy regions; not found in drift soil. Vaccinium macrocarpon Ait. Cranberry. Common in open places in the tamarack swamps and peat bogs south of Lake Maxinkuckee. Not at Lake Cicott. According to the accounts of old settlers, very large cranberry bogs ex- isted when the country was first occupied. The bogs or marshes now existing are small and are rapidly disappearing. Epigaea repens L. Arbutus. Not seen. Gaultheria procumbens L. Wintergreen. Frequent in low, damp woods about the lakes. Andromeda polifolia LL. With the Cranberry and Pitcher-Plant, in peat bogs chiefly; common where it does occur. Not in Coulter’s catalogue. Cassandra calyculata. Don. Leather-Leaf. With the last; common. 126 Monotropa uniflora L. Indian Pipe. Rare; east of Lake Cicott. Monotropa Hypopitys L. Pine-sap. Rare; with the last. (No other members of the Heath family were seen. ) Dodecatheon Meadia L. Shooting-Star. A few plants in a wet meadow east of Cicott. Not seen in other localities. Trientalis Americana Pursh. Star-Flower. In tamarack swamps; common where it does occur. Steironema ciliatum Rat. General, but nowhere abundant. Steironema longifolium G. In swamps; common. Lysimachia stricta Ait. Plentiful in a small swamp south of Lake Cicott; no notes on its occurrence elsewhere. ; Apocynum androsaemifolium L. Spreading Dogbane. General in sandy soils, and common along the railroads. Apocynum cannabinum L. Indian Hemp. Not as frequent as the last. Asclepias verticillata L. About the lakes; rare. Acerates longifolia Ell. On the high, sandy, south bank Lake Cicott. Sabbatia angularis Pursh. This handsome plant is common on the moist, sandy shores of Lake Cicott, and was not seen in any other locality. Gentiana crinita Froel. Fringed Gentian. General in wet places, but not common. Gentiana quinqueflora Lam. Not seen. Gentiana Andrewsti Grisb. Closed Gentian. Rare; in moist woods. Gentiana alba Muhl. A single plant in seed found in the summer of 1895 east of Lake Cicott. Frasera Carolinensis Walt. American Columbo. A score or so of plants oc- cur in the dry, sandy woods west of Logansport; not seen elsewhere. Menyanthes trifoliata L. Buckbean. In bogs with the Pitcher-plant and Cran- berry; common here. Phacelia bipinnatijida Michx. In the Wabash Valley about Logansport, on rocky and hilly places; common; very fetid. Phacelia Purshii Buckley. Common in cultivated grounds at Logansport as a weed; this year it bloomed freely in the fields at Longcliff up to November 27, not having been injured by a previous temperature of 22 degrees. Mertensia Virginica D. C. Virginia Cowslip, Bluebells. In two localities in the valley west of Logansport; rare. Lithospermum arvense L. Wheat-thief, Corn Gromwell. A weed common along the railroads, and has taken possession of some fields. Lithospermum hirtum Lehm. Common in sandy soils. 127 Echium vulgare. The Viper’s Bugloss, or Blue-weed. Occurs along the B. & O. Railroad east of Turkey Lake, in Kosciusko County; it will quite likely soon appear in this region. Chelone glabra L. Turtle-head. Frequent in wet places. Pentstemon pubescens Sol. Common in sandy soils. Pentstemon leevigatus Sol. Rare; in drift soils about Logansport. Veronica Anagallis L. Water Speedwell. Rare. Castilleia coccinea Spreng. Painted Cup. About the lakes; rare. Pedicularis lanceolata Michx. Occasionally seen in wet places. Utricularia species. None found in flower and I have no notes on its pres- ence in the waters of this region, although it must certainly be found. I have seen it in Carroll county on the south and in Kosciusko County to the northeast. Tecoma radicans Juss. Trumpet Creeper. Along the railroads. Ruellia ciliosa Pursh. In sandy soils, frequent. Verbena angustifolia Michx. Common in the thin wind-blown, sandy soils, often barely covering the underlying limestone, west of Logansport; also occurs sparingly near the river. Not seen at the lakes. Pycnanthemum lanceolatum Pursh. Mountain Mint. About the lakes, fre- quent. The bruised leaves exhale a strong odor resembling peppermint. Pyenanthemum linifolium Pursh. Common in dry, sandy soils about the lakes. Searcely odorous. Calamintha Nuttallii Gray. On wet limestone ledges along the Wabash River below Logansport; here plentiful. Not seen elsewhere. Not reported in Coul- ter’s Catalogue oi the Plants of Indiana. Scutellaria galericulata L. Sculleap. Frequent near water. Physostegia Virginiana Benth. False Dragon Head. Frequent. Plantago Patagonia. The only species of Plantago observed besides P. major and P. lanceolata was the above, or a variety of it. It grew near a railroad in Logansport. Polygonum sagittatum L. Arrow-leaved Tear-thumb. Occasional in wet places. Direa palustris L. Leather-Wood. Common in low, moist, drift soil, woods near Logansport. I do not remember seeing it in the sandy soils at the lakes. Comandra umbellata Nutt. Bastard Toad-flax. General in dry, sandy soils; common east of Lake Cicott. Euphorbia dentata Michx. Abundant in one locality, at the base of a lime- stone bluff, west of Logansport. Not seen elswhere. 128 Ulmus fulva Michx. Slippery Elm, Red Elm. Is a common forest tree in drift soils, often very large. Betula lenta L. Cherry Birch, Sweet Birch. Occurs sparingly in the tama- rack swamps at Delong, south of Lake Maxinkuckee. Betula pumila L. Low Birch. Not rare about the lakes. No notes on Carya, Quercus or Salix. Coniferw. The only species seen were of Larix and Juniperus; the latter is general, but nowhere abundant. Larix Americana Michx. occurs plentifully in the so-called tamarack swamps, and these are being limited more and more in size and number. Orcuips. A careful search was made for orchids, and the following list gives all the species found : Liparis loeselii Richard. Tway-blade. A few plants on a moist hillside south of Lake Cicott. The plants were past bloom when found, and a dried specimen was compared with those in the herbarium of Purdue University. Spiranthes cernua Richard. Rare; in low, moist woods south of Cicott. Godyera pubescens R. Br. Rattlesnake Plantain. Rare; in woods southeast of Cicott; plants were in leaf only. Calopogon pulchellus R. Br. Common in swamps about the lakes. Pogonia ophioglossoides Nutt. In a peat bog at DeLong; here common. Habenaria bracteata R. Br. Rein-Orchis. A group of three plants found in the thin sandy woods west of Logansport. Habenaria lacera R. Br. Ragged Fringed Orchis. Two plants found in peat bog with Pogonia. Cypripedium pubescens Willd. Large Yellow Lady’s-Slipper. Rare in the woods southeast of Cicott; not seen elsewhere. Cypripedium spectabile Salisb. Showy Lady’s-Slipper. In the low grounds on the southern extremity of Lake Maxinkuckee; rare. Cypripedium acaule Ait. Stemless Lady’s-Slipper. Common in one locality, a small, dense tamarack swamp east of Monterey. Aletris farinosa L. Star Grass. Very rare; in low ground on the edge of a woods south of Cicott. Allium cernuum Roth. Wild Onion. Very common in many places and in all kinds of situations. Tall and showy in the wet meadows and swamps east of Lake Cicott; less showy on moist limestone ledges on the Wabash; small and stunted in crevices of dry limestone west of Logansport. Allium Canadense Kalm. Wild Garlic. Lake Cicott; rare. 129 Camassia Fraseri Torr. Wild Hyacinth. In drift soils in the valley; very rare and almost extinct. Maianthemum Canadense Desf. About Lake Maxinkuckee, plentiful in a few comparatively dry tamarack swamps. Lilium Philadelphicum L. Wild Orange-red Lily, Wood Lily. At the lakes; seldom seen. Lilium Canadense L. Wild Yellow Lily. With the last and rare. Medeola Virginiana L. Not seen. Trillium nivole Rid. Not seen. Yofieldia glutinosa Willd. Swamp east of Lake Cicott; rare. Melanthium Virginicum L. Bunch Flower. Withthe last; rare. Theswamp about one mile east of Lake Cicott, although containing only a few acres, is re- markable for the number of rare species occurring in it. Melanthium and Tofieldia were not seen elsewhere; the former is a tall plant, not readily over- looked, while the latter is quite small. Tradescantia. The form with smooth leaves, few in number, is very common in sandy soils, especially east of Lake Cicott, and bloomsearly in the spring. The form with hairy leaves and blooming later is rare and was seen in drift soils only. Peltandra undulata Raf. A few plants on edge of tamarack swamp, east of Monteray. ; Scheuchzeria palustris L. In one locality only, a peat bog south of DeLong; here plentiful. Not in Coulter’s Catalogue. Potamogetons. No notes. PP. natans is common in the Wabash River, with a narrow-leaved form resembling P. pauciforus. Naias. I do not remember seing any within the region embraced in this paper. (Have seen plants in Turkey Lake, in Kosciusko County.) Cyperacee. Not being familiar with this large order, I have not given it attention; my few notes are not worth reproducing. Panicum clandestinim L. (?) Some large plants, up to four feet in height, with stinging hair, occur in a wet meadow on the edge of a thicket near the old canal, three miles west of Logansport. The specimens taken were not in bloom, and hence the doubt about their identity. Zizania, Water, or Wild Rice. No notes on its occurrence; absent ? Alopecuris geniculatus L. Var. aristatulus, Torr. A few plants found on the dirt, chiefly peat, thrown out in making a ditch through the tamarack swamp south of DeLong. Phragmites communis Trin. A small patch occurs near the southern end of Lake Maxikuckee. Stalks 8 to 12 feet high. 130 NorEes ON SOME PHANEROGAMS NEW OR RARE TO THE STATE. By W. S. BLATCHLEY. At the winter meeting of this Academy in 1889, I presented a paper entitled ‘“Some Plants New to the State List,” in which seven species were mentioned from Monroe County, and fourteen from Vigo County, as not having been previ- ously recorded in any published list of Indiana plants. The paper was severely criticised at the time by one or two members of the Society, the species being said to be wrongly determined or to have been previously mentioned. My ardor for writing botanical papers was somewhat quenched by this criticism, but time has since proved that all identifications, with but a single exception, were correct, and no previous Indiana record for any one of the remaining twenty species has been or can be pointed out. The paper in question was never published, and but four of the plants therein mentioned have been recorded from other portions of the State. This fact, to- gether with the additional one that I have in my note books numerous records of plants taken within the past five years at various localities in the State, which, if published, would greatly extend the known range of such species, has led to the preparation of the present paper. In it the stations and habitat of ninety-three species of Indiana plants are re- corded, and brief notes are in many instances given regarding their abundance, variations, etc. Of these, thirty-three species, including thirteen of those men- tioned in my 1889 paper, have not heretofore been recorded in print as occurring in the State; while thirty-seven have been recorded from but one other station in the State, and that in almost every instance distant from the one in which it has been collected by myself. The remaining twenty-three species have not been recorded from more than two stations in the State and they in localities widely different, as ‘‘Jetferson and Lake counties,” or ‘‘Gibson and Noble counties.” Specimens of all the plants mentioned are in my private herbarium or in that of DePauw University, which, in 1893, came into possession of about 600 species of plants collected by me. Those species represented in the DePauw herbarium are marked with an asterisk in the list which follows. The date given is that upon which the species was collected, or, where collected more than once, the earliest at which it has been noticed in bloom. The nomenclature and arrange- ment are those of the new ‘‘ Catalogue of the Pteridophyta and Spermatophyta of Northeastern North America,” published in 1894 as a memoir of the Torrey Botanical Club. Where the name in the catalogue mentioned differs from that 131 in Gray’s Manual, 6th Ed., the name used in the latter work is given in parenthe- sis as a synonym. if *2 =I Botrychium ternatum obliquum Milde. Grape Fern. Found in a few localities in Vigo county. Distinguished from the other forms of the species by its height, 10 to 14 inches, its more compound fruiting portion, and the oblong divisions of the sterile segment, which are very oblique at the base. Recorded in the State Catalogue from Jefferson county. Equisetum fluviatile L. Swamp Horse-tail. (FE. limosum L.) Found abundantly in the shallow water around the margins of the Goose Pond in Vigo county. Not given in the State Catalogue, nor in any of the published lists, but recorded in Botanical Gazette from Lake County. May 3. Potamogeton diversifolius Raf. Pond-weed. (P. hybridus Michx. ) Frequent in a pond south of Fair Ground, Vigo county. Oct. 3, 1889. The first Indiana record. Potamogeton spirillus Tuckerm. Occurs sparingly in the Five-Mile Pond, Vigo county. July 19. The first record. Zannichellia palustris L. Horned Pond-weed. This species grew in abundance in the pond south of the blast furnace at Terre Haute in the years 1889-93. The surface of this pond seldom froze in winter on account of the warm stream of water from the furnace flowing into it. Since the furnace shut down the pond has dried up and the plant has disappeared. The first record for the State. Echinodorus cordifolius (L.) Griseb. Upright Bur-head. (E. rostratus Engelm. ) Several acres of this plant grew in 1890 on the site of Conover’s Pond, Vigo county, which had been drained the previous year. The first record, its range being given in Gray’s Manual, sixth edition, as ‘‘Tllinois to Florida, Missouri and Texas.” Panicum autumnale Bose. Diffuse Panicum. Frequent in Vigo county, on sandy hillsides and banks along railways. Recorded before by Higley and Raddin from the ‘‘ sand ridges south of Whiting, Ind.” 132 10. "11, The flowers of this grass are, when in their prime, a grayish-purple in color, and, when wet with dew, reflect the morning sunlight in a peculiar and pleasing manner. Panicum minus Muhl. Wood Panicum. A spetimen, so named by Mr. Nash, of Columbia University, N. Y., was taken from a dry hillside in Hipple’s coal mine woods, Vigo county, where it is frequent. The first record. Panicum pubescens Lam. Hairy Panicum. Another species named for me by Mr. Nash. It is frequent along the T. H. & L. Railway in Vigo county. The first record. Homalocenchrus lenticularis (Michx.) Seribn. Catch-fly Grass. ( Leersia lenticularis Michx. ) Taken but once, October 6, 1893, from the margin of Five-Mile Pond, Vigo county. The first record. Sporobolus asper (Michx.) Kunth. Drop-seed grass. Occurs sparingly along sandy banks and hillsides in Vigo county. August 30. The first record. Cyperus spectosus Vahl. Recorded before only from Jefferson county. Taken in low, sandy soil in Vigo county, where it is scarce. Varies much in size. A specimen taken at Heckland, October 14, 1896, had six umbels, the stalk of each apparently springing from the surface of the ground, and the whole plant but 23 inches in height. Eleocharis capitata (L.) R. Br. Spike Rush. Grows along the mucky margins of the Five-Mile Pond, Vigo county. Identification verified by N. L. Britton. Recorded before in ‘ Botanical Gazette,” VII, 3, 1882, by E. J, Hill, from a slough south of Whiting, Ind., and described by him as new under the name of LE. dispar. Itisa plant of southern range, and, up to the time of Hill’s record, it had not been found north of Florida and Texas, except west of the Rocky Mount- ains. It probably occurs in suitable localities throughout the western half of Indiana. 14. 15. *16, ine 18. 19: 133 Stenophyllus capillaris (L.) Britton. (Fimbristylis eapillaris Gray.) Occurs sparingly in Vigo county, along sandy banks and borders of fields. Recorded before from Lake county. Grows in dense, circular tufts; the hair-like stems rarely a foot in hight. Wolfiia columbiana Karst. Found in abundance in the Goose Pond, Vigo county, in 1890. ‘*Stagnant waters in the northern counties.” —State Catalogue. Medeola virginiana L. Indian Cucumber Root. Occurs on high, dry, wooded hills in Monroe county, in company with Microstylis ophioglossoides Nutt. and Lycopodium complanatum L.; scarce. Recorded in B. & C. Flora from Jefferson and Lake counties. Habenaria flava (L.) A. Gray. Greenish Orchis. (H. virescens Spreng. ) Taken in some dense, damp woods near Heckland, Vigo county, June 10, 1891. Recorded before from Noble county. Achroanthes unifolia (Michx.) Raf. Adder’s Tongue Orchis. (Microstylis ophioglossoides Nutt. ) A single specimen was taken at Coal Creek, Vigo county, Sept. 28, 1893. In Monroe county a number of specimens were secured from high hills, where they were found in company with Medeola virginiana L., Pogo- nia verticillata Nutt., and in the midst of clumps of the moss Polytrichum commune L. Specimens taken by the writer in Arkansas were also found on high hills, though the habitat given in Gray’s Manual is ‘‘low, mois ground.” Leptorchis lihifolia (L.) Kuntze. Twayblade. (Liparis hiiifolia Richard. ) Rare in rich woods in both Monroe and Vigo counties. June 11. Leptorchis loeselii (L.) MacM. Twayblade. (Liparis loeselii L. ) A number of specimens were taken in a tamarack swamp in Fulton county, July 14, 1894. Heralectris aphyllus (Nutt.) A. Gray. Taken by the writer on a high wooded hill two miles south of Wyan- dotte Cave, Crawford county, July 25, 1896. 10 134 *99 23. #24, #26. 27. The first Indiana record, the range in both the Manual and I}lustrated Flora being given as ‘‘ Kentucky and Missouri to Florida and Mexico.” Polygonum arifolium L. Halberd-leaved Tear-thumb. Scarce in Vigo county; in ravines and along borders of small streams. Mentioned in my paper ‘‘On Plants New to the State List,” read before the Academy in 1889, Since recorded from Steuben and Noble counties. Polygonum emersum (Michx.) Britton. CE: muhlenbergii Watson. ) Frequent in Vigo county along sandy margins of ponds. Noted be- fore in Steuben and Lake counties. Polygonum ramosissimum Michx. Found in low, sandy ground near a marsh south of the Fair Ground, Vigo county ; scarce. The first record. Chenopodium boscianum Mogq. Taken in Vigo county, October 17, 1896, in open, sandy woods, two miles east of Terre Haute. The first Indiana record. The flowers much smaller than in allied species; on slender recurved branches; the black seeds easily separated from the enclosing pericarp. Arenaria serpyllifolia L. Thyme-leaved Sandwort. Occurs sparingly in Vigo county in low, sandy soil about the margins of several of the larger ponds. Noted in the list of Higley & Raddin as being found in Lake county and by Hesslar (Proc. Ind. Acad., 18938, 269) as occurring in Fayette county. Anemone caroliniana Walt. Carolina Anemone. Found in Vigo county in one locality on a wooded hillside, 53 miles north of Terre Haute. First brought to my notice in 1894 by Miss Nora Arnold, a pupil in the high school. She stated that they had occurred abundantly in the one locality for 12 or thirteen years to her knowledge, and how much longer she did not know. The first record, the Manual range being “ Illinois to Nebraska and Southward.” Ranunculus obtusiusculus Rat. Water Plantain Spearwort. Noted in one locality, the border of a marsh near the Goose Pond, Vigo county, June 22, 1890. Recorded from Noble county by Van Gorder under the name of R. alis- maefolius Geyer. 29. *30. bao Es 34. 39. 135 Ranunculus purshii Richards. (R. multijfidus terrestris Gray.) Occurs sparingly about the borders of the Five-Mile Pond, Vigo County. June l. The first record. Dentaria heterophylla Nutt. Diverse-leaved Toothwort. Occurs sparingly in Monroe county in thickets and rich, moist woods. Recognized as a distinct species in the new Check List. Noted as such in my paper read before the Academy in 1889, though Dr. Coulter in his list of Jefferson County plants stated that it was, in his opinion, a variety of D. laciniata Muhl. In Monroe county it blooms at least two weeks later, and no connect- ing forms were noted. Of a specimen submitted to Dr. Coulter, he wrote: “Tt looks very much like typical D. heterophylia Nutt., and is as near it as anything I have seen from the State.” The first Indiana record. Draba caroliniana Walt. Carolina Whitlow Grass. Frequent in Vigo county along the banks of the old canal and on sandy hillsides near it. One of a MSS. list of additions to State Catalogue furnished me by Dr. J. M. Coulter. Locality not given. Descurainia pinnata (Walt.). Britton. Tansy Mustard. (Disymbrium canescens Nutt. ) Frequent in Vigo county along the gravelly banks of railways and canal. Recorded only from Tippecanoe county. April 20. Arabis dentata T. and G. Toothed Rock-Cress. Rare in Vigo and Monroe counties, along gravelly banks or rocky hill- sides. Recorded before from Gibson county. May 3, 1891. Arabis hirsuta (L.) Scop. Hairy Rock Cress. Found by the writer in Monroe, Montgomery and Vigo counties. Grows along rocky hillsides. Recorded by Van Gorder as being scarce in Noble county. Sedum telephioides Michx. Collected along the hillsides at Coal Creek, Vigo county, by Dr. B. W. Evermann in 1889. April 30. The State Catalogue record is ‘‘ Knobs,” Clark county. 136 *36. a ee) (ve) 40, 41. Parnassia earoliniana Michx. Grass of Parnassus. This species was recorded by Stanley Coulter, Proc. Ind. Acad. Sci., 1894, 105, as being found in Noble and Kosciusko counties, the latter record being based on a specimen collected by the writer, now in DePauw herbarium, It has since been noted by myself at Lake Maxinkuckee, Marshall county, and in a marsh on the banks of White River one mile south of Broad Ripple, Marion county. Opulaster opulifolius (L.) Kuntze. Nine-Bark. ( Physocarpa opulifolia Raf. ) Recorded in the State list from Gibson, Jefferson and Monroe counties. This handsome flowering shrub has been noted by the writer as grow- ing plentifully on the banks of White River below Broad Ripple, Marion county, and on the banks of the Wabash just south of the city of Wabash, Wabash county. It has also been recorded from Wayne and Lake coun- ties, so that its range undoubtedly includes the whole State. Geum macrophyllum Willd. Taken in the borders of rich open woods two miles east of Terre Haute, Vigo county, June 26, 1892. The first Indiana record, Sanguisorba canadensis L. Canadian Burnet. (Poterium canadense Benth. and Hook.) Occurs along the borders of ditches and damp virgin prairies near Heckland, Vigo county. In flower from August 10 to October 20. The first Indiana record, the range of Manual being ‘‘ Newf. to moun- tains of Georgia, west to Michigan.”’ Trijol um reflerum L. Buffalo Clover. Rare in Vigo county, along open sandy hillsides and borders of prairies. Heretofore noted from Marion county. May 28. Amorpha fruticosa L. False Indigo. River Locust. Frequent along the bed and sides of the old canal both north and south of Terre Haute, and as far north as Montezuma, Parke county. Recorded from Gibson. Falcatu pitcheri (T. & G.) Kuntze. Large-leaved Hog Peanut. (Amphicarpea pitcheri T. & G.) Found sparingly along damp hillside thickets in Vigo county. The first Indiana record. Leatlets much larger than in F. comosa L., the blade often more than 3 inches long; pods—ten or more—1} inches long, borne on a long, hairy rachis; seeds, 5 mm. in length. 44, 45, 46. 48. *49, 137 Polygala polygama Walt. Pink Polygala. Vigo county, in small numbers, along the Vandalia Railway, one mile east of Terre Haute. Recorded before from Lake and St. Joseph counties. Euphorbia heterophylla L. Occurs in Vigo county, along the banks of oid canal near Five-Mile Pond. The first Indiana record. The pods of this and allied species, when dry, burst open with a snap- ping or crackling noise, and project the seeds to a distance of several feet. Callitriche heterophylla Pursh. Water Starwort. Vigo county, in ponds; frequent. April 30. Recorded from Gibson county. Rhus aromatica Ait. Fragrant Sumach. (Rhus canadensis Marsh. ) Recorded in the State list from Jefferson and Lake, the two extremes of the State. Taken by the writer in Monroe and Crawford counties. Grows on rocky hillsides along streams. Rhamnus caroliniana Walt. Carolina Buckthorn. A shrub or small tree of southern range which occurs as far north as Crawford and Harrison counties, Indiana, where it was first noted by the writer November 5, 1896. Straggling in habit; 10 to 20 feet high, with peach-like leaves, glossy green above; bark smooth and light colored; the wood bright yellow; fruit, a black drupe resembling a cherry. Hillsides along Blue River near Wyandotte cave, and roadsides between there and Corydon; scarce. The first Indiana record, the Manual range being ‘‘ N. J., Va. to Ky. and southwest.” Hibiscus lasiocarpus Cav. Grows in prairie swamp near Heckland, Vigo county. Recorded before from Gibson. Hibiscus militaris Cay. Halberd-leaved Rose Mallow. Frequent along the sandy banks of old canal between Ft. Harrison, Vigo county, and Montezuma, Parke county. ‘‘ Knobs,” and Jefferson county are the two previous records. July 10. Hypericum aseyron L. Great St. Johnswort. Banks of larger streams in Monroe and Putnam counties; scarce. Mentioned in my 1889 paper. Since recorded from Noble county by Van Gorder. 138 51. 52. *5)5, 57. 58. Hypericum densiflorum Pursh. Found on edge of river bank in woods just below Ft. Harrison, Vigo county, Oct. 12, 1896. The first record for Indiana; the Manual range being ‘‘ Pine barrens of N. J. to glades of Ky., Ark. and southward.” Helianthemum canadense (L.) Michx. Frost-weed; Rock-rose. Vigo county, on a sandy hillside near Five-Mile Pond; frequent locally. May 28. Recorded from the sand hills of Lake county; also from Noble. Viola lanceolata L. Lance-leaved Violet. Margins of Goose Pond and moist prairies at Heckland, Vigo county. April 16. : The previous records are Lake and Jefferson counties. Rotala ramosior (L.) Keehne. Vigo county, in ditches and along margins of ponds; scarce. Jefferson and Clark counties are its previous records. Ammannia coccinea Rottb, Ammannia. (Ammannia latifolia L. Gray’s Manual, 5th ed.) Noted in both Vigo and Monroe counties; scarce in the latter. Aug. 10 to Oct. 20. Recorded from Gibson. Decodon verticillatus (L.) Ell. Swamp Loosestrife. (Nescea verticillata H BK.) Occurs rarely in Monroe, Vigo and Marshall counties. Recorded in State Catalogue from ‘‘Gibson and Posey. Rare.” Re- corded since from Noble and Steuben. It therefore probably occurs in suitable localities throughout the State. (Enothera sinuata L. Vigo county, about the borders of a sandy cultivated field near Ft. Harrison; scarce. May 14, 1891. Probably a railroad migrant from the South, the Manual range being ““N. J. to Fla., west to E. Kansas and Texas.” The first Indiana record. Myrvophyllum verticillatum L. Water Milfoil. Ponds of Vigo County; scarce. May 2. Mentioned without note in the Steuben County Flora. 59. *60. 61. *62. *63. *64. 66. *67. 139 Eulophus americanus Nutt. Borders of damp prairie, near Heckland, Vigo County; scarce. Octo- ber 5, 1889. Recorded from Gibson County. Cornus circinata L’Her. Round-leaved Dogwood. Borders of open, moist woods four miles southeast of Terre Haute; scarce. May 8. Recorded from Lake County. Hypopitys hypopitys (L.) Small. Pine-sap. False Beech-Drops. Found on high, dry wooded hillsides in both Monroe and Vigo coun- ties; rare. A specimen taken in Monroe, June 30, 1886, had the raceme 21 flowered. Recorded from Jefferson and Noble counties. Gentiana andrewsii albiflora Britton. White Gentian. (Gentiana alba Muhl.) Grows in one locality in Vigo county, a wooded hillside north of Terre Haute near the Five-Mile Pond; scarce. September 23, 1888. Tippecanoe and Noble counties are its other State records. Gentiana saponaria L. Soapwort Gentian. Vigo county along the borders of prairies; scarce. September 15. Its previous State record is Lake county. Obolaria virginica L. Collected on several occasions in both Monroe and Vigo counties, but rare ineach. Three plants, taken in doors by Prof. Evermann on Janu- ary 26, bloomed on February 11. Its other State record is Clifty Falls, Jefferson county. Phlox bifida Beck. Dwarf Phlox. In the State Catalogue this species is said to be ‘common in Tippe- canoe.” It has been taken by me in both Vigo and Monroe counties; in the former being very common on the sandy hillsides north of Terre Haute. April 7. HAydrophyllum canadense L. Canada Waterleaf. Noted heretofore from Jefferson and Laporte counties. It occurs also sparingly on the sides of deep wooded ravines in both Monroe and Vigo counties. Macrocalyx nyctelea (L.) Kuntze. Ellisia. (Ellisia nyctelea L.) Rare in Vigo county, having been taken but once from a damp spot in sandy open woods, two miles east of Terre Haute. May 25. The first Indiana record. 140 68. 69. ~i oo 74. Cunila organoides (L.) Britton. Common Dittany. (Cunila mariana L.) Occurs frequently on the summits of dry rocky hills in Monroe county. June 20. Recorded in the State Catalogue from the ‘‘ Knobs.” Synandra hispidula (Michx.) Britton. Large-flowered Mint. (Synandra grandiflora Nutt. ) Taken by the writer in Monroe, Putnam, Vigo and as far north as Wa- bash county, though its range is given in the Barnes & Coulter Flora as ‘*Banks of the Ohio and its tributaries.” May 25. Stachys cordata Riddell. Heart-leaved Hedge Nettle. Borders of damp upiand thickets in Vigo county; scarce. ‘‘ Jefferson and Gibson” are its previous records. Trichostema dichotomum L. Blue Curls. Bastard Pennyroyal. Discovered by Professor Evermann, September 1, 1889, in sandy soil on the banks of the Wabash River south of Terre Haute, Vigo county. A species of southern range, probably introduced in the past by the commerce of the river. Its first Indiana record. Gratiola spherocarpa Ell. Hedge Hyssop. Taken in both Monroe and Vigo counties; scarce. April 30. In the State Catalogue recorded from ‘‘ Barrens of Southern Indiana.” Wulfenia houghtoniana ( Benth.) Greene. (Synthyris houghtoniana Benth. ) Found in one locality on sandy hillside one-half mile southeast of Five- Mile Pond, Vigo county, where it was uncommon. ‘‘Tippecanoe and northward” is the only previous record. Afzelia macrophylla (Nutt.) Kuntze. Mullein Foxglove. (Seymeria macrophylla Nutt. ) On dry hillsides in Montgomery, Putnam and Vigo. ‘“Near the Ohio and Wabash” was recorded in the Barnes and Coulter Flora. Orobanche ludovicana Nutt. Broom-rape. (Aphyllon ludovicianum Gray.) Banks of Wabash River near brick yards above Terre Haute, Vigo county; frequent locally. Parasitic on the roots of the Great Horse-weed, Ambrosia trifida L. Discovered by Prof. Evermann October 2, 1889. The first Indiana record, its Manual range being ‘‘ Minnesota to IIli- nois and Texas.” 76. mio: 80. *81. 141 Plantago aristata Michx. (Plantago patagonica aristata Gray.) Evansville & Terre Haute Railway and canal banks south of Terre Haute, Vigo county; scarce. June 24, 1888. The first record for the State. Viburnum moile Michx. Found along the fence-rows and margins of dry upland prairies below Youngstown, Vigo county; scarce. The leaves larger, more rounded, thicker and more soft and downy than those of V. dentatum L. _ Recorded from Jefferson county. Willoughbya scandens (L.) Kuntze. Climbing Hemp-weed. ( Mikania scandens L. ) A handsome twining member of the Compositae. Found in abundance covering the shrubs growing south of the wagon bridge across Sandy Hook creek, five miles east of Hebron, Porter county, September 21, 1897. Recorded before from Gibson county by Dr. Schneck. Manual range, ““E. New Eng. to Ky. and southward.” Lacinaria spicata (L.) Kuntze. (Liatris spicata Willd. ) Virgin prairies near Heckland, Vigo county; scarce. Aug. 17. Recorded from Jefferson and Lake. Chrysopsis villosa (Pursh) Nutt. Golden Aster. Along the sandy banks of the old canal between Ft. Harrison and Five- Mile Pond, Vigo county. The first record for the State, its range being given as “ Wisconsin to Kentucky and westward.” / Solidago odora Ait. Sweet Golden-rod. Near Heckland, Vigo county, from borders of prairies; rare. Sept. 15. Recorded before only from Gibson county, by Dr. Schneck, who, accord- ing to State Catalogue, ‘‘was inclined to doubt this species.” Dr. J. M. Coulter, to whom my specimen was sent for verification, noted it as ‘‘a good find,” so that it must be rare in the State. It is regarded as a valid species by the authors of the Catalogue of the Flora of Northeastern North America. Solidago rigidiuseula (T. & G.) Porter. (Solidago speciosa angustata T. & G.) Clearings and borders of prairie at Heckland, Vigo county. Sept. 5. The first Indiana record. 142 *82. 84. 85. *87. 88. Solidago serotina Ait. In woods along the borders of the Wabash River below Ft. Harrison, Vigo county; frequent locally. Recorded from Jefferson county. Sept. 8. Solidago speciosa Nutt. Une of the most handsome of the Golden-rods. Grows plentifully in the prairie at Heckland, Vigo county. Aug. 25, The first Indiana record. Euthamia caroliniana (L.) Greene. Slender-leaved Golden-rod. (Solidago tenuifolia Pursh. ) Frequent in Vigo and Monroe counties; along shaded banks, usually in sandy soil. Aug. 21. Noted before from Jasper county. Sericocarpus linifolius (L.) B.S. P. (Sericocarpus solidagineus Nees. ) Borders of prairies at Heckland, Vigo county, where it is scarce. Recorded from Floyd county in B. & C, Flora. Aster drummondii Lindl. Drummond’s Aster. Low open pastures and prairies; frequent in Vigo county. The first record for the State, its range being given by Gray as “Illinois to Minne- sota and Kansas.” Aster ericoides L. Heath-like Aster. Fence rows and old fields, in open, dry soil. Common in Monroe, scarce in Vigo county. Recorded in B. & C, Flora only from Jefferson. Aster linariifolius LL. Double Bristled Aster. On dry, sandy hillside near Five-Mile Pond, Vigo county; scarce. Also near Miller’s, Lake county. Recorded in the State Catalogue from the ‘‘Knobs” under the name of Diplopappus linartifolius Hook. Readily known by the shortness of the stems, which grow in clumps, and by the rigid linear leaves. Heads large and showy. Ambrosia bidentata Michx. Two-toothed Ragweed. Roadsides and borders of cultivated fields between Glen, Vigo county, and Staunton, Clay county; common locally. First noted August 23, 1895. The first record for the State, its Manual range being ‘‘ Prairies of Illinois, Missouri and Southward.” 143 90. Bidens trichosperma (Michx.) Britton. Tickseed Sunflower. (Coreopsis trichosperma Michx.) Occurs sparingly in Monroe county in swamps along the bottom lands of Bean Blossom Creek. August 10, 1886. Recorded in B. & C. Flora from Jefferson county. 91. Hymenopappus caroliniensis (Lam.) Porter. (H. seabiosceus L’ Her. ) Found sparingly on the side of a sandy ridge northeast of Seventh Street Bridge across Lost Creek, Vigo county. May 31, 1890. The first record for the State, its.range being given in the Manual as **Tlinois and Southward.” 92. Senecio lobatus Pers. Butterweed. Taken on several occasions in 1891 and 1892 from low, damp places about ponds and ditches in Vigo county. The first Indiana record, its Manual range being ‘‘ North Carolina to Southern L[llinois, Missouri and Southward.” 93. Lactuea hirsuta Muhl. Hairy Wild Lettuce. (Lactuca sanguinea T. & G.) Borders of prairies and dry, sandy fields in Vigo county; scarce. Recorded from Gibson county by Dr. Schneck. PeErRiopiciry OF Root PrREessuRE. By M. B. THomas. The fact that the roots of plants absorb water and force it up through the stem, producing bleeding whenever the stem is injured, was discovered by Hales in 1721, and since that time numerous investigators have examined this phenom- enon of root absorption in a more or less exhaustive way until we have to con- cern ourselves only with an inquiry iuto its daily variations and see if there is not some law governing the changing phenomenon that will give us a more com- plete insight into this important physiological problem in plant growth. The general matter of the periodicity of root pressure in forcing water through stems in opposition to gravity was studied by Sachs, and his observations form a basis for our present work. He made experiments regarding the time of maxi- mum and minimum pressure with a few common plants, and his results are too well known to need extended description. The conclusions of his experiments have been to fix the time of maximum pressure at 9-11 A. M., with a decrease 144 through the p. M. and early night, when a minimum was reached. After this the pressure increased until it attained the maximum during the following A. M. Sachs further showed that the periods of maximum and minimum pressure were independent of small variations in temperature. The work of Sachs was done by the use of crude instruments that required constant attention, and it seemed that an instrument of precision, making auto- matic records, would enable one to add something to the work already done on the subject of root pressure. In 1890 a rude instrument was made of wood and iron, and some few experiments conducted on the subject. Later a machine of more accurate working was constructed at the college workshop in Crawfordsville, and this formed a pattern for the one made at Lafayette under the supervision of Dr. Arthur. In the evolution of the apparatus to its present condition changes have been introduced that brings the machine into a form easily used by the average student and capable of giving accurate results. For our work on the subject of root pressure many plants were grown from seeds in the greenhouse, and were used when the stems were 4-5 mm. in diameter. With those plants secured from out of doors or at other green houses, they were brought in weeks before the experiments and given ample time to adjust them- selves to any changes in their surroundings. The results show that the latter plants corresponded in their records with those grown in the green house from seeds. For the experiments the attachment of the plant to the machine was made in the usual way under water, and the apparatus placed on an iron pier to prevent jarring. The records of temperature were made by a self-recording ther- mometer. The clock used in the root pressure machine would run for eight days, and an experiment when properly started needed no attention until its comple- tion, or until the time when the pressure was insufficient to show itself on the rods of the instrument. The increasing weight of the column of mercury usually produced this result in 4-5 days. The smoked rods with the record of the peri- odicity were placed on sensitive paper, and the lines printed for permanent pres- ervation. Temperature cards were preserved along with these for comparison. The plants experimented upon were fuchsia, bean, geranium, grape, sunflower, ° tomato, etc. Occasionally upon the attachment of the plant a decided negative pressure in the stem would be observed. This was especially noted in the grapevine growing out of doors, where the records were made. The negative pressure was so great that the water and part of the mercury were pulled down into the stem and the particles of mercury could be found in the ducts upon splitting the twigs an inch or more from the top, where the attachment was made. This phenomenon was * 145 observed by Sachs, and is, no doubt, due to the fact that where active transpira- tion is going on no root pressure exists, but transpiration or other current do not permit the ducts to become filled with water, but, rather, they contain rarified air that allows the water poured in on top of the cut surface to be drawn down in the stem. A study of the records warrant the following general statements regarding the relation between temperature and root pressure: Under usual conditions there can be no relation between the periodicity of root pressure and the daily variations in temperature, the latter being between 50° F. and 90° F., as determ- ined in the course of the experiments. Even where the periods of maximum and minimum temperature were reversed in the test, and the reversed condition con- tinued for several successive days, no appreciable effect was noticed in the period- icity of root pressure. The changes in temperature above or below certain limits may alter the regularity of the times of maximum and minimum pressure periodicity, but do not interfere with the main cycles of greater or less pressure. The time element is the all important one, and for most plants the period of maximum pressure is 12 M., with the limits between 9 A. M. and 1 P. M. No appreciable difference exists between the times of maximum pressure in the variety of plants studied and certainly none whatever in a large number of specimens of the same species even though they may have been grown under different conditions. The age of the plant seems to make no difference in the times of maximum and minimum periodicity or its general behavior in the experiment, except, as would be expected, a large and vigorous plant shows more difference between the amount of maximum and minimum pressure than a small and less vigorous one. In different genera marked differences exist as to the maximum amount of root pressure and in some it is so small that at no time can it be measured except with great difficulty, The amount of water present in the soil within certaiu limits does not affect the time of periodicity or amount discharged, but in very dry soil, where the roots become wilted, changes are evident as the result of the loss of the turgidity of the root. A consideration of the relation between root pressure and the other phe- nomena in living plants will be interesting in this connection. With regard to its relation to transpiration, the latter can not be explained by the former, since, at the most, it is not sufficient to lift the water above 80-90 feet. Root pressure furnishes only a part of the water used in transpiration, as was shown by our own 146 and previous experiments, ! and no root pressure was found in plants during rapid transpiration. The time of greatest transpiration seems to bear no relation to the time of greatest or least root pressure, and changes in temperature that affect the former do not influence the latter to any degree. Where no transpiration is going on the root pressure may produce sufficient pressure in the plants of medium height to force the water out through the water pores of the leaves, or in some cases producing blistering in the tissues of the stem, as in the well-known case of the Oedema of the tomato. ? The relation of the root pressure with growth does not warrant any statement as to the influence of one upon the other. The time of either the maximum or minimum periods of each do not correspond, and changes in temperature that af- fect growth produce no changes in the constancy of the root pressure. Studies regarding the relation between root pressure and assimilation show all negative results, and the changes producing variations in the latter have no effect on the former. The same may be said of the relation between root pressure and respiration. . In view of these facts we are warranted in the following general conclusions. The periodicity of root pressure seems to be inherent in the plant, and has either been acquired by previous adaptation to environments, or as the results of the action of some constant or periodic changes in the plant. As with the periodicity of growth and other periodic phenomena it does not always follow that a periodic change has not been produced by some constantly or continuously acting agent. Root pressure does not seem to have any relation to the previous periodicities of the vital activities of the plant when the top was connected with the roots. The measure of the root pressure seems to be the osmotic activity of the root hairs, and is probably due to the presence of organic acids and other substances in the rhizoids that show great affinity for water. Although the organic acids increase in the cells at 50°-60° F., yet their in- crease does not seem to make any appreciable difference in the periodicity. This is true even when the temperature of the soil is brought up to 55° F., ap- proaching the time of minimum pressure. The fact that seems inexplicable is that, when the temperature is raised above the point where the organic acids decompose (60° F.) tin most plants, the roots may show an increase in their osmotic activity at the daily period of maximum 1DeVries, Arb. Les. Bot. Inst. (B. I, p. 228). 2Atkinson, G. F., Bull. Cornell Exp. Station, No. 83, 1893. 3DeVries, Bot. Zeitung, 1877, 8. 1-10. 4DeVries, Bot. Zeitung, 1883, 8. 850. 147 pressure. The absence of a top to the plant, and its consequent loss of periods of maximum and minimum oxidation, which are the real causes of the variation in the quantity of organic acids in the cell,° “may be the reason for the failure to produce the expected results. The time of periodicity of root pressure is con- stant in the same genus, but some species may show greater absolute pressure than others. This may be due to accidents in growth, etc. The fact of the periodicity of root pressure seems to be established beyond the possibility of a doubt, and capil- arity and similar phenomena, as suggested by Prof. C. B. Clark’ and others, can not account for the facts observed. NotTEs ON THE FLORA OF THE LAKE REGION OF’ NORTHEASTERN INDIANA. By W. W. CHIPMAN. A glance at any map of Indiana showing the lakes and marshes will convince one of their special abundance in the north part of the State; and many more will be observed in the northeastern counties than in the northwestern. In the Fifteenth Report of the State Geologist of Indiana?, Dr. John M. Coulter divides the State into seven botanical regions, one of which he calls the ‘‘Lake Region.” Included in this ‘‘ Lake Region” are the sixteen northernmost counties of the State, with the exception of the very northwestern counties, Lake and Porter. I would separate from his Lake Region some of the most northeastern coun- ties, and claim for this territory sufficient peculiar conditions for plant growth to merit its being considered a distinct botanical region, and would call it ‘‘The Lake Region of Northeastern Indiana.” OUTLINE OF THE REGION. Aline drawn from the vicinity of Warsaw, Kosciusko County, north along the line of the C., C., C. & St. L. R. R. to its intersection with the northern boundary of the county, and from thence northeast through LaGrange, LaGrange County, to the northern boundary of the State; and a line drawn from the vicin- ity of Warsaw east along the line of the P., Ft. W. & C. R. R. to its intersection 5Ward, Proceedings of Royal Soc., Vol. XLVII, pp. 393-443. ®Warbung, Untersuchungen, etc., pp. 77-92. 7Linnean Soc. Journal. 115th Rep. State Geologist Ind., p. 256. 148 with the eastern boundary of the county, and from thence northeast through Waterloo, DeKalb County, to the eastern boundary of the State, would enclose approximately this Lake Region of Northeastern Indiana. I would not attempt to bound it by any invariable line. The characteristic conditions for plant growth found in the center of the region may at some places extend somewhat beyond the limits given, and at other places may not reach them. The region includes, in general, all of Steuben County and Noble County, the northeast part of Kosciusko County, the southeast part of LaGrange County, and the extreme north part of Whitley County. This part of the State has for some time appeared to me to present conditions for plant growth different even from the rest of the northern counties contained in Dr. Coulter’s ‘‘Lake Region,” and I am glad to have it proven by Dr. Dryer in his geological report of Steuben County? that this region as outlined above has separate and distinct geological features. After speaking of the drift left by the Saginaw ice and the Erie ice, and the confused mass of drift left by their union, he says*: ‘‘Such a belt or drift forms the Saginaw-Erie interlobate moraine, which in Indiana stretches across the counties of Steuben, LaGrange, Noble, Whitley and Kosciusko. Thus are the peculiarities of topography and soil in that region accounted for.” 5 It is not claimed that plants characteristic of the region are not found in the neighborhood of lakes of northern Indiana outside of its limits. The proportion of lakes and their characteristic surroundings outside of the Northeastern Indiana Lake Region, is so small when compared with such condi- ions in the region, that plants found farthest from the lakes, together with others entirely foreign will predominate in the other northern counties. In a report in 1874, by G. M. Levette?, upon the geology of the northern tier of counties, including a greater part of the region under discussion and the most northern counties of Dr. Coulter’s Lake Region, he says®: ‘‘On the eastern side of the district, the land originally timbered is largely in excess of prairies and openings, but, as we go west the proportion of prairie land increases.” In the same report he says of Elkhart County®: ‘‘ Only a small per cent. is covered with peat-bogs, lakes and marshes.” Of St. Joseph County he says’: ‘‘ Diversi- ed with prairies, oak, openings, and rolling timber lands;” and’, ‘‘small tracts } ? d p $ ? Do ) 217th Rep. State Geologist Ind., 1891. 3 Tdem, p. 182. 45th Rep. State Geologist, Ind., 1874. > Idem, p. 482, ® Tdem, p. 452. 7 Tdem, p. 457. 149 of low, marshy ground.” Of LaPorte County’: ‘The central and southern parts are mostly prairie;” and only’, ‘‘small marshy spots and peat-bogs” to the north. Marshall County.is spoken of in another report by W. H. Thompson® as mostly prairie and large tracts of barren land. These references to small percentagé of lakes, swamps and bogs from these northern counties not in the lake region under discussion, when compared with the continued references, everywhere, to the large percentage of such conditions in the northeast Indiana lake region, would seem to be sufficient authority for b : ; . . s. A separating it from the ‘‘lake region,” as formerly considered. OUTLINE OF THE BOTANICAL WORK DONE IN THE REGION. A Flora of Steuben County was published in 1892 by E. Bradner'®, and a Flora of Noble County in 1893 by W. B. Van Gorder!!. So far as I can ascertain, no geological report has ever been made for Kosciusko County, and no specimens of plants preserved, other than those in my herbarium. In company with Prof. A. B. Crowe, of Ft. Wayne, and Thomas A. Davis, of Goshen, I made a short collecting trip through the lakes and marshes in the northeastern part of Kosciusko County, during the last of June and the first of July, 1894; and I have made collections in the more immediate vicinity of Warsaw since 1893. During the summer of 1896 I spent several weeks in the study of the grasses and sedges of the immediate vicinity of Warsaw, under Dr. Stanley Coulter, but owing to rains and floods making it impossible to get to desirable low regions, and to the fact that I was limited to a part of each day by other work, I was able to collect and study but some forty species. I may say that it is at the suggestson of Dr. Coulter that I attempt this paper. The Floras of the two counties mentioned, and my own collections will be re- ferred to as a basis for deductions, since the three counties thus covered will com- prise the greater part of the region, and no reports of the botony of the other counties—only small parts of which are included in the region—have been made. GENERAL PHYSIOGRAPHIC CONDITIONS. The climate throughout the region is the same; there being only about forty miles difference in latitude and sixty miles in longitude. The general surface of the country is rolling, and almost hilly to the north, sloping in general to the *Idem, p. 462. "15th Rep. State Geologist Ind., p. 178. 1° 7th Rep. State Geologist Ind., 1891-2, p. 135. 118th Rep. State Geologist Ind., 1893, p. 33. 11 150 southwest. About one-third of the region was originally covered with heavy tim- ber, and the soil of this part is a clayey loam. The soil of the very small areas of prairie land is a sandy loam, and the swamps are filled with rich, black muck and peat many feet deep. This is the general distribution, but pure sand and clay are often found by themselves, over more or less extensive areas. Occasion- ally sand and muck are found in combination. These different soils furnish sustenance for a flora of a widely varied species, while those thriving best in wet soil or growing in water will predominate. ; LOCAL PHYSIOGRAPHIC CONDITIONS. In the northern part of Steuben County, to the extreme northeast of the region, are localities of pure sand of rather extensive area, and lakes entirely surrounded by sand and lime deposits, around whose edges, and in whose bot- toms, scarcely any vegetation is to be found. Sandy spots devoid of vegetation are occasionally found throughout the region, but of very limited extent. The Steuben County tracts are quite peculiar to their immediate vicinity, and per- haps should not be included. In none of the other counties do we find entire lakes so destitute of vegetation. I have counted over ten plants in Bradner’s list!? characteristic of a barren soil which are not found so far, or only occa- sionally, in the rest of the region. In general, there would seem to be the greatest prevalence of plants characteristic of lighter sandy soil in Steuben County, the greatest prevalence of plants indicative of a wet, peaty soil in Kosciusko County, and rather more of a mixture of the two in Noble County, between. But a very general uniformity of species will be found throughout the region, which will increase with closer study and more extended collecting. PHYSIOGRAPHIC CHANGES. 1. Low Swamps. The lakes are for the most part surrounded by low lands or marshes, which show that the lakes were once of much greater extent. Soil is accumulating around these lakes by the growth and decay, from season to season, of the rank vegetation around the edges, and this process is continually diminish- ing the size of the lakes, forming large marshes, which are being drained by ditching and tiling. A great deal of valuable land has thus been- reclaimed and successtully farmed. 1217th Rep. State Geologist Ind., 1891-2, p. 135. 151 The result of this change is a decreasing area for water plants, but an increasing area for swamp plants, which area is again converted into cultivated dry land. While this is a slow process, and has not materially decreased the size of the lakes very lately, yet a great deal of swamp land which formerly was over- flowed at periods of high water has been, within the past twenty years, so success- fully drained as to make dry, tillable land. The amount of swamp land in Kosciusko County at present is not one-half what it was twenty years ago; but there was so much land of this character then, that the remainder, with the lakes added, is sufficient to designate this as a true lake region. The same changes have taken place to a greater or less extent in all the other counties of the region. But few species have, in all probability, been yet lost to this flora by these changes, but the abundance of many species must be greatly reduced. By means of this system of drainage the land passes from the wettest swamp through all gradations to dry, solid land, and the plants growing on it change in a like manner. I have in mind a certain swamp, which was an outlot of the city of Warsaw, Kosciusko County, in which grew, fifteen or sixteen years ago, great quantities of Typha latifolia L., Sagittaria variabilis Englem., Cypeous strigosus L., and such plants as grow in the wettest swamps. Open ditches were put through and the soil was gradually dried. These plants gradually disappeared, and such plants as Lobelia syphilitica L., Lobelia cardinalis L., Lysimachia stricta Ait., Iris versicolor L., and Potentilla fruticosa L., were noticed. As the ground further dried out, and these began to disappear, others were observed, such as Parnassia Caroliniana Michx., Viola palmita L., var cucullata Gray, Viola Canadensis L., and Gerardia purpurea L. Even these finally disappeared, until one can now only occasionally find a plant of Viola palmata L., var cucullata Gray, and such weeds as grow in a pasture lot—thistles, burdock, ete. This land has, under my observation, undergone these complete transforma- tions as regards its soil and plant life, and is only an example of numerous similar instances throughout the entire region. The rich black muck soil thus formed and mixed with some sand and lime (which latter shows itself in places in marl deposits) produces plants of exceptional size, shows many specimens of rapid growth and unusual development, and affords much material for study along that line. This reclaimed soil has proven specially adapted to the growth of celery, and Warsaw is becoming a large shipping point for celery of exceptionally fine quality. 152 2. Tamarack Swamps. Much of this peat or muck land was formerly covered with tamarack, Larix Americana Michx. The trees grew very near to one another and formed a very dense forest, often with an undergrowth of hus venenata DC., and Betula pumila L. The tamarack has for the most part been cut down, and where standing, the trees are often dead. The drying of the soil takes away one essential condition to their growth. In and near a few tamarack swamps still standing I collected the only specimens of Betula pumila L., I have seen in Kosciusko County. It is not reported from Noble County by Van Gorder?!*, but is from, Steuben County, by Bradner !#, so that it is probably found sparingly throughout the region and dis- appearing with the tamaracks. About ten years ago I collected one specimen of Cypripedium acaule Ait., in the edge of a tamarack swamp in the vicinity of Warsaw, Kosciusko County. In 1882 Dr. Coulter?® lists it as found in a tamarack swamp in Noble County. Mr. Van Gorder gives reference to the ‘‘ Editors of the Botanical Gazette, 1881,” as his authority for listing it in his Noble County Flora'**. It is not reported from Steuben County by Mr. Bradner‘+, and has not been seen in Kosciusko County since the specimen mentioned. The authors of the Lake County list ?® claim that as the only Indiana station, and mark it ‘‘local.” The specimen has evidently been lost to this flora by absence of proper conditions for growth. In connection with the decadence of tamarack swamps in this region, it has been observed that a great many of the plants listed by Dr. Jno. Coulter!’ as being characteristic plants of his ‘‘ Lake Region” are not at present the charac- teristic plants of the ‘‘ Lake Region of Northeastern Indiana.” Of his list of twenty plants, Betula pumiia L., Tofieldia glutinosa Willd., Lilium superbum L., Ruellia. eiliosa Pursh., Solidago stricta Ait., Ribes rubrum L., Potentilla argentea L., and Myriaphyllum spicatum L., are very rarely found; while Cypripedium acaule Ait., Oxalis acetasella L., Aster longifolius Lam., and Vaccinium Pennsyl- vanicum Lam., have not been reported since that time. Arabis lyrata L., and Lechea major Michx., are only occasionally found. Hlodes campanulata Pursh., 1318th Rep. State Geologist Ind., 1893, p. 33. 1417th Rep. State Geologist Ind., 1891-92, p. 135. 25 Bot. Gazette, V. Sup. I., 1882, Flora of Indiana. 16 Higby, Wm. K., and Raddin, Chas. S., Flora of Cook Co., Il., anda part of Lake Co., Ind. Bull Chicago Acad. Sei. IT. 17 15th Rep. State Geologist Ind., p. 259. *Mr. Van Gorder recently reports it personally found in Noble County, but it is by no means common. 153 Maianthemum Canadense Destf., and Allium cernuum Roth., are found more com- monly, but not in such abundance as to be termed characteristic of the region. This only leaves two plants of the list which now remain as characteristic, viz. : Lobelia Kalmii L., and Seutellaria galericulata L. It is true, of course, that Dr. Coulter’s ‘‘ Lake Region” covered more terri- tory than the “‘ Lake Region of Northeastern Indiana,” but this latter was in- cluded, and formed a very considerable part of it, and the fact that only two of his list can now be called characteristic of our smaller Lake Region has its sig- nificance. It must be that the entire north part of the State has undergone a noticeable change in conditions producing its characteristic plants, or that this northeastern part under consideration has alone changed, or that we have here conditions dif- ferent from the remainder of the former Lake Region which were existent at that time. Most of Dr. Coulter’s observations were along the line of the L. S. & M. S. R. R.—largely in St. Joseph County—and only touching our region in Noble County. It is quite probable that the observations at that time did not extend so thoroughly in our region as in the districts to the north and west, where there was not such an abundance of lakes and pure lake forms. * The tamarack and associated swamp plants are more frequent in Dr. Coulter’s list than our present lake plants and swamp plants free from tamarack surround- ings. Our most common species of this latter class, now so abundant, can scarcely be of very recent introduction, and this would seem to show that our pure lake plants were not even then (1886) so abundant in the remainder of Coulter’s Lake Region as in this part of it which we call the Lake Region of Northeastern Indiana, proving more conclusively the distinctiveness of this region. The gradual disappearance of the tamarack is no doubt general throughout northern Indiana, and the list referred to would not include so many characteristic plants for any northern county as when made, yet it would seem evident that the list never con- tained as many plants peculiar to our region as to the counties north and west of us, and that there always have been more pure lake forms in the counties included in the Northeastern Indiana Lake Region than in the remainder of northern Indiana. From the frequent references which will occur to Lake County as the only other station, or one of a few other stations, for a number of the plants peculiar to the Northeastern Indiana lake region, it may be inferred that Lake County as a whole is very similar to this region, and, with the intervening territory, should be in- cluded. When the lists of this region and the lists of Lake County are compared it will be found that there are many plants not in common. 154 - A large part of Lake County is the sandy region—to which we have no paral- lel—left by the receding of Lake Michigan to its present bounds. There are in northwestern Lake County—the southeast part of the region covered by Higley and Raddin’s catalogue—some lakes and marshes which present conditions similar somewhat to our own. These localities in Lake County have been so thoroughly examined that it is not strange to find some of our less frequent species also ‘very infrequent” there. Most of all the references made are to plants very rare or local in Lake County. Many of our common species would not be found in Lake County, and very many common Lake County species would not be found here at all. While Lake County offers similarities in a small part of its territory, the Lake region of Northeastern Indiana and the Lake County region, as a whole, are dissimilar. Notes IN GENERAL, UPoN OccURRENCE AND DISTRIBUTION OF RARE oR IN- TERESTING SPECIES. Those who have published lists covering any part of Northeastern Indiana do not claim them to be complete, and doubtless new plants are yet to be observed. By comparing the partial catalogues referred to with my own collections I find a total of some nine hundred and fifty species reported from the ‘‘ Lake Region of Northeastern Indiana.” It is to be regretted that Mr. Bradner has not given in his catalogue'* any notes as to abundance of species, or to distribution over the territory. With the exception of one or two instances it is impossible to tell whether a supposable rare plant is rarely or more commonly met with, or in what kind of soil, or under what conditions it is found. If scarce, whether it is recently noticed and just appearing, or whether formerly seen and just disappearing. With the geology of the county given by townships in the same volume, Mr. Van Gorder’s reference’ ® to scarcity or abundance, and to locality by townships, is very helpful. It would seem that much more importance should be placed on these anno- tations than is often done. The helpfulness of richly annotated lists is double that of those with bare names of species. 18]7th Rep. State Geologist Ind. 1891-2, p. 135. 1918th Rep. State Geologist Ind. 1893, p. 33. 155 PLANTS NOT GIVEN IN COULTER’S LIST. 2° During my collecting in Kosciusko County I have found seven plants not re- ported in Coulter’s List. On the sandy, low shore of Chapman’s Lake, Kosciusko County, I found, in 1894, two specimens only of Epilobium Adenocaulon Haussk. Although growing very near each other they have a very different aspect, and so far as I could judge from the manual description I had a specimen of E. glandu- losum Lehm., which Trelease says”! does not occur in the United States. The specimens were both sent to Dr. Trelease, and he writes me that they are both E. adenscaulon, much as they appear different; and that EF. adenscaulon is very variable. So far as I can ascertain EF. adenscaulon has never been found in In- diana with the exception of the two specimens I possess; and it is interesting to note that Beal & Wheeler?” do not list it from Michigan farther south than Keewenaw County, the very northermost county of the Upper Peninsula. Anychia Capillacea DC., I have found in Kosciusko County in two places in quite abundance—on the east shore of Tippecanoe Lake in woods, and in a simi- lar situation in Winona Park, Winona Lake. The manual?® says, ‘‘ More abun- dant northward,” but it is not given by Beal & Wheeler, as found in Michigan, just north of us. Higley & Raddin?* list it as found in Riverside, Ill., Cook County, but do not list it from Lake County, in their list of Cook County, I1., and Lake County, Indiana, plants. Specimens of Bidens Beckii Torr. were found by me in 1893 in the slow waters of the Tippecanoe River, near Warsaw, Kosciusko County. I could find no list of any section in Indiana containing this species, and reported the same to Dr. Jno. M. Coulter. Since then I have found it mentioned as rare in Lake County, and by Bradner from Steuben County.”° I failed to find it elsewhere, nor could it be found in the same place the next year. I found, in 1894, a few specimens of Asclepias phytaloccoides Pursh. near Chapman’s Lake, Kosciusko County. It is not in Couiter’s list, but I have since 2°Bot. Gazette V, Sup. I, 1882, Flora of Indiana. From which all future references to “Coulter’s List’’ or to the “‘State Flora’’ are taken. 21Monograph Genus Epilobium, p. 100. 22Mich. Flora, 1892, W.J. Beal and C. F. Wheeler, Agricultural College, Mich. From this work all future references to Beal & Wheeler, or Michigan Flora, or to:plants of Mich. are taken. 23Gray’s Manual, 6th Edition. All references to Manual are Gray’s 6th Ed. 24Bull. Chicago Acad. Sci., Vol. II, No. 1, 1891. From which all future references to Lake County are taken. 2°17th Rept. State Geologist Ind., 1891-2, p. 135. From which all future references to “Bradner’s List’’ or “Steuben Co.’’ are taken. 156 found it reported from Lake County ‘‘rare,” from Central Eastern Indiana?® “rare,” but more common in Noble County’? and Steuben County than elsewhere, showing that this lake region must offer peculiar suitable conditions for its growth. Trifolium Lybridum L. is fast becoming common in this flora, and is mixing so with Trifolium repens L., it seems quite impossible to find T. repens very often true to the type. It is reported from the other counties of this region as quite common, while to the northwest, in Lake County, it is listed as infrequent, as also in Beal & Wheeler’s ‘‘ Michigan Flora.” Boutelona racemosa Lag. I found this last summer (1896), on a hillside in Winona Park, Kosciusko County; very abundant in one plat about one rod square, but seen nowhere else. It is not listed by Troop in his ‘‘ Grasses of Indi- ana,”’* nor do I find it listed anywhere from Indiana except by Bradner, from Steuben County, in this region. Eleocharis quadrangulata R. Br., is not listed by Dr. Coulter, but is marked ‘‘rare” in the Manual. This was found last summer (1896) in Winona Lake; quite abundant in one locality. It is reported from South Michigan as rare, and from Steuben County by Bradner. Outside of these two reports from this region, I find only one other report from Indiana, and that in the appendix to the Lake County list, in one locality only. PLANTS IN COULTER’S LIST, BUT NEW TO OR RARE IN THIS REGION. Eleocharis avata R. Br., though given in Coulter’s List as common to the State, is not reported in any local list of the south part of the State at my command, and is ‘‘infrequent” in Michigan to the north, but I found a few specimens at Winona Lake, Kosciusko County, and it is reported from Steuben County, this region. This northeast part of Indiana would seem to be more suited to it than other parts of the State. It is ‘‘ very infrequent” in Lake County. Hibiscus Moschentos L. is only reported from the ‘‘ knobs” in Coulter’s list, and I can find no other report of it from this State than in Lake County. I found a large clump of it on the Tippecanoe River, Kosciusko County, in 1893. In-1894 I found about six plants of Parietaria Pennsylvanica Muht., on a sandy shore of Turkey Lake, Kosciusko County. Coulter’s list reports it only from the banks of the Ohio. I can find no other locality in the State from which it is re- ported, except from Lake County, and then marked “rare.” 2619th Rept. State Geologist, 1882, “Flora of Central Eastern Indiana,’’ A.J. Phinney, M. D., p.196. From which all references to Cent. Eastern Ind. are taken. 2718th Rept. Ind. State Geologist, 1893, p.33. From which all future references to “Noble Co.’ or “Van Gorder’s List’’ are taken. ' ee 29 Ind. Agri. Expt. Sta., Lafayette, Purdue Univ., 1889. “ Grasses of Indiana.’’ —J. Troop. 157 I found in 1893, on waste ground, Kosciusko County, one specimen of Ipomee hederacea Jacq., which is the only discovery of the species I can find north of Centrai Indiana, nor is it reported from Michigan, to the north. A few specimens of Myriaphyllum heterophyllum Michx., which I found in Boydston’s Lake, Kosciusko County, are the only plants of the species I can find reported from the north part of the State, but from Steuben County, this region, and from Lake County. [ would add Kosciusko County as another locality, for four plants mentioned in Dr. Stanley Coulter’s paper?° before the Academy last year, as occurring at only one or two stations in the north part of the State. They are Liparis heselii Richard., Menyanthes trifoliata L., Aster umbellatus Mill., and Galium boreale L. Other plants, not previously reported from the north part of the State, or if so, only from Lake County, could be stated as having been found in this Northeastern Indiana Lake Region. SOME GENERAL OBSERVATIONS. In this connection I would call attention to the listing of Prunus Pennsylva- nica L. f., in a list of the common timber trees of seven counties in this immediate section.?” Is this not a mistake? Should it not be Prunus serotina Ekoh.? P. Pennsylvanica is not in Coulter’s list, and is not reported from this region by any list whatever other than this reference. It is marked ‘‘very rare” from Central Eastern Indiana, and also ‘‘rare along the lake shore,” in Lake County. Beal & Wheeler say in ‘‘Michigan Flora,” ‘‘ Very abundant on sandy soil in the north half of the State, but less common southward, where -P. serotina takes its place.” P. serotina is surely the only wild cherry here which could be used for lumber (the only other tree of this genus found here—P. Americana Marshall—being too small), and should be substituted in the list referred to for P. Pennsylvanica. I would also call attention to some species listed by Bradner & Van Gorder, which appear to me to be probable errors. Mr. Van Gorder lists from Noble County, ‘‘ Hepatica acutiloba DC., Liver leaf, common”; as does also Mr. Bradner, from Steuben County, and neither list Hi. triloba Chaix. In all my collecting in Kosciusko County I have never seen H, acutilobs, while H. triloba is one of our most common spring plants. I am well aware that the two species are apt to approach each other, and that transi- tion forms are apt to be found, but am well acquainted with the two species, having been able to find at Crawfordsville, Indiana, with close searching for two 2°Proc. Ind. Acad. Sci., 1895, p. 183. 55th Rept. State Geologist Ind., 1873. Observations by G. M. Levette, p. 434. 158 seasons, nothing but H. acutiloba, and tind nothing in Kosciusko County but i, triloba, the scapes of which seldom grow to the height of those of aeutiloba. It would seem strange that such an apparent difference should exist between counties of the same region, and I feel quite certain, since these lists report but one form, it must be H. triloba. Mr. Bradner lists from Steuben County, ‘‘Claytonia Caroliniana Michx., Spring Beauty.” Mr. Van Gorder reports from Noble County only C. Virginica L., and that is the only species reported from Kosciusko County. It is not at all probable that C. Caroliniana is found so far south in this longi- tude. Beal & Wheeler say Caroliniana is not found in the south part of Michigan. It is reported from Lake County, where the conditions are more like those of Northern Michigan, and it seems very certain that the plants referred to in Mr. Bradner’s list should be written C. Virginica. Nowhere can I find Viburnum nudum L. reported outside the limits given in Gray’s Manual, 6th edition, viz.: ‘‘From N. J. to Florida,” except from Steu- ben County by Bradner, and if it be correct, is worthy of mention as an entirely new plant to this region. Mr. Bradner also reports Typha augqustifolia L. from Steuben County, which is very rare indeed, and deserves special notice. I have not corresponded with either Mr. Van Gorder or Mr. Bradner, nor seen their collections, and draw the above conclusions wholly from general obser- vation. It is worthy of note that Nelumbo lutea Pers. is reported from Blue River Lake, Whitley County *!—a part of this region. This is the only reported local- ity in Indiana, except Lake County, and the species is very rare in the Central States. This region, as a whole, seems to possess a flora considerably different from that which it had a decade since; to have lost many of its northern forms, and to have gained some southern forms. Introduced species from the east and west have been brought in by the railroads. The climate is much milder than form- erly, and the various conditions for plant growth materially changed. Until re- cently it has not had as much attention from botanists as other sections of the State. A more careful study of the flora will surely develop interesting facts. There is much to be done along the line of cryptogamic botany. Surely the ter- ritory as outlined is worthy the designation of a separate and characteristic region, and will repay the more extended investigations of botanists. 5 17th Rept. State Geologist Ind., pp. 166. 159 CONTRIBUTIONS TO THE FLoRA oF INpDrIANA, No. IV. By SrantEy Coulter. The preceding papers in this series are those entitled Sarifragacee of Indiana (Proc. Ind. Acad. Sci., 1894, pp. 103-107); A Preliminary List of Plants Growing in the Vicinity of Washington, Daviess County (Proc. Ind. Acad. Sci., 1895, pp. 169-182) ; Noteworthy Indiana Phanerogams (Proc. Ind. Acad. Sci., 1895, pp. 183- 198). Thé notes are incidental to the preparation of the catalogue of the flora of the State, and are in a measure supplemental to that work. Many plants which were originally included in this contribution have been omitted, because of their inclusion in much fuller detail than I could possibly have given in the papers of Messrs. W. S. Blatchley and Robert Hessler, M. D., published in these proceedings. With the exception, therefore, of a few forms to which I desire to call attention, the body of this paper concerns the composite of the State, with special reference to their distribution. Coptis trifolia Salisb. Mr. Van Gorder reports this plant as very abundant in certain localities in both Noble and DeKalb counties. So far as has come to my knowledge, this is the only record of the plant in the State authenticated by herbarium specimens. Its range and habits of growth would indicate its pres- ence in the swamp regions of our northern counties. Ailanthus glandulosus Desf. This tree, not as yet included in the lists of the forest trees of the State, seems to have become thoroughly naturalized, and is entitled to a place in our flora. In Jefferson county it has escaped from cultiva- tion and covers entire hillsides, notably in the vicinity of Madison and Hanover college. The growth is so dense and rapid as to make it a somewhat doubtful acquisition. A thicket of Ailanthus in full foliage gives a very fair idea of the appearance of semi-tropical undergrowth. The tree should be included in the flora of the State. Sullivantia Ohionis Torr. and Gray. This form, the distribution of which I limited (Saxifragacee of Indiana, Proc. Ind. Acad. Sci., 1894, p. 104) to a single station at Clifty Falls, Jefferson county, must have an added station in Clark county. The determination of Dr. C. R. Barnes, questioned in that communica- tion, has been verified by abundant specimens found among the duplicates in Purdue university. The Clark county station is of the same general, character as that at Clifty Falls, the plant clinging to the vertical sides of moist limestone cliffs, by no chance seeming to leave this apparently barren position for the deeper and richer soils surrounding. The plant in our region may be considered as the most characteristic of the limestone cliffs. 160. Juniperus Virginiana L. The apparently rapid increase of this cedar through- out southern Indiana is worthy of note. Within ten years the number of well- grown forms has increased at least fourfold. The explanation of this increase is to be found in the almost universal fencing of regions formerly wild, and the con- sequent restriction of cattle ranges. It is an extremely suggestive example of the almost immediate effect of a modification of the factors entering into the struggle for existence. It is incidentally suggestive of the fact that when reforestration is attempted, the young forest areas must be as carefully guarded as are flower or vegetable gardens, Tipularia discolor Nutt. This rare orchid is reported by Prof. A. H. Young as having been found at the Clifty Falls station, in Jefferson county, the past sea- son. This is much south of its central range, although in its easterly range it ex- tends as far south as Florida. The plant affects sandy woods, while the Clifty Falls Station can offer noth- ing except a thin limestone soil or a heavy, cold clay. The record is verified by herbarium specimens. The composite of Indiana, so far as reported to the survey, number 213 species, distributed through 55 genera. The Asters lead with 32 reported species, Solidago coming second with 28. The other larger genera are Helianthus, 13 species; Hupatorium, 7 species; Erigeron and Coreopsis each with 6 species; Bidens, Silphium and Liatris each with 5 species. Owing to imperfect notes and “‘ scrappy ” material the work, especially in the Asters and Solidagos, was extremely difficult. While doubtless many errors occur, there has been a constant endeavor to elim- inate all doubtful references. In some cases specimens have not been seen, but where admitted the original specimens have been passed upon by some well-known expert. Very few of Dr. Schneck’s specimens have come into my hands, but all of his doubtful forms were referred at the time of collection to Dr. Gray. It may be assumed that all admitted forms have been inspected or passed upon by some botanist entitled to speak with authority. It may be intimated here that apparently no other family responds so quickly to changed conditions. The response, even to slight changes, is often very marked. Many Asters and some Solidagos present fairly distinct forms, determined appar- ently merely by the amount of light or shade. Others indicate clearly the amount of moisture in the soil. Because of this ready response to environmental changes a determination of a form from a single specimen is often an impossibility. I have felt compelled in some cases to omit from the list forms of apparently correct determination until fuller notes or a larger suite of specimens proved them not to be environmental variations. 161 With but few exceptions, the composites within our bounds do not come into full flower until July and August. Asa rule the flowering season is long, many genera blossoming abundantly from Juiy until checked by the frosts. From the middle of August they determine the physiognomy of the vegetation over the entire area of the State. This is especially true in the prairie region and in open fields. Indeed, the great majority of the composites of Indiana are found in their greatest abundance and luxuriance in dry soils and in regions exposed to the full action of the sun. They seem to be xerophytes of the xerophytes. Some species of Eupatorium, Liatris spicata and other forms, however, furnish exceptions as regards dryness of soil, while Po/ymnia and a few others give excep- tion as to light. Certainly in no-other family in our area can xerophytic adap- tations be so satisfactorily studied. While the flowering season is so extended, and the consequent number of achenes formed enormous, it is probable that but a small proportion of them germinate. Theseedlings, also, in all cases in which experiments were tried, were remarkably sensitive to changes in temperature and moisture. Almost every other form used was more hardy in the seedling stage than the compositae. Ex- ceptions to this were the Ambrosias and Lactuca Canadensis L. In the series of experiments the percentage of seeds germinating was very small in the composite, with the exception of Arctium, where the per cents, in three experiments were, 87.5, 80, and 87.5. In Bidens 20 per cent. was the highest, in Lactuea 25 per cent., in Am- brosia 20 per cent.,-while in Cnicus out of three plantings of 30 achenes each, only two achenes germinated. Under the same conditions Abutilon Avicenner Gaertn, in two experiments guve 100 per cent., and in a third, 96.7. The seedlings of this plant were extremely hardy, withstanding wide ranges of temperature and moisture. Solanum nigrum L, Datura stramonium L., and Scrophularia nodosa L.., Marilandica Gray, invariably showed germination per cents. above eighty-five. The plants, other than composites, are introduced simply for purposes of com- parison. The data given above are derived from a large number of germination experiments conducted in the Laboratories of Purdue university. In these ex- periments I have endeavored to eliminate possible error, and to give, so far as could be determined, natural conditions. The experiments cover some 30 com- posite species distributed among 15 genera, and 450 species representing families other than the composite. The material was gathered in almost every instance with extreme care in order that conclusions might be based upon known condi- tions. So far as the experiments go concerning composite, I am convinced that the distribution of this family is largely limited, first, by the small germination percentage of the achenes; second, by the extreme sensitiveness of the seedlings 162 to heat and moisture changes. A series of pots containing seedlings was subjected to an artificial drought of five days. Of theeleven species of composites all except Ambrosia died. Often species of other families, only Serophularia nodosa Marilandica died. Repetitions of tke experiment showed similar results. Another line of ex- periments showed that the composite seedlings were unable to withstand any con- siderable change in temperature, being much more affected by temperature in- crease than by its decrease. An increase of 5° C., from 25° C. to 30° C, usually proving sufficient to kill them or greatly retard their growth. When it is remem- bered that the distribution of composites is for the most part in dry soil, in places exposed to the full force of the sun, it is apparent that large numbers of seedlings must perish. It is possible that the danger of a spread of these forms through seed dissemination has been overestimated. Another fact indicated by the experiments was that the achenes of the earlier and later flowers were rarely viable, this being especially true in Helianthus. It is somewhat surprising that in a family so dominating in species and indi- viduals there is not included a greater number of ‘‘ worst weeds.” Considering the immense size of the family, the number is astonishingly small. Taraxacum invades the lawns; the Lactucas, Cnicus, Arctvwm and Erigeron the fields; but none of them compare in noxious features with forms from other fam- ilies. Ambrosia, which overruns waste fields, I find is considered by the farmers as a positive benefit to the land. Evrigeron, which a few years ago was a great annoyance, seems to have yielded to cultivation, and to have practically lost its place among bad weeds. Doubtless in some places it is still annoying, but the evidence is that it disappears from carefully cultivated fields. Chrysanthemum Leucanthemum L. is certainly bad, but is of restricted range. Bidens is annoying to the sheep-raiser, but does not otherwise rise to the rank of a ‘‘bad” weed. For the most part the composite seem perfectly content to occupy waste places, and readily yield to man the possession of the soil. So far as I have been able to discover, none of the species are poisonous, if I except a few reported instances of poisoning by forms of Cnicus. Most of these cases, I think, can be referred to personal idiosyncrasy. I have tested all the forms of Cnaicus upon myself and upon numbers of students without results other than were referable to the mechanical action of the prickles. Nanthium Cana- dense Mill. is said to be poisonous to the touch.! If this be true, the forms found in the State, X. spynosum L. and X. strumarium L., are to be regarded with sus- picion by persons susceptible to plant poisoning. It is to be remembered, how- ever, that even the known poisonous plants are only poisonous to a small percent- 1White, Dermatitis renenata. Boston, 1887. 163 age of those touching them, and many are only poisonous in certain stages of their growth. Save for the medicinal value of some few forms, none within the State are of economic value, if Jerusalem artichoke (Helianthus tuberosus L.) and the Dande- lion ( Taraxacum officinale Weber), both of which are occasionally used as food, are excepted. Very few of the composite are eaten by animals, except by accident or under pressure of hunger. They are also largely free, at least the Indiana forms, from plant diseases. Their limitation in numbers and distribution I believe to be largely determined by the causes named earlier in this paper. It is not the purpose of this paper to give a full list of the forms found in the State, but rather to call attention to the more general facts concerning their distribution. I. LOCAL FORMS. The species included in this list, so far as has come to my knowledge, are only reported from a single locality. A close examination of the list will show that in many cases this apparently restricted State range is but an indication of territory that has been closely and continuously worked. Vernonia altissima Nutt. Reported from Tippecanoe county by Messrs. Laben and Conner. The distinction between this form and V. fasciculata Michx., turns upon the character of the inflorescence and the surface of the achene. Any one familiar with the varied inflorescence of V. fasciculata will see that the ulti- mate distinction is upon the character of the achene. In fasciculata the achene is smooth; in altissima hispidulous on the ribs. In the specimens reported the achenes were hispidulous on the ribs and the plant was referred to altissima Nutt. Further examination of the genus showed that the achenes of V. Noveboracensis Willd., showed the same characters. The character of the involucral scales, how- ever, excludes the form from Noveboracensis. V. altissima Nutt. is, therefore, added to the State flora. In a general way the plant has the inflorescence and achene of Noveboracensis, the involucral scales of fasciculata, and leaves intermediate between the two. Its appearance is strongly suggestive of the possibility of its being a hybrid form. Mikania scandens L. Reported from Gibson and Posey counties by Dr. J. 2 Schneck. ‘‘Sandy thickets along streams; rare.” There seems to be no reason 27th Rep. Geol. Sury. Ind., 1875, p. 525. 164 why this plant should not be found in other localities. It, presumably, from what is known of its distribution, came into the State from the north and east.* Liatris squarrosa Willd. Gibson and Posey counties, Dr. J. Schneck. ‘‘ Dry soil; rare.”* Another form which is probably of much wider range than present reports indicate. Chrysopsis villosa, Nutt. Keported from Vigo county by W. S. Blatchley, “Frequent; banks of old canal, prairies, etc.” * This species has evidently entered our territory from the west and may be found in the western tier of counties. Solidago squarrosa Muhl. Reported from Floyd county in 1837 by Dr. A, Clapp, and not since recorded in the State. A number of species found in the Clapp collection are in similar case. Their disappearance from our flora empha- sizes the importance of continuous regional study in order that we may have more accurate knowledge of plant movements. Solidago petiolaris Ait. Specimens by Baird and Taylor from Clark county have been referred to this species. The specimens are not entirely satisfactory, but there seems no doubt of the accuracy of the reference. The plant entered the State flora from the southwest. Solidago odora Ait. Gibson and Posey counties, Dr. J. Schneck. ‘‘Sandy soils, scarce.” Specimens have not been examined, but the species is admitted for reasons indicated earlier in the paper. Solidago rupestris Rat. Reported from Clark county by Baird and Taylor. The inclusion of Indiana in the range of this species in the 6th edition of the Manual was doubtless based upon this collection. Brachycheta cordata Torr. and Gray. Jefferson county. For full notes on this form reference is made to Noteworthy Indiana Phanerogams, in Proc. Ind. Acad. Sci., 1895, p. 189. Servocarpus solidagineus Nees. In the Clapp collections of 1834-37, from Floyd county. It does not seem to have been recorded since that time. Aster macrophyllus L. This form from the north is reported from Noble county, by Mr. W. B. Van Gorder. Aster Drummondii Lindl. Reported as ‘‘frequent in low, open pastures and prairies”® in Vigo county, by W.S. Blatchley. A western form very close to A. sigittifolius Willd., and possibly a mere geographical variety. °Tbid, p. 534. * Blatchley, W.S., Compositex of Vigo County. In ed. * 7th Rep. Geol. Surv. Ind., 1875, p. 536. ® Blatchley, W.S. Composite Vigo county. In ed. * Since this was in type, Mr. W.S. Blatchley, under date of September 26, 1897, sends me abundant specimens of this form from Lake county. He reports itas “‘ growing plentifully over bushes on the mucky margin of a stream, four miles east of Hebron.’’ 165 Aster vimineus Lam., folvolosus Gray. This form is reported from Franklin county by O. M. Meyncke. So far as I am able to judge the reference is correct, although the well-known difficulty of separating the group of species in which it is found renders absolute vertainty impossible. Aster junceus Ait. Reported from Clarke county by Baird and Taylor is in all probability not a member of the State flora. The very scant specimen I have examined from the Clark county locality is probably A. Novi-Belgii L. As the specimens fit the latter as well as they do junceus, range probabilities lead to the exclusion of A. junceus Ait., from the State flora. Ambrosia bidentata Michx. Reported as ‘‘common, dry prairies” ’ in Gibson and Posey counties by Dr. Schneck. From the west and probably to be found as far north as Vermillion county, although the Gibson and Posey county station the only one reported. Rudbeckia specuosa Wenderoth. Reported from Jefferson county by J. M. Coulter. The specimen has not been examined, but is admitted upon the author- ity of the collector. Rudbeckia fulgida Ait. Reported by Dr. A. J. Phinney from Jay, Delaware, Wayne and Randolph counties. Dr. Phinney states that his specimens were veri- fied by Dr. John M. Coulter. The species is therefore admitted, although so marked a form should not rest upon a single reference. Helianthus rigidus Desf. Jay, Delaware, Wayne and Randolph counties, Dr. A. J. Phinney. The form is very characteristic and could scarcely be mis- taken. It is probably a member of the State flora, although its more natural lo- cation would be the western portion of the State. Helianthus occidentalis Riddell. St. Joseph county. Reported by Dr. Charles R. Barnes and verified by abundant specimens. Helianthus tomentosus Michx. Reported from Clark county by Baird and Taylor, is probably an incorrect reference. No specimens have been examined and the range probabilities are sharply against its presence in the State. Coreopsis auriculata L. Clark county, Baird and Taylor. Coreopsis discoidea Torr. and Gray. A specimen of this species is in the Pur- due herbarium labelled Gibson county. No collector’s name is given. The plant is not included in Dr. Schneck’s Flora of Lower Wabash Valley. The identification is correct, the only question which arises is concerning the locality. I know of no collector other than Dr. Schneck in that region. Upon the specimen, the species is admitted to the flora. 7 7th Geol. Rep. Ind., 1875, p. 537. 12 166 Bidens Beckii Torr. Reported by W. W. Chipman from a single locality in Kosciusko county. Mr. Chipman secured abundant material of this interesting species which is northern in mass distribution. Hymenopappus scabiosaevs, L’Her. ‘‘ Scarce on sandy knolls”’* in Vigo county Reported by W. S. Blatchley. This is only one of a large number of plants added to our flora by the careful investigations of Mr. Blatchley. The plant entered the State from the southwest. Verifying specimens in De Pauw univer- sity herbarium. Artemisia Canadensis Michx. Lake county, E. J. Hill. For full report see Noteworthy Indiana Phaneroygams, Proc. Ind. Acad. Sci., 1895, p. 191. Artemisia annua L. A Gibson county specimen with no further data. In- vestigation indicates that it is probably not uncommon in the State, although not. definitely reported from other localities. Artemisia Absinthium L. Escaped and well established in Gibson and Posey counties. Not reported from any other locality. Senecio palustris Hook. This species, reported from Clay county by D. T. MacDougal, is represented by specimens in the DePauw herbarium. I have ex- amined the forms and believe the determination accurate. Range probabilities ? seem would suggest the form to be S. lobatus Pers., but the ‘‘ 20 or more rays’ sufficient grounds for holding to the original reference. It is probable that the range as indicated in the manual! should be somewhat extended southward. Cacalia tuberosa Nutt. Reported from LaPorte, LaPorte county, by Dr. C. R. Barnes. I have also found this species in fair abundance in the low ground to the south and west of Pine Lake, near LaPorte. Abundant herbarium specimens verify the reference. The form has probably a much more general distribution through the northern portion of the State in wet lands. Cnicus horridulus Pursh. Reported from Putnam county by D. T. MacDougal, with verifying specimen in herbarium of DePauw university. The reference is incorrect. The specimen is Cnicws lanceolatus Hoffm., in which the leaf prickles have a yellowish caste. With this exception the form is the typical lanceolatus. Cnisus horridulus is a coast plant, and should be excluded from the State flora. Cnicus Pitcheri Torr. Lake county, E. J. Hill.° Cnicus pumilus Torr. Lake county, E. J. Hill.+° Cnicus Hillii, W. M. Canby. Lake county, E. J. Hill.*! 5SBlatchley, W.S.: Composite of Vigo county. In ed. *Coulter, Stanley: Noteworthy Indiana Phanerogams, Proc. Ind. Acad. Sci., 1895, p. 193. 1eThid., p. 193. UThid , p. 193. 167 Cichorium Intybus L. Reported from Noble county by W. B. Van Gorder. This form escapes readily from cultivation, and to my personal knowledge has made a foothold for itself in several localities in the State. This is notably true in Jefferson county. The only specimens, however, are from Noble county. Hieracium Canadense Michx. Reported from Lake county by E. J. Hill. The form will probably be found to be confined to the northern counties in favor- able localities, its mass distribution being northerly. Hieracium longipilum Torr. ‘‘Prairies and open woods, common,’’!? Gibson and Posey counties, Dr. J. Schneck. From the north. Prenanthes serpentaria Pursh. Listed from Clark county by Baird and Taylor. No specimens have been examined. The species is eastern in its distribution, and the reference is probably incorrect. Excluded from the State flora in absence of verifying specimens. The following forms seem to be limited within the State to the northern counties: Solidago stricta Ait. Reported from St. Joseph county by Dr. C. R. Barnes, and from Noble county by W. B. Van Gorder. From the north, and probably to be found in favoring localities in low, damp ground in the northern tier of counties. Solidago uliginosa Nutt. Lake, St. Joseph and Noble counties. Solidago Riddellii Frank, Reported from Noble county by W. B. Van Gor- der; from Tippecanoe county by Prof. Hussey; from Jay, Delaware, Randolph and Wayne by Dr. Phinney. The Noble county reference is well authenticated and sufficient to admit form to State flora. The Tippecanoe county specimen is unsatisfactory, being both scant and incomplete. No special feature excludes it from the reference, nor, on the other hand, does any marked character require the reference. I am inclined to think the Tippecanoe county specimen, S. Ohio- ensis, Riddell, a species of known occurrence in the county. Dr. Phinney’s specimens are not accessible. As it stands, Noble county is the only authenticated station for the species. Solidago tenuifolia Pursh. Reported from Jasper county by Dr. C. R. Barnes, and authenticated by abundant specimens in the Purdue herbarium. Also included by Dr. Phinney in his list of Jay, Delaware, Wayne and Randolph counties. Coreopsis palmata, Nutt. Laporte and St. Joseph counties, reported by Dr. Barnes. Specimens in Purdue herbarium. Probably from the northwest. 127th Geol. Surv. Ind. 1875, p. 541. 168 Artemisia caudata Michx. This species, which has heretofore had its sole sta- tion in Lake county, but which I intimated should be found more widely distrib- uted,1° has an additional station reported in Fulton county by Dr. Robert Hessler. The specimens were examined and are unquestionable. Artemisia Canadensis Michx.1® Prenanthes racemosa Michx.'!* Formerly reported only from Lake and Noble counties, has been reported from Cass county by Dr. Hessler. Abundant speci- “mens were submitted to the survey. The following species, so far as can be determined, seem to be restricted in range to the southern portion of the state. It is probable, however, that more extended study will extend many of these ranges. Elephantopus Carolinianus Willd. Reported only from Gibson, Posey, Jeffer- son, Clark, Daviess and Vigo counties. Eupatorium celestinum L. Reported from Gibson, Posey, Jefferson, Franklin, Monroe and Daviess counties. There seems to be no reason why it should not be found throughout the State, as the mass distribution of the form is northward. Solidago neglecta Torr. and Gray. Reported from Jefferson county by John M. Coulter, and from Clark county by Baird and Taylor. The Clark county specimen has not been examined. The Jefferson county specimen in the Purdue herbarium is S. arguta Ait. In absence of further data, the form is excluded from State flora, the range probabilities being against its occurrence in the locali- ties cited. If found in the State it will probably be in the swamps of the northern counties. Solidago Shortii Torr. and Gray. Floyd county, 1837, Dr. A. Clapp. Re- ported also from Clark county by Baird and Taylor. Indiana probably repre- sents the eastern limit of this species. Boltonia asteroides L’ Her. Reported from Gibson, Posey and Jefferson coun- ties. Also includedin Dr. A. J. Phinney’s list of the central-eastern counties. Aster ericoides L., villosus Torr. and Gray. This variety should be, and prob- ably is, fairly abundant in the State. It is, however, only definitely reported from Jefferson, Franklin and Vigo counties. Erigeron divaricatus Michx. In the Sixth Edition, Gray’s Manual, the range given is ‘‘Indiana to Minnesota, and southward.” The species, however, is only reported from Jefferson, Gibson and Posey counties. In both localities it is said ce to be ‘‘not abundant.” 13 Coulter, Stanley: Noteworthy Indiana Phanerogams. Proc. Ind. Acad. Sci., 1895, p. 191. tS Tibids, pes 1925 To'Tbid:, p. 191. 169 Pluchea camphorata DC. In Jefferson county, on river banks. 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