Gc 974.3 T38hi v.l 1792582 M.L REYNOLDS HISTORICAL GENEALOGY COLLECTION / Qo ALLEN COUNTY PUBLIC LIBRARY 3 1833 01188 3177 Digitized by the Internet Archive in 2010 with funding from Allen County Public Library Genealogy Center http://www.archive.org/details/historyofvermont01inthom F HISTORY VERMONT, N ATU11A L, CIVIL AND STATISTICAI IN THREE PARTS, APPENDIX 185a H\ ZADOCK THOMPSttBL THE NEWBERRY LIBRARY C h i C A G O $urliiigtiui: PUBLISHED BY THE AUTHOR. STACY .^ JAMESON, PKlKTKRS. 1SG3. 1792582 • co ^ CO ,{i. -3 Ol :f Zt '.'] H -J- ■p ■_; i— i o n d " r. B o " be " -- -* ►d t-j in CD ^ :I. £ '^ O 3 O ~* . ■ ~ c+ — . j7 ^ r- N 5 i-* ,_; . 93 ■ Xi 3 r~ p: tr1 0< b =3 M <*= c^ - -; *^, N. Entered according to act of Congress, in the .year 1853, by ZADOCK THOMPSON, in the Clerk's office of the District Court, for the District of Vermont. PRELIMINARY REMARKS. A little more than ton years have now elapsed sinee the publication of my Natural, Civil and Statistical History of Vermont. In that work I endeavored to collect and present as concisely and clearly as I was able, and, at the same time, as fully as the state of knowledge and my prescribed limits would permit— I. An account of the Natural History of the State, embracing its physical geography, zoology, botany and mineralogy. II. The Civil History of the State, comprehending the settlement of the ter- ritory, the organization of the government, and the progress of legislation and improvement, together with a full account of the controversy with New York, the negotiations with the British in Canada, and of our various political, literary and religious institutions. III. A Historical and Statistical Gazetteer, embracing a full account of all the counties, towns, streams, &c, in the State, arranged in alphabetical order. Since the publication of that work, rail roads and the magnetic telegraph have been introduced into the State, and very considerable changes have taken place. A Geological Survey of theState has been commenced, but was discontinued,without any full publication of the results ; in consequence of which, the greater part of the discoveries made and the facts elicited, have been lost to the State and the world ; while a very small additional appropriation in 1847, would have secured to the State a Final Report on the Geology of Vermont, which would have been not only creditable to the State Geologist, but an honor and treasure to theState. But notwithstanding the loss, which has been occasioned, by this penny wise and pound foolish policy of the legislature, our general knowledge of the geology, and of the mincralogical productions of tlio State, has been greatly enlarged by the information elicited and made public during the continuance of the survey. During the last ten years, I have spent a large portion of my time in collecting and preserving facts in relation to the natural and civil history of the State, thinking that the time might possibly come, when I should be warranted in the publication of a new and improved edition of the whole work. But the new materials having largely accumulated, and the number of copies of the original work, on hand, beingsuch as to afford no encouragement for a speedy republica- tion of the entire work, I concluded to select some of the principal items into the form of an Appendix, which might be bound with the remaining copies of the original work, and also be bound separately for those who already have the origi1 n.il work and desire the Appendix. partment of Natural History. This is not owing to any lack of materials fur making additions to the other parts, but because those materials could not be so conveniently used in .heir separate condition. Additions to a work of this nature PRELIMINARY REMARKS. are, necessarily , fragmentary ; and to be used advantageously, they must be in" corporate*! by re-writing the whole. But as this could not be done without re- printing the whole, I have selected, for the Appendix, such materials as I thought would be most interesting and useful in their separate state ; and these, fov the most part, relate to Natural History. Since the publication of my work in 1S412, much light has been thrown upon the early history of our State by the antiquarian researches of Henry Stevens, Esq., and facts have been developed, which remove the mystery from certain transactions in our revolutionary struggles. But the introduction of these mat- ters into the Appendix would require a repetition of much of the history of that period, to make it intelligible, and, consequently, more room than can he spared for it. The history of our legislation during the last ten years, if fully written, would furnish an interesting and instructive chapter; but that, too, is excluded lor the want of room. Perhaps the most important acts of legislation within the time, are those which relate to schools and the sale of alcoholic liquors. But, these several acts have not yet been fully tested by experience. The general school law of 1845, appeared to have been drawn with much care, and to promise an efficient provision for the advancement of primary education in the State, and it is to be regretted that it had not been more fully tested, before it was mutilated by repeals and additional enactments ; and was violated by the body which enac- ted it, by their neglect to appoint a State Superintendent of Schools. But in spite of all obstacles, I am happy in believing that the cause of education is advancing, and that one of the most efficient causes of this advancement in our large villages, is the establishment of Union Schools. These schools furnish to the children of the poor the same advantages which are enjoyed by those of the rich, for pursuing the higher branches of study, and thus afford a universal stim- ulus in all the classes in the several schools, which form the union. To almost every article in the (.iazctteer, alterations and additions might be made, but, for the reasons already stated, it was deemed inexpedient. If life and health should be spared for a few years longer, it would afford me much sat- isfaction to re-write the whole work, and, by incorporating in it the additional material, make it more worthy of the approval and patronage of my fellow citi- zens, but, as the great expense would preclude me from the possibility of being able to publish a new edition, that satisfaction is not likely to be realized. Z. THOMPSON. Burlington, April (J, 1853. THOMPSON'S VERMONT JJart jFirat, NATURAL HISTORY OF VERMONT, CHAPTER I. DESCRIPTIVE AND PHYSICAL GEOGRAPHY OF VERMONT- Section 1. Situation, Boundaries, Extent and Divis- ions. Situation. — Vermont is situated in the northwestern corner of New England, and lies between the parallels of 42J 44' and 45° of north latitude, and between 3° 35' and 5° 29' of east longitude from the Capitol of the United States at Washing- ton, or between 71° 33' and 73° 25' of west longitude from Greenwich Observa- tory.* The most eastern extremity of tuiU's given in this work arc in nil cases reckoned from the L'aptlol of the United States. The longi- tude of the dipnoi from Greenwich, according to the most recent observations, in ?7J 1' 43". It is very much to he lamented that the longitude of places in Vermont is so imperfectly known. We are not aware that a single point within the mate lias been determined with any pretensions to ac- curacy. True, a few solar eclipses have lieen ob- served and some calculations have been made, for the purpose of deducing from them the longitude of the places ; but the only observations within our knowledge, which have hitherto boen regarded as entitled to any degree of confidence, were those of tho sohir eclipse of 181 1 , made at Burlington by Prof. James Dean ami John Johnson, Esq., and at Kul- land by Dr. Williams. The longitude of the Uni- versity of Vermont, deduced from these observa- tions by Dr Bowdilch, was 733 14' 34", and of Hilt- hind court house 72° 57' '27' ' west from Greenwich observatory, and in accordance with these has the longitude of the different parts of the state been laid down upon our maps. In 1838, the author pre- pared, with much caie, lor observing the large solar .eclipse of that yen/, for the purpose of determining Px.i. J Vermont is in the township of Canaan^ and the most western in the township of Addison. This state lies nearly in the middle of the north'lemperate zone. The longest day at the south line of the state, is 15h. l)m. i)s.,and at the norlh line, 15h. 25 m. 50s. Boundaries. — Vermont is bounded on the north by the province of Canada, on the east by New Hampshire, on the south by Massachusetts, and on the west by New York. The north line of the state runs upon the parallel of latitude 45» north. Tins line was first surveyed by commissioners appointed by the provinces of New York and Canada, in the year 1767. Jt was afterwards run, but very erroneously, by I. Collins and I. Carden. in 1772. In 180.6, Dr. Samuel Williams made some observations with the view of ascertaining the true north lineof the state, and still further observations were made ia 1818, by Messrs. Hassler and Tiarks, sur- veyors under the treaty of Ghent. Ac- \\ v i)f the University. Hut the oppoilu- UvoraMc.the sun being hid by clouds „.-alcr part of the eclipse. Of the be- ginning he had a tolerable observation, and from this alone he carefully calculated the longitude by I>r. BowdiUh's piecept.s, and the result waa 73u 10' 30,J for the longitude of the University , or about 4m. less than was obtained from the preceding obser and, as he is inclined, from other cir think it as near an npprcxi to the loo giiudo as any yet obtained, lie has adopted it io tlii* work. NATURAL HISTORY OF VERMONT. Part I. cording to the latter, the -15th parallel lies a little to the southward of the line pre- viously established, but it is not yet finally settled. The eastern boundary was t s- tablished by a decree of George III, July 20th, 1764, winch declared the western bank, of the Connecticut river to be the western boundary of New Hampshire". The southern boundary is derived from a royal decree- of March -1th, 1740, and was surveyed by Richard Hazcn, in Feb- ruary and March, 1741 . This line, which was the divisional line between Massachu- setts and New Hampshire, was to run due west from a point three miles to the north- ward of Patucket falls, till it reached the province of Now York. It was run by the compass, and ten degrees allowed for westerly variation of the magnetic needle. This being too great an allowance, the line crossed the Connecticut river 2' 57" to the northward of a due west line. In consequence of this error, New Hamp- shire lost 59,873 acres, and Vermont 133,- 897 acres, and the south line of the state is not parallel with the north line. The western boundary was settled by the gov- ernments of Vermont and New York at the close of their controversy, in 1790. This line passes along the western boun- daries of the townships of Pownal, Ben- nington, Shaftsbury, Arlington, Sandgate, Rupert, Pawlet, Wells and Poultney, to Poultney river ; thence along the middle of the deepest channel of said river, East bay and lake Champlain to the 45th de- gree of north latitude, passing to the east- ward of the islands called the Four Broth- ers, and to the westward of Grand Isle and IslelaMotte. The portion of this line between the southwest corner of the state and Poultney river, was surveyed in 1813 and 1814, and the report and plan of the survey are in the office of the Secretary of State at Montpelier. Extent and Area. — The length of Ver- mont from north to south is 157 A miles, and the average width from east to west 57A miles, which gives an area of 9,056 -}- square miles, or 5,795,960 acres. The length of the north line of the state is 90 miles, and of the south line 41 miles, but, on account of the great bend of the Con- necticut to the westward, the moan width of the state is considerable less than the mean between these two lines, as above stated. The width of the state from Rarnct to Charlotte through Mont- pelier, which is 50 miles nearer to the northern than to the southern boundary, is only about 60 miles. On account of the irregularities in the western and east- ern boundaries, bol ii these lines are lon- ger than the mean 1 ingth of the state, the former being about 175 miles, and the lat- ter, following the course of the Connecti- cut, 215 miles.'- The state is divided into two equal parts by the parallel ut' 4-ld. 9m. north latitude, and also by the meri- dian in Id. 19m. of east longitude. These two lines intersect each other near the' western line of Northfield, and about 10 miles south westerly from Montpelier, and the point of intersection is the geogrujihi- cal cadre of the stale. Divisions. — The Green Mountains ex- tend quite through the state from south to north, and, following the western range, divide it into two very nearly equal parts. These form the only natural division, with the exception of the waters of lake Champlain, which divide the county of Grand Isle from the counties of Franklin and Chittenden, and the several islands which compose that county, from each other, and from the main land. For civil purposes the state is divided into 14 coun- ties, which are sub-divided into 245 town- ships, and several small gores of hind, which are not yet annexed to, or funned into, townships. The names of the coun- ties, the date of their incorporation, thu shire towns, and the number of towns in each county at the present time (1842,) are exhibited in the following table : CniP. L DESCRIPTIVE GEOGRAPHY. KiCK OF THE COUNTRY. MU.NCH'AI. SUMMITS. D I A G It A M %%\Ofthe relative, altitudes of some of the principal Heights in Vermont ahure the sen. I. or Worth I'otik. ofAUi 107tl i i -ll.St t'ui.ic-1's Hump, -- i.tOau'Plirowsbury Mountain, ■J«J83iTJin None, or South Peak ulWIunalielJ M. J924 Killiiigton Peak, ■ 3700 Equinox Mountain, Manchester, Ascatnoy Mountain, # 20G3 Middleuury turnpike 19 J-2,Poru turnpike, loe:! Kcyo* lumjtiko, - 951 Summit levolnt Roxlmry, . . . .— SOS Summit level at Williainatownj — 791 Manchwter villiugo 48.1 Montpelier villiago, 430 Norwich University, - 370iUuiv(irsity of Vermont, .... — 00;Sur face of Lake Champiain, • •==z -.*0» >-~V,-?.,r,--^£2^ Section II. Face of the country. Mountains — Tlie surface of Vermont is generally uneven. A few townships along the margin of lake Champiain may be called level j but with these exceptions, the whole state consists of hills and val- leys, alluvial Hals and gentle acclivities, elevated plains and lofty mountains. The celebrated range of Green Mountain;', which give name to the state, extends quite through it from 6outli t< . north, keep- ing nearly u middle course between Con- necticut river on the east and lake Cham- plain on the west. From the line of Mas- sachusetts to the southern part of Wash- ington county, this range continues lofty, and unbroken through by any considera- ble streams; dividing the counties of Windham, Windsor and Orange from the counties of Bennington, Rutland and Ad- dison. In this part of the state, the com- munication between the eastern and west- ern sides of the mountain was formerly dillicult, and the phrase, going urn- tlu ■iiiouutain, denoted an arduous business. But on account of the great improvement of ]" mint on, ul.cn is, if tli rue arc a 1 )f(>i MS iu in t to commit ition, e ie ivo ilrl tin i' i ink- *'A as thee ightli. ■ of the roads, more particularly in their more judicious location near the streams, the dilriculty of crossing the mountain has nearly vanished. In the southern partof Washington count}', the Green Mountains separate into two ranges. The highest of these ranges, bearing a little east of north, continues along the eastern boundaries of the counties of Chittenden and Franklin, and through the county ol Lamoille to Canada line ; while the other range strikes oil' much more to the east through the southern and eastern parts of Washing- ton county, the western part of Caledonia county and the north western part of Es- sex county to Canada. This last, is called the height of lands, and it divides the waters, which fall into Connecticut river, in the north part of the state, from those which fall into lake CJiamplaih and lake Meinphrcmagog. This branch of theGreon Mountains, though it no where rises ko high as niauy points of the western branch, is much more uniformly elevated : yet the acclivity is so gentle as to admit of easy roads over it in various placi s. The western range, having been broken through by the rivers Winooski, Lamoille and Missisco, is divided into several sec- tions, these rivers having opened passa- ges for good roads along their banks, while NATURAL HISTORY OF VERMONT. Chap. I. MOUNTAINS. KIVI'.US AMI STKKAM3. the intervening portions are so high and eteep as not to admit of roads being made ov^t' them, with the exception of that por- tion lying between the Lamoille and Mis- b'isco. This part of the Green Mountains presents some of the . most lofty summits in the state ; particularly the Nose and Chin. in Mansfield, and Camel's Hump in Huntington. These, together with other important mountains and summits in the Btate, are exhibited in the foregoing table and cut, and will also be described in the Gazetteer, under their respective names. The sides, and, in most cases, the sum- mits of the mountains in Vermont, are covered with evergreens, such as sprace, hemlock and fir. On this account the French, being the first civilized people who visited this part of the world, early gave to them the name of Verd Mont, or Green Mountain ; and when the inhabi- tants of the New Hampshire Grants as- sumed the powers of government, in 1777, they adopted this name, contracted by the omission of the letter d, for the name of the new state.* * This name is said to hnvo been adopted upon the recommendation of Dr. Thomas Young — (see part 2d, page lOti.) The following account of die Christening of the Green Mountains, is given by the ltev. Samuel Peters in his life of the Rov. Hugh Peters, published ul New York in lbOT. " Veid-Mont was a name given to the Green Mountains in October, 1763, by the Rev. Dr. Peters, the first clergyman who paid a visit to the 30,000 settlers in that country, in t he presence of Col. Taplin, Col. Willes, Col. Peters, Judge Pe- ters and many others, who were proprietors of a large number of townships in that colony. The ceremony was performed on the top of a rock standing on a high mountain, then named Mount Pisgah because it provided to the company a clear sight of lake Champlain at the west, and of Con- necticut river at the east, and overlooked all the trees and hills in the vast wilderness at the north and south. The bapiism was performed in the following manner: Priest Peters stood on the pinnacle of the rock, when he received a bottle ot spirits from Col. Taplin ; then haranguing the company with a short history of the infant settle- ment, and the prospect of its becoming an impreg- nable barrier between the British colonies on the south and the laie colonies of the French on the north, which might be returned to their late own- ers for the sake of governing America by the dif- ferent powers of Europe, he continued, ' We have here met upon the rock Elain, standing on Mount Pisgah. which makes a part of thetvei lasting hitl,the spine of Asia, Afi icaand Anieri(:a,holding together tlie terrestrial ball, and dividing the Atlantic from the Pacific ocean — lo dedicate and consecrate this extensive wilderness to God manifested in the flesh, and to give it a new name worthy of the Athenians and ancient Spartans, — which new name is Verd Mont, in token that her mountains and hills shall be ever green and shall never die.' Rivers and Streams. — The rivers and streams lying within the state of Vermont are very numerous, but small. They, in most cases, originate among the Green Mountains, and their courses are short and generally rapid. Connecticut river washes the whole eastern border of the state, but belongs to New Hampshire, the western margin of that stream forming the boundary line between New Hamp- shire and Vermont. The Connecticut re- ceives the waters from 3,700 square miles of our territory. It receives from Ver- mont, besides numerous smaller streams, the waters of the eleven following rivers, viz : Wantasticook, or West, fcjaxton's, Williams', Black, Ottaquechy, White, Ompompanoosuc, Wait's, Wells', Pas- suinpsic, and Nulhegan. Clyde, Barton and Black river run northerly into Mem- phremagog lake. Missisco, Lamoille, Winooski and Poultney river and Otter creek flow westerly into lake Champlain, and the Battenkill and Hoosic westerly into Hudson river. Deerfield river ruii3 southerly from Vermont and falls into the Connecticut in Massachusetts ; and the Coatacook and Pike river head in the north part of the state and run northerly into Canada, the former uniting with Massuippi river at Lenpxville and the lat- ter falling into the head of Missisco bay. All these streams and many smaller ones will be described in the Gazetteer under their respective names. No country in the world is better sup- plied with pure and wholesome water than Vermont. There are scarcely any farms in the state which are not well wa- tered by springs, or brooks; and none, with the exception of those upon the isl- ands in lake Champlain, which are not in the vicinity of one, or more, considerable mill stream. But while Vermont is so abundantly supplied with water, there is, probably, no part of our country in which so little stagnant water is found. The waters of the lakes and ponds are usually clear and transparent, and nearly all the springs and streams are brisk and lively. It is a common remark that the streams in this state have diminished very 'much in size, since the country began to be cleared and settled, and it is doubtless true to some extent. Many mills, which lie then poured out the spirits and cast the bottle upon the rock F.lnni." Thero is no doubt that the name Verd Mont had been applied to this range of mountains long pre- vious to the above transaction, (if, indeed, it evor took place;) hut we do not find that tlie name Verd Mont, or Vermont, was ever applied to the territory generally known as the New Hampshire Grants, previous to tho declaration of the independence of the territory in January, 1777. CuiP. 1. DESCRIPTIVE GEOGRAPHY. I AB I i ANU I'ONtJS. LAKE CilAMI'J-AlJf. formerly had an abundance, have ceased to receive the necessary supply of water during a considerable portion of the year ; and many mill sites, which were once thought valuable, have, from the same cause, become entirely useless. One of the principal causes of this diminution of ou» »trruni!) is supposed to be the cutting down of the forests, which formerly threw off immense quantities of vapor into- the aUnoaphcrc, which was again precipitated Upon the earth in rain and snow. But it u believed that the quantity of water Which annually passes off in our streams ia not t»o much less than formerly as is generally imagined. Before the country waa cleared, the whole surface of the Ft.. oinl was deeply covered with knives, tniiM, and logs, and the channels of all U»r stnallri streams were much obstruct- ed by the asm*. The consequence was, that, when the anows dissolved in the spring, or the raina fell in the summer, the waters were retained among the leave*, or retarded by the other obstruc- tion*, so aa to pass off slowly, and the streams were kept up, nearly uniform as to sire, during the whole year. But since the country has become settled, and the obstructions, which retarded the water, removed by freshets, when the snows melt or the rains fall, the waters run off from the surface of the ground quickly, the streams are raised suddenly, run rap- idly, and aoon subside. In consequence of the water being thus carried off more rapidly, the streams would he smaller than formerly during a considerable part of the year, even though the quantity of water be the same. It is a well known fact that the freshets in Vermont are Snore sudden and violent than when the Country nti new. Tb* watrra of the lake*, ponds and otrram* arr universally soft, mutable with •nop, mud in gr.nrral free from foreign substance*. And the same may be said of most of the springs, particularly on the Greeu Mountains, and in that portion of the state lying east of these mountains. The waters of most of the springs and wells in the western part of the state are rendered hard and unsuitable for Washing by the lime they hold in solu- tion, and there are many springs which are highly impregnated with Epsom salts, and others containing iron, sulphuretted hydrogen, &c. These mineral springs will be described in another place. Lakes and Pomls. Small lakes and ponds are found in all parts of Vermont, but there are no large bodies of water which lie wholly \ ithin the state. Lake Champlain lies bet ,veen this state and the state 'of New York, and more than half o^ it within the limits of Vermont. It ex- tends in a straight line from south to north, 102 miles along the western boun- dary, from Whitehall to the 45th degree of latitude, and thence about 24 miles to St. Johns in Canada, affording an easy communication with that province and with New York. This lake is connected with Hudson river, at Albany, by a canal t>4 miles in length ; so that the towns ly- ing on the shores of Lake Champlain have direct communication by water with the cities of Troy, Albany, Hudson, and New York, and, by means of the great western canal, with the great western lakes. The length of this lake from: south to north, measured in a straight line from one extremity to the other, and sup- posing it to terminate northerly at St. Johns, is 12G miles. Its width varies from one fourth of a mile to 13 miles, and the mean width is about-l^ miles. This would give an area of JJG? square miles, two thirds of which lie within the limits of Vermont. The waters, which this lake receives from Vermont, are drained, by rivers and other streams, from 4Utid miles of its territory. Its depth is generally sufficient for the navigation of the largest vessels. It received its present name from Samuel Champlain, a French noble- man, who discovered it in the sprimr of 161)9, and who died, at Quebec in 1635, and was not drowned in its waters, as has- been often said.* One of the names giv- en to this lake by the aborigines is said to have been Caniudcri- Guarunte, signifying the mouth or door of the country.! If so, it was very appropriate, as it forms the gate-way between the country on the St, Lawrence and that on the Hudson. The name of this lake in the Abenaqui tongue was Pctawd-lovque, signifying alternate land and water, in allusion to the numer- ous islands and projecting points of land along the lake. Previous to the settle- ment of the country by Europeans, this lake had long been the thorough-fare be- tween hostile and powerful Indian tribes, and its shores the scene of many a mortal conflict. And after the settlement, it continued the same in reference to the French and English colonies, and subse- quently in reference to the English in Canada and the United States. In con- sequence of this peculiarity of its loca- tion, the name of Lake Champlain stands connected with some of the most interest- ing events in the annals of our country; and the transactions associated with the names of Ticonderoga, and Crown Point, See Part II, p. 2. fSpaflonl'sGaz.ofN.Y., p. 03. NATURAL HISTORY OF VERMONT. Part J. MKMl'MIO. BAYS, SWAJIPS, and Pla.ttsbiirglir and many other places, united with the variety and beauty of the scenery, the neatness and accommodation of rile steamboats, and tlie unrivalled ex- cellency of their commanders, render a tour through this lake one of the most in- teresting and agreeable to the enlightened traveller. A historical account of the most important transactions upon Lake Champlain, together with some account of the navigation of the lake, and partic- ularly of the steamboats which have been built upon it, will be found in part second, and a much more minute description of the lake under its name in part third. Memphrcmngog lake is situated on the north line of the state, and about midway between lake Champlain and Connecticut river. It extends from south to north, and is nearly parallel with lake Cham- plain. It is 30 miles long, and the aver- age width about two miles. One third part of this lake lies in Vermont; the oili- er two thirds in Canada. The name of this lake in the Aben ,qui tongue was Mt:m-plow-buuauc, signifying a large ex- panse of water. Tins, together with nu- merous smal! hikes and ponds, which lie wholly within the state, will be described in part third, either under their names, or in the account of the towns in winch they are situated. There is abundant evidence that most of our lakes and ponds were formerly much more extensive than they are at present, and that they have been diminished, both by the deposit of earthy matter brought in by the streams, and !."y the deepening of the channels at then- outlets ; and there is also sufficient proof of the former existence of many ponds in this state, which have long since become bay dry land by the operation of the same causes. Several of these will be pointed out in the descriptions of the rivers in part third, particularly in the description of Winooski river, Rarton river, &.o. Bays. — The shores of Lake Cham- plain are indented by numerous bays, most of which are small and of little con- sequence. Missisco bay is the largest of these, and belongs principally to Vermont, lying between the townships of Alburtvh and llighgate, and extending some dis- tance into Canada. The other bays of most consequence, lying along the east shore of the lake and belonging to Ver- mont, are M'Quam bay in Swanton, Re- lamaqueen bay lying between St. Albans and Georgia, Mallets bay in Colchester, Burlington bay between Appletree point and Red Rocks point, Shelburne bay be- tween lied Rocks point and Pottier's point, Button bay in Forrisburgh, and Kast bay between" We. Lhaven una7 White- hall. Resides these there, are several smaller bays lying along the east shore of Lake Champlain, and a considerable at the south end of Lake Memphremaa„e called Scuth bay. Most of these b;i_ys will lie mure particularly described under their names in part third, and also some of the most important bays lying along the west shore of Lake Champlain, and belonging to New York. Swamps. — These are hardly of suffi- cient importance to deserve a separate no- tice. Though considerably numerous, they are, in genera!, of small extent, and, in meny eases, have been, or may be drained and converted into excellent lands. They are most common in (he northern and northeastern parts of the state. In 'the county of Kssex are several unsettled townships, which are said to be made up of hills and mountains with swansps lying between theni, which ren- der 2hem to a great extent incapable of settlement. There is a considerable tract of swampy land at the south end of Mem- pi. r. mngog lake, and another in rligh ■i:nrri lands, which consist of a dark, deep and fertile alluvial deposit. These intervales arc level tracts lying b lit little higher than the ordinary height of the water in the streams, and are in most cases subject to being flooded, when the water is very high. They were, while in a state of na- ture, covered with a heavy growth of for- est trees, such as oak, butternut, elm, bultomvood, walnut, ash, and some other kinds. Back of these flats were frequent- ly others, elevated a few feet higher, and covered with white pine. Still further back, the land rises, in most eases very gradually, into hills and upland plains, and the soil becomes harder and more gravelly, but very little diminished in richness and fertility. The timber upon these lands, wliich constitute the greater part of tiie state, was principally sugar maple, beech and birch, interspersed Willi bass, ash, elm, butternut, cherry, horn- beam, spruce and hemlock. And still fur- ther hack the lands rise into mountains, which are in general timbered with ever- greens, such as spruce, hemlock and fir. The loftiest mountains are generally rocky nnd the summits of some few of them consist of naked rock, with no other traces of vegetation {ban a few stinted shrubs and mosses; but they are, in general, thickly covered with timber to their very tops. Along the western part of the state, and bordering upon Like Cham- plain, are extensive tracts of light sandy ■oil, which were originally covered with white, pitch and Norway pine, and in the northern part of the state, swamps are numerous which were well stored with tamarack nnd white cedar. A more full account of the native vegetables found in tins slate will be given in a subsequent Chapter. Since the country h.is been oJccrrd, tl„. *.,il he*, in gen.-ral, been fiitnn! tntl'u iciiily free from stone to ad- mit of e*»y cultivation, and to be vitv productive in corn, p rain and grass. With- out manuring the intervales usually pro- duce large crops, nnd are easily cultiva- ted, but these crops are liable, occasion- oily, to be destroyed by floods— the same agency which produces the fertility of the noil on which they grow. All parts are, however, sufficiently fertile amply to re- ward the labors of the husbandman, and ln£, In-i'iiiidij it will o\pre,s our iiiciuiin;' nn;if! I.i i i!j ami intelligibly 10 tlin greater part of our mailers, than any oilier \sn could employ, ll may he derive. Irani inter—within, mid vallis—a. vale, or ralley ; and in it, specific higiiifciUion, it denotes lho.su allu- vial fl.il«, lyii.Salo.i- the ioui-iii:i of si roa.:n, whicl. ha>u hern, or occasionally uie overdnwod in conse- quence of i he risirijjofilie water. For tho use oftli. word in Liiis sunsn, wo have Uie authority of \it, Bulkmin and Hi. Willi., i.s, the historian* of Nun Hampshire and Vermont, nnd other ^ooU vviiters. the farmer who is saving and industrious seldom fails of having his Ham filled with fodder for his horses, cattle and sheep, his granary with corn, wheat, rye, oats, peas and beans, and his cellar with pota- toes, apples, and other esculent vegeta- bles. A sufficient quantity of grain tor the supply of the inhabitants might easily be raised in all parts of the state, yet the greater part, of the lands are better adapt- ed for grazing than for tillage. The hills and mountains, which are not arable on account of their steepness, or rock-;, afford the best of pasturage for cattle and sheep. Of the fruits, nuts, berries, &c, which grow in Vermont, both 'wild and cultiva- ted, a more particular account will be given in a subsequent chapter on the bota- ny of the state. Medicinal Springs. — There are in Ver- mont springs which are more or less im- pregnated with mineral, or gaseous sub- stances, but none which have yet ac- quired a very general or permanent celeb- rity for their curative properties. Along the shore of Lake Chnmplain, in the counties of Addison nnd Rutland, the wa- ters generally are impregnated with Ep- som salts, (sulphate of magnesia). Some of the springs are so highly charged with these sails, in the dryer parts of the year, that a pail full of the water will produce a pound of the salts. They have been manufactured, for medicinal purposes, in some quantities, and, did the price of the article make it an object, they might be made here to almost any extent. The medicinal properties of most of the waters iu this state, which have acquired any notoriety, are derived from gaseous and not from mineral substances. In dif- ferent towns in the northeastern part of the state, are springs of cold, soft and clear water, which are strongly improo- nateil with sail ■tti tntl said to resemble the Harrow-Gate wati rs in England, and those of Ballcastle and Castli'inain in Ireland. These waters are found to be efficacious in scrofulous and many other cutaneous complaints, and the springs at Newbury, Tunbridge, Flard- wick, &C, have been much resorted to by valetudinarians in their vicinity. Of medicinal springs on the we- 1, side of the Green Mountains, those of Claren- don andAlbnrgh have acquired the great- est notoriety. It is now about 1(1 years ince the springs at Clarendon began to d tlii ir immediate neigh- tion has been annually extending, and the number of visiters increasing, till Ihe'y have at length become n place of consider- able resort for the alllicted from various sprm hi y, Sire NATURAL HISTORY OF VERMONT. Part CLARENDON SPRINGS, CLARENDON AND PLYMOUTH CAVE! parts of the country. They are situated in a picturesque and beautiful region, 7 miles southwest from Rutland, and have, in their immediate vicinity, good accommo- dations for 500 visiters. The waters are found to be highly efficacious in affections of the liver, dispepsia, urinary and all cu- taneous complaints, rheumatism, invete- rate sore eyes, and many others, and they promise fair to go on increasing in noto- riety and usefulness. These waters differ in their composition from any heretofore known, but resemble most nearly the •German Spa water. For their curative properties they are believed to be indebted wholly, to the gases they contain. They have been analyzed by Mr. Augustus A. Hayes, of Roxbury, Mass., with the fol- lowing results. One gallon, or 235 cubic inches of the water contained, Carbonic acid gas 46. 16 cubic inch. Nitrogen gas 9.G3 " " Carbonate of Lime 3.02 grains. Murate of Lime ~i Sulphate of Soda V2.74grs. Sulphate of Magnesia ) One hundred cubic inches of the gas which was evolved from the water, con- sisted of Carbonic acid gas 0.05 cubic inches. Oxygen gas 1.50 " " Nitrogen gas 98.45 ■" " The Alburgh springs do not differ ma- terially from the springs at Newbury, Tunbridge, and other places in the north- eastern part of the state, owing their med- icinal properties principally to the sul- phuretted hydrogen gas, which they con- tain. Caves. There are no caves in Vermont which will bear comparison with some of tthe caverns found in other parts of the world, and yet we have several, which )dre deserving the attention of the curi- ous. Those at Clarendon, Plymouth and Danby are the most interesting. The •Clarendon cave is situated on the south- easterly side of a mountain in the wester- ly part of that town. The descent into it is through a passage 2£ feet in diameter and 31 feet in length, and which makes an angle of 35 or 40u with the horizon. It then opens into a room 20 feet lcng, 12£ wide, and 18 or 20 feet high. The floor, sides and roof of this room are all of solid rock, but yery rough and uneven. From the north part of this room is a pas- sage about 3 feet in diameter and 24 feet in length, but very rough and irregular, which leads to another room 20 feet wide, 30 feet long and 18 feet high. This room, being situated much lower than the first, is usually filled witt water in the spring of the year, and water stands in the low- est parts of it at all seasons'.* The Plymouth caves are situated at tha base of a considerable mountain, on the southwest side of Black river, and about 50 rods from that stream. They are ex- cavations among the lime rock, which have evidently been made by running water. The principal cave was discov- ered about the first of July, 1818, and on the 10th of that month was thoroughly explored by the Author, who furnished the first description of it, which was published shortly after in the Vermont Journal at Windsor. The passage into this cavern is nearly perpendicular, about the size of a common well, and 10 feet in depth. This leads into the first room which is of an oval form, 30 feet long, 20 wide, and its greatest height about 15 feet. It appears as if partly filled up with loose stones, which had been thrown in at the mouth of the cave. From this to the second room is a broad sloping passage. This room is a little more than half as large as the first. The bottom of it is the lowest part of the cave, being about 25 feet below the surface of the ground, and is composed principally of loose sand, while the bottoms of all the other rooms are chiefly rocks and stones. The passage into the third room is 4 feet wide and 5 high, and the room is 14 feet long, 8 wide, and 7 high. The fourth room is 30 feet long, 12 wide, and 18 high, and the rocks, which form the sides, in- cline towards each other and meet at the top like the ridge of a bouse. The fifth room, very much resembling an oven in shape, is 10 feet long, 7 wide, and 4 high, and the passage into it from the third room is barely sufficient to admit a person to crawl in. At the top of this room is a conical hole, 10 inches across at the base and extending 2 feet into the rock. From the north side of the second room are two openings leading to the sixth and seventh, which are connected together, and each about 15 feet long, 7 wide, and 5 high. From the seventh room is a narrow pas- sage which extends northerly 15 or 16 feet into the rocks, and there appears to terminate. When discovered, the roof and sides of this cavern were beautifully ornamented with stalactites, and the bot- tom with corresponding stalagmites, but. most of these have been rudely broken off and carried away by the numerous visit- ers. The temperature, both in winter and summer, varies little from 44£°, which s about the mean temperature of the cli- mate of Vermont in that latitude. A few * Williams' History of Vermont, vol. I, p. 29, Chap. 1. DESCRIPTIVE GEOGRAPHY. CLIMATE AND TEMPEKAT URE. M Ml OKI >!.< M, 10 \L JOURNALS rods to the westward of this cavern there is said to be another which is about two thirds as large. Section 111. Climate and Meteorology. Temperature.— /Though situated in the middle of the north temperate zone, the climate of Vermont is subject to very considerable extremes both of heat and cold, and the changes of temperature are often very sudden. The usual annual range of the thermometer, in the shade, is from about 92° above to 22° below zero on Furenhcit's scale, though it is some- times known to rise as high as 100°, and at other tunes to sink as low as 3G°, and cvun to 39° or 40° below zero. But so great a degree of cold as I hut last men- tioned, which is the freezing point of mercury, has not, to our knowledge, been experienced but twice since the means of measuring temperature have been in use in the state, and these were both in the year 1335; the first on the 4th of January, and tin? second on the morning of the 16th of December. The temperature of the 4th of January, as noted at several places in this state, was as follows : Mont- pelier —40", White River -*-40°, Bradford —38°, Newbury —36°, Norwich —36°, Windsor —34°, f lydepark —36°, Rutland —30°, and Burlington — 26° ; and the temperature varied but little from the above at those places on the 16th of De- cember. For some time after the iirst settlement of Vermont the thermometer was hardly known in this part of the country ; and since that instrument has become common, very few meteorological journals have been kept, and those few have not, in general, been kept with suffi- cient care to render them of much value, nor have many of them been preserved in a condition to be accessible to those who may wish to consult them. And hence we possess few accurate data, either for determining the mean annual tempera- ture of the different sections of the state, or for settling the mooted question with regard to a change of climate correspond- ing to the clearing and cultivating of the country. The results of the principal ob- servations, to which we have access, and which have been made in this state, to ascertain the temperature of the months and the mean annual temperature, are contained in the following tables : Rutland Burlington. Windsor. Burlington. MONTHS. Williams. Sunders. Fowler Thompson. 178'*. 1803-8. IS06. 1828. 1832. 1833 1838. 1839. 1840. 1641 January, 18.UU 144* 22,0* 25.0J 19.7 22.8 26.1 IS.6 12.2 2.>.3 February, 16.5 18.9 26.5 31.1 19.3 15.3 12.3 24.2 28.4 19.6 March, 32.0 28.5 30. 3 32.4 30.8 28.2 32.6 36.6 31 .4 25.3 April, 41.0 39.5 38.1 3!) .2 39.4 46.1 35.8 4G.3 47.0 39.1 May, no.o 56 3 57.1 57.6 52.4 57.0 51.7 53.3 57 2 52.8 June, GID 66.6 66 1 69.7 61.3 59.6 68.1 60.7 65 6 67.1 July, 67.5 68.2 63.5 70.1 68.5 66.2 71.8 71.5 71.6 68.9 August, 67.5 67.6 64.3 70.2 63.3 63.3 G7.5 63.3 72 5 70.5 K picmbct 57.0 f)7.1 62 1 GO. 8 58.7 57.2 60.5 GO.G 58.3 61.9 O loUr, II (I 43.2 49.5 Hi. 7 47.7 44.9 46.8 50.8 48 0 15.0 Norcinbcr, 37.0 33.5 36.2 33.9 35.6 34.5 31.3 34.0 35.6 35.3 December, 300 24.7 24. G 29.3 47.6 23.6 43.8 21.7 43.3 19.1 ~43T6 26.2 21 1 2G.4 43.6 434 456 45.7 THT Meteorological observations at W'dliamstown by lion. Elijah Paine MONTHS. 1 829 1830 lTT 1831 10.9 1832 171 1 833 19.3 1834 12.5 1835 TiT) I83G 17.3 1837 ~9?7 1838|1839 23.9 15^3 1640 9.0 1 64 1 January, 21.6 February, 10.9 14.3 14.6 14. G 13.5 26.5 12.6 1(1.5 16.7 9.9 20.8 23.7 15.8 March, 23.5 26.4 26.4 25.4 23.5 27.2 25.1 22.9 23. G 30.0 25 S 26.0 21.1 Apr.l, 36.6 44.6 39.8 41.2 41.7 36.1 34.5 3G.5 31.2 41.2 4d.7 31 7 May, 64.8 49.6 53.2 54.7 48.9 48.0 S1.fi 45 !l 48.5 48.7 51 .7 17.7 June, 58.7 58.9 G4.8 59.3 55.4 57.4 59 4 58 8 (III li 63.0 54.9 63 1 July, 60.2 64. 1 64.4 G3.3 G2.3 G8.2 64 .6 G5.4 61 .2 66.2 G5.2 64.8 G2G August, 60.7 G0.7 G3.G G3.5 59.5 60.5 60.9 57 II 59 8 61.6 61.4 54 G 54.2 64.6 63 '.) September, 47.!) 51 .4 53.0 53.9 52.7 50.0 53 3 52,(1 October, 42.6 44.4 44.6 43.9 1 1 .2 39.7 47.8 34.5 39.0 39.7 45.4 41.9 36 5 November, December, 29.7 38.2 30.9 31.7 29.5 29.6 28.7 30.G 25.3 28.1 3(1 2 20.4 2, .3 24.0 •ToTt" 7. J 39.4 19.7 21.1 ig.o 4(h2~ 13.1 38.8 17.8 14.4 37\5 14.1 21.4 39TT [4072 ill 39.9 21.7 39.5 "Wo Pr. i. 2 10 NATURAL HISTORY OF VERMONT Part i. MEAN TEMiT.KATUKt: AT 1SII KI.I N (i TON AND WILLIAMSTOWN. With the exception of the first three columns in the first of the two preceding tables, the particulars of which are not known, all the means for the months have been deduced from three daily obser- vations, taken at sun-rise, 1 o'clock, P. M. and 9 in the evening. Now, as the tliree -daily observations at Burlington synchronize for several years with those at Williamstown, the two tables enable us to make a very accurate comparison of the mean temperature of the two places ; and the comparison shows that the mean temperature of Burlington, although sit- uated 22' farthest north, is about 5° wann- er than that of Williamstown, that of the former being 44.0° and the latter 3D.4P. But the cause of this difference is obvi- ous in the location of the two places, Bur- lington being situated on the margin of lake Chainplain, and the place of obser- vation elevated only 250 feet above it, while Williamstown lies among the Green Mountains near the geographical centre of the state, and, the place of Judge Paine's observation, elevated 1500 feet above the lake.* The mean annual temperature of Bur- lington, deduced from all of the 12 years observations in the preceding table, is 44.1?, and from the seven years observa- tions by the author 44.9°, but, as the year LSl-i"i was very remarkably warm, that should, perhaps, be set aside, and the mean of the other six, 41.4°,, taken as prob- ably a fair statement of the mean annual temperature of Burlington. The mean annual temperature of Williamstown, de- duced from the whole of Judge Paine's observations, is 40. o°.. Many perennial springs, and deep wells are found to continue nearly of the same temperature, both in summer and winter, and to be but very little atl'ected by the changes of temperature which are constantly going on at the surface of the earth ; the temperature of these may, therefore, be regarded as a pretty fair in- dication of the mean annual temperature of the climate. The temperature of a well 40 feet deep, belonging to Mr. Sam- uel Reed, in Burlington, has been ob- served and noted during the year 1841 as follows, the first number after the day of the month being the depth in feet to the surface of the water at the time of the observation: Jan. 1, 14 — 4GU, Feb. 12, ]8— 44.J°, April 14, 16—44°, Junel, 10— 44°, July 20, 10— 46£Q, and Dec. 8, 20— 45^°, giving a mean of 45.1°, or .3° higher than that deduced from the daily obser- vations. Winds. — For small sections of country the prevailing winds usually take their direction from the position of the moun- tains and valleys. That is veiyjmuch the case in Vermont. Through the valley of the Connecticut and of lake Chainplain the winds usually blow in a northerly or southerly direction, while easterly and westerly winds are comparatively of rare occurrence. In the valley of lake Cham- plain east winds are exceedingly rare, as will be seen by the following tables.* Along our smaller rivers, particularly the Winooski and the Lamoille, the prevail- ing winds are from the northwest. The following tables contain 'the result of observations made at Burlington, for leven years, d at Rutland for one year. In the journal kept by the author at Burlington, and from which the ta- bles on Ihe following page were copied, tliree observations of wind and weather were entered each day, which synchro- nize with the observations of tempera- ture for the same years in the preceding table, on the ninth page. The following table contains the results of five years observation at Burlin< by Dr. Saunders, and one year at Rutland, by Dr. Williams. Place. I Time. INo.Obs.l n |ne| e Is k| s Iswlw I hw I fair, jelody Burlington! 1S03— si 1682173911191 lW 25 431 18 1025 1 676 Rutland | J 7811 | L095|153|13|16|76|272|I82|125|256I| 45i»| 64:5 rain snwifogl hunt o,;i 127 19 i * The author has in journal kept ut 11 y<: s possession a meteorologi- [iark by l»r. Ariel Hiutioon, I iu 1 1 o< 1 of 9 years, of which ho hud intended tu inrtcrt an abstract; but, finding the thrco daily ob- seivations to have been made too near iho warmest part of the day to furnish the truo moan tempera- tureof the 24 hours, and consequently unsuitable for comparison with the other tallies, ho concluded in. i to insert it. In order in render meteorological observations of service in determining the relative temperature of places, uniformity in the method of ol'thji renders a great part if the journals which have been kept nearly useJoa * Alth iugh, nt Burlingto 1, w e sel, wind Inn i the east snlliciei lly h rung vanus upi , nui .-hi relies, it t line tier part of the i ight and morning, when the weather i s lai -, to breeze fr< in the en st, which is do iMI. by the ro ling dow i of the c ild a r ito tains to supply tl e rareltict other win Is, it is 1 1 icily ;i what ocr.i 1- 111 1 we ■ii ihc lio| are local mil limit it ti nn tl a dilt'ereii illloi'lio i, as in. In died by 1 Clouda in ^ioiis ol tl euti losph DESCRIITIVE GEOGRAPHY 11 METKOUOLOGICAL TAKI.E. IlEl: AT BURLINGTON. « 1 !i 1 1 1 1 too»n!-.ooooo— icco CO 1 1 -S 1 w cr co /.'to i^ TrTo~t^~tOCo"o— j .' CM ~ob • - -= 1 ri im i> c r-. d i: co o - t cm « oo to CCCOi-Kr-HTOCCC-.M C. K Ol r- n ?1 M H U W T « 1^ o CO II l.O r/_ CO ~. ■= oo o» CC CO Oi l.O J- 1 CM CM r-i i— 01 r^ i- (M T -V CO j-i c» <^ r. ?: Of t — a co a to oo 3 1 o» r — co- io io «^ -a -o rr ~ a. i iO i.O tO IO to i0 <- <-.<0 -^ CO tji 1 A i\ nnHNlOM IO tD i" rt O O oo z 1 CO i-i t^ CO "T< Xj CM i-i T CM 0) -r j r-i .0-) i-i ■- CM i— ':o * i 00 CM CM CM ift to 00 coy CM CO C i 1- * 1 O.i CO 10 o ^r to o to TT CO 10 '-. g i c f r. tt c n ot O! ^ m n ;» CO e i 10 CO CO to O CI CO J! C CO C 10 H — T X ~J CO 00 T C i^ 1- (- (~ m « k ^r co m io io co co cm cm TJ< «l c-i -r i— oo co - .to co c; -t r. - -a-coCMCMco-^'CO'^'Trcoi-^-^i 5 a i (OHlsCnOKUiONHO o 1^ S 1 I--. T CM CM LO 1-- CO CO' 1> O CM r-i -— « i Cnnmncinoo o co o CO CO « i ^-iC-^rHOCOi-l^-O^-lOr-l oo S 1 R 1 COOCOC01.-*1 io ic"^ o -v t» o Co ■<* co 1^ CO CI CM 0 1 n CM — n Ol i— CM CM "of- CM 3 1 * 1 CNritOrtC-lTOCOOIMTrCl CO — / i- -: - :i / — oo / i io 2>| rS. ■*? co CM CM CM CO CO CO CM CM IA\ 1 f-crtonowcoocioM o II co t co c c: c co co c co c co co cr_. co co co co co co co co co co CO I | -j u. ~ < ~ -.-.<•/. c ig --1 r- II - -a >- co i> '- ,>' co'-'c.- > ° -: u. ~ < ^ -. -= < k oy, Q o at U H < s 1 - i i M«SI« SOOOCOW-W <• 1 1 OOi'CNMSiOni'OC s g •: 1 2-1 i0 CO CM O /- — /. CO i0 CO T o - «- co to to c. t vo — i- -r c» T CO CM " i-i r-i — < Ol r-l T CO II r- t ?: i- = otKi^io-r. W 7i co cm CM in — ■-■ ~ co co cm ll n to to co to co co io cm o o x «r ia ..-. l- to o iw- t- w o o II t -r to to to to i^ nj to i^ co io 1 - a v. 1 1 t- -v o» »o CM w co'o^^CcorcM •*? i, 1 * 1 ClOCO-Ct-COC.KCMCOC) 5 ,'-: '? 1 -i; = :cr,r,;iocH o s oooc-Tncooccn 0:! "I rt^ci---^i-'': -too s - CM- C CI^-lO 1., tt CO r- CO -r i.O T CO -T O) 'O CO 1.0 T CO CM "^r i— coo o T^< T.oTco "eo i>. -* " 1 cKt!cr<«rtO«o:(i' — ;:i s o i-i o ^ o o o co o » OOOOl-iOlOCOr-lOCM^-l 2 - r: : c c ti - ?: ?! - oi ^ ss % cNwnocoor^toouioc -': ■ co so i.O rr ..o co co co -r co co cm s8 - HHOOCh«n(DM /j c; tr c? -^ i.o cO"-r i-i cm c« i- tt 1 ""« •1" 3T| ?. iC § ?. 3 § So co 5. o § S o 2 r11 ^ 5 L: r U L: S i- 2 I; | 1 11 i^<^i to O T CM t£ ■;- tc ao x id c. cm t i.o t- co cm co o -— Vr « « io ^ « o «c*o oi— o z 1 t^CMto-^COOOOOCMCMCOXi io (M CO ■» O l.O O O n M "* 1.0 i.O c 1 « 1 -rc«"^ci- — — co oi co co C J_; — -^ t^ -T~0J CO x w 1 7" 5 1 co or. - _ — oi _ -, :. % co oo i_- =o = _i r. e ~ = -o /. - ffo«;-Ba oso-oo S - "2" » i s S 1 «0«- rirlTTOOOMM CMOOOr-lOt-i.riOOOOO 0^ - C i0 l» c — 0> — — i -? 0> 0) i0 t- CO CO T ^ iT K ?! n tM Ol Tf to CO fc to —i -r co -ii t- co x io t^ io -r CO "3" CO T CO o> CM CO rr -C CO CO lU.lllUl "IA* CO !>. co — CO — CO CO O CO ■— CO c. oo =. cs a r. - r^ o c; c. en 00 CO o 5 o cotcoocoorococroc co CO 00 CO CO CO CO CO CO CO CO CO CO 00 f-l CO A fa S » October, 5.GG 1.40 1.65 4.05 6.01 2.98 0.45 3.76 0.83 •3 November, 4.10 2.17 G.25 3.01 1.91 3.78 2.57 '> gg 2.47 k December, 3.49 2 3G 1.G5 2.27 1.59 0.92 2.G8 2.41 3.02 a Total, 41.17 29.18 43.30 39.59 49.21 30.83 27.99 :S7.28 32.71 ■S The depth of water, which falls during a rain storm or thunder shower, is much less than people generally suppose. A fall of 4 or 5 inches during a severe thun- der shower would not be thought at all extravagant by persons who have paid no attention to the accurate measurement of the quantity which fell. But during the seven years observations at Burlington contained in the above table, the depth of water which fell in one shower has nev- er exceeded two inches, and the whole amount in 24 hours has, in only one in- stance, exceeded three inches, and that Was on the 13th of May, 1833, when the fall of water was 3.54 inches. Snow. — For more than three months of the year the ground is usually covered with snow, but the depth of the snow, as. well as the time of its lying upon the ground, vary much in the different parts of the slate. Upon the mountains and high lands, snows fall earlier anil deeper, and lie later in the Spring than upon the low lands and valleys, anil it is believed that they fell much deeper in all parts of the state, before the country was much cleared, than they have for many years past. As little snow falls at Burlington, probably, as at any place in the state. The following table exhibits the amount at this place for the last five winters : Fa I of Snow at Bui ling ton in the winters of 1837-8. Inc. 1838 -'9. Inc. 1839- -'40. Inc. 1840-1. Inc. 184l-'2. Inc. Nov. 9, 2 Oct. 29, 1 Nov. 0, 2 Oct. 26, n Oe.t. 8, 2 " 26, b Nov. 7, 3A u 9, h Nov. 22, 7 " 26, 3* Dec. 10, 3 " l!», o Dec. n, 3 " 26,27, 34 " 29, 3 11, 1 " 28, o " 16, 9 Dec. 7, 6 Dec. 2, 1 " 18, 3 Dec. 7, A u 17, 1 " 22 3 " 14, 15 » 28, 1 " 17, 1 " 28, 5 " 27, 8 " 16, Jan. 15, 1 " 1-, 4 " 29, 4 Jan. 2, 10 Jan. 0 " 19, 2 " 23, G Jan. 5, 4 "6, 11, 5 " 9. 0 " 28, 12 " 29, 1 " 15, H (i 22 25 8A " 27 3 Feb. 11, h Jan. 4, 1 « 23, 6 30, Feb. 17, 15 " 13, 3 " 5, U Feb. 26, 1 Feb. 2, 2< u 00 1 " 17, 8 " 28, 1 Marcl i 7, 1 " G, 10, 41 " 26, 4 " 22, 1 Feb. 2, 1 " 10, 9 " 17,27, March 7, 5 March, 6, G " 8, 2 " 24, 7 March 7, 5 " 15, 1 " 21, 1 " 27, 4 9, 4 " 26, " 28, 2 Marcl 3, 1 " 29 " 30, 3 " 19, 5 Apr. G,13, 2 April, 2, 1 April 13, 3,1 " 22 92A 64 60 1 41 I 48 Chap. 1. DESCRIPTIVE GEOGRAPHY. 13 SLEIGHING PEAIIANCKS OK IilKDS AND HLOSSOMi In 1838-'0, sleighs run from December 23, to January 8, but tliere was no good sleighing during the winter. In 1839-40 sleighing was excellent from December 1m', to February 5, fifty one days. In 184U- '-11, sleighs run from November 22, to November 20, and from December 7, to December 12, but the sleighing was not good. From December 27, the sleighing was good till the 8th of January, after which there was no good sleighing, al- though sleighs continued to run till the 20th of March. In 1 841-'2, sleighing tol- erable from December lri, to January 20, after (hat no good sleighing though sleighs run at several periods for a few days at a time. The deepest snows, which fall in Ver- mont, arc usually accompanied by a north or northeasterly wind, but there is some- time! a considerable fill of snow with a northwesterly, or southeasterly wind. A long continuance of south wind usually brings rain, both in winter and summer. Although snows are frequent in winter and rains in summer, storms are not of long continuance, seldom exceeding 24 hours. Storms from the east, which are common on the sea board, do not often reach the eastern part of this slate, and on the west side of the Green Mountains they arc wholly unknown, or rather, they come to that portion of the country from « northeastern, or southeastern direction. Thunder showers are common in the months of June, July and August, but •cldotn at other seasons. They usually come from the west, or southwest, but are not often violent or destructive, and very little damage is ever done by hurricanes or hail. The crops oftener suffer from an excess, than from a deficiency ,of moisture, though seldom from either. Seasons. — During the winter the ground is usually covered with snow, seldom ex- ceeding one or two feet deep on the low lands, but often attaining the depth of three or four feet on the high lands and mountains. The weather is cold, and, in general, pretty uniformly so, with occa- sional snows and driving winds, till the beginning of March, when with much boisterous weather there begin to appear some slight indications of spring. About the 20th of that month the snows begin to disappear, and early in April the ground is usually bare. But the snows fall some weeks earlier and lie much later upon the mountains than upon the low lands. The weather and state of the ground is usually such as to admit of sowing wheat, rye, oats, barley and peas, the latter part of April. Indian corn is commonly planted about the 20th of May, flowers about the 20th of Jul}', and is ripe in October. Po- tatoes are planted any time between the 1st. of May and the 10th of June. Frosts usually cease about the 10th of May and commence again the latter part of Sept., but in some years slight frosts have been observed, at particular places, in all the summer months, while in others, the ten- derest vegetation has continuedgreen and flourishing till November. The observa- tions contained in the following table will afford the means of comparing the springs of a few years past. They are gathered from the Meteorological journal kept by the author at Burlington : 1 Bobim Bong Uiirn Gurr ill i R.id 1'lum I'liitn and Grab Common 1 tut- it. Sparrow! Swallow* Uloss Ulll. Ulosaom. Cher les Apple Apple \ Ml MIOO. teen. liloss Ulll. Blossom. Blossom. Iftfe April 28 May [) May 12 May l(i IMS. » 23 " 1) May 12 u k; " 22 1838 Mar. 2T. Mar. 8S " 20 " 12 " 14 " 20 Mav 21 June 3 lwnn • •• 23 " 2d it 21 " 4 »■ 7 it 12 » 15 May 18 1837 " 2<> » 23 " 30 " 1G " 19 " 28 " 30 June 2 1838 it o;{ » 31 May 2 " M " 22 " 26 June 1 ii 9 is:*:) it 25 " 25 April 20 " 4 " 12 ii 14 May 22 May 26 1840 " 15 it 2i « 21 " 3 « 12 ii 17 " 20 " 23 1*41 " 27 it 07 " 27 " 23 " 25 ti 26 ii oil " 31 Vegetation, upon the low lands and along the margin of the lakes and large streams, is, in the spring, usually, a week or ten days in advance of that upon the high lands and mountains ; but frosts usu- ally occur, in the fall, earliest upon the low lands, allowing to each nearly the same time of active vegetation. The low lands, however, enjoy a higher tempera- ture, and bring fruits and vegetables to maturity which do not succeed well upon the high lands. To the above remark, with regard to early frosts, there are sev- eral exceptions. On the low islands and shores of lake Cham plain, vegetation is frequently green and flourishing long after the frosts have seared it in other parts of the state, and, along several of the rivers, 14 NATURAL HISTORY OF VERMONT. Part I. Ol'l.NKSO AM) (LOSir LAKE CHAM I' LA IN. MSAIM'K AI1ANC : >>' T1IK 1CJ vegetation is protected by the morning fogs for some time after its growth lias been stopped upon the uplands. The early part of the autumn is usually pleas- ant and agreeable and the cold advances gradually, but as it proceeds the changes become more considerable and frequent, and the great contrast between the tem- perature of the day and night at this sea- son render much precaution necessary in order to guard against its injurious effects upon health. The ground does not usu- ally become much frozen till some time in November, and about the 25th of that month the ponds and streams begin to be covered with ice, and the narrow parts of lake Chainplain become so much frozen as to prevent the navigation from White- hall to St. Johns, and the line boats go in- to winter quarters, but the broad portions of the lake continue open till near the first of February, and the ferry boats from Bur- lington usually cross till the first of Jan- uary. The following table contains the times of the closing and the opening of the broad lake opposite to Burlington, and when the steamboats commenced and stopped their regular trips through the lake from Whitehall to St. Johns, for sev- eral years past : Lake Lake Mncboats Line Cliampl'n Chnmpl'p comene'd Boats Year. closed. opened. running. s topped. 1816 Feb. il 1817 Jan. 20 Apr. 16 1818 Feb 2 Apr. 15 1810 Mar. 4 Apr. 17 Apr. 25 1820 C Feb. 3 I Mr. 8 Feb. Mar. 12 1821 Jan. lf> Apr. 21 1822 Jan. 2-1 Mar. 3D 1823 Feb. 7 Apr. ;") Apr. 15 1824 Jan. 22 Feb. 11 1825 Feb. !> 1826 Feb. 1 Mar. 24 18*27 Jan. 21 Mar. 31 1828 not ulos'd 1829 Jan. 31 Apr. Apr. 6 1830 1831 Apr. 11 1832 Feb. 6 Apr. 17 Apr. 23 1833 Feb. 2 Apr. 6 Apr. 8 1834 Feb. 13 Feb. 20 Apr. 4 Dec. 5 1835 f JanlO \ Feb 7 Jan. 23 Apr. 12 1 1 Apr. 21 Nov. 29 1836 Jan. 27 Apr. 21 Apr. 25 Nov. 2!) 1837 Jan. L~> Apr. 26 Apr. 29 Dec. 10 J 838 Feb. 2 Apr. 13 Apr. 19 Nov. 26 1830 Jan. 25 Apr. 6 Apr. 1 1 Nov. 28 1840 Jan. 25 Feb. 2l) Apr. 11 1841 Feb. 18 Apr. J 1 Apr. 28 Dec. 1 18421 not ckw'd Apr. 13 It frequently happens that the ice con- tinues upon the lake for seme time alter the snows are gone in its neighborhood and the spring considerably advanced. In such seasons the ice often disappears very suddenly, instances having been observed of the lake being entirely cov- ered with ice on one day and the next day no ice was to be seen, it all having dis- appeared in a single night. People m the neighborhood, being unable to account for its vanishing thus suddenly in any other way, have very generally supposed it to sink. This opinion is advanced in the account of this lake contained in Staf- ford's Gazetteer of New York, and the anomaly is very gravely attempted to be accounted for on philosophical principles. Rut the true explanation of this phenom- enon does not require the absurdity of the sinking of a lighter body in a heavier. It is a simple result of the law by which heat is propagated in fluids. That bodies are expanded, or contracted, according to the increase or diminution of the heat they contain, is a very general law of nature. Fresh water observes this law, when its temperature is above 40°, but below 40° the law is reversed, and it expands with the reduction of temperature. When winter sets in, the waters of the lake arc much warmer than the incum- bent atmosphere. The surface, therefore, I of the water communicates, its heat to the atmosphere, and, becoming heavier in consequence, sinks, admitting the warmer water from below to the surface. Now since heat is propagated in fluids almosten- tirelybythe motion of the fluids, this cir- culation will go on, if the cold continues, till all the water from the surface downward to the bottom is cooled down to the tem- perature of 40°. It will then cease. The colder water now being lighter than that below, will remain at the surface and soon be brought down to the freezing point and congealed into ice. This accounts for the ioe taking soonest where the water is most shallow, and also for the closing of the broad parts of the lake earliest in those winters in which there is most high wind, the process of cooling being facilitated thereby. After the ice is formed over the lake, and during the coldest weather, the great mass of water, after getting a i'rw inches below the ice, is of a temperature 8" above the freezing point. While the cold is se- vere, the ice will continue to increase in thickness, but the mass of water below the ice will be unaffected by the tempera- ture of the atmosphere above. Now the mean annual temperature of the climate in the neighborhood of lake Chainplain Chap. 1. DESCRIPTIVE GEOGRAPHY. 15 JIIKMATIUN OF ANCHOR-ICE. SMOKV ATMOSI'l|]:UE. LAKt DAYS. does not vary much from 45°, and this is about the uniform temperature of the earth at some distance below the surface. While then the mass of the waters of the lake is at 40*, and ice is forming at the toj>, the earth, beneath the water, is at the temperature of 45°, or r>u warmer than the water. Heat will, therefore, be constantly imparted to the water from beneath, when the temperature of the water is less than 45°. The only effect of this communica- tion of heat to the water from beneath, (luring the earlier and colder parts of the winter, is to retard the cooling of the lake and the formation of ice upon its surface. Bat after the cold abates in the end of winter uud beginning of spring, so that the lower parts of the ice are not affected l.y the frusta from above, the heat, which i» communicated from In-low, acts upon the under surface of the ice, ami, in con junction with the sun's rays, which pass through the transparent surface and are intercepted by the more opaque parts below,* dissolves the softer portions, rendering it porous and loose like wet snow, while the upper surface of the ice, hardened by occasional frosts, continues comparatively more compact and firm. In this state of things, it often happens that, by a strong wind, a rent is made in the ice. The waters of the lake are immedi- ately put in motion, the rotten ice falls in- to small fragments, and, being violently agitated, in conjunction with the warmer water beneath, it all dissolves and van- ished in the course of a few hours. There is one phenomenon, which is of common occurrenncc in many of our streams, during the coldest part of win- ter, siid which may not at first appear !•■«. n< liable with what has been said •l«.tc, and that is, the formation of ice Baton the (tone* ut the bottom of the »'m «ii,p, uiiul!y called anthor ice. Au- thor lea »• formed at falls and places where tin- current is so rapid that ice is not formed upon the surface. In the case of running wnter, and particularly where the water is not deep and the current rapid, over a rough bottom, the tempera- ture of the whole mass is probably reduced nearly or tV of the heavens. Its np. |»4rrnt diarnet'-r was about 'JO', or two «*.-.f •?» that of the moon, and the color of Hs i-,'M »»»»<■!> white and dazrlmg, like Uut at iron m a fornarr in a state of fu- •*••. It left a long train of light behind it, sad just at the tune of disappearance a violent scintillation was observed, and the fragments detached continued luminous at considerable distance from the main body of the meteor, hut no meteoralites are known to have fullen. Five or six minutes after the disappearance of the mrtcor, a very distinct report was heard accompanied by a jarring of the earth, like the report of a cannon at the distance of five or six miles. Now, assuming the correctness of the above data, and that the report was given at the time of the scintillation, the distance of the meteor was then between 70 and 80 miles, and its diameter about one third of a mile. Another, and still more remarkable me- teor, was seen frcn this state as well as from the rest of New England, and from New York and Canada, about JO o'clock in the evening of the 9th of March, 1822. From observations made at Burlington and Windsor, Prof. Dean computed its course to be S. 35° W., its distance from Burlington 59 miles and from Windsor 8:? miles, and its height above the earth about 37 miles when it first appeared, and when it disappeared its distance from Burling- ton was 144 miles and its distance from Windsor 133 miles and its height 29 miles. According to these computations, at the first appearance of the meteor, it was ver- tical over the unsettled parts of Essex county in the state of New York, and at its disappearance, it was over the western part of? Schoharie county in the same state. Several other meteors of this kind have been observed, the most remarkable of which was seen from the northern part of the state and from nearly the whole of Lower Cunada, about 4 o'clock in the morning of the 28th .of May, 1634. It be- ing a time when people generally were in bed and asleep, comparatively few had the opportunity of seeing it. Many, however, were awakened by its light, and still more by its report. Residing then at Hatley in Canada, which is 15 miles north of the north line of Vermont at Derby, we were suddenly awakened by a noise resembling that of a large number of heavy carriages driven furiously over a rough road or pavement, and by a shaking of the house, which caused a rattling of every door and window. Supposing it to he an earth- quake, we sprung out of bed and reached the door two seconds at least before the sound ceased. The atmosphere was calm and the sky was perfectly clear, with the exception of a narrow train of cloud or smoke, extending from southwest to north- east, and at considerable distance to the northward of the zenith. It was nearly motionless, and was apparently at a vastly greater height than clouds usually lie. Indeed there was something so peculiar in its appearance as to make it the sub- ject of remark and careful observation till after sunrise, when it gradually vanished, although at this time we had no reason to suspect its connexion with the noise and shaking of the earth, which had awaken- ed us. We, however, soon learned thn! a remarkable meteor had been seen, ami that its course lay along the very line oc- cupied by the remarkable cloud above mentioned. From an intelligent young man, who was fishing at the time on Mas- suippi lake in Hatley, and who had a full view of the meteor during the whole time it was visible, we learned that it made its Pt. i. 18 NATURAL HISTORY OF VERMONT. Part J. HEW ENGLAND EARTHQUAKES. AURORA BOREALIS. appearance at a point a little north of •west at an elevation of about 35°, passed the meridian at a considerable distance north of the zenith and disappeared in the northeast with an altitude of about 25°. He thought its apparent magnitude to be 8 or 10 times that of the moon, and that it was visible about 10 seconds. It was of a fiery red color; brightest when it first appeared, and gradually decreased in brill- iancy, all the time throwing oil" sparks, till it disappeared. About 4 minutes af- ter the vanishing of the meteor, a rumb- ling or rattling sound, which sensibly agitated the surface of the lake, com- menced in the point where the meteor was first seen, and following the course of the meteor died away at the point where the meteor vanished. This meteor was vertical on a north and south line, about 50 miles to the northward of Derby in this state, or nearly over Shipton in Canada, and its altitude must have been at least 30 miles, and still the agitation it pro- duced in the atmosphere was such as to break considerable quantities of glass in the windows at Shipton, Melbourne and some other places. The course of this meteor was mostly over an unsettled Country. The most remarkable circum- stances attending this meteor were the train of smoke which it left behind, and the long continued noise and shaking of the earth. Since the settlement of New England, there have been recorded a considerable number of earthquakes, and several have been noticed in Vermont. The sound accompanying these is usually described as having a progressive motion ; and that, and the shaking of the earth have been supposed to be produced by the rushing of steam through the cavities in the interior of the earth, but the effect known to have been produced by the meteor last de- scribed, furnishes strong reasons for sus- pecting that the cause of many, and per- haps of all the earthquakes which have occurred in New England, has been in the atmosphere above instead of the earth beneath. Had this meteor passed with- out being seen, the sound and shaking of the earth, which it produced, would have been regarded as a real earthquake, and its origin in the atmosphere would not have been suspected. Aurora Doreulis. — This meteor has been very common in Vermont, ever since the first settlement of the state ; but in some years it is of more frequent occurrence, and exhibits itself in a more interesting and wonderful manner than in others. Its mostcommon appeal nice is thatof streams of white light shooting up from near the horizon towards a point not far from the zenith; but at times it assumes forms as various and fantastic as can well be im- agined, and exhibits all the colors of the rainbow. It is not uncommon that it takes, the form of concentric arches spanning the heavens from west to east, usually at the north, but sometimes passing through the zenith, or even at considerable distance to the south of it. At times the meteor is apparently motionless, but it is not an un- common thing for it to exhibit a violent undulating motion like the whipping of a flag in a brisk wind. But it is so variable in its appearance, that it is vain to attempt its description. We will, however, men- tion a few of the remarkable occurrences of this meteor which have fallen under our own observation, and some of the at- tending circumstances. On the 12th of October, 1819, at about 7 o'clock in the evening, the Aurora Bo- realis assumed the form of three luminous resplendant arches, completely spanning the heavens from west to east. The low- est arch was in the north a little below the pole star, the second about midway between the pole star and the zenith, and the third 10° or 15° to the southward of the zenith. These bells gradually spread out till they became blended with each other, and the whole concave heavens was lit up with a soft and beautiful glow of white light. It would then concentrate to particular points whose brightness would equal that of an ordinary par- helion, and around them would be exhib- ited the prismatic colors melting into each other in all their mellow loveliness. The motions of the meteor were rapid, undu- latory and from north to south varying a little towards the zenith. The sky was clear and of a deep blue color where it was not overspread by the meteor. It was succeeded in the morning of the 13th by a slight fall of snow with a northwest wind. The aurora exhibited itself in a manner very similar to the above in the evening of the 3d of April, 18:20, and sev- eral times since. But the most remarkable exhibition of this meteor, which has fallen under our own observation, was in the evening of the 25th of January, 1837. It first attract- ed our attention at about half put G o'clock in the evening. It then consisted of an arcli of faint red light extending from the north west and terminating nearly in the east, and crossing the meridian 15 or 20° north of the zenith. This arch soon assumed a bright red hue and grad- ually moved towards the south. To the northward of it, the sky was nearly black, in which but few stars could be seen. Next .? Chap. 1. DESCRIPTIVE GEOGRAPHY. 19 AURORA BOREALli MAGNETIC VARIATION. to the red belt was a belt of white light, and beyond this in that direction, the sky was much darker than usual, but no clouds were any where to be seen. The red belt, increasing in width and brightness, ad- vanced towards the south and was in the zenith of Burlington about 7 o'clock. The light was then equal to the full moon, and the snow and every other object from which it was reflected, was deeply tinged with a red or bloody hue. Between the red and white belts, were frequently ex- hibited streams of beautiful yellow light, and to the northward of the red light were frequently seen delicate streams of blue and white curiously alternating and blending with each other. The most prominent and remarkable belt was of a blood-red color, and was continually va- rying in width and intensity. At eight o'clock, the meteor, though still brilliant, had lo»t moat of it* unusual properties. This meteor, when very brilliant, is usually regarded as an indication of an approach- ing storm, but, like other signs, it often fails. It is most common in the months of March, September and October, but it is not unusual in the other months. Magnetic Variation. — Very few obser- vations have hitherto been made in Ver- mont for the purpose of determining the variation of the magnetic needle, and these few have generally been made with a common surveyor's compass, and, prob- ably, in most cases, without a very cor- rect determination of the true meridian; and hence they cannot lay claim to very minute accuracy. But since such obser- vations may serve to present a general view of the amount and change of varia- tion, since the settlement of the state, we have embodied those to which we have hud access, in the following table. Magnetic Variation in Vermont. 1'luc* uf OUemtion. Dale. Vati. west. Latitude. Lon.w.G'h Authorities. Burlington, 17113 7° 36' 44° 28' 73° Dr. S. Williams. " 1818 7 30 ♦' it J. Johnson, Esq. ti 1622 7 42 " tt " it 1830 8 10 » " " «t isni 8 15 f " » it 183'2 8 25 " " u tt 1834 8 50 f " " tt 1837 8 45 tt ' since 1805, and of 3" previous to that time. And al- though he thought the change of varia- tion may not have been perfectly uni- form, yet he was of opinion that a table constructed with the above variation would not differ materially from the truth. The following is such a table. Magnetic Variation at Burlington. Year Vat.v»iVear. Var.w Year. V 1785 17r<<) 1787 1788 178!) 1790 1701 1792 1793 17IU 1795 1796 1797 1798 1799 7°12'1800 7 9 1801 7 61802 7 31803 7 0 1804 6 571805 6 541806 6 5111807 6 481808 6 451809 6 421810 6 39J1811 6 361812 6 3411813 6 301814 6°27 6 24 621 6 18 6 1 6 12 618 6 24 6 30 6 36 6 42 6 4^ 6 54 7 0 7 6 Year. Var.w Year. 1815 7C12' 1830 1816 7 18 1831 1817 7 24 1832 1818 7 30 1833 1819 7 36 1 834 1820 7 42 1 835 1821 7 48 1836 1822 7 54 IH37 1823 8 0 1838 1824 8 6 1839 1825 8 12 1840 1826 8 18 1841 1827 8 24 1842 1828 8 30 1843 1829 8 36 1844 8°42' 8 48 8 54 9 0 9 6 9 12 9 18 9 21 9 30 9 36 9 42 9 48 9 54 10 0 10 6 20 NATURAL HISTORY OF VERMONT Pakt. I KEMARKABLF, SEASONS. GREAT FRESHET. COMI'AKISON OF CLIMATES. Remarkable Seasons. Although the mean temperature of Vermont has not usually varied much from year to year, yet seasons have occasionally occurred, which hecame, for a time, proverbial on account of their unusual coldness, or heat, or on account of an excess or deficiency of sn,ow or rain. Of the years, which were remarkable .on any of these ac- counts in early times, we have no accu- rate records. But it is universally con- ceded that the year 1816, was the coldest, and perhaps the dryest during the early part of summer, ever known in Vermont, although we have no meteorological ob- servations for that year, and are therefore unable accurately to compare the temper- ature of its seasons with other years. Snow is said to have fallen and frosts to have occurred at some places in this State in every month of that year. On the 8th of June, snow fell in all parts of the State, and upon the high lands and mountains, to the depth of five or six inches. It was accompanied by a hard frost, and on the morning of the 9th, ice was half an inch thick on shallow, standing water, and icicles were to be seen a foot long. The weather continued so cold that several days elapsed before the snow disappear- ed. The corn, which was up in many places, and other vegetables, were killed down to the ground, and, upon the high lands, the leaves of the trees, which were about two thirds grown, were also killed and fell off. The summer was not only excessively cold, but very dry. Very little Indian corn came to maturity, and many families suffered on account of the scarcity of bread stuffs and their conse- quent high prices. The year, 1828, was nearly as remark- able for warmth as 1816 was tor cold. The mean temperature of all the months of this year, with the exception of April, was higher than their average mean, and the temperature of the year 3° higher than the mean of the annual temperatures which have been observed. The broad parts of lake Champlain were not frozen over during the winter. The year 1830 was distinguished on ac- count of the great quantity of water which fell in rain and snow, and especially for one of the most extensive and destruc- tive freshets ever known in Vermont. Up to the 15th of July, the weather was exceedingly cold as well as wet. It then changed, and became suddenly and ex- cessively warm. The following table shows the height to which the ther- mometer rose in the shade, on each day from the loth of July to the 21st, inclu- sive. July 15. Thursday, . . . 94° « Hi. Friday, . , . . 92 " 17. Saturday, . . . 92£ " 18. Sunday, .... 92 " 19. Monday, . ... 90 " 20. Tuesday, . . . 91 " 21. Wednesday, . . 94 Nor was the heat much diminished in the absence of the sun. In some cases the thermometer stood as high as e0° during the whole night, and it sunk but little below 80"" during any part of the time included in the above table. Another such succession of hot days and nights was perhaps never experienced in the state. From the loth up to Saturday the 24th, the weather was for the most part clear and calm. On Saturday afternoon, the rain commenced and continued with only short intermissions, till Thursday following. During the 5 days from Sat- urday noon to Thursday noon, the fall of water at Burlington, exceeded 7 inches, and of this 3 85 inches fell on the 26th in the space of about 16 hours, and this is believed to be one of the greatest falls of water, in that length of time, ever known in Vermont. The VVinooski, which was most affected of any of our large streams, was at its greatest height in the afternoon of Tuesday the 27th, and was then from 4 to 20 feet, according to the width of the channel, higher than had ever before been observed. Although the county of Chit- tenden, and the northern p.1rts of the county of Addison, seemed to be the sec- tion upon which the storm spent its great- est force, yet its disastrous effects were felt with unusual severity throughout the valley of lake Champlain, and in all the northern and central parts of the state, and the destruction of property in bridges, mills, buildings and growing crops was great, almost beyond computation. But its most melancholly effect was the de- struction of human life. By a change of the channel of New Haven river, in the town of New Haven, during the night, between the 26th and 27th, several build- ings containing families were insulated, and afterwards swept away by the waters. Of 21 persons, who were thus surprized and washed away, 7 only escaped ; the remaining 14 found a watery grave." The whole quantity of water which fell at Burlington, in 1830, measured 59.3 in. being half as much again as the mean an- nual quantity, and probably exceeding the amount in any other year since the state was settled. Comparative, view of the Climate. — As Vermont extends through 2° 16' of lati- tude, there is, as might be expected, a * See part III. Article, flew Huvon. Chap 1. DESCRIPTIVE GEOGRAPHY. 21 CLIMATE OF AMERICA AND EUROPE. CAUSES OF DIFFERENCE. sensible difference between the tempera- ture of the northern and southern parts, and there is a difference still more mark- ed between the elevated and mountainous parts and the lower country along our lakes and rivers; but observations are too limited to enable us to form any accurate comparison between the different sections of the state." Between the climate of this Btate and that of those portions of other 8tates, lying in the same latitude, there is no material difference, with the excep- tion, perhaps, of the sea-coast of New Hampshire and Maine, whose mean an- nual temperature may be a little higher. But between Vermont and the countries of Europe, lying in the same latitude, there in a remarkable difference, the tem- perature of the latter being no less than ''iL higher than ours; and there is a hke contrast, increasing towards the north, Uu.cn the whole western coast of Eurvpfl and the eastern coast of North America. This singular contrast was observed by the earliest navigators, who visited the coast of North America, and has since been confirmed by numerous meteorolog- • As llio extremes of host and cold were not ted m ilui preceding meteorological tables, we liavo colluded iu the following table the extronicR of cold which have been entered at sunrise upon journals kept at three different places within the • (at* since 1629. Degrees in all cases below zero. ical observations. A comparison of the journals kept in this country with those kept in Europe shows us that the climate of Vermont, which lies in the latitude of the southern part of France, is as cold as that of Denmark, situated 11 or 12° fur- ther nonh. The following table exhibits pretty nearly the mean temperatures a- long the coasts of the two continents, with the differences, from the 30th to the 6Uth degree of latitude. Tabic. r**r. If lUuil.UUWH. Burlington. llydepark. 1M3 Keh 5. 11° IKW Jan. 31, w ItCll Dec. 9i. 18 Dec. 14° l&M 1 . '.. 94, 99 Jan. 26, 16 i- vl Jan. 19, 96 Jan. 19, 20 Dcc.15, 12° l«t !'«-. 15, Id Jan. 21, 2d li» i • . 4, 91 Jan. 4, 36 It* Peb 9, '-Si Feb. 18, 34 i-vrj J... 4 It*. 11, in l>ee 22, 15 Jin. 20, 34 •«*> IS Jan 91, 13 Feb. 2, 93 i*» J . -> V « , It Jan. 24, 16 leb 10, 22 !**• l«a. le, 17 Jan. la, 16 J Ml »-•*.. », ■ Jan. 4. 10 It ««ill appear from various observations and ciif uminntoi, that during calm weather, when lb* sua doe* not shine, the temperature of vallies and low situations is lower than that of the high lands, but in \iiwly weather and when the sun tbinrs, it is coldest on the high lands. In confir- mation of this statement, in part, wo give the fol- lowing extract of a letter to the author from the Hon. Elijah Paine, of Williamstown, (see pnges 9 an I 10.) " I have found," says he, " that in ex- tremely cold, still weather, the mercury in the ibnuiometer at Burlington, Montpelier, at North- Acid, on Dog river, on the low lands at the mocting-house in this town, at Wood.Hock, Hano- ver, N. if., and even nt Albany, N. Y., has some- limes been 14 degrees lower than in mine. Some- times, even in March, I have found the difference equally great, when the wind was light ami the weather very cool fi.r the. season. But the reverse is the ease in extremely cold, windy weutlior. I bare known my thermometer in such weather 11 degrees lower than tcme of those I have men- tioned." Lat-i Eurove. America. Differ- tuile. Mean 'J emp. Mean Temp. ences, 30 •> 70.1° 66.8" 3.3° 35 66.5 60.5 6.0 40 63.1 54.2 8.9 45 56.8 45.0 118 50 50.8 37.9 12.9 55 46 0 28 0 18 0 60 40.0 18 0 22.0 A contrast so remarkable, as is exhibit- ed in the preceding table, has been the source of much speculation, but, as it ap- pears to us, without throwing much light upon the true cause of the phenomenon. Among the earliest writers who at- tempted to account for it was Father Bres- ani, an Italian Jesuit, who spent most of his life in Canada. He says that " a cer- tain mixture of dry and moist makes ice, and that in Canada there is a remarkable mixture of water and dry san*dy soil ; and hence the long duration of cold and great quantities of snow." To this he adds an- other cause, which is "the neighborhood of the northern sea, which is covered with monstrous heaps of ice, more than 8 months of the year." FatherCharlevoix, who visited Canada in 1720, and from whose travels the forgoing opinions of Bresani are taken, says" that, in his opin- ion," " no person has explained the cause, why this country is so 'much colder than France in the same latitude." "Most writers," he continues, "attribute it to the snow lying so long and deep on the ground. But this only makes the difficul- ty worse. Whence those great quanti- ties of snow?" His own opinion is that the cold and snow are to be attributed to the mountains, woods and lakes. Many European writers have supposed the great lakes, which abound in the country, to be the cause of the coldness of our cli- mate ; while others have imagined that there must be a chain of very high moun- tains in the interior of the continent, run- ning from southwest to northeast, which produce the coldness of our north wester- ly winds. Doct. Dwight supposes these * Charlevoix's Travels in America, Vol. 1. p. 130- 22 NATURAL HISTORY OF VERMONT. Part I. CHANGE OF CLIMATE. CUUKENTS OF THE OCEAN- winds to be descending currents from the higher regions of the atmosphere; and hence their coldness. Doct. Holyoke at- tributed the coldness of our climate to the extensive forests of evergreens. Doct. Williams, the able historian of Vermont, attributed it to the forest state of the country-, and has endeavoured to prove that, eighteen centuries ago, the climate of Europe was even colder than that of America at the present time.* But other writers have, with equal plausibility, shown that no considerable change has taken place in the mean temperature of Europe within that period. f The fact, moreover, that the western coasts of America, which are wholly uncultivated, are very much warmer than the eastern coasts of Asia in the same latitude, which are cultivated to considerable extent, shows that these differences of tempera- ture do not depend upon cultivation, nor, indeed, upon any of the causes which have been mentioned, but upon some more general cause. And this cause, we be- lieve, is to be sought in the inlluence of the ocean upon the prevailing winds in high northern latitudes. We regard the ocean as the great equalizer of tempera- ture upon the surface of our globe — as the instrument for distributing the heat of the equatorial regions towards the poles and bringing thence cold towards the equator, and thus meliorating the climate of both. We look upon it as a truth es- tablished both by theory and fact that there is a general circulation of the wa- ters of the ocean between the equatorial and polar regions— that the warm water from the equator is flowing along the sur- face of the ocean towards the poles, while the colder water from the poles is ad- vancing along the bottom of the ocean to- wards the equator. Such a motion of the waters might be inferred, as the result of the unequal distribution of heat through the oceanic mass, increased by the rota- tion of the earth on its axis. But inde- pendent of this, facts furnish indubitable proof of its existence. The temperature of the earth, at a distance below the sur- face, being a pretty correct index of the mean temperature of the climate, with- out the circulation we have supposed, the temperature of the ocean at consider- able depths, ought, particularly in the warmer parts of the year, to be as high, at least, as the mean annual tem- perature. But on the contrary, observa- tion proves it to be much lower. In lati- tude fciT", where the mean temperature is 39°, Lord Mulp-rave found, on the 20th Willian Hi, i, Vol f Edinburgh Review, Vol. XXX, p. 25. of June, when the temperature of the air was 48£°, that the temperature of the ocean at" the depth of 4081) feet, was 26", or tiJ below the freezing point. On the 3 1st of August, in latitude 6'.)° where the annual temperature is 38°, that of the air being 59£°, the temperature of the water at the depth of 41138 feet was 32°.* At the tropic where the temperature does not vary more than 7° or 8° during the year, at the depth of 3600 feet the tem- perature of the water was found to be on- ly .r):S->, while that of the air was 84°, making a difference of 31°, and indicating a degree of cold in the lower parts of the ocean nearly 25° more intense than is ever experienced in the atmosphere in that latitude, t How else can we account for the coldness of these waters, but by suppos- ing them to come from higher latitudes in the manner we have described ? Of the opposite motion of the warmer waters along the surface of the Atlantic ocean, from the equatorial towards the polar regions, the gulfstream, the currents setting along the western coasts of Nor- way, and the vast quantities of tropical productions, lodged upon the costs and islands of the northern ocean, afford a- bundaut proof. Now this transportation of the colder waters towards the equator and of the warmer waters towards the poles, serves, as already remarked, to mitigate the other- wise intolerable heat of the fornrer, and the excessive cold of the latter; and af- fords an obvious manifestation of the wis- dom and goodness of providence. And it is to the influence of the warm superfi- cial waters of the ocean, which have come from tropical regions, upon the winds, or currents of the atmosphere, that we are to look for the cause of the differ- ence of temperature in the climate of the eastern coasts of North America and the western coasts of Europe, ami also in that of the eastern coasts of Asia and the west- ern coasts of North America. If we ob- serve the gulf stream, which is only a concentration by the trade winds of those warm waters which are flowing norther- ly along the surface of the ocean, we shall perceive it to be very narrow, pre- senting to Hie atmosphere only a small surface of its warm water, while nenr the American coast. But as it proceeds to the northeist its warm wafers are spread out upon the surface of the ocean and are thrown directly along or upon the west- ern coasts of Europe. Observation also shows that the prevailing winds in high northern latitudes, are from a north west- * Com t Phil. it Rumfonl's Essays, Vol. II. Transactions, 1752. -c 301. Chap. 2. QUADRUPEDS OF VERMONT. CLASSIFICATION OF ANIMALS. IKDF.RS OF MAMMALIA. erly direction, or passing nearly at right angles across the great northeasterly cur- rent of the ocean, and we believe it to be the influence of these warm waters of the ocean upon the westerly and northwester- ly winds, which produces the phenomenon in question. On the eastern coasts of North America, these winds come from mountainous, snowy regions, or from lakes and seas, which are covered with ice the greater part of the year; and hence they are excessively eold. In their progress over the Atlantic, they are grad- ually wanned by imbibing heat from the surface of the ocean, so that when they arrive upon the continent of Europe, their temperature is so much elevated as to produce the remarkable difference obser- ved between the climates of the coasts of the two continents.* CHAPTER II. QUADRUPEDS OF VERMONT. Preliminary Observations. All animals are divided by Baron Cu- vier, the celebrated French naturalist, whose arrangement we shall endeavor mainly to follow, into four general divis- ion^ viz. 1. I'ertcbratcd animals, or such a-, have a spine, or back bone, II. Mollis- tout animals, or such as have no skele- ton, [II. Articulated animals, whose trunk is divided into rings, and IV. Radiated unimaU, or zoophytes 'l\w first division embraces the mammalia, the birds, the rep- tiles and the fishes; the second, the shell fishes; the thud, the insects, and the fourth, polypi In this work we shall at- «< nipt but little beyond an account of our tertcbralrd and moluscous animals. MAMMALIA. Th* Mammalia are such animals ns Mrcal* thru VOUOff, and are divided by Carter into the following orders : I. HtwM,--haring two hands and three kinds of teeth. Man is the only species. II. Quadrumana — animals having four hands and three kinds of teeth. Mon- kirc and baboons belong to this order. III. C'amicora — having three kinds of t*Mh and living principally upon animal food, as the dog, cat, ivc. IV. Afarru/Ha/ to-producing their young prematurely and bringing them to perfec- tion in an abdominal pouch, which inclos- es the teats, of which the opossum is an example. V. Rodentia — have large incisory teeth suitable for gnawing, and grinders with flat or tuberculated crowns, but no canine teeth, as the rat, beaver, &lc. VI Edentata — having no incisory teetli in either jaw, and in some genera no teeth at all, of which the sloth and ant eater are examples. VII. Puc/njdcrmata having either three or two kinds of teeth, toes variable in number and furnished with strong nails or hoofs, and the digestive organs not funned for ruminating, as the horse, elephant and hog. VIII. Ruminantia — having no incisory teeth in the upper jaw, cloven hoofed feet, and four stomachs fitted for rumina- ting, or chewing the cud, as the ox, sheep, deer, &C. IX. Cctar.ca — Aquatic animals having their bodies shaped like fishes, as the whale, dolphin, &c. Of these nine orders of animals, only three are found in Vermont, in a wild state. These are the Carnivora, the Ro- dentia and the Ruminantia. We have one order more, the Pachi/da-mat.a, among our domestic quadrupeds, including the horse, ass and hog. • 111 dr.*.., Daniult in I, I! for ll.o I of ennti llU»i»lc,l hy in condi i«t. (.vi.Muro of l In; a riMil , but, tt 1I.0 hi Uuoma dryer and wl >lo<;icaI essays cn- flier temperature of Mils in a different tlio northwesterly winds lpor rtnd Unit tho caloric, sutiun, raises the general mspliere on the western i proceed eastward, they :. thoy reach thu eastern If tl for to b<3 condf lo not produce an elevatic of of the moinenon undet consideration, the quantity of in the eastern in proportion us thu tcmperaluro ii|jhpr, hut so far as observations extend tho ru- se of this seems to he tiue, the quantity of nun tho eastern eoust being greatest. 24 NATURAL HISTORY OF VERMONT. Part I. CATALOGUE OF QUADRUPEDS, CARNIVEROUS ANIMALS. JiATS. QUADRUPEDS OF VERMONT. The following, is a catalogue of the na- tive quadrupeds of Vermont, arranged in the order, in which they are described in the following pages : Order CAHSiyonx-Carnivcrous Animals. Vcspcrtilio subulatus, " pruiuosus, " carolinensisy " noctivagans, Sorez Forsteri, " brevicaudus, Scalops canadensis, Condijlura macroura, Ursus anu.ricanus, Procyon lotor, (iulo luscus, Mustela vulgaris, " crminca, " visun, " canadensis, u martes, Mephitis a nuricanus, Lutra brasiliensis, Canis lupus, " falous, " var.decussatus " var.argentatus Felis canadensis, " rufa, " concolor, Phoca vitulina, Say's Rat. Hoary Bat. Carolina Bat. Silver-haired Bat. Forster's Shrew. Short tail Shrew. Shrew Mole. Star-nosed Mole. Black Bear. Raccoon. Wolverene. Weasel. Ermine. Mink. Fisher Martin. Pine Martin. Skunk. American Otter. Wolf. Red Fox. Cross P'ox. Black or SilverFox. Lynx. Bay Lynx. Catamount. Common Seal. Order Rodentia — Gnawing Animals. Castor fiber, Fiber zibcthicus, Jlrvicola riparius, Mus decumanus, " rattus, " musculus, Gerbillus canadensis, Jlrctomtjs monax, Sciurus r.increus, " niger, " lutdsonius, " striata s, Pteromys volucclla, Hystrix dorsata, Lepus americanus, " virginianus, Beaver. Musk Rat. Meadow Mouse. Norway Rat. Black Rat. Common Mouse. Jumping Mouse. Woodchuck. Gray Squirrel. Black Squirrel. Red Squirrel. Stiped Squirrel. Flyino- Squirrel. Hedge Hog. Rabbit. Hare. Order Ruminantia- Ruminating Animals. Cervus alecs, Moose. " canadensis, Elk. " virginianus, Common Deer. Order CARN1VORA. The animals of this order have three kinds of teeth, a simple, membranaceous stomach, and short intestines. They live principally on flesh, or animal food. Genus Vespertilio. — Linnaus. Genaic Characters. — Teeth from 32 to 36, — incisors A canines 1. I grind. .4.1 A-H to 5.5 Upper incisors in pairs, cylindrical and pointed; the anterior grinders simply conical, posterior having short points or prominences. Nose, simple, without grooves, or wrinkles; ears, with an auriculum, lateral ami more or less large ; tongue smooth, and not protractile; index finger with but one phalanx, the middle with three, tho annular and little finger with two; tad comprised in the interfumoral membrane ; sebaceous glands under the skin of the face, which vary in different species. The bats consist of a great number of species, but they agree very nearly in their general form and habits. They pro- duce and nourish their young in the man- ner of other quadrupeds, but unlike them they .are furnished with delicate mem- branous wings upon which they spend much of their time in the air, thus seem- ing to form the connecting link between the quadrupeds and birds. They are noc- turnal in their habits, lying concealed during the day, but venturing abroad on the approach ofevening, during the early part of which they may be seen flitting lightly and noiselessly through the air in quest of food, which consists chiefly of in- sects. At such times they often enter the open windows of our dwellings and imetimes commit depredations upon our larders, being exceedingly fond of fresh meat. Their nocturnal habits manifest themselves in the domesticated state as well as the wild, and it is with difficulty that they are made to mount upon their wings, or take food during the day, but in the evening they devour food vora- ciously and fly about the room without reluctance. On the approach of winter bats retire to dry caverns and hollow trees here they suspend themselves by the hooked nails of their hind feet, and thus remain in a torpid state during the win- ter. They void their excrement, which found in abundance in these retreats, by reversing their position and suspend- ng themselves by the hooks upon their thumbs till their object is accomplished, when they resume their former position. Bats produce their young in June or July, and have from one to three at a time. The teats of the female are situated on e chest and to these, as we are assured by Dr. Godman, (Nat. His. I. 56.), the young attach themselves so firmly as to be carried about by the mother in her flight, till they have attained a considera- ble size. The four following species are all that have hitherto been distinguished in Vermont. It is, however, probable that othersmay hereafter be detected. Chat. l2. QUADRUPEDS OF VERMONT • 41 A I.AI. Akol.lNA HAT. SAY'S BAT- Vuftrl ilio sululotus. — Sat. DtSCftirTIOK. — Head short, broad and flat; dow blunt with a small, tlut, naked mi, ill. , eyes smull, situated near the tan and covered with fur; ears longer U»»a Ih« head, thin ovate, obtuse, and l» iv at the baae behind ; tragus thin, W«-%jlv tuttiUtr below, tapering upwards »*J tvJ.r.g m an obtUM lip, at about two lk*t4t Um> krtfbt ofth* rar ; color of tin- hack tvHommIi bio*n. the belly yellow 4»h fraj ; ftor aoft and floe, and black tail towards the rooti ; head covered with fur, excepting about the nostrils; color blackish about the mouth; whiskers few, •hort and stiff; membrane between the hind legi broad, thinly covered with fur next the body, and tapering to a point near the extremity of the tail, which it envelopes; toes of the hind feet long; hooked thumb including the nail \ of an inch. Length of the specimen before me, from the nose to the insertion of the tail, 2 inches; tail 1J inches; spread of the wings, 10 inches. HlSToRY. — This Bat seems to be distrib- uted very generally through the conti- nent. It was first described scientifically by Mr. Say, in the notes to the account of Long's expedition, from a specimen ob- tained at the foot of the Rocky Moun- tains. It was afterwards minutely descri- bed by Dr. Richardson from specimens ob- tained on the upper branches of the Sas- katchewan and Peace rivers.* Speci- men! have since been obtained from Lab- rador, Georgia, Ohio, New Hampshire and Columbia river. It is one of the small- est, and, I think, the most common Bat found in Vermont, especially in the cen- tral mountainous parts, where it enters the houses in the evening and is easily raptured. The specimen, from which my description was drawn was taken in Wa- terbury. THE HOARY BAT. Vcspertilio pruinosus. — Say. Description. — Ears broad, shorter than the head, broadly emarginate behind,hairy on the outside more than half the length. Fauna Boreali At Ft I. ina, pa 4 and at the central part of the inside , tra- gus bent, club-shaped and blunt at the tip. Canine teeth large and prominent; incisors in the upper jaw conical with a tubercle near the base, very near the ca- nines, and nearly in a line with them ; snout cartilaginous ami moveable ; nos- trils wide apart. Eyes black and promi- nent. Fur on the body blackish brown at. its base, then pale 'brownish yellow, then brownish and terminated with clear, delicate white, like hoarfrost; furonthe throat, on and about the ears, and on the inside' of the wings towards their base, fulvous; snout, chin, margin of the ears and tin' posterior part of the wing mem- brane, blackish ; the anterior part of the wings and the base of the fur on the in- lerfeinoral membrane, dark chestnut. Tail, wholly end. raced in the inlerfemoral men. bra.,,-, which is thickly covered with fur, except at the very posterior extremi- ty. Length of the specimen before me, from the snout to the extremity of the tail, 5j inches ; spread of the wings, when fully extended, Hi£ inches. History. — This bat was also first de- scribed by Say in Long's expedition and has since been minutely described by Richardson,* Coopert and others. It has been found in most pails of the United States and was obtained by Dr. Richardson as far north as ]at.54?. It is not common in Vermont, but is occasionally met with. The only Vermont specimen, which I have examined, and that from which the pre- description was drawn, was sent e by my friend, David Reed, Esq., of Colchester. It was taken at his place in Colchester the latter part of October, 1841, and was kept alive for some time in a large willow basket with a fiat cover of the same material. On opening the bas- ket, lie was almost invariably found sus- pended by his hind claws from the central part of the cover. When the basket was open, he manifested little tear, or disposi- tion to 11 y, or get away, durinn- the day time, but in the evening would readily mount on the wing and fly about the room, and on lighting always suspended himself by his hind claws with his head downward. He ate fearlessly and vora- ciously of fresh meat when offered to him, but could not be made to eat the common house fly. CAROLINA BAT. / 'fujiertilio ca rolincnsis.—G rorrRov. Description. — Ears rather large and naked. except on the backside near the cedii me a * Fiuina Ho real j Aniei t Am.uls N, V Lyceu IV. 54. 26 NATURAL HISTORY OF VERMONT. Part I. SU.VEK-IIAIKI'.II BAT. FORSTER S SHREW. head, einarginate on the outer posterior edge, tragus shorter and less pointed than in Say's Rat. Head long and narrow; canine teeth very prominent; snout, in- terfemoral and wing membranes black and entirely naked; a few scattering hairs on the feet. Fur on the head and back long and color uniform bright ferrugin- ous ; beneath yellowish brown; last joint ot'the tail not enveloped in the membrane. Bones supporting the membrane very ap- parent. Length of the specimen before me, from the snout to the extremity of the tail 4 7 inches, head and body 3 inches, tail 1.7, fire arm 1.8, tibia .7, spread of the wings 11.5 inches. History. — Of the history of this bat I know nothing. It is said to be quite common in the southern states particular- ly in the Carolinas and Georgia and also on Lonjr Island near New York. The only specimen I have seen and that from which the above description was made, was ta- ken in Burlington, and deposited in the museum of the college of Natural Histo- ry of the University of Vermont by Mr. John II. Morse, a student of the Univer- sity. A Vermont specimen of this species is also preserved in the museum of Nat. His. of Middlebury college. SILVER-HAIRED BAT. Vesptrtilio noctivagans. — Le Conte. Description. — Ears dusky black, rath- er large, naked on the anteriqr portion, somewhat ovate and obtuse, with two emarginations, on the outer posterior bor- der, produced by two plaits; naked with- in, and with the tragus moderate, ovate and obtuse. Color above, a uniform dark dusky brown, approaching to black. On the back the fur is somewhat glossy and tipped with silvery white, forming an interrupted line across the shoulders, and thence irregularly mixed down the centre of the back. Interfemoral mem- brane thickly hairy on the upper part be- coming thinner downward and naked near the border. Tip of the tail projecting about a line beyond the membrane. Feet hairy. Wing membrane entirely naked. Beneath very similar to the upper parts, though the light colored tips of the hairs are more yellowish. Total length 3.6 in- ches, tail 1 f>, fore-arm 1.8, tibia .8, spread of (he wings 11 inches. History. — This Rat I have not seen in Vermont, but 1 am informed by my friend Prof. Adams that there is a specimen of it, which was taken in this state, in the museum of Natural History of Middlebu- ry College. The above is Mr. Cooper's U N. V. Lvccnn lis. Vol. IV. n. 9 description of this Rat*, who says that " it was first described in 1831 by Major Lo Conteand Dr. Harlan, and that it may be easily recognized by its dark black-brown fur tipped with white on the back." It was named V. noctivagans by Le Conto and V. .Judiboni, by Harlan, and the for- mer of these names is retained, because Le Conte's account was first published. Genus S o r r.x . — Linnccus. Generic Characters. — Teeth variable from 39 lo 34. The two middle upper incisors honked and denlated at their ba-,e ; the. lower ones slanting and elongated ; lateral incisors small, usually live on each side above, and two below; grinders, most commonly 4 on each side ahoro, and 3 below. The body is covered with fine, short fur ; toes, five on each foot, separate, fur- nished with hooked nails not proper for digging: head and nose elongated, the latter moveable ; ears short and rounded ; eyes small but visible. «ssS FORSTER'S SHREW. So ret t'orstcri. — Richardson. Description. — Color yellowish brown or dark olive above, bluish white or cin- erous beneath ; base of the fur plumbeous for two thirds its length both above and below ; teeth white at the base and at their points, deep chestnut brown ; tail long, four sided, covered with short hair and terminated in a fine pencil of hairs; feet small, light flesh-colored and nearly nuked; nails slender and white ; whiskers half an inch long, light brown. Length of the head and body 2 inches, tail 1.4, head .9, from the eye to the point of the nose .3. History. — This little animal is occa- sionally met with in our pastures and fields, having their places of retreat in stone walls and under old fences and logs. The specimen from which the above de- scription was made was taken in Bridge- water and is now in my possession. This shrew was first described by Dr. Richard- son who says that it is common throughout the fur countries, even as far north as the 67° of latitude and that its delicate Toot- steps are often seen imprinted on the snow when the temperature is 40 or .r>0° below zero.* It is also found according to Dr. Rachman on Long Island in the vicinity of New York.t *Fauna Horeali, vol. I. page 0. [Journal Acad. Nut. Sci. of t'liil. vol. VII. CUAP. fi. QUADRUPEDS OF VERMONT. 27 iHuHT-TAU.EO SHREW. illlli.W MOLE- THE SHORT-TAILED SHREW. Sorez tirccicaudus. — Say. Description. — Color of the head, body and tail dark plumbeous brown above, a little lighter beneath ; lips naked fleshy and flesh-colored J extremity of the snout brown, notched ; teeth tipped with dark chestnut brown at their points fading in- to white »t their base ; feet flesh-colored, nrtrl) naked and .lender ; nail* slender, • kite on th<- fore feci, and on the hind (. external ear, opening large. Total length of the specimen before me 4-8 inches, to the origin of the tail 3-8, tail 1, head 1-1, hind foot to the point uf the longest nail .6. Huron*. — This species of Shrew bears a very considerable resemblance to the bhrew mole in its general appearance, but is much inferior to it in size, and dif- fer* from it remarkably in the structure of ila fore feet. As they seldom venture in- to cleared fields, very little is known of their habits, but in the woods they are of- ten *• en and heard rustling among the leaves and digging little holes into the ground, probably in quest of food. This and the preceding species are occasionally caught and brought in by cats ; but they will seldom attempt to eat them on ac- count, probubly, of their disagreeable mus- ky odor. In addition to the foregoing we certainly have one other species, and pro- bably mure, but they require further ex- amination. Genus Scalops. — Cuvier. Generic Characters. — Teeth 36 to 44 — Incisors f canines .«'.ed mole. THE BLACK BEAK. THE STAR-TJOSED MOLE. Condylura macroura. — Harlan. Description. — Color dark brown ap- proaching to black; body cylindrical; nose long, tapering and surrounded at the ex- tremity by a fringed membrane, having twenty points; tail nearly as long as the body, strangulated at the base and then becoming suddenly enlarged as if swollen and thence tapering to a point. The tail is scaly and sparsely covered with stiff hairs. The tore legs very short ; the paws large and naked, excepting the ed- ges, which are fringed with stiff hairs; nails long and flat with cutting edges. The hind feet are naked, long and nar- row, and the nails long, slender and sharp resembling birds claws; eyes concealed and very small; no external ear, 4 pec- toral mammae ; length from the nose to the insertion of the tail 4.7 inches, tail 2.8 inches, hand .7 inches, longest nail .3 inch- es, hind foot 1. History. — This animal being rare, its habits are not well understood They ap- pear, however, from what is known of them, to be similar to those of the other moles. They are usually found about old buildings, fences and stone-walls, and they occasionally find their way into cellars of dwelling houses. I have two specimens of this animal, both of which were before me, while making out the foregoing description. The color of one is a little darker than the other, but they scarcely differ in any other respects. They were both caught in Burlington, one in lc'3U, in the cellar of the Rev. G. G. Ingersoll, and the other in 1840, on the surface of the ground in a door-yard. Their fore feet are so closely attached to their bodies, that they serve but little pur- pose except for digging, and their prog- ress upon the surface of the ground, is ex- tremely slow, labored and awkward. Like the shrew moles, they probably reside most of the time in the ground and ven- ture abroad only in the night. On ac- count of their clumsiness they are fre- quently drowned in cisterns and tubs of water and are sometimes brought in by cats ; but cats are not fond of eating them on account of the musky odor which they have in common with the shrew and shrew mole. It proceeds, as in the other cases, from a while viscous lluid contain- ed in a sack near the vent. - Genus Ursus. — Linnaus. Generic Character!; — Teeth, 32 to 44,— incis- ors S. tannics 1..L grinders ±.i to 1-1. Three of the grinders on each side in each jaw, are lar"e, with square tuberculous crowns ; the other are small, most of which appear late and are shed early. Body thick, covered with Strong hair; ea,s Ion" and slightly pointed ; toes, five, furnished with strong, curved claws, calculated for climbing or burrowing ; tail, short. THE BLACK BEAR. Ursus americawus. — Pallas. Description. — Color shining black ; hair long and not curled; nose fawn col- ored, projecting, brightest about the an- gle of the mouth, and terminated by a naked black snout; forehead slightly arch- ed ; ears oval, rounded at the tip and far apart ; palms and soles of the feet short in comparison with the brown bear ; claws black and strong with the hairs of the feet projecting over them ; tail short. History. — The specimen from which our description is drawn was killed in Williston in 1833, and presented to the College of Natural History of the Univer- sity of Vermont. It measures 6 feet from the nose to the tail ; tail 2 inches; height of the ears 4 inches ; height to the top of the shoulders 3 feet; rump 2 feet 4 in- ches. This Bear, which is found through- out all the woody parts of North America, was formerly very common in Vermont, and continues so plentiful at the present day, that our Legislature continue in force a law allowing a bounty of $5 each, for its destruction. It appears from our Treasurer's reports for several years past that the number of bears for which the bounty has been paid has varied from 40 to :".() annually. The black bear, under ordinary circumstances, is neither Very camiverous nor very ferocious. Its fa- vorite food consists of vegetables, such as Indian corn, nuts, berries and roots. But when these fail, it is compelled by neces- sity rather than choice to resort to ani- mal food. In such cases, impelled by hunger, it will sometimes attack and de- stroy young cattle, sheep and hogs, but Cup. 2. QUADRUPEDS OF VERMONT. 29 T1IK KACCOO." T1IK WOLVERENE. will seldom, if ever, attack a person ex- cept in defence ol* its cubs, or when pro- voked, or wounded. The early settlers of tliiti State suffered most from them in consequence of their ravages upon their fields of Indian corn. They entered the fields in the night when the corn was in the milk and broke down and devoured the ears with great greediness ; and it wus a common business for the settlers to watch for them with guns and shoot them while committing their depredations ; and in this way large numbers were annually killed. During the fall, when their food is ubundant, bears usually become very fut, and, as tlie winter sets in, they retire to ■umu natural den among the rocks, or uprooted trees, or into souk- hollow tree, wfeera liny remain in a torpid stale and • illiiul fi«»tl until the return of warm weather in lhc Spring. The female pro- duces her young during Iter hibernation and has from one to five at a litter, but the more common number is two. Their pe- riod of gestation is about 15 or 1