UC-NRLF 2Dfi ! } mm • H ;.' ;ffi^ii I LIBRARY UNIVERSITY OF CALIFORNIA J PRELIMINARY REPORT OX THE NATURAL HISTORY OF THE STATE OF VERMONT BY AUGUSTUS YOUNG; STATLJ NATURALIST. DOCUMENTS KPA.tTM FEB I.'- *RY u BURLINGTON: C H A U N G E.Y G 0 0 I) II I 0 IT. 185G-. . 810LOG* L1BRARV IN SENATE, Oct. 23, 1856. Referred to the Committee under the 4th Joint Rule. IN SENATE, Oct. 23, 1856. Reported. Ordered to lie — and that the Secretary procure one thousand copies to be printed for the use of the General Assembly. 257 REPORT. To His Excellency. EYLAND FLETCHER, Governor of the State of Vermont : — SIR : On the twenty-ninth day of February, 1856, I had the honor of receiving from His Excellency GOVERNOR ROYCE the appointment of State Naturalist, to supply, until the next session of the General Assembly, the office which was rendered vacant by the death* of Professor Zadock Thompson. Conscious that my present position is more attributable to the generous hopes of your predecessor than to any merits of my own, I hesitated awhile, by reason of failing health, to assume upon my self its weighty cares. Having, however, for many years devoted a portion of my time, and all of my leisure hours, to the study of Natural History, and especially of my native State, and become somewhat familiar with the physical resources of Vermont, and feeling anxious that the work, in which Professor THOMPSON was engaged at the time of his death, should be prosecuted to its com pletion without interruption, I ventured, not however without some misgivings, to take upon myself the burden of its duties. As soon, therefore, as circumstances and a proper regard for the feelings of the family of my deceased friend would justify my so doing, I commenced my official service, and in due time, made a careful examination of the progress which had been made by my predecessors towards a " thorough prosecution and completion of the Geological Survey/' The first object of my enquiry was to ascertain the requirements of the Stsuutc.s authorizing a Geological Survey of the State \ and * fc-te Appendix Nh. 'L 6 I found that to the history of the legislation of Vermont on this subject is attached no want of interest. The matter of a Geolo^i- cal Survey of Vermont was first brought to the consideration of the General Assembly during the administration of Gov. Jenison, in 1836, and in the following year (October session, 1837,) the sub ject was referred to the Committee on Education, in whose behalf the late Gov. Eaton submitted to the Senate a carefully prepared report,* accompanied by able and important documents. Although the subject was discussed at each succeeding session of the Gener al Assembly, the first Act was not passed until October, A. D. 1844,t and the second act received the executive sanction in De cember, 1853 1 — the one making provision for the Survey, r.nd the other providing for its completion. The duties devolving upon the State Geologist, by virtue of the Act of 1844, are clearly set forth in the third section of said Act, and are as follow : " It shall be the duty of the State Geologist, as soon as practicable, to commence and prosecute a thorough Geological Survey of the State, embracing therein a full and scien tific examination and description of the rocks, soils, metals and minerals ; make careful and complete assays and analyses of the same ; and annually, on before the first day of October, to report to the Governor the progress of the work, the most efficient and economical manner of conducting it, and an estimate of the ex pense for the ensuing year/'t By virtue of this Act, Gov. Slade appointed, as State Geologist, Professor Charles B. Adams, at that time Professor of Chemistry and Natural History in Middlebury College, who entered upon his duties on the first day of March, 1845, and who made four annual reports upon the Survey indicating its advancement, which reports were duly submitted by the Governor to the General Assembly, and printed and distributed among the people. The Legislature having made no provision for embodying the facts which were gathered during the three years of the Survey in a systematic report, and having failed to make any appropriation for a con tinuance of the work, the Survey was suspended— the manu scripts, field-books and specimens being locked up in about fifty * See Appendix No. 5. f See Append x No. 2. $ Sec Appendix No. 3. boxes, and in that plight, remaining at Burlington and Mont- pel ier.* In 1848, the General Assembly passed a Joint Resolution pro viding for the preservation of the materials for completing the Geological Survey, as follows : "Resolved by the Senate and House of Representatives, That all collections of minerals, field- notes, and all preparations and materials amassed by the State Geologist for a final report upon the Geological Survey, be brought together by some suitable person to be appointed by the Governor5 and be deposited in the State House, under the care of the State Librarian, that nothing may be lost, and that the State may have the benefit of these collections, whenever the State sh^ll deem it expedient to " prosecute the Survey to completion. "t Governor Coolidge commissioned Professor Zadock Thompson to carry into effect the foregoing resolution, whose report, under date of October llth, 1849, is respectfully referred to and made a part of this communication.* A final Geological Report, embracing the entire results of his labors and those of his Assistants, was never made by Prof. Ad ams, and on the nineteenth day of January, 1853, he died on the Island of St. Thomas, West Indies, summoned hence in the prime of his life and usefulness. In the month of October, following the decease of Prof. C. B. Adams, the General Assembly passed "An Act to provide for completing the Geological Survey of the State," in and by which Prof. Zadock Thompson was appointed State Naturalist, with the following duties : " to enter as soon as practicable upon a thorough prosecution and completion of the Geological Survey of the State, embracing therein a full and scientific examination and descrip tion of its rocks, soils, metals and minerals ; make careful and complete assays and analyses of the same ; and prepare the results of his labors for publication, under the three following titles, to wit: First — Physical Geography, Scientific Geology, and Mineral ogy- Second, Economical Geology, embracing Botany and Agricul ture. *See Appendix No. 4. fSee Session Laws, 1848. p. 36, No. 53. Third.— General Zoology of the State.*" It will be noticed, upon comparison, that so far as regards Phys ical Geography, Scientific and Economical Geology and the con comitant science of Mineralogy, the Statutes of 1844 and 1853 imposed similar duties upon the State Geologist and State Natu ralist — to which there can be, probably, no well-planted objection except to that requirement by which he is expected to make "care ful and complete analyses of soils " with a view to a special appli cation of Geology to Agriculture. Upon the doubtful utility of this requirement, 1 propose to ofler some remarks in their proper place. By the act of 1853, Botany and the General Zoology of the State are added to the previous act of 1844, thereby obviously contem plating a complete Natural History of Vermont, in three parts or subdivisions — a design which, if Providence had permitted Prof. Thompson to carry out to completion, would have possibly surpassed any thing of the kind in any of our sister States. It was one of Professor Thompson's most ardent earthly aspirations that he might be allowed to present to the world in an entire, well-planned and well-executed work, the Physical Geography, and Natural History of his native State ; and from the liberal Views which prompted the passage of the act of 1653 it is obvious that a like laudable feeling and ambition pervaded the General Assembly. But in the death of Professor Thompson such ex pectations have been disappointed ; arid we may be compelled to satisfy ourselves with or rather to submit to such a Geological Survey as has, in general, been satisfactory to different States in our Union, consisting of carefully prepared and arranged reports upon the Natural History of Vermont. It is no disparagement to any living Naturalist or Geologist to express a doubt whether for many years to come there will be found among us another gen tleman so ardent in his feelings upon the subject, or so well fitted by life-long series of observations and scientific examinations, to execute on behalf of the State a task ot such magnitude and im portance as was the late and highly gifted State Naturalist, Pro. lessor Zadock Thompson. We may, however, gather consolation in the fact that so fur as * Sec .Appendix No- 3. 9 the Zoology and Botany of Vermont are concerned, we have the results of the unwearied explorations and observations of Prof. Thompson, embodied in his Natural History of Vermont which was published in October 1842, and, beside this, we have record of his more recent and matu:e labors embraced in an Appendix to his History of Vermont which was published by him in a small volume of sixty four pages, in April, 1853 — five years after the Geological Survey, under Professor Charles B. Adams as chief ond Messrs S. R. Hall of Craftsbury and Zadock Thompson of Burlington, as assistants, had been suspended, It is reasonable to suppose that if Professor Thompson had been permitted to live and finish the work which the Legislature had commissioned him to perform, valuable additions would have been made to his botanical catalogue as printed in his History and Appendix, and undoubtedly many plants would have been discover ed nnd zoological discoveries made to reward his patient and enter prising research. Such plants and animals — however small or insignificant — are by no means unworthy the study or beneath the notice of any scientific enquirer : but it may be seriously ques tioned whether, since Professor Thompson, upon whom especial reliance was placed nnd in whom the hopes of the State centred, is «lead and no longer able to answer the expectations which a grateful people indulged, the General Assembly would authorize or justify the expense which is incident to the compilation and publication of those parts of the Natural History of the State which comprised the departments of Botany and Zoology — even upon a reasonable assurance that such a work would not be in any wise slighted in the hands of others than those for whom it was designed. Apart from this consideration I have thus far been unable to ascertain that subsequent to his appointment as State Naturalist in October 1853, he had been subjected to any consider able expense in preparing materials for the publication of the se cond and third volumes of the Natural History of the State, as contemplated by the Statute of 1853. His attention had been chiefly bestowed upon a preparation for publication of a volume relating to the Physical Geography, Scientific Geology and Min eralogy of Vermont. It may be possible that the materials already collected and pre pared by Professor Thompson would have been sufficient to en- 10 able him to compile the three volumes contemplated by the act of 1853 by the addition of such extracts from his published works as may have been appropriate ; but it may admit of some doubt whether any other person would be justified in making use of the same printed matter for the same purpose. The fact has been communicated to me that a large edition of his Natural, Civil and Statistical History of Vermont yet remains unsold, and I am un willing to believe that inasmuch as his literary and scientific works constituted the chief legacy to his wife and family, any one wrould suggest or recommend any measure tending to lessen the sale of his valuable books or infringe upon the copy-right in which his family must feel no slight interest. If however, the widow and heirs of the late State Naturalist can be induced to waive their right and interpose no objection to a judicious use of that part of Professor Thompson's history which relates to the Natural His tory of the State, then there would remain no obstacle or objec tion in the way of using all of the labors of the late State Natu ralist in carrying out the plan contemplated by the act of 1853. Under these circumstances and influenced by the considerations which I have briefly mentioned I have esteemed it to be my duty for the present and until these suggestions are communicated to the Legislature, to forbear any attempts to collect or arrange ma terials for the Botanical and Zoological compartments of the pro posed work, and have confined my labors and restricted my enquir ies to those matters which relate more particularly to the Geolog ical department in connection with Mineralogy. My predecessor, Professor Thompson, at the time of hisxleath had for causes to which I shall hereafter particularly advert, made but slight progress in preparing his reports for publication. I find, however, among the great number of papers, and collection of matter from which the materials for his final reports were to be drawn, a programme of his contemplated work contained in three small pamphlets in manuscript* executed in his remarkably neat and methodical manner, purporting to present the title-pages and tables of contents of the three proposed volumes. Each volume was entitled" Natural History of Vermont " — the first being devot ed to Geology ; the second to Botany ; and the third to Zoology.* The contents of the first volume were divided into four parts, viz : . * See Appendix No. 9, 11 Scenograpliic Geology — Scientific Geology — Mineralogy and Economical Geology — all constituting in my judgment, an excel lent and most comprehensive programme : and, perhaps, no better and more methodical table of contents on the Geology of the State could be devised. The contents under the head or title of Sceno- graphicGeology relate to the aspect of the country,Mountains, Hills Watersheds, Valleys, Chasms, Caves, Springs, Streams, Ponds, Lakes, Swamps. On these subjects Professor Thompson has left a few pages in manuscript carefully enveloped as if prepared for the press : but aside from these papers I have been unable to dis cover many traces of his progress in writing out the proposed work for publication. I have deemed it proper and incumbent upon me to allude to these facts in order to present a correct view of the present con dition of the Geological Survey. Should it be thought advisable to postpone for the present further labors in the department of Botany and Zoology, it seems as if the materials already acquired together with such as may be obtained or prepared at a moderate expense n ight enable some competent Naturalist to arrange for publication such a final report of the Geological Survey as was originally contemplated by the act of 1844. The expense of such a report would be inconsiderable as compared with the benefits which would accrue, provided the analyses of the different soils of the State were dispensed with. With regard to the chemical analyses of soils I would suggest that in order to have them of practical use or of scientific interest they should be made with extreme care and thoroughness and must, of necessity, involve greater expense than their very doubt ful utility to the agricultural interest of the State would warrant.. The agricultural interest of a State is greatly paramount to any other and, in fact, to all other interests combined. " To subdue the earth," to make it perpetually fruitful is the province of agri culture and he must be a public benefactor who can discover some, special means whereby the farmers of Vermont are enabled to in crease their profits and diminish their labors, and he is doing the State some service who can induce the farming interest to adopt the best mode of preparing the soil and putting it to the most prof itable use and to dispose of its products most advantageously to the soil and its owner : for thereby he advances the intelligence. 12 and promotes the happiness of those who pursue a delightful but necessarily laborious calling. I owe it to candor to express my doubt whether any Geologist however skillful or Naturalist how ever learned or scientific, can, by traversing the State, collecting and arranging statistics of the average crops and calling the at tention of farmers, to the well-known deposits of marl, muck, lime &c., in their respective vicinities, succeed in supplying the place of intelligent enquiry and careful observation in an enlightened farming community. There is no royal road to the successful pur suit of Agriculture any more than to any branch of domestic in dustry or department of science. In regard to the chemical analysis of soils arid some of the requisites of a valuable analysis I propose to offer a few remarks. A plant derives the principal part of its sustenance from the soil. The soil must contain certain fertilizing elements in due propor tions to secure the perfect growth of the plant. If the soil be deficient in one or more of these essential elements, chemical anal ysis can detect the cause of the evil and point out the remedy "But," says Dr. John D. Easter, " the growth of plants is influ enced by a multitude of other circumstances to which chemical analysis can furnish no clue, a soil may abound in all the elements of a very fertile one and yet be perfectly barren. The soil of the great Colorado desert in California, which I have recently anal ysed, furnishes a good example of this. It possesses in abundance every element necessary to extreme fertility, but is entirely barren from the want of water. The reverse of this also frequently occurs. The chemist re ceives a specimen of the soil, in the chemical constitution of which he can detect no deficiency, and in his laboratory, he can assign no cause for its alleged unproductiveness. An examination of the lo cality probably shows him that it is underlaid by a stiff, tenacious sub-soil, which retains an excess of watei\ and no provision has been made for drainage. The difference in the mechanical texture of stiff and loose soils is familiar to every one. The fertility of many stiff clays may be seriously impaired by ploughing too wet, rendering them tough and impenetrable to the tender rootlets of plants. In this case, as no chemical change takes place, the chemist in his laboratory would seek in vain for the cause of the difficulty. 13 Every attempt to improve the character of the soil must, there fore, be preceded by a judicious consideration of its mechanical texture, its power of absorbing and retaining water, and its capa city for heat. Hence it is important that the agricultural chemist should, if possible, himself examine the locality in order fully to estimate the wants of the soil. The employment by every State of an agricultural chemist, who should visit in person every part of the State, is therefore, strongly to be recommended. In the next place it is requisite that an analysis of the soil, in order to be of much value should be thorough. It must include sepa rate estimations of the parts soluble in water and in acids, and the insoluble portion. For the portion soluble in water represents what is available for the wants of the growing crop, while the por tion soluble in dilute acids, is the index of what may by decomposi tion become the food of plants. This undecomposed portion of the soil may often, by the application of lime, ashes and other caustic manures, be more speedily decomposed and rendered available. The analysis should include also, if possible, the sub-soil as well as the surface soil, in order to guide the former in the process of deepening his soil. There are, of late, many advocates of indis criminate deep ploughing. But a fertile soil may be underlaid by a barren sub-soil, by throwing up large quantities of which the fertility of a field may be destroyed for years. The subsoil, not unfrequently. contains large quantities of protoxide of iron and other substances which are not injurious to vegetation until they have been subjected to the action of the atmosphere. On the other hand, the subsoil often contains elements of fertility which are not so abundant in the surface soil, in which case deep ploughing will improve both. It is important that the agriculturist should know these differences, in order that he may know where he should plough deep and where refrain. A still more important consideration is, that no analysis can be of any value to the farmer who is not himself a chemist, unless it be accompanied by a discussion of the indications it affords, and a recommendation of suitable means of improvement. Our agri cultural journals and reports abound in analyses which are about as intelligible to the unscientific farmer as the inscriptions on the pyramids, or a chapter from La Place's Mechanique Celeste. Most of our intelligent farmers know that lime, phosphoric acid, 14 and the alkalies, play important parts in the economy of vegetation, but few of them have any idea how much of these valuable ingredi ents is requisite to fertility, or what are the best means of supply ing their deficiency. Until every farmer is also a chemist, an an alysis of a soil or manure which is not followed by a commentary on its defects or virtues, leaves him just where the diagnosis of a disease, without a prescription for its relief, leaves the patient. He is no wiser nor better off than before. It will not do to presume that when the chemist pronounces what a soil contains, the agri culturist will know what it ought to contain, and how to supply its wants. Every farmer should insist upon an interpretation of the analysis furnished him by the chemist."* In regard to the benefits to be derived by the agricultural inter est from chemical analyses of soils, I beg leave to quote from published letters written by President Hitchcock of Amherst College and by Prof. Benjamin Silliman, Jun. of Yale College, New Haven, Connecticut. President Hitchcock in a lettert to our first State Geologist says : " I should not think it strange if some should be disappointed, as they have been in other States, by anticipating too much from the mere analyses of soils. The impression is very strong through the community that the chemist, by such an analysis, can determine what is wanting to render a soil fertile or what renders it barren. Now even admitting that he could do this, an analysis of the soil from almost every farm in the State, nay, from almost every field, would be necessary to make it of much value; and it is not generally known that every such analysis, accurate enough for this purpose^ could not consume less than two or three weeks. But I do not be lieve that agricultural chemistry is yet far advanced enough to en able the chemist to say in many cases what ingredient added will be sure to render a barren soil prolific ; although it is more easy to detect hurtful ingredients. But the analysis of some of the prevailing soils of the State (for example those from the limestone, mica slate, gneiss and and argillaceous slate regions,) will enable you to make suggestions that may be of great use." Professor Silliman, Jr., in his correspondence! with Professor * See Appendix No 10. •f-See First annual Report on the Geology of the State of Vermont by Prof. Adams, pp. 07, 68. JSee Prof. Adams' Second Annual Report on the Geology of Vermont, pp. 202, 263. 15 Adams, makes the following expressive remarks : " I hardly know what answer to make to your enquiry about the terms for analyz ing one hundred specimens of soils, &c. Our customary charge in analysis has been five dollars for every determination. This makes a round bill, but not more than a fair quid pro quo for the labor and skill required. It is the rate affixed by the joint agreement of several chemists. However we always make an abatement from it in case of many analyses of the same sort. No doubt, a sort of analysis of a soil may be made for five dollars, all told, but what sort I will not say. In my opinion the present state of science demands that an analysis of a soil, to be of any use whatever, must be minute, and ought to comprise at least ten separate determin ations, besides the ultimate analysis ol the whole mass, by alka line fusion, which is useful as showing the extreme resource of the soil. We now think that we must have — First, an analysis of the matter soluble from the soil by water alone ; Second, the amount of the matters soluble in dilute hydrochloric acid; Third, the ul timate analysis by fusion, as just suggested; Ldstlij, we ought to know the mechanical condition of the soil, technically called its mechanical analysis, which requires a series of sittings, washings and weighings, distinct from all the preceding. Going through all these numerous but essential steps on sixteen soils for * * * * -\ye made him a bill of five hundred dollars. The difference between fertility and barrenness is comprised within such narrow limits that only a minute analysis of the sort I have sketched, can be of much use. Agriculture gains nothing from any further multipli cation of such analyses as the bulk of those which in past years have filled Geological and Agricultural Reports. We have enough such already. Unless an analysis of a soil can do something more than people have hitherto been content with, the result will soon be that agriculturists will, with reason, question the utility of chemical analyses as of any practical benefit." If therefore, the foregoing quotations from the pens of the most accomplished geologists in the Union are to be treated as author itative in the premises, any attempt to analyze the almost infinite variety of soils in Vermont with a view to subserve the agricultu ral interests of the State would involve an expenditure which by reason of any accruing benefit could not perhaps well be justified. Thus the agricultural chemistry of the state is properly and chiefly 1G referred to the observation and experience of its intelligent citi zens and farmers who by no means treat the science of agricul ture with disrespect and do not reject what is called book-knowl edge on the subject as contained in the numerous periodicals and other works devoted to agriculture which are so generally circula ted in their midst. It is not for a moment to be presumed that the intelligent farm ers of Vermont are wholly ignorant of the difference in the nature and fertilizing qualities of the soils pervading more extended tracts or ranges of the State and which have been chiefly produced by the disintegration of the different kinds of rocks which under lie or are in the vicinity of the soils which have been formed from simple minerals composing the rocks and consequently partake more or less of their mineral and chemical characters. A general acquaintance with the different simple minerals and their characters of which these extensive ranges of rock are com posed (and no new chemical analysis is required for this purpose,) enables us to get a general but imperfect understanding of the chemical composition of the soils which overlie or accompany them. It may here be remarked that those ranges of rocks and their ac companying soils run nearly North and South, and hence their dif ference becomes very apparent in travelling East or West across the State. This general difference in the chemical constituents of the several ranges of soil is doubtless all that was intended to be conveyed by President Hitchcock when he says that suggestions in regard to the " prevailing soils of the State (for example those from the limestone, mica slate, gneiss and argillaceous slate regions,) may be of great value." * Aside from the considerations which those quotations embody and enforce, it is proper to add that the commonly received opin ion that the soils of a country have originated from the rocks immediately under them is somewhat erroneous. All soils are derived from rocks broken or pulverized and so disseminated that the ruins of one rock may be supposed to be mixed with the ruins of a great many others. Every soil, therefore, may be regarded as a mixture of many soils and may be supposed to have come from many and often from wide spread localities. " If every par- *See Prof. Adams' "First Annual Report on the Geology of Vermont," p. 68. IT tide in a cubic foot of earth were to be endowed with instinct and were to rise up and take its departure for its original rocky home, I have no doubt," says Professor J. A. Nash, '; there would be a wide scattering, and I believe an extent of travel would be shown quite surprising to those who have not reflected on the sub ject." It must be conceded therefore, that soils do not always depend for their composition or capabilities upon the rocks immediately underlaying them. Soils usually come from wide-spread regions generally North and North-west of their present location. Ver mont soils however partake more of the character of the adjacent rocks than the soil of any other section of the Union. Under these circumstances to which I have alluded in very brief and, I fear, un satisfactory terms. I venture to suggest that the further chemical analyses of soils ought to be postponed until they can be made up on a more extensive scale than is contemplated by the existing law. The time has scarcely yet arrived when the State of Ver mont can employ an agricultural chemist to visit in person every part of the State with the view of examining the dificrent soils and their physical or mechanical condition or their climatic loca tion and thus be enabled to make a practical and scientific report upon the chemical composition and fertilizing elements of such soils as may be subjected to such analysis and examination. But with respect to both the qualitative and quantitative anal ysis of the rocks and minerals of the State, there are abundant and controlling reasons why this requirement of the Statute should be faithfully observed by the State Naturalist. The min eral wealth of Vermont yet remains undeveloped. To the exam ination, description and arrangement of mineral substances already known or partially so ; to determining the character of certain rocks and minerals so as to indicate their economical uses and to prevent useless experiments and wasteful expenditures of time and money, have the labors of my predecessor been to a great degree devoted. Circumstances to which allusion has already been made have conspired to prevent the results of those researches from being hitherto systematically arranged and presented to the public in such a manner as to be of the greatest practical benefit and most scientific interest. There is such a diversity of soils in Vermont as to render the 3 18 Green Mountain State one of peculiar interest. The Western or Prairie States have soils so similar in many respects throughout their geographical limits, that an analysis of one part may be of service in determining the chemical composititon of another,where~ as the minerals of Vermont are as various as its surface soils, and its surface soils are so diversified as to have challenged the attention of admirers of the beautiful and picturesque as wellas of scientific ob servers for many years. The extensive and inexhaustible quarries of limestone and marble, serviceable both as objects of architectu ral beauty and agricultural utility; the beds of serpentine or verd antique which so extensively abound in Roxbury, Cavendish, Lud- low, Lowell, Westfield, Troy and elsewhere ; — the vast hills of granite lying in the eastern part of Vermont, ranging from the Provincial line of the boundary of Massachusetts, which have been so advantageously quarried for building purposes and of whose beauty and utility the State House at Montpelier is the most im posing exponent ; the large slate quarries which have been wrought so extensivelv and contributed so much to the wealth of Vermont because of their peculiar excellence and which appear to be in no wise inferior to the best slates of Wales ; the iron ores of various kinds which seem to be inexhaustible and extend from the northern to the southern limits of the State and are found principally on the western side of the Green Mountain range ; the large beds of manganese lying in Bennington, Rut land and Addison Counties and to a greater or less extent in other localities extending to the Province of Canada and which are of such utility in the manufacture of chloride of lime, useful in bleaching processes ; the beds of sulphuret of iron or copperas ore which are situate in Strafford, Corinth, Shrewsbury and other places and which under congressional protection have banished foreign copperas from American markets ; the large beds of steatite or soapstone which have been advantageously wrought in Grafton, Bridgewater, Bethel, Cavendish, Moretown, Water- ville, and other parts of Eastern Vermont ; the beds of porcelain clay in Monkton and other localities together with fire clay of which the best fire-bricks for furnaces are made ; the beds of copper, lead ore and other metals — all these and others which I have not mentioned, render Vermont a most interesting field of enquiry for the scientific and economical Naturalist. 19 Many of the ores, metals and other minerals enumerated in this report have been carefully " assayed" or resolved into their constituent parts, and the results of such analysis carefully noted and preserved. It may be necessary, however, in view of their vast importance and utility to supply such deficiencies as may be found to exist, that the chemical analysis of each valuable metal or mineral may be presented, in a properly arranged descriptive table made convenient for the use and reference of those interested in such important items of intelligence. While, for reasons heretofore given, the analyses of soils may not be practicable, and are of very doubtful general utility, there can be no limit to the importance of an analysis of the ores, metals and other minerals which constitute so great an element in the wealth of the State. Jn fact its utility can hardly be ex aggerated. While impressed with the importance of a complete develop ment of all departments of the Natural History of the State which savor of practical utility, and aware of and duly appre ciating the natural and laudable wants and wishes of the people of Vermont in this particular, I am by no means insensible to the manifold attractions which our State presents to the scientific or theoretical enquirer. While the geological surveys of New Hamp shire by Professor Charles T. Jackson, of Massachusetts by President Edward Hitchcock, of New York by William W. Ma ther, Dr. Ebenezer Emmons, Prof. Gardner Vanuxem and Prof. James Hall, and of the Province of Canada by Sir William Ed- mond Logan, have greatly tended to develope their mineral and natural resources, it cannot be expected that Vermont will be backward in ascertaining the extent and variety of her internal resources. The enlightened policy which gave origin to the ex isting law providing for a completion of the Geological Survey will undoubtedly bear the Survey onward to its proper consumma tion. Although the science of Geology is yet in its infancy, and the theories of to-day may give place to the more plausible theo ries of to-morrow, yet whatever of permanent scientific interest attaches to the Geological Survey of Vermont ought to be re corded and presented to the world so soon as the Survey is com pleted and the entire field has been thoroughly explored. The objects of scientific interest in the Natural History of Ver- 20 mont are so numerous as to have attracted the attention of the best naturalists of the world. There can be no doubt but the thorough completion of the Geological Survey will bring to light many valuable discoveries — valuable in the two-fold view of econ omy and science. " Vermont," says President Hitchcock, " is considered as the disputed ground in respect to certain problems of sublime interest." The rock formations in Vermont are ex ceedingly complicated both in respect to their mineral composition and to their geological order and age. While the greater part of the rocks exhibit plains of sedimentary deposit and thus give proof of an aqueous origin, they are also very crystalline in their structure and indicate that during some period of their history they have been subjected to a very powerful metamorphic agen cy. The series of rocks which are presented to the eye are in volved in so great obscurity in regard to their geological periods or epochs as to have puzzled geologists for many years.* Taking into view the adjacent parts of New York and New Hampshire, we have three ranges of mountains nearly parallel : the Adi- rondac on the West, the White Mountains on the East and the Green Mountains lying between them separated from the former by the valley of Lake Champlain, and from the latter by the val ley of the Connecticut river. The Adirondac and the White Mountains differ entirely in their character from the Green Moun tains, for while the two former consist principally of granite and other igneous rocks, the latter, with the exception of a few trap dykes and a range of serpentine, is composed of highly meta morphic and crystalline shales. Aside from the peculiarity of the rock formations, the Geology of our State is interesting by reason of the numerous deposits of marine shells of the pleistocene period — some of which according to the late State Naturalist, are more than two miles inland from Lake Champlain, and, at least, two hundred feet above its level. The interest attached to the Geological Survey of a State so rich in natural and mineral curiosities as Vermont, will increase as the Survey advances. As the useful minerals continue to be more generally understood and more freely developed, and while the means of prosperous enterprize are continued to her citi- *See Appendix, No G and 7. 21 zens, we are enabled to have some glimpses of the relative age and connection of the rocks of the State as well as of some of the causes which have so modified and diversified the coast of this portion of our earth. So, too, we have a fair promise of being able to trace the connection of the rocks of Vermont with those of Canada, and of other States, as well as of other parts of the globe. Moreover the discovery of rare organic remains by my prede cessor has awakened considerable interest among paleontologists, and the paramount authority of fossils in ascertaining the rela tive ages of strata is maintained with additional force. I need not say that the moral influence of such discoveries, and in fact of the study of Natural History generally, must be healthful and elevating, for such discoveries u constitute the links in the mighty chain of causes and effects to connect created with uncreated mind." It is a source of painful regret that the career of Professors Thompson and Adams closed before the work assigned to them by the Legislature had been fully performed. It was the dying lamentation of Professor Thompson, who loved his native State and her people and devoted his life to an enquiry into her Civil and Natural History, that Providence could not permit him to finish the work for which he was appointed. It is due to his memory to state, that apart from the inroads upon his time and opportunities for research which disease had made during the latter part of his life, he met with obstacles in the way of completing the Geological Survey which were almost insurmountable. One and the chief of these he has alluded to in the following term s which I find among the various manuscripts which he left, and which by virtue of my appointment have been entrusted to my examination and custody. " In the first place I have been very much disappointed in re lation to the field-notes of our former State Geologist, the late Prof. C. B. Adams. I was aware during the progress of his la bors, that he kept many of his notes in a short hand of his own contriving, and remonstrated with him for so doing. Still I hoped to make out enough from them, to save the trouble of going over any considerable portion of the ground again. But in this I have been greatly disappointed. His notes I find to be exceedingly 22 brief and so obscurely expressed in a system of contractions to which he has left no key, that I find it nearly impossible to derive any information from them. After spending much time over these notes to very little purpose, I applied to Prof. Adams' widow, thinking it possible that she might be so well acquainted with his method of taking notes as to be able to decipher them ; but she declined undertaking it, thinking it doubtful about being able to make out anything from them which would be of service to me.'J With regard to the collection of " minerals, field-notes, maps and all preparations amassed by the first State Geologist for a final report upon the Geological Survey," I would here state that they were duly deposited in the State House in the care of the State Librarian, and subsequently taken into the custody of the Jate State Naturalist. The specimens which were in a proper con dition for a State Cabinet were suffered to remain at Montpelier, and the other specimens which have been since partially examined, trimmed and catalogued, I have ordered to be transported to Mont pelier. Those specimens which were in a proper condition have been temporarily arranged in the room set apart for that purpose, and the residue are collected in room No. 37 of the State House, to be distributed at an early day to the literary and medical in stitutions of the State which are entitled to the same, and the bal ance to be in readiness for future foreign exchanges when deemed desirable. Although at present not in such order and perfection as might be wished, yet they indicate the abundance and variety of the mineral wealth of Vermont, and suggest the benefits which will undoubtedly flow from its thorough development. In regard to the size of the specimens for the several collections, the rule adopted at the outset of the Geological Survey prescribed that, when the materials admitted, the specimens were to be three inches square and not less than one inch in thickness. Eight suites of these minerals duly trimmed, numbered and named were to be preserved, whose destination was to be as follows : One (and the best one when there was a choice,) for a State Collection at Montpelier ; one for the University of Vermont ; one for Middle- bury College ; one for Norwich University ; one for each of the Medical Colleges at Castleton and Woodstock; one for the Troy Conference Academy at Poultney and one to be the property of the State Geologist. With some exceptions, the specimens of more than two thou- 23 Band in each suite have been duly delivered to such of the afore^- mentioned institutions as were willing to pay the expenses of trans portation from the geological depots at Middlebury and Burling ton. A few fossils and specimens which have been recently trim med ana ticketed, have not yet been forwarded to their final destination. Rare and valuable specimens are placed where the State Na turalist can have ready access to them while preparing for publi cation his final Report on the Natural History of the State. The number of specimens of rocks, fossils and minerals, which are to un dergo a " full and scientific examination" is very great, and of these many minerals and metals are to be "described" in a full and scientific manner, to meet the requirements of the Statute of 1853. Apart from this laborious duty, careful and complete as says and analyses are to be made, by means of which a determin ation of the value of different ores and minerals can be secured j and when these duties of examination, description and analysis are performed, the results of the State Naturalist's labors are to be systematized and prepared for publication in the mode prescribed by the Statute. In the progress of the Geological Survey under Prof. Adams, he was assisted in the field labor by the Rev. Zadock Thompson, and the Rev. S. R. Hall of Craftsbury ; and the chemical analyses were performed in the well furnished laboratory of Yale College, by Denison Olmsted, Jun., of New Haven, Conn., who was com missioned as Assistant Geologist, and served in that capacity un til his death, August 15th, 1846. The report of Mr. Olmsted, forms a part of Prof. Adams' Second Annual Report, and is a valu able portion of the Appendix. Subsequently to Mr. Olmsted's death, Mr. Thomas S. Hunt, now of Montreal, was appointed As sistant State Geologist, in order that his valuable services might be secured in the Mineralogical department of the Survey, and his reports of the chemical analyses made by him were communicated to Professor Adams and appended to his reports on the Geological Survey, before Mr. Hunt accepted the position which he now holds of Chemist and Mineralogist to the Geological Survey of Canada. Other experienced gentlemen were engaged in field labor and as assistants. Dr. S. P. Lathrop, Messrs. L. F. Locke and Edward 24 Hitchcock, Jim., arc favorably noticed in Prof. Adams' Reports, and to Prof. Louis Agassiz of Cambridge ; Prof. James Hall and Dr. Ebenezer Emmons of Albany, N. Y ; Dr. Asa Fitch of Sa lem, N. Y; Prof. Benjamin Silliman, Jun., of New Haven, Conn., Dr. Samuel W. Thayer, now of Burlington, Vt., Dr. James Rob- bins of Chester, Vt., and others, was Prof. Adams greatly indebted for advice, assistance and friendly co-operation in his professional and responsible labors. If Prof. Adams had completed his origin al design of preparing a final Geological Report, the value of the services and aid of these learned gentlemen might have been in calculable. I am not aware that my predecessor Professor Thompson was regularly aided in his arduous task by an assistant Naturalist. He was, however, in constant correspondence with prominent Natu ralists in this country and abroad, and in intimate relations with his friend and medical adviser, Samuel W. Thayer, M. D., who has taken great interest in all matters connected with the Geological Survey of Vermont from its start, and also with Professor James Hall, of Albany, N. Y., who rendered aid near the close of Pro fessor Thompson's life in cataloguing valuable fossils, and in ma king scientific examination of rare trilobites which Professor Thompson had obtained in his researches throughout the State. Professor Henry Erni, then a Professor of Chemistry, Pharmacy and Toxicology in the Medical Department of the University of Vermont, made on his behalf some chemical analyses which are preserved in part among the manuscripts which were left incom plete by Professor Thompson at the time of his death. I greatly fear that a large portion of the labors of these assistants and cor respondents cannot now be made available to the world by reason of lapse of time and other untoward causes. Undoubtedly the vast array of notes and memoranda belonging to the Survey would have been of inestimable value if they had been prepared and kept in a more methodical and intelligible manner, and the difficulty of compiling final reports would have been materially lessened and their value greatly enhanced. At the last session of the General Assembly I find that the following resolution was adopted :* "Resolved by the Senate and House of Representatives, That *See Appendix, No. 3. 25 the Sergeant-at-Arms be and is hereby directed to set apart and prepare the committee room, numbered fourteen, for the use of the State Naturalist for the deposit and arrangement of the speci mens collected and to be collected in the Geological, Botanical and Zoological^Survey of the State." * This resolution which was so opportunely offered and adopted is prospective in its character and evidently contemplates the formation of a State Cabinet of the Natural History of Vermont — a purpose which will meet with the approval of every thought ful citizen. This important step has undoubtedly been taken towards the formation of such a Cabinet for the purpose of col lecting and preserving to all time, valuable specimens of the Nat- Ural History of the State, and affording a safe and attractive re pository for the discoveries resulting from the future researches of inquisitive and scientific inquirers. The minerals and other geological specimens already collected in great numbers by the State Geologist and State Naturalist will form the basis of the State Cabinet as this Resolution implies, to which great additions can hereafter be made in the botanical and zoological departments of Natural History. The State House seems to be the most central and, therefore, the most appropriate locality for such a Cabinet. Visited as the Capitol is and always will be at all times of the year, every rare object in such a Cabinet would be universally seen and duly ap preciated. Those persons who are making new discoveries in the mineral wealth of Vermont, and are desirous of exhibiting new and beautiful specimens of marble, serpentine, steatite, &c., to the largest number and in the most imposing and attractive manner would naturally contribute to it. Such contributions, originating as they might, possibly, in a wish to advertise the rare products of a particular locality will, of course, greatly tend to increase the beauty and add to the value of the State Cabinet. Such a collection as this resolution implies will also facilitate the too much neglected study of our Geology and Natural His tory. If the rocks of Vermont are arranged in such a collection according to their respective counties and the organic remains * See Appendix No. 8. 4 26 there exhibited, reveal the connection or prove the separation of certain strata and groups of rocks, the student of nature after examining them in the State Cabinet can at once repair to the localities where the rocks abound and thus familiarize himself in a short time with the Geology of the State. The wide range of animal and vegetable life* which belongs to Vermont will also present a wide field for scientific examination and the State Cabinet ought in time to possess specimens of all animals and vegetables which have lived or grown in Vermont, and each speci men presented or collected should be carefully preserved and named and the locality of each properly noted and all specimens calcu lated to illustrate the Ornithology, Erpetology, Icthyology and Entomology of the State should have a " local habitation and a name," in such a State Cabinet as the resolution contemplates. Since the adoption of this resolution, the Sergeant-at-arms has prepared the room assigned to the department of Natural History, under the advice of the late State Naturalist with the view to exhi bit until a more spacious room is procured, such specimens as are in readiness for the State Cabinet. The minerals and other objects collected by the State Geologist and State Naturalist which have been too long locked up and there by rendered comparatively useless for any pratical purpose will upon being properly prepared, labelled and arranged be greatly enhanced in value. The duty of such a preparation and arrange ment has been intrusted to my assistant Albert D Hager, "Esq., of Proctorsville, Vermont, whose experience and skill fit him for the thorough and acceptable execution of this important trust and I respectfully submit to your perusal Mr. Hager's Report which is appended to this communication and bespeak for the suggestions contained therein a thoughtful consideration. I take also this opportunity to express my grateful acknowledg ment to my friend George F. Houghton, Esq., of St. Albans, Ver mont, to whom I have issued a commission as Assistant State Na turalist and who has rendered me important service in the course of my labors as State Naturalist. I have thus presented to your Excellency, in as brief a manner as the number and nature of the topics alluded to in this commu nication would permit, the several facts which tend to indicate the present condition of the Geological Survey. Although the Stat- 27 ute of 1853 requires no report to be made until " sufficient facts and materials shall have been collected upon the subject of Phys ical Geography, Scientific Geology and Mineralogy of the State to form a volume of not less than five hundred pages octavo," yet the peculiar circumstances I have referred to and the natural and laudable curiosity of the people of the State in regard to a matter in which they have manifested great interest from the outset of the Geological Survey, seemed to require of me a plain and un varnished statement of such facts and explanations as would satis fy all reasonable enquiries. In drawing this communication to an abrupt close I would, with due diffidence, express a hope that this statement and the appen dix thereto may be laid before the General Assembly at your early convenience if your Excellency deem it proper, with such accompanying executive remarks as may secure to it a patient perusal and a candid consideration. I have the honor to remain Your Excellency's obedient servant, AUGUSTUS YOUNG, State Naturalist. ST. ALBANS VERMONT, October 10th, 1856. REPORT OF ALBERT D. HAGER, ASSISTANT STATE NATURALIST. HON, AUGUSTUS YOUNG. State Naturalist : DEAR SIB. : — In compliance with the instructions em braced in the commission of Assistant State Naturalist which you were kind enough to issue to me, I lost no time in _ proceeding to the Geological depot at Burlington. This depot, as you are aware, was a small building near the dwelling house of the late State Naturalist which had been used for a number of years by Professors Adams and Thompson during the continuance of their geological labors. I found that several boxes had been duly pack ed with minerals, and were in readiness to be forwarded to their final destination. Much the larger proportion of specimens, how ever, were in trays and required to be carefully assorted prepara tory to being packed and boxed up. Inasmuch as the value of mineralogical cabinets greatly depends upon the character of the specimens, and a correct statement of their locality and proper ties, I aimed to pack each mineral and fossil with great care, wrapping with each specimen in all cases the appropriate label indicating its name and locality and in every instance of doubt had reference to the Catalogues which you entrusted to me for my examination and guidance. You are aware that the specimens had been twice partly ar ranged by the late State Geologist and late State Naturalist ; and the disadvantages under which I labored were increased by the system of short hand which Professor Adams used in his memo randum books. This short hand and initials, written for the most part jn pencil were in many cases perplexing and unintelligible. But in every instance where reliable information of the locality of all speci^ mens could not be had, they were placed among those where local- 30 ity was uncertain or unknown — certainty being an indispensible desideratum in the formation of a cabinet of minerals. In the instructions given by His Excellency Governor Slade to the first State Geologist, he was directed " to procure one suite of specimens fora State collection, and one for each of the three liter ary, and two medical colleges, and one for the Troy Conference Academy at Poultney.* Some of these institutions have not sent for their quota, and, unfortunately the number received by each institution was not minuted down in the books connected with the Geological Survey in such a manner (if at all) as to be a guide to any one but those who forwarded them. Probably the late Pro fessors Adams and Thompson would have had no difficulty in discharging this part of their duty— while others might be greatly embarrassed who have no access to their private correspondence or key to their memoranda. But I have endeavored to assign to each institution its quota of minerals as set apart and numbered by Professor Thompson — packing the contents of each tray and box and noting them care fully in my book of memoranda ; and agreeably to your order, have forwarded them to Montpelier, so that the entire collection of minerals obtained by Professors Adams and Thompson is now at the Capitol either in number fourteen or number thirty-seven of the State House except what have already been forwarded to their final destination. The number already collected for the suites as con templated by Governor Slade amounts to about twenty-seven hundred specimens for the State Cabinet, and a like number for each of the aforementioned literary institutions and medical col leges of Vermont, or about twenty thousand specimens, including a large number of surplus specimens which may be useful for fu ture exchanges. It will be my aim to collect, pack and get in readiness all of the minerals and fossils assigned for each institution, so that each col lege and literary institution can procure its quota upon applica tion at the State House, during the session of the Legislature, and if I am present at the Capitol I shall take pleasure in facili tating their delivery. With respect to other kinds of property belonging to the State which was stored in the geological depot at Burlington, I took *See Professor Adams First Annual Report, page 7. 31 them into my custody under your directions and forwarded them to Montpelier. They consist of the following articles : sixty-three boxes for holding and packing minerals, one hundred trays for holding and assorting minerals, one table, one anvil and block, five maps, fifty sections of maps, two chairs, two sledges, six hammers, one drill, one iron bar, one box chisel, one tape measure, and a valuable barometer. Sixty-two boxes and seventeen trays filled with minerals and fossils, were forwarded from Burlington and delivered at the State House. In pursuance of the Joint Resolution of the Legislature passed in 185c, the Sergeant-at-Arms has fitted up room numbered four teen in the State House, under the advice and suggestions received from Prof, Thompson in his lifetime. This room is assigned for the " use of the State Naturalist, and for the deposit aud arrange ment of the specimens collected and to be collected in the geologi cal, botanical and zoological survey of the State." In the arrangement of the cases as made by order of the late State .Naturalist, it is apparent that they were intended for the re ception of specimens of the birds, fishes, reptiles, insects and other objects calculated to illustrate the Natural History of Vermont, as well as for the reception of Vermont minerals and fossils. I have accordingly arranged the geological specimens in the division originally designed for their reception — thinking it high ly probable that the State of Vermont might at no distant day procure if possible the very valuable private collection of the pro ducts of the State, which Prof. Zadock Thompson had taken pains to collect during the last thirty years of his life, and which col lection is now in the possession of Mrs. Thompson, his widow, at Burlington. This being exclusively a Vermont collection, and embracing objects in all departments of Natural History, ought to be preserved entire, and it has occurred to me that the most ap propriate place for its exhibition and preservation would be at the State House. In room numbered thirty-seven I found about twenty-five hun dred geological and mineralogical specimens trimmed and number ed — a due proportion of which I have removed to room numbered fourteen and arranged in the case prepared under the direction of Prof. Thompson ; but the case being insufficient for the reception of the entire number of specimens, another case was made at my suggestion which will be soon filled with specimens. 32 At first glance, it might appear that the State Cabinet contains too many specimens from the same or adjacent localities ; and to the casual observer, a greater degree of interest in the mineralogy of the State might be awakened, if the specimens were fewer in number and art had been employed to exhibit the beauty of each to its greatest advantage. For instance, the polished specimen of Isle La Motte marble, and the beautiful slabs of Verde Antique marble from Roxbury and Cavendish, elicit the admiration of each spectator, while the rough and unpolished rocks from the same quarries possibly attract no notice whatever. But the careful student of Natural History and the ardent de votee of geological science desire an exhibition of the material in the rough, and all the forms in which it is found in its natural bed. Such enquirers are not satisfied with a superficial glance at the numerous fossils found in and forming the Isle La Motte mar ble, and contemplating the changes that have been wrought to render whole races of animated nature extinct and entombed as he sees them, and with a great stride pass from them to an examina tion of the beautiful statuary marbles of Vermont. He desires to examine the intervening groups to determine if possible, whether there be any connection between the two varieties, and if so, to note the difference arid ascertain the producing cause. It is found that as the limestone approaches the upheaved rocks it becomes saccharoidal or sparry, and apparently destitute of fos sils, and eminent geologists are of opinion that our beautiful white marbles are of fossiliferous origin, and altered by the agency of heat and other causes, and that the white unspotted memorial stones in our burying places are themselves the charnel house of myriads of beings that once crawled upon ocean's bed, or sported in the waters of the mighty deep. In arranging the minerals in the case ordered by Professor Thompson I have endeavored to follow as nearly as possible the plan adopted by your predecessors ; but in the new case I propose with your consent, to vary so far from their plan as to present on a label the full name of the mineral or fossil with that of the locality and d .nor when known ; by means of which the spectator will be relieved from the disagreeable necessity of consulting a vol uminous catalogue to ascertain the required facts and I propose to append the appropriate number to the label and place it in itd proper place upon the catalogue; 33 I would in this connection, remark that the minerals in the State collection as well as those sent to and designed for the different col leges and institutions before mentioned, have been hitherto barely numbered ; and in order to ascertain their names, locality &c. reference to a corresponding number in manuscript catalogue was necessary, to supply the desired information. It occurred to me (and your directions clearly point out this desideratum,) that the names and locality should be legibly written or printed and affixed k/each specimen, and thus afford the spectator the required infor mation from an inspection of the mineral itself. Accordingly I have thought it desirable to have printed labels placed upon the minerals with their appropriate number corresponding to the one on the catalogue, and have ordered a suitable quantity of labels to be printed so as to supply the differ ent institutions having a like collection of minerals from the same localities and collected by the same geologist. These labels when in readiness will be transmitted to their final destination upon ap plication of those interested-. It would give me great pleasure if I could arrange the mine rals and fossils in groups and in the order in which they occur; For instance, I would be glad to arrange in one case the rocks and fossils belonging to the Champlain division by themselves, so as to indicate the natural order in which the formations occur — be ginning with the calciferous sandstone and following in order the birds-eye limestone, Isle La Motte limestone, Trenton limestone, tltica slate and Hudson River shales to the red sandstone formation; In another case there might be arranged the Taconic group of rocks, giving a separate place to the subdivisions of roofing slatej sparry limestone, magnesian slate, Vermont marbles and granular quartz, and so on, until all the minerals and fossils of the State of Vermont are represented fully, and each in its proper place. With this arrangement there should be appended to each case a brief description of the group or system therein exhibited, its locality, extent, position and age, compared with other groups represented in adjacent cases. But in the small room assigned by the Legislature for the ex hibition of the specimens already collected, and hereafter to be col- 5 84 lected to illustrate the Natural History of the State of Vermont, this arrangement could not be thoroughly carried out. If, how ever the Legislature should deem it expedient to assign the ad joining room on the east, and order an opening to be made so as to unite the two rooms, there would be ample space to carry out the plan I have suggested, and thus exhibit in a convenient man ner the various specimens of scientific and economical interest with which Vermont, more than any other State in the Union abounds. I would, in this connection, remark that many prominent citi zens of our State have shown their willingness and desire to pro mote the success of this undertaking by making voluntary contri butions to the State collection, and others have expressed a de termination to do so, now that suitable cases are prepared for the reception and exhibition of specimens. To such as propose furnishing specimens of marble, slate, stea tite,