The Geology of the Elizabeth Mine, Vermont
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Poster Final
Evidence for polyphase deformation in the mylonitic zones bounding the Chester and Athens Domes, in southeastern Vermont, from 40Ar/39Ar geochronology Schnalzer, K., Webb, L., McCarthy, K., University of Vermont Department of Geology, Burlington Vermont, USA CLM 40 39 Sample Mineral Assemblage Metamorphic Facies Abstract Microstructure and Ar/ Ar Geochronology 18CD08A Quartz, Muscovite, Biotite, Feldspar, Epidote Upper Greenschist to Lower Amphibolite The Chester and Athens Domes are a composite mantled gneiss QC Twelve samples were collected during the fall of 2018 from the shear zones bounding the Chester and Athens Domes for 18CD08B Quartz, Biotite, Feldspar, Amphibole Amphibolite Facies 18CD08C Quartz, Muscovite, Biotite, Feldspar, Epidote Upper Greenschist to Lower Amphibolite dome in southeast Vermont. While debate persists regarding Me 40 39 microstructural analysis and Ar/ Ar age dating. These samples were divided between two transects, one in the northeastern 18CD08D Quartz, Muscovite, Biotite, Feldspar, Garnet Upper Greenschist to Lower Amphibolite the mechanisms of dome formation, most workers consider the VT NH section of the Chester dome and the second in the southern section of the Athens dome. These samples were analyzed by X-ray 18CD08E Quartz, Muscovite Greenschist Facies domes to have formed during the Acadian Orogeny. This study diraction in the fall of 2018. Oriented, orthogonal thin sections were also prepared for each of the twelve samples. The thin sec- 18CD09A Quartz, Amphibole Amphib olite Facies 40 CVGT integrates the results of Ar/Ar step-heating of single mineral NY tions named with an “X” were cut parallel to the stretching lineation (X) and normal to the foliation (Z) whereas the thin sections 18CD09B Quartz, Biotite, Feldspar, Amphibole, Muscovite Amphibolite Facies grains, or small multigrain aliquots, with data from microstruc- 18CD09C Quartz, Amphibole, Feldspar Amphibolite Facies named with a “Y” have been cut perpendicular to the ‘X-Z’ thin section. -
Mineral Industries and Geology of Certain Areas
REPORT -->/ OF TFIE STATE GEOLOGIST ON THE S 7 (9 Mineral Industries and Geology 12 of Certain Areas OF -o VERMONT. 'I 6 '4 4 7 THIRD OF THIS SERIES, 1901-1902. 4 0 4 S GEORGE H. PERKINS, Ph. D., 2 5 State Geologist and Professor of Geology, University of Vermont 7 8 9 0 2 4 9 1 T. B. LYON C0MI'ANV, I'RINTERS, ALILiNY, New VORK. 1902. CONTENTS. PG K 1NTRODFCTION 5 SKETCH OF THE LIFE OF ZADOCK THOMPSON, G. H. Perkins ----------------- 7 LIST OF OFFICIAL REPORTS ON VERMONT GEOLOGY ----------------- -- -- ----- 14 LIST OF OTHER PUBLICATIONS ON VERMONT GEOLOGY ------- - ---------- ----- 19 SKETCH OF THE LIFE OF AUGUSTUS WING, H. M. Seely -------------------- -- 22 REPORT ON MINERAL INDUSTRIES, G. H. Perkins ............................ 35 Metallic Products ------------------------------------------------------ 32 U seful Minerals ------------------------------------------------------- 35 Building and Ornamental Stone ----------------------------------------- 40 THE GRANITE AREA OF BAItRE, G. I. Finlay------------------------------ --- 46 Topography and Surface Geology ------------------------------------ - -- 46 General Geology, Petrography of the Schists -------------------------- - -- 48 Description and Petrography of Granite Areas ----------------------------51 THE TERRANES OF ORANGE COUNTY, VERMONT, C. H. Richardson ------------ 6i Topography---------------------------- -............................. 6z Chemistry ------------------------------------------------------------66 Geology -------------------------------------------------------------- -
The Geology of the Lyndonville Area, Vermont
THE GEOLOGY OF THE LYNDONVILLE AREA, VERMONT By JOHN G. DENNIS VERMONT GEOLOGICAL SURVEY CHARLES G. DOLL, Stale Geologist Published by VERMONT DEVELOPMENT COMMISSION MONTPELIER, VERMONT BULLETIN NO. 8 1956 Lake Willoughby, seen from its north shore. TABLE OF CONTENTS ABSTRACT ......................... 7 INTRODUCTION 8 Location 8 Geologic Setting ..................... 8 Previous Work ...................... 8 Purpose of Study ..................... 9 Method of Study 10 Acknowledgments . 11 Physiography ...................... 11 STRATIGRAPHY ....................... 16 Lithologic Descriptions .................. 16 Waits River Formation ................. 16 General Statement .................. 16 Distribution ..................... 16 Age 17 Lithological Detail .................. 17 Gile Mountain Formation ................ 19 General Statement .................. 19 Distribution ..................... 20 Lithologic Detail ................... 20 The Waits River /Gile Mountain Contact ........ 22 Age........................... 23 Preliminary Remarks .................. 23 Early Work ...................... 23 Richardson's Work in Eastern Vermont .......... 25 Recent Detailed Mapping in the Waits River Formation. 26 Detailed Work in Canada ................ 28 Relationships in the Connecticut River Valley, Vermont and New Hampshire ................... 30 Summary of Presently Held Opinions ........... 32 Discussion ....................... 32 Conclusions ...................... 33 STRUCTURE 34 Introduction and Structural Setting 34 Terminology ...................... -
Vermont Geology History Slideshow
Vermont’s Geologic History May 1st Earth’s Early History GEOLOGIC TIME SCALE The Archean and Proterozoic Eons make up the bulk of Earth’s history Oldest Rocks Found So Far The Formation of Earth: This date comes from rocky meteorites, similar in composition to Earth, that formed ~4.6 Ga (billion years ago). Rocks of Archean Age (3.8–2.5 Ga) occur on every continent. The closest Archean rocks to us are in northern Minnesota. During the Proterozoic Eon (2.5–0.54 Ga) plate tectonic processes similar to those operating today began. Rocks of Proterozoic Age (2.5–0.54 Ga) make up large parts of the continents. In combination with the older Archean rocks, these old rocks make up the core of most continents. Most rocks in New England formed during the Phanerozoic Eon. This is the time when fossils are abundant and pervasive. Stratigraphic Column: Sedimentary rocks occurring in the Champlain Valley are displayed as a vertical stack, oldest at the bottom and youngest at the top. Purple = Shale Blue = Limestone Grey = Dolostone Orange = Sandstone Continuous layers of sedimentary rock consisting of the same type or types of rock are given names, e.g. The “Glens Falls Limestone” or The “Monkton Formation.” You’ve seen some of these rocks on today’s field trip. Vermont Geologic History Dunham dolostone Cheshire Quartz Sandstone: ~530 million years old Gneiss: ~1,100 million years old The oldest rocks in Vermont are gneisses. These rocks are ~1.0–1.3 billion years old. Graph shows the Pressure/Temperature “environments” that different metamorphic rocks form in. -
This Is the Bennington Museum Library's “History-Biography” File, with Information of Regional Relevance Accumulated O
This is the Bennington Museum library’s “history-biography” file, with information of regional relevance accumulated over many years. Descriptions here attempt to summarize the contents of each file. The library also has two other large files of family research and of sixty years of genealogical correspondence, which are not yet available online. Abenaki Nation. Missisquoi fishing rights in Vermont; State of Vermont vs Harold St. Francis, et al.; “The Abenakis: Aborigines of Vermont, Part II” (top page only) by Stephen Laurent. Abercrombie Expedition. General James Abercrombie; French and Indian Wars; Fort Ticonderoga. “The Abercrombie Expedition” by Russell Bellico Adirondack Life, Vol. XIV, No. 4, July-August 1983. Academies. Reproduction of subscription form Bennington, Vermont (April 5, 1773) to build a school house by September 20, and committee to supervise the construction north of the Meeting House to consist of three men including Ebenezer Wood and Elijah Dewey; “An 18th century schoolhouse,” by Ruth Levin, Bennington Banner (May 27, 1981), cites and reproduces April 5, 1773 school house subscription form; “Bennington's early academies,” by Joseph Parks, Bennington Banner (May 10, 1975); “Just Pokin' Around,” by Agnes Rockwood, Bennington Banner (June 15, 1973), re: history of Bennington Graded School Building (1914), between Park and School Streets; “Yankee article features Ben Thompson, MAU designer,” Bennington Banner (December 13, 1976); “The fall term of Bennington Academy will commence (duration of term and tuition) . ,” Vermont Gazette, (September 16, 1834); “Miss Boll of Massachusetts, has opened a boarding school . ,” Bennington Newsletter (August 5, 1812; “Mrs. Holland has opened a boarding school in Bennington . .,” Green Mountain Farmer (January 11, 1811); “Mr. -
TRANSPORTATION THEME Statewide, Vermont
VERMONT TRANSPORTATION THEME Statewide, Vermont Prepared for: Prepared by: Vermont Agency of Transportation Louis Berger 1 National Life Drive 20 Corporate Woods Blvd. Montpelier, Vermont 05633-5001 Albany, New York 12211 June 21, 2018 Cover Image Source A) Landscape Change 1938 A B) Landscape Change 1990 F C) Landscape Change [1890] D) Landscape Change 1940 E B E) Stoddard 1898 C F) Landdscape Change [1906] D VERMONT TRANSPORTATION THEME Statewide, Vermont Prepared for: Vermont Agency of Transportation 1 National Life Drive Montpelier, Vermont 05633-5001 Prepared by: Louis Berger 20 Corporate Woods Blvd. Albany, New York 12211 June 21, 2018 TABLE OF CONTENTS I. Vermont Transportation Theme .................................................................................... 1 A. Introduction .......................................................................................................... 1 B. Waterways ............................................................................................................ 3 Early Water Transportation (1750-1790) ............................................................. 3 Golden Age of Water Navigation (1790-1870) ................................................... 5 Decline of Water Commerce (1870-1940) .......................................................... 7 Resurgence of River Commerce and Recreational Boating (1940-1978) ........... 9 C. Roads.................................................................................................................... 10 Military Roads (1759-1781) -
Structures in the Dog River Fault Zone Between Northfield and Montpelier, Vermont
University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1987 Structures in the Dog River Fault Zone between Northfield and Montpelier, Vermont Westerman, David S. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Westerman, David S., "Structures in the Dog River Fault Zone between Northfield and Montpelier, Vermont" (1987). NEIGC Trips. 413. https://scholars.unh.edu/neigc_trips/413 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. A -6 STRUCTURES IN THE DOG RIVER FAULT ZONE BETWEEN NORTHFIELD AND MONTPELIER, VERMONT David S. Westerman Department of Earth Science Norwich University Northfield, Vermont 05663 INTRODUCTION The purposes of this trip are to examine the lithologic and structural character of rocks exposed in the Dog River fault zone (DRFZ) along a traverse between Northfield and Montpelier, Vermont, and in the process to better understand their tectonic significance. The rocks exposed within the DRFZ have long been recognized as significant from a stratigraphic standpoint, but recognition of their structural character is recent. This author has done detailed mapping along only a 10-mile section of the zone, but reconnaissance studies suggest that its structural character is similar north to the Quebec border and south as far as Randolph, Vermont, a distance of about 80 miles. -
The Prosper Valley Vignettes
THE PROSPER VALLEY VIGNETTES - A natural and cultural history of the watershed connecting the Vermont towns of Barnard, Bridgewater, Pomfret and Woodstock – By Corrie Miller, Winter 2006/07 By Corrie Miller, Winter 2006/07 THE PROSPER VALLEY VIGNETTES: At Home in the Valley – An Introduction My love affair with this valley began with a herd of cattle. I had just gotten a job in Woodstock and was driving along Route 12 to look at an apartment in Barnard. At the urging of a flashing yellow light, I slowed my car to a stop in front of a line of cows crossing the road. At the time, I didn’t know that I would take the apartment and travel this corridor every day for a year, eventually becoming familiar with every turn in the river and every slope on the surrounding hills. I also didn’t know that I would return to this valley three years later to do my master’s research, this time leaving my car behind and donning a pair of hiking boots to explore the same stream and hills in greater depth. In that moment as I watched the cows cross the road, I only knew that the valley already felt like home. Gulf Road Cut (left). Barnard, VT. Cut walls of bedrock mark the entrance into the Prosper Valley on Route 12. Photo courtesy of NPS. Gulf Brook Headwaters (right). Barnard, VT. Water drains the surrounding highlands and converges in this cascading stream in the Barnard Gulf, establishing the Gulf Brook. Each morning on my drive south to Woodstock, I crested the hill near the Barnard Gulf and coasted down the steep grade into the basin I now know as the Prosper Valley. -
MINERAL COLLECTING in VERMONT by Raymond W. Crant
MINERAL COLLECTING IN VERMONT by Raymond W. Crant Vermont Geological Survey, Charles C. Doll, State Geologist Department of Water Resources, Montpelier, Vermont SPECIAL PUBLICATION NO, 2 1968 LIST OF ILLUSTRATIONS Figures Page 1. Index Map of Vermont Mineral L()cIities . 3 38. Slate Quarry, Poultney ............................................. 31 2. Metaiimrphic Map of Vermont ................................. 4 .39. NI ap showing the location of the mineral area, Rouiid 3. Geo logic NI ap of Vernio i it ....................................... 7 Hill, Shrewshorv................................. ..................... 32 4. Topograpl ii NI a!) S y 0)1)0 Is ....................................... 10 40. Map showing the location of the Molybdenite Prospect 5. Map showing the location of the Vermont Kaolin Coin- (1) and Copperas Hill Mines (2), Cuttingsville .............32 paiiy Quarry (1) and Monkton Iron Ore Beds (2) ......... 14 41. Map showing the location of the Marble Quarry, Dorset 6. Map showing the location of the Huntley Quarry, Leices- Nit., South Danhv ..................................................... 33 terJunction ............................................................. 15 42. Map showing the location of the Devil's Den, Nit. Tahor 34 7. Calcite crystals from the Huntley Quarry, Leicester 43. Smoky Quartz crystal from Devil's Den, Mt. Tabor ...... .34 Junction (times 1.6) .................................................. 15 44. Map showing the location of the Roacicuts on Route 155, 8. Map showing the location of -
Stratigraphie Sequence of the Gile Mountain and Waits River Formations Near Royalton, Vermont
Stratigraphie sequence of the Gile Mountain and Waits River Formations near Royalton, Vermont GEORGE W. FISHER I jjepartment Qf Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland 21218 PAUL KARABINOS ABSTRACT been controversial. This uncertainty has the Gile Mountain belt near Royalton, The stratigraphie sequence of the Gile given rise to numerous difficulties in inter- Vermont, show that the Gile Mountain Mountain and Waits River Formations, preting the regional structure of eastern Formation is younger than the Waits River two major Silurian-Devonian lithostrati- Vermont. Extensive sequences of compo- Formation, indicating that the belt is a graphic units in eastern Vermont, has long sitionally graded beds at 19 localities across syncline. Canada * • t? * * i * *r ; * T v . Figure 2. Compositionally graded beds of micaceous quartzite rhythmically interbedded with garnet-mica schist in Gile Mountain Formation, 50 m east of contact with Waits River Formation in a Figure 1. Extent of Gile Mountain (Dgm) and Waits River pasture 2.8 km west of Royalton, Vermont (loc. A, Fig. 7). View is (Dwr) Formations in eastern Vermont, adapted from Doll and looking north; grading indicates tops to east, toward Gile others (1961); rectangle indicates area shown in Figure 7, at Royal- Mountain Formation. S! is parallel to bedding; S2 is parallel to pen. ton, Vermont. Pen is 16 cm long. Geological Society of America Bulletin, Part I, v. 91, p. 282-286, 7 figs., May 1980, Doc. no. 00506. 282 Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/91/5/282/3418989/i0016-7606-91-5-282.pdf by guest on 27 September 2021 GILÈ MOUNTAIN AND WAITS RIVER FORMATIONS, VERMONT 283 INTRODUCTION vidual graded beds can be traced laterally (see Fig. -
Thomas Pollard: a Cornish Miner in the Appalachians
Thomas Pollard: A Cornish Miner in the Appalachians By Collamer M. Abbott The nomadic life of a large number of Ap sided at the mine in Vershire, then in \'{fest palachian miners is epitomized in the life of Fairlee, a mile and a half to the east, and finally TI1omas Pollard. Like many of his fellow work in Post Mills, three miles to the southeast. Pol ers, Pollard-superintendent of the Ely copper lard ultimately moved to a fmm he purchased in mine in Vershire, Vermont, dwing the 1850s and Dover, New jersey. There he lived the rest of 1860s--was used to pulling up stakes and mov his life w hile actively exploring, prospecting, and ing to other mines, near or far. A Cornish miner developing mines from Pennsylvania to Maine with extensive practical experience, he was al for investors still interested in Appalachian de ways on the go, prospecting, superintending, or posit<; despite the boom on the western mining developing mineral deposits for those capitalists ti·ontier. willing to invest in speculative ente1p1ises along Pollard stayed put through the 1860s and into the Appalachian Chain during the last half of the 1870s, during his tenure as "captain" and the nineteenth century. As did other veterans superintendent of the mine in Vershire, fanning of Cornish harclrock mining, Pollard inspired his pmpe1ty, selling and trading his produce, and confidence in investors who knew nothing about boarding single miners. Although Pollard says the subject. Thomas Pollard's diaries, now in vety little about his wife in his dia1y, she, with the collections of the Vermont Historical Soci the help of hired girls, carried the burden of ety, can help us both see and interpret the pat boarding d1e miners. -
4.PART-1.Pdf
Part One The Physical Setting The Physical Setting s naturalists, land managers, and hikers, we constantly look for patterns in the landscape that help us make sense of the natural world. Of the things A that create patterns of natural community distribution, four are especially important and far reaching. The nature of the bedrock that underlies Vermont has a major influence on the topography of the land, the chemistry of the soils, and the distribution of particular plants, especially when the bedrock is near the surface. The surficial deposits (the gravels, sands, silts, and clays that were laid down during and after the Pleistocene glaciation) can completely mask the effect of underlying bedrock where these deposits are thick. Climate affects natural community distribution, both indirectly by causing glaciation and directly by influencing the distribution of plants and animals. Finally, humans have their impacts on the land, clearing, planting, reaping, mining, dredging, filling, and also conserving natural lands. Table 1: Geologic Time Scale Era Periods Time Significant Events in Vermont Geology (Millions of years before present) PrecambrianPrecambrian Over 540 Grenville Orogeny joins plates in Grenville supercontinent and uplifts Adirondacks. Paleozoic Cambrian 540 to 443 Plates move apart. Green Mountains and Ordovician Taconic rocks laid down in deep water of Iapetus Ocean. Champlain Valley and Vermont Valley rocks laid down in shallow sea. Taconic Orogeny adds Taconic island arc to proto-North America, raises Green Mountains and causes major thrusting. Iapetus Ocean begins to close. Silurian 443 to 354 Vermont Piedmont rocks laid down in eastern Devonian Iapetus. Acadian Orogeny adds eastern New England to proto-North America and changes Green Mountains.