Dorset Village Plan
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Taconic Physiography
Bulletin No. 272 ' Series B, Descriptive Geology, 74 DEPARTMENT OF THE INTERIOR . UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR 4 t TACONIC PHYSIOGRAPHY BY T. NELSON DALE WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS. Page. Letter of transinittal......................................._......--..... 7 Introduction..........I..................................................... 9 Literature...........:.......................... ........................... 9 Land form __._..___.._.___________..___._____......__..__...._..._--..-..... 18 Green Mountain Range ..................... .......................... 18 Taconic Range .............................'............:.............. 19 Transverse valleys._-_-_.-..._.-......-....___-..-___-_....--_.-.._-- 19 Longitudinal valleys ............................................. ^...... 20 Bensselaer Plateau .................................................... 20 Hudson-Champlain valley................ ..-,..-.-.--.----.-..-...... 21 The Taconic landscape..................................................... 21 The lakes............................................................ 22 Topographic types .............,.....:..............'.................... 23 Plateau type ...--....---....-.-.-.-.--....-...... --.---.-.-..-.--... 23 Taconic type ...-..........-........-----............--......----.-.-- 28 Hudson-Champlain type ......................"...............--....... 23 Rock material..........................'.......'..---..-.....-...-.--.-.-. 23 Harder rocks ....---...............-.-.....-.-...--.-......... -
Preliminary Bedrock Geologic Map of the Chittenden Quadrangle Rutland County, Vermont
U.S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Preliminary Bedrock Geologic Map of the Chittenden Quadrangle Rutland County, Vermont By Nicholas M. Ratcliffe U.S. Geological Survey Open File Report 97-703 1997 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards nor with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. INTRODUCTION The bedrock of the Chittenden quadrangle consists of Middle Proterozoic through Cambrian metasedimentary and metaigneous rocks that lie along the western flank of the Green Mountain massif in south-central Vermont. The Green Mountain massif is cored by highly deformed and extensively retrograded schists and schistose gneisses derived from once high-grade gneisses that were intruded and originally metamorphosed during the Grenville orogeny prior to about 950 Ma. Upper Proterozoic through Cambrian metaclastic rocks, referred to as the western cover sequence, form a cover sequence that was deposited unconformably on the older schists and gneisses. The upper part of the cover sequence consists of marine-shelf carbonate rocks of the Vermont Valley sequence that developed on the stable Atlantic-type continental margin prior to the deformation in the Taconian orogeny during the Middle to Upper Ordovician. In the Taconian orogeny, rocks of this area were thrust faulted and metamorphosed to biotite grade. The basement rocks were altered by low-grade remetamorphism and hydration to such an extent that the Grenvillian mineral assemblages, schistosity, and gneissosity are presently barely recognizable. -
Green Mountain National Forest Supervisor’S Office 1-802-747-6700 TTY 1-802-747-6765
Green Mountain United States Department of Agriculture National Forest Forest Service Eastern Region Record of Decision R9-GM-FEIS- Final Environmental Impact Statement ROD February 2006 To Accompany the Land and Resource Management Plan This document is available in large print. Contact the Green Mountain National Forest Supervisor’s Office 1-802-747-6700 TTY 1-802-747-6765 The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, or marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326-W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250- 9410 or call (202) 720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Record of Decision Final Environmental Impact Statement to accompany the Land and Resource Management Plan Green Mountain National Forest Eastern Region Milwaukee, Wisconsin February 2006 Responsible Agency USDA Forest Service Responsible Official Randy Moore, Regional Forester Gaslight Building, Suite 800 626 E. Wisconsin Avenue Milwaukee, WI 53203 414-297-3765 For further information contact Melissa -
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. -
VT Sheet3 DMU CMU Final
U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the SCIENTIFIC INVESTIGATIONS MAP 3184 U.S. GEOLOGICAL SURVEY STATE OF VERMONT, VERMONT AGENCY OF NATURAL RESOURCES, BEDROCK GEOLOGIC MAP OF VERMONT MARCIA K. McNUTT, DIRECTOR VERMONT GEOLOGICAL SURVEY SHEET 3 OF 3 (FRONT) LAURENCE R. BECKER, STATE GEOLOGIST CORRELATION OF MAP UNITS (Some lesser units listed in the Description of Map Units may not be shown here. Asterisk indicates U-Pb zircon age.) NEW HAMPSHIRE PLUTONIC SUITE Zfc 2 OTHER DEVONIAN Carbonaceous albite schist member—Gray to medium-dark-gray, Y lga Ludlow Mountain aplitic gneiss (Middle Mesoproterozoic)—Light-gray to Owwu Sandy phyllite, granofels, and cherty phyllite (Upper Ordovician)—Gray and Belvidere Mountain Structural Complex (Cambrian and Neoproterozoic) Compton Formation (Lower Devonian) Oarq Coarsely porphyritic, greenish-gray, light-bluish-gray, or medium-bluish-gray GRANITES rusty-weathering, carbonaceous albite-chlorite-quartz-muscovite schist, contain- white, very fine grained microcline-plagioclase-quartz (±magnetite) aplitic gneiss; grayish-green rocks associated with Whipstock breccia on Whipstock Hill but of metarhyolite tuff, lapilli tuff, and tuff breccia. Quartz and plagioclase pheno- STAGE GRANITE BLACK FRENCH AND PLUTONS STAGE Brandon Lignite POND ing porphyroblasts of black albite. Unit resembles gray albitic granofels and contains sparing amounts of biotite, and secondary muscovite. Unit interpreted to uncertain correlation Zbu Ultramafic rocks—Brown to white-weathering, green, massive, moderately to Dco Metasandstone member—Light-gray to tan, micaceous, locally calcareous crysts commonly as large as 5 mm DIKES MOUNTAIN AGE UNCERTAIN 2 2 Tmb GRANITE GRANITE schist of the Hoosac Formation (Zhab) be border facies of Y lgg. -
The Vermont Stone Trail 2016
The Vermont Stone Trail A Visitor’s Guide to Granite, Marble and Slate in the Green Mountain State Lake Willoughby Photo courtesy Annalie Babson Table of Contents The 2 The Story of Stone in Vermont Vermont 6 Southern Region Stone Trail 14 Central Region 32 Northern Region A Visitor’s Guide to Granite, Marble and Slate in the Green Mountain State Using this Guide The information in this guide is arranged into southern, central and northern regions of Vermont. Each section begins with a map Serendipity and the dynamic nature of the earth’s showing the number and location of landmarks and points of interest crust gave Vermont rare and excellent deposits of described in the guide pages. The guide pages include a landmark granite, marble and slate. With hard work, description and graphic icons creativity and the efforts of many, each of these indicating the type of stone, features and activities for each resources has been developed into a highly location. successful industry that continues to offer products Landmark Legend that are sought after throughout the world. Type of stone The Vermont Stone Trail is a guide to geological Marble regions of Vermont where granite, marble and slate Slate Granite were quarried, manufactured and utilized. Combination Vermont’s diverse geologic resources have been Other Dimensional used to create some of the finest buildings, Stone provocative memorials and stunning works of art Landmark features and activities found around the world. The Vermont Stone Trail Geology Above: A historical photo of a Boutwell, Milne & Varnum Company Quarry, Barre. invites visitors and residents alike to find a wealth Quarries/ On the cover: An artist uses the pointing machine method to reproduce a marble sculpture in the early 20th century. -
The Surficial Geology and Hydrogeology of Dorset, Vermont
THE SURFICIAL GEOLOGY AND HYDROGEOLOGY OF DORSET, VERMONT By David J. De Simone and Marjorie Gale June 2009 Vermont Geological Survey 103 South Main Street Logue Cottage Waterbury, VT 05671-2420 Laurence R. Becker Vermont State Geologist Introduction Field work for this project was carried out during the 2006 and 2007 field seasons. Data analysis and map revisions were done in 2008 and completed in 2009. Maps discussed in this report are: 1. Surficial Geology 2. Stratigraphic Cross Sections 3. Field Data Sites 4. Springs, Seeps & Water Well Locations 5. Deglacial History 6. Depth to Bedrock 7. Bedrock Topography 8. Discharge Areas and Possible Shallow Overburden Aquifers 9. Hydrogeologic Units 10.Recharge Potential to Bedrock Aquifer 11.Potentiometric Surface Map and Groundwater Flow Lines Location and Geologic Setting The town of Dorset encompasses portions of the West Rupert, Manchester, Peru, Dorset and Danby 1:24000 topographic quadrangles and covers approximately one quadrangle of area. Two major valleys separate three upland regions. The Dorset Valley trends northwest and contains the West Branch Batten Kill that flows southeast into Manchester. In the vicinity of Dorset Village, there is a broad drainage divide consisting of wetlands. North of this divide, the Mettawee River enters the valley from head waters in the central upland region and flows northwest into New York. The upper Mettawee River represents a notable east-west tributary valley referred to as Mettawee Hollow. In the east, the East Dorset Valley trends north-northeast and is a continuation of the Vermont Valley. The Batten Kill flows southward from a divide just north of the village of East Dorset. -
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 -
Town of Sunderland Hazard Mitigation Plan
Town of Dorset DRAFT Hazard Mitigation Plan January 20, 2015 PUBLIC HEARING Town of Dorset PO Box 715 112 Mad Tom Road East Dorset, VT 05253 Table of Contents Section Page I. Introduction and Purpose 1 A. Purpose 1 B. Mitigation Goals 1 II. Town Profile 2 III. Planning Process 3 IV. Hazard Analysis 4 A. Hazard Assessment 4 B. Vulnerability Analysis 31 V. Mitigation Programs 36 A. Mitigation Goals for the Town of Dorset 36 B. Review of Existing Plans that Support Hazard Mitigation in 36 Dorset C. Current Program 39 D. Mitigation Projects 40 E. Monitoring and Revising This Plan 48 VI. References 49 List of Tables Table Page(s) Table 1. Number of buildings by type. 2 Table 2. Planning committee members 3 Table 3. Dates of planning meetings and public and agency review 3 Table 4. Total number of flood events by type and year for 6 Bennington County Table 5. Significant flood events affecting Bennington Count 6-7 Table 6. Structures by type in flood hazard zones in Dorset, VT 8 Table 7. Total number of winter storm events by type and year for 9 Bennington County Table 8. Significant winter storm events in Bennington County and 9-12 Dorset Table 9. Summary of wind events in Bennington County 14 Table 10. Significant wind events in Bennington County 14-15 Table 11. Hail events in Bennington County 16-17 Table 12. Dorset normal temperatures and precipitation for 1981 to 18 2010 Table 13. Palmer drought indices from 1980 to 2012 for western 19-20 Vermont (including Bennington County) Table 14. -
5. PART-2.Pdf
Part Two Biophysical Regions of Vermont Biophysical Regions of Vermont ne of the most rewarding parts of studying a landscape and its natural communities is appreciating all the factors that work together to cause Ovariation within that landscape. When we study the landscape of the world, we look to climate to explain most of the broad patterns of geographic variation. As we look more closely, say at the North American continent, climate is still the overrid- ing feature that causes variation, but we begin to see influences from other factors such as geological history. As we look even more closely, for example at the state of Vermont, we begin to see that landforms and soils, along with human history, influence variations as well. The biophysical regions of Vermont presented in Figure 2 help organize the landscape into smaller units that share features of climate, geology, topography, soils, natural communities, and human history. Although each region has variation within it, all are widely recognized as units that are more similar than they are different. Figure 2 was developed by analyzing existing land classification maps and by assessing biological and physical data with new analytical techniques (Girton 1997). The map was created so that land managers from all state and federal land managing agencies, as well as private land managers, could have a single map of biophysical regions to work with as a way of organizing their planning and thinking about natural communities in Vermont. Although our map shows Vermont only, the regions have no political boundaries, and they do not end at Vermont’s border. -
The Northeastern Caver Cumulative Index (Volumes I – Xlvii, 1969 – 2016)
THE NORTHEASTERN CAVER CUMULATIVE INDEX (VOLUMES I – XLVII, 1969 – 2016) by Steve Higham Rev. 1 - Nov. 23, 2016 PARTIAL LIST OF SECTIONS ARTICLE INDEX page 2 Accidents, safety, hazards, rescue page 2 Biology page 4 Book reviews page 5 Cartoons and drawings page 5 Cave description and exploration page 7 Cave lengths and lists page 17 Caving organizations, conventions, meetings page 18 Conservation, ownership, management page 20 Cover photos page 22 Equipment and techniques page 24 Geology, hydrology page 25 History page 26 Humor, poetry, fiction, creative page 30 Northeastern Caver page 31 Other page 32 People page 33 AUTHOR INDEX page 34 CAVE INDEX page 92 Connecticut page 92 Maine page 94 Massachusetts page 98 New Hampshire page 104 New Jersey page 109 New York page 110 Rhode Island page 129 Vermont page 130 Ontario page 138 Quebec page 138 The codes used in the cave index are as follows: a accident, rescue g geology/hydrology o owners, access, gating b biology h history p photograph c conservation i illustration r rumor or report d description m map x location Each entry is coded "xx-yyy", where the first two digits indicate the volume and the digits after the dash indicate the page number. "(S)" indicates that the article appears in the Speleodigest for the year of publication. Also, "(abs)" = abstract. Editors of The Northeastern Caver: 1969-1971 Chuck Porter 1972-1974 Bill Gregg 1974-1976 Thom Engel 1974-1979 Doug Hauser 1976-1979 Thom Engel (assistant editor) 1978-1979 Jim Cullen (assistant editor) 1979 Thom Engel 1979 Toms Smith (issue editor) 1979 Doug Hauser (assistant editor) 1979 Jim Cullen (assistant editor) 1979 Peter Quick 1979-1984 Toms Smith 1979 Warren Hall (issue editor) 1979 Connie Hall (issue editor) 1984-1989 Thom Engel 1990- Chuck Porter The table below shows the first page number of each issue in volumes I to XLVII: 1 ISSUE NO. -
Report Geology of Vermont
REPORT ON THE GEOLOGY OF VERMONT: DESCRIPTIVE, THEORETICAL, ECONOMICAL, AND SCENOGRAPHICAL; BY EDWARD HITCHCOCK, LL.D., ALBERT D. HAGER, A.M., EDWARD HITCHCOCK, JR., M.D., CHARLES H. HITCHCOCK, A.M., PROFESSOR OF HYGIENE AND PHYSICAL CULTURE IN AMHERST COLLEGE. GEOLOGIST TO THE STATE OF MAINE. IN TWO VOLUMES. PUBLISHED UNDER VE AUTHORITY OF THE STATE LEGISLATURE, BY ALBERT D. HAGER, PROOTORSVILLE, VT. VOL. I. PRINTED BY THE CLAREMONT MANUFACTURING COMPANY, CLAREMONT, N. 11. 1861. NQTE. The Principal of the Survey desires to state, that the publication of this Report has been entirely under the direction of Mr. A. D. HAGER. In consequence of the great increase of the matter above the original estimate, the work has been a difficult one, and demanded not only much labor, but rigid economy, and great pecuniary responsibility and sacrifice. Yet, as the public will see, it has been carried through in excellent taste, and compares most favorably with the style of analogous Reports in other States. The citizens of Vermont are certainly much indebted to Mr. Hager for his faithful, judicious and persevering efforts - without which, these volumes never could have seen the light in a form so satisfactory. It is but justice, also, to say, that Mr. Hager was fortunate in securing the services of the Messrs. Goddard, of Claremont, for the printing. Had they not possessed unusual skill in deciphering illegible manuscripts and correcting proofs, in some cases where from distance or other causes they had not passed under the eye of the authors, errors would S have abounded where now we trust they are rare.