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Municipal Plan for the Town and Village of Ludlow, Vermont
Municipal Plan For the Town and Village of Ludlow, Vermont Adopted by the Ludlow Village Trustees on October 8, 2019 Adopted by the Ludlow Select Board on October 7, 2019 Ludlow Municipal Plan Adopted October 2019 Adopted by the Ludlow Village Trustees on January 2, 2018 Adopted by the Ludlow Select Board on December 4, 2017 Amended by the Ludlow Select Board on November 7, 2016 Amended by the Ludlow Select Board on August 3, 2015 Amended by the Ludlow Village Trustees on August 4, 2015 Adopted by the Ludlow Select Board on November 5, 2012 Adopted by the Ludlow Village Trustees on March 5, 2013 This Ludlow Municipal Plan was developed in 2018-2019 by the Ludlow Planning Commission with assistance from the Southern Windsor County Regional Planning Commission, Ascutney, VT. Financial support for undertaking this and previous revisions was provided, in part, by a Municipal Planning Grant from the Vermont Agency of Commerce and Community Development. Photo Credits: Many of the pictures found throughout this document were generously provided by Tom Johnson. ii Ludlow Municipal Plan Adopted October 2019 Contents 1 Introduction .................................................................................................................................. 1 1.1 Purpose .................................................................................................................................. 1 1.2 Public Process ....................................................................................................................... 1 1.3 -
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 ....---...............-.-.....-.-...--.-......... -
Town of Bristol Outdoor Recreation, Gateway to the Green Mountains Bristol Is in Northeastern Addison County, at the Western
Town of Bristol Outdoor Recreation, Gateway to the Green Mountains Bristol is in northeastern Addison County, at the western foot of the Green Mountains. The New Haven River flows out of the mountains and through town. Parks • Bristol Town Green- Center of town with a fountain and bandstand. Link for history- Bristol Core • Bristol Veterans Memorial Park- Wooded park with paths across a roaring waterfall. Link for history- Bristol Core • Sycamore Park-A day use recreation area, swimming and fishing. Link for history- Bristol Core • Eagle Park-handicapped access, picnic tables. • Bartlett’s Falls- (New Haven Gorge or known as the Toaster) Waterfalls and slab rocks to lounge on. Biking Bristol is the home of VBT Vermont Bicycle Tour and a stopping way for Sojourn and Backroads bike tours. The mountain biking is being cultivated, there is the VMBA chapter of Addison County Bike Club which has a focus in Middlebury. Most trails in Bristol area are privately owned and maintained. The Watershed Trail link Green Mountain Family Campground map Hinesburg Town Forest trails map (14mi from town) Water Sports Bristol Pond is great for canoeing, Stand Up Paddleboarding, fishing, and kayaking New Haven River is known for white water kayaking and part of the New Haven Ledges Race, bringing kayakers from all over New England to drop over the Bartlett’s Falls. • Baldwin Creek • Bristol Pond (Winona Lake) • Monkton Pond (Cedar Lake) • Lake Dunmore Hiking Bristol is the Gateway into the Green Mountains, there are many trails that surround the town and there are more to come. • Watershed Trail link • Bristol Cliffs map • Coffin Trail – In the development stages link • Trail around Bristol – In the development stages Town of Bristol Outdoor Recreation, Gateway to the Green Mountains Bristol Ledges Trail Round trip hiking distance: 3 miles Difficulty: Easy The Bristol Ledges Trail is the perfect hike for when you’re looking for something short and close by, but with super sweet views. -
Summer 2021 Long Trail News
NEWS Quarterly of the Green Mountain Club SUMMER 2021 555 New End-to-Enders The Most Ever Recorded [FROM AGE 7 TO 80] CONTENTS Summer 2021, Volume 81, No. 2 The mission of the Green Mountain Club is to make the Vermont mountains play a larger part in the life of the people by protecting and maintaining the Long Trail System and fostering, through education, the stewardship of Vermont’s hiking trails and mountains. Quarterly of the Green Mountain Club Michael DeBonis, Executive Director Chloe Miller, Communications Manager & Long Trail News Editor Richard Andrews, Volunteer Copy Editor Sylvie Vidrine, Graphic Designer Green Mountain Club 4711 Waterbury-Stowe Road Waterbury Center, Vermont 05677 Phone: (802) 244-7037 Fax: (802) 244-5867 E-mail: [email protected] Website: greenmountainclub.org The Long Trail News is published by The Green Mountain Club, Inc., a nonprofit organization founded in 1910. In a 1971 Joint Resolution, the Vermont Legislature Julia LanzDuret-Hernandez on Mount Mansfield. designated the Green Mountain Club the “founder, sponsor, defender and protector of the Long Trail System...” FEATURES Contributions of manuscripts, photos, illustrations, and news are welcome from ❯ The Mountains That Made Me members and nonmembers. 5 by Julia LanzDuret-Hernandez The opinions expressed byLTN contributors are not necessarily those of GMC. 6 ❯ Congratulations to the 2020 End-to-Enders The Long Trail News (USPS 318-840) is published quarterly by The Green Mountain and Side-to-Siders Club, Inc., 4711 Waterbury-Stowe Road, ❯ Waterbury Center, VT 05677. Periodicals 8 A Day in the Life: Long Trail Thru-Hiker postage paid at Waterbury Center, VT, and additional offices. -
7 the Geology of the Bennington Area
I S; 5, •-' -"•L - THE GEOLOGY OF THE BENNINGTON AREIA, VERMONT By ItV £ JOHN A MACFAD\ EN, JR t "I VERMON I GEOLOGIC \L SURVEY :• CHARLiS G. DOLL Stale Geologist Published by S S VERMON'! DEVELOPMEf\ t COMMISSION •• MONTPELIER VE! MONT S S S S S • BiLETIN NO. 7 - 1956 S ' S S - THE GEOLOGY OF THE BENNINGTON ARF A, VERMONT By JOHN A. MACFAD\ 1N, JR £ I VERMON I GEOLOGIC 'LL SURVEY CHARLCS G. DOLL State Geologist 4 / • •• • . • • Published by VERMONT DEVELOPMEr''1' COMMISSION MONTPELIER VERIONT I • .BPLLETIN NO. • • • 1956 • •• •. •• eBr.4.n TABLE OF CONI1NTS / ' I PAGE 1 / ABSTRACT ......................... 7 i oRatlsn4 1 INTRODUCTION ........................ 8 0 Location. ......................... PWtney 8 Physiogiaphy and Glaciation ................. 9 Purpose of Study ....................... 11 I / I, Method of Study ...................... 11 I 0.> Regional Geologic Setting .................. 11 Vt. ) N.H. Previous Work ....................... 13 Acknowledgments . I ( 14 I I STRATIGRAPHY ........................ 15 I oManshular 1 General Statement .................... is I' Pre-Cambrian Sequence ......... ' .....16 / Mount Holly Gneiss ..................... 16 So.s.tqa 3r- I. I I Stamford Granite Gneiss................. 17 Lower Cambrian Sequence .................. 17 41 Mendon Formation ................... 17 I • —4 ( Cheshire Quartzite ................... 20 •• #3 Dunham Dolomite ..................... 21 'S Monkton Quartzite .................. 22 ------\-------- Winooski Dolomite ................... 23 -
A Transect Through the Pre-Silurian Rocks of Central Vermont
University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1987 A Transect Through the Pre-Silurian Rocks of Central Vermont; The Lincoln Massic and Its Immediate Cover; The Pre-Silurian Hinterland Along the Valleys of the White and Mad Rivers, Central Vermont; Metamorphism of Pre-Silurian Rocks, Central Vermont; Regional Geochemical Variations in Greenstones from the Central Vermont Appalachians Rolfe Stanley Vincent DelloRusso Sharon O'Loughlin Eric Lapp Thomas Armstrong Follow this and additional works at: https://scholars.unh.edu/neigc_trips See next page for additional authors Recommended Citation Rolfe Stanley, Vincent DelloRusso, Sharon O'Loughlin, Eric Lapp, Thomas Armstrong, Jeffrey Prewitt, Jerome Kraus, Gregory Walsh, Christine Kimball, Athene Cua, Jo Laird, and R. A. Coish, "A Transect Through the Pre-Silurian Rocks of Central Vermont; The Lincoln Massic and Its Immediate Cover; The Pre- Silurian Hinterland Along the Valleys of the White and Mad Rivers, Central Vermont; Metamorphism of Pre-Silurian Rocks, Central Vermont; Regional Geochemical Variations in Greenstones from the Central Vermont Appalachians" (1987). NEIGC Trips. 421. https://scholars.unh.edu/neigc_trips/421 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]. Authors Rolfe Stanley, Vincent DelloRusso, Sharon O'Loughlin, Eric Lapp, Thomas Armstrong, Jeffrey Prewitt, Jerome Kraus, Gregory Walsh, Christine Kimball, Athene Cua, Jo Laird, and R. -
2. Biophysical Regions and a Landscape Perspective for Conservation and Management
2. BIOPHYSICAL REGIONS AND A LANDSCAPE PERSPECTIVE FOR CONSERVATION AND MANAGEMENT ermont is rich with wildlife, largely because we have an abundance As a Vermont and diversity of habitat that supports the needs of many species. landowner, you will VThese habitats include extensive areas of interconnected forests of many types, swamps and lakeside marshes, fens and bogs, cliffs and caves, need to carefully seeps and vernal pools, fields and grasslands, and streams, rivers, and ponds. An important conservation goal is to maintain this diverse array consider the effects of of habitats to continue to support Vermont’s wildlife resources and all the values they provide. your actions and plan Achieving this goal over the long term will be challenging, given the continued loss and degradation of habitat associated with development. for effective habitat As a Vermont landowner, you will need to carefully consider the effects of your actions and plan for effective habitat management and conservation management and on at least three scales. First, you need to consider the needs of individual conservation on at species where they occur, especially those species that are particularly sensitive to changes in their surroundings. For example, American least three scales. woodcock require shrub wetlands for feeding, adjacent to old fields for courtship. Second, you need to consider the distribution and condition of all habitats and natural communities in your local area and across the state. This is the best insurance that you will provide the habitat requirements for a broad range of species. And third, you need to consider large, landscape-scale features, such as large areas of contiguous forest and the habitat that connects them. -
Route 2 • St. Johnsbury, Vermont 802-274-1219
A1 A2 2 | Summer Fun The Record | 2018 As a GOOD NEIGHBOR boarding student at St. Johnsbury Academy, you can expect no less than a life-changing learning experience. “ What I love most about the Academy is the diverse group of students in the boarding community and the friendships “ I love the Academy because I have developed there.” it has given me so many “ Living on campus full-time opportunities to learn Sam C. was a life-changing experience Academy boarding student and explore.” for me!” from Lyme, New Hampshire Oshun S. Alison R. Academy boarding student Academy boarding student from Montgomery Center, from Montpelier, Vermont Vermont We are SJA. An independent, coeducational, boarding and day school for grades 9-12 and postgraduate year located in St. Johnsbury, Vermont. Our GOOD NEIGHBOR boarding for students from Vermont, Learn more at: program reduces tuition New Hampshire, and Quebec. stjacademy.org/neighbor A3 The Record | 2018 Summer Fun | 3 Inside The ‘County’ Fair Necessities 5 This Year’s Fair Schedule 6 An Uphill Battle 8 Other Suggested Hiking Trails 9 Farmers’ Markets & Things To Do 12 Crossing The Line At The Haskell 18 33 Other Cultural Institutions 20 Sounds Of Summer 21 PUBLISHER Todd M. Smith Hills Are Alive At Dog Mountain 24 — 5 Area Arts Venues 26 EDITOR ADVERTISING Enjoy A Current Event By Canoe 27 Leah Carey SALES Area Swimming Holes 29 — Julie Poutre, 24 LAYOUT Brooke Dolloff, The Region’s Golf Coures 33 Andrew McGregor Glen Jardine, — Sylvie Weber COVER DESIGN — Glen Jardine ADVERTISING 27 — DESIGN & COVER PHOTO PRODUCTION Paul Hayes Jeana Desilets CONTACT US Advertising: [email protected] News: [email protected] Phone: 802-748-8121 Web: caledonianrecord.com A PUBLICATION OF THE CALEDONIAN-RECORD On the Cover: Lily Farr, right, and Saffron attend the Levitt AMP St. -
APPALACHIAN WORKSHOP Lkmf
G-o9Q eA-w- JQA—vii: Gioj"- kj tzb 4s• IØ So APPALACHIAN WORKSHOP lKMF JNtSTY OF Vth1Oft1T LTOft VT I2;LoXPiItti ir QUEBEC VEROT APPALACHIAN WORKS+OP Apr11 14 - 16, 1989 Kalkin Hall, University of Vermont Burlington, Vermont Co-Sponsored by: The Department of Geology Visiting Lecture Series The Canadian Studies Program The Graduate College, University of Vermont EDITORS Maurice Coipron and Barr,' Doolan Department of Geology • University of Vermont Burlington, Vermont Cover: Perspective block diagram of the Québec- Vermont Orogen (from Dóolan, 1989; see Doolan, this volume). Additional copies are available upon request from: Vermont Geological Society, Inc. P.O. Box 304 twfontpelier, Vermont 05602 PROGRAM AND CONTENTS SATURDA V. APRIL 15, 1989 8:00 - INTRODUCTORY REMARKS I. EVOLUTION OF THE ANCIENT NORTH AMERICAN MARGIN IN THE QUEBEC REENTRANT ............................................................................. 1 Chairperson: Charles A. Ratté 8:15 - Stephen Kumarapeli* and Hillar Pintson: Geochronologic constraints on the timing of rifting and continental breakup at the Sutton Mountains triple junction...........3 8:40 - William M. Dowling: Paleogeographic analysis of the preshelf facies in the Oak Hill and Camels Hump Groups: constraints on syn-rift and post-break-up subsidence in theQuébecreentrant ...........................................................................................................5 9:05 - Charlotte Mehrtens: The Cambrian platform and platform margin in northwestern Vermont..............................................................................................................................8 -
Trip I DEGLACIAL HISTORY of the LAKE CHAMPLAIN-LAKE GEORGE
163 . Trip I DEGLACIAL HISTORY OF THE LAKE CHAMPLAIN-LAKE GEORGE LOWLAND by G. Gordon Connally Lafayette College Easton, Pennsylvania and Leslie A. Sirkin Adelphi University Garden City, New York GENERAL GEOMORPHOLOGY The Lake Champlain and Lake George Valleys are two separate physiographic units, situated in separate physiographic provinces (see Broughton, et al., 1966). The Champlain Valley lies in the St. Lawrence-Champlain Lowlands while the Lake George trough lies in the Adirondack Highlands. It is the continuous nature of the deglacial history of the two regions that links them together for this field trip. Indeed, the deglacial history of the regions begins at the north end of the Hudson-Mohawk Lowlands near Glens Falls, New York. Physiography The Champlain Valley lies between the Adirondack Mountains of New York on the west and the Green Mountains of Vermont on the east. Lake Champlain occupies most of the valley bottom and has a surface elevation of about 95 feet. The Great Chazy, Saranac, Ausable, and Bouquet Rivers enter the valley from the Adirondacks while the Mississquoi, Lamoille, and Winooski Rivers and Otter Creek enter from the Green Mountains. Figure 1 shows the general physiography and the field trip stops. According to Newland and Vaughan (1942) Lake George occupies a graben in the eastern Adirondacks. The'surface of Lake George is about 320 feet above sea level and it drains into Lake Cham plain via Ticonderoga Creek at its northern end. In general, Lake George marks the divide between southerly flowing Hudson River drainage and northerly flowing St. Lawrence River drainage. 164 Great Chazy Lamoille R. -
OROGRAPHY 9 and Covered with a Coating of Clay Which Smoothed Over Its Inequalities and Concealed Most of the Underlying Rocks
OROGRAPHY 9 and covered with a coating of clay which smoothed over its inequalities and concealed most of the underlying rocks. Since its emergence the surface has been but slightly altered by drainage channels cut across it. Orographical maps of Eastern and Western Canada, showing elevations above sea-level, will be found on pages 8 and 10 of this1 volume. Canadian Shield.—The portion of the Precambrian continent whose exposed surface still forms a large part of Canada has an area of about two and a half million square miles. Its northern border crosses the Arctic archipelago and the eastern lies beyond Baffin island and Labrador and reaches the depressed area occupied by the St. Lawrence river, a short spur or point crossing this valley at the outlet of lake Ontario to join the Adirondack mountains in New York. The southern boundary runs from the spur west to Georgian bay, skirts the north shore of lake Huron and sweeps almost around the ancient depressed area occupied by lake Superior. The western edge, from the lake of the Woods and lake Winnipeg, bears northwest to the western end of lake Athabaska, and passes through the basins occupied by Great Slave and Great Bear lakes, reaching the Arctic ocean east of the Mackenzie River delta. In detail, the surface features of the Canadian Shield are irregular; but, viewed broadly, it has the conforma tion of a great plain, depressed toward the centre and in the north, and slightly elevated along the eastern and southern borders, where it presents a rather steep outward slope. -
A Guide to the Hiking Capital of Southern Vermont
A guide to the Hiking Capital of Southern Vermont 1 Introduction Welcome to Mendon, known throughout Vermont as the “Gateway to the Green Mountains.” Mendon is blessed with the best mountain scenery in southern Vermont. Killington Peak (Vermont’s second highest summit), Mendon Peak (the highest summit in Vermont without a marked trail to the top), Blue Ridge (overlooking the Otter Creek Valley) and Bald Mountain and East Mountain (both overlooking Rutland City and beyond) are all within our town boundary. Nearby Pico Peak further adds to the dramatic mountain skyline that we all enjoy. Over 90% of our town is forested and over 50% is protected in the Green Mountain National Forest, three Vermont State forests (Coolidge, Aitken and Jeffords) and the Rutland City forest. Hiking trails abound in Mendon, from the world-famous Long Trail/Appalachian Trail corridor to casual saunters like the Tamarack Notch loop to opportunities for bushwhacking up untrammeled summits like Mendon Peak. You can understand why we proclaim Mendon to be the hiking capital of southern Vermont. This ”Hike Mendon” trail guide is your ticket to mountain adventure. It is not intended as a comprehensive tenth-of-a-mile by tenth-of-a-mile trail guide. You will not find GPS coordinates anywhere. Many sources available in print and on-line do all that very well. Rather it is a guidebook that will help you find trail heads, alert you to where the trail goes left or right or straight up and what to expect in different seasons, including winter. There are also sections on hiking our snowmobile and back country ski trails and descriptions on where to start your bushwhack for those trail-less summits.