Lake Champlain Voyages of Discovery: Bringing History Home
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Weathersfield Amended Munici
CHARTERED BY Town CHARTERED BY NEW HAMPSHIRE NEW YORK AUGUST 20, 1761 of APRIL 8, 1772 Weathersfield, Vermont Website: http://www.weathersfield.org Town Plan Adopted July 15th, 2004 Amended September 15th, 2005 TOWN OF WEATHERSFIELD, VERMONT TOWN PLAN Proposed Amendments Weathersfield Planning Commission Stephen A. Walasewicz, Chairperson Rene Bergeron Peter M. Daniels Julie A. Levy Steven J. Melanson Weathersfield Conservation Commission Marianne E. Walsh, Chairperson Annmarie J. Christensen Diana L. Day Christopher Harris Robert A. LaCasse Nathan G. McKeen Anna B. Sykas Weathersfield Select Board C. Peter Cole, Chair Henry C. Cobb, Jr., Vice-Chairperson Norman John Arrison, Board Clerk Daniel E. Boyer Patricia W. Daniels http://www.weathersfield.org Thanks to the Southern Windsor County Regional Planning Commission, Weathersfield Conservation Commission, and community members for their work on this plan. e Adopted July 15th, 2004 Amended September 15th, 2005 TOWN OF WEATHERSFIELD, VERMONT TOWN PLAN Table of Contents Acknowledgments Inside Front Cover Introduction ............................................................................... 1 Historical Background ....................................................... 1 Why and How a Town Plan is Used ..................................... 3 What is in a Town Plan? .................................................... 5 Goals and Objectives .......................................................... 8 Implementation Procedures ................................................ 9 Relationship -
Vermont Department of Environmental Conservation Agency of Natural Resources
Vermont Department of Environmental Conservation Agency of Natural Resources WATER INVESTMENT DIVISION National Life Building, DAVIS 3 1 National Life Drive Montpelier, VT 05620-3510 FAX: (802)828-1552 Ms. Megan Moir, Assistant DPW Director of Water Resources Authorized Representative City of Burlington 234 Penny Lane Burlington, VT 05401 January 14, 2021 Expiration Date: January 14, 2026 Re: Manhattan Drive Outfall Repairs Project Vermont/ USEPA Clean Water Revolving Loan Number RF1‐2xx (Pending) Notice of Intent to Issue a Finding of No Significant Impact Dear Megan: The Department of Environmental Conservation intends to issue a Finding of No Significant Impact (FONSI) for the Manhattan Drive Outfall Repairs Project. The project has positive environmental impacts consisting of the reduction of erosion and sediment movement into the adjacent waters of the state and improved reliability and resiliency of the adjacent municipal sewer and stormwater systems. This project additionally involves impacts to wetlands and floodplains in the form of permitted wetlands impacts and de minimus floodplain impacts. Otherwise, this project may have been eligible for Categorical Exclusion from detailed environmental review; additionally, the direct and indirect environmental effects of the project are still not significant enough to necessitate an Environmental Impact Statement (EIS). The Department's environmental review procedures require a 30‐day public comment period following the issuance of a Notice of Intent to Issue a Finding of No Significant Impact. If no public comments received during that period demonstrate that this Notice of Intent is in error, then the Finding of No Significant Impact will become effective. Page 2 of 2 Megan Moir, Authorized Representative, City of Burlington Manhattan Drive Outfall Repairs Finding of No Significant Impact January 14, 2021 Copies of documents supporting a Finding of No Significant Impact are enclosed. -
List of Vermont Water Bodies Known with an Aquatic Invasive Species
Key: List of Vermont water bodies known AL - alewife SS - starry stonewort BN - brittle naiad SWF - spiny water flea with an aquatic invasive species CLP - curly-leaf pondweed VLM - variable-leaved watermilfoil EF - European frogbit WC - water chestnut Updated Apr. 2016 EWM - Eurasian watermilfoil ZM - zebra mussel These species are considered the most problematic in Vermont Water body Town AL BN CLP EF EWM SWF SS VLM WC ZM Arrowhead Mountain Lake Milton X Austin Pond Hubbardton X Beaver Wetland Mendon X Beaver Pond Proctor X Beebe Pond Hubbardton X X Berlin Pond Berlin X Big Marsh Slough Highgate X X X X Black Pond Hubbardton X X Black River Springfield X Blissville Wetland Pond Blissville X Broad Brook Vernon X Brookside Pond Orwell X X Brownington Pond Brownington X Bullis Pond Franklin X X Burr Pond Sudbury X X Cabot Clark Marsh Highgate X Castleton River Castleton X Cedar Lake Monkton X Chipman Pond Tinmouth X Clay Brook Warren X Clyde Pond Derby X Coggman Creek X Coggman Pond West Haven X X X Connecticut River, Herricks Cove Rockingham X Connecticut River, Hoyts Landing Springfield X X Connecticut River, TransCanada launch Concord X Connecticut River, Wilder Dam Hartford X Cranberry Pool Highgate X X X Crystal Lake Barton X Daniels Pond Glover X Dead Creek Ferrisburgh X Dead Creek Highgate X X Deweys Mill Pond Hartford X Echo Lake Hubbardton X Fairfield Pond Fairfield X X Fairfield Swamp Pond Swanton X Fern Lake Leicester X X Forest Lake Calais X Frog Pond Orwell X Gale Meadows Pond Londonderry X Glen Lake Castleton X X 1 Water -
Dams and Reservoirs in the Lake Champlain Richelieu River Basin
JUST THE FACTS SERIES June 2019 DAMS AND RESERVOIRS IN THE LAKE CHAMPLAIN RICHELIEU RIVER BASIN MYTH Water released from tributary dams in the United States causes flooding in Lake Champlain and the Richelieu River. FACT Water levels in Lake Champlain and the Richelieu River Generally, mass releases of water from flood control are primarily affected by precipitation from rain or dams are avoided. In addition to compromising the snowmelt. structural integrity of the dams, mass releases would also endanger the very communities that these dams are built Because of its size, Lake Champlain can store a lot of to protect. water; the flood control dams and reservoirs in the basin, which are very small in comparison to the lake, do not When conditions force the release of more water than significantly change water levels of the lake and river as hydropower plants can handle, the increase in water they release water. levels immediately below the dam will be much greater than the increase on Lake Champlain. This is true even during high water and flooding events. Consider, for instance, when Lake Champlain and the Richelieu River experienced extreme flooding between April and June 2011, the additional releases flowing from Waterbury Reservoir—the largest flood control reservoir in the Vermont portion of the basin, contributed less than 2 centimetres (¾ inch) to the elevation of Lake Champlain and the upper Richelieu River. International Lake Champlain-Richelieu River Study Board FACT FACT Dams in the US portion of the basin are built for one of Waterbury Reservoir in Vermont is the largest reservoir two purposes: flood control or hydroelectric power. -
Champlain Valley (Why Are Clay Soils Where They Are?)
Geomorphic history of the Champlain Valley (why are clay soils where they are?) part 1) How did landscape evolve and where do “clay” minerals come from? part 2) How were they deposited in Lake Vermont/ Champlain Sea? part 3) Can we predict the distribution of “clay” thickness? (…can we compare prediction with what people observe) 500,000,000 years Today ~500,000,000 years: Sediments of “Champlain Valley Sequence” deposited on shoreline of ancient ocean Monkton quartzite + Taconic Slates Limestones + Marbles ~460,000,000 years: Collision of island arc causes thrusting + metamorphism Champlain Thrust Fault Champlain Thrust: -Exposed at Snake Mtn + Mt. Philo -delineates boundary between “low” and “mid” grade metamorphic rocks -Marbles pf middlebury syncline folded along back of thrust -Topography of Addison County reflects erodibility of bedrock: T1: lower surface: “low grade” sedimentary rocks below thrust (e.g. shale) T2: upper surface: “mid grade” meta-sedimentary rocks above thrust (e.g. marble) Green Mountains= “high grade” metamorphic rocks (e.g. schist and gneiss) T1 T2 Green Mtn gneiss Geologic map of Addison County Taconics Part 2: How were clays deposited in Lake Vermont and the Champlain Sea? 500,000,000 years Today ~96,000 - 20,000 years (i.e. yesterday…): Champlain Valley sat below 1-3 km of ice Soils and clay minerals from previous inter-glacial cycles were stripped by advancing glaciers Rocks were ground into “clay size fraction” and trapped under ice retreating glacial ice withdrew from Champlain Valley between ~14-13 kyr Many depositional features in Champlain Valley record ice retreat -Layers of “basal till” deposited beneath ice sheets (coarse, angular, poorly sorted debris) -Meltwater streams flow between glacier and hillslopes -Sedimentary deposits accumulate, leaving ‘kame terraces’ when glacier retreats Lake Vermont had 2+ stages: Coveville: Ice dammed in So. -
Apologetic Resources
APOLOGETIC RESOURCES A Young Earth ministry perspective, namely contrasting Scripture to true science now and during the ages. By Dr. Jim Pagels [email protected] 9/2016 Editor Dr. John Fricke, Emeritus Professor of Biology, Concordia University, Ann Arbor, Michigan. Copyright This book is offered as an educational resource on a no cost basis. Contents are not to be reproduced for the purpose of sale. Note that all Scriptural passages are taken from the English Standard Version. 1 I HAVE NO GREATER JOY THAN TO HEAR THAT MY CHILDREN WALK IN THE TRUTH III JOHN 1:4 Forward - Although there is much young Earth information available from commercial sources and on the internet, it was the impression of this writer that no resource that deals with basic topical issues correlating the young Earth philosophy and science exists for professional church workers. To this end, Apologetic Resources is being offered. Intended Audience – The intended audience of this reference material is primarily use by professional church workers, i.e., teachers, pastors, youth workers, etc., namely those who choose to uphold the literal interpretation of Genesis and the inerrancy of Holy Scripture. The focus in this regard is Young Earth Creationism and the catastrophic nature of the global Genesis Flood keeping in mind that Genesis 1-11 is foundational to most of the significant doctrines of Holy Scripture. Of course, laymen may well also find this reference a valuable resource. There is obviously a realistic interplay between Scripture, apologetics and true science. The goal of this document is to provide clarity to this interaction. -
A Retrospective on Archaeology at Fort William Henry, 1952-1993: Retelling the Tale of the Last of the Mohicans David R
Northeast Historical Archaeology Volume 20 Article 2 1991 A Retrospective on Archaeology at Fort William Henry, 1952-1993: Retelling the Tale of The Last of the Mohicans David R. Starbuck Follow this and additional works at: http://orb.binghamton.edu/neha Part of the Archaeological Anthropology Commons Recommended Citation Starbuck, David R. (1991) "A Retrospective on Archaeology at Fort William Henry, 1952-1993: Retelling the Tale of The Last of the Mohicans," Northeast Historical Archaeology: Vol. 20 20, Article 2. https://doi.org/10.22191/neha/vol20/iss1/2 Available at: http://orb.binghamton.edu/neha/vol20/iss1/2 This Article is brought to you for free and open access by The Open Repository @ Binghamton (The ORB). It has been accepted for inclusion in Northeast Historical Archaeology by an authorized editor of The Open Repository @ Binghamton (The ORB). For more information, please contact [email protected]. A Retrospective on Archaeology at Fort William Henry, 1952-1993: Retelling the Tale of The Last of the Mohicans Cover Page Footnote I want to thank Paul Huey for impressing upon me the importance of studying older, unpublished, artifact collections. While it may appear more exciting to tackle "new" sites, we have a strong ethical obligation to make sure that older excavations are published, even when the original research was directed by others. I also wish to thank Mike Palumbo, Curator at Fort William Henry, for many stimulating conversations and for giving me access to photographs and artifacts from the 1950s excavation; and thanks go to the Fort William Henry Corporation for allowing me to reproduce archival photographs. -
030321 VLP Fort Ticonderoga
Fort Ticonderoga readies for new season LEE MANCHESTER, Lake Placid News TICONDEROGA — As countered a band of Mohawk Iro- name brought the eastern foothills American forces prepared this quois warriors, setting off the first of the Adirondack Mountains into week for a new war against Iraq, battle associated with the Euro- the territory worked by the voya- historians and educators in Ti- pean exploration and settlement geurs, the backwoods fur traders conderoga prepared for yet an- of the North Country. whose pelts enriched New other visitors’ season at the site of Champlain’s journey down France. Ticonderoga was the America’s first Revolutionary the lake which came to bear his southernmost outpost of the War victory: Fort Ticonderoga. A little over an hour’s drive from Lake Placid, Ticonderoga is situated — town, village and fort — in the far southeastern corner of Essex County, just a short stone’s throw across Lake Cham- plain from the Green Mountains of Vermont. Fort Ticonderoga is an abso- lute North Country “must see” — but to appreciate this historical gem, one must know its history. Two centuries of battle It was the two-mile “carry” up the La Chute River from Lake Champlain through Ticonderoga village to Lake George that gave the site its name, a Mohican word that means “land between the wa- ters.” Overlooking the water highway connecting the two lakes as well as the St. Lawrence and Hudson rivers, Ticonderoga’s strategic importance made it the frontier for centuries between competing cultures: first between the northern Abenaki and south- ern Mohawk natives, then be- tween French and English colo- nizers, and finally between royal- ists and patriots in the American Revolution. -
Constraints on Lake Agassiz Discharge Through the Late-Glacial Champlain Sea (St
Quaternary Science Reviews xxx (2011) 1e10 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Constraints on Lake Agassiz discharge through the late-glacial Champlain Sea (St. Lawrence Lowlands, Canada) using salinity proxies and an estuarine circulation model Brandon Katz a, Raymond G. Najjar a,*, Thomas Cronin b, John Rayburn c, Michael E. Mann a a Department of Meteorology, 503 Walker Building, The Pennsylvania State University, University Park, PA 16802, USA b United States Geological Survey, 926A National Center, 12201 Sunrise Valley Drive, Reston, VA 20192, USA c Department of Geological Sciences, State University of New York at New Paltz, 1 Hawk Drive, New Paltz, NY 12561, USA article info abstract Article history: During the last deglaciation, abrupt freshwater discharge events from proglacial lakes in North America, Received 30 January 2011 such as glacial Lake Agassiz, are believed to have drained into the North Atlantic Ocean, causing large Received in revised form shifts in climate by weakening the formation of North Atlantic Deep Water and decreasing ocean heat 25 July 2011 transport to high northern latitudes. These discharges were caused by changes in lake drainage outlets, Accepted 5 August 2011 but the duration, magnitude and routing of discharge events, factors which govern the climatic response Available online xxx to freshwater forcing, are poorly known. Abrupt discharges, called floods, are typically assumed to last months to a year, whereas more gradual discharges, called routing events, occur over centuries. Here we Keywords: Champlain sea use estuarine modeling to evaluate freshwater discharge from Lake Agassiz and other North American Proglacial lakes proglacial lakes into the North Atlantic Ocean through the St. -
Folklore of Springfield Vermont
nn.,^'r.'=^"''CH LIBRARIES 3 3433 07954360 3 FOI.KLORE SPRINGFIELD VERMONT :.«OWN l>>CilNT rx.OCK HO'./SC hij iM. Eva Baker ^1 ^t u.-^^:,".^ Folklore of Springfield iPnlklor? nf ^prmgftiHh mm By MARY EVA BAKER 4. ti Illusirated by Russell W. Porter and Horace S. Brown Springfield, Vermont 1922 THE NC"/ VG-^K PUBLIC lib..a:^y 427259 A ASrOR, LENOX AND TILDEN FOUXDATIONS R 1929 L Copyright, 1922 by M. E. Baker ^ , Publishers Th^ Altrurian Club of Springfield. Vt. Printers Springfield printing Corp.. Springfielc TO THE General Lewis Morris Chapter, Daughters of the American Revolution, Descendants of those Heroes Whose Fortitude and Patriotism is Unparalleled in History AND TO The Altrurian Club, That so Loyally Serves Its Motto, ".Vo/ for Ourselves, but for Others." These Pages are Dedicated "Thy Hork. faithful daughters, is noble as wise, ''The soul with its love is aglow; "A nation uill hail thee! thine own hearts approve, '\ind thy deeds through the centuries go.'' Credit is due the Misses Grace and Alice Wheeler, Mrs. Mary Toivnsend Bow- en, Miss Edna I. Lockwood, Clarence E. Morse, H. G. Tapper and E. W. Barnard for some of the incidents found in this book; also Mr. and Mrs. Everett Eaton for help in tracing certain subjects. Contents PAGE NO. I. Making a Wilderness Into a Township 1 II. How a Swamp Became the Village Square 7 III. The Common and Incidents Connected With It ... 17 IV. Old Bridges 24 V. The Romance of the Trees 32 VI. Old Weathervanes and Old Bells 39 VII. Revolutionary Heroes 43 VIII. -
Welcome to the Walk of Change Nature Trail
Welcome to the Walk of Change 3. Monarch butterflies former land clearing for farming. The size of the 6. Is this The End? Monarch butterflies have one of the most stones may reveal whether the adjacent land was As you walked to this stop you may have noticed Nature Trail unusual and extreme life cycles of North used for crops or pasture. Stone piles or walls with a change in light and temperature. You just walked American butterflies. Adults migrate north, large rocks usually suggest the adjacent land was through a climax community. In this case, it is a Here at Knight Island State Park, the arriving in the northeast early in the growing a mowed field or a pasture in which only the large patch of mature forest. This does not mean the end landscape has been affected by many physical season. After mating, a female lays her eggs rocks needed to be removed. Small stones need to of change, though, or static condition in the forest. environmental and cultural factors over the on Common Milkweed, like you can see here. be removed from cultivated plots annually. This New growth slows as the forest canopy becomes geologic timescale. These include weather pile of small stones reveals that the surrounding enclosed with fewer, larger trees that are more extremes, glaciers, human habitation and area was used for crops. The crops grown on spaced out. At this state in a forest’s evolution, livestock grazing. Enjoy a walk along the Knight Island were beans, com and peas. change is brought by natural events such as storms trail system, and keep watch for signs of Common milkweed bringing wind and ice, or from cultural means like these changes; you might even witness some logging. -
What Is Science?
What is Science? Dana Desonie, Ph.D. Say Thanks to the Authors Click http://www.ck12.org/saythanks (No sign in required) AUTHOR Dana Desonie, Ph.D. To access a customizable version of this book, as well as other interactive content, visit www.ck12.org CK-12 Foundation is a non-profit organization with a mission to reduce the cost of textbook materials for the K-12 market both in the U.S. and worldwide. Using an open-content, web-based collaborative model termed the FlexBook®, CK-12 intends to pioneer the generation and distribution of high-quality educational content that will serve both as core text as well as provide an adaptive environment for learning, powered through the FlexBook Platform®. Copyright © 2014 CK-12 Foundation, www.ck12.org The names “CK-12” and “CK12” and associated logos and the terms “FlexBook®” and “FlexBook Platform®” (collectively “CK-12 Marks”) are trademarks and service marks of CK-12 Foundation and are protected by federal, state, and international laws. Any form of reproduction of this book in any format or medium, in whole or in sections must include the referral attribution link http://www.ck12.org/saythanks (placed in a visible location) in addition to the following terms. Except as otherwise noted, all CK-12 Content (including CK-12 Curriculum Material) is made available to Users in accordance with the Creative Commons Attribution-Non-Commercial 3.0 Unported (CC BY-NC 3.0) License (http://creativecommons.org/ licenses/by-nc/3.0/), as amended and updated by Creative Com- mons from time to time (the “CC License”), which is incorporated herein by this reference.