Vermont Water Quality Standards Environmental Protection Rule Chapter 29A
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DEERFIELD RIVER WATERSHED Assessment Report
DEERFIELD RIVER WATERSHED Assessment Report 2004-2008 Downstream of Fife Brook Dam The Commonwealth of Massachusetts Executive Office of Environmental Affairs The Commonwealth of Massachusetts Executive Office of Environmental Affairs 251 Causeway Street, Suite 900 Boston, MA 02114-2119 Mitt Romney GOVERNOR Kerry Healey LIEUTENANT GOVERNOR Tel: (617) 626-1000 Fax: (617) 626-1181 Ellen Roy Herzfelder or (617) 626-1180 SECRETARY http://www.state.ma.us/envir November 19, 2004 Dear Friends of the Deerfield River Watershed: It is with great pleasure that I present you with the Assessment Report for the Deerfield River Watershed. The report helped formulate the 5-year watershed action plan that will guide local and state environmental efforts within the Deerfield River Watershed over the next five years. The report expresses some of the overall goals of the Executive Office of Environmental Affairs, such as improving water quality, restoring natural flows to rivers, protecting and restoring biodiversity and habitats, improving public access and balanced resource use, improving local capacity, and promoting a shared responsibility for watershed protection and management. The Deerfield River Watershed Assessment Report was developed with input from the Deerfield River Watershed Team and multiple stakeholders including watershed groups, state and federal agencies, Regional Planning Agencies and, of course, the general public from across the Watershed. We appreciate the opportunity to engage such a wide group of expertise and experience as it allows the state to focus on the issues and challenges that might otherwise not be easily characterized. From your input we have identified the following priority issues: • Water Quantity • Water Quality • Fish Communities • Wildlife and Terrestrial Habitat • Open Space • Recreation I commend everyone involved in this endeavor. -
Native Americans Ol'
Native Americans ol' Clarendon, Vermont *This is only a report of my early findings. This is subject to charge as new evidence and facts arise. I\rly research has led me to cliscover two groups of Native Americiurs that could have resided in Clarendon and one other that may have simply passed through time to time. The tribe of Native l[mericans that has the highest likelihood of being in Clarendon isi the Mahican, specifically the subdivision Mahican proper. Their territory extended from Poughkeepsie, New York to Deerfield, I\4assachusetts, and extended flrttrest north in Rutland. It is important to mention that tlhey are not to be mistaken with the Mohegan tribes of Connecticut; however, they do have lineage witkr one another. As a side note, the Mahicans have lineage with the Lenape and ['equot. Other names for the Mahicans is as follows: Akochakanen (koquois name that means "Those who,speak a strangertongue"), Canoe Indians (Given by colonists), Hikanagi/Nhilcana (Given by the Shawnee), Laups (Given by the French), Orunges (,Given by a school textbook author, Chauvignerie, who rvas referring to a specific Mahican tribe in 1736), River Indians (Given by the Dutch), and Uragees (Again given by an author, Colden, in reference to a specific tribe of the.Mahicans 1747). Mahicans were hunters of southwestem and western Vermont. lheir langrllge belonged to the linguistic family of the Algonquian, spoken with an r-dialect. Sieldom did they settle anywhere in Vermont to stay due to the fact that they were typically hLunters, hotvever, it is not irnprobable that they had permanent selllements in Clarendon.r Historic territory of the |tdahicans l Swanton, John R., The lndion Tribes of North America,1953 pg. -
1 Hartford Agricultural Oral History Project Interview Transcription June 29, 2012 White River Junction, VT Interviewer: Ka
HOHP_Schaal_Transcript Hartford Agricultural Oral History Project Interview Transcription June 29, 2012 White River Junction, VT Interviewer: Kaitlin O’Shea Interviewees: Pete Schaal Location: White River Junction, VT Time: 8:30am KO: Kaitlin O’Shea PS: Peter Schaal The Hartford Agricultural Oral History Project, the 2012 segment, is funded by the US Department of the Interior, National Park Service, for the Certified Local Government Program of Vermont’s annual program under the provisions of the National Historic Preservation Act. Previously, Hartford’s agricultural oral history has been documented primarily through volunteers, often with interview recordings and transcriptions occurring at separate phases with different people. In 2009, additional historical research was provided through the 2009 Vermont Barn Census. The purpose of this agricultural oral history project is to document the history of local residents who grew up or worked on a farm in the Town of Hartford. The Town is comprised of five villages: White River Junction, Hartford, Wilder, Quechee and West Hartford, in addition to several smaller hamlets. TIME & TRANSCRIPTION TOPICS 00:00:01 00:00:01 Introductions KO: Today is Friday June 29, 2012. I am Kaitlin O’Shea and I am interviewing Pete Schaal for the Hartford Agricultural Oral History Project. Good morning and thank you for having me. PS: Good morning Kaitlin. It’s a pleasure to have you down. Farming, KO: So you said that you were farming in the ‘50s. Can you tell me 1950s. Family where you grew up and a little bit about your family? farm in MA; Guernsey PS: Sure. We started farming at a small scale in a little town called cattle; [Stow in Massachusetts]. -
Town of Hartford Draft Town Plan
TOWN OF HARTFORD DRAFT TOWN PLAN March 11, 2019* Prepared by the Hartford Planning Commission with the assistance from the Hartford Department of Planning and Development Services and the Town Plan Steering Committee * This Plan has been updated since the 2/22/19 Draft. The additions are highlighted in red and underlined, and deletions are highlighted in red with the slash-out feature. In some instances, these reflect relocation and not substantial changes. INTRODUCTION INTRODUCTION TO TOWN PLANNING According to the book, “Essentials of Land Use Planning and Regulation” by the Vermont Land Use Education and Training Collaborative, “the municipal plan is the visionary document that assesses the current status of a community and lays out a vision for the future.” Used interchangeably with the term “Town Plan”, it is an in-depth, comprehensive, long range study that provides the framework for future decisions regarding land use, transportation, community facilities and services, utilities, natural resources, historic resources, and housing. It is a guide that establishes a strategy on how to grow while managing the community’s resources and maintaining a high quality of life. The Town Plan provides the basis for public and private investment. It also establishes an implementation program that provides a means of achieving the community vision. HARTFORD’S GEOGRAPHY Hartford, Vermont is located at the confluence of the White and Connecticut Rivers and includes a third river, the Ottauquechee. It is also at the junction of Interstate Highways 89 and 91 and the junction of U.S. Highways 4 and 5 on the eastern side of Vermont about halfway up the state. -
Town of Shrewsbury, Vermont Local Hazard Mitigation Plan
Town of Shrewsbury, Vermont Local Hazard Mitigation Plan Date of Adoption Prepared by the Town of Shrewsbury With the assistance of The Rutland Regional Planning Commission Table of Contents 1. Introduction……………………………………………………………………………………..……...2 2. Purpose……………………………………………………………………………………………..…..3 3. Community Background……………………………………………………………………………….3 4. Planning Process…………………..……………………………………………………………….…..6 4.1. Plan Changes……………………………………………………………………………………...7 5. Community Hazard Inventory and Risk Assessment…………………………………………………10 5.1. Low Risk Hazards………………………………………………………………………………..11 Aircraft Crashes……………………………………………………………………………….….11 Continuity of Government/Record Retention…………………………………………………….11 Hazardous Materials, Radiological and Chemical/Biological Incidents…………………………11 Drought…………………………………………………………………………………………...12 Earthquakes……………………………………………………………………………………….12 Structure Fires…………………………………………………………………………………….13 Temperature Extremes…………………………………………………………………………....13 Terrorism………………………………………………………………………………………….13 Water Supply Contamination………………………………………………………………….....13 Winter Storms, Ice Storms, and Power Outages………………………………………………....14 Wildfires and Forest Fires………………………………………………………………………..14 5.2. Medium Risk Hazards…………………………………………………………………………...14 Climate Change………………………………………………………………………………….14 Dam Failure……………………………………………………………………………………...14 5.3. High Risk Hazards……………………………………………………………………………….15 Floods, Fluvial Erosion, and Ice Jams…………………………………………………………...15 Highway and Railroad Accidents………………………………………………………………..17 -
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 -
The New Deal Versus Yankee Independence: the Failure of Comprehensive Development on the Connecticut River, and Its Long-Term Consequences
The New Deal versus Yankee independence: The failure of comprehensive development on the Connecticut River, and its long-term consequences Eve Vogel1 Department of Geosciences, UMass Amherst With assistance from Alexandra Lacy 2011 alumna (BS, Environmental Sciences), UMass Amherst Adapted from: Vogel, Eve and Alexandra Lacy. Forthcoming. The New Deal versus Yankee independence: The failure of comprehensive development on the Connecticut River, and its long-term consequences. The Northeastern Geographer 4 (2) Introduction For a person familiar with federal dams on major rivers in the American West or South, a visit to an Army Corps of Engineers dam in New England’s largest river basin, the Connecticut, can be a startling experience. Instead of an extended reservoir, one looks down from the empty heights and on both sides sees only a small river far below. Nor is there the fanfare – the visitors center, the historical information, the celebratory propaganda. Simply finding one of the Connecticut River’s federal dams can take some effort. None are on the mainstem. One must drive through the bucolic New England byways and forested hills to find a dam on a tributary (See Figure 1). For New Englanders, the near-invisibility of federal dams may not seem surprising. New England’s history and identity, including the Connecticut Valley’s, seem to rest with the small- to medium-scale development of rivers with mill dams during the 17th thru 19th centuries (e.g. Delaney 1983; Steinberg 1991). It might be more startling for many to learn that during the mid- twentieth century, the federal government did build a series of very large dams in the Connecticut Basin, which have had profound effect on the river. -
Glover Flood Resilience Element
FLOOD RESILIENCE PLAN for the Town of Glover, Vermont Prepared by Meghann Carter NorthWoods Stewardship Center East Charleston, VT in cooperation with the Glover Planning Commission and Glover Selectboard February, 2015 Paid for in part by the Barton Hydro Project Municipal Planning Grant Introduction With an all-hazards mitigation plan now written and pending approval, the Town of Glover is obligated to begin to address identified pertinent hazards, one of which is flooding and fluvial erosion. The purpose of this plan is to identify key hazard areas which are most likely to be affected by flood and fluvial erosion and to propose potential actions to minimize these hazards and their impacts. Potential major points of impact include dams, culverts, bridges, and infrastructure such as roads and buildings within the floodplains. Goals (1) Identify areas of greatest risk to flooding and fluvial erosion within the Town of Glover. (2) Develop recommendations for future actions to create a flood-and fluvial erosion-safe Glover, minimizing threats to public safety, property, and water quality. Flooding and Fluvial Erosion in Vermont Flooding and fluvial erosion are Vermont’s most common and costly types of natural disaster and over time, many compounding factors have increased Vermont’s susceptibility to flood damage. As climate change affects global temperature fluctuations, storms of greater power and higher frequency are anticipated, and indeed this trend has been observed in recent decades. This trend had led to global, state, and regional efforts to better prepare for these events by identifying sensitive resources, key areas of vulnerability, and implementing mitigations. In the interest of promoting local flood resilience, as of July 1, 2014, according to new legislation (Act 16), any newly adopted or readopted municipal or regional plan must have a Flood Resilience Plan Element. -
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 ...................... -
Nutrient Loading and Impacts in Lake Champlain – Missisquoi Bay and Lake Memphremagog
Nutrient Loading and Impacts in Lake Champlain – Missisquoi Bay and Lake Memphremagog Missisquoi Bay. IJC Collection Lake Memphremagog. IJC Collection Missisquoi Bay Cyanobacteria. Pierre Leduc Prepared by the International Joint Commission April 21, 2020 Table of Contents I. Synthesis Document ........................................................................................................................ 3 A. Context ........................................................................................................................................ 3 Cyanobacteria .................................................................................................................................. 3 Actions and Consequences of Non-action ........................................................................................ 3 The Governments’ Reference ........................................................................................................... 4 IJC’s Approach to the Reference ...................................................................................................... 5 Workshops to Review Science and Policy on Nutrient Loading ........................................................ 6 Public Meeting and Online Consultation .......................................................................................... 6 B. IJC Analysis of SAG Reports ....................................................................................................... 7 C. Common Basin Recommendations and IJC Recommendations -
Surface Waters of Vermont
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 424 SURFACE WATERS OF VERMONT BY C. H. PIERCE Prepared in cooperation with the STATE OF VERMONT WASHINGTON GOVEENMENT PBINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BK PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 25 CENTS PER COPY CONTENTS. Introduction.............................................................. 5 Cooperation................................................................ 8 Division of work.......................................................... 8 Definition of terms......................................................... 9 Explanation of data........................................................ 9 Accuracy of field data and computed results................................ 11 Gaging stations maintained in Vermont..................................... 12 St. Lawrence River basin................................................. 13 Lake Champlain drainage basin......................................... 13 General features................................................... 13 Gaging-station records.............................................. 14 Lake Champlain at Burlington, Vt.............................. 14 Lake Champlain outlet (Richelieu River) at Chambly, Province of Quebec.1................................................. 20 Poultney Eiver near Fair Haven, Vt............................ 25 Otter Creek at Middlebury, -
Quechee Gorge State Park Trail System
Quechee Gorge State Park Trail System North Quechee Main St Ottauquechee River e ag ill V ee ech Dewey’s Qu to 4 Rt Mill to US Pond to Quechee V illage dam r e t n e C e r u t a N S N I V o Dewey’s Mill Rd 4 t Parking Visitor Center to White Ri ver Jct Restrooms Quechee Gorge Picnic area Bridge Wheelchair accessible Quechee Trail Gorge Trail Pets allowed on leash Campground Ottauquechee River y Cliff l n o s r Foot trail e p m shaded areas are private property a d c registere 0 200 400 800 scale in feet rev. 11/06 Variable trail conditions may exist; please use caution. Check with the Quechee Gorge Visitor Center for current conditions. Quechee Gorge Geology Legacy of the Ice Age West of Quechee Village, Vermont, the Ottauquechee River flows eastward within a broad and shallow valley. At Dewey’s Mills, just east of Quechee Village, the river turns abruptly southward and plunges into the narrow, rocky cleft of Quechee Gorge, 165 feet deep and over a mile in length. p re-g lac ia What caused this deep and spectacular natural feature? l O tt a Long before Quechee Gorge was formed, the Ottauquechee River u qu made a more gradual southward bend about a mile east of the present site of echee River the Gorge (Fig. 1). About 100,000 years ago, Earth’s climate cooled dramatically. The massive Laurentide Ice Sheet formed in northern Canada and flowed southward over New England (Fig.