Stevens-Wells-Waits-Ompompanoosuc River Basin Water Quality Management Plan
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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 -
Surface Water Location of Use Watershe D Town Documentation of Existing
Table A.3. Existing uses of waters for fishing in Basin 14 (RM is river mileage measured from the river terminus) Surface Location of Use Watershe Town Documentation of Existing Use Water d Stevens From Patneaude Lane to Stevens Barnet DFW identifies fishing as an existing River Connecticut River excluding River use based on fishing stocking criteria Barnet Falls, RM 0-2.2 Stevens From Peacham Hollow Brook Stevens Barnet DFW identifies fishing as an existing River to Barnet Center Road RM River use based on fishing stocking criteria 3.8-4.8 Jewett Within Roy Mountain WMA. Stevens Barnet DFW identifies fishing as an existing Brook RM 0.1-1.7 River use based on public access Wells River From Ricker Pond to Wells River Groton, DFW identifies fishing as an existing Newbury/ Ryegate town Ryegate use based on fish stocking criteria line. RM 6.4-16.2 Wells River From below the Boltonville Wells River Newbury DFW identifies fishing as an existing Falls for 0.5 miles. RM 4.6 – use based on fish stocking criteria 5.1 Wells River From .2 miles above the Wells River Newbury DFW identifies fishing as an existing Tenney Pond tributary to use based on fish stocking criteria above Adams Paper and public lands Company Dam. RM 1.7-2.6 East Brook Within Pine Mountain WMA. Wells River Topsham/G DFW identifies fishing as an existing RM 0.9-1.8 roton use based on public access Keenan Within Pine Mountain WMA Wells River Topsham/G DFW identifies fishing as an existing Brook RM. -
Woodsville, New Hampshire and Wells River, Vermont
Woodsville, New Hampshire and Wells River, Vermont 1 2021 Woodsville/Wells River 4th of July Celebration Schedule of Events 9:00 AM Flea Market Opens 11:00 AM Gigantic Parade Until 1:00 PM Barry Hayes 12:30 PM Midway Opens -Vertical Entertainment NH 2:00-8:00 Dunk Tank 1:00-3:00 DJ Mike 2:00-9:00 BINGO Under the Tent 3:00-5:00 Back Shed String Band 5:00-8:00 DJ Mike 8:00-10:00 The Sled Wrenches—opener Bim Tyler 9:00 Parade Winners Announced 9:00 Raffle Drawing - Winners Announced 10:00 PM Immense Fireworks Display! ABSOLUTELY NO PETS ALLOWED ON THE COMMUNITY FIELD 2 Paul “The Barber” Tetreault Paul was known as “The Barber” in Woodsville for well over 60 years. His first shop was located in the Wentworth Hotel Building until a fire destroyed the building and he was forced to re-locate next door in the Mt. Gardner View Apartment Building. After many years at that location, a broken waterpipe and ensuing water damage caused him to re- locate once again to 83 Central Street. He loved his loyal customers who fol- lowed him from shop to shop where they found Paul ready to cut hair and always up-to-date and ready to discuss all the local happenings. Paul and his wife, Lorayne, raised 4 children in North Haverhill. Over the years, the family grew to include 13 grandchildren, 17 great grandchildren and 1 great-great grandchild. Paul served in the NH Army National Guard and was honorably discharged in September 1960. -
Progress Report on River Basin Water Quality Management Planning During 2010
PROGRESS REPORT ON RIVER BASIN WATER QUALITY MANAGEMENT PLANNING DURING 2010 A REPORT FOR: HOUSE & SENATE COMMITTEE ON AGRICULTURE HOUSE & SENATE COMMITTEE ON NATURAL RESOURCES AND ENERGY JANUARY 2011 PREPARED BY: VERMONT AGENCY OF NATURAL RESOURCES DEPARTMENT OF ENVIRONMENTAL CONSERVATION WATER QUALITY DIVISION 103 SOUTH MAIN STREET WATERBURY, VT 05671 www.vtwaterquality.org Introduction..........................................................................................................................................................3 Section 1) Statewide Surface Water Management Strategy - a Framework for Statewide Efforts to Guide Surface Water Management.................................................................................................................................5 Protecting & Improving Surface Waters by Managing Stressors ....................................................................5 What are the 10 Major Stressors affecting Vermont’s surface waters? ...........................................................6 Using the Stressor Approach to Evaluate Program Effectiveness ...................................................................6 Tactical Basin Planning: Managing waters along a gradient of condition.......................................................6 WQD Ambient Surface Water Monitoring & Assessment Strategy................................................................6 Public Input......................................................................................................................................................6 -
Appendices for the West, Williams and Saxtons Rivers and Adjacent Connecticut River Tributaries
Appendices for the West, Williams and Saxtons Rivers and adjacent Connecticut River Tributaries Contents Appendices for the West, Williams and Saxtons Rivers and adjacent Connecticut River Tributaries ....................................... 1 Appendix A – Existing Uses ........................................................................................................................................................................................ 2 Appendix B. 1 – Dams in the Basin ............................................................................................................................................................................ 9 Appendix B. 2 – Coordination Plan ......................................................................................................................................................................... 12 Appendix B – 3. How a Dam Affects a River ............................................................................................................................................................ 19 Appendix B – 4. Whitewater Paddling Releases on the West River ........................................................................................................................ 20 Appendix B – 5. VDFW Whitewater Release Memo ................................................................................................................................................ 22 Appendix C – Fisheries Assessment Summary ........................................................................................................................................................ -
WATERS THAT DRAIN VERMONT the Connecticut River Drains South
WATERS THAT DRAIN VERMONT The Connecticut River drains south. Flowing into it are: Deerfield River, Greenfield, Massachusetts o Green River, Greenfield, Massachusetts o Glastenbury River, Somerset Fall River, Greenfield, Massachusetts Whetstone Brook, Brattleboro, Vermont West River, Brattleboro o Rock River, Newfane o Wardsboro Brook, Jamaica o Winhall River, Londonderry o Utley Brook, Londonderry Saxtons River, Westminster Williams River, Rockingham o Middle Branch Williams River, Chester Black River, Springfield Mill Brook, Windsor Ottauquechee River, Hartland o Barnard Brook, Woodstock o Broad Brook, Bridgewater o North Branch Ottauquechee River, Bridgewater White River, White River Junction o First Branch White River, South Royalton o Second Branch White River, North Royalton o Third Branch White River, Bethel o Tweed River, Stockbridge o West Branch White River, Rochester Ompompanoosuc River, Norwich o West Branch Ompompanoosuc River, Thetford Waits River, Bradford o South Branch Waits River, Bradford Wells River, Wells River Stevens River, Barnet Passumpsic River, Barnet o Joes Brook, Barnet o Sleepers River, St. Johnsbury o Moose River, St. Johnsbury o Miller Run, Lyndonville o Sutton River, West Burke Paul Stream, Brunswick Nulhegan River, Bloomfield Leach Creek, Canaan Halls Stream, Beecher Falls 1 Lake Champlain Lake Champlain drains into the Richelieu River in Québec, thence into the Saint Lawrence River, and into the Gulf of Saint Lawrence. Pike River, Venise-en-Quebec, Québec Rock River, Highgate Missisquoi -
Vermont Master Angler Report
Vermont Master Angler Program 2016 Annual Report Shawn Jud Good Kratzer Prepared by FISH & WILDLIFE DEPARTMENT The Vermont Master Angler Program Vermont’s wealth of waters and abundant fish populations provide THE VERMONT MASTER many opportunities to experience outstanding fishing. The Vermont ANGLER PROGRAM Master Angler Program recognizes the achievements of anglers who HIGHLIGHTS THE DIVERSITY catch trophy-sized fish from Vermont waters and celebrates the fishes’ OF FISH SPECIES IN VERMONT accomplishments in surviving and growing to such exceptional sizes. WATERS THAT OFFER UNIQUE The Master Angler program is a length-based program that sets “trophy AND CHALLENGING ANGLING sized” benchmarks for 33 eligible fish species. While these trophy sized OPPORTUNITIES. fish are a challenge to catch, they are attainable for anglers that develop the necessary knowledge and skills. The Master Angler program encourages anglers to target species that haven’t traditionally been considered sport fish. To do so, they need to grow as anglers and improve their knowledge of fish habitat, behavior, and feeding preferences and develop new skills required to target and catch these species. Award Categories The program offers two award categories for adults and youths: Trophy Angler: Anglers catching a fish exceeding the minimum qualifying length in any of the 33 species categories receive a certificate commemorating their catch. Their names and catches are also included in the Vermont Master Angler Annual Report, posted annually on the Vermont Fish & Wildlife website. Master Angler: Anglers demonstrating the skill necessary to catch multiple species that all exceed the minimum qualifying lengths, in the same calendar year, are recognized as “Vermont Master Anglers” and receive a lapel pin at the end of the year. -
The Impact of Railways on Stanstead: 1850 to 1950 J
Document generated on 10/02/2021 2:08 p.m. Histoire Québec The impact of railways on Stanstead: 1850 to 1950 J. Derek Booth Volume 14, Number 3, 2009 URI: https://id.erudit.org/iderudit/11391ac See table of contents Publisher(s) Les Éditions Histoire Québec ISSN 1201-4710 (print) 1923-2101 (digital) Explore this journal Cite this article Booth, J. D. (2009). The impact of railways on Stanstead: 1850 to 1950. Histoire Québec, 14(3), 10–18. Tous droits réservés © Les Éditions Histoire Québec, 2009 This document is protected by copyright law. Use of the services of Érudit (including reproduction) is subject to its terms and conditions, which can be viewed online. https://apropos.erudit.org/en/users/policy-on-use/ This article is disseminated and preserved by Érudit. Érudit is a non-profit inter-university consortium of the Université de Montréal, Université Laval, and the Université du Québec à Montréal. Its mission is to promote and disseminate research. https://www.erudit.org/en/ VOL nin n \ ni i mi The impact of railways on Stanstead: 1850 to 1950 by J. Derek Booth D' J. Derek Booth was educated at McGill and is Professor Emeritus of Geography at Bishop's University. He is the author of several books on the role of railways in Quebec. This article is based on a lecture by Derek Booth on the occasion of the opening of the Stanstead Historical Society's Summer 2005 exhibition, "Arrival and Departure: The Regional Train." Le Dr J. Derek Booth a fait ses études à l'Université M'Gill; il est actuellement professeur émérite de géographie à l'Université Bishop's. -
FLOODING in the MASSAWIPPI BASIN DURING the 20TH CENTURY Norman Jones Bishop's University
107 FLOODING IN THE MASSAWIPPI BASIN DURING THE 20TH CENTURY Norman Jones Bishop's University RESUME L'histoire des inondations dans les Cantons de l'Est quebecois n'a jamais ete etudiee en detail. Cet article relate I'histoire des inondations dans Ie bassin hydrographique de la riviere Massawippi au 2CF siecle d'un point de vue joumalistique, archivistique et physiographique. Les donnees proviennent de plusieurs joumaux locallX, en particulier du Sherbrooke Record, des photos d'archives reunies par fe Centre de recherche des Cantons de l'Est, des mesures faites de fa physiographie du bassin et des donnees climatiques foumies par Environnement Canada. L'analyse de ces divers types de donnees revele qu'il y a eu des inondations dans Ie bassin de la Massawippi a 6S des 100 demieres annees. Ces inondations ont cause des dommages allX infrastructures gouvemementales, des inconvenients et des pertes d'ordre personnel ainsi que des pertes commerdales, particulierement dans Ie secteur agricofe. Certaines preuves indiquent une augmentation possible de fa frequence des inondations vers fa fin du siecle. La partie inferieure du bassin, Lennoxville et Ie sud de fa ville, est Ie secteur qui a ete Ie plus souvent touche. ABSTRACT The history of flooding in the Eastern Townships of Quebec has never been studied in detail. This article describes the history of flooding in the Massawippi Drainage Basin throughout the 20th century, from a newspaper media, archival and physical geographic perspective. The data are derived from a number of local newspapers, particularly the Sherbrooke Record, from archival photographs collected by the Eastern Townships Research Centre, from measurements of the basin's physiography, and from climate data provided by Environment Canada. -
Geology of the Memphremagog Map Area •
GM 15279 GEOLOGY OF THE MEMPHREMAGOG MAP AREA • C 4 / Jç- I f Ministère des Richesses Neureiles, Québec SERVICE DES GITES MIN Aq, No GM—. 77 \V) C CN`.i:ii;i:T`l'S Chapter 1 Introduction. Chapter II General character o. <.:ty District. Chapter III General'Geology. Chapter IV Structural Geology. .Chapter V Historical Geology. Chapter VI Economic. Geolo gy. Plate I T .7:Tassri;~p~±-- Bunker Brook, - i+'itc:! Bay valley the north. Plate Il Parallel valleys, the second is that of the Tomifobia River and the pronounced valley die:;. is that of Bunker. Brook. • Plate III Looking southeast across Fitch Bay. 77i`.ls o 'Stanstead granodiorite in right background. Plate IV Whetstone Island. The low flat area in the fore•-. ground is underlain by Devonian limestone. hills in the background are of Stanstead diorite. Plate V Looking northwest toward Lake Massaw p i. ground shows .type of topography west of Bunker fault . In the background the ridge east of the .fault can be traced.far to right. .Plate VI Drag `'olds south of Ayer' s Cliff in the Tomifobia • interbedded slates and•limestone. Plate VII Biotite segregation in Stanstead granodior?. Plate VIII Biotite streaks. in Stanstead granodiorite. Plate IX Parallel pegmatite veins in Stanstead granodiorite m' • a _- _•- • . ..- .. --L- ~ Plate X Stanstead Granite Company's quarry at Gran i te-U < i le, showing the excellent sheeting and ideal working conditions. Plate XI Serpentine hill. u~ Figure Index map showing the location of the I:emphre- ma.gog area. Figure. 2. Showing location of diorite areas and points from which specimens were collected. -
Surficial Geology of the Eastern Half of the Saint Johnsbury 7.5 X 15 Minute Quadrangle
I, Springston, G. and Haselton, G.; 1999, Surficial Geology of the Eastern Half of the St. Johnsbury 7.5 X 15 Minute Quadrangle: Vermont Geological Survey Open File Report VG99-8, 5 plates and text. Surficial Geology of the Eastern Half of the Saint Johnsbury 7.5 x 15 Minute Quadrangle • by George E. Springston and George M. Haselton May, 1999 Current Addresses: George E. Springston George M. Haselton 81 East Hill Road 7 Esty Road Plainfield, VT 05667 Westmoreland, NH 03467-4506 (802) 454-1220 • (603) 399-8425 Executive Summary The purpose of this study is to map and interpret the surficial geologic deposits and related landforms of a part of the St. Johnsbury/Danville area. The depth to ledge across most of the study area is generally less than 20 feet and is commonly less than 10 feet. Only in the major stream valleys is the depth to bedrock generally 20 feet or more. By far the greatest depths to bedrock are in the Passump sic River Valley, where the surficial deposits are commonly greater than 100 feet thick. The oldest surficial deposits encountered in the study area consist of two varieties of glacial till: The lowermost of these is a firm, silt-rich till known as basal till and the uppermost is a looser, sandy till known as ablation till. These materials were deposited by the North American Ice Sheet during the last of several glacial episodes which occurred during the Pleistocene Epoch. Deposits of sand and gravel in the study area are of two broad types: Ice-contact deposits which formed from sediments deposited in contact with glacial ice, and glacial outwash which formed from sediments deposited beyond the margin of the glacial ice. -
New Hampshire!
New Hampshire Fish and Game Department NEW HAMPSHIRE FRESHWATER FISHING 2021 DIGEST Jan. 1–Dec. 31, 2021 Go Fish New Hampshire! Nearly 1,000 fishable lakes and 12,000 miles of rivers and streams… The Official New Hampshire fishnh.com Digest of Regulations Why Smoker Craft? It takes a true fisherman to know what makes a better fishing experience. That’s why we’re constantly taking things to the next level with design, engineering and construction that deliver best-in-class aluminum fishing boats for every budget. \\Pro Angler: \\Voyager: Grab Your Friends and Head for the Water Years of Worry-Free Reliability More boat for your bucks. The Smoker Craft Pro Angler The Voyager is perfect for the no-nonsense angler. aluminum fishing boat series leads the way with This spacious and deep boat is perfect for the first feature-packed value. time boat buyer or a seasoned veteran who is looking for a solid utility boat. Laconia Alton Bay Hudson 958 Union Ave., PO Box 6145, 396 Main Street 261 Derry Road Route 102 Laconia, NH 03246 Alton Bay, NH 03810 Hudson, NH 03051 603-524-6661 603-875-8848 603-595-7995 www.irwinmarine.com Jan. 1–Dec. 31, 2021 NEW HAMPSHIRE Fish and Game Department FRESHWATER FISHING 2021 DIGEST Lakes and Rivers Galore I am new to Fish and Game, but I was born and raised in New Hampshire and have spent a lifetime working in the outdoors of our Granite State. I grew up with my friends ice fishing for lake trout and cusk on the hard waters of Lake Winnipesaukee and Lake Winnisquam with my father and his friends.