Cleaning up Hudson River Pcbs Project Brochure
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Freshwater Fishing: a Driver for Ecotourism
New York FRESHWATER April 2019 FISHINGDigest Fishing: A Sport For Everyone NY Fishing 101 page 10 A Female's Guide to Fishing page 30 A summary of 2019–2020 regulations and useful information for New York anglers www.dec.ny.gov Message from the Governor Freshwater Fishing: A Driver for Ecotourism New York State is committed to increasing and supporting a wide array of ecotourism initiatives, including freshwater fishing. Our approach is simple—we are strengthening our commitment to protect New York State’s vast natural resources while seeking compelling ways for people to enjoy the great outdoors in a socially and environmentally responsible manner. The result is sustainable economic activity based on a sincere appreciation of our state’s natural resources and the values they provide. We invite New Yorkers and visitors alike to enjoy our high-quality water resources. New York is blessed with fisheries resources across the state. Every day, we manage and protect these fisheries with an eye to the future. To date, New York has made substantial investments in our fishing access sites to ensure that boaters and anglers have safe and well-maintained parking areas, access points, and boat launch sites. In addition, we are currently investing an additional $3.2 million in waterway access in 2019, including: • New or renovated boat launch sites on Cayuga, Oneida, and Otisco lakes • Upgrades to existing launch sites on Cranberry Lake, Delaware River, Lake Placid, Lake Champlain, Lake Ontario, Chautauqua Lake and Fourth Lake. New York continues to improve and modernize our fish hatcheries. As Governor, I have committed $17 million to hatchery improvements. -
NY Excluding Long Island 2017
DISCONTINUED SURFACE-WATER DISCHARGE OR STAGE-ONLY STATIONS The following continuous-record surface-water discharge or stage-only stations (gaging stations) in eastern New York excluding Long Island have been discontinued. Daily streamflow or stage records were collected and published for the period of record, expressed in water years, shown for each station. Those stations with an asterisk (*) before the station number are currently operated as crest-stage partial-record station and those with a double asterisk (**) after the station name had revisions published after the site was discontinued. Those stations with a (‡) following the Period of Record have no winter record. [Letters after station name designate type of data collected: (d) discharge, (e) elevation, (g) gage height] Period of Station Drainage record Station name number area (mi2) (water years) HOUSATONIC RIVER BASIN Tenmile River near Wassaic, NY (d) 01199420 120 1959-61 Swamp River near Dover Plains, NY (d) 01199490 46.6 1961-68 Tenmile River at Dover Plains, NY (d) 01199500 189 1901-04 BLIND BROOK BASIN Blind Brook at Rye, NY (d) 01300000 8.86 1944-89 BEAVER SWAMP BROOK BASIN Beaver Swamp Brook at Mamaroneck, NY (d) 01300500 4.42 1944-89 MAMARONECK RIVER BASIN Mamaroneck River at Mamaroneck, NY (d) 01301000 23.1 1944-89 BRONX RIVER BASIN Bronx River at Bronxville, NY (d) 01302000 26.5 1944-89 HUDSON RIVER BASIN Opalescent River near Tahawus, NY (d) 01311900 9.02 1921-23 Fishing Brook (County Line Flow Outlet) near Newcomb, NY (d) 0131199050 25.2 2007-10 Arbutus Pond Outlet -
Waterbody Classifications, Streams Based on Waterbody Classifications
Waterbody Classifications, Streams Based on Waterbody Classifications Waterbody Type Segment ID Waterbody Index Number (WIN) Streams 0202-0047 Pa-63-30 Streams 0202-0048 Pa-63-33 Streams 0801-0419 Ont 19- 94- 1-P922- Streams 0201-0034 Pa-53-21 Streams 0801-0422 Ont 19- 98 Streams 0801-0423 Ont 19- 99 Streams 0801-0424 Ont 19-103 Streams 0801-0429 Ont 19-104- 3 Streams 0801-0442 Ont 19-105 thru 112 Streams 0801-0445 Ont 19-114 Streams 0801-0447 Ont 19-119 Streams 0801-0452 Ont 19-P1007- Streams 1001-0017 C- 86 Streams 1001-0018 C- 5 thru 13 Streams 1001-0019 C- 14 Streams 1001-0022 C- 57 thru 95 (selected) Streams 1001-0023 C- 73 Streams 1001-0024 C- 80 Streams 1001-0025 C- 86-3 Streams 1001-0026 C- 86-5 Page 1 of 464 09/28/2021 Waterbody Classifications, Streams Based on Waterbody Classifications Name Description Clear Creek and tribs entire stream and tribs Mud Creek and tribs entire stream and tribs Tribs to Long Lake total length of all tribs to lake Little Valley Creek, Upper, and tribs stream and tribs, above Elkdale Kents Creek and tribs entire stream and tribs Crystal Creek, Upper, and tribs stream and tribs, above Forestport Alder Creek and tribs entire stream and tribs Bear Creek and tribs entire stream and tribs Minor Tribs to Kayuta Lake total length of select tribs to the lake Little Black Creek, Upper, and tribs stream and tribs, above Wheelertown Twin Lakes Stream and tribs entire stream and tribs Tribs to North Lake total length of all tribs to lake Mill Brook and minor tribs entire stream and selected tribs Riley Brook -
Town of Arlington Hazard Mitigation Plan Arlington, Vermont
Town of Arlington Hazard Mitigation Plan Arlington, Vermont April 8, 2019 Revised May 23, 2019 Revised July 15, 2019 Adopted August 26, 2019 Table of Contents List of Tables ........................................................................................... 2 List of Figures ......................................................................................... 3 I. Introduction ...................................................................................... 1 A. Purpose ............................................................................................................................................... 1 B. Mitigation Goals .................................................................................................................................. 2 II. Town Profile ...................................................................................... 2 A. Regional Context ................................................................................................................................. 2 B. Demography and Land Use ................................................................................................................. 2 C. Economic and Cultural Resources ....................................................................................................... 3 D. Critical Facilities .................................................................................................................................. 3 III. Planning Process .............................................................................. -
Autumn 2008 Newsletter.Pub
The Hoosic River Voice New s from the Hoosic River W atershed Association Autum n 2008 Vermont Un-assessed Waters Project financed by the sale may fly, and stone fly larvae.) of the state’s con- Vermont regularly assesses BMI servation license populations on most of the state’s plates), Kelly has streams (usually on a once-every- begun the Vermont several-years basis), but the state al- Un-assessed Waters locates its resources over a large area Project on Hoosic to capture water quality trends and and Batten Kill identify major sources of pollution. tributaries in Ver- As a result, about 18% of Vermont’s mont. watercourses have never been sam- The goal of the pro- pled. ject is to determine In Basin 1, this is changing. In water quality on un- 2008, for the first time, BMIs were assessed streams by sampled on seven Hoosic tributaries sampling and that had never before been assessed. Steve Fiske VT DEC aquatic biologist (L), and Kelly Nolan, analyzing ben- (Kelly also sampled at five sites in HooRWA monitoring coordinator, discuss physical habitat at thic macroinver- the Batten Kill watershed.) Barney Brook in Bennington in September. tebrate (BMI) In each watershed, Kelly has used populations, and Vermont DEC sampling protocols The Hoosic is undeniably special, documenting high water quality and data processing quality assur- but in at least one respect we are not tributaries in Basin 1. (BMIs are the ance/quality control methods, ensur- alone. With the Batten Kill, we are creatures that live on the bottom of ing that the information collected is the only Vermont watersheds which our streams, critters like caddis fly, comparable and compatible with data drain to the Hudson River. -
Distribution of Ddt, Chlordane, and Total Pcb's in Bed Sediments in the Hudson River Basin
NYES&E, Vol. 3, No. 1, Spring 1997 DISTRIBUTION OF DDT, CHLORDANE, AND TOTAL PCB'S IN BED SEDIMENTS IN THE HUDSON RIVER BASIN Patrick J. Phillips1, Karen Riva-Murray1, Hannah M. Hollister2, and Elizabeth A. Flanary1. 1U.S. Geological Survey, 425 Jordan Road, Troy NY 12180. 2Rensselaer Polytechnic Institute, Department of Earth and Environmental Sciences, Troy NY 12180. Abstract Data from streambed-sediment samples collected from 45 sites in the Hudson River Basin and analyzed for organochlorine compounds indicate that residues of DDT, chlordane, and PCB's can be detected even though use of these compounds has been banned for 10 or more years. Previous studies indicate that DDT and chlordane were widely used in a variety of land use settings in the basin, whereas PCB's were introduced into Hudson and Mohawk Rivers mostly as point discharges at a few locations. Detection limits for DDT and chlordane residues in this study were generally 1 µg/kg, and that for total PCB's was 50 µg/kg. Some form of DDT was detected in more than 60 percent of the samples, and some form of chlordane was found in about 30 percent; PCB's were found in about 33 percent of the samples. Median concentrations for p,p’- DDE (the DDT residue with the highest concentration) were highest in samples from sites representing urban areas (median concentration 5.3 µg/kg) and lower in samples from sites in large watersheds (1.25 µg/kg) and at sites in nonurban watersheds. (Urban watershed were defined as those with a population density of more than 60/km2; nonurban watersheds as those with a population density of less than 60/km2, and large watersheds as those encompassing more than 1,300 km2. -
Central Library of Rochester and Monroe County · Historic Monographs Collection
Central Library of Rochester and Monroe County · Historic Monographs Collection Central Library of Rochester and Monroe County · Historic Monographs Collection A FOB THE TOURIST J1ND TRAVELLER, ALONO THE LINE OF THE CANALS, AND TUB INTERIOli COMMERCE OF THE STATE OF NEW-YORK. BT HORATIO GATES SPAFFORD, LL. IX AUTHOR OF THE GAZETTEER Of SKW-IOBK. JfEW-YOBK: PRIXTEB BY T. AND J. SWORDS, No. 99 Pearl-street. 1824. Prfee SO Ceats. Central Library of Rochester and Monroe County · Historic Monographs Collection Northern-District of New-York, In wit: BE it remembered, thut on the twelfth day of July, in the forty-ninth year of the Inde pendence of the United States of America, A. D 1824. Harutio G. Spajford, of the said District, hath deposited in this Office the title of a Book, the right whereof he claims as Author, in the word& following, to wit: **A Pocket Guide for the Tourist and Traveller, along the line of the Canals, and the interior Commerce of the State of New-York. By Horatio Gates Spaffor'dyLL.D. Author of the Gazetteer of Nete-York." In conformity to the Act of the Congress of the United States, entitled, " An Act for the Encouragement of Learn ing, !>y securing the Copies of Maps, Charts, and Books, to the Authors and Proprietors of such Copies, during the times therein mentioned;" and also to the Act, entitled " An Act, supplementary to an Act, entitled ' An Act for the Encou ragement of Learning, !>y securing the Copies of Maps, Charts, and Hooks, to the Authors and Proprietors of such Copies during the times therein mentioned,' and extending the Benefits thereof to the Arts of Designing, Engraving, and Etching Historical and other Prints." R. -
Rayburn, Desimone, and Frappier B4-1
Rayburn, DeSimone, and Frappier B4-1 NEW INSIGHTS INTO GLACIAL LAKES VERMONT AND ALBANY By John A. Rayburn1, Dept. of Geology, SUNY New Paltz, New Paltz, NY 12443 David J. DeSimone2, DeSimone Geoscience Investigations, Petersburg, NY 12138 Amy B. Frappier3, Department of Geosciences, Skidmore College, Saratoga Springs, NY 12866 Email addresses: [email protected], [email protected], [email protected] INTRODUCTION The first comprehensive study of the proglacial lakes in the Hudson and Champlain Valleys was published by J.B. Woodworth in 1905 (NYSM Bulletin 84). He noted that “Lake Albany doubtless began on the south in the waters standing in front of the retreating ice sheet prior to the opening of the Mohawk outlet of the great glacial lakes to the west. As soon as the ice retreated in the valley to a position north of Albany and the drainage of Lake Iroquois came into the Hudson Valley Lake Albany properly came into existence”. While glacial lacustrine sediments in the Champlain Valley were originally attributed by Upham (1889), Baldwin (1894), Peet (1904), and others to be a separate Glacial Lake Champlain, Woodworth notes that its confines were somewhat larger and proposed the name of Glacial Lake Vermont, and that to the south it was certainly confluent with Glacial Lake Albany as he defined. “The outlet of theses ice-dammed waters at this early stage of confluence across the present divide of the Hudson and Champlain basins is a matter which concerns the interpretation of Lake Albany on the south and is considered in that connection. Lake Vermont may be said properly to have come into existence when in consequence of a local lowering of waters south of Fort Edward a discharge began across a barrier into the Hudson Valley to the south.” While Woodworth (1905) only described one Lake Albany level, he noted under Lake Vermont that there were the Quaker Springs, Coveville, and Fort Edward levels. -
Vermont Agency of Natural Resources Watershed Management Division Batten Kill Walloomsac Hoosic
Vermont Agency of Natural Resources Watershed Management Division Batten Kill Walloomsac Hoosic TACTICAL BASIN PLAN The Hudson River Basin (in Vermont) - Water Quality Management Plan was prepared in accordance with 10 VSA § 1253(d), the Vermont Water Quality Standards1, the Federal Clean Water Act and 40 CFR 130.6, and the Vermont Surface Water Management Strategy. Approved: Pursuant to Section 1-02 D (5) of the VWQS, Basin Plans shall propose the appropriate Water Management Type of Types for Class B waters based on the existing water quality and reasonably attainable and desired water quality management goals. ANR has not included proposed Water Management Types in this Basin Plan. ANR is in the process of developing an anti-degradation rule in accordance with 10 VSA 1251a (c) and is re-evaluating whether Water Management Typing is the most effective and efficient method of ensuring that quality of Vermont's waters are maintained and enhanced as required by the VWQS, including the anti-degradation policy. Accordingly, this Basin Plan is being issued by ANR with the acknowledgement that it does not meet the requirements of Section 1-02 D (5) of the VWQS. The Vermont Agency of Natural Resources is an equal opportunity agency and offers all persons the benefits of participating in each of its programs and competing in all areas of employment regardless of race, color, religion, sex, national origin, age, disability, sexual preference, or other non-merit factors. This document is available upon request in large print, braille or audiocassette. VT Relay Service for the Hearing Impaired 1-800-253-0191 TDD>Voice - 1-800-253-0195 Voice>TDD Hudson River Basin Tactical Plan Overview 2 | P a g e Basin 01 - Batten Kill, Walloomsac, Hoosic Tactical Basin Plan – Final 2015 Table of Contents Executive Summary .................................................................................................................................... -
Washington County, New York Data Book
Washington County, New York Data Book 2008 Prepared by the Washington County Department of Planning & Community Development Comments, suggestions and corrections are welcomed and encouraged. Please contact the Department at (518) 746-2290 or [email protected] Table of Contents: Table of Contents: ....................................................................................................................................................................................... ii Profile: ........................................................................................................................................................................................................ 1 Location & General Description .............................................................................................................................................................. 1 Municipality ............................................................................................................................................................................................. 3 Physical Description ............................................................................................................................................................................... 4 Quality of Life: ............................................................................................................................................................................................ 5 Housing ................................................................................................................................................................................................. -
Freeze-Up Ice Jams
ICE JAM REFERENCE AND TROUBLE SPOTS Ice Jam Reference Ice jams cause localized flooding and can quickly cause serious problems in the NWS Albany Hydrologic Service Area (HSA). Rapid rises behind the jams can lead to temporary lakes and flooding of homes and roads along rivers. A sudden release of a jam can lead to flash flooding below with the addition of large pieces of ice in the wall of water which will damage or destroy most things in its path. Ice jams are of two forms: Freeze up and Break up. Freeze up jams usually occur early to mid winter during extremely cold weather. Break up jams usually occur mid to late winter with thaws. NWS Albany Freeze Up Jam Criteria: Three Consecutive Days with daily average temperatures <= 0°F NWS Albany Break Up Jam Criteria: 1) Ice around 1 foot thick or more? And 2) Daily Average Temperature forecast to be >= 42°F or more? Daily Average Temperature = (Tmax+Tmin)/2 Rainfall/snowmelt with a thaw will enhance the potential for break up jams as rising water helps to lift and break up the ice. A very short thaw with little or no rain/snowmelt may not be enough to break up thick ice. ** River forecasts found at: http://water.weather.gov/ahps2/forecasts.php?wfo=aly will not take into account the effect of ice. ** Ice jams usually form in preferred locations in the NWS Albany HSA. See the “Ice Jam Trouble Spots” below for a list of locations where ice jams frequently occur. Ice Jam Trouble Spots **This is not an all inclusive list, but rather a list of locations where ice jams have been reported in the past. -
How's the Water? Hudson River Water Quality and Water Infrastructure
HOW’S THE WATER? Hudson River Water Quality and Water Infrastructure The Hudson River Estuary is an engine of life for the coastal ecosystem, the source of drinking water for more than 100,000 people, home to the longest open water swim event in the world, and the central feature supporting the quality of life and $4.4 billion tourism economy for the region. This report focuses on one important aspect of protecting and improving Hudson River Estuary water quality – sewage-related contamination and water infrastructure. Untreated sewage puts drinking water and recreational users at risk. Water quality data presented here are based on analysis of more than 8,200 samples taken since 2008 from the Hudson River Estuary by Riverkeeper, CUNY Queens College, Columbia University’s Lamont- Doherty Earth Observatory; and from its tributaries by dozens of partner organizations and individual 21% community scientists. Water infrastructure information Hudson River Estuary samples presented here is based on data from the Department that failed to meet federal safe of Environmental Conservation and Environmental swimming guidelines Facilities Corporation, which administers State Revolving Funds. 44 Municipally owned wastewater While the Hudson River is safe for swimming at most treatment plants that locations on most days sampled, raw sewage overflows discharge to the Estuary and leaks from aging and failing infrastructure too often make waters unsafe. The Hudson’s tributaries $4.8 Billion – the smaller creeks and rivers that feed it – are often Investment needed in sources of contamination. wastewater infrastructure in the Hudson River Watershed To improve water quality, action is needed at the federal, state and local levels to increase and prioritize infrastructure investments.