Upper Hudson River Watershed

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Upper Hudson RNortih Evlba er Watershed Keene Elizabethtown Moriah Newcomb Headwaters North Hudson Crown Point Long Lake Hudson River Upper Schroon River Ticonderoga Minerva Schroon Cedar Boreas Indian Lake River River Hague Chester Horicon Jessup Lower Schroon River Johnsburg River East Brance Bolton Lake Pleasant Sacandaga River Upper Arietta Thurman Warrensburg Sacandaga Morehouse River Stony Creek Stony Lake George Wells East Stony Creek West Branch Creek Queensbury Hartford Sacandaga River Kingsbury Hadley Lake Luzerne Day Glens Falls Hebron Hope Benson Lower Sacandaga Moreau Black Argyle West Stony River Snook Fort Edward Creek Edinburg Creek Corinth Kill Northampton Stratford Northumberland Salem Bleecker Wilton Greenwich Headwaters Caroga Middle Greenfield Batten Batten Kill Mayfield Sacandaga Kill Providence Fish Jackson River Saratoga Springs Ü Saratoga Broadalbin Creek JohnstownGloversville Milton Owl 0 2.755.5 11 16.5 22 Galway Easton Miles Gloversville Cambridge Perth Kill Malta White Creek Stillwater Charlton Ballston Hoosick Walloomsac Upper Hudson River Watershed Anthony River Lower Hoosic Kill Mohawk River Watershed River Clifton Park Halfmoon SchaghticokePittstown Hudson River Estuary Watershed Waterford Middle Hoosic Cohoes Grafton River Hudson and Mohawk Rivers Brunswick Green Island Petersburgh Watervliet Stream Channels Troy Upper Hoosic Berlin River Town County Stephentown Watershed Boundary Dataset and National Hydrography Dataset from USGS. Sources: Esri, GEBCO, NOAA, National Geographic, Garmin, HERE, Geonames.org, Civil Boundaries from the NYS Office of Information Technology Services GIS Program Office. and other contributors, Esri, Garmin, GEBCO, NOAA NGDC, and other contributors.

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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.
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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
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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.
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Thursday,May19,201111:50:38AM G:\002200-002299\002260\HR07_02_03\Graphics\Trifold\CleaningupHudsonTrifold-April2011.cdr R O P T E L C A T T fEngineers of I N O CsSPRUDSITE SITE SUPERFUND SUPERFUND PCBs PCBs ® E N SAm Corps Army US M A Hudson Hudson River River N G O E R I N V C N Y E U S N E I T T E A D T S 020H0.20-laigu usnTrifold.cdr-4/18/11-GRA Hudson up 002260.HR07.02.03-Cleaning 58 9-07 r olfe 88 596-3655 (888) toll-free or, 792-4087, (518) rdigifrainpoeline: phone information dredging rjc,cl eea lcrcs24-hour Electric's General call project, oakqetoso oc ocrsaotthe about concerns voice or questions ask To or yappointment. by hours rdy :0am o43 .. ihevening with p.m., 4:30 to a.m. 8:00 Friday, h il fiehusaeMna through Monday are hours Office Field The [email protected] 58 4-39o 86 1-40Toll-Free 615-6490 (866) or 747-4389 (518) usnFls Y12839 NY Falls, Hudson 2 oe anStreet Main Lower 421 eilpooo h usnRvradisfloodplain its and River Hudson the of photo Aerial usnRvrFedOffice Field River Hudson Coordinator aiaRomanowski, Larisa omnt Involvement Community Floodplain P Contact: EPA River pig2011 Spring www.epa.gov/hudson Floodplain fiea h drs eo rlgo to on log or below address the at Office ii,cl,o rt oteHdo ie Field River Hudson the to write or call, Visit, Source: Microsoft Corporation, 2009 PCBs o oeInformation: More For usnRiver Hudson r needed. are odtriei nei lau measures cleanup interim if determine to laigUp Cleaning sdt upeetacmrhniestudy comprehensive a supplement to used usn h eut ftesmln ilbe will sampling the of results The Hudson.
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Eastern NY Excluding Long Island 2014
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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.
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Water-Quality Assessment of the Hudson River Basin in New York and Adjacent States −
Water-quality Assessment Of The Hudson River Basin In New York And Adjacent States − Analysis of available nutrient, pesticide, volatile organic compound, and suspended-sediment data, 1970-90 By Patrick J. Phillips and Dorothea W. Hanchar _____________________________________ U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 96-4065 Troy, New York 1996 i U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon Eaton, Director For additional information Copies of this report can be write to: purchased from: U.S. Geological Survey District Chief Branch of Information Services U.S. Geological Survey, WRD Federal Center 425 Jordan Road Box 25425 Troy, N.Y. 12180 Denver, CO 80225-8286 ii FOREWORD The mission of the U.S. Geological Survey (USGS) is to assess the quantity and quality of the earth resources of the Nation and to provide information that will assist resource managers and policymakers at Federal, State, and local levels in making sound decisions. Assessment of water-quality conditions and trends is an important part of this overall mission. One of the greatest challenges faced by water-resources scientists is acquiring reliable information that will guide the use and protection of the Nation's water resources. That challenge is being addressed by Federal, State, interstate, and local water-resource agencies and by many academic institutions. These organizations are collecting water-quality data for a host of purposes that include: compliance with permits and water-supply standards; development of remediation plans for a specific contamination problem; operational decisions on industrial, wastewater, or water-supply facilities; and research on factors that affect water quality.
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52 Hudson River Basin 01325000 Sacandaga River At
52 HUDSON RIVER BASIN 01325000 SACANDAGA RIVER AT STEWARTS BRIDGE, NEAR HADLEY, NY LOCATION.--Lat 43°18'41", long 73°52'04", Saratoga County, Hydrologic Unit 02020002, on left bank 1.0 mi downstream from Stewarts Bridge, 1.1 mi west of Hadley, 1.4 mi upstream from mouth, and 1.5 mi downstream from Stewarts Bridge hydroelectric plant. DRAINAGE AREA.--1,055 mi2. PERIOD OF RECORD.--September 1907 to current year. Published as "near Hadley" 1907-l910, "at Hadley" 1911-32 and "at Conklingville" 1932-52. Records published for both sites October 1951 to September 1952. REVISED RECORDS.--WSP 1302: 1908. WSP 1432: 1910-12, 1916-21, WDR NY-83-1: 1968(M), 1971-72(M), 1976-77(M), 1979(M). GAGE.--Water-stage recorder and crest-stage gage. Datum of gage is 582.00 ft above NGVD of 1929. Prior to Jan. 1, 1911, nonrecording gage at site about 1 mi upstream at different datum. Jan. 1, 1911 to Sept. 30, 1932, water-stage recorder at site 0.8 mi downstream at datum 8.82 ft lower than present datum. Oct. 1, 1932 to Sept. 30, 1952, water-stage recorder at site 3.6 mi upstream at datum 85.47 ft higher than present datum. REMARKS.--No estimated daily discharges. Records good except those below about 50 ft3/s, which are fair. Flow regulated by Great Sacandaga Lake since Mar. 27, 1930 (see station 01323500); discharge over spillway, part or all or several days in 1983, 1990, 1993, 2000, 2003-04 (only spillage since completion of Conklingville Dam in 1930).
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