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Saturday, May 2, 2020 | History

3 edition of Hydrogeologic data for the Lower Connecticut River Basin, Connecticut found in the catalog.

Hydrogeologic data for the Lower Connecticut River Basin, Connecticut

J. W. Bingham

Hydrogeologic data for the Lower Connecticut River Basin, Connecticut

by J. W. Bingham

  • 70 Want to read
  • 29 Currently reading

Published by The Dept. in [Hartford] .
Written in English

    Places:
  • Connecticut,
  • Middlesex Co.,
  • New London Co.
    • Subjects:
    • Hydrology -- Connecticut -- Middlesex Co.,
    • Hydrology -- Connecticut -- New London Co.,
    • Borings -- Connecticut -- Middlesex Co.,
    • Borings -- Connecticut -- New London Co.

    • Edition Notes

      Bibliography: p. 6.

      Statementby J. W. Bingham, F. D. Paine, and L. A. Weiss, prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection.
      SeriesConnecticut water resources bulletin ;, no. 30
      ContributionsPaine, F. D., joint author., Weiss, L. A. joint author., Geological Survey (U.S.), Connecticut. Dept. of Environmental Protection.
      Classifications
      LC ClassificationsTD201 .C65 no. 30, GB705.C8 .C65 no. 30
      The Physical Object
      Pagination59 p. :
      Number of Pages59
      ID Numbers
      Open LibraryOL4858524M
      LC Control Number75624020

      Hydrologic modelling of a complex hydrogeo logic basin: Evrotas River Basin area of the watershed) was Mm 3, the karstic recharge wa s Mm 3, the evapotranspiration was Mm 3, . Library of Congress Cataloging in Publications Data. Garabedian, Stephen P. Water Quality in the Connecticut Housatonic, an, d Thames River Basins, Connecticut, Massachusetts, New Hampshire Ne, w York, and Vermont, / by Stephen P Garabedian p cm -- (U S Geologica l Surve circulary, ) Includes bibliographica referencel s.

      Connecticut River Conservancy is the voice for the Connecticut River watershed, from source to sea. We collaborate with partners across four states to protect and advocate for your rivers and educate and engage communities. We bring people together to prevent pollution, improve habitat, and promote enjoyment of your river and its tributary streams. @article{osti_, title = {Hydrogeological restrictions to saline ground-water discharge in the Red River of the North drainage basin, North Dakota}, author = {Strobel, M L}, abstractNote = {Discharge of saline water from bedrock aquifers along the eastern margin of the Williston basin is restricted by surficial glacial till and lacustrine deposits in the Red River of the North drainage.

      Water-chemistry data for selected springs, geysers, and streams in Yellowstone National Park Wyoming, (USGS Open-File Report ) Suspended-sediment concentration and pool sedimentation data for the Gibbon River, Yellowstone National Park, Wyoming, September through October (USGS Open-File Report ). I was hopeing to find more details about the history and construction of the Dams on the Connecticut Lakes. Rivers have always been the lifeblood of the surrounding populations, this book covers a lot of that as well as the the Science of how a river is formed and how it has been tamed to support the vibrant growing economy of the time.4/5(2).


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Hydrogeologic data for the Lower Connecticut River Basin, Connecticut by J. W. Bingham Download PDF EPUB FB2

This report contains geologic, ground-water, and quality-of-water data collected and compiled for a water resources investigation of the upper Connecticut River basin, Connecticut by the U.S. Geological Survey in financial cooperation with the Connecticut Department of Environmental Protection.

These data, together with surface-water data, were collected at sites shown on plate A and are, with. The upper Housatonic River basin covers an area of about square miles in western Connecticut and includes the towns of Bridgewater, Brookfield, Canaan, Cornwall, Kent, New Fairfield, New Hilford, North Canaan, Salisbury, Sharon, Sherman and Warren and parts of Bethel, Bethlehem, Danbury, Goshen, Litchfield, Morris, Newtown, Norfolk, Ridgefield, Roxbury, Southbury, Torrington and Washington.

STATE OF CONNECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION HYDROGEOLOGIC DATA FOR THE UPPER CONNECTICUT RIVER BASIN,CONNECTICUT By Robert and ical Survey 72’ Prepared by the U.

GEOLOGICAL SURVEY in cooperation with the CONNECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION CONNECTICUT WATER Cited by: 4. STATE OF CONNECTICUT WATER RESOURCES COMMISSION HYDROGEOLOGIC DATA FOR THE ’LOWER HOUSATONIC RIVER BASIN,CONNECTICUT By an and William ical Survey 73* 72" 73" Prepared by the U.

GEOLOGICAL SURVEY ~n cooperation with the CONNECTICUT WATER RESOURCES COMMISSION CONNECTICUT WATER RESOURCES Cited by: 2. Lower Connecticut River Connecticut book. CT River at Montague, MA (MNTM3) CT River at Northampton, MA (NHMM3) - High Flow Forecast Location.

CT River at Holyoke Dam, MA (HLUM3) - High Flow Forecast Location. CT River at Holyoke, MA (HLYM3) - High Flow Forecast Location. Chicopee River at Indian Orchard, MA (INDM3) Westfield River at Westfield, MA (WSFM3). Connecticut River was guided by the Policy Committee and the Technical Committee for Fisheries Management of the Connecticut River Basin.

The importance of this formally-structured, coordinating and regulatory body to the restoration program was recognized in when Congressional consent was given to the Connecticut River Basin Atlantic Salmon. Buy Hydrogeologic data for the Lower Connecticut River Basin, Connecticut (Connecticut water resources bulletin) by J.

W Bingham (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : J. W Bingham. Current data typically are recorded at to minute intervals, stored onsite, and then transmitted to USGS offices every 1 to 4 hours, depending on the data relay technique used.

Recording and transmission times may be more frequent during critical events. Connecticut Drainage Basins is the most detailed delineation of natural drainage basins available on a statewide basis for Connecticut. It includes watersheds for Connecticut rivers, streams, brooks, lakes, reservoirs and ponds included on ,scale minute topographic quadrangle maps published by the U.S.

Geological Survey (USGS. The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for miles ( km) through four rises at the U.S.

border with Quebec, Canada, and discharges at Long Island Sound. Its watershed encompasses five U.S. states and one Canadian province, 11, square miles (29, km 2) via tributaries, 38 of which are major : Long Island Sound.

USGS CONNECTICUT RIVER AT THOMPSONVILLE, CT. PROVISIONAL DATA SUBJECT TO REVISION. -- Data temporarily unavailable for the time period specified -- pH, water, unfiltered, field, standard units. Most recent instantaneous value: EDT.

Connecticut River Watershed Boundary. defined by the hyrographic and topographic criteria that delinate an area of land upstream from a specific point on a river, stream, or similar surface waters. The Wilburforce Foundation provides funding to maintain and develop Data.

CONNECTICUT RIVER BASIN ANADROMOUS FISH RESTORATION: Coordination and Technical Assistance FR Annual Progress Report October 1, - Septem U.S. Fish and Wildlife Service Connecticut River Coordinator's Office Kenneth Sprankle, Project Leader East Plumtree Road Sunderland, MA "March " Also shows minor civil divisions and flood warning projects.

Includes source materials note and index of "Watersheds." "" Available also through the Library of Congress. Connecticut River, longest stream in New England, rising in the Connecticut lakes in northern New Hampshire, U.S.

After flowing about 9 miles (14 km) through New Hampshire, it moves roughly southwestward and forms the border between New Hampshire and Vermont for. Welcome to the Headwaters region of the Connecticut River.

Over miles from the sea, the river is wild and cold, with trout to match. The Connecticut rises in tiny Fourth Lake, accessible by a footpath along the US/Canadian border and then through protected land.

A Brief Geological History of the Connecticut River Valley By Prof. Richard D. Little [Please see the 3 rd edition of Dinosaurs, Dunes, and Drifting Continents and/or the DVDs Flow of Time and Rise and Fall of Lake Hitchcock for more in-depth content. They are available at your local library or order from “publications” on the home page of this web site.].

The Mattabesset River as delineated on present-day maps flows out of Harts Ponds in the town of Berlin and travels miles ( km) east to the Connecticut River, passing Kensington and later forming the boundary between Middletown and Cromwell. Further south, the Coginchaug River (or "winding meadow") flows from an upland meadow in Durham, northwards to the Mattabesset just upstream of.

The Flow of Time - Million Years of Geohistory in the Connecticut River Valley With animations and a bit of humor, geologist-educator Richard Little takes you through the amazing events of the last million years in the Connecticut River Valley region, and shows you why.

USGS Current Water Data for Connecticut. Click to hide state-specific text. ICE EFFECTS ON STREAMFLOW - During winter, ice formation may cause stage and discharge values to appear higher than expected.

Ice effects may be minor (occurring only at night and early morning) with baseline flows obvious, or the effects may be major (stage constantly. A standardized mapping of natural drainage basins in Connecticut was completed in by the Connecticut Department of Environmental Protection (DEP).

This drainage basin system divided Connecticut into 8 major basins, 45 regional basins, subregional basins, 2, local basins, and 7, small drainage basin areas.The Connecticut River Conservancy partnered with the Passumpsic Valley Land Trust to remove the East Burke dam on the East Branch of the Passumpsic River in East Burke, VT.

The concrete dam was built in at the same location as previous timber crib dams (the first was built in ).

The Connecticut River is the longest river in New England. Designated the “long tidal river” by the Algonquian peoples of southern New England, it stretches over miles and passes through four states—starting at the northern tip of New Hampshire along the Quebec border and passing through Vermont, Massachusetts, and Connecticut on its way to Long Island Sound.