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Page 5058, results 126426 - 126450

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Sediment characteristics of Tennessee streams and reservoirs
Stanley W. Trimble, William P. Carey
1984, Open-File Report 84-749
Measured suspended-sediment data and reservoir sedimentation data have been analyzed to determine sediment yields and transport characteristics of Tennessee streams. Measured suspended-sediment is mostly silt and clay size material even in the sand-bed channels of western Tennessee. Unmeasured load accounts for less than 10 percent of the total sediment load...
Geohydrology of the valley-fill aquifer in the Cohocton area, upper Cohocton River, Steuben County, New York
David B. Terry, Timothy S. Pagano, Martha L. Shaw, Arlynn W. Ingram
1984, Water-Resources Investigations Report 85-4040
The Cohocton valley-fill aquifer, composed of outwash, kame, and alluvial sand and gravel, is highly productive and is in hydraulic contact with the Cohocton River. Potential well yields range from 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow water-table conditions and vulnerable to...
Geohydrology of the valley-fill aquifer in the Bath area, Lower Cohocton River, Steuben County, New York
Timothy S. Pagano, D.B. Terry, M.L. Shaw, A.W. Ingram
1984, Water-Resources Investigations Report 85-4095
The Bath valley-fill aquifer, southern New York, composed of outwash, ice-contact, and ice-disintegration sand and gravel, is highly productive and is in many areas in hydraulic contact with the Cohocton River. Potential well yields range 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow...
Climatic data for Williams Lake, Hubbard County, Minnesota, 1983
A.M. Sturrock, D.O. Rosenberry, L.G. Engelbrecht, W.A. Gothard, T. C. Winter
1984, Open-File Report 84-247
Research on the hydrology of Williams Lake, north-central Minnesota includes study of evaporation. Presented here are those climatic data needed for energy-budget and mass-transfer studies,including: water-surface temperature, dry-bulb and wet-bulb air temperatures, wind speed, precipitation, and solar radiation. Data are collected at raft and land stations....
Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma
Robert B. Morton
1984, Open-File Report 84-445
A study of water-quality degradation due to brine contamination was made in an area of about 1,700 square miles in east-central Oklahoma. The study area coincides, in part, with the outcrop of the Vamoosa-Ada aquifer of Pennsylvanian age.Water samples collected from 180 wells completed in the Vamoosa-Ada aquifer, and at...
Cost effectiveness of the stream-gaging program in Maine; A prototype for nationwide implementation
Richard A. Fontaine, M. E. Moss, J.A. Smath, W. O. Thomas
1984, Water Supply Paper 2244
This report documents the results of a cost-effectiveness study of the stream-gaging program in Maine. Data uses and funding sources were identified for the 51 continuous stream gages currently being operated in Maine with a budget of \$211,000. Three stream gages were identified as producing data no longer sufficiently needed...
Water-level hydrographs for observation wells in Virginia, 1982
Stephen Farrington, Natalie Carrington, W.V. Daniels Jr.
1984, Open-File Report 84-134
Water-well data for 1982 are presented from 147 observation wells in Virginia. Historical data from two wells are also included. A description of each observation well is provided that gives the well location, site identification number, hydrologic unit, owner, aquifer, well characteristics, general remarks, period of record, and extreme measurements...
Cost effectiveness of the stream-gaging program in northeastern California
S.H. Hoffard, V.F. Pearce, Gary D. Tasker, W.H. Doyle
1984, Water-Resources Investigations Report 84-4127
Results are documented of a study of the cost effectiveness of the stream-gaging program in northeastern California. Data uses and funding sources were identified for the 127 continuous stream gages currently being operated in the study area. One stream gage was found to have insufficient data use to warrant cooperative...
Test well DO-CE 88 at Cambridge, Dorchester County, Maryland
Henry Trapp Jr., LeRoy L. Knobel, Harold Meisler, P. Patrick Leahy
1984, Water Supply Paper 2229
Test well DO-CE 88 at Cambridge, Maryland, penetrated 3,299 feet of unconsolidated Quaternary, Tertiary and Cretaceous sediments and bottomed in quartz-monzonite gneiss. The well was drilled to provide data for a study of the aquifer system of the northern Atlantic Coastal Plain. Twenty-one core samples were collected. Six sand zones...