Water resources of the Heber-Kamas-Park City area north-central Utah, with a section on a gravity and aeromagnetic survey of Heber and Rhodes Valleys
Claud H. Baker Jr., D. L. Peterson
1970, Technical Publication 27
This report on the water resources of the Heber-Kamas-Park City area was prepared by the U. S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights. The primary purpose of the report is to provide the Division of Water Rights with the basic hydrologic...
Hydrology reconnaissance of the Sink Valley area, Tooele and Box Elder Counties, Utah
Don Price, E.L. Bolke
1970, Technical Publication 26
This is the sixth in a series of reports by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, which describe the water resources of selected basins in western Utah. Areas covered by previously published reports in this series are shown in...
Field trip guidebook to the hydrogeology of the Rock-Fox River basin of Southeastern Wisconsin
C. L. R. Holt Jr., R. D. Cotter, J. H. Green, P. G. Olcott
1970, Wisconsin Geological & Natural History Survey Information Circular 17
On this trip we will examine some hydrogeologic characteristics of glacial features and emphasize ground-water management within the Rock-Fox River basin. Field stops will include the hydrogeology of a classical glacial terrane--the Kettle moraine--and the management of ground-water resources for industrial, municipal, agricultural, and fish-culture purposes. Descriptions of the geology,...
A test of flushing procedures to control salt-water intrusion at the W. P. Franklin Dam near Ft. Myers, Florida and The magnitude and extent of salt-water contamination in the Caloosahatchee River between La Belle and Olga, Florida
Durward H. Boggess
1970, Information Circular 62
During low-flow periods, salty water from the tidal part of the Caloosahatchee River moves upstream during boat lockages at the W. P. Franklin Darn near Ft. Myers, Florida, as shown on figure L Salty water enters the lock chamber through openings of the downstream sector gates which separate tidal and...
A hydrologic analysis of the New Jersey Pine Barrens region
Edward C. Rhodehamel
1970, New Jersey Division of Water Policy and Supply Water Resources Circular 22
No abstract available....
Statistical summaries of New Jersey streamflow records
Stanley L. Laskowski
1970, New Jersey Division of Water Policy and Supply Water Resources Circular 23
In 1961 the U.S. Geological Survey prepared a report which was published by the State of New Jersey as Water Resources Circular 6, "New Jersey Streamflow Records analyzed with Electronic Computer" by Miller and McCall. Basic discharge data for periods of record through 1958 were analyzed for 59 stream-gaging stations...
Water in Maryland: a review of the Free State's liquid assets
Patrick N. Walker
1970, Educational Series 2
Temperature and water-quality conditions of the Patuxent River estuary, Maryland, January 1966 through December 1967
Robert L. Cory, Jon W. Nauman
1970, Chesapeake Science (11) 199-209
The effect of power plant cooling water in raising natural water temperatures at a location near the power plant on the Patuxent River estuary is clearly evident from thermograph records. Surface temperature at a station 333 m (1,000 ft) downstream from the discharge canal was raised an average of about...
Hydrogeologic data for the Lower Arkansas River Valley, Colorado
Thomas J. Major, R. Theodore Hurr, John Ezra Moore
1970, Ground Water Basic Data Report 21
Geology and ground water resources, Williams County, North Dakota
Theodore F. Freers, C. A. Armstrong
1970, North Dakota Geological Survey Bulletin 48
Williams County, in northwestern North Dakota, is located near the center of the structural and sedimentary Williston basin. The preglacial sedimentary formations beneath the county are as much as 14,828 feet thick. Their beds dip generally to the south except along the flanks of the north-south striking Nesson anticline in...
Geology and ground water resources of Grand Forks County
Dan E. Hansen, Jack Kume, T. E. Kelly, Q.F. Paulson
1970, Bulletin 53
Grand Forks County in northeastern North Dakota is underlain by glacial drift, westward-dipping Paleozoic and Mesozoic sedimentary rocks and Precambrian igneous and metamorphic rocks. Glacial drift that covers the bedrock reaches a maximum thickness of 455 feet. It can be differentiated into 5 drift sheets, each of which in turn...
Preliminary geologic investigation of the Apollo 12 landing site: Part A: Geology of the Apollo 12 Landing Site
E.M. Shoemaker, R. M. Batson, A.L. Bean, C. Conrad Jr., D.H. Dahlem, E. N. Goddard, M. H. Hait, K.B. Larson, G. G. Schaber, D. L. Schleicher, R. L. Sutton, G.A. Swann, A. C. Waters
1970, Book chapter, Apollo 12 preliminary science report (NASA SP-235)
This report provides a preliminary description of the geologic setting of the lunar samples returned fromt he Apollo 12 mission. A more complete interpretation of the geology of the site will be prepared after thorough analysis of the data....
Geology and ground water resources of Wells County, North Dakota
John P. Binemie, George A. Falgle, Ronald J. Bred, John R. Reid, Frank Buturla Jr.
1970, Bulletin 51
Wells County is in east-central North Dakota on the eastern flank of the Williston Basin. It is underlain by 4000 to 6000 feet of Paleozoic and Mesozoic rocks that dip gently to the west. The uppermost Cretaceous rocks, the Hell Creek, Fox Hills and Pierre Formations, lie directly beneath the...
Water Resources Data for California, 1969; Part 2: Water Quality Records
1970, Water Data Report CA-69-2
Water-resources investigations of the U.S. Geological Survey include the collection of water-quality data on the chemical and physical characteristics of surface and ground-water supplies of the Nation. Theses data for the 1969 water year for the quality of surface water in California are presented in this report. Data for a...
Water Resources Data for California, 1969; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley
1970, Water Data Report CA-69-1-2
Surface-water records for the 1969 water year for California, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report. Records for a few pertinent gaging stations in bordering States also are included. The records were collected and computed by the...
Water Resources Data for California, 1969; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley
1970, Water Data Report CA-69-1-1
Surface-water records for the 1969 water year for California, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report. Records for a few pertinent gaging stations in bordering States also are included. The records were collected and computed by the...
Water Resources Data for California, 1966, 1967, 1968; Part 3: Ground Water Records
1970, Water Data Report CA-68-3
Ground-water records for wells in California in which periodic measurements of water level have been made during the years 1966-68 are given in this report. The records were collected and processed by the U.S. Geological Survey, Water Resources Division, under the overall supervision of R. Stanley Lord, district chief in...
Water Resources Data for California, 1968; Part 2: Water Quality Records
1970, Water Data Report CA-68-2
Water-resources investigations of the U.S. Geological Survey include the collection of water-quality data on the chemical and physical characteristics of surface- and ground-water supplies of the Nation. These data for the 1968 water year for the quality of surface water in California are presented in this report. Data for a...
Hydrogeologic data for the Upper Housatonic River basin, Connecticut
Robert L. Melvin
1970, Connecticut Water Resources Bulletin 22
The upper Housatonic River basin covers an area of about 700 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,...
Hydrogeologic data for the lower Housatonic River basin, Connecticut
I.G. Grossman, William E. Wilson
1970, Connecticut Water Resources Bulletin 20
This report contains hydrologic and geologic data collected for an investigation of the lower Housatonic River basin by the U.S. Geological Survey in financial cooperation with the Connecticut Water Resources Commission. The report also summarizes data that are available in other publications. The towns within the 557 square mile area...
Water resources inventory of Connecticut Part 4: Southwestern coastal river basins
Robert B. Ryder, Michael A. Cervione Jr., Chester E. Thomas Jr., Mendall P. Thomas
1970, Connecticut Water Resources Bulletin 17
The 44O square miles of the southwestern coastal river basins (394 square miles of which are in Connecticut) yield about 183 billion gallons, or 23.9 inches of runoff during an average year. This amount of runoff is almost entirely derived from precipitation falling on the basins, and is eventually discharged...
Base-flow study of Suamico River basin, Oconto, Brown, Shawano and Outagamie counties, Wisconsin
Robert W. Devaul
1970, Report
The Suamico River is a gaining stream throughout its entire reach. No loss of water from the streams was noted between any measuring sites. The August 12 measurements were made during base-flow period when flow duration was about 50 to 55 percent (table 2). The August 28 measurements were made...
Base-flow study of Little Suamico River basin Oconto, Brown and Shawano counties, Wisconsin
Robert W. Devaul
1970, Report
The Little Suamico River is a gaining stream throughout its entire reach. No loss of water from the streams was noted between any measuring sites. The August 13 measurements were made during a base-flow period when flow duration was about 50 to 55 percent (table 2). The August 27, 28...
Base-flow study of East River basin Brown and Calumet counties, Wisconsin
Robert W. Devaul
1970, Report
Streams in the East River basin gain ground water throughout most of their reaches, however, ground-water pumping of the Green Bay - DePere area may reduce the water being gained by the streams from ground water. The August 13, 14 measurements were made during base-flow period when flow duration was...
Base-flow study of Duck Creek basin Brown and Outagamie counties, Wisconsin
Robert W. Devaul
1970, Report
Streams in the Duck Creek basin gain ground water throughout most of their reaches, however, ground-water pumping of the Green Bay - DePere area may reduce the water being gained by the streams from ground water. The August 11, 12 measurements were made during base-flow period when flow duration was...
