Adel A. R. Zohdy, Dallas B. Jackson, Robert J. Bisdorf
1975, Open-File Report 75-130
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateKarl W. Stauffer
1975, Open-File Report 75-360
The areal distribution of heavy minerals in 99 samples from stream sands in the southern Hazara District, West Pakistan, indicates that the metamorphic grade of the rocks in the area increases toward the northwest. Minerals of potential economic value in the heavy-mineral samples include scheelite from the Oghi-Batgram-Battal area and...
George William Moore, Larry A. Beyer
1975, Open-File Report 75-330
No abstract available....
John P. D’Agostino
1975, Open-File Report 78-896
No abstract available....
R.M. Slade Jr., J.M. Taylor
1975, Report
The U.S. Soil Conservation Service is actively engaged in the implementation of flood- and soil-erosion reducing measures in Texas under the authority of "The Flood Control Act of 1936 and 1944" and "Watershed Protection and Flood Prevention Act" (Public Law 566), as amended. The Soil Conservation Service has found that...
Alex E. Dong
1975, Report
Donner Lake is easily accessible to the metropolitan areas of Sacramento and San Francisco and is close to many recreational areas in the Sierra Nevada. The lake is used for recreation and is bordered by commercial establishments, summer vacation homes, and a large state campground. Domestic wastes around the lake...
Edward D. Jenkins, Marilyn E. Pabst
1975, Report
Northwestern Kansas, an area of 8,050 square miles (21,000 square kilometres), is a flat to gently rolling plain that is dissected by the Smoky Hill and Republican Rivers. Loessial soils underlying the plain are ideal for cultivation.The climate is semiarid with the mean annual precipitation ranging from 16 to 21...
Stephen C. Wolf
1975, Open-File Report 75-166
No abstract available....
R.D. Steger
1975, Report
No abstract available....
R.M. Slade Jr.
1975, Report
No abstract available....
H.D. Buckner
1975, Report
No abstract available....
H.J. Davidson
1975, Report
No abstract available....
Jack Rawson, H.J. Davidson
1975, Report
No abstract avaiable....
J. K. VanZandt
1975, Report
No abstract available....
J. N. Lee
1975, Report
No abstract available....
J.P. Fisher, H. D. King
1975, Report
No abstract available....
B.B. Hampton
1975, Report
No abstract available....
B.B. Hampton
1975, Report
No abstract available....
R.N. Mitchell
1975, Report
The purpose of this report is to present rainfall and runoff data for the Waller Creek and Wilbarger Creek study areas for the 1973 water year (October 1, 1972 to September 30, 1973)....
John D. Sims, Michael J. Rymer
1975, Open-File Report 75-144
Clear Lake, California is located in the California Coast Ranges about 120 km north of San Francisco and is the largest freshwater lake wholly within California. The lake basin is tectonically controlled (Anderson, 1936; Brice, 1953, Sims and Rymer, 1974) and the area seismically active (Coffman and von Hake, 1973).Interest...
Eleanora I. Robbins, William J. Perry Jr., James A. Doyle
1975, Open-File Report 75-307
Use of palynological zones defined by Brenner and Doyle from the Cretaceous outcrop belt in Maryland, Delaware, and New Jersey permit correlation of the Cretaceous section in four wells drilled to basement in the Salisbury Embayment in the Eastern Shore of Maryland and in Accomack Co., Virginia. These correlations, supplemented...
C. L. Hummel
1975, Open-File Report 75-2
No abstract available....
Edward J. Pluhowski
1975, Open-File Report 75-249
Large-turbidity features along the 275-kilometre long south shore of Lake Ontario were analyzed using LANDSAT-1 images. The ESIAC system developed by the Stanford Research Institute, was used to obtain enlargements and false-color renditions of turbidity plumes. After projection on a video screen, individual turbidity features were analyzed, mapped, and photographed.The...
Patrick A. Glancy, T. L. Katzer
1975, Open-File Report 75-179
No abstract available....
Norman S. MacLeod, George Walton Walker, Edwin H. McKee
1975, Open-File Report 75-348
Rhyolitic domes, flows, and ash-flow tuffs of Miocene to Holocene age form an important part of the thick sequence of Cenozoic volcanic rocks that cover southeastern Oregon east of the Cascade Range. Rhyolitic domes 11-17 m.y. old are widespread, particularly in the easternmost part of the state and in adjacent...