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Page 6101, results 152501 - 152525

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Publication Extents

Not all publications have extents, not all extents are completely accurate
The Mesaverde group at Sunnyside, Utah
Harold Brodsky
1960, Open-File Report 60-18
The Mesaverde group of Late Cretaceous age at Sunnyside, Utah consists in ascending order; the Blackhawk formation, Castlegate sandstone and the Price River formation. The Mancos shale inter-tongues with the Blackhawk formation.The Mancos shale formed in an offshore marine environment, the Blackhawk formation formed in a mixed marine and continental...
Gravity survey in part of the Snake River Plain, Idaho — A preliminary report
Harry L. Baldwin Jr., David P. Hill
1960, Open-File Report 60-11
During the early summer of 1959, a total of 1,187 gravity stations were occupied on the western part of the Snake River plain in Idaho. An area of 2,000 square miles extending from Glenns Ferry, Idaho, to Caldwell, Idaho, was covered with a station density of one station per two...
Evaporation control research, 1955-58
Robert R. Cruse, Guy Earl Harbeck
1960, Water Supply Paper 1480
One hundred fifty-two compounds and compositions of matter were screened as potential evaporation retardants. The homologous straight-chain fatty alkanols are considered the best materials for retardants. Several methods of application of the alkanols to the reservoir surface were investigated. Although wick-type drippers for the application of liquids and cage rafts...
Flood-frequency analyses, Manual of Hydrology: Part 3
Tate Dalrymple
1960, Water Supply Paper 1543-A
This report describes the method used by the U.S. Geological Survey to determine the magnitude and frequency of momentary peak discharges at any place on a stream, whether a gaging-station record is available or not. The method is applicable to a region of any size, as a river basin or...
Borehole geophysical methods for analyzing specific capacity of multiaquifer wells : ground-water hydraulics
Gordon D. Bennett, Eugene P. Patten Jr.
1960, Water Supply Paper 1536-A
Conventional well-logging techniques, combined with measurements of flow velocity in the borehole, can provide information on the discharge-drawdown characteriBtic8 of the several aquifers penetrated by a well. The information is most conveniently presented in a graph showing aquifer discharges as functions of the water level in the well at a...