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Page 5913, results 147801 - 147825

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Gravimetric effects of petroleum accumulations--A preliminary summary
Thane Hubert McCulloh
1966, Circular 530
Negative gravity anomalies of very local extent and with amplitudes of 1.2 milligals or less have been observed over some known petroleum and natural gas fields in southern California and South Dagestan, U.S.S.R. Field evidence, laboratory measurements, and theory indicate that these anomalies are mainly the result of hydrocarbon pore...
Tectonic creep in the Hayward fault zone, California
Dorothy H. Radbruch-Hall, M. G. Bonilla
1966, Circular 525
Tectonic creep is slight apparently continuous movement along a fault. Evidence of creep has been noted at several places within the Hayward fault zone--a zone trending northwestward near the western front of the hills bordering the east side of San Francisco Bay. D. H. Radbruch of the Geological Survey and...
Evaporation study in a humid region, Lake Michie, North Carolina
J.F. Turner Jr.
1966, Professional Paper 272-G
The mass-transfer and water-budget techniques of calibrating a reservoir for evaporation were evaluated through a study of Lake Michie, N.C. The techniques appear adequate for estimation of lake evaporation and net seepage in humid regions where lake storage is affected by streamflow and ground-water seepage, under conditions no more adverse...
Hydrologic reconnaissance of Point Reyes National Seashore area, California
R. H. Dale, S. E. Rantz
1966, Open-File Report 66-22
This report summarizes the results of a hydrologic reconnaissance of the Point Reyes National Seashore area, the primary purpose of which was to appraise potential sources of water supply at park sites where visitor accommodations are proposed. Point Reyes National Seashore is a peninsular area on the California coast about...
Water resources of the Pomme de Terre River Watershed, West-central Minnesota
R. D. Cotter, L. E. Bidwell
1966, Hydrologic Atlas 220
The watershed is underlain by water-bearing glacial drift, cretaceous rocks, and Precambrian crystalline rocks.  It is an elongate basin 92 miles long and has a drainage area of 977 square miles.  The Pomme de Terre River flows within an outwash valley discharging into the Minnesota River at Marsh Lake....
Recharge studies on the High Plains in northern Lea County, New Mexico
John S. Havens
1966, Water Supply Paper 1819-F
The area described in this report is that part of the southern High Plains principally within northern Lea County, N. Mex. ; it comprises about 1,400,000 acres. Hydrologic boundaries isolate the main aquifer of the area, the Ogallala Formation, from outside sources of natural recharge other than precipitation on the...