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Page 5857, results 146401 - 146425

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Petrography of the Athol quadrangle, Massachusetts
Anita Louise Mook
1967, Open-File Report 68-185
The Athol quadrangle of north-central Massachusetts is underlain by high-grade metamorphosed amphibolites, gneisses, schists, calc-silicate gneisses, quartzites, and orthogneisses. These include the Monson Gneiss of Middle Ordovician or older age, the Partridge Formation of Middle Ordovician age, and the Middle to Late Devonian Hardwick Granite of the New Hampshire Plutonic...
Preliminary geologic section from Pahute Mesa, Nevada Test Site, to Enterprise, Utah
P. J. Barosh
1967, Open-File Report 67-11
The 154-mile long geologic cross section trends nearly perpendicular to the structural grain of the Basin-Range province in Nevada, and in Utah extends eastward into the transition zone between the Basin-Range and Colorado Plateau provinces. The structure is characterized by complex thrust: faults, involving uppermost Precambrian to lower Mesozoic sedimentary...
Preliminary geologic map of Ellipse III-9-5 and vicinity
R.S. Saunders, T.A. Mutch
1967, Open-File Report 68-197
Ellipse III-9-5 is in a level area between Mare Cognitum and Oceanus Procellarum, approximately 125 km southeast of the crater Lansberg. Mare material within the map area is covered with a greater number of subdued craters than typical smooth mare. ...
Water-resources of the Antelope Valley-East Kern Water Agency area, California
R. M. Bloyd Jr.
1967, Open-File Report 67-21
The Antelope Valley-East Kern Water Agency (AVEK) area, most of which is within the Mojave Desert region of southern California, lacks adequate water resources to sustain the existing rate of ground-water pumpage for irrigation, industrial, and domestic use. However, by 1972 the California Aqueduct, a part of the California Water...
Preliminary geologic map of Lunar Orbiter site orb III P-9
H. A. Pohn
1967, Open-File Report 68-215
Lunar Orbiter site III P-9 occupies a lowland area between Mare Cognitum and Oceanus Procellarum, approximately 135 km southeast of the crater Lansberg and approximately 240 km due south of the crater Reinhold. ...
General field and office procedures for indirect discharge measurements
M. A. Benson, Tate Dalrymple
1967, Techniques of Water-Resources Investigations 03-A1
The discharge of streams is usually measured by the current-meter method. During flood periods, however, it is frequently impossible or impractical to measure the discharges by this method when they occur. Consequently, many peak discharges must be determined after the passage of the flood by indirect methods, such as slope-area,...