Charles F. Knudson
Carl A. Posey, editor(s)
1973, Earthquake Information Bulletin (USGS) (5) 18-20
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Publication Extents
Not all publications have extents, not all extents are completely accurateCarl A. Posey
1973, Earthquake Information Bulletin (USGS) (5) 8-11
Carl A. von Hake
1973, Earthquake Information Bulletin (USGS) (5) 25-27
1973, Report
No abstract available....
Wilbur C. Ballance
1973, Report
Inflatable straddle packers were used to isolate and test 19 intervals ranging from 56 to 747 meters (183 to 2,450 feet) each in hole UAe-2, Amchitka Island, Alaska. Packer seats were poor in part of the hole because of unstable wall conditions. Thus, some zones had to be tested several...
J.G. Rogers Jr., O. Maller
1973, Physiological Psychology (1) 199-200
The preference of male red-winged blackbirds for solutions of sucrose and sucrose with 0.03 M sodium chloride was tested, using a two-bottle choice test. Preliminary experiments demonstrated that the birds were indifferent to 0.03 M NaCl in water. Both control and experimental animals exhibited indifference to the solutions at the...
J.G. Cronin, C.R. Follett, G.H. Shafer, P.L. Rettman
1973, Bulletin 6310
The Brazos River Basin in Texas extends from the New Mexico State line southeastward to the Gulf of Mexico. The basin is about 600 miles long and ranges in width from 1 to 120 miles--an area of about 42,000 square miles, which includes all or parts of 69 counties. About...
Alton F. Robertson
1973, Florida Bureau of Geology Report of Investigations 64
The Lakeland ridge area of this investigation covers about 300 square miles in northwest Polk County in central Florida. The growth of industry, phosphate mining, and citrus production as well as population growth during the last two decades has resulted in an increase in ground-water pumpage from about 11 billion...
Clyde A. Wilson
1973, Report 166
Coke County, located in semiarid west-central Texas, where large ranches, small farms, and oil production are the main bases of the economy, has a small supply of ground and surface water. Of the approximately 1,900 acre-feet of fresh to moderately saline ground water used in 1968, industry used 880 acre-feet,...
M.L. Maderak
1973, Report 170
Wheeler and eastern Gray Counties are in the east·central part of the Texas Panhandle. The two counties are characterized by rolling to fairly rugged topography with many sand-dune areas and a well developed drainage system....
William M. Sandeen, John B. Wesselman
1973, Report 163
The Chicot and Evangeline aquifers are the only hydrologic units bearing fresh (less than 1,000 milligrams per liter dissolved solids) or slightly saline water (1,000-3,000 milligrams per liter dissolved solids in Brazoria County. These aquifers are composed of gravel, sand, silt, and clay of Pliocene, Pleistocene, and Holocene age....
C. E. Roberson, Robert Schoen
1973, Journal of Research of the U.S. Geological Survey (1) 367-370
Some thermal water sources of the Snake River basin, Idaho, are near saturation with respect to fluorite. That mineral was identified by X-ray diffraction in precipitates induced in three water samples by adding sodium fluoride. The derived solubility product (KS0) for zero ionic strength was close to that calculated from...
E. G. Crosthwaite
1973, Water Information Bulletin 32
The results of drilling test holes to depths of approximately 1,000 feet in the Mud Lake region show that a large part of the region is underlain by both sedimentary deposits and basalt flows. At some locations, predominantly sedimentary deposits were penetrated; at others, basalt flows predominated. The so-called Mud...
Joe S. Downey
1973, Bulletin 64-2
The objectives of the hydrologic investigation in Griggs and Steele Counties, N. Dak. (fig. 1) were to: (1) determine the location, extent, and nature of the major aquifers; (2) evaluate the occurrence and movement of ground water, including recharge and discharge; (3) estimate the quantities of water stored in the...
Gerald G. Schaber
1973, Book chapter, Apollo 17 preliminary science report
Orbital photographs taken at low-Sun illumination during both the Apollo 15 (ref. 30-14) and Apollo 17 missions have provided excellent data on the lava flows in the southwestern Mare Imbrium. These photographs have been used recently to present a detailed photogeologic evaluation of these flows and their role in mare...
Joseph M. Boyce, Arthur L. Dial Jr.
1973, Book chapter, Apollo 17 preliminary science report (NASA SP-330)
The lunar maria formed at different times and in multiple stages of extrusion. An understanding of their evolution is essential in placing the Apollo samples in a regional context and in interpreting the regional geology of a vast part of the lunar surface....
David H. Scott
1973, Book chapter, Apollo 17 preliminary science report (NASA SP-330)
Apollo 17 permission geologic studies of the Taurus-Littrow region of the Moon revealed numerous small structures, in both mare and terra, having somewhat similar morphologies and variously resembling fault scarps, flow fronts, and mare ridges. Many of these features are too small to be identified on Lunar Orbiter IV photographs,...
Gene Simmons, David Strangway, Peter Annan, Richard G. Baker, Lawrence Bannister, Raymond E. Brown, William Cooper, Dean Cubley, Joseph deBettencourt, Anthony W. England, John Groener, Jin-Au Kong, Gerald LaTorraca, James Meyer, Ved Nanda, David Redman, James Rossiter, Leung Tsang, Joseph Urner, Raymond Watts
1973, Book chapter, Apollo 17 preliminary science report (NASA SP-330)
The surface electrical properties (SEP) experiment was used to explore the subsurface material of the Apollo 17 landing site by means of electromagnetic radiation. The experiment was designed to detect electrical layering, discrete scattering bodies, and the possible presence of water. From the analysis of the data, it was expected...
Richard J. Pike
1973, Book chapter, Apollo 17 preliminary science report (NASA SP-330)
Morphometry, the quantitative study of shape, complements the visual observation and photointerpretation in analyzing the most outstanding landforms of the Moon, its craters (refs. 32-1 and 32-2). All three of these interpretative tools, which were developed throughout the long history of telescopic lunar study preceding the Apollo Program, will continue...
J.C. Maher, W.M. Trollman, J.M. Denman
1973, Book
The following list of references includes most of the geological literature on the San Joaquin Valley and vicinity in central California (see figure 1) published prior to January 1, 1973. The San Joaquin Valley comprises all or parts of 11 counties -- Alameda, Calaveras, Contra Costa, Fresno, Kern, Kings, Madera,...
H. J. Moore, G.L. Tyler
1973, Book chapter, Apollo 17 preliminary science report (NASA SP-330)
Stereoscopic photographs taken by the metric and panoramic cameras can be used to obtain information on the roughness and slope-frequency distributions of lunar surfaces (see appendix to this part). Bistatic radar on board Apollo 14, 15, and 16 spacecraft may also be used to obtain information on lunar surface roughness...
Sherman S.C. Wu, Francis J. Schafer, Gary M. Nakata, Raymond Jordan
1973, Book chapter, Apollo 17 preliminary science report (NASA SP-330)
Stereoscopic photographs of the Moon taken by the metric and panoramic cameras on board the service module of Apollo spacecraft provide a source for quantitative data on lunar topography. The accuracy of the topographic data depends, in part, on the repeatability of elevation measurements. The repeatability depends on contrast in...
I.L. Tailleur, B. L. Mamet, J.T. Dutro Jr.
1973, American Association of Petroleum Geologists Bulletin (57) 1348-1352
New collections of foraminifers and macrofossils from Nuka Ridge, the type area of the enigmatic Nuka Formation, demonstrate that the type Nuka Formation is not a continuous stratigraphic sequence as originally described. Paleontologic evidence indicates the presence of a structurally repeated sequence at Nuka Ridge consisting of Upper Mississippian (Meramec...
Don E. Wilhelms
1973, Book chapter, Apollo 17 preliminary science report (NASA SP-330)
Apollo 17 metric photographs (fig. 29-26) provide the best available coverage for geologic interpretation of northern Mare Crisium and the northern Crisium basin. The area was covered previously by low-resolution telescopic and Lunar Orbiter IV photographs and by oblique, high-illumination, or low-resolution photographs from earlier Apollo missions. One region in...
W.R. Muehlberger, R. M. Batson, E.A. Cernan, V. L. Freeman, M. H. Hait, H. E. Holt, K. A. Howard, E.D. Jackson, K.B. Larson, V. S. Reed, J. J. Rennilson, H.H. Schmitt, D. H. Scott, R. L. Sutton, D. Stuart-Alexander, G.A. Swann, N.J. Trask, G. E. Ulrich, H. G. Wilshire, E.W. Wolfe
1973, Book chapter, Apollo 17 preliminary science report
The Apollo 17 lunar module (LM) landed on the flat floor of a deep valley that embays the mountainous highlands at the eastern rim of the Serenitatis basin. Serenitatis, the site of a pronounced mascon, is one of the major multi-ringed basins on the near side of the Moon. The...