Publications
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Effects of the Bear Valley and San Juan Bautista earthquakes of 1972 on Geodimeter line lengths Effects of the Bear Valley and San Juan Bautista earthquakes of 1972 on Geodimeter line lengths
Measurements of lines of the California Geodimeter network in the vicinity of the epicenters of four 1972 earthquakes (magnitudes 4.7, 4.7, 4.8, and 5.1) along the San Andreas fault system indicate that no significant anomalous changes in line length preceded or accompanied those earthquakes. Within the precision of measurement, the data are consistent with a linear change in line length...
Authors
W.H. Prescott, James C. Savage
Geophysical observations on northern part of Georges Bank and adjacent basins of Gulf of Maine Geophysical observations on northern part of Georges Bank and adjacent basins of Gulf of Maine
Continuous-seismic-reflection and magnetic-intensity profiles provide data for inferences about the geology of the northern part of Georges Bank and the basins of the Gulf of Maine adjacent to the bank. Basement is inferred to be mostly sedimentary and volcanic rocks of Paleozoic age that were metamorphosed and intruded locally by felsic and mafic plutons near the end of the Paleozoic...
Authors
R. N. Oldale, J.C. Hathaway, William P. Dillon, J. D. Hendricks, James M. Robb
Selected chlorinated hydrocarbons in bottom material from streams tributary to San Francisco Bay Selected chlorinated hydrocarbons in bottom material from streams tributary to San Francisco Bay
As part of a study of the environmental quality of San Francisco Bay, bottom material from 26 streams tributary to the Bay were analyzed for chlordane, DDD, DDE, DDT, and PCB residues. These compounds were present in essentially all streams tested. Chlordane proved to be ubiquitous, with a concentration range similar to that of the other compounds. Noteworthy was the occurrence in one...
Authors
LeRoy M. Law, Donald F. Goerlitz
North polar region of Mars: Imaging results from Viking 2 North polar region of Mars: Imaging results from Viking 2
During October 1976, the Viking 2 orbiter acquired approximately 700 high-resolution images of the north polar region of Mars. These images confirm the existence at the north pole of extensive layered deposits largely covered over with deposits of perennial ice. An unconformity within the layered deposits suggests a complex history of climate change during their time of deposition. A...
Authors
J.A. Cutts, K.R. Blasius, G.A. Briggs, M. H. Carr, Ronald Greeley, Harold Masursky
Simulated “true color” images from ERTS data Simulated “true color” images from ERTS data
No abstract available.
Authors
Eric M. Eliason, Pat S. Chavez, Laurence A. Soderblom
Orange material in the Sulpicius Gallus formation at the southwestern edge of Mare Serenitatis Orange material in the Sulpicius Gallus formation at the southwestern edge of Mare Serenitatis
Orange and red materials were observed and photographed in the dark mantle of the Sulpicius Gallus Formation on the southwestern rim of the Serenitatis basin. These materials occur only within the dark mantle that overlies old rilled mare and highland units and are absent on the younger mare unit in this area. Orange and red materials occur predominantly as halos, patches, or rays around...
Authors
Baerbel K. Lucchitta, H.H. Schmitt
Tectonic significance of the Kodiak-Bowie seamount chain, northeastern Pacific Tectonic significance of the Kodiak-Bowie seamount chain, northeastern Pacific
The hypothesis of a fixed melting spot reference frame (M) for relative plate motion is tested in the northeastern Pacific Ocean, where the Kodiak-Bowie seamount chain intersects the northern triple junction between the Pacific, American, and Juan de Fuca plates. Available age determinations on Kodiak and Giacomini Seamounts provide an estimated average rate of volcanic propagation along...
Authors
Eli A. Silver, Roland E. von Huene, James K. Crouch
Interstitial water studies on small core samples, Leg 22 Interstitial water studies on small core samples, Leg 22
Interstitial waters from Leg 22 in the Indian Ocean revealed two unique results: Site 214, on the Ninetyeast Ridge, penetrated through a 30-meter sequence of fine-grained basalt and reentered hard, silty clay containing carbonate skeletal debris. Such a basalt layer may well have been impervious and extensive enough to seal off underlying (fossil) seawater of Paleocene age. However...
Authors
Frank T. Manheim, Lee S. Waterman, Frederick L. Sayles
Diffusimetry (diffusion constant estimation) on sediment cores by resistivity probe Diffusimetry (diffusion constant estimation) on sediment cores by resistivity probe
Measurement of formation factor (ratio of rock resistivity to interstitial water resistivity) from sediment cores provides an indirect measurment of the tortuosity of the fluid channels in the sediments. From these measurements one can estimate the diffusion coefficient of the sediment with depth. The F (formation factor) values for Indian Ocean sediments varied from 1.6 for a clayey...
Authors
Frank T. Manheim, Lee S. Waterman
Deposition of zinc and cadmium by marine bacteria in estuarine sediments Deposition of zinc and cadmium by marine bacteria in estuarine sediments
Mixed cultures of marine bacteria isolated from the sediments of Corpus Christi Harbor were examined for their ability to assimilate or precipitate radioactive zinc and cadmium from solution. Test data indicate that during summer, when bacterial activity is at a maximum, the bacteria and their metabolic byproducts play a significant role in the removal of zinc and cadmium from seawater...
Authors
C.J. McLerran, Charles W. Holmes