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Apollo 12 voice transcript pertaining to the geology of the landing site Apollo 12 voice transcript pertaining to the geology of the landing site
This document is an edited record of the conversations between the Apollo 12 astronauts and mission control pertaining to the geology of the landing site. It contains all discussions and observations documenting the lunar landscape, its geologic characteristics, the rocks and soils collected, and the lunar surface photographic record along with supplementary remarks essential to the...
Authors
N. G. Bailey, G. E. Ulrich
The 1959 Hebgen Lake, Montana, earthquake: Two geological points of view The 1959 Hebgen Lake, Montana, earthquake: Two geological points of view
No abstract available.
Authors
Irving J. Witkind
Influence of rainfall and ancient landslide deposits on recent landslides (1950-71) in urban areas of Contra Costa County, California Influence of rainfall and ancient landslide deposits on recent landslides (1950-71) in urban areas of Contra Costa County, California
No abstract available.
Authors
Tor Helge Nilsen, Barbara L. Turner
Probable effects of the Leviathan Creek basin landslide, Alpine County, California Probable effects of the Leviathan Creek basin landslide, Alpine County, California
No abstract available.
Authors
Patrick A. Glancy, T.J. Katzer
Peritidal lithologies of Cambrian carbonate islands, Carrara Formation, southern Great Basin Peritidal lithologies of Cambrian carbonate islands, Carrara Formation, southern Great Basin
The Carrara Formation is a heterogeneous sequence of quartzites, siltstones, shales, limestones, dolostones, and mixed terrigenous-carbonate rocks. It is Early and Middle Cambrian in age (Stewart, 1970; Palmer, 1971). Figure 32-1 illustrates the general distribution of Carrara lithologies along a transect approximately normal to depositional strike (Fig. 32-2). The formation contains...
Authors
Robert B. Halley
Earthquake mechanism and displacement fields close to fault zones: Report on the Sixth GEOP Research Conference Earthquake mechanism and displacement fields close to fault zones: Report on the Sixth GEOP Research Conference
The Sixth Geodesy/Solid Earth and Ocean Physics (GEOP) Research Conwas held on February 4–5, 1974, at the Institute of Geophysics and Planetary Physics, University of California, San Diego, in La Jolla, California. It was attended by about 100 persons. James N. Brune, program chairman, opened the conference and delivered the introductory address, a somewhat extended version of which is...
Authors
Craig R. Allen, Jon Berger, Ivan I. Mueller, James C. Savage, J. Weertman
Geodetic determination of strain at the Nevada Test Site following the Handley event Geodetic determination of strain at the Nevada Test Site following the Handley event
Repeated surveys of a trilateration network (aperture greater than 20 km) centered on ground zero for the HANDLEY event, a nuclear explosion at the Nevada Test Site with yield in excess of 1 megaton, suggest that the explosion induced an east-west extension of the network by more than 50 mm. In the year following the detonation, this deformation reversed such that the final configuration
Authors
James C. Savage, W. T. Kinoshita, W.H. Prescott
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