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Preseismic and coseismic deformation associated with the Hollister, California, earthquake of November 28, 1974 Preseismic and coseismic deformation associated with the Hollister, California, earthquake of November 28, 1974
The epicenter of the Hollister earthquake (ML = 5.1) of November 28, 1974, is located near the center of an 81‐line trilateration network which has been surveyed annually since 1971. Five lines in the neighborhood of the epicenter were surveyed just 2 days before the earthquake, and two other lines nearby were surveyed 48 days earlier. Although some of these measurements suggest a...
Authors
James C. Savage, Mary Ann Spieth, W.H. Prescott
Strain accumulation on the San Andreas Fault near Palmdale, California Strain accumulation on the San Andreas Fault near Palmdale, California
Precise distance measurements of a 10×25 km 15‐station trilateration network that spans the San Andreas fault west of Palmdale, California, have been repeated annually in the period 1971–1975. The network appears to be deforming under simple uniform tensor shear of about 0.21±0.03 μstrain/yr with the direction of maximum right‐lateral shear parallel to the local strike of the San Andreas...
Authors
W.H. Prescott, James C. Savage
Evidence of post-Pleistocene faults on New Jersey Atlantic outer continental shelf Evidence of post-Pleistocene faults on New Jersey Atlantic outer continental shelf
Recently obtained high-resolution seismic profiles (400-4,000-Hz band) show evidence of faults in shallow sedimentary strata near the edge of the Atlantic continental shelf off New Jersey. Apparent normal faults having a throw of about 1.5 m displace sediments to within 7 m of the sea floor. The faults appear to be overlain by undeformed horizontal beds of relatively recent age. Several...
Authors
R. E. Sheridan, H.J. Knebel
Sclerochronology: a tool for interpreting past environments Sclerochronology: a tool for interpreting past environments
X-radiographs of stony coral slabs reveal two types of annual density bands. Detailed studies of these bands in relation to known variations in air temperatures indicate that sclerochronology is a valid tool for documenting time sequences and changing environmental conditions on a coral reef.
Authors
J. Harold Hudson, Eugene A. Shinn, Robert B. Halley, Barbara H. Lidz
Effects of local geological conditions in the San Francisco Bay region on ground motions and the intensities of the 1906 earthquake Effects of local geological conditions in the San Francisco Bay region on ground motions and the intensities of the 1906 earthquake
Measurements of ground motion generated by nuclear explosions in Nevada have been completed for 99 locations in the San Francisco Bay region, California. The recordings show marked amplitude variations in the frequency band 0.25 to 3.0 Hz that are consistently related to the local geological conditions of the recording site. The average spectral amplifications observed for vertical and...
Authors
Roger D. Borcherdt, James F. Gibbs
Structure and evolution of Bering Sea shelf south of St. Lawrence Island Structure and evolution of Bering Sea shelf south of St. Lawrence Island
The virtually featureless Beringian shelf south of St. Lawrence Island is underlain structurally by at least 14 basins. Encompassing a total area of more than 300,000 sq km, most of the basins are either elongate structural sags, grabens, or half (asymmetric) grabens beneath the outer shelf. The regional trend of these basins is northwest, parallel with that of the continental margin...
Authors
Michael S. Marlow, David W. Scholl, Alan K. Cooper, E. C. Buffington
Coral reef recovery in Florida and the Persian Gulf Coral reef recovery in Florida and the Persian Gulf
Long-term observations and study of coral reef destruction by hurricanes in the Florida Keys show, surprisingly, that although corals are devastated on a grand scale during storms, recovery is rapid. Recovery occurs because of the widespread scattering of live fragments, many of which become growth sites of new colonies. Reef recovery from death by chilling in the Persian Gulf was well...
Authors
Eugene A. Shinn
Textural variation within Great Salt Lake algal mounds Textural variation within Great Salt Lake algal mounds
This chapter discusses textural variation within the Great Salt Lake algal mounds. Great Salt Lake algal mounds contain: (1) a framework of non-skeletal, algally induced aragonite precipitates; (2) internal sediment; and (3) inorganic cement. These three elements create a variety of laminated, poorly laminated, and unlaminated internal textures. Interior framework precipitates bear...
Authors
Robert B. Halley
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 1976 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 1976
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.
Authors
J.B. Townshend, J.E. Papp, M.J. Moorman, C.E. Deadmon, S.P. Tilton
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 1976 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 1976
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.
Authors
J.B. Townshend, J.E. Papp, M.J. Moorman, C.E. Deadmon, S.P. Tilton