Publications
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Influence of San Gabriel submarine canyon on narrow-shelf sediment dynamics, southern California Influence of San Gabriel submarine canyon on narrow-shelf sediment dynamics, southern California
Variations in the concentration of total suspended particulate matter (TSM) collected 1 m above bottom, changes in vertical profiles of light transmission, and substrate textural patterns reveal a corridor for preferential sediment transport on San Pedro continental shelf, California. During the winter, this corridor, designated the preferential transport corridor (PTC), is defined by...
Authors
Herman A. Karl
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, November 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, November 1980
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, E.A. Sauter, S.P. Tilton
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: October 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: October 1980
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
John B. Townshend, J.E. Papp, E.A. Sauter, S.P. Tilton
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska, December 1980
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, E.A. Sauter, S.P. Tilton
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1980
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
John B. Townshend, J.E. Papp, E.A. Sauter, S.P. Tilton
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: March 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: March 1980
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
John B. Townshend, J.E. Papp, E.A. Sauter, S.P. Tilton
Earthquake potential and ground motions for the Pillar Mountain landslide, Kodiak, Alaska Earthquake potential and ground motions for the Pillar Mountain landslide, Kodiak, Alaska
No abstract available.
Authors
George W. Moore, Robert A. Page, John C. Lahr
Holocene geomagnetic secular variation in the western United States: implications for the global geomagnetic field Holocene geomagnetic secular variation in the western United States: implications for the global geomagnetic field
A record of Holocene geomagnetic secular variation in the western 14 United States has been measured from volcanic rocks dated by 14C. Analysis of errors associated with the paleomagnetic techniques used suggests that all laboratory measurement errors are smaller than those introduced by deformation of the volcanic units and the errors of orientation of cores in the field. The dispersion...
Authors
Duane E. Champion
Tools to avoid landslide hazards and reduce damage Tools to avoid landslide hazards and reduce damage
No abstract available.
Authors
William J. Kockelman
Geodolite measurements of deformation near Hollister, California, 1971-1978 Geodolite measurements of deformation near Hollister, California, 1971-1978
A 24‐station trilateration network spanning the San Andreas and Calaveras faults near Hollister, California, has been surveyed each year between 1971 and 1978, inclusive. Two moderate (ML = 5) earthquakes have occurred within the network during the interval. No convincing preseismic or coseismic anomalies associated with those earthquakes have been identified. The deformation of the...
Authors
James C. Savage, W.H. Prescott, Michael Lisowski, N. King
Deformation across the Salton Trough, California, 1973-1977 Deformation across the Salton Trough, California, 1973-1977
A trilateration network extending across the San Andreas, San Jacinto, and Elsinore faults in the vicinity of the Salton Sea, California, has been surveyed to very high precision several times in the 5‐year interval 1973–1977. The average strain across the entire network is essentially a uniaxial north‐south contraction at the rate of about 0.3 μstrain/a. There is no substantial strain
Authors
James C. Savage, W.H. Prescott, Michael Lisowski, N. King
Strain accumulation rates in the western United States between 1970 and 1978 Strain accumulation rates in the western United States between 1970 and 1978
The rate of dilatation and the rate and direction of shear have been determined from trilateration data for 23 Geodolite networks in the western United States. Sixteen nets are located along the San Andreas fault system between Point Reyes, California, and the United States‐Mexico border. Other locations are across the Garlock fault in California; across Puget Sound near Seattle...
Authors
W.H. Prescott, James C. Savage, W. T. Kinoshita