Publications
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In-situ measurements of seismic velocity at 27 locations in the Los Angeles, California region In-situ measurements of seismic velocity at 27 locations in the Los Angeles, California region
Studies conducted in the San Francisco Bay Region (Gibbs, Fumal and Borcherdt, 1980) have shown that average shear-wave velocity can be readily tied to quantitative estimates of ground motion such as ground amplification and earthquake intensity. Furthermore, when certain physical properties of the geologic materials such as texture, hardness and fracture spacing are observed during...
Authors
James F. Gibbs, Thomas E. Fumal, Edward F. Roth
Polarization of bay-type geomagnetic disturbances in the Rio Grande Rift, New Mexico Polarization of bay-type geomagnetic disturbances in the Rio Grande Rift, New Mexico
No abstract available.
Authors
James N. Towle
Test and calibration of the Seismic Research Observatory Test and calibration of the Seismic Research Observatory
The Seismic Research Observatory (SRO) network is generating an important new data base for seismological research. The SRO systems have extended both the range and resolution of seismic measurements beyond the limits of conventional seismographs and the data are recorded in digital format making it convenient to automate processing and analysis. The SRO network now comprises 12 stations...
Authors
Jon Peterson, Charles R. Hutt, L. Gary Holcomb
Exploratory trench across the Pleasant Valley Fault, Nevada Exploratory trench across the Pleasant Valley Fault, Nevada
An exploratory trench was excavated across the 1915 trace of the Pleasant Valley fault 60 km south of Winnemucca, Nevada, to get information on the history of recent displacements on a fault that had produced a major earthquake in historic time, and on the appearance of such a fault in a trench cut in gravels, sands and silts of an alluvial fan. The trench exposed 16 mappable sedimentary...
Authors
Manuel G. Bonilla, H. A. Villalobos, R. E. Wallace
Preliminary observations of noise spectra at the SRO and ASRO stations Preliminary observations of noise spectra at the SRO and ASRO stations
The seismic noise spectra presented in this report were derived from SRO and ASRO station data for the purpose of evaluating the performance of the seismic instruments. They are also useful for constructing a spectral estimate of earth noise at a quiet site based on noise samples obtained from a network of globally distributed sites. It is hoped that the spectra will be usefull for other...
Authors
Jon Peterson
Speculations on processes responsible for mesoscale current lineations on the continental shelf, southern California Speculations on processes responsible for mesoscale current lineations on the continental shelf, southern California
A side-scan sonar survey of San Pedro shelf, California, reveals areas of mesoscale current lineations oriented approximately north-northeast in water depths of 20-25 m. Widths of sand ribbons range from 40 to 120 m and intervening erosional furrows, from 15 to 50 m. A conceptual model shows that the scale and orientation of current lineations agree with the dimensions and axial...
Authors
Herman A. Karl
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: February 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: February 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
Evolution of the continental margin of southern Spain and the Alboran Sea Evolution of the continental margin of southern Spain and the Alboran Sea
Seismic reflection profiles and magnetic intensity measurements were collected across the southern continental margin of Spain and the Alboran basin between Spain and Africa. Correlation of the distinct seismic stratigraphy observed in the profiles to stratigraphic information obtained from cores at Deep Sea Drilling Project site 121 allows effective dating of tectonic events. The...
Authors
William P. Dillon, James M. Robb, H. Gary Greene, Juan Carlos Lucena
Landslides and related features, Virginia and West Virginia: Charlottesville 1° x 2° sheet Landslides and related features, Virginia and West Virginia: Charlottesville 1° x 2° sheet
No abstract available.
Authors
Robert J. Hackman, Roger E. Thomas
Seismic properties investigation of the Springer Ranch landslide, Powder River basin, Wyoming Seismic properties investigation of the Springer Ranch landslide, Powder River basin, Wyoming
A recent and rapid increase since the mid-1970's in commercial and residential development in the Powder River Basin, Wyoming and Montana, is caused by exploitation of vast coal and other resources in the basin. One geologic hazard to such development is landsliding. A landslide sufficiently representative of others in the area was chosen for detailed seismic studies. Studies of this...
Authors
C.H. Miller, A.L. Ramirez, T.G. Bullard
Surface faulting near Livermore, California, associated with the January 1980 earthquakes Surface faulting near Livermore, California, associated with the January 1980 earthquakes
The earthquakes of 24 January (Ms 5.8) 1980 north of Livermore, California, and 26 January (Ms 5.2), were accompanied by surface faulting in the Greenville fault zone and apparently in the Las Positas fault zone also. The surface faulting was discontinuous and of small displacement. The main rupture within the Greenville fault zone trended about N.38°W. It was at least 4.2 km long and...
Authors
Manuel G. Bonilla, James J. Lienkaemper, J. C. Tinsley