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Stability of sulfur slopes on Io Stability of sulfur slopes on Io

The mechanical properties of elemental sulfur are such that the upper crust of Io cannot be primarily sulfur. For heat flows in the range 100–1000 ergs cm−2, sec−1, sulfur becomes ductile within several hundred meters of the surface and would prevent the formation of calderas with depths greater than this. However, the one caldera for which precise depth data are available is 2 km deep...
Authors
Gary D. Clow, M. H. Carr

Plastic deformation of MgO(A12O2)1·1 spinel at 0·28TM preliminary results Plastic deformation of MgO(A12O2)1·1 spinel at 0·28TM preliminary results

Prism-shaped single crystals of MgO(Al2O3)n spinel (n 1.1) have been compressed to significant plastic strain at a temperature of 400°C (∼0·28 TM) in controlled experiments under a superimposed hydrostatic pressure of 1·4 GPa. Compression of crystals approximately parallel to , and resulted in simple yield behaviour at axial stress differences of 1940, 3720, and 4300 MPa respectively...
Authors
Stephen H. Kirby, P. Veyssiere

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

Nuclear event time histories and computed site transfer functions for locations in the Los Angeles region Nuclear event time histories and computed site transfer functions for locations in the Los Angeles region

This report presents a collection of Nevada Test Site (NTS) nuclear explosion recordings obtained at sites in the greater Los Angeles, Calif., region. The report includes ground velocity time histories, as well as, derived site transfer functions. These data have been collected as part of a study to evaluate the validity of using low-level ground motions to predict the frequency...
Authors
A. M. Rogers, P. A. Covington, R.B. Park, R. D. Borcherdt, D. M. Perkins

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

U.S. strong-motion programs U.S. strong-motion programs

No abstract available.
Authors
Roger D. Borcherdt, R. B. Matthiesen

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 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
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