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Landslide risk assessment Landslide risk assessment

Landslide risk can be assessed by evaluating geological conditions associated with past events. A sample of 2,4 16 slides from urban areas in West Virginia, each with 12 associated geological factors, has been analyzed using SAS computer methods. In addition, selected data have been normalized to account for areal distribution of rock formations, soil series, and slope percents. Final...
Authors
P. Lessing, C.P. Messina, R.F. Fonner

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: November 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: November 1983

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, L.Y. Torrence, P.A. Franklin

Sea-floor-mounted rotating side-scan sonar for making time-lapse sonographs Sea-floor-mounted rotating side-scan sonar for making time-lapse sonographs

A rotating side-scan sonar system was designed to make time-lapse sonographs of a circular area of the sea floor. To construct the system, the transducers of a commercial side-scan system (frequency 105 kHz; pulse length 0.1 ms; horizontal beam width 1°; vertical beam width 20°; beam depressed 10° with respect to horizontal) were mounted 2 m above the sea floor on a vertical shaft that...
Authors
David M. Rubin, David S. McCulloch, Harry R. Hill

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: June 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: June 1983

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, L.Y. Torrence, T.K. Cunningham

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: January 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: January 1983

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, T.K. Cunningham, L.Y. Torrence

Sensitivity of selected geomagnetic properties to truncation level of spherical harmonic expansions Sensitivity of selected geomagnetic properties to truncation level of spherical harmonic expansions

A two day selection of MAGSAT data is fit by spherical harmonic series truncated at increasing levels NF in the range 2
Authors
E.R. Benton, Ronald H. Estes, R.A. Langel, L.A. Muth

Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling

Gravity models computed for a profile across the long-wavelength paired negative-positive Bouguer anomalies of the southern Appalachian Mountains show that the large negative anomaly can be explained by a crustal root zone, whereas the steep gradient and positive anomaly east of the root may be explained equally well by three different geometries: a suture zone, a mantle upwarp, or a...
Authors
Deborah R. Hutchinson, John A. Grow, Kim D. Klitgord

Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan) Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan)

A close spatial and temporal association between three aseismic uplift episodes and subsequent large (M ≈ 7) earthquakes on the Izu Peninsula, Japan, suggests a causal relation. Quaternary geology, as well as studies by other workers, indicates a volcanic origin for the observed uplift, and we use a simple inflation model constrained by leveling data to compute the expected increments in...
Authors
Wayne R. Thatcher, James C. Savage

Ice sculpture in the Martian outflow channels Ice sculpture in the Martian outflow channels

Many landforms in Martian outflow channels have characteristics that suggest sculpture by glaciers, ice streams, or ice sheets. Viking Orbiter and terrestrial satellite images were examined at similar resolution to compare features of the Martian outflow channels to features produced by the movement of ice on earth. Many resemblances were found. They include the anastomoses, sinuosities...
Authors
Baerbel K. Lucchitta

Reflection—refraction of general P- and type-I S-waves in elastic and anelastic solids Reflection—refraction of general P- and type-I S-waves in elastic and anelastic solids

The reflection and refraction of general (homogeneous or inhomogeneous) plane P and type-I S(SV) body waves incident on plane boundaries are considered for general linear viscoelastic solids. Reflection—refraction laws, physical characteristics of the waves, and the nature of critical angles are examined in detail at welded boundaries and a free surface. General visco-elasticity with no...
Authors
Roger D. Borcherdt
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