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Landslides and related ground failures from the May 2, 1983, Coalinga, California earthquake Landslides and related ground failures from the May 2, 1983, Coalinga, California earthquake
No abstract available
Authors
E. L. Harp, R. C. Wilson, D. K. Keefer
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 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
Chryse Basin channels: low-gradients and ponded flows. Chryse Basin channels: low-gradients and ponded flows.
Gradients on the floors of the Martian outflow channels that are derived from radar-elevation profiles across Lunae Planum and Chryse Basin have much lower values than those obtained from the U.S. Geological Survey's topographic map. Whereas the gradients of Maja and Ares Valles are similar to those of the catastrophic flood channels in the Scablands of Washington State, the gradients of...
Authors
Baerbel K. Lucchitta, H.M. Ferguson
Talc in the suspended matter of the northwestern Atlantic Talc in the suspended matter of the northwestern Atlantic
Knowledge of the distribution, concentration, and composition of suspended particulate matter in seawater is important to the understanding of sedimentation processes on the Continental Shelf. Because the surfaces of both organic and inorganic particles have high affinities for pollutants, such as certain trace metals, chlorinated hydrocarbons, and petroleum (Bothner et al., 1981a)...
Authors
Lawrence J. Poppe, John C. Hathaway, Carol M. Parmenter
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 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: October 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: October 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
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: May 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: May 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
Proceedings of Workshop XIV: earthquake hazards of the Puget Sound region, Washington Proceedings of Workshop XIV: earthquake hazards of the Puget Sound region, Washington
This conference, the fourteenth in a series sponsored by the Earthquake Hazards Reduction Program, was held October 13-15, 1980 at Lake Wilderness, Washington. The stated purpose of the conference was to assess progress and the state of knowledge of earthquake hazards in the Puget Sound region of Washington. The small size of the group and the pleasant informal setting of the Lake...
Authors
Robert S. Crosson, Muriel L. Jacobson
High paleointensities of the geomagnetic field from thermomagnetic studies on rift valley pillow basalts from the Mid- Atlantic Ridge High paleointensities of the geomagnetic field from thermomagnetic studies on rift valley pillow basalts from the Mid- Atlantic Ridge
Nineteen pillow basalts dredged within the rift valley of the Mid-Atlantic Ridge at36.8°N were studied by the Thellier stepwise heating method in order to determine the paleointensity of the geomagnetic field when they erupted on to the sea floor. Previously reported fission track ages are 2,000 to 6,000 years for the youngest rocks (mainly olivine basalts) and 10,000 to 100,000 years...
Authors
M. Prevot, E. A. Mankinen, S. Gromme, A. Lecaille
Crustal structure of the northern mississippi embayment and a comparison with other continental rift zones Crustal structure of the northern mississippi embayment and a comparison with other continental rift zones
Previous geological and geophysical investigations have suggested that the Mississippi Embayment is the site of a Late Precambrian continental rift that was reactivated in the Mesozoic. New information on the deep structure of the northern Mississippi Embayment, gained through an extensive seismic refraction survey, supports a rifting hypothesis. The data indicate that the crust of the...
Authors
Walter D. Mooney, M.C. Andrews, A. Ginzburg, D.A. Peters, R. M. Hamilton
Furrowed outcrops of Eocene chalk on the lower continental slop offshore New Jersey Furrowed outcrops of Eocene chalk on the lower continental slop offshore New Jersey
A sea bottom of middle Eocene calcareous claystone cut by downslope-trending furrows was observed during an Alvin dive to the mouth of Berkeley Canyon on the continental slope off New Jersey. The furrows are 10 to 50 m apart, 4 to 13 m deep, linear, and nearly parallel in water depths of 2,000 m. They have steep walls and flat floors 3 to 5 m wide, of fine-grained sediment. Mid-range...
Authors
James M. Robb, John R. Kirby, John C. Hampson, Patricia R. Gibson, Barbara Hecker
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 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