Publications
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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
International geomagnetic reference field 1980; charts and grid values International geomagnetic reference field 1980; charts and grid values
No abstract available.
Authors
Eugene B. Fabiano, N.W. Peddie, D.R. Barraclough, A.K. Zunde
Summaries of technical reports, Volume XV Summaries of technical reports, Volume XV
The research results described in the following summaries were submitted by the investigators on November 15, 1982 and cover the 6-month period from April 1, 1982 through September 30, 1982. These reports include both work performed under contracts administered by the Geological Survey and work by members of the Geological Survey. The report summaries are grouped into the four major...
Authors
Muriel L. Jacobson, Thelma R. Rodriguez, Wanda H. Seiders
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 1983 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 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: 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
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: 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
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
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
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
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