Publications
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Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 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: March 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: March 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
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
Holocene geomagnetic secular variation in the western United States: implications for the global geomagnetic field Holocene geomagnetic secular variation in the western United States: implications for the global geomagnetic field
A record of Holocene geomagnetic secular variation in the western 14 United States has been measured from volcanic rocks dated by 14C. Analysis of errors associated with the paleomagnetic techniques used suggests that all laboratory measurement errors are smaller than those introduced by deformation of the volcanic units and the errors of orientation of cores in the field. The dispersion...
Authors
Duane E. Champion
Debris-flow deposits of Early Miocene age, Deadman Stream, Marlborough, New Zealand. Debris-flow deposits of Early Miocene age, Deadman Stream, Marlborough, New Zealand.
Detailed analysis is presented of a conformable succession of conglomerates and sandstones lying between massive marine mudstones. The coarse sediments reflect deposition by a spectrum of subaqueous debris-flow mechanisms during an early pulse of tectonism that ultimately resulted in Plio-Pleistocene eversion of the Kaikoura Mountains. Sparse pebbly mudstones and rare sandy conglomerates...
Authors
D.W. Lewis, M.G. Laird, R.D. Powell
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 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: October 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: October 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: July 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 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: May 1980 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: May 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
Estimating the costs of landslide damage in the United States Estimating the costs of landslide damage in the United States
Landslide damages are one of the most costly natural disasters in the United States. A recent estimate of the total annual cost of landslide damage is in excess of $1 billion {Schuster, 1978}. The damages can be significantly reduced, however, through the combined action of technical experts, government, and the public. Before they can be expected to take action, local governments need...
Authors
Robert W. Fleming, Fred A. Taylor
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
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