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Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: May 1976 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: May 1976

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, M.J. Moorman, C.E. Deadmon, S.P. Tilton

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1976 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1976

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, M.J. Moorman, C.E. Deadmon, S.P. Tilton

Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: February 1976 Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: February 1976

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, M.J. Moorman, C.E. Deadmon, S.P. Tilton

Analysis of seismograms from a downhole array in sediments near San Francisco Bay Analysis of seismograms from a downhole array in sediments near San Francisco Bay

A four-level downhole array of three-component instruments was established on the southwest shore of San Francisco Bay to monitor the effect of the sediments on low-amplitude seismic ground motion. The deepest instrument is at a depth of 186 meters, two meters below the top of the Franciscan bedrock. Earthquake data from regional distances (29 km ≤ Δ ≤ 485 km) over a wide range of...
Authors
William B. Joyner, Richard E. Warrick, Adolph A. Oliver

Geomagnetic array control circuit Geomagnetic array control circuit

No abstract available.
Authors
Roger Lescelius, D. H. Rohret, R. A. Sneddon, J.N. Towle, D.V. Fitterman

Landslide problems at West Valley Nuclear Service Center, New York: An assessment and recommendations for study Landslide problems at West Valley Nuclear Service Center, New York: An assessment and recommendations for study

Problems due to landslides prompted a visit to the West Valley Nuclear Service Center (WVNSC) near Springville, New York, on March 15 and 16, 1976. From this visit a report was prepared and contains the following: An assessment of the landslide conditions. An assessment of the immediacy of the landslide problems. A suggested study program for reducing the landslide hazard to an...
Authors
Robert W. Fleming
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