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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

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

Geodolite measurements of deformation near Hollister, California, 1971-1978 Geodolite measurements of deformation near Hollister, California, 1971-1978

A 24‐station trilateration network spanning the San Andreas and Calaveras faults near Hollister, California, has been surveyed each year between 1971 and 1978, inclusive. Two moderate (ML = 5) earthquakes have occurred within the network during the interval. No convincing preseismic or coseismic anomalies associated with those earthquakes have been identified. The deformation of the...
Authors
James C. Savage, W.H. Prescott, Michael Lisowski, N. King

Deformation across the Salton Trough, California, 1973-1977 Deformation across the Salton Trough, California, 1973-1977

A trilateration network extending across the San Andreas, San Jacinto, and Elsinore faults in the vicinity of the Salton Sea, California, has been surveyed to very high precision several times in the 5‐year interval 1973–1977. The average strain across the entire network is essentially a uniaxial north‐south contraction at the rate of about 0.3 μstrain/a. There is no substantial strain
Authors
James C. Savage, W.H. Prescott, Michael Lisowski, N. King

Strain accumulation rates in the western United States between 1970 and 1978 Strain accumulation rates in the western United States between 1970 and 1978

The rate of dilatation and the rate and direction of shear have been determined from trilateration data for 23 Geodolite networks in the western United States. Sixteen nets are located along the San Andreas fault system between Point Reyes, California, and the United States‐Mexico border. Other locations are across the Garlock fault in California; across Puget Sound near Seattle...
Authors
W.H. Prescott, James C. Savage, W. T. Kinoshita

Geodimeter measurements of strain during the Southern California Uplift Geodimeter measurements of strain during the Southern California Uplift

A review of geodimeter measurements made along the ‘big‐bend’ section of the San Andreas fault in southern California indicates no significant increment in strain during the period of major uplift (late 1959 to mid‐1963). Specifically, no evidence of an increment in compressional strain normal to the San Andreas fault at the time of the uplift was found. Geodolite measurements at four...
Authors
James C. Savage, W.H. Prescott

Fresh-water cementation of a 1,000-year-old oolite Fresh-water cementation of a 1,000-year-old oolite

Calcite cementation of aragonite ooid sand is producing oolite on Joulters Cays, Bahamas. During the last 1,000 years, calcite cement has formed at an average rate of between 27 and 55 cm3 /m3 /yr and is derived from dissolution of ooid aragonite in fresh water. The dissolution-reprecipitation of carbonate minerals in the aquifer results in ground waters of unusually high Sr content. Sea...
Authors
R. B. Halley, P. M. Harris
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