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Articles
Strain in Southern California: Measured Uniaxial North-South Regional Contraction
1 U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025
The plate tectonics model of the Pacific moving northwest relative to North America implies that the regional strain in California should be simple shear across a vertical plane striking N45°W or equivalently equal parts of north-south contraction and east-west extension. Measurements of the strain accumulation at seven separate sites in southern California in the interval 1972 through 1978 indicate a remarkably consistent uniaxial north-south contraction of about 0.3 part per million per year; the expected east-west extension is absent. It is not clear whether the period from 1972 through 1978 is anomalous or whether the secular strain in southern California is indeed a uniaxial north-south contraction. Revised on August 8, 1978
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Science. ISSN 0036-8075 (print), 1095-9203 (online)