No fault in Parkfield prediction.No fault in Parkfield prediction Parkfield, the tiny California town that straddles the San Andreas fault San Andreas fault, great fracture (see fault) of the earth's crust in California. It is the principal fault of an intricate network of faults extending more than 600 mi (965 km) from NW California to the Gulf of California. , is where seismologists are waiting for an earthquake to happen (SN:4/13/85,p,228). Because magnitude 6 earthquakes have rattled the Parkfield fault segment about every 22 years since 1857, and since the last quake was in June 1966, scientists predict that the next quake will occur in 1988, with a five-year margin for error. Some recent studies, however, have cast doubt on this forecast. At the meeting of the American Geological Union last December, two papers suggested that possible errors in the sites of quakes prior to 1922 mean that the Parkfield "clock" is not as regular as some think. But now, in a paper in the Sept. 26 SCIENCE, two researchers at the U.S. Geological Survey The term geological survey can be used to describe both the conduct of a survey for geological purposes and an institution holding geological information. A geological survey in Menlo Park Menlo Park. 1 Residential city (1990 pop. 28,040), San Mateo co., W Calif.; inc. 1874. Electronic equipment and aerospace products are manufactured in the city. Menlo College and a Stanford Univ. research institute are there. 2 Uninc. , Calif., offer another line of evidence in support of the 1988 prediction. Paul Segall and Ruth Harris studied geodetic lines spanning the San Andreas San Andreas is an Anglicisation of the Spanish language San Andrés (Saint Andrew, the Apostle). It may refer to:
pe·ri·o·dic·i·ty n. 1. of earthquakes. "Our results suggest that the strain released in the 1966 earthquake will most likely recover between 1984 and 1989," they write, "although it is possible that this will not occur until 1995." When it is recovered, "sufficient elastic strain elastic strain A form of strain in which the distorted body returns to its original shape and size when the deforming force is removed. See more at strain. will be stored for a [magnitude 6] earthquake to rupture the Parkfield fault segment." |
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