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Triton Triton

No abstract available.
Authors
William B. McKinnon, Randolph L. Kirk

Pebble orientation on large, experimental debris-flow deposits Pebble orientation on large, experimental debris-flow deposits

Replicable, pronounced orientation of discoid pebbles (≥8 mm) embedded on surfaces of large (∼10 m3) experimental debris-flow deposits reveals that strongly aligned, imbricate fabric can develop rapidly over short distances in mass flows. Pebble long axes aligned subparallel to deposit margins as well as subparallel to margins of surge waves arrested within the deposits. Pebble alignment...
Authors
Jon J. Major

The coseismic slip distributions of the 1940 and 1979 Imperial Valley, California, earthquakes and their implications The coseismic slip distributions of the 1940 and 1979 Imperial Valley, California, earthquakes and their implications

Geodetic arrays observed by the U.S. Coast and Geodetic Survey span the Imperial fault in southern California. For the 1940 M 7.1 Imperial Valley earthquake, a 1934–1941 triangulation network has sufficient resolution to allow inversion for the coseismic slip distribution on fault segments 5 to 25 km long extending from the surface to a depth of 9 km. The estimated right-lateral slip is...
Authors
Nancy E. King, Wayne R. Thatcher

The Loma Prieta, California, Earthquake of October 17, 1989: Forecasts The Loma Prieta, California, Earthquake of October 17, 1989: Forecasts

The magnitude (Mw) 6.9 Loma Prieta earthquake struck the San Francisco Bay region of central California at 5:04 p.m. P.d.t. on October 17, 1989, killing 62 people and generating billions of dollars in property damage. Scientists were not surprised by the occurrence of a destructive earthquake in this region and had, in fact, been attempting to forecast the location of the next large...
Authors
Ruth A. Harris

Chapter C. The Loma Prieta, California, Earthquake of October 17, 1989 - Building Structures Chapter C. The Loma Prieta, California, Earthquake of October 17, 1989 - Building Structures

Several approaches are used to assess the performance of the built environment following an earthquake -- preliminary damage surveys conducted by professionals, detailed studies of individual structures, and statistical analyses of groups of structures. Reports of damage that are issued by many organizations immediately following an earthquake play a key role in directing subsequent...
Authors
Mehmet Çelebi

The Loma Prieta, California, earthquake of October 17, 1989: Landslides The Loma Prieta, California, earthquake of October 17, 1989: Landslides

Central California, in the vicinity of San Francisco and Monterey Bays, has a history of fatal and damaging landslides, triggered by heavy rainfall, coastal and stream erosion, construction activity, and earthquakes. The great 1906 San Francisco earthquake (MS=8.2-8.3) generated more than 10,000 landslides throughout an area of 32,000 km2; these landslides killed at least 11 people and...
Authors
David K. Keefer, Michael W. Manson, Gary B. Griggs, Nathaniel Plant, Robert L. Schuster, Gerald F. Wieczorek, David G. Hope, Edwin Harp, J. M. Nolan, Gerald E. Weber, William F. Cole, Dale R. Marcum, Patrick O. Shires, Bruce R. Clark
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