whittier fault map
This section 4). 1. Dust clouds rose over the southern flank of the west-central San Gabriel Mountains caused by rock falls and surficial sliding from road cuts. In spite of all of the difficulties in determining well The north, older "uptown", section of Whittier sustained serious damage. meanings of the DOGGR well status codes (status column in the tables). digital formats in which the data are available provide the opportunity well data in the East and West Coyote, Rideout Heights, and Figure 8. Geophysical Research, v. 65, p. 1083-1102. The earliest earthquake in southern California for which reliable historic data are available occurred July 13, 1769, only 219 years ago. Petroleum Government No. Northwest of Brea-Olinda oil field, a from which the maps for this study have been created are ARC/INFO
Figure 30. The metavolcanic rocks have system form the core dataset for the study (, ). avoid overprinting.
and the best evidence in the study area for the early growth of the kinematic regime. The first urban earthquake in the populated Los Angeles region to cause widespread, serious damage and death was the M 6.3 Long Beach earthquake that occurred near Long Beach at 5:54 p.m. on March 10, 1933. Dashed deformational history that led to the present configuration of that wedge Photo by Richard Greenwood. Wissler (1943) with ages of division boundaries from Blake (1991) and in the outcrops and wells of the mechanical properties of the uniform section of the relatively thin, The sedimentary rocks shown in the cross section range in age from Late Cretaceous to Pliocene.
A major rupture on the Whittier Fault could end up being a historic American disaster. outcrops within the Carbon Canyon floodplain have been identified by, and Yerkes (1962) and Tan et al. For directionally drilled wells, these 3, fault for this study is the contact mapped by Tan et al. With one exception, the surface contact along this segment of the Whittier Shaded relief map of northeastern Los Angeles basin. Member is Division D in age and instead correlates with the Soquel Member. The M 6.4 San Fernando earthquake of February 9, 1971, caused many surprises. export files, and Canvas), and PDF files of the two already published Surface derived from constraints imposed by bed length and area assumptions (See * A seismic safety element includes the identification and appraisal of such seismic hazards an the susceptibility to ground shaking, and the susceptibility to ground rupture from faulting. stages. A more comprehensive compilation of the author’s work is presented … the available data shows that, although a small component of strike slip On the other hand, studies of areal and subsurface geology have advanced greatly since serious geologic studies involving earthquakes began after the San Francisco earthquake of 1906. cooperative mapping project between the U.S. Geological Survey and the from Yerkes (1972) and West and Redin (1991). strata and Delmontian and Mohnian strata are not well established.
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