3 edition of Strong-motion data from the Whittier Narrows aftershock of October 4, 1987 found in the catalog.
Strong-motion data from the Whittier Narrows aftershock of October 4, 1987
by U.S. Dept. of the Interior, U.S. Geological Survey, Books and Open-File Reports Section, distributor] in [Denver, Colo.?
Written in English
|Other titles||Strong motion data from the Whittier Narrows aftershock of October 4, 1987|
|Statement||by E. Etheredge and R. Porcella; with contributions from R. Maley ... [et al.]|
|Series||Geological Survey open-file report -- 88-38, U.S. Geological Survey open-file report -- 88-38|
|Contributions||Porcella, R. L, Geological Survey (U.S.)|
|The Physical Object|
Cambridge Core - Solid Earth Geophysics - Active Faults of the World - by Robert YeatsCited by: Zone 4 indicates the highest level of seismicity (see Figure ). Each zone was allocated a factor, or coefficient, from to ; this value was a multiplier representing the acceleration value for which the building was to be designed. These values indicate a fourfold range in acceleration values between Zones 1 and 4.
Abstract. An overview of the most important developments in Engineering (or Strong Motion) Seismology is presented alongside Professor Keiiti Aki’s contributions, who is one of the founders of this field. The mechanics of earthquake rupture are discussed with due emphasis on the various physical phenomena. The presentation is made in a tutorial manner, borrowing freely from Keiiti Aki’s Cited by: The Whittier Narrows earthquake occurred in the southern San Gabriel Valley and surrounding communities of southern California at a.m. PDT on October 1. The moderate magnitude blind thrust earthquake was centered several miles north of Whittier in the town of Rosemead, had a relatively shallow depth, and was felt throughout.
Strong motion data from the Hollister earthquake of Febru Open-File Report By: M.J. Salsman and R.D. Forshee. Taly, N. , The Whittier Narrows, California Earthquake of October 1, - Performance of Buildings at California State University, Los Angeles, Earthquake Spectra: May , Vol. 4, No. 2, pp. Revisiting Earthquake Lessons - Nonstructural Components.
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STRONG-MOTION DATA FROM THE WHITTIER NARROWS AFTERSHOCK OF OCTOBER 4, The ML= Whittier Narrows earthquake of October 1, triggered accelerographs at 52 stations in the Los Angeles region that are operated as a part of the National Strong-Motion Instrumentation Network (NSMIN).
Strong-Cited by: 1. The Whittier Narrows earthquake occurred in the southern San Gabriel Valley and surrounding communities of southern California at a.m. PDT on October 1. The moderate magnitude blind thrust earthquake was centered several miles north of Whittier in the town of Rosemead, had a relatively shallow depth, and was felt throughout southern California and southern time: a.m.
PDT. Get this from a library. Strong-motion data from the Whittier Narrows aftershock of October 4, [E C Etheredge; R L Porcella; Geological Survey (U.S.)]. STRONG-MOTION DATA FROM THE WHITTIER NARROWS AFTERSHOCK OF FEBRU The ML= Whittier Narrows earthquake of October 1, triggered accelerographs at 52 stations in the Los Angeles region that are operated by the U.S.
Geological Survey as a part of the National Strong-Motion Instrumentation Network (NSMIN).File Size: KB. The ML aftershock that occurred on October 4,was located 2 km northwest of the main shock at a depth of km, with a strike-slip mechanism on a vertical plane [Haukkson and Jones, this issue].
Shakal et al.  collected the data from 22 strong motion. CSMIP STRONG-MOTION RECORDS FROM THE WHITTIER, CALIFORNIA EARTHQUAKE OF 1 OCTOBER [A.F., et al. Shakal] on *FREE* shipping on qualifying : Shakal, A.F., et al.
Focal mechanisms affect the pattern of the peak accelerations of the October 1,Whittier Narrows earthquake and its October 4 aftershock. The peak accelerations observed on 21 Strong Motion Ins Cited by: The source parameters of the Whittier Narrows mainshock have been studied using local seismic network data [Hauksson and Jones, this issue], local strong motion data [Wald et al., ], regional broadband data from northern California [Bolt et al., this issue], and regional as well as teleseismic data [Bent and ttelmberger, this issue].
Data Organization and Format. The OctoUTC, MwWhittier Narrows, California Earthquake data recorded by the USGS National Strong-Motion Network (NSMN) are available via the NSMP ftp server in the folder (directory) "_". Particularly hard hit was the western part of the city of Whittier (Photos 1 and 2).
Seismologists reported an unusually small number of aftershocks through Saturday, October 3. Then on Sunday, October 4 at a.m., an aftershock of magnitude (M) occurred. CSMIP STRONG-MOTION RECORDS FROM THE WHITTIER, CALIFORNIA EARTHQUAKE OF 1 OCTOBER (Report OSMS ) (Ring-bound) [A.F., et al.
Shakal] on *FREE* shipping on qualifying offers. Technical data report by Division of Mines and Geology. Seismograms, maps, graphs and ground response data. B&W illustrations and photos. The largest aftershock, a M quake, occurred on October 4, @ am and was located about 3km northwest of the epicenter of the October 1st earthquake.
It killed one person, injured several, and caused additional property damage in Alhambra, Los Angeles, Pico Rivera, and Whittier.
The October 1,Whittier Narrows earthquake (ML=) ws located at 34°'N, °'W, at a depth of +/ km in the northeastern Los Angeles basin. Andrew Michael. Research Geophysicist Earthquake Science Center. Email:Spatial variations in stress within the Whittier Narrows, California, aftershock sequence: new techniques and results, J.
Geophys. Res., 96, Displaced rocks, strong motion and the mechanics of shallow faulting associated with the Hector Mine. Buildings damaged by the Whittier Narrows, California, earthquake of 1 October were concentrated in several areas, most of which were located 8 to 10 km from the epicenter (corresponding to the critical incidence for SV waves) and were near topographic irregularities, such as the northern part of Whittier, just south of Puente Hills.
The purpose of this study is to show the possibility Cited by: The 24 November Superstition Hills earthquakes occurred on the conjugate northwest-striking right-lateral Superstition Hills fault and a previously unknown northeast-striking left-lateral structure defined by a lineation of hypocenters extending from the Superstition Hills fault to the Brawley seismic by: The Coalinga earthquake struck at p.m.
Monday, May 2 of that year, in Coalinga, California. The shock was felt from the greater Los Angeles Area north to Susanville in Lassen County, and between the Pacific Coast and western than 5, aftershocks were recorded through J of which had a magnitude of or larger.
It measured on the moment magnitude scale Areas affected: Central California, United States. Strong ground motion estimation is a relatively new science. (GMPE) using strong motion data, estimate a of 75 MPa for the Whittier Narrows M thrust. FIGURE Southwest-looking perspective of the Puente Hills blind thrust fault (contoured in kilometers), which ruptured to produce the M 6 Whittier Narrows earthquake of (white dot).
Relocated aftershocks (red dots) delineated a north-dipping plane, and seismic reflection surveys (colored contours) showed that this fault extends toward.
Strong motion is ground motion of sufficient amplitude and duration to be potentially damaging to a building or other structure. This turn-of-the-century wooden residence in Los Gatos sustained major damage when it moved off its foundation during the Octo.
Strong-motion data from the July 8, North Palm Springs earthquake and aftershocks Open-File Report By: R.L. Porcella, E.C. Etheredge, R.P. Maley, and J.C. Switzer.Between (Whittier-Narrows earthquake) and (Hector Mine earthquake), this network contributed invaluable strong motion data (about three component records), which will be studied by earthquake engineering researchers for many years to come.
Download: Download full-size image; Fig. Los Angeles and Vicinity Strong Motion Cited by: Valuable measurements of many significant earthquakes in the United States and abroad have been made by the California stations, including seismograms from major regional earthquakes such as those in (San Francisco), (Lompoc), (San Francisco), (Parkfield), (San Fernando), and (Whittier Narrows).