3 edition of Strong-motion data from the October 1, 1987 Whittier Narrows earthquake found in the catalog.
Strong-motion data from the October 1, 1987 Whittier Narrows earthquake
|Statement||by E. Etheredge and R. Porcella ; with contributions from R. Maley ... [et al.]|
|Series||Geological Survey open-file report -- 87-616, U.S. Geological Survey open-file report -- 87-616|
|Contributions||Porcella, R. L, Maley, R. P, Geological Survey (U.S.)|
|The Physical Object|
The Sierra Madre earthquake occurred on June 28 at local time with a moment magnitude of and a maximum Mercalli intensity of VII (Very strong).The thrust earthquake resulted in two deaths, around injuries, and damage estimated at $–40 million. The event occurred beneath the San Gabriel Mountains on the Clamshell–Sawpit Fault, which is a part of the Sierra Madre Local date: 28 June For example, the Landers Earthquake (M ) in the Mojave Desert was a big hazard but did not represent a big risk because of the low population of the affected area. On the other hand, the Whittier Narrows Earthquake (M ) was a much smaller hazard but a larger risk because it struck in the middle of Los Angeles.
The Loma Prieta earthquake of Octo , again proved the reliability of hinge and joint restrainers, but the tragic loss of life at the Cypress Street Viaduct on I in Oakland emphasized the necessity to immediately accelerate the column-retrofit phase of the seismic-retrofit program for bridges with a higher funding level for both. On October 1, , the Magnitude Whittier Narrows earthquake shook the Los Angeles area, causing significant shear damage to the I/I-5 Separation. Based on PEQIT’s investigation, Caltrans began developing contract plans to retrofit bridges with single-column bents (a substructure unit supporting each end of a bridge span).
The Rapid Raw Strong Motion (RRSM) is an entirely automated system that uses open data from EIDA. It provides earthquake information and strong motion parameters including PGA and PGV within minutes of any event. The Engineering Strong-Motion database (ESM) is a reviewed archive of accelerometric waveforms from events with magnitudes above The earthquake was centered at Whittier Narrows, Southern California, on October 1, , with M = (BKS), M = × 10 25 dyne-cm (BKS). The array, called the Strong Motion Array Taiwan-One (SMART 1), was installed in northeast Taiwan, which is currently much .
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Get this from a library. Strong-motion data from the October 1, Whittier Narrows earthquake. [E C Etheredge; R L Porcella; R P Maley; Geological Survey (U.S.)]. The magnitude (ML) Whittier Narrows earthquake of October 1,triggered strong-motion instrumentation at 52 stations operated in the Los Angeles area as part of the National Strong-Motion Instrumentation Network (NSMIN).
The purpose of this report is to provide information about the data recorded during the earthquake, including a Cited by: 7. 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. Get this from a library. Processed strong-motion records, Whittier Narrows, California earthquake, October 1, volume 1, USGS-NSMIN stations within 15 KM of the epicenter.
[A Gerald Brady; P N Mork; L C Seekins; Geological Survey (U.S.)]. 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.
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. UTC Whittier Narrows, California Earthquake Downloads in ".zip" format uncorrected ( M B ; uncompresses to MB). On November 4,at press time for this issue, CALTECH announced revised magnitudes for the October Whittier Narrows earthquakes: October 1, M ; October 4, M editor.
PHOTO 7 Photo 7. Detail of damaged, unreinforced brick building in uptown Whittier. Much destruction occurred to such buildings in the area. CONCLUSIONS. In particular, the Whittier Narrows (October ), Sierra Madre (June ), Northridge (January ) and Chino Hills (July ) earthquakes were considered in the studies reported here.
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: Influence of Focal Mechanism on Peak Accelerations of Strong Motions of the Whittier Narrows, California, Earthquake and an Aftershock JOHN E.
VIDALE University of California, Santa Cruz Focal mechanisms affect the pattern of the peak accelerations of the October 1, Whittier Narrows earthquake and its October 4 aftershock. Internet Data Reports. Archives: Internet Data Reports for Earthquakes of Include Lower Magnitude Earthquakes with Data.
Earthquake Name Date/Time (sorted in UTC) Event ID Latitude Longitude Magnitude Region Record Count; Bodie: 05/08/ PDT (UTC - 7). 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].
october pb earthquake engineering research center evaluation of seismic performance of aten-storyrc building during the whittier narrows earthquake by eduardo miranda vitelmo v. bertero reproduced by u.s. department of commerce national technical information service springfield, va l _ college of engineering.
Strong Motion Data Catalog Search Accelerograph Record descriptions from NCEI's Earthquake Strong Motion Database If you wish to retrieve the entire inventory database, go to the bottom of this page and click the Clear Form button and the Search Database button.
The October 1,Whittier Narrows earthquake (ML=) ws located at 34°'N, °'W, at a depth of +/ km in the northeastern Los Angeles basin. Acceleration response records obtained during the October 1, Whittier‐Narrows earthquake (M s = ) from the 32‐story, vertically irregular Wilshire Finance Building, of which the cross section changes from a nominally rectangular shape to a triangular one, are analyzed.
The building was instrumented with 21 channels of synchronized sensors, consisting of 12 uniaxial. 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.
Other Sources of Earthquake Strong Motion Data and Information. COSMOS, Consortium of Organizations for Strong-Motion Observation Systems; Four mirror sites of the European Strong Motion Database: United Kingdom, Greece, Italy, Iceland; National Strong Motion Program (NSMP), U.S.
Geological Survey; California Geological Survey. The moment tensor showed a mixture of thrust and left-lateral strike-slip faulting. This earthquake is similar to the Mw October 1, Whittier Narrows earthquake, located approximately 18 miles to the northwest. How-ever, the Whittier Narrows main shock was a pure east-west thrust faulting earthquake.
Strong motion. In earlythe San Fernando Valley was the scene of a dense network of strong-motion seismometers, which provided a total of seismograms. This made the earthquake the most documented event, at the time, in terms of strong-motion seismology; by comparison, the Alaska earthquake did not provide any strong motion affected: Greater Los Angeles Area.
Whittier Narrows earthquake. Sensors were sited on the main dam's crest and downstream face. The Whittier Narrows earthquake of October 1, provided an excellent record of the seismic response and performance of Puddingstone dam.
This local magnitude earthquake on the newly discovered Whittier FaultCited by: 1.Rupture model of the Loma Prieta earthquake from the inversion of strong-motion and broadband teleseismic data Possible explanation of damage pattern by the Whittier Narrows, California, earthquake of 1 October Rupture process of the M s Superstition Hills, California, earthquake determined from strong-motion Cited by: