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Where can I learn more about the 1989 Earthquake?
The 1989 Loma Prieta earthquake occured on October 18, 1989 at
00:04 UTC in the Santa Cruz Mountains of
Central California.
- Date: October 18, 1989 at 00:04 UTC (October 17, 1989 at 05:04 PM local time)
- Location: 37.040 -121.877
- Depth: 16.79 km
- Magnitude: 6.9 Mw, 7.1 Ms, 6.7 Ml
- Faulting:This earthquake was the first major event
to occur along the San Andreas fault zone since the
1906
earthquake. The Loma Prieta earthquake ruptured the southernmost 40
km of the 1906 break, in comparable amounts of right-lateral strike
slip and reverse slip motion. The average strike-slip displacement
was 1.2 meters while the average reverse-slip displacement was 1.6 meters.
This type of motion is not typical of the San Andreas fault and suggests
that the earthquake occurred on a sub-parallel fault and not on the
San Andreas itself. Consequently, the potential for a damaging
earthquake on the San Andreas in the Santa Cruz mountains may still exist.
- Deaths: 63
- Injuries: 3,757
- Property Damage: $ 5,900,000,000. At the time, this was
the most costly natural disaster in the United States.
Because of its proximity to the San Francisco Bay Area, the earthquake
was felt extensively over the area:
16 km ( 10 miles) ENE ( 61 degrees) of Santa Cruz, CA
22 km ( 13 miles) WSW ( 244 degrees) of Morgan Hill, CA
34 km ( 21 miles) S ( 177 degrees) of San Jose, CA
47 km ( 29 miles) N ( 5 degrees) of Monterey, CA
71 km ( 44 miles) S ( 188 degrees) of Livermore, CA
91 km ( 57 miles) SSE ( 158 degrees) of Oakland, CA
95 km ( 59 miles) SSE ( 150 degrees) of San Francisco, CA
100 km ( 62 miles) SSE ( 159 degrees) of Berkeley, CA
As we pass the 10th anniversary of this earthquake, it is appropriate
to look back and see what we have learned.
This earthquake has been extremely well-studied and numerous
resources are available. Here is a brief list.
Maps
Seismograms
At the time of the Loma Prieta earthquake, the Berkeley
Seismological Laboratory operated a small network of 16-bit digital seismometers. Because of the limited digital range
of the 16-bit systems, all of these instruments "clipped". In addition,
some of the seismometers displayed non-linear effects from the strong
shaking. The data were useful for providing P-wave travel times in
order to locate the earthquake, but it was not possible to use the
amplitude information until the
largest amplitude waves had passed. Here are two example seismograms
from these recordings.
The difficulties experienced in 1989 were motivation for the
upgrade of the Berkeley
Digital Seismic Network in 1991. Today the BDSN consists of 28
broadband stations with 24-bit digitizers. Each station consists of
a broadband seismometer and a strong-motion instrument in order to
ensure that the full range of ground motions are recorded on scale.
- Recording from BKS
- Recording from CMB
- McNutt, S., and Sydnor, R. (ed.),The Loma Prieta (Santa Cruz Mountains), California, Earthquake
of 17 October 1989, CDMG Special Publication 104, 1990.
- National Research Council,Practical Lessons from the Loma Prieta
Earthquake,
National Academy Press, 1994.
- Schultz, S., and R. Wallace, The San Andreas Fault, USGS General Interest Publication, 1989.
This "General Interest Publication" is a nice introduction to the
San Andreas for a general audience.
- Seismological Society of America (ed),The 1989 Loma Prieta, California, Earthquake
and its effects, Bulletin of the Seismological Society of America, Vol. 81, 1991.
- Spudich, P. (ed.), The Loma Prieta, California, Earthquake of
October 17, 1989 - Main shock characteristics, USGS Professional
Paper 1550, Denver, CO, 297 pp., paperback, 1996.
- Wallace, R.R. (ed.), The San Andreas Fault System, California, USGS Professional Paper 1515, Denver, CO, 283 pp., paperback, 1990.
A collection of review articles on the San Andreas Fault, covering the evolution, physiography, seismicity, and deformation along the fault. Excellent reference.
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