The September 3, 2000 Yountville Earthquake
A magnitude (M) 5.2 earthquake occurred at 1:36 AM on September
3, 2000 in the mountains 10 miles northwest of the town of Napa,
near Yountville, CA. Although seismologists initially thought that
the earthquake occurred on the West Napa fault, accurate locations
now indicate that the earthquake occurred about 3 miles west of this
fault.
Earthquakes of this size can occur anywhere throughout the Bay
Area on deep faults that cannot be observed through geologic mapping
of the Earth's surface. For example, a M 5.7 earthquake occurred on
March 3, 1986 in the East Bay hills, about 10 miles northeast of San
Jose, near Mt Lewis. This earthquake generated nearly 2000
aftershocks over a period of a year and a half, yet geologists have
been unable to identify any fault at the surface that can be related
to these earthquakes at depth.
The Yountville quake occurred on a northwest oriented fault, and
rupture occurred through right-lateral strike-slip motion (Yountville
focal mechanism),typical of events in central California. As of
10AM 09/11/2000 PDT, there have been only 18 aftershocks within 5
miles (8 km) of the epicenter, ranging in magnitude from 1.2 to 2.6.
It is unlikely that any of these aftershocks have been felt.
|
Yellow dots indicate historical seismicity, from 1970 -
Aug. 31, 2000. Red dots indicdate seismicity from Sept. 1 -
Sept. 8, 2000, including the Sept. 3rd M 5.2
mainshock. |
Strong motion instruments recorded unusually high levels of
shaking in the city of Napa as a result of the September
3rd Magnitude-5.2 earthquake near Yountville, California.
Recordings of strong shaking by stations operated throughout the
region by the U.S. Geological Survey (USGS), the California
Department of Conservation's Division of Mines and Geology (CDMG),
and UC Berkeley demonstrate that peak shaking levels in the city of
Napa were amplified five to eight times relative to a station
located in the mountains less than a mile from the earthquake
epicenter (example
of accelerograms). Both the high levels and local amplification
help explain the surprising concentration of earthquake damage
throughout the city, according to scientists from the three
agencies.
The highest recorded level of shaking came from an instrument
located in a fire station north of the city of Napa, approximately
six miles from the epicenter. The shaking there was 50 percent of
the force of gravity. This means that buildings at the site were
subjected to a horizontal force that was 50 percent of the
building’s weight. A station located south of town, near Napa
College, recorded a peak shaking level nearly as high. Both
recordings are substantially higher than expected for a magnitude
5.2 earthquake and are consistent with the significant damage that
the city suffered.
While earthquake shaking levels depend on the distance from the
earthquake source, the high level of ground shaking in Napa also
appears to be the result of two other factors: first, the
amplification of shaking by young sediments along the Napa River (map
of Quaternary surface deposits), and second, the focusing of
strong motion to the southeast, the direction the earthquake rupture
propagated. A regional map of shaking levels (ShakeMap)
can be viewed on the web. The offset of the strongest shaking to the
southeast from the epicenter, and the amplification within the basin
of sediments underlying Napa and along the northern shore of San
Pablo Bay are also clear and can best be viewed in the web map of
instrumental intensity.
The M5.2 event is the largest earthquake in this area since 1969
when two earthquakes, magnitude 5.6 and 5.7, struck Santa Rosa about
80 minutes apart. These earthquakes are associated with the Rodgers
Creek fault system (historical
seismicity)
In fact, these 3 events are the only earthquakes with magnitude
greater than 5.0 to hit the region 50-60 mi north of San Francisco
Bay since 1906. However, in the past year there have been several
magnitude 4 or greater events in this same region
1) A magnitude 4.7 event near Bolinas on 8/17/99 (ShakeMap)
2) A magnitude 4.3 event south of Santa Rosa on 9/22/99 (ShakeMap)
3) A series of 3 earthquakes, magnitudes 4.0, 4.2, 4.0 near
Cloverdale between January 10-18, 2000 (ShakeMaps for M4.0,
M4.2,
M4.0)
It is not clear whether the increase in seismicity in this region
reflects the end of a long period of seismic quiescence. If so, then
this would indicate that the levels of stress are perhaps
sufficiently high that larger quakes could be expected soon for the
region. A similar seismicity pattern was observed in the 50-year
period preceding the 1906 earthquake (seismicity
time line). However, there is too little data available on which
to alter the formal probabilities for the seismic hazard in this
region (Earthquake
Probability Study for the San Francisco Region). Clearly, had
such an argument been put forth after the two earthquakes that
rocked Santa Rosa in 1969, the subsequent 30 years of earthquake
activity in this region would have proven the argument to be flawed.
This earthquake injured 25 people, including 2 people critically.
70 people sought shelter at Red Cross facilities. Damage estimates
are rising and range from $10 to $50M. On Wed, Sept 6, Governor
Davis declared a state of emergency in the Napa Valley. A request
has been made for federal funds. As of September 8, the City of Napa
building inspectors have issued 168 "yellow tags" and 16 "red
tags". |