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- Notations:
- An earthquake registering
a preliminary magnitude of ML
5.0 (NCSN), Mw 4.7 (UC Berkeley) was detected 01:06:18 UTC,
August 18, (6:06 p.m. PDT) along the coast of Marin County of
Northern California. The focal depth was placed at a depth of
6.9 km and and the fault plane solution suggested predominately
reverse motion along a northwest trending fault plane, with a
slight strike-slip component. (See
fault plane solution)
-
- The quake was centered
about 17 miles north-northwest of San Francisco at Bolinas Bay
and the small coastal town of Bolinas. (Location
Maps) It was centered either along the northern segment
of the San Andreas Fault where it comes briefly back on shore
north of San Francisco or a nearby fault splay. The northern
segment of the San Andreas Fault is considered locked and has
not produce a M5+ earthquake north of the Golden
Gate since the powerful 1906 San Francisco ~M8
earthquake. In 1957, however, a M5.3
jolt occurred just west of Daly City but it occurred along the
peninsula segment of the San Andreas Fault and not the locked
northern segment. The Daly City quake caused over $1 million
in damage and injured 40 people.
-
- Preliminary reports
indicate the quake was strongly felt in the epicentral area and
as far away as Gilroy, Vacaville, Livermore, and Santa Rosa.
Items toppled from tables and shelves in homes, hanging objects
swung, and pictures shook on walls. Commercial items, like bottles
and other light objects, are said to have toppeled in one Safeway
store and there is a report of a few windows being cracked or
broken. Most people reported the shaking lasted about 5-10 seconds.
There have been no reports of injuries at this time.
-
- One of the most common
comments witin the hundreds of "Felt Earthquake Reports"
received by Seismo-Watch was the noise that accompanied the quake.
Most in the epicentral region heard a loud explosion-like sound,
manying thinking it was a bomb or an accident of some sort. Sounds
are common with moderate to large earthquakes, however, most
sounds are commonly described as freight trains passing by or
through the house, of course, depending on how close one is to
the epicenter.
-
- While the fault motion
is rather surprising, the 1957 Daly City earthquake also had
reverse-slip motion. For the most part, the San Andreas Fault
is a strike-slip type of fault.
-
- Curiously, there have
been only a few aftershocks at this time. The largest was a M2.6 at 11:44 p.m., August 17,
which was locally felt. As a precaution, the USGS have issued
an aftershock warning which states the following probabilities:
10% chance of a M5.0 or larger quake in the next
7 days; 5-10% chance of a quake larger than
the main quake; and there is a likelihood of between 3-12 M3+ aftershocks.
Update: 9:30
p.m. PDT, August 18, 1999.
- Other News Reports:
San
Francisco Chronical
KTVU
- TV News Channel 2
KRON
- TV NewsCenter4 - Video
(requires REAL Player)
Marin
Independant Journal
San Francisco
Examiner
CNN
Reuters
Did
you feel this tremor? Send
us a quick note on what you felt.
-
A
similar copy of this earthquake report was sent to subscribers
of the Seismo-Watch
Earthquake Fax Alert Bulletins within an hour of the event.
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