USGS/Cascades Volcano Observatory, Vancouver, Washington
DESCRIPTION:
Mount Hood Seismic Network
Mount Hood Seismic Monitoring
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From:
Swanson, Cameron, Evarts, Pringle, and Vance,
1989, IGC Field Trip T106: Cenozoic Volcanism in the Cascade Range and
Columbia Plateau, Southern Washington and Northernmost Oregon:
American Geophysical Union Field Trip Guidebook T106
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Felt earthquakes on Mount Hood occur every 2 years on the average.
Seismic monitoring, in effect since 1977
(Weaver et.al., 1982), indicates a generalized
concentration of earthquakes just south of the summit area and 2-7 kilometers
below sea level.
From:
Scott, et.al., 1997,
Geologic History of Mount Hood Volcano, Oregon -- A Field-Trip Guidebook:
USGS Open-File Report 97-263
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Earthquakes
occur sporadically at Mount Hood, typically as short-lived swarms of
small events (less than or equal to magnitude 3.5) that locate chiefly on the
south flank and below the summit at depths of less than 11 kilometers
(information from USGS and University of Washington Geophysics
Program).
One to several swarms per year have been recorded since the
seismic system was upgraded in 1980.
Pacific Northwest Seismic Network
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[Map,30K,InlineGIF]
Oregon and Southern Washington -
University of Washington's Pacific Northwest Seismic Network (PNSN)
-- Modified from: University of Washington Geophysics Program, 1999,
includes seismic station location map and link to PNSN
From:
Scott, et.al., 1997,
Volcano Hazards in the Mount Hood Region, Oregon:
USGS Open-File Report 97-89
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A regional seismic network operated jointly by
the U.S. Geological Survey and the
Geophysics Program
at the University of Washington detects and locates
earthquakes around Mount Hood. As many as 50
earthquakes have been recorded in one year, but the
events are seldom strong enough to be felt by people
on the volcano. Most occur in swarms of several events
that are located below the summit area or the south
flank at depths of less than 10 kilometers (6 miles).
An increase in this level of earthquake activity would
be noticed quickly. At monitored volcanoes similar to
Mount Hood, a notable increase in seismicity has
occurred days to months before the onset of eruptions.
From:
Wright and Pierson, 1992; and
the University of Washington's Geophysics Program
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Information on Pacific Northwest earthquake activity and hazards
is provided by the
Pacific Northwest Seismic Network (PNSN)
which operates seismograph stations and locates earthquakes
in Washington and Oregon. The PNSN
is operated jointly by the University of Washington, the University of Oregon,
and Oregon State University, and is funded by the U.S. Geological Survey, the
Department of Energy, and the State of Washington. The PNSN
is based at the Geophysics Program of the University of Washington in Seattle,
and is a member of the Council of the National Seismic Systems (CNSS), a group
of regional network operators who cooperate to locate and catalog earthquakes
throughout the United States.
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Pacific Northwest Seismic Network (PNSN) Information
Return to:
[Mount Hood Volcano Menu] ...
[Mount Hood Earthquakes and Seismicity Menu] ...
[Earthquakes and Seismicity Menu] ...
URL for CVO HomePage is:
<http://vulcan.wr.usgs.gov/home.html>
URL for this page is:
<http://vulcan.wr.usgs.gov/Volcanoes/Hood/Seismicity/hood_seismic_network.html>
If you have questions or comments please contact:
<GS-CVO-WEB@usgs.gov>
12/26/06, Lyn Topinka