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DESCRIPTION:
Mount Hood Seismic Network


Mount Hood Seismic Monitoring

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
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
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

Map, click to enlarge [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
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
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.

Click button for MORE Pacific Northwest Seismic Network (PNSN) Info Pacific Northwest Seismic Network (PNSN) Information


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12/26/06, Lyn Topinka