Page Overview

WASHINGTON

28 February 01
Origin Time
18 h 54 min 31 sec
Location
47.17N 122.73W
Magnitude
7.0M
Depth
49.0 km

Tectonic setting of this earthquake

Most earthquakes in this region are subduction zone earthquakes. As the oceanic plate subducts beneath the continental plate, large compressive forces build up. Slip along the plate interface manifests as earthquakes.

The animation on the left shows typical fault motion for this region.
(movement is exaggerated)

More fault animations

More about plate movement and boundaries (To USGS)
More about locating earthquakes (To USGS)


Frequency of such earthquakes

The map on the left shows all earthquakes (yellow circles) that have occurred in the region from 1973 to the present with magnitude greater that 5.0. The red star shows the epicenter of this earthquake and the black lines represent plate boundaries (click map to enlarge - new window will open)

Plot showing magnitude-frequency relation of earthquakes
Plot your own map of historic events for a given region

More seismicity maps


Seismic Waves
Predicted P-Wave Travel Times (from the USGS)
City
Distance
(degrees)
Travel Time
(min:secs)
Arrival Time
UTC
Phase
Golden, Colorado 14.70 3:24.8 18:57:57.8 Pn
Anchorage, Alaska 21.03 4:39.3 18:59:12.3 P
Ottawa, Canada 32.15 6:22.5 19:00:55.5 P
Mexico City, Mexico 33.69 6:35.9 19:01:08.9 P
Honolulu, Hawaii 38.31 7:15.3 19:01:48.3 P
San Juan, Puerto Rico 54.06 9:19.0 19:03:52.0 P
Bergen, Norway 64.83 10:33.4 19:05:06.4 P
Tokyo, Japan 69.43 11:02.6 19:05:35.6 P
London, England 70.08 11:06.5 19:05:39.5 P
Lima, Peru 71.68 11:16.3 19:05:49.3 P
Moscow, Russia 76.17 11:42.5 19:06:15.5 P
Beijing, China 78.59 11:56.1 19:06:29.1 P
Agana, Guam 81.97 12:14.2 19:06:47.2 P
Rome, Italy 82.87 12:18.9 19:06:51.9 P
Kathmandu, Nepal 101.32 13:45.0 19:08:18.0 Pdiff
Wellington, New Zealand 104.05 13:57.1 19:08:30.1 Pdiff
Palmer Station, Antarctica 122.74 15:20.1 19:09:53.1 Pdiff

Nairobi, Kenya

130.97 15:56.6 19:10:29.6 Pdiff
Earthquakes generate seismic waves which travel through the earth. The map shows the time at which p-waves generated by this earthquake arrived at a few cities world wide. In general, seismic wave amplitudes at any location on earth are dependent on the magnitude of the earthquake and the distance from the earthquake. If the seismic waves are large near an urban center, extensive loss of human life and damage to human property may result. (click map to enlarge - new window will open)

More about seismic waves
More about seismic hazards and mitigation


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