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Mount St. Helens

Mountain information
NameMount St. Helens
Elevation8365 ft (2549.7 m)
Prominence4605 ft (1403.6 m)
LocationSkamania County, Washington, USA
RangeCascade Range
RegionUS-WA
Sourcegnis
TypeActive stratovolcano
Age< 40,000 yrs
Last eruption2004 � July 10, 2008
First ascent1853 by Thomas J. Dryer
Easiest routeHike via south slope of volcano (closest area near eruption site)

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Mount St. Helens is an active stratovolcano located in Skamania County, Washington, in the Pacific Northwest region of the United States. It is 96 mi (154.5 km) south of Seattle, Washington and 50 mi (80.5 km) northeast of Portland, Oregon. Mount St. Helens takes its English name from the British diplomat Lord St Helens, a friend of explorer George Vancouver who made a survey of the area in the late 18th century. The volcano is located in the Cascade Range and is part of the Cascade Volcanic Arc, a segment of the Pacific Ring of Fire that includes over 160 active volcanoes. This volcano is well known for its ash explosions and pyroclastic flows.

Mount St. Helens is most notorious for its catastrophic eruption on May 18, 1980, at 8:32 am PDT which was the deadliest and most economically destructive volcanic event in the history of the United States. Fifty-seven people were killed; 250 homes, 47 bridges, 15 mi (24.1 km) of railways, and 185 mi (297.7 km) of highway were destroyed. A massive debris avalanche triggered by an earthquake measuring 5.1 on the Richter scale, caused an eruption, reducing the elevation of the mountain's summit from 9677 ft (2949.5 m) to 8365 ft (2549.7 m) and replacing it with a 1 mi (1.6 km) wide horseshoe-shaped crater. The earthquake was caused by a sudden surge of magma from the Earth's mantle. The debris avalanche was up to 0.7 cumi (2.9 km3) in volume. The Mount St. Helens National Volcanic Monument was created to preserve the volcano and allow for its aftermath to be scientifically studied.

As with most other volcanoes in the Cascade Range, Mount St. Helens is a large eruptive cone consisting of lava rock interlayered with ash, pumice, and other deposits. The mountain includes layers of basalt and andesite through which several domes of dacite lava have erupted. The largest of the dacite domes formed the previous summit, and off its northern flank sat the smaller Goat Rocks dome. Both were destroyed in the 1980 eruption.


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