Mount St. Helens Eruption May 18, 1980 (2010) US Geological Survey (USGS)
more at
http://scitech.quickfound.net
"
USGS scientists recount their experiences before, during and after the
May 18,
1980 eruption of
Mount St. Helens.
Loss of their colleague
David A. Johnston and 56 others in the eruption cast a pall over one of the most dramatic geologic moments in
American history."
Public domain film from the
United States Geological Survery (USGS).
http://en.wikipedia.org/wiki/Mount_St._Helens
Mount St. Helens is an active stratovolcano located in
Skamania County, Washington, in the
Pacific Northwest region of the United States. It is 96 miles (
154 km) south of
Seattle, Washington, and 50 miles (80 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 a.m.
PDT, 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 miles (24 km) of railways, and 185 miles (298 km) of highway were destroyed. A massive debris avalanche triggered by an earthquake measuring
5.1 on the
Richter scale caused an eruption that reduced the elevation of the mountain's summit from 9,677 ft (2,950 m) to 8,
365 ft (2,550 m), replacing it with a 1 mile (1.6 km) wide horseshoe-shaped crater. The debris avalanche was up to 0.7 cubic miles (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
...
On March 20, 1980, Mount St. Helens experienced a magnitude 4.2 earthquake;[2] and, on March 27, steam venting started. By the end of April, the north side of the mountain had started to bulge. On May 18, with little warning, a second earthquake, of magnitude 5.1, triggered a massive collapse of the north face of the mountain. It was the largest known debris avalanche in recorded history. The magma in St. Helens burst forth into a large-scale pyroclastic flow that flattened vegetation and buildings over 230 square miles (600 km2). More than 1.5 million metric tons of sulfur dioxide were released into the atmosphere. On the
Volcanic Explosivity Index scale, the eruption was rated a five (a
Plinian eruption).
The collapse of the northern flank of St. Helens mixed with ice, snow, and water to create lahars (volcanic mudflows). The lahars flowed many miles down the
Toutle and
Cowlitz Rivers, destroying bridges and lumber camps. A total of 3,900,
000 cubic yards (3,000,000 m3) of material was transported 17 miles (27 km) south into the
Columbia River by the mudflows.
For more than nine hours, a vigorous plume of ash erupted, eventually reaching 12 to 16 miles (20 to 27 km) above sea level. The plume moved eastward at an average speed of 60 miles per hour (
100 km/h) with ash reaching
Idaho by noon.
Ashes from the eruption were found collecting on top of cars and roofs next morning, as far as the city of
Edmonton in
Alberta, Canada.
By about 5:30 p.m. on May 18, the vertical ash column declined in stature, and less severe outbursts continued through the night and for the next several days. The St. Helens May 18 eruption released 24 megatons of thermal energy; it ejected more than 0.67 cubic miles (2.79 km3) of material. The removal of the north side of the mountain reduced St. Helens' height by about 1,
300 feet (
400 m) and left a crater 1 mile (1.6 km) to 2 miles (3.2 km) wide and 0.5 miles (
800 m) deep, with its north end open in a huge breach. The eruption killed 57 people, nearly 7,000 big game animals (deer, elk, and bear), and an estimated 12 million fish from a hatchery. It destroyed or extensively damaged over
200 homes, 185 miles (298 km) of highway and 15 miles (24 km) of railways.
Between 1980 and
1986, activity continued at Mount St. Helens, with a new lava dome forming in the crater. Numerous small explosions and dome-building eruptions occurred. From
December 7,
1989, to January 6,
1990, and from
November 5, 1990, to
February 14,
1991, the mountain erupted with sometimes huge clouds of ash...