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Date/Time Thumbnail Dimensions User Comment; current: 01:53, 7 December 2007: 884 × 569 (104 KB): Murraybuckley {{Information |Description=svg map of the 1980 mount st helens ash fallout, info from usgs map |Source=self-made |Date=6 dec 2007 |Author= Murraybuckley |Permission= all rights released |other_versions= png version [[Image:1980_St._
By comparison, the eruption of Mount St. Helens on May 18, 1980, was 0.25 cubic miles (1.0 km 3) in volume. [7] By contrast, the most powerful human-made explosive device ever detonated, the Tsar Bomba , had a yield of 50 megatons, whereas the eruption at La Garita was about 5,000 times more energetic.
The ash cloud produced by the eruption, as seen from the village of Toledo, Washington, 35 mi (56 km) to the northwest of Mount St. Helens: The cloud was roughly 40 mi (64 km) wide and 15 mi (24 km; 79,000 ft) high. Ash cloud from Mt. St. Helens as captured by the GOES 3 weather satellite at 15:45 UTC.
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Mount St. Helens, once the fifth-tallest peak in Washington State, lost about 1,300 feet from its height of 9,677, according to the USGS. The highest part of the crater rim on the southwestern ...
The upper part of the North Fork Toutle River watershed was redirected to the crater of Mount St. Helens itself until 1982. The river's headstreams begin on a volcanic ash deposit roughly 3 miles (5 km) long and 200 feet (61 m) deep, which is the source of much of the excess sediment.
Jim Erickson covered the 1980 eruption of Mount St. Helens for The News Tribune and published a book chronicling the 40th anniversary in 2020, offered by The History Press. Show comments Advertisement
Mount St. Helens showed significant activity on March 8, 2005, when a 36,000-foot (11,000 m) plume of steam and ash emerged—visible from Seattle. [43] This relatively minor eruption was a release of pressure consistent with ongoing dome building.