Osceola Mudflow
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The Osceola Mudflow, also known as the Osceola Lahar, was a debris flow and lahar in the U.S. state of Washington that descended from the summit and northeast slope of Mount Rainier, a volcano in the
Mount Rainier with its main summit, Columbia Crest (14410 feet) at the center. Emmons Glacier covers most of the visible flank of the mountain with Disappointment Cleaver visible below Gibraltar Rock, right of the sharp pointed Little Tahoma (11138 feet). Liberty Cap (14112 feet) is visible on the right center skyline behind Russell Cliff.
Mount Rainier
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Mount Rainier, also known as Tahoma, is a large, active stratovolcano in the Cascade Range of the Pacific Northwest in the United States. The mountain is located in Mount Rainier National Park about 5
Osceola Mudflow
…also known as the Osceola Lahar, was a debris flow and lahar in the U.S. state of Washington that descended from the summit and northeast slope of Mount Rainier, a volcano in the Cascade Range during a period of eruptions about 5,600 years ago. It traveled down the west and main forks of the White River, passed…
Mount Rainier's northwestern slope viewed aerially just before sunset on September 6, 2020
Mount Rainier seen from the International Space Station
West face of Mount Rainier from an aircraft