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Davet
Sunday 30th of June 2024, 07:24:50 PM
The Osceola flow began either as an avalanche or series of avalanches near the summit of Mount Rainier but had transformed to a lahar within 2 km (1.2 mi) of where it was initiated as it incorporated significant amounts of water from within the volcano's hydrothermal system.[1] The sector collapse formed a 1.8 km (1.1 mi) wide horseshoe-shaped crater, open to the northeast, almost the same size as the crater produced by the 1980 eruption of Mount St. Helens. Most of the Osceola crater has been filled in by subsequent lava eruptions, most recently about 2,200 years ago.[2]