Lava Flows
Lava Flows
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Volcanic Hazards at Mount Rainier
Because of its elevation (4,392 m), relief, hydrothermal alteration, icecap, glacier-fed radial valleys, and proximity to encroaching suburbs of the Seattle-Tacoma metropolis, Mount Rainier is the most threatening volcano in the Cascades. Its next eruption could produce volcanic ash, lava flows, and avalanches of intensely hot rock and volcanic gases, called pyroclastic flows.
Geology and History Summary for Mount Rainier
Volcanism occurs at Mount Rainier and other Cascades arc volcanoes because of the subduction of the Juan de Fuca Plate off the western coast of North America.
Lava Flows at Mount Rainier
he primary hazard to people from lavaflows is low, but a more serious hazard arises when such flows come into contact with snow and ice.
The Eruption History of Mount Rainier
Timeline of eruptions at Mount Rainier.
Holocene, or Post-Glacial, Eruptions of Mount Rainier
We know more about the recent volcanism at Mount Rainier because deposits postdate extensive glaciation and therefore are well preserved.
Future Eruptions at Mount Rainier
Mount Rainier is behaving about as it has over the last half-million years, so all evidence suggests that the volcano will continue to erupt, grow, and collapse.