United States · Stratovolcano
Mount Rainier
Rainier
- Type
- Stratovolcano
- Elevation
- 4392m
- Last eruption
- 1450
- Type
- Stratovolcano
- Country
- United States
- Region
- North America / High Cascades Volcanic Arc
- Elevation
- 4392m
- Coordinates
- 46.853, -121.760
- Last eruption
- 1450
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic andesite
Geological summary
Mount Rainier is a heavily glaciated andesitic volcano in the Puget Sound region. Large Holocene mudflows from collapse have reached as far as the Puget Sound lowlands. The present summit was constructed within a large crater breached to the NE, formed by collapse during a major explosive eruption about 5,600 years ago that deposited the widespread Osceola Mudflow. Rainier has produced eruptions throughout the Holocene, including about a dozen during the past 2,600 years; the largest of these occurred about 2,200 years ago. The present summit cone is capped by two overlapping craters. Extensive hydrothermal alteration of the upper portion of the volcano has contributed to its structural weakness; an active thermal system has caused periodic melting on flank glaciers and produced an elaborate system of steam caves in the summit icecap. Reported uncertain 19th-century eruptions, including a possible but not confirmed phreatic eruption in 1894, have not left identifiable deposits.
From Wikipedia
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 59 miles (95 km) south-southeast of Seattle. At 14,406 ft (4,391 m) it is the highest mountain in the U.S. state of Washington, the most topographically prominent mountain in the contiguous United States, and the tallest in the Cascade Volcanic Arc.
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Eruption history
27 recordedGlossaryDetailed timeline
- 1894VEI 1Observed1894-11-21 – 1894-12-24
- 1882VEI 2Method not stated1882-07-02 – end unknown
- 1879VEI 2Method not stated1879-07-02 – end unknown
- 1870VEI 2Method not stated1870-07-02 – end unknown
- 1858VEI 2Method not stated1858-07-02 – end unknown
- 1854VEI 2Method not stated1854-07-02 – end unknown
- 1843VEI 2Method not stated1843-07-02 – end unknown
- 1450 (±100 yrs)VEI ?Geological estimate1450 – end unknown
- 910 (±500 yrs)VEI ?Geological estimate910 – end unknown
- 440 (±100 yrs)VEI ?Geological estimate440 – end unknown
- 150 BCEVEI ?Geological estimate150 BCE – end unknown
- 250 BCE (±200 yrs)VEI 4Geological estimate250 BCE – end unknown
- 400 BCE (±50 yrs)VEI ?Geological estimate400 BCE – end unknown
- 500 BCE (±50 yrs)VEI ?Geological estimate500 BCE – end unknown
- 610 BCE (±100 yrs)VEI ?Geological estimate610 BCE – end unknown
- 650 BCE (±50 yrs)VEI ?Geological estimate650 BCE – end unknown
- 700 BCE (±50 yrs)VEI ?Geological estimate700 BCE – end unknown
- 2550 BCEVEI 3Geological estimate2550 BCE – end unknown
- 2750 BCEVEI 2Geological estimate2750 BCE – end unknown
- 3650 BCEVEI 3Geological estimate3650 BCE – end unknown
- 3850 BCE (±200 yrs)VEI ?Geological estimate3850 BCE – end unknown
- 4850 BCEVEI 2Geological estimate4850 BCE – end unknown
- 5050 BCEVEI 3Geological estimate5050 BCE – end unknown
- 5350 BCEVEI 3Geological estimate5350 BCE – end unknown
- 5550 BCEVEI 2Geological estimate5550 BCE – end unknown
- 7800 BCE (±300 yrs)VEI ?Geological estimate7800 BCE – end unknown
- 8050 BCEVEI 3Geological estimate8050 BCE – end unknown
Nearby volcanoes
External links
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