United States · Shield volcano
Belknap Crater
Belknap
- Type
- Shield volcano
- Elevation
- 2094m
- Last eruption
- 475

- Type
- Shield volcano
- Country
- United States
- Region
- North America / High Cascades Volcanic Arc
- Elevation
- 2094m
- Coordinates
- 44.285, -121.842
- Last eruption
- 475
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Shield
- Major rock type
- Andesite / Basaltic andesite
Geological summary
The Belknap Crater area near McKenzie Pass in Oregon, north of the Three Sisters volcanoes, was the source of one of the largest concentrations of youthful volcanism in the Cascade Range. The basaltic to basaltic andesite Belknap shield volcano, topped by the Belknap Crater pyroclastic cone and the Little Belknap shield volcano immediately to the east, have produced widespread late Holocene lava flows on all sides, much of which took place between about 3,000 and 1,500 years ago. Eruptions from the NE base of Belknap crater produced lava flows that traveled 15 km W into the McKenzie River valley.
From Wikipedia
Belknap Crater is a shield volcano in the Cascade Range in the U.S. state of Oregon. Located in Linn County, it is associated with lava fields and numerous subfeatures including the Little Belknap and South Belknap volcanic cones. It lies north of McKenzie Pass and forms part of the Mount Washington Wilderness. Belknap is not forested and most of its lava flows are not vegetated, though there is some wildlife in the area around the volcano, as well as a number of tree molds formed by its eruptive activity.
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Eruption history
4 recordedGlossaryDetailed timeline
- 475 (±215 yrs)VEI 2Geological estimate475 – end unknownBelknap Crater
- 685 BCE (±50 yrs)VEI 2Geological estimate685 BCE – end unknownSouth Belknap and Twin Craters
- 1071 BCE (±241 yrs)VEI 0Geological estimate1071 BCE – end unknownLittle Belknap
- 5050 BCEVEI ?Geological estimate5050 BCE – end unknown
Nearby volcanoes
External links
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