Tumalo Volcanic Center | |
Elevation Ft: | 1955 |
Range: | Cascade Range |
Coordinates: | 44.099°N -121.541°W |
Age: | More than 500,000 years[1] |
Volcanic Arc: | Cascade Volcanic Arc |
Last Eruption: | Pleistocene |
The Tumalo volcanic center of Central Oregon is viewed as a source of large-volume Pleistocene ashflows, in the US state of Oregon.[2]
How big was the volcanic eruption? Imagine a cube of lava, one that's 1.5miles long by 1.5miles wide by 1.5miles high.
Ashflows include
The area has many rhyolitic domes, such as Melvin Butte, plus andesitic cinder cones, including those of the Triangle Hill and Triangle Peak area, whose composition is similar to the Tumalo Tuff (and Bend Pumice), and Shevlin Park Tuff.
This area has andesitic and mafic cinder cones, such as Lava Butte.[3] and rhyolite domes.[4] Viscous rhyolite domes extruded to the surface.[5]
The Tumalo Volcanic Center's ashy pumice was quarried for concrete. This concrete effectively built the city of Bend, Oregon
Pumice from the Tumalo Volcanic Center composes Oregon State University–Cascades's expansion, into a pumice mine.[6]