Tumalo Volcanic Center

The Tumalo volcanic center of Central Oregon is viewed as a source of large-volume Pleistocene ashflows, in the US state of Oregon.[2]

Tumalo Volcanic Center
Highest point
Elevation1,955 ft (596 m)
Coordinates44°05′56″N 121°32′28″W
Geography
Parent rangeCascade Range
Geology
Age of rockMore than 500,000 years[1]
Volcanic arcCascade Volcanic Arc
Last eruptionPleistocene

The eruption, ashflows included

How big was the volcanic eruption? Imagine a cube of lava, one that's 1.5 miles (2.4 km) long by 1.5 miles (2.4 km) wide by 1.5 miles (2.4 km) high.[1]

Ashflows include

  1. Desert Spring Tuff,
  2. Bend Pumice
  3. Tumalo Tuff, and
  4. Shevlin Park Tuff.

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.[2]

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]

Ways the Tumalo Volcanic Center's ashflows have been used

The Tumalo Volcanic Center's ashy pumice was quarried for concrete. This concrete effectively built the city of Bend, Oregon[1]

Pumice from the Tumalo Volcanic Center composes Oregon State University–Cascades's expansion, into a pumice mine.[6]

See also

References
  1. Ross, Erin. "Oregon Public Broadcasting". Oregon Public Broadcasting.
  2. "Smithsonian".
  3. Harris 2005, p. 33.
  4. Plummer & McGeary 1988, p. 54.
  5. Faculty of the School of Geography 2006.
  6. Klemetti, Erik (July 31, 2019). "The Hidden Volcanoes of Central Oregon".
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