McDermitt Caldera

McDermitt Caldera
McDermitt Caldera

Location of the caldera in Oregon and Nevada

Highest point
Coordinates 42°00′05″N 117°59′48″W / 42.00139°N 117.99667°W / 42.00139; -117.99667Coordinates: 42°00′05″N 117°59′48″W / 42.00139°N 117.99667°W / 42.00139; -117.99667
Geography
Location Harney County, Oregon
Malheur County, Oregon
Humboldt County, Nevada
Geology
Age of rock About 19 million years (Miocene)
Mountain type Caldera
Last eruption About 16 million years ago (Miocene)

The McDermitt Caldera is a large, oval-shaped caldera west of McDermitt in southeastern Oregon and northern Nevada in the United States. It is about 28 miles (45 km) wide north to south and 22 miles (35 km) wide east to west.[1] The western part of the caldera is in the Trout Creek Mountains, and the northern part is in the Oregon Canyon Mountains.[1][2]

The caldera was formed when a lava dome made of rhyolite collapsed about 16 million years ago. The lava dome had been built by volcanic eruptions starting about 19 million years ago.[1][2] Significant ore deposits are buried in the caldera, including mercury and uranium, which were mined at more than eight sites in the caldera during the 20th century. Mercury at these mines was extracted in large amounts, and it came mostly from cinnabar.[1][3] The McDermitt Mine, located on the eastern edge of the caldera in Nevada, was the last active mercury mine in the United States before it shut down in 1992.[4] Uranium was discovered in the caldera in 1953, and it was extracted mainly at the Moonlight mine on the caldera's southwestern edge.[1][5] Other deposits in the caldera contain ores of antimony, cesium, and lithium.[6]

Kleinite, a rare yellow mineral containing mercury (formula: (Hg2N)(Cl,SO4)·nH2O) from the McDermitt Mine[7]

References

  1. 1 2 3 4 5 Rytuba, James J. (1976). "Geology and Ore Deposits of the McDermitt Caldera, Nevada–Oregon" (PDF). United States Geological Survey. Retrieved 3 August 2015.
  2. 1 2 Ryuba, James J.; Conrad, Walter K. (1981). Goodell, P. C.; Waters, A. C., eds. "Petrochemical Characteristics of Volcanic Rocks Associated with Uranium Deposits In The McDermitt Caldera Complex". Studies in Geology. American Association of Petroleum Geologists: 63. Retrieved 3 August 2015.
  3. Orr, Elizabeth L.; Orr, William N. (1999). Geology of Oregon (5th ed.). Dubuque, Iowa: Kendall/Hunt Publishing Company. p. 93. ISBN 0-7872-6608-6. OCLC 42944922.
  4. "Mercury" (PDF). United States Geological Survey. January 2012. Retrieved 6 August 2015.
  5. Dahlkamp, Franz J. (2010). Uranium Deposits of the World: USA and Latin America. Volume 2. Berlin, Germany: Springer Science+Business Media. pp. 282, 290. ISBN 978-3-540-78559-0.
  6. Rytuba, James J.; McKee, Edwin H. (30 September 1984). "Peralkaline ash flow tuffs and calderas of the McDermitt Volcanic Field, southeast Oregon and north central Nevada". Journal of Geophysical Research. 89 (B10): 8616–8628. doi:10.1029/JB089iB10p08616. Retrieved 6 August 2015.
  7. Kleinite from McDermitt
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