Earth:McDermitt Caldera

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Short description: Extinct volcanic caldera in Nevada and Oregon
McDermitt Caldera
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Highest point
PeakJordan Meadow Mountain
Elevation6,816 ft (2,078 m) [1]
Coordinates [ ⚑ ] 41°51′01″N 118°02′12″W / 41.85028°N 118.03667°W / 41.85028; -118.03667[2]
Dimensions
Length28 mi (45 km) north–south [3]
Width22 mi (35 km) east–west [3]
Geography
LocationHarney County, Oregon
Malheur County, Oregon
Humboldt County, Nevada
Range coordinates [ ⚑ ] : 42°00′05″N 117°59′48″W / 42.00139°N 117.99667°W / 42.00139; -117.99667
Geology
Age of rock19 million years (Miocene)
Mountain typeCaldera
Last eruption16.39 ± 0.02 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) long north–south and 22 miles (35 km) wide east–west.[3] The western part of the caldera is in the Trout Creek Mountains, and the northern part is in the Oregon Canyon Mountains.[3][4] The highest point of the McDermitt Caldera is Jordan Meadow Mountain at 6,816 feet (2,078 m), which is part of the Montana Mountains of Humboldt County, Nevada.[1][5]

McDermitt Caldera is possibly the oldest of a sequence of calderas formed by the Yellowstone hotspot.[6] The caldera was preceded by a lava dome that had been built by volcanic eruptions of rhyolite starting about 19 million years ago.[3][4] This lava dome collapsed into a caldera in an eruption between 16.37 and 16.41 million years ago.[6] A lake subsequently formed in the caldera, and it deposited varved sediments, diatomite, opal, carbonaceous material, and mafic lavas.[7]

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.[3][8] 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.[9] Uranium was discovered in the caldera in 1953, and it was extracted mainly from a rhyolite brecciated fault zone at the Moonlight mine on the caldera's southwestern edge.[3][7][10] The uranium ore minerals include uraninite and coffinite. The age of the uranium formation is assumed to be the same as the caldera tuff, which is approximately 16.1 million years.[7] Other deposits in the caldera contain ores of antimony, cesium, and lithium.[11][12] The Thacker Pass lithium deposit, located within the caldera, is a prospect that in 2017 was said to be the most significant lithium-clay resource in the U.S.[13]

See also

References

  1. 1.0 1.1 Rytuba, James J.; Glanzman, Richard K. (1978). "Relation of Mercury, Uranium, and Lithium Deposits to the McDermitt Caldera Complex, Nevada-Oregon". United States Geological Survey. p. 8. https://pubs.usgs.gov/of/1978/0926/report.pdf. 
  2. "Jordan Meadow Mountain". United States Geological Survey. 12 December 1980. https://geonames.usgs.gov/apex/f?p=gnispq:3:::NO::P3_FID:847379. 
  3. 3.0 3.1 3.2 3.3 3.4 3.5 3.6 Rytuba, James J. (1976). "Geology and Ore Deposits of the McDermitt Caldera, Nevada–Oregon". United States Geological Survey. http://pubs.usgs.gov/of/1976/0535/report.pdf. 
  4. 4.0 4.1 Rytuba, 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 178: 63–72. http://archives.datapages.com/data/specpubs/mineral1/data/a178/a178/0001/0050/0063.htm. Retrieved 3 August 2015. 
  5. "Jordan Meadow Mountain - 6,816' Nevada". https://www.listsofjohn.com/peak/44852. 
  6. 6.0 6.1 Henry, Christopher D.; Castor, Stephen B.; Starkel, William A.; Ellis, Ben S.; Wolff, John A.; Laravie, Joseph A.; McIntosh, William C.; Heizler, Matthew T. (17 July 2017). "Geology and evolution of the McDermitt caldera, northern Nevada and southeastern Oregon, western USA" (in en). Geosphere 13 (4): 1066–1112. doi:10.1130/GES01454.1. ISSN 1553-040X. Bibcode2017Geosp..13.1066H. 
  7. 7.0 7.1 7.2 Nash, J. Thomas (2010). "Volcanogenic Uranium Deposits: Geology, Geochemical Processes, and Criteria for Resource Assessment". USGS Open-File Report 2010-1001. United States Geological Survey. pp. 17–22. https://pubs.usgs.gov/of/2010/1001/pdf/OF10-1001.pdf. 
  8. Orr, Elizabeth L.; Orr, William N. (1999). Geology of Oregon (5th ed.). Dubuque, Iowa: Kendall/Hunt Publishing Company. p. 93. ISBN 978-0-7872-6608-0. OCLC 42944922. 
  9. "Mercury". United States Geological Survey. January 2012. http://minerals.usgs.gov/minerals/pubs/commodity/mercury/mcs-2012-mercu.pdf. 
  10. Dahlkamp, Franz J. (2010). Uranium Deposits of the World: USA and Latin America. 2. Springer. pp. 282, 290. ISBN 978-3-540-78559-0. 
  11. 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. Bibcode1984JGR....89.8616R. 
  12. Borden, Buddy; Harris, Tom (November 2017). "Economic and Fiscal Impacts From New Lithium Mine and Lithium Processing Operations in Humboldt County, Nevada". University of Nevada, Reno. https://www.diversifynevada.com/wp-content/uploads/2020/02/Lithium_Impacts_Final_Report_November_2017.pdf. 
  13. Bradley, Dwight C.; Stillings, Lisa L.; Jaskula, Brian W.; Munk, LeeAnn; McCauley, Andrew D. (2017). Schulz, Klaus J.; DeYoung, Jr., John H.; Seal II, Robert R. et al.. eds. Critical Mineral Resources of the United States—Economic and Environmental Geology and Prospects for Future Supply (Report). Professional Paper. United States Geological Survey. doi:10.3133/pp1802K. ISSN 2330-7102. 
  14. "Kleinite". Mindat.org. Hudson Institute of Mineralogy. http://www.mindat.org/min-2225.html. 

External link