Mammoth Mountain

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For the ski area, see Mammoth Mountain Ski Area.
Mammoth Mountain
Mammoth Mountain.jpg
Mammoth Mountain from U.S. Route 395
Elevation 11,059 ft (3,371 m) NAVD 88[1]
Prominence 1,647 ft (502 m)[2]
Location
Location Inyo National Forest,
Madera / Mono counties, California, U.S.
Range Sierra Nevada
Coordinates 37°37′50″N 119°01′57″W / 37.630626492°N 119.032625631°W / 37.630626492; -119.032625631Coordinates: 37°37′50″N 119°01′57″W / 37.630626492°N 119.032625631°W / 37.630626492; -119.032625631[1]
Topo map USGS Mammoth Mountain
Geology
Type Lava dome complex[3]
Age of rock About 50,000 to 200,000 years
Last eruption 1260 ± 40 years[3]
Climbing
Easiest route Gondola[4]

Mammoth Mountain is a lava dome complex west of the town of Mammoth Lakes, California in the Inyo National Forest of Madera County and Mono County.[3] It is home to a large ski area on the Mono County side.

Mammoth Mountain was formed in a series of eruptions that ended 57,000 years ago. However, Mammoth still produces hazardous volcanic gases that kill trees and caused ski patroller fatalities in 2006.[5]

Geology[edit]

Mammoth Mountain is a lava dome complex in Mono County, California. It lies in the southwestern corner of the Long Valley Caldera[6] and consists of about 12 rhyodacite and dacite overlapping domes.[7] These domes formed in a long series of eruptions from 110,000 to 57,000 years ago, building a volcano that reaches 11,059 feet (3,371 m) in elevation.[8] During this time, massive dacite eruptions occurred roughly every 5000 years.[9] The volcano is still active with minor eruptions, the largest of which was a minor phreatic (steam) eruption 700 years ago.[3]

Mammoth Mountain also lies on the South end of the Mono-Inyo chain of volcanic craters.[10] The magma source for Mammoth Mountain is distinct from both the Long Valley Caldera and the Inyo Craters.[3][11][12]

Mammoth Mountain is composed primarily of dacite and rhyolite,[13] some of which have been altered by hydrothermal activity from fumaroles (steam vents).[14]

Volcanic gas discharge[edit]

Mammoth is outgassing large amounts of carbon dioxide out of its south flank, near Horseshoe Lake, causing mazuku in that area. The concentration of carbon dioxide in the ground ranges from 20 to 90 percent CO2. Measurements of the total discharge of carbon dioxide gas at the Horseshoe Lake tree kill area range from 50 to 150 short tons (45 to 140 t) per day. This high concentration causes trees to die in six regions that total about 170 acres (0.69 km2) in size (see photo, above).[15]

The tree kills originally were attributed to a severe drought that affected California in the late 1980s and early 1990s. Another idea was that the kills were the result of a pathogen or other biological infestation. However neither idea explained why all trees in the affected areas were killed regardless of age or health. Then in March 1990, a United States Forest Service ranger became ill with suffocation symptoms after being in a snow-covered cabin near Horseshoe Lake.[16]

Measurements around the lake found that restrooms and tents had a greater than 1% CO2 concentration (toxic), and a deadly 25% concentration of CO2 in a small cabin. CO2 concentrations of less than 1% are typical and healthy in most soils, however soil concentrations of CO2 in the tree kill areas ranged from 20% to 90%. This overabundance of CO2 was found to be the cause of the tree kills because tree roots need to absorb O2 directly and the high CO2 level reduced available O2. Researchers also determined that Mammoth releases about 1,300 short tons (1,200 t) of CO2 every day. As of 2003 the concentration of carbon dioxide in soil gas at Mammoth Mountain is being monitored on a continuous, year-round basis at four sites—three at Horseshoe Lake and one near the base of Chair 19 at the ski area.[15]

The most likely sources of the CO2 are degassing of intruded magma and gas release from limestone-rich metasedimentary rocks that are heated by magmatic intrusions. The remarkable uniformity in chemical and isotopic composition of the CO2 and accompanying gases at different locations around Mammoth Mountain indicates that there may actually be a large reservoir of gas deep below the mountain from which gas escapes along faults to the surface.[15] Measurements of helium emissions support the theory that the gases emitted in the tree kill area have the same source as those discharged from Mammoth Mountain Fumarole.[12][17] There is evidence that the rate of CO2 discharge has been declining,[18] with emissions peaking in 1991.[19]

In April 2006, three members of the Mammoth Mountain Ski Area ski patrol died while on duty. All three died from suffocation by carbon dioxide when they fell into a fumarole on the slopes of the mountain.[20]

Recreational use[edit]

Mammoth Mountain is home to the Mammoth Mountain Ski Area, the highest ski resort in California. Mammoth is notable for the unusually large amount of snowfall it receives compared to other Eastern Sierra peaks—about 400" annually—due to its location in a low gap in the Sierra crest.[21] In the summer months the ski gondolas are used by mountain bikers and tourists who wish to get a summit view of Long Valley Caldera directly to the east and Sierra peaks to the west, south and north.[4] To the south of the mountain, a number of lakes that serve as tourist attractions in the summer.

References[edit]

  1. ^ a b "706 702 2=Mammoth". NGS data sheet. U.S. National Geodetic Survey. Retrieved 2014-01-16. 
  2. ^ "Mammoth Mountain, California". Peakbagger.com. Retrieved 2009-08-03. 
  3. ^ a b c d e "Mammoth Mountain". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1203-15-. Retrieved 2008-12-18.
  4. ^ a b Jones, Finn-Olaf (2008-02-29). "Mammoth Mountain Ski Area". Ski Guide (The New York Times). Retrieved 2008-08-18. 
  5. ^ Hymon, Steve; Covarrubias, Amanda (2006-04-09). "How Routine Turned to Tragedy at Mammoth". Los Angeles Times. Retrieved 2011-05-09. 
  6. ^ Martini, B.A.; Silver, E.A., Potts, D.C. and Pickles, W.L. (July 2000). "Geological and geobotanical studies of Long Valley Caldera, CA, USA utilizing new 5m hyperspectral imagery". Geoscience and Remote Sensing Symposium, 2000. Proceedings. IGARSS 2000. IEEE 2000 International 4. Institute of Electrical and Electronics Engineers. pp. 1376–1378. doi:10.1109/IGARSS.2000.857212. Retrieved 2008-08-18. 
  7. ^ "Long Valley Caldera and Mono-Inyo Craters Volcanic Field, California". Volcano World. Archived from the original on 2008-01-14. 
  8. ^ Lewicki, Jennifer L.; Jens Birkholzer and Chin-Fu Tsang (February 2006). Natural and Industrial Analogues for Release of CO
    2
    from Storage Reservoirs: Identification of Features, Events, and Processes and Lessons Learned
    (PDF). United States Department of Energy/Office of Scientific and Technical Information. Retrieved 2008-08-18.
     
  9. ^ Harris, Stephen L. (2005). Fire Mountains of the West (3rd ed.). Missoula, Montana: Mountain Press Publishing Company. ISBN 0-87842-511-X. 
  10. ^ David P. Hill; Roy A. Bailey, Michael L. Sorey, James W. Hendley II, and Peter H. Stauffer (May 2000). Living With a Restless Caldera—Long Valley, California - U.S. Geological Survey Fact Sheet 108-96. Online Version 2.1. United States Geological Survey. Retrieved 2008-08-18. 
  11. ^ Hildreth, Wes (2004-09-14). "Volcanological perspectives on Long Valley, Mammoth Mountain, and Mono Craters: several contiguous but discrete systems". Journal of Volcanology and Geothermal Research (Elsevier B.V.) 136 (3–4): 169–198. Bibcode:2004JVGR..136..169H. doi:10.1016/j.jvolgeores.2004.05.019. Retrieved 2008-08-18. 
  12. ^ a b DePaolo, Don; Mike Sorey, Bill Evans, Chris Farrar, Andrea Cook, Laura Hainsworth and John Rogie. "Volcanic Hazards and CO2 Emissions: Mammoth Mountain Long Valley Caldera, California". Center for Isotope Geochemistry - Nobel Gas Isotope Geochemistry. Lawrence Berkeley National Laboratory. Retrieved 2008-08-19. 
  13. ^ "Geologic History of Long Valley Caldera and the Mono-Inyo Craters volcanic chain, California". United States Geological Survey. Retrieved 2008-08-18. 
  14. ^ Pease, Robert C. "Hydrothermal System of the Long Valley Caldera". Volcanoes of the Eastern Sierra Nevada: Geology and Natural Heritage of the Long Valley Caldera. Retrieved 2010-05-07. 
  15. ^ a b c "Carbon Dioxide and Helium Discharge from Mammoth Mountain". USGS Volcano Hazards Program Long Valley Observatory. United States Geological Survey. 2001-12-27. Archived from the original on 2010-05-28. Retrieved 2008-08-18. 
  16. ^ Farrar, C.D.; J. M. Neil; J. F. Howle (1999). "Magmatic Carbon Dioxide Emissions at Mammoth Mountain, California". Water-Resources Investigations report 98-4217. USGS. 
  17. ^ "Helium Discharge at Mammoth Mountain Fumarole (MMF)". United States Geological Survey. 2003-07-30. Archived from the original on 2010-06-02. Retrieved 2008-08-19. 
  18. ^ Farrar, C.D.; Bergfeld, D. (December 2007). "Magmatic Carbon Dioxide Emissions From Mammoth Mountain, California -- A Decreasing Trend From 1996 to 2007". American Geophysical Union, Fall Meeting 2007. American Geophysical Union. Retrieved 2008-08-18. 
  19. ^ Sorey, Michael L.; Christopher D. Farrar, Terrance M. Gerlach, Kenneth A. McGee, William C. Evans, Elizabeth M. Colvard, David P. Hill, Roy A. Bailey, John D. Rogie, James W. Hendley II, and Peter H. Stauffer (2007-07-09). Invisible CO
    2
    Gas Killing Trees at Mammoth Mountain, California - U.S. Geological Survey Fact Sheet 172-96
    . Online Version 2.0. United States Geological Survey. Retrieved 2008-08-19.
     
  20. ^ Covarrubias, Amanda; Doug Smith (2006-06-07). "3 Die in Mammoth Ski Patrol Accident". Los Angeles Times. Retrieved 2013-01-08. 
  21. ^ Burak, S.A.; R.E. Davis (2001). "Preliminary evaluation of snow accumulation patterns based on storm type, Mammoth Mountain, California, 1996-2001". Proc. Western Snow Conference. Archived from the original on 2007-09-30. 

Further reading[edit]

  • Alt, David; Donald Hyndman (2000). Roadside Geology of Northern and Central California. Missoula, Montana: Mountain Press Publishing Company. ISBN 0-87842-409-1. 

External links[edit]