| Mammoth Mountain | |
| Elevation Ft: | 11059 |
| Elevation Ref: | [1] |
| Prominence Ft: | 1647 |
| Prominence Ref: | [2] |
| Country: | United States |
| State: | California |
| Subdivision2 Type: | Counties |
| Subdivision3 Type: | Protected area |
| Map: | USA California#USA |
| Coordinates: | 37.6306°N -119.0326°W |
| Topo: | USGS Mammoth Mountain |
| Type: | Lava dome complex |
| Age: | About 50,000 to 200,000 years |
| Last Eruption: | 1260 ± 40 years |
| Easiest Route: | Gondola |
| Fetchwikidata: | ALL |
Mammoth Mountain is a lava dome complex partially located within the town of Mammoth Lakes, California, in the Inyo National Forest of Madera and Mono Counties. It is home to a large ski area primarily on the Mono County side.
Mammoth Mountain was formed in a series of eruptions that ended 57,000 years ago. Mammoth still produces hazardous volcanic gases that kill trees.
Mammoth Mountain is a lava dome complex in Mono County, California. It lies in the southwestern corner of the Long Valley Caldera and consists of about 12 rhyodacite and dacite overlapping domes. These domes formed in a long series of eruptions from 110,000 to 57,000 years ago, building a volcano that reaches 11059feet in elevation. During this time, massive dacite eruptions occurred roughly every 5000 years. The volcano is still active with minor eruptions, the largest of which was a minor phreatic (steam) eruption 700 years ago.
Mammoth Mountain also lies on the south end of the Mono-Inyo chain of volcanic craters. The magma source for Mammoth Mountain is distinct from those of both the Long Valley Caldera and the Inyo Craters.[3] Mammoth Mountain is composed primarily of dacite and rhyolite, part of which has been altered by hydrothermal activity from fumaroles (steam vents).[4]
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 . Measurements of the total discharge of carbon dioxide gas at the Horseshoe Lake tree-kill area range from 50to per day. This high concentration causes trees to die in six regions that total about 170acres in size (see photo).
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 U.S. Forest Service Ranger became ill with suffocation symptoms after being in a snow-covered cabin near Horseshoe Lake.
Measurements around the lake found that restrooms and tents had a greater than 1% concentration (toxic) and a deadly 25% concentration of in a small cabin. concentrations of less than 1% are typical and healthy in most soils; however, soil concentrations of in the tree-kill areas ranged from 20% to 90%. This overabundance of was found to be the cause of the tree-kills because tree roots need to absorb O2 directly and the high level reduced available O2. Researchers also determined that Mammoth releases about 1300ST of 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.
The most likely sources of the 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 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. 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.[5] There is evidence that the rate of discharge has been declining,[6] with emissions peaking in 1991.
In April 2006, three members of the Mammoth Mountain Ski Area ski patrol died while on duty when a fumarole caused a snow bridge to collapse under the patrollers.[7] The 2005/2006 winter season delivered significant snow depth of .[8] As the ski patrollers assessed the fumarole for skier safety, the perimeter snow collapsed, dropping the patrollers into the bottom of the fumarole, exposing them to extremely high levels of carbon dioxide.[9] It is unclear if they died as a result of the fall or as a result of the gas.
Mammoth Mountain is home to the Mammoth Mountain Ski Area, founded by Dave McCoy in 1953. Mammoth is a ski, snowboard, and snowmobile mountain during the winter months. Mammoth is the highest ski resort in California and is notable for the unusually large amount of snowfall it receives compared to other Eastern Sierra peaks—about 400inches annually and about 300 out of 365 days of sunshine—due to its location in a low gap in the Sierra crest. The ski area has more than 3500acres of skiable terrain, with 3100feet of vertical serviced by 25 lifts.[10] 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. To the south of the mountain, there are a number of lakes that serve as tourist attractions in the summer.