McDermitt Caldera
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| McDermitt Caldera | |
|---|---|
 Geologic cross-section of McDermitt Caldera | |
| Highest point | |
| Peak | Jordan Meadow Mountain |
| Elevation | 6,816 ft (2,078 m)[1] |
| Coordinates | 41°51′01″N 118°02′12″W / 41.85028°N 118.03667°W[2] |
| Dimensions | |
| Length | 28 mi (45 km) north–south[3] |
| Width | 22 mi (35 km) east–west[3] |
| Geography | |
  McDermitt Caldera Location of the caldera in Oregon and Nevada  McDermitt Caldera McDermitt Caldera (Nevada) | |
| Location | Harney County, Oregon Malheur County, Oregon Humboldt County, Nevada |
| Range coordinates | 42°00′05″N 117°59′48″W / 42.00139°N 117.99667°W |
| Geology | |
| Rock age | 19 million years (Miocene) |
| Mountain type | Caldera |
| Last eruption | 16.39 ± 0.02 million years ago (Miocene) |
McDermitt Caldera is a Miocene caldera west of McDermitt in southeastern Oregon and northern Nevada in the United States. The oval-shaped caldera is about 28 miles (45 km) wide north–south and 22 miles (35 km) wide east–west.[3] It was formed by the Yellowstone hotspot about 16.4 million years ago.[4]
The highest point at McDermitt Caldera is 6,816 feet (2,078 m) above sea level at Jordan Meadow Mountain, which is part of the Montana Mountains of Nevada.[1][5]
Before American settlement, the area was occupied by the seminomadic Shoshone and Northern Paiute people. Beginning in the mid-19th century, ranching became the primary human activity. The caldera contains significant ore deposits, some of which have been exploited. Mercury and uranium were mined in the 20th century, and exploration with an eye toward future lithium extraction began around 2017.
The caldera is also an important ecological region for endangered species such as sage grouse and the Lahontan cutthroat trout. Sage grouse populations here are particularly healthy despite declines elsewhere in the western United States.
The caldera lies in a remote region along the Oregon–Nevada state line west of McDermitt and north of Winnemucca, Nevada. It is loosely shaped like a raindrop oriented north–south, with the wider end on the north.[3]
The caldera forms a endorheic basin within the larger Great Basin region in the western United States where water does not flow to the ocean.[6] The western part of the caldera is in the Trout Creek Mountains, and the northern part is in the Oregon Canyon Mountains.[3][7] The Montana Mountains, which contain the caldera's highest point, lie near the center of the caldera.[1][6]
McDermitt Caldera is in an arid high-altitude landscape. The Cascade Range to the west creates a rain shadow that includes this region. Standing water is rare, with annual rainfall under 10 in (250 mm). Temperatures are extreme, with winter lows approaching −10 °F (−23 °C) and summer highs approaching 105 °F (41 °C).[8]
Geology
McDermitt Caldera is possibly the oldest caldera in the Yellowstone hotspot track,[4] a path of volcanic features that are progressively younger to the northeast, extending across southern Idaho to Yellowstone Caldera. As the North American plate moved southwest relative to the underlying hotspot, volcanism migrated northeast from the McDermitt area.[9] The western part of the hotspot track is within the larger Basin and Range Province, where ongoing tectonic extension since about 17 million years ago has created the alternating mountain ranges and sedimentary basins typical of northern Nevada and southeastern Oregon.[10]
McDermitt Caldera formed from the collapse of a lava dome between 16.37 and 16.41 million years ago. The lava dome had been built by eruptions producing rhyolite beginning about 19 million years ago.[3][7] A lake subsequently formed in the caldera, depositing varved sediments, diatomite, opal, and organic matter amidst lava flows and tuffs.[11] During later volcanic activity, uplift of the caldera drained the lake,[8] and hydrothermal fluids moved upward through the lakebed sediments, carrying additional ore-bearing minerals.[6][8] The youngest volcanic activity at the caldera is 14.9 million years old.[12]
Other volcanic features in Oregon that are related to the Yellowstone hotspot include Smith Rock, which is part of the Crooked River caldera (older than McDermitt Caldera),[13] and the Columbia River Basalt Group, most of which is about the same age as McDermitt Caldera.[14]
History
The Shoshone and Northern Paiute people inhabited the lands in and around McDermitt Caldera before the United States expanded in the region. Before the mid-19th Century they lived a seminomadic lifestyle following migratory animals and seasonal foods.[15] These people fought American settlers in a series of battles during the 19th Century but were eventually removed to reservations throughout the West.
Fort McDermit was established by the U.S. Army east of the caldera in 1866 as part of this campaign. It was named for Lt. Col. Charles McDermitt, who was killed in a skirmish with Native Americans nearby in 1865.[16] The nearby community was named McDermitt after the fort, which also lends its name to the caldera.[17]
U.S. soldiers killed dozens of indigenous people at Thacker Pass in the late-1800s. The area has since became an important spiritual site for these tribes and ceremonies are held here to memorialize those killed. The native people continue to hunt and forage for traditional food sources in the region. The historical significance of the site, as well as the ecological resources, have led Native tribes to oppose lithium mine development in the 21st Century.[18]
Ranching by American settlers began during the conflict with resident natives and continues to this day. A stage road from Virginia City, Nevada to Silver City, Idaho passed near the caldera.[19]
Mercury and uranium were mined during the 20th Century with the latter being discovered in 1953. Lithium was discovered in the 1970s and the last mercury mine closed in 1992.[20][21] Abandoned mines and associated waste piles remain.[22]
Exploration for lithium extraction was approved by the federal government in 2017 with significant opposition from environmental, native, and agricultural groups.[23]
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