|Elevation||10,308 ft (3,142 m) at Mount Sheridan|
|Location||Yellowstone National Park, Wyoming, United States|
|Topo map||USGS Yellowstone National Park|
|Type||Caldera and supervolcano|
|Age of rock||640,000 years |
|Last eruption||1350 BC ± 200 years |
The Yellowstone Caldera is the volcanic caldera and supervolcano located in Yellowstone National Park in the United States, sometimes referred to as the Yellowstone Supervolcano. The caldera and most of the park are located in the northwest corner of Wyoming. The major features of the caldera measure about 34 by 45 miles (55 by 72 km).
The caldera formed during the last of three supereruptions over the past 2.1 million years: the Huckleberry Ridge eruption 2.1 million years ago (which created the Island Park Caldera and the Huckleberry Ridge Tuff), the Mesa Falls eruption 1.3 million years ago (which created the Henry's Fork Caldera and the Mesa Falls Tuff) and the Lava Creek eruption 640,000 years ago (which created the Yellowstone Caldera and the Lava Creek Tuff).
Volcanism at Yellowstone is relatively recent with calderas that were created during large eruptions that took place 2.1 million, 1.3 million, and 640,000 years ago. The calderas lie over a hotspot where light, hot, molten rock from the mantle rises toward the surface. While the Yellowstone hotspot is now under the Yellowstone Plateau, it previously helped create the eastern Snake River Plain (to the west of Yellowstone) through a series of huge volcanic eruptions. The hotspot appears to move across terrain in the east-northeast direction, but in fact the hotspot is much deeper than terrain and remains stationary while the North American Plate moves west-southwest over it.
Over the past 18 million years or so, this hotspot has generated a succession of violent eruptions and less violent floods of basaltic lava. Together these eruptions have helped create the eastern part of the Snake River Plain from a once-mountainous region. At least a dozen of these eruptions were so massive that they are classified as supereruptions. Volcanic eruptions sometimes empty their stores of magma so swiftly that they cause the overlying land to collapse into the emptied magma chamber, forming a geographic depression called a caldera.
The oldest identified caldera remnant straddles the border near McDermitt, Nevada-Oregon, although there are volcaniclastic piles and arcuate faults that define caldera complexes more than 60 km (37 mi) in diameter in the Carmacks Group of southwest-central Yukon, Canada, which are interpreted to have formed 70 million years ago by the Yellowstone hotspot. Progressively younger caldera remnants, most grouped in several overlapping volcanic fields, extend from the Nevada-Oregon border through the eastern Snake River Plain and terminate in the Yellowstone Plateau. One such caldera, the Bruneau-Jarbidge caldera in southern Idaho, was formed between 10 and 12 million years ago, and the event dropped ash to a depth of one foot (30 cm) 1,000 miles (1,600 km) away in northeastern Nebraska and killed large herds of rhinoceros, camel, and other animals at Ashfall Fossil Beds State Historical Park. The United States Geological Survey ("USGS") estimates there are one or two major caldera-forming eruptions and 100 or so lava extruding eruptions per million years, and "several to many" steam eruptions per century.
The loosely defined term 'supervolcano' has been used to describe volcanic fields that produce exceptionally large volcanic eruptions. Thus defined, the Yellowstone Supervolcano is the volcanic field which produced the latest three supereruptions from the Yellowstone hotspot; it also produced one additional smaller eruption, thereby creating West Thumb Lake 174,000 years ago. The three super eruptions occurred 2.1 million, 1.3 million, and 640,000 years ago, forming the Island Park Caldera, the Henry's Fork Caldera, and Yellowstone calderas, respectively. The Island Park Caldera supereruption (2.1 million years ago), which produced the Huckleberry Ridge Tuff, was the largest and produced 2,500 times as much ash as the 1980 Mount St. Helens eruption. The next biggest supereruption formed the Yellowstone Caldera (640,000 years ago) and produced the Lava Creek Tuff. The Henry's Fork Caldera (1.2 million years ago) produced the smaller Mesa Falls Tuff but is the only caldera from the Snake River Plain-Yellowstone (SRP-Y) hotspot that is plainly visible today.
Non-explosive eruptions of lava and less-violent explosive eruptions have occurred in and near the Yellowstone caldera since the last supereruption. The most recent lava flow occurred about 70,000 years ago, while a violent eruption excavated the West Thumb of Lake Yellowstone around 150,000 years ago. Smaller steam explosions occur as well; an explosion 13,800 years ago left a 5 km (3.1 mi) diameter crater at Mary Bay on the edge of Yellowstone Lake (located in the center of the caldera). Currently, volcanic activity is exhibited via numerous geothermal vents scattered throughout the region, including the famous Old Faithful Geyser, plus recorded ground swelling indicating ongoing inflation of the underlying magma chamber.
The volcanic eruptions, as well as the continuing geothermal activity, are a result of a great cove of magma located below the caldera's surface. The magma in this cove contains gases that are kept dissolved only by the immense pressure that the magma is under. If the pressure is released to a sufficient degree by some geological shift, then some of the gases bubble out and cause the magma to expand. This can cause a runaway reaction. If the expansion results in further relief of pressure, for example, by blowing crust material off the top of the chamber, the result is a very large gas explosion.
According to the analysis of earthquake data in 2013, the magma chamber is 80 km (50 mi) long and 20 km (12 mi) wide. It also has 4,000 km3 (960 cu mi) underground mass, of which 6–8% is filled with molten rock. This is about 2.5 times bigger than scientists had previously imagined it to be; however, scientists believe that the proportion of melt in the chamber is much too low to allow another supereruption.
Due to the volcanic and tectonic nature of the region, the Yellowstone Caldera experiences between 1000 and 2000 measurable earthquakes a year. Most are relatively minor, measuring a magnitude of 3 or weaker. Occasionally, numerous earthquakes are detected in a relatively short period of time, an event known as an earthquake swarm. In 1985, more than 3000 earthquakes were measured over several months. More than 70 smaller swarms have been detected between 1983 and 2008. The USGS states these swarms are likely caused by slips on pre-existing faults rather than by movements of magma or hydrothermal fluids.
In December 2008, continuing into January 2009, more than 500 quakes were detected under the northwest end of Yellowstone Lake over a seven-day span, with the largest registering a magnitude of 3.9. The most recent swarm started in January 2010 after the Haiti earthquake and before the Chile earthquake. With 1620 small earthquakes between January 17, 2010 and February 1, 2010, this swarm was the second largest ever recorded in the Yellowstone Caldera. The largest of these shocks was a magnitude 3.8 on January 21, 2010 at 11:16 PM MST. This swarm reached the background levels by February 21. On March 30, 2014, at 6:34 AM MST, a magnitude 4.8 earthquake struck Yellowstone, the largest recorded there since February 1980.
The last full-scale eruption of the Yellowstone Supervolcano, the Lava Creek eruption which happened nearly 640,000 years ago, ejected approximately 240 cubic miles (1,000 km3) of rock, dust and volcanic ash into the sky.
The upward movement of the Yellowstone caldera floor between 2004 and 2008 — almost 3 inches (7.6 cm) each year — was more than three times greater than ever observed since such measurements began in 1923. From mid-summer 2004 through mid-summer 2008, the land surface within the caldera moved upward as much as 8 inches (20 cm) at the White Lake GPS station. By the end of 2009, the uplift had slowed significantly and appeared to have stopped. In January 2010, the USGS stated that "uplift of the Yellowstone Caldera has slowed significantly" and that uplift continues but at a slower pace. The U.S. Geological Survey, University of Utah and National Park Service scientists with the Yellowstone Volcano Observatory maintain that they "see no evidence that another such cataclysmic eruption will occur at Yellowstone in the foreseeable future. Recurrence intervals of these events are neither regular nor predictable." This conclusion was reiterated in December 2013 in the aftermath of the publication of a study by University of Utah scientists finding that the "size of the magma body beneath Yellowstone is significantly larger than had been thought." The Yellowstone Volcano Observatory issued a statement on its website stating,
Although fascinating, the new findings do not imply increased geologic hazards at Yellowstone, and certainly do not increase the chances of a 'supereruption' in the near future. Contrary to some media reports, Yellowstone is not 'overdue' for a supereruption.
Other media reports were more hyperbolic in their coverage.
A study published in GSA Today identified three fault zones that future eruptions are most likely to be centered on. Two of those areas are associated with lava flows aged 174,000–70,000 years, and the third area is a focus of present-day seismicity.
Hydrothermal explosion hazard
Studies and analysis may indicate that the greater hazard comes from hydrothermal activity which occurs independently of volcanic activity. Over 20 large craters have been produced in the past 14,000 years, resulting in such features as Mary Bay, Turbid Lake, and Indian Pond which was created in an eruption about 1300 BC.
In a 2003 report, USGS researchers proposed that an earthquake may have displaced more than 77 million cubic feet (2,200,000 m3) (576,000,000 US gallons) of water in Yellowstone Lake, creating colossal waves that unsealed a capped geothermal system leading into the hydrothermal explosion that formed Mary Bay.
Further research shows that earthquakes from great distances reach and have effects upon the activities at Yellowstone, such as the 1992 7.3 magnitude Landers earthquake in California’s Mojave Desert that triggered a swarm of quakes from more than 800 miles (1,300 km) away and the 2002 7.9 magnitude Denali fault earthquake 2,000 miles (3,200 km) away in Alaska that altered the activity of many geysers and hot springs for several months afterward.
Yellowstone hotspot origin
The source of the Yellowstone hotspot is controversial. Some geoscientists hypothesize that the Yellowstone hotspot is the effect of an interaction between local conditions in the lithosphere and upper mantle convection. Others suggest a deep mantle origin (mantle plume). Part of the controversy is due to the relatively sudden appearance of the hotspot in the geologic record. Additionally, the Columbia Basalt flows appeared at the same approximate time, causing speculation about their origin.
- Iceland hotspot and Iceland plume describes aspects of volcanic processes
- Long Valley Caldera, Valles Caldera, La Garita Caldera: examples of other calderas close to but not related to Yellowstone.
- "Mount Sheridan,vbe 3 Wyoming". Peakbagger.com. Retrieved December 31, 2008.
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- as determined by geological field work conducted by Bob Christiansen of the United States Geological Survey in the 1960s and 1970s.
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- Johnston, Stephen T.; Wynne, P. Jane; Francis, Don; Hart, Craig J. R.; Enkin, Randolph J.; Engebretson, David C. (1996). "Yellowstone in Yukon: The Late Cretaceous Carmacks Group". Geology 24 (11): 997, 998. Bibcode:1996Geo....24..997J. doi:10.1130/0091-7613(1996)024<0997:YIYTLC>2.3.CO;2.
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- West Thumb Lake is not to be confused with West Thumb Geyser Basin. The caldera created West Thumb Lake, and the underlying Yellowstone hotspot keeps West Thumb Geyser Basin active. See Fig. 22. See also File:Yellowstone Caldera map2.JPG.
- Newhall, Christopher G.; Dzurisin, Daniel (1988) Historical Unrest at Large Calderas of the World: U.S. Geological Survey Bulletin 1855
- This qualitative statement is easily verified by reviewing the Yellowstone area in Google Earth
- "Origin and evolution of silicic magmatism at Yellowstone" (PDF). University of Oregon.
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- Witze, Alexandra (2013). "Large magma reservoir gets bigger". Nature. doi:10.1038/nature.2013.14036.
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- Johnson, Kirk (January 31, 2010). "Hundreds of Quakes Are Rattling Yellowstone". The New York Times. Retrieved January 23, 2014.
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- Molten Rock Fills Yellowstone Volcano at Record Rate Newswise, Retrieved on September 2, 2008.
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- Smith, Robert B.; Jordan, Michael; Steinberger, Bernhard; Puskas, Christine M.; Farrell, Jamie; Waite, Gregory P.; Husen, Stephan; Chang, Wu-Lung; O'Connell, Richard (November 20, 2009). "Geodynamics of the Yellowstone hotspot and mantle plume: Seismic and GPS imaging, kinematics and mantle flow" (PDF). Journal of Volcanology and Geothermal Research 188 (1–3): 26–56. doi:10.1016/j.jvolgeores.2009.08.020.
- Alert Archive Search. volcanoes.usgs.gov
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- "Monitoring Upgrades Result in New Insight Into Yellowstone's Magma System" (Press release). Yellowstone Volcano Observatory (USGS). December 19, 2013. Retrieved January 2, 2014.
- Burnett, Jim (January 1, 2014). "Reactions To Yellowstone Supervolcano Study Ranged From Hysteria To Ho-Hum". National Parks Traveller. Retrieved January 2, 2014.
- Richard A. Lovett (September 20, 2012). "Yellowstone Supervolcano Discovery—Where Will It Erupt?". National Geographic.
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- See list of off-line references in mantleplumes.org/CRB.html
- Ivanov, Alexei V. (February 7, 2007). "The Columbia River Flood Basalts: Consequence of subduction-related processes". MantlePlumes.org. Retrieved December 31, 2008.
- Breining, Greg (2007). Super Volcano: The Ticking Time Bomb beneath Yellowstone National Park. St. Paul, MN: Voyageur Press. ISBN 978-0-7603-2925-2.
A popularized scientific look at the Yellowstone area's geological past and potential future
- Vazquez, J.A.; Reid, M.R. (2002). "Time scales of magma storage and differentiation of voluminous rhyolites at Yellowstone caldera". Contributions to Mineralogy & Petrology (Wyoming) 144 (3): 274–285. Bibcode:2002CoMP..144..274V. doi:10.1007/s00410-002-0400-7.
- Sutherland, Wayne; Sutherland, Judy (2003). Yellowstone Farewell. Spur Ridge.