Hydrothermal explosion

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Small 2009 hydrothermal explosion in Biscuit Basin, Yellowstone National Park Hydrothermal explosion at Biscuit Basin.jpg
Small 2009 hydrothermal explosion in Biscuit Basin, Yellowstone National Park

Hydrothermal explosions occur when superheated water trapped below the surface of the Earth rapidly converts from liquid to steam, violently disrupting the confining rock. Boiling water, steam, mud, and rock fragments are ejected over an area of a few meters up to several kilometers in diameter. Although the energy originally comes from a deep igneous source, this energy is transferred to the surface by circulating meteoric water or mixtures of meteoric and magmatic water rather than by magma, as occurs in volcanic eruptions. The energy is stored as heat in hot water and rock within a few hundred feet of the surface.

Contents

Hydrothermal explosions are caused by the same instability and chain reaction mechanism as geysers but are so violent that rocks and mud are expelled along with water and steam. [1]

Cause

Hydrothermal explosions occur where shallow interconnected reservoirs of water at temperatures as high as 250 °C underlie thermal fields. Water usually boils at 100 °C, but under pressure its boiling point increases, causing the water to become superheated. A sudden reduction in pressure causes a rapid phase transition from liquid to steam, resulting in an explosion of water and rock debris. [2] During the last Ice Age, many hydrothermal explosions were triggered by the release of pressure as glaciers receded. [3] Other causes are seismic activity, erosion, or hydraulic fracturing. [4]

Yellowstone

Indian Pond, a 3,000 year old, 350-430 metres (1,150-1,410 ft) diameter hydrothermal explosion crater in Yellowstone National Park Indian Pond (hydrothermal explosion crater) (Holocene; Yellowstone, Wyoming, USA) 3.jpg
Indian Pond, a 3,000 year old, 350–430 metres (1,150–1,410 ft) diameter hydrothermal explosion crater in Yellowstone National Park

Yellowstone National Park is a thermally active area with an extensive system of hot springs, fumaroles, geysers, and mudpots. There are also several hydrothermal explosion craters, which are not to be confused with calderas, which are collapse features. Eight of these hydrothermal explosion craters are in hydrothermally cemented glacial deposits, and two are in Pleistocene ash-flow tuff. [1] Each is surrounded by a rim composed of debris derived from the crater, 30 to 100 feet high. [3]

More than 20 large hydrothermal explosions have occurred at Yellowstone, approximately one every 700 years. [2] The temperature of the magma reservoir below Yellowstone is believed to exceed 800 °C causing the heating of rocks in the region. If so, the average heat flow supplied by convection currents is 30 times greater than anywhere in the Rocky Mountains. Snowmelt and rainfall seep into the ground at a rapid rate and can conduct enough heat to raise the temperature of ground water to almost boiling.

The phenomena of geyser basins are the product of hot ground water rising close to the surface and occasionally bubbling through. Water temperatures of 238 °C at 332 meters have been recorded at Norris Geyser Basin. [5] Pocket Basin was originally an ice-dammed lake over a hydrothermal system. Melting ice during the last glacial period caused the lake to rapidly drain, causing a sudden change in pressure triggering a massive hydrothermal explosion. [1]

Geysers

A hydrothermal explosion is similar to a geyser's eruption except that it includes surrounding rock and mud and does not occur periodically. [6]

One well-known hydrothermal geyser is Old Faithful which throws up plumes of steam and water approximately every hour and a half on average. Rarely has any steam explosion violently hurled water and rock thousands of feet above the ground; however in Yellowstone's geological history these colossal events have been recorded numerous times and have been found to have created new hills and shaped parts of the landscape.

The largest hydrothermal explosion ever documented was located near the northern edge of Yellowstone Lake, on an embankment commonly known as "Mary Bay". Now consisting of a 1.5 mile crater, it was formed relatively recently, approximately 13,800 years ago. It is believed this crater was formed by a sequence of several hydrothermal explosions in a short time. What triggered this series of events has not yet been clearly established, but volcanologists believe a large earthquake could have played a role by accelerating the melting of nearby glaciers and thus depressurizing the hydrothermal system. Alternatively, rapid changes in the level of Yellowstone Lake may have been responsible.

Recent explosions

Most of Yellowstone's recent large hydrothermal explosions have been the consequence of sudden changes of pressure deep within the hydrothermal system. Generally, these larger explosions have created craters in a north–south pattern (between Norris and Mammoth Hot Springs). It is estimated that all of the known hydrothermal craters were created between 14,000 and 3,000 years ago. Volcanologists believe no magma has ever broken through the fragile crust of Yellowstone Park or stirred the movement of magma in the reservoir beneath Yellowstone.

Several small hydrothermal explosions have been recorded since the opening of Yellowstone National Park. During the 1880s, Excelsior Geyser in Midway Geyser Basin was known for significant hydrothermal explosions. [7] Other explosions have been linked to seismic events, such as during the 1959 Hebgen Lake earthquake, [8] while others are linked to changes in plumbing below geysers or hot springs, such as the 1989 explosion at Porkchop Geyser in the Norris Geyser Basin. [9] Small hydrothermal eruptions occur nearly yearly, [10] although many occur in Yellowstone's backcountry. [7]

On 23 July 2024, a small hydrothermal explosion was witnessed by several tourists coming from the Black Diamond Pool hot spring in Biscuit Basin. [11] The explosion, probably caused by a change in the plumbing under the hot spring, launched a plume of water and rock fragments 400–600 feet (120–180 m) into the air. [12] Although there were no injuries, the explosion forced the closure of Biscuit Basin for the rest of the 2024 season. [7]

See also

Related Research Articles

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A geyser is a spring with an intermittent discharge of water ejected turbulently and accompanied by steam. The formation of geysers is fairly rare, and is caused by particular hydrogeological conditions that exist only in a few places on Earth.

<span class="mw-page-title-main">Fumarole</span> Volcanic opening that emits hot gases

A fumarole is a vent in the surface of the Earth or another rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids. Fumaroles are characteristic of the late stages of volcanic activity, but fumarole activity can also precede a volcanic eruption and has been used for eruption prediction. Most fumaroles die down within a few days or weeks of the end of an eruption, but a few are persistent, lasting for decades or longer. An area containing fumaroles is known as a fumarole field.

<span class="mw-page-title-main">Stratovolcano</span> Type of conical volcano composed of layers of lava and tephra

A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica, with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi).

<span class="mw-page-title-main">Old Faithful</span> Geyser in Yellowstone National Park in Wyoming, United States

Old Faithful is a cone geyser in Yellowstone National Park in Wyoming, United States. It was named in 1870 during the Washburn–Langford–Doane Expedition and was the first geyser in the park to be named. It is a highly predictable geothermal feature and has erupted every 44 minutes to two hours since 2000. The geyser and the nearby Old Faithful Inn are part of the Old Faithful Historic District.

<span class="mw-page-title-main">Geothermal areas of Yellowstone</span> Geyser basins and other geothermal features in Yellowstone National Park

The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.

Hydrothermal circulation in its most general sense is the circulation of hot water. Hydrothermal circulation occurs most often in the vicinity of sources of heat within the Earth's crust. In general, this occurs near volcanic activity, but can occur in the shallow to mid crust along deeply penetrating fault irregularities or in the deep crust related to the intrusion of granite, or as the result of orogeny or metamorphism. Hydrothermal circulation often results in hydrothermal mineral deposits.

<span class="mw-page-title-main">Geology of the Lassen volcanic area</span> Geology of a U.S. national park in California

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<span class="mw-page-title-main">Yellowstone Caldera</span> Volcanic caldera in Yellowstone National Park in the United states

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<span class="mw-page-title-main">Phreatic eruption</span> Volcanic eruption caused by an explosion of steam

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<span class="mw-page-title-main">Castle Geyser</span> Geyser in Yellowstone National Park, Wyoming

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<span class="mw-page-title-main">Grand Prismatic Spring</span> Largest hot spring in the United States

The Grand Prismatic Spring in Yellowstone National Park is the largest hot spring in the United States, and the third largest in the world, after Frying Pan Lake in New Zealand and Boiling Lake in Dominica. It is located in the Midway Geyser Basin.

<span class="mw-page-title-main">Artemisia Geyser</span>

Artemisia Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.

<span class="mw-page-title-main">Excelsior Geyser</span> Dormant fountain-type geyser in the Midway Geyser Basin of Yellowstone National Park

Excelsior Geyser Crater, formerly known as Excelsior Geyser, is a dormant fountain-type geyser in the Midway Geyser Basin of Yellowstone National Park in the United States. Excelsior was named by the Hayden Geological Survey of 1871.

<span class="mw-page-title-main">Explosive eruption</span> Type of volcanic eruption in which lava is violently expelled

In volcanology, an explosive eruption is a volcanic eruption of the most violent type. A notable example is the 1980 eruption of Mount St. Helens. Such eruptions result when sufficient gas has dissolved under pressure within a viscous magma such that expelled lava violently froths into volcanic ash when pressure is suddenly lowered at the vent. Sometimes a lava plug will block the conduit to the summit, and when this occurs, eruptions are more violent. Explosive eruptions can expel as much as 1,000 kg (2,200 lb) per second of rocks, dust, gas and pyroclastic material, averaged over the duration of eruption, that travels at several hundred meters per second as high as 20 km (12 mi) into the atmosphere. This cloud may subsequently collapse, creating a fast-moving pyroclastic flow of hot volcanic matter.

<span class="mw-page-title-main">Solitary Geyser</span>

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<span class="mw-page-title-main">Yellowstone Plateau Volcanic Field</span> Volcanic field in Southern United States with three major calderas

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<span class="mw-page-title-main">Giant Geyser</span> Geyser in Yellowstone National Park

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<span class="mw-page-title-main">Hot Creek (Mono County)</span> River in California, United States

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<span class="mw-page-title-main">Giantess Geyser</span>

Giantess Geyser is a fountain-type geyser in the Upper Geyser Basin of Yellowstone National Park. It is known for its violent and infrequent eruptions of multiple water bursts that reach from 100 to 200 feet. Eruptions generally occur 2 to 6 times a year. The surrounding area may shake from underground steam explosions just before the initial water and/or steam eruptions. Eruptions may occur twice hourly, experience a tremendous steam phase, and continue activity for 4 to 48 hours. The Geyser last erupted on August 26, 2020, after a six-year, 210 day hiatus. A follow-up eruption occurred 15 days later on 10 September 2020. Another eruption occurred on 11 August 2021

<span class="mw-page-title-main">Geothermal activity</span> Activity resulting from underground heat

Geothermal activity is a group of natural heat transfer processes, occurring on Earth's surface, caused by the presence of excess heat in the subsurface of the affected area, usually caused by the presence of an igneous intrusion underground. Geothermal activity can manifest itself in a variety of different phenomena, including, among others, elevated surface temperatures, various forms of hydrothermal activity, and the presence of fumaroles that emit hot volcanic gases.

References

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  2. 1 2 Morgan, L. A.; Shanks, W. P.; Pierce, K. L. (2006), "Super eruption environments make for "super" hydrothermal explosions: Extreme hydrothermal explosions in Yellowstone National Park", AGU Fall Meeting Abstracts, 2006, American Geophysical Union, Fall Meeting 2006: V33C–0689, Bibcode:2006AGUFM.V33C0689M
  3. 1 2 Robert Baer Smith; Lee J. Siegel (2000), Windows into the earth: the geologic story of Yellowstone and Grand Teton national parks, Oxford University Press US, pp. 64–66, ISBN   0-19-510597-4
  4. Rose, William Ingersoll (2004), Natural hazards in El Salvador, Geological Society of America, pp. 246–247, ISBN   0-8137-2375-2
  5. "Supervolcano Yellowstone". Archived from the original on 2014-08-05. Retrieved 2008-05-20.
  6. Angus M. Thuermer (2009-05-25), Yellowstone Explosion: Geologists Witness Rare Yellowstone Explosion, The Jackson Hole News & Guide
  7. 1 2 3 "Update on the July 23 Biscuit Basin hydrothermal explosion". nps.gov. National Park Service. Retrieved 1 August 2024.
  8. "Hydrothermal explosions in Yellowstone National Park | U.S. Geological Survey". www.usgs.gov. U.S. Geological Survey. Retrieved 1 August 2024.
  9. "The day that Porkchop Geyser exploded | U.S. Geological Survey". www.usgs.gov. U.S. Geological Survey. Retrieved 1 August 2024.
  10. Poland, Michael. "A small hydrothermal explosion at Norris Geyser Basin | U.S. Geological Survey". www.usgs.gov. U.S Geological Survey. Retrieved 1 August 2024.
  11. Musa, Amanda (25 July 2024). "Yellowstone's popular Biscuit Basin is closed for the summer after hydrothermal explosion". CNN. Retrieved 1 August 2024.
  12. Poland, Michael. "The July 23, 2024, hydrothermal explosion at Biscuit Basin | U.S. Geological Survey". www.usgs.gov. U.S. Geological Survey. Retrieved 1 August 2024.