Aguajito

Last updated
El Aguajito
El Aguajito volcano.jpg
Highest point
Elevation 1,300 m (4,300 ft) [1]
Coordinates 27°36′N112°32′W / 27.600°N 112.533°W / 27.600; -112.533 [1]
Geography
Geology
Mountain type Caldera
Last eruption Pleistocene

El Aguajito (also called Santa Ana caldera) is a caldera volcano located on the Gulf of California in Mexico.

It is located between the Tres Virgenes volcano and the La Reforma caldera.

Related Research Articles

A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface. Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018.

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<span class="mw-page-title-main">Santa Ana Volcano</span> Large stratovolcano in El Salvador

The Santa Ana Volcano or Ilamatepec is a large stratovolcano located in the Santa Ana department of El Salvador. At 2,381 metres (7,812 ft) above sea level, it is the highest volcano in the country. It is located immediately west of Coatepeque Caldera.

<span class="mw-page-title-main">Almolonga</span> Stratovolcano in Guatemala

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<span class="mw-page-title-main">Maipo (volcano)</span> Mountain in Argentina

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<span class="mw-page-title-main">San Salvador (volcano)</span> Complex volcano in El Salvador

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<span class="mw-page-title-main">Coatepeque Caldera</span> Caldera in El Salvador

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<span class="mw-page-title-main">Elysium Mons</span> Martian volcano

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<span class="mw-page-title-main">Zavaritski Caldera</span> Volcanic crater in the Kuril Islands, Russia

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<span class="mw-page-title-main">Cosigüina</span> Stratovolcano in Nicaragua

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<span class="mw-page-title-main">Chinameca (volcano)</span> Stratovolcano in central-eastern El Salvador

Chinameca is a stratovolcano in central-eastern El Salvador. It lies north of San Miguel volcano and rises over the town of Chinameca. The volcano is topped by a 2 kilometres (1.2 mi) wide caldera known as Laguna Seca el Pacayal, and a satellite cone on the west side, Cerro el Limbo, rises higher than the caldera rim. Fumaroles can be found on the north side, and it has been the site of a geothermal exploration program.

<span class="mw-page-title-main">El Valle (volcano)</span>

El Valle is a stratovolcano in central Panama and is the easternmost volcano along the Central American Volcanic Arc which has been formed by the subduction of the Nazca Plate below Central America. Some time prior to 200,000 years ago, the volcano underwent a huge eruption event that caused the top of the volcano to collapse into the empty magma chamber below forming a large caldera. Several lava domes have developed inside the caldera since the collapse—forming Cerro Pajita, Cerro Gaital and Cerro Caracoral peaks. Prior to research in the early 1990s, it was thought that no active volcanism existed within Panama. But radioactive dates from El Valle show that the volcano last erupted as recently as 200,000 years ago.

<span class="mw-page-title-main">Biblis Tholus</span> Martian volcano

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<span class="mw-page-title-main">Volcanoes of east-central Baja California</span> Group of volcanoes in the center-east of the Baja California peninsula

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<span class="mw-page-title-main">Jovis Tholus</span> Martian geographical feature

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<span class="mw-page-title-main">Ceboruco</span> Volcano in central western Mexico

Ceboruco is a dacitic stratovolcano located in Nayarit, Mexico, northwest of the Trans-Mexican Volcanic Belt. The largest eruption, the Jala Plinian eruption, was around 930 AD ±200, VEI 6, releasing 11 cubic kilometres (2.6 cu mi) of tephra. The most recent and best documented eruption from Ceboruco lasted from 1870–1875, with fumarole activity lasting well into the 20th century. The mountain features one large caldera, created during the Jala eruption, with a smaller crater nested inside that formed when the Dos Equis lava dome collapsed during the Coapales eruption around 1100 AD. Within both of these craters, are several explosive volcanic features, including scoria deposits, lava domes, and pyroclastic domes, or cinder cone volcanoes.

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<span class="mw-page-title-main">Volcanic crater lake</span> Lake formed within a volcanic crater

A volcanic crater lake is a lake in a crater that was formed by explosive activity or a collapse during a volcanic eruption.

<span class="mw-page-title-main">Kīlauea Caldera</span> Crater of a shield volcano in the Hawaii

The Kīlauea Caldera, officially gazetted as Kīlauea Crater, is a caldera located at the summit of Kīlauea, an active shield volcano in the Hawaiian Islands. It has an extreme length of 2.93 mi (4.72 km), an extreme width of 1.95 mi (3.14 km), a circumference of 7.85 mi (12.63 km) and an area of 4.14 sq mi (10.7 km2). It contains Halemaʻumaʻu, an active pit crater near the caldera's southwestern edge.

References

  1. 1 2 "El Aguajito". Global Volcanism Program . Smithsonian Institution . Retrieved 2007-03-31.