Mud volcano in the context of Gobustan Rock Art Cultural Landscape


Mud volcano in the context of Gobustan Rock Art Cultural Landscape

⭐ Core Definition: Mud volcano

A mud volcano or mud dome is a landform created by the eruption of mud or slurries, water and gases. Several geological processes may cause the formation of mud volcanoes. Mud volcanoes are not true igneous volcanoes as they do not produce lava and are not necessarily driven by magmatic activity. Mud volcanoes may range in size from less than a meter high and 1 or 2 meters across, to 700 meters tall and 10 kilometers wide. Smaller mud exudations are sometimes referred to as mud-pots.

The mud produced by mud volcanoes is mostly formed as hot water, which has been heated deep below the Earth's surface, begins to mix and blend with subterranean mineral deposits, thus creating the mud slurry exudate. This material is then forced upwards through a geological fault or fissure due to local subterranean pressure imbalances. Mud volcanoes are associated with subduction zones and about 1100 have been identified on or near land. The temperature of any given active mud volcano generally remains fairly steady and is much lower than the typical temperatures found in igneous volcanoes. Mud volcano temperatures can range from near 100 °C (212 °F) to occasionally 2 °C (36 °F), some being used as popular "mud baths".

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Mud volcano in the context of Temryuk

Temryuk (Russian: Темрю́к, IPA: [tʲɪmˈrʲʉk]) is a town and the administrative center of Temryuksky District in Krasnodar Krai, Russia, located on the Taman Peninsula on the right bank of the Kuban River not far from its entry into the Temryuk Bay, amid a field of mud volcanoes. The seaport of Temryuk is situated 4 kilometers (2.5 mi) from the town itself. Population: 41,413 (2020), 38,046 (2010 census); 36,118 (2002 census); 33,163 (1989 Soviet census); 26,600 (1975).

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Mud volcano in the context of Phreatic eruption

A phreatic eruption, also called a phreatic explosion, ultravulcanian eruption or steam-blast eruption, occurs when magma heats ground water or surface water. The extreme temperature of the magma (anywhere from 500 to 1,170 °C (930 to 2,100 °F)) causes near-instantaneous evaporation of water to steam, resulting in an explosion of steam, water, ash, rock, and volcanic bombs. At Mount St. Helens in Washington state, hundreds of steam explosions preceded the 1980 Plinian eruption of the volcano. A less intense geothermal event may result in a mud volcano.

Phreatic eruptions typically include steam and rock fragments; the inclusion of liquid lava is unusual. The temperature of the fragments can range from cold to incandescent. If molten magma is included, volcanologists classify the event as a phreatomagmatic eruption. These eruptions occasionally create broad, low-relief craters called maars. Phreatic explosions can be accompanied by carbon dioxide or hydrogen sulfide gas-emissions. Carbon dioxide can asphyxiate at sufficient concentration; hydrogen sulfide acts as a broad-spectrum poison. A 1979 phreatic eruption on the island of Java killed 140 people, most of whom were overcome by poisonous gases.

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Mud volcano in the context of Yanar Dag

Yanar Dagh (Azerbaijani: Yanar Dağ, lit.'burning mountain') is a natural gas fire that burns perpetually on a hillside on the Absheron Peninsula near Baku, the capital of Azerbaijan, a country known as "the Land of Fire". Flames rise up to 3 metres (9.8 ft) from a thin, porous layer of sandstone.

The Yanar Dagh flame burns steadily, fueled by a continuous seep of gas from beneath the surface. Unlike the nearby mud volcanoes of Lokbatan or Gobustan, there is no mud or liquid discharge at Yanar Dagh.

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