(geology) A conical accumulation of variable admixtures of sand and rock fragments, the whole resulting from eruption of wet mud and impelled upward by fluid or gas pressure. Also known as hervidero; macaluba.
| Sci-Tech Dictionary: mud volcano |
(geology) A conical accumulation of variable admixtures of sand and rock fragments, the whole resulting from eruption of wet mud and impelled upward by fluid or gas pressure. Also known as hervidero; macaluba.
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| Wikipedia: Mud volcano |
The term mud volcano or mud dome is used to refer to formations created by geo-excreted liquids and gases, although there are several different processes which may cause such activity. Temperatures are much cooler than igneous processes. The largest structures are 10 km in diameter and reach 700 metres in height.
About 20% of released gases are methane, with much less carbon dioxide and nitrogen emitted. Ejected materials often are a slurry of fine solids suspended in liquids which may include water (frequently acidic or salty) and hydrocarbon fluids.
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A mud volcano may be the result of a piercement structure created by a pressurized mud diapir which breaches the Earth's surface or ocean bottom. Temperatures may be as low as the freezing point of ejected materials, particularly when venting is associated with the creation of hydrocarbon clathrate hydrate deposits.
Mud volcanoes are often associated with petroleum deposits and tectonic subduction zones and orogenic belts; hydrocarbon gases are often erupted. They are also often associated with lava volcanoes; in the case of such close proximity, mud volcanoes emit incombustible gases including helium, whereas lone mud volcanoes are more likely to emit methane.
In Azerbaijan, eruptions are driven from a deep mud reservoir which is connected to the surface even during dormant periods, when seeping water still shows a deep origin. Seeps have temperatures up to 2–3 °C above the ambient temperature.[1]
Approximately 1,100 mud volcanoes have been identified on land and in shallow water. It has been estimated that well over 10,000 may exist on continental slopes and abyssal plains.
Most liquid and solid material is released during eruptions, but various seeps occur during dormant periods.
First order estimates of mud volcano emissions have recently been made (1 Tg = 1 million metric tonnes).
Mud volcanoes are generally few in Europe, but dozens can be found on the Taman Peninsula of Russia and the Kerch Peninsula of southeastern Ukraine. In Italy, they are common in the northern front of the Apennines and in Sicily. Another relatively accessible place where mud volcanoes can be found in Europe are the Berca Mud Volcanoes near Berca in Buzău County, Romania, close to the Carpathian Mountains.
Many mud volcanoes exist on the shores of the Black Sea and Caspian Sea. Tectonic forces and large sedimentary deposits around the latter have created several fields of mud volcanoes, many of them emitting methane and other hydrocarbons. Features over 200 meters high exist in Azerbaijan, with large eruptions sometimes producing flames of similar scale (see below). Iran and Pakistan also possess mud volcanoes in the Makran range of mountains in the south of the two countries. In fact, the world's largest and highest volcano is located in Balochistan, Pakistan.[6]
China has a number of mud volcanoes in Xinjiang province. There are also mud volcanoes at the Arakan Coast in Myanmar (Burma). There are two active mud volcanoes in South Taiwan, and several inactive ones.
The island of Baratang, part of the Great Andaman archipelago in the Andaman Islands, Indian Ocean, has several sites of mud volcanic activity. There was a significant eruption event in 2003.
A drilling accident offshore of Brunei in 1979 caused a mud volcano which took 20 relief wells and nearly 30 years to stop the eruption.
Drilling or an earthquake may have resulted in the Sidoarjo mud flow on May 29, 2006, in the Porong subdistrict of East Java province, Indonesia. The mud covered about 440 hectares, or 1,087 acres (4.40 km2), and inundated four villages, homes, roads, rice fields, and factories and displaced about 24,000 people, killing 14. The gas exploration company was operated by PT Lapindo Brantas. In 2008, it was termed the world's largest mud volcano and is beginning to show signs of catastrophic collapse, according to geologists who have been monitoring it and the surrounding area. A catastrophic collapse could sag the vent and surrounding area by up to 150 meters in the next decade. In March 2008, the scientists observed drops of up to 3 meters in one night. Most of the subsidence in the area around the volcano is more gradual, at around 0.1 cm per day. Now named Lusi, the mud volcano appears to be a hydrocarbon/hydrothermal hybrid. Lusi is actually a contraction of Lumpur Sidoarjo, where lumpur is the Indonesian word for "mud".
In Pakistan there are more than 80 active mud volcanoes, all of them in Baluchistan province; there are about 10 locations having clusters of mud volcanoes. In the west, in Gwadar District, the mud volcanoes are very small and mostly sit in the south of Jabal-e-Mehdi toward Sur Bandar. Many more exist in the north-east of Ormara. The remainder are in Lasbela District and are scattered between south of Gorangatti on Koh Hinglaj to Koh Kuk in the North of Miani Hor in the Hangol Valley. In this region, the heights of mud volcanoes range between 800 to 1550 feet. The most famous is Chandaragup. The biggest crater found is about 450 feet in diameter. Most mud volcanoes in this region are situated in out-of-reach areas having very difficult terrain. Dormant mud volcanoes stand like columns of mud in many other areas.
Azerbaijan and its Caspian coastline are home to nearly 400 mud volcanoes, more than half the total throughout the continents. In 2001, one mud volcano 15 kilometers from Baku made world headlines when it suddenly started ejecting flames 15 meters high.[7]
Mud volcanoes of the North American continent include:
South American mud volcanoes include:
The name of Yellowstone National Park's "Mud Volcano" feature and the surrounding area is misleading; it consists of hot springs, mud pots and fumaroles, rather than a true mud volcano. Depending upon the precise definition of the term mud volcano, the Yellowstone formation could be considered a hydrothermal mud volcano cluster. The feature is much less active than in its first recorded description, although the area is quite dynamic. Yellowstone is an active geothermal area with a magma chamber near the surface, and active gases are chiefly steam, carbon dioxide, and hydrogen sulfide.[8]
The mud volcano in Yellowstone was previously a mound, until suddenly, it tore itself apart into the formation seen today.[9]
Recently, possible mud volcanoes have been identified on Mars.[10]
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
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