A subglacial volcano , also known as a glaciovolcano , is a volcanic form produced by subglacial eruptions or eruptions beneath the surface of a glacier or ice sheet which is then melted into a lake by the rising lava . Today they are most common in Iceland and Antarctica ; older formations of this type are found also in British Columbia and Yukon Territory , Canada .
8-536: Slag Hill is a subglacial volcano associated with the Mount Cayley volcanic field in British Columbia , Canada . It consists of glassy, augite -phyric basaltic andesite in steep-sided, glassy, finely jointed domes and one small, flat-topped bluff . The finely jointed domes are similar to those of Ember Ridge . There are quench features at Slag Hill, which is suggesting that the volcanic activity
16-748: The Grímsvötn Volcano beneath the Vatnajökull ice sheet erupted and caused a Jökulhlaup that affected more than 750 km (290 sq mi) and destroyed or severely damaged several bridges. Sonia Esperanca, program director in the National Science Foundation commented on the danger of subglacial volcanoes: "When an ice-covered volcano erupts, the interplay among molten magma, ice and meltwater can have catastrophic results." In 2008, British Antarctic Survey scientists led by Hugh Corr and David Vaughan, reported (in
24-485: The Grímsvötn caldera erupted, melting 3 km of ice and giving rise to a large glacial lake outburst flood . The shape of subglacial volcanoes tends to be quite characteristic and unusual, with a flattened top and steep sides supported against collapse by the pressure of the surrounding ice and meltwater. If the volcano eventually melts completely through the ice layer, then horizontal lava flows are deposited, and
32-467: The eruption, the heat of the lava from the subglacial volcano melts the overlying ice. The water quickly cools the lava, resulting in pillow lava shapes similar to those of underwater volcanoes . When the pillow lavas break off and roll down the volcano slopes, pillow breccia , tuff breccia, and hyaloclastite form. The meltwater may be released from below the ice as happened in Iceland in 1996 when
40-591: The journal Nature Geoscience ) that 2,200 years ago, a volcano erupted under the Antarctica ice sheet (based on airborne survey with radar images). The biggest eruption in Antarctica in the last 10,000 years, the volcanic ash was found deposited on the ice surface under the Hudson Mountains , close to Pine Island Glacier . Many scientists believe that liquid water exists many kilometers below
48-459: The surface of Mars, but at this point in time it is impossible to drill to those depths with the rovers in existence. Meredith Payne and Jack Farmer of Arizona State University have studied images from the Viking and Mars Orbiter cameras in search of possible sub-glacial volcanoes that could carry microbes to the surface. It is possible to track catastrophic subglacial volcano eruptions in time with
56-610: The top of the volcano assumes a nearly level form. However, if significant amounts of lava are later erupted subaerially , then the volcano may assume a more conventional shape. In Canada the volcanos have been known to form both conical and nearly level shapes. The more distinctly flat-topped, steep-sided subglacial volcanoes are called tuyas , named after Tuya Butte in northern British Columbia by Canadian geologist Bill Mathews in 1947. In Iceland, such volcanoes are also known as table mountains . Subglacial eruptions often cause jökulhlaups or great floods of water. In November 1996
64-583: Was subglacial . Slag Hill was formed throughout the Pleistocene period, but its most recent volcanic activity produced a lava flow on its western lobe that shows no evidence of ice-contact volcanism. This indicates the lava flow was erupted less than 10,000 years ago after the last glacial period . This article about a location on the Coast of British Columbia , Canada is a stub . You can help Misplaced Pages by expanding it . Subglacial volcano During
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