Gas emission crater

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The Yamal crater [ru] -- Top: 2015, bottom: heaving mound and the crater formed after the explosion Yamal crater.jpg
The Yamal crater  [ ru ] Top: 2015, bottom: heaving mound and the crater formed after the explosion

A gas emissions crater or GEC is a crater that is left by an explosion that is believed to be caused by an overheated buildup of gas stuck below a layer of permafrost. [1] The gas is methane (also known as "natural gas") and is generally believed by experts to have sept up from large underground reserves toward the Earth's surface "through some kind of geological fault," [1] getting trapped when they reach the bottom of the permafrost. [1] [2] [3] First known to have occurred in 2013, they are occurring solely in Siberia, where there are large stores of natural gas below a melting surface layer of permafrost. [1] They are believed to be a byproduct of global climate change, since the warming of Siberia's climate weakens the permafrost enough to allow a sub-surface methane buildup to cause an outburst. [1] [4] The release of this previously trapped methane into the atmosphere is also likely to increase the speed of global climate change. [1]

Contents

Gas emission craters were first spotted in 2013; [5] later satellite analysis has indicated that it was formed sometime between October 9 and November 1, 2013. Most famously, the discovery of the Yamal crater  [ ru ] in 2014 quickly drew the attention of world media. [6] As of 2020, there were 17 known gas emissions craters, all of which are in the circumpolar regions of Western Siberia, on either the Yamal Peninsula or the neighboring Gydan Peninsula, which both sit atop large underground methane reserves. [4] They are variously located on land as well as at the bottom of rivers and lakes. Soon after their discovery, the term "gas emissions crater" was proposed and subsequently accepted by the scientific community.

Cause

Cryovolcanism on the Earth Cryovolcanism on the Earth.png
Cryovolcanism on the Earth

Initially, with the sudden global fame of the Yamal crater  [ ru ], various hypotheses of its origin were put forward, including military tests, meteorite impact, UFOs, or the collapse of an underground gas facility. [7] [8] Later, in September 2018, a group of researchers from Moscow State University published an article in the journal Scientific Reports that claimed that the Yamal crater was the first cryovolcano discovered on Earth. [9]

A summary of the suggested two groups of models for the GECs formation. 09eartharxiv gecsmanuscript.jpg
A summary of the suggested two groups of models for the GECs formation.

Subsequently, however, in the course of scientific research, the scientific community has come to the general conclusion that the crater was formed as a result of the so-called gas release an underground explosion of methane hydrates which ejects into the air all the rock and soil above it (along with releasing the methane itself). [10] [1] [2] [3] More specifically, their formation most likely occurs under the influence of fluid-dynamic processes in permafrost, which lead to the appearance of zones of accumulation of free natural gas near the surface. In this case, when the reservoir pressure of the accumulated gas fluids exceeds the pressure of the overlying strata, an avalanche-like outburst of gas-saturated rocks may occur.

See also

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<span class="mw-page-title-main">Permafrost</span> Soil frozen for a duration of at least two years

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<span class="mw-page-title-main">Sergey Zimov</span>

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References

  1. 1 2 3 4 5 6 7 Pakalolo (2024-01-16). "Siberia's exploding tundra craters mystery may have been solved". DailyKOS. Retrieved 2024-01-17.
  2. 1 2 Guenot, Marianne (2024-01-15). "The mystery of Siberia's strange exploding craters may have finally been solved". Business Insider. Retrieved 2024-01-17.
  3. 1 2 3 Hellevang, Helge; Ippach, Mats Rouven; Westermann, Sebastian; Nooraiepour, Mohammad (2023-12-07). "Formation of giant Siberian gas emission craters (GECs)". Working paper. doi:10.31223/X59Q3K . Retrieved 2024-01-17.
  4. 1 2 Gray, Richard (1 December 2020). "The mystery of Siberia's exploding craters". BBC.
  5. Katie Hunt (17 February 2021). "Mysteries of massive holes forming in Siberian permafrost unlocked by scientists". CNN.
  6. Gates, Sara (16 July 2014). "Giant hole forms in Siberia, and nobody can explain why". HuffPost. Retrieved 28 December 2014.
  7. "Воронка на Ямале признана криовулканом — National Geographic Россия" (in Russian). Nat-geo.ru. Archived from the original on 2019-01-28. Retrieved 2019-02-13.
  8. Bogoyavlensky, Vasily (October 2015). "Gas Blowouts on the Yamal and Gydan Peninsulas" (PDF). GEO ExPro. Vol. 12, no. 5. GEO Publishing Ltd. pp. 74–78. ISSN   1744-8743 . Retrieved 27 July 2016.
  9. Sergey N. Buldovicz; Vanda Z. Khilimonyuk; Andrey Y. Bychkov; Evgeny N. Ospennikov; Sergey A. Vorobyev; Aleksey Y. Gunar; Evgeny I. Gorshkov; Evgeny M. Chuvilin; Maria Y. Cherbunina; Pavel I. Kotov; Natalia V. Lubnina; Rimma G. Motenko; Ruslan M. Amanzhurov (10 September 2018). "Cryovolcanism on the Earth: Origin of a Spectacular Crater in the Yamal Peninsula (Russia)". Scientific Reports. 8 (13534). doi:10.1038/s41598-018-31858-9. ISSN   2045-2322. PMC   6131154 . Archived from the original on 2018-09-13.
  10. Buldovicz et al. 2018.