A fissure is a long, narrow crack opening along the surface of Earth. The term is derived from the Latin word fissura, which means 'cleft' or 'crack'. Fissures emerge in Earth's crust, on ice sheets and glaciers, and on volcanoes.
Ground fissure
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A ground fissure, also called an earth fissure, is a long, narrow crack or linear opening in the Earth's crust. Ground fissures can form naturally, such as from tectonic faulting and earthquakes, or as a consequence of human activity, such as oil mining and groundwater pumping.[2][3] Once formed, ground fissures can be extended and eroded by torrential rain.[4] They can be hazardous to people and livestock living on the affected surfaces and damaging to property and infrastructure, such as roads, underground pipes, canals, and dams.[2][5][6][7]
In circumstances where there is the extensive withdrawal of groundwater, the earth above the water table can subside causing fissures to form at the surface.[8][9] This typically occurs at the floor of arid valleys having rock formations and compacted soils with a high percentage of fine-grained material.[7][5]
Crevasse
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A crevasse, also called an ice fissure, is a deep linear crack in an ice sheet or glacier resulting from the opposing force produced by their movement at different rates of speed. The force builds until their associated shear stress is sufficient to break the ice along the faces. The breakage often forms vertical or near-vertical walls, which can melt and create seracs, arches, and other ice formations.[10] A crevasse may be as deep as 45 m (148 ft) and as wide as 20 m (66 ft).[11] A crevasse may be covered, but not necessarily filled, by a snow bridge made of the previous years' accumulation and snow drifts. The result is that crevasses are rendered invisible, and extremely dangerous to anyone attempting to traverse a glacier.[12]
Types of crevasses
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Fissure vent
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A fissure vent, also known as a volcanic fissure or eruption fissure, is a long volcanic vent through which lava erupts. Fissure vents are connected to deep magma reservoirs and are typically found in and along rifts and rift zones.[14] They are commonly associated with shield volcanoes. Over time fissure vents form spatter cones and can feed lava channels and lava tubes.[15]
Karst terrain
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Karst terrain or simply karst are vast regions of barren land with rocky ground and generally consisting of nearby caves, fissured ground, and sinkholes. Although these regions normally have moderate to heavy rainfall, they are noticeably devoid of vegetation and characteristically have no lakes, rivers, or streams on their surface. They form when large to massive veins of soluble aggregate like limestone, gypsum, or dolomite are excavated by underground torrents of flowing water.[16][17]
Karst aquifers
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In the United States, about 40% of the groundwater used for drinking comes from karst aquifers.[18] Some of these areas are well known vacation destinations like Carlsbad Caverns and Mammoth Cave. Karst aquifers are a vital resource in the US; about 20 percent of the land surface in the US is classified as karst. Other parts of the world with large areas of karst include the Caribbean, China, and Australia.
Typical karst hydrogeology consists of a network of interconnected fissures, fractures, and conduits emplaced within permeable rock. Most of the groundwater flow occurs through a network of openings, while groundwater is held in storage within the geological structures themselves.
See also
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edit- ^ "Volcano Watch — A recap of the Kamoamoa fissure eruption on its third anniversary". www.usgs.gov. Retrieved 25 September 2021.
- ^ a b Yang, Chengshen; Lu, Zhong; Zhang, Qin; Zhao, Chaoying; Peng, Jianbing; Ji, Lingyun (May 2018), "Deformation at longyao ground fissure and its surroundings, north China plain, revealed by ALOS PALSAR PS-InSAR" (PDF), International Journal of Applied Earth Observation and Geoinformation, 67: 1, Bibcode:2018IJAEO..67....1Y, doi:10.1016/j.jag.2017.12.010
- ^ Berkeley, UC. "The Mystery about Earthquake Fissures". seismo.berkeley.edu.
- ^ Carlson, Grace; Carnes, Lorraine K.; Cook, Joseph P. (4 September 2019). "Exploring Arizona earth fissures: An anthropogenic geologic hazard". Geologic Excursions in Southwestern North America. doi:10.1130/2019.0055(04). ISBN 978-0-8137-5655-4. Retrieved 24 September 2021.
- ^ a b "Earth Fissures, Subsidence & Karst in Arizona". AZGS. 12 July 2017. Retrieved 21 September 2021.
- ^ "USGS: Volcano Hazards Program Glossary - Fissure". volcanoes.usgs.gov. Retrieved 21 September 2021.
- ^ a b Star, Tony Davis Arizona Daily. "Record Pinal County fissure shows Arizona is still prone to shifting earth levels". Arizona Daily Star. Retrieved 22 September 2021.
- ^ Lund, W.R.; DuRoss, C.B.; Kirby, S.M.; McDonald, G.N.; Hunt, G.; Vice, G.S. (2005). The Origin and Extent of Earth Fissures in Escalante Valley, Southern Escalante Desert, Iron County, Utah. Special Study. Utah Geological Survey. ISBN 978-1-55791-730-0. Retrieved 21 September 2021.[page needed]
- ^ Inkenbrandt, P.; Lund, W.; Lowe, M.; Knudsen, T.; Bowman, S. (2014). Investigation of land subsidence and earth fissures in Cedar Valley, Iron County, Utah. Special Study. Utah Geological Survey. ISBN 978-1-55791-891-8. Retrieved 21 September 2021.[page needed]
- ^ van der Veen, C (1990). "Crevasses on Glaciers". Polar Geography. 23 (3): 213–245. doi:10.1080/10889379909377677.
- ^ Crevasse by National Geographic
- ^ Dodds, Klaus (24 October 2017). "Fissure". Society for Cultural Anthropology. Retrieved 26 September 2021.
- ^ a b Holdsworth, G (October 1956). "Primary Transverse Crevasses". Journal of Glaciology. 8 (52): 107–129. doi:10.1017/S0022143000020797.
- ^ "Geology glossary". www.volcanodiscovery.com. Retrieved 25 September 2001.
- ^ "How Volcanoes Work". sci.sdsu.edu. Archived from the original on 28 February 2018. Retrieved 26 September 2021.
- ^ "Karst | geology". Encyclopedia Britannica. Retrieved 26 September 2021.
- ^ "Karst Aquifers: Colorado Plateau Karst". www.usgs.gov. Retrieved 26 September 2021.
- ^ "Karst Aquifers". www.usgs.gov. Retrieved 27 September 2021.