Английская Википедия:Columnar jointing
Шаблон:Short description Шаблон:Use dmy dates Шаблон:See also
Columnar jointing is a geological structure where sets of intersecting closely spaced fractures, referred to as joints, result in the formation of a regular array of polygonal prisms, or columns. Columnar jointing occurs in many types of igneous rocks and forms as the rock cools and contracts. Columnar jointing can occur in cooling lava flows and ashflow tuffs (ignimbrites), as well as in some shallow intrusions.[1] Columnar jointing also occurs rarely in sedimentary rocks, due to a combination of dissolution and reprecipitation of interstitial minerals (often quartz or cryptocrystalline silica) by hot, hydrothermal fluids and the expansion and contraction of the rock unit, both resulting from the presence of a nearby magmatic intrusion.[2]
The columns can vary from 3 meters to a few centimeters in diameter, and can be as much as 30 meters tall.[1] They are typically parallel and straight, but can also be curved and vary in diameter.[1] An array of regular, straight, and larger-diameter columns is called a colonnade; an irregular, less-straight, and smaller-diameter array is termed an entablature.[3] The number of sides of the individual columns can vary from 3 to 8, with 6 sides being the most common.[1]
formation
Places
Some famous locations in the United States where columnar jointing can be found are Devils Tower in Wyoming, Devils Postpile in California and the Columbia River flood basalts in Oregon, Washington and Idaho. Other famous places include the Giant's Causeway in Northern Ireland and Fingal's Cave on the island of Staffa, Scotland.[4]
Devils Tower
Devils Tower in Wyoming in the United States is about 40 million years old and Шаблон:Convert high.[1] Geologists agree that the rock forming Devils Tower solidified from an intrusion, but it has not been established whether the magma from this intrusion ever reached the surface. Most columns are 6-sided, but 4, 5, and 7-sided ones can also be found.[5]
Giant's Causeway
Шаблон:Main article The Giant's Causeway (Irish: Clochán An Aifir) on the north Antrim coast of Northern Ireland was created by volcanic activity 60 million years ago, and consists of over 40,000 columns.[1][6] According to a legend, the giant Finn McCool created the Giant's Causeway, as a causeway to Scotland.[7]
Sōunkyō Gorge
Шаблон:Main article Sōunkyō Gorge, a part of the town of Kamikawa, Hokkaido, Japan, features a Шаблон:Convert stretch of columnar jointing, which is the result of an eruption of the Daisetsuzan Volcanic Group 30,000 years ago.
Deccan Traps
Шаблон:Main article The late Cretaceous Deccan Traps of India constitute one of the largest volcanic provinces of Earth, and examples of columnar jointing can be found in St. Mary's Island in the state of Karnataka.[8]
High Island Reservoir
Formed in Cretaceous, the columnar rocks are found around the reservoir and the islands nearby in Sai Kung, Hong Kong. It is special that the rocks are not mafic, but felsic tuff instead.
Makhtesh Ramon
The columnar jointed sandstone of the HaMinsara (Carpentry Shop) in the makhtesh (erosion cirque) of Makhtesh Ramon, Negev desert, Israel.
Cerro Kõi
There are several examples of columnar jointed sandstones in the greater Asunción region of Paraguay. The best known is Cerro Kõi in Areguá, but there are also several quarries in Luque.
Mars
Шаблон:Main article Several exposures of columnar jointing have been discovered on the planet Mars by the High Resolution Imaging Science Experiment (HiRISE) camera, which is carried by the Mars Reconnaissance Orbiter (MRO).[9][10]
Sawn Rocks
Sawn Rocks, in Mount Kaputar National Park close to Narrabri, New South Wales, Australia, features 40 meters of columnar jointing above the creek and 30 meters below the surface.[11]
Basaltic Prisms of Santa María Regla
Шаблон:Main article Alexander von Humboldt documented the prisms located in Huasca de Ocampo, in the Mexican state of Hidalgo.
Columnar basalt of Tawau (Batu Bersusun)
At Kampung Balung Cocos, Tawau, Malaysia, the river flows through the area of columnar basalt. One section is seen vertically high on river bank. The rest lies on river bank. The water flows from the lowest area forming waterfall.
Gorge of Garni, Armenia
The Garni Gorge is situated 23 km east of Yerevan, Armenia, just below the village of the same name. This portion of the Garni Gorge is typically referred to as the "Symphony of the Stones." On a promontory above the gorge the first-century AD Temple of Garni may be seen.
See also
References
- ↑ 1,0 1,1 1,2 1,3 1,4 1,5 Oregon State University > Volcano World > ... > Columnar Jointing. Accessed 29 December 2013.
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ southernhebrides.com > Staffa - A Geological Marvel. Accessed 29 December 2013.
- ↑ U.S. National Park Service > Devils Tower > Geologic Formations. Accessed 29 December 2013.
- ↑ National Trust > Giant's Causeway. Accessed 29 December 2013.
- ↑ Northern Ireland Tourist Board > Causeway Coast & Glens > The Giant's Causeway > Folklore and Legend Шаблон:Webarchive. Accessed 29 December 2013.
- ↑ Geological Survey of India > Columnar Basalt Retrieved 17 April 2020.
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite journal
- ↑ Sawn Rocks walking track, Mount Kaputar National Park NSW National Parks and Wildlife Service. Retrieved 3 January 2019.
External links
- Aydin, A., and J. Zhong (nda) Columnar Joints, Multiple Joint Sets, Rock Fracture Knolwedgebase, Stanford University, Stanford, California.
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