isostasy wikipedia - EAS
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Isostasy (Greek ísos "equal", stásis "standstill") or isostatic equilibrium is the state of gravitational equilibrium between Earth's crust (or lithosphere) and mantle such that the crust "floats" at an elevation that depends on its thickness and density. This concept is invoked to explain how different … See more
In the 18th century, French geodesists attempted to determine the shape of the Earth (the geoid) by measuring the length of a degree of latitude at different latitudes (arc measurement). A party working in Ecuador was … See more
• Archimedes' principle – Buoyancy principle in fluid dynamics
• William Bowie (engineer) – American geodetic engineer
• Lau, Gotland – District of the island of Gotland, Sweden See more• Oldham, Richard Dixon (1922). "Isostasy" . Encyclopædia Britannica (12th ed.). See more
The depth of compensation (also known as the compensation level, compensation depth, or level of compensation) is the depth below which … See more
Deposition and erosion
When large amounts of sediment are deposited on a particular region, the immense weight of the new sediment may cause the crust below to sink. Similarly, when large amounts of material are eroded away from a … See more• Lisitzin, Eugenie (1974). Sea-level changes. Amsterdam: Elsevier Scientific Pub. Co. ISBN 9780080870441. Retrieved 23 March 2022. See more
Wikipedia text under CC-BY-SA license - https://en.wikipedia.org/wiki/Talk:Isostasy
- Isostatic effects of plate tectonics is quite clear and consistent with the other headings. Isostasy and plate tectonics as a heading would have important historical connotations not covered in the section. Vsmith 03:11, 16 August 2005 (UTC)Reply[reply] "A second significant cause of eustatic sea level rise is thermal expansion of sea water, when t...
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- https://en.wiktionary.org/wiki/isostasy
Webisostasy (usually uncountable, plural isostasies) The state of balance or pressure equilibrium thought to exist within the Earth's crust, whereby the upper lithosphere floats …
- https://id.wikipedia.org/wiki/Isostasi
Isostasi (Bahasa Yunani ísos "sama", stásis "berhenti") atau keseimbangan isostatik adalah keadaan di mana keseimbangan gravitasi antara kerak bumi (atau litosfer) dan mantel secara sedemikian rupa. Sehingga kerak bumi dapat mengapung pada ketinggian tertentu dengan bergantung pada ketebalan dan kepadatannya. Konsep ini menjelaskan bagaimana ketinggian topografi yang berbeda dapat muncul di permukaan bumi. Meskipun awalnya didefinisikan dala…
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- https://commons.wikimedia.org/wiki/Category:Isostasy
WebCategory:Isostasy. From Wikimedia Commons, the free media repository. Italiano: Isostasia. ·. geodynamics. subfield of geophysics dealing with dynamics of the Earth. …
- https://wiki.tfes.org/Isostasy
WebIsostasy is a concept in the Geology invoked to explain why the Earth's structures do not behave in accordance to Gravity, which states that greater mass should have greater …
- https://commons.wikimedia.org/wiki/File:Isostasy.svg
WebFile:Isostasy.svg. From Wikimedia Commons, the free media repository. File. File history. File usage on Commons. File usage on other wikis. Metadata. Size of this PNG preview …
- https://ja.wikipedia.org/wiki/アイソスタシー
Webアイソスタシー ( 英: isostasy )とは、比較的軽い 地殻 が、重く流動性のある 上部マントル に浮かんでおり、地殻の 荷重 と地殻に働く 浮力 がつり合っているとする説、ま …
Isostasy - Wikipedia @ WordDisk
https://www.worddisk.com/wiki/IsostasyWebIsostasy (Greek ísos "equal", stásis "standstill") or isostatic equilibrium is the state of gravitational equilibrium between Earth's crust (or lithosphere) and mantle such that the …
- https://pt.wikipedia.org/wiki/Isostasia
WebIsostasia, ou movimento isostático, é o termo utilizado em Geologia para se referir ao estado de equilíbrio gravitacional, e as suas alterações, entre a litosfera e a astenosfera …
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