isostasy
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English
[edit]Etymology
[edit]From iso- + Ancient Greek στάσις (stásis, “a standing”).
Pronunciation
[edit]Noun
[edit]isostasy (usually uncountable, plural isostasies)
- (geology) The state of balance or pressure equilibrium thought to exist within the Earth's crust, whereby the upper lithosphere floats on denser magma beneath.
- 2003, Bill Bryson, A Short History of Nearly Everything, BCA, page 155:
- The process of vertical movement, known as isostasy, was a foundation of geological belief for generations, though no-one had any really good theories as to how or why it happened.
- 2004, Richard Fortey, The Earth, Folio Society, published 2011, page 173:
- A great thickness of comparatively light sedimentary rocks accumulating in a geosyncline would ultimately ‘rebound’ because of isostasy – like a depressed rubber duck bouncing back upwards in a bath.
- 2022, Thomas Halliday, Otherlands, Penguin, published 2023, page 247:
- When a continent carries an ice sheet, the weight of that sheet distorts the equilibrium, the isostasy that causes the crust to float as it does.
Derived terms
[edit]Related terms
[edit]Translations
[edit]the state of balance of the Earth's lithosphere floating on the magma
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