51Թ

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geosyncline

[ jee-oh-sin-klahyn ]

noun

Geology.
  1. a portion of the earth's crust subjected to downward warping during a large span of geologic time; a geosynclinal fold.


geosyncline

/ ˌːəʊˈɪŋɪ /

noun

  1. a broad elongated depression in the earth's crust containing great thicknesses of sediment
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

geosyncline

/ ŧ′ō-ĭī′ /

  1. A usually elongate, basinlike depression along the edge of a continent, in which a thick sequence of sediments and volcanic deposits has accumulated.
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Derived Forms

  • ˌDzˈԲ, adjective
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51Թ History and Origins

Origin of geosyncline1

First recorded in 1890–95; geo- + syncline
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Example Sentences

Examples have not been reviewed.

He said the pit is at the end of a geosyncline, a deposit of coal shaped like a canoe that stretched about two-thirds of a mile from bow to stern.

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The mountain range can only arise where the geosyncline is deeply filled by long ages of sedimentation.

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For long ages and through a succession of geological epochs, sedimentation had proceeded so that the accumulations of Palaeozoic and Mesozoic times had collected in the geosyncline formed by their own ever increasing weight.

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When yielding has begun in any geosyncline, and the materials are faulted and overthrust, there results a considerably increased thickness.

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Again, the ancient and modern volcanoes and earthquakes of Europe are associated with the geosyncline of the greater Mediterranean, the Tethys of Mesozoic times.

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