Definitions
from The American Heritage® Dictionary of the English Language, 5th Edition.
- noun A usually elongate, basinlike depression along the edge of a continent, in which a thick sequence of sediments and volcanic deposits has accumulated.
from The Century Dictionary.
- noun In geology, a considerable tract in which the strata are bent into a great trough with many minor undulations on the flanks.
from Wiktionary, Creative Commons Attribution/Share-Alike License.
- noun geology A large, linear
depression in theEarth 'scrust in whichsediment accumulates.
Etymologies
from Wiktionary, Creative Commons Attribution/Share-Alike License
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Examples
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The park's principal geomorphic feature is the north-east to south-east geosyncline which is surrounded by raised folds and high mountains.
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"geosyncline," a vast trough, or cradle, being slowly filled with sediment brought down by the rivers from the adjoining shores.
Time and Change John Burroughs 1879
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Well, where it faltered was at the edge of a geosyncline, the orogenesis is much later than this area.
Cattle Town 2010
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This ecoregion is relatively young, perhaps less than 10,000 years old, and developed in a great geosyncline between the Guiana Plateau and the Andes Range.
Llanos 2007
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Well, where it faltered was at the edge of a geosyncline, the orogenesis is much later than this area.
Dinosaur Planet McCaffrey, Anne 1978
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"Evidently then," continued the professor, "the atoll is simply an annular terminal moraine of detritus shed alluvially into the sea, thus leaving a geosyncline of volcanic ash embedded with an occasional trilobite and the fragments of scoria, upon which we now stand."
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Mesozoic times had collected in the geosyncline formed by their own ever increasing weight.
The Birth-Time of the World and Other Scientific Essays John Joly 1895
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Again, the ancient and modern volcanoes and earthquakes of Europe are associated with the geosyncline of the greater Mediterranean, the
The Birth-Time of the World and Other Scientific Essays John Joly 1895
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When yielding has begun in any geosyncline, and the materials are faulted and overthrust, there results a considerably increased thickness.
The Birth-Time of the World and Other Scientific Essays John Joly 1895
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Now, let us suppose, in the trough of the geosyncline, and upon the top of the normal layer, a deposit of, say, 10 kilometres (6.2 miles) of sediments is formed during a long period of continental denudation.
The Birth-Time of the World and Other Scientific Essays John Joly 1895
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