A geosyncline is a part of the earth's crust that is prone to
downward warping during a long span of geologic time. It is a large
depression that contains very thick deposits.
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a very large depression on the earths surface, like trough,
which contains mounds of sedimentary and volcanic rocks.
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Dwight Eugene Mayo has written:
'The development of the idea of the geosyncline' -- subject(s):
Geosynclines
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A geosyncline is a belt of sedimentary deposits that accumulate
within the ocean along the margin of a continent - on the
continental shelf and slope.