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eugeosynclinal

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eu⋅ge⋅o⋅syn⋅cline

[yoo-jee-oh-sing-klahyn, -sin-]
–noun Geology.
a former marine zone, bordering an ocean basin, marked by very thick deposits of sediment in which the products of volcanic activity are associated with clastic sediments.

Origin:
1940–45; eu- + geosyncline


eu⋅ge⋅o⋅syn⋅cli⋅nal, adjective
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Based on the Random House Dictionary, © Random House, Inc. 2009.
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