˜yÐÄvlog

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eugeosyncline

[ yoo-jee-oh-sing-klahyn, -sin- ]

noun

Geology.
  1. 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.


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Other ˜yÐÄvlog Forms

  • ±ð³Ü·²µ±ðo·²õ²â²Ô·³¦±ô¾±î€ƒn²¹±ô adjective
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˜yÐÄvlog History and Origins

Origin of eugeosyncline1

First recorded in 1940–45; eu- + geosyncline

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