geosynclinal

/ˌdʒioʊsɪnˈklaɪnəl/
adjective
  1. Relating to a large, long, deep depression in the Earth's crust where thick layers of sediment accumulate, often associated with mountain building.
    • Geologists study geosynclinal deposits to understand ancient tectonic activity.
    • Geosynclinal basins can hold thousands of meters of sediment over millions of years.
    • The geosynclinal theory helped explain the formation of many mountain ranges.
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