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This topic has appeared in the English Wikipedia rankings 1 time. It first appeared on 2026-07-17 and was most recently seen on 2026-07-17.
The Intermontane terranes were a group of volcanic island arcs that formed in the Panthalassa Ocean during the Triassic period. These terranes developed above subduction zones and were later accreted to the western margin of North America during the Jurassic. Offshore, a separate assemblage known as the Insular belt evolved independently. The ocean basin between the Intermontane terranes and the North American craton is known as the Slide Mountain Ocean, remnants of which are preserved in the Slide Mountain terrane. Some tectonic models suggest multiple, possibly parallel subduction systems, analogous in part to the modern Philippine Mobile Belt.
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