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Okinawa Trough

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Through Lithosphere

Description

It is a back-arc basin formed by extension within the continental lithosphere behind the far deeper Ryukyu Trench-arc system. The thickness of the crust in the northern Okinawa Trough is 30 km, thinning to 10 km in the southern Okinawa Trough. It has a large section more than 1,000 metres (3,300 ft) deep and a maximum depth of 2,716 metres (8,911 ft).

The Okinawa Trough still in an early stage of evolving from arc type to back-arc activity, and features volcanoes such as the Yonaguni Knoll IV.

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