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Along the north-south axis of the fjord is the trace of an inactive great fault system known as the Lynn Canal Chatham Strait trough.
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Lateral grounding-zone wedges are identified at the northern and southern lateral margins of the Amundsen Gulf and M'Clure Strait troughs, respectively, and are interpreted to have been formed roughly contemporaneously by ice streams in Amundsen Gulf and M'Clure Strait.
After 2 Ma, crustal stretching in the Okinawa Trough deepened Tsushima Strait facilitating inflow during every successive interglacial.
By that time, Thad merged with a trough over the Tatar Strait.
These suggest that the East China Sea and the Japan Sea became more influenced by the Kuroshio and Tsushima currents, respectively, from 1.5 2.0 Ma onwards due to the stretching of the Okinawa Trough and the deepening of the Tsushima Strait.
It flows along the western part of the Okinawa Trough and leaves the continental slope via the Tokara Strait (Fig. 2) reaching the southern island of Japan at ~30 °N.
Influenced by a trough east of Asia, Irma began to re-curve into the Luzon Straits on November 25.
A trough mouth fan located on the continental shelf suggests that it extended along M'Clure Strait and was grounded at the shelf edge.
The TWC inflow was probably initiated by the opening of the southern strait and the migration of the Kuroshio water into the East China Sea, which almost coincided with the formation of the Okinawa Trough (Shinjo 1999).
Trough June 5.
"Detroit" simply means "strait".
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