Agulhas Passage

The Agulhas Passage is an abyssal channel located south of South Africa between the Agulhas Bank and Agulhas Plateau. About 50 km (31 mi) wide, it connects the Natal Valley and Transkei Basin in the north to the Agulhas Basin in the south and is the only near-shore connection between the south-western Indian Ocean and South Atlantic Ocean.

The formation of the Agulhas Passage was initiated by the Gondwana break-up some 160 million years ago (Ma) and the rifting of the Somali and Mozambique Basins, an event associated with the formation of the ocean floor in the Weddell Sea 147 Ma.

Between the Agulhas Bank and the Agulhas Passage the boundary between the Earth's crust and the mantle (the Moho) ascend from 25 to 14 km (15.5 to 8.7 mi) over 50 km (31 mi) which is normal for a continent-ocean boundary. The crustal thickness under the Agulhas Passage varies from 6 to 10 km (3.7 to 6.2 mi) which is equally normal for oceanic crust. It is possible, however, that volcanic flows from the Agulhas Plateau large igneous province (LIP) added crustal material to the Agulhas Passage (which is 160-120 Ma) during the LIP formation (100-80 Ma) and that the crust under the passage was originally thinner.

The sedimentary layers are very thin in the western Agulhas Passage, in places only 8 m (26 ft). In the central parts of the passage, in contrast, they can reach 1,300 m (4,300 ft) and form sediment drifts. The southern part is affected by thinning and erosion.

The Agulhas Current, the western boundary current of the Indian Ocean, flows south through the Natal Valley, Transkei Basin, and Agulhas Passage into the south-east Atlantic Ocean where it retroflects back into the Indian Ocean as the Agulhas Return Current. In the Indian Ocean, the Agulhas Current is dissipated into a gyre which finally brings parts of the water mass back to the Natal Valley.

...
Wikipedia