Walvis Ridge

The Walvis Ridge stretches some 3,000 km (1,900 mi) from the African continental shelf to the Tristan da Cunha hotspot, separating the Angola and Cape Basins.

The Walvis Ridge (walvis means whale in Dutch and Afrikaans) is an aseismic ocean ridge in the southern Atlantic Ocean. More than 3,000 km (1,900 mi) in length, it extends from the Mid-Atlantic Ridge, near Tristan da Cunha and the Gough Islands, to the African coast (at 18°S in northern Namibia).[1] The Walvis Ridge is one of few examples of a hotspot seamount chain that links a flood basalt province to an active hotspot. It is also considered one of the most important hotspot tracks because the Tristan Hotspot is one of few primary or deep mantle hotspots.[2]

  1. ^ Goslin et al. 1974, Introduction, p. 469
  2. ^ Sager 2014, pp. 2–5

Walvis Ridge

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