Tristan hotspot
The Tristan hotspot is a volcanic hotspot which is responsible for the volcanic activity which forms the volcanoes in the southern Atlantic Ocean. It is thought to have formed the island of Tristan da Cunha and the Walvis Ridge on the African Plate. Geology. It is also believed to be closely connected with the Paraná and Etendeka flood basalt provinces, which formed over the hotspot during the opening of the South Atlantic Ocean. The Tristan and Gough hotspots are widely spaced end-members of the volcanic system that generated the Walvis Ridge on the African plate and the  Rio Grande Rise on the South American plate beginning at when the Paraná and Etendeka traps formed. Whether or not Tristan and Gough represent two distinct volcanic centers is still debated. The hotspots of the eastern South Atlantic formed along the plume generation zones (PGZs) of the African large low seismic velocity province (LLSVP). LLSVPs are dense and stable structures, and most of the plumes, kimberlites, and large igneous provinces (LIPs) on Earth can be rotated back to the PGZs. All major African LIPs (Karoo, Paraná-Etendeka, and Agulhas) formed at the PGZs of the African LLSVP but the Tristan -Gough hotspot was the only hotspot located at a spreading boundary and therefore the only African hotspot that started to form a volcanic trail. Palaeoclimatic and evolutionary role. Based on molecular estimates, found that the "Homo"-"Pan" divergence occurred (in contrast to earlier estimates that suggested around 5 Ma). Arnason et al. also estimated the "Platyrrhini"-"Catarrhini" divergence to have occurred around and found that the latter evolved in South America before their dispersal into Africa. Arnason et al. hypothesised that the Rio Grande-Walvis Ridge system was exposed above sea level and formed a chain of islands across the South Atlantic  during the Maastrichtian and Palaeocene allowing the primates to disperse across the ocean. Other researchers dismiss the hypothesis of Arnason et al. instead favouring a less spectacular rafting event. Other hints of transoceanic island hopping in the fossil record is "Lavocatavis", a flightless terror bird found in Eocene layers in Algeria, the only found outside South America.