Bouvet Island 247 years after its discovery. The Norwegian Polar Institute established a research station, made of shipping containers, at Nyrøysa in 1996. On 23 February 2006, the island experienced a magnitude 6.2 earthquake whose epicentre was about away, weakening the station's foundation and causing it to be blown to sea during a winter storm. In 2014, a new research station was sent from Tromsø in Norway, via Cape Town, to Bouvet. The new station is designed to house six people for periods of two to four months. In the mid-1980s, Bouvetøya, Jan Mayen, and Svalbard were considered as locations for the
Agulhas Bank nearly two-thirds of present-day South Africa. Basaltic lavas were extruded 183 Mya to form the Karoo large igneous province; a volcanism caused by the Bouvet hotspot which is linked to the Gondwana break-up. The Bouvet hotspot was located in or near present-day South Africa from the late Triassic 220 mya and until the Africa-Antarctica breakup 120 mya. The Bouvet hotspot track stretches south-east from the African continent, near the South Africa-Mozambique border, and east of the AFFZ down to Bouvet Island/Bouvet Triple Junction in the South Atlantic. 100 Mya, the region where the triple junction was located passed over the