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
Bouvet Triple Junction Conrad transform and Bouvet transform. Conrad transform is named after . Bouvet Island is the highest point on the southern wall of the Bouvet transform. Up to 10 million years ago the Mid-Atlantic Ridge and the two deep transform valleys of Conrad and Bouvet met in one point. Thus the triple junction was of the ridge-fault-fault (RFF) type. Conrad transform, stretching to the west, connected the end of the Mid-Atlantic Ridge to the South American-Antarctic Ridge. Bouvet transform linked it to the Southwest Indian Ridge on the eastern side. Currently Conrad transform and Bouvet transform are no longer connected to