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 Bouvet Triple Junction The Bouvet Triple Junction is a geologic triple junction of three tectonic plates located on the seafloor of the South Atlantic Ocean. It is named after Bouvet Island, which lies 275 kilometers to the east. The three plates which meet here are the South American Plate, the African Plate, and the Antarctic Plate. The Bouvet Triple Junction is an R-R-R type, that is, the three plate boundaries which meet here are mid-ocean ridges: the Mid-Atlantic Ridge (MAR), the Southwest Indian Ridge (SWIR), and the South American-Antarctic Ridge (SAAR). There are two prominent transform valleys in the area: