The Antarctic plate started tosubduct beneath South America 14 million years ago in theMiocene epoch. At first it subducted only in the southernmost tip ofPatagonia, meaning that theChile triple junction lay near theStrait of Magellan. As the southern part of theNazca plate and theChile Rise became consumed by subduction the more northerly regions of the Antarctic plate began to subduct beneath Patagonia so that the Chile triple junction lies at present in front ofTaitao Peninsula at 46°15' S.[5][6] The subduction of the Antarctic plate beneath South America is held to have upliftedPatagonia as it reduced the previously vigorous down-dragging flow in theEarth's mantle caused by the subduction of theNazca plate beneath Patagonia. Thedynamic topography caused by this uplift raisedQuaternary-agedmarine terraces and beaches across the Atlantic coast of Patagonia.[6]
^Jiang, Wei-Ping; E, Dong-Chen; Zhan, Bi-Wei; Liu, You-Wen (2009). "New Model of Antarctic plate Motion and Its Analysis".Chinese Journal of Geophysics.52 (1):23–32.doi:10.1002/cjg2.1323.ISSN2326-0440.