It is mostly surrounded by the Antarctic Plate, the western border being a subduction zone.

The same holds for the African, Eurasian, and Antarctic plates.

This event was followed by low-angle extensional faulting along the East Antarctic plate.

The Antarctic plate movement is estimated at least 1 centimeter/per year towards the Atlantic Ocean.

It separates the African Plate to the north from the Antarctic Plate to the south.

The Phoenix Plate began subducting under the Antarctic Plate.

A major decrease in spreading rate, and the convergence rate with the Antarctic Plate occurred around 52.3 Ma.

The plateau was built by volcanic eruptions associated with the Kerguelen hotspot, and now lies on the Antarctic plate.

Likewise the African, Eurasian and Antarctic Plates.

The relative motion between the Scotia plate and the Antarctic plate on the western boundary is roughly 13 mm/yr.

During the Late Cretaceous exhumation, the Antarctic plate was extended east and west due to low-angle faulting.

The southerly side is a complex boundary with the Antarctic Plate and the Scotia Plate.

The arc has formed due to subduction of the Antarctic Plate under the South American Plate.

The Southern edge of the plate is bordered by the Antarctic plate forming the South Scotia Ridge.

The Antarctic Plate is a tectonic plate containing the continent of Antarctica and extending outward under the surrounding oceans.

It was an intraplate earthquake, as it occurred about 1000 km north of the (constructive) boundary between the Indo-Australian and Antarctic plates.

The Bellingshausen Plate was an ancient tectonic plate that fused onto the Antarctic Plate.

The three plates which meet here are the South American Plate, the African Plate, and the Antarctic Plate.

The trenchward migration of the spreading center is attributed to the subduction of the Phoenix Plate under the Antarctic Plate.

The granites were formed later as the Australian Plate collided with the Antarctic Plate 1160 million years ago as molten rock rose to the surface.

Surrounded by 2 major and 3 minor plates, its tectonic location is generally reflective of the relative motion between the Antarctic plate and the South American plate.

The Western edge of the plate is bounded by the Antarctic plate, forming the Shackleton Fracture zone and the Southern Chile trench.

The rift is simply a mid-ocean ridge where seafloor spreading occurs and drives part of the West Antarctic plate into the stronger East Antarctic craton.

It formed as a result of subduction of the Nazca Plate and Antarctic Plate underneath the South American Plate.

A change in motion between the South American plate and the Antarctic plate would have severe effects, causing seafloor spreading and the formation of the Scotia plate.

The Antarctic plate is roughly 60,900,000 square kilometers.

It is mostly surrounded by the Antarctic Plate, the western border being a subduction zone.

The Antarctic plate movement is estimated at least 1 centimeter/per year towards the Atlantic Ocean.

It separates the African Plate to the north from the Antarctic Plate to the south.

A major decrease in spreading rate, and the convergence rate with the Antarctic Plate occurred around 52.3 Ma.

During the Late Cretaceous exhumation, the Antarctic plate was extended east and west due to low-angle faulting.

The relative motion between the Scotia plate and the Antarctic plate on the western boundary is roughly 13 mm/yr.

The Phoenix Plate began subducting under the Antarctic Plate.

The southerly side is a complex boundary with the Antarctic Plate and the Scotia Plate.

The plateau was built by volcanic eruptions associated with the Kerguelen hotspot, and now lies on the Antarctic plate.

The arc has formed due to subduction of the Antarctic Plate under the South American Plate.

The Southern edge of the plate is bordered by the Antarctic plate forming the South Scotia Ridge.

The Antarctic Plate is a tectonic plate containing the continent of Antarctica and extending outward under the surrounding oceans.

The Bellingshausen Plate was an ancient tectonic plate that fused onto the Antarctic Plate.

The three plates which meet here are the South American Plate, the African Plate, and the Antarctic Plate.

The granites were formed later as the Australian Plate collided with the Antarctic Plate 1160 million years ago as molten rock rose to the surface.

The trenchward migration of the spreading center is attributed to the subduction of the Phoenix Plate under the Antarctic Plate.

Surrounded by 2 major and 3 minor plates, its tectonic location is generally reflective of the relative motion between the Antarctic plate and the South American plate.

The Western edge of the plate is bounded by the Antarctic plate, forming the Shackleton Fracture zone and the Southern Chile trench.

A change in motion between the South American plate and the Antarctic plate would have severe effects, causing seafloor spreading and the formation of the Scotia plate.

The West Antarctic Rift is located just west of the Transantarctic Mountains, and is considered to be the largest influence in driving the Antarctic plate motion.

The American-Antarctic Ridge (AAR) is a tectonic spreading center between the South American Plate and the Antarctic Plate.

The Rodrigues Triple Point is a R-R-R triple junction in the southern Indian Ocean, where the African, the Indo-Australian and the Antarctic Plates meet.

The Isthmus of Ofqui lies close to the Chile Triple Junction where the Nazca Plate, the South American Plate, and the Antarctic Plate meets.

Marine geophysical data indicates that motion between the South American plate and the Antarctic plate shifted from N-S to WNW-ESE accompanied by an eightfold increase in the separation rate.