Far-field stresses triggered by portions of the northern boundary stress the African plate. Intraplate stresses are the driving forces in the South American plate
Ghana is located on the African tectonic plate. It is situated on the western part of the plate, near the boundary with the South American plate.
The North American and Eurasian Plates in the North Atlantic and the South American and African Plates in the South Atlantic border the Mid-Atlantic Ridge.
The Mid-Atlantic Ridge is not actually a tectonic plate, but a divergent boundary between plates where new oceanic crust is being created on the floor of the Atlantic Ocean. To the north, it marks the boundary between the Eurasian Plate and the North American Plate. To the south, it separates the African Plate from the South American Plate.
It forms a convergent boundary with the South American Plate, divergent.
The tectonic plate that pushes on the eastern edge of the South American Plate is the African Plate. The boundary where the two plates meet is known as the South American-African Plate boundary, which is a transform boundary where the plates slide past each other horizontally. This boundary is responsible for the formation of the East African Rift Zone.
convergent
Far-field stresses triggered by portions of the northern boundary stress the African plate. Intraplate stresses are the driving forces in the South American plate
Ghana is located on the African tectonic plate. It is situated on the western part of the plate, near the boundary with the South American plate.
The North American and Eurasian Plates in the North Atlantic and the South American and African Plates in the South Atlantic border the Mid-Atlantic Ridge.
The Antarctic plate is directly south of the African plate. It is a divergent boundary.
The plates that correspond to the Mid-Atlantic Ridge are the North American Plate, Eurasian Plate, South American Plate, African Plate, and Antarctic Plate. The ridge runs down the center of the Atlantic Ocean, marking the boundary between the Eurasian Plate and North American Plate to the east, and the South American Plate and African Plate to the west.
A convergent plate boundary occurs between the Nazca Plate and the South American Plate. The Nazca Plate is subducting beneath the South American Plate, leading to the formation of the Andes mountain range.
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
It is a convergent/destructive plate boundary.
A constructive plate margin or spreading centre known as the Mid-Atlantic-Ridge.
The South American Plate and the Nazca Plate are separated by a convergent boundary, specifically a subduction zone. This is where the Nazca Plate is forced under the South American Plate, creating the Andes mountain range and causing volcanic activity.