convergent
The Mid-Atlantic Ridge separates the North American plate from the African plate. This ridge runs through the Atlantic Ocean and marks the boundary where the two plates are moving apart.
The southern half of the Mid-Atlantic Ridge separates the South American Plate from the African Plate.
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.
It separates the Eurasian Plate and North American Plate in the North Atlantic, and the African Plate from the South American Plate in the South Atlantic.
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.
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.
The boundary separating the African Plate from the Arabian Plate is a divergent boundary. This type of boundary occurs where tectonic plates move away from each other, leading to the formation of new crust. Specifically, this divergence is associated with the East African Rift system, which is characterized by rifting and volcanic activity as the plates move apart.
African Plate
The Mid-Atlantic Ridge separates the North American Plate and the Eurasian Plate in the northern segment, while it separates the South American Plate and the African Plate in the southern segment. This mid-ocean ridge is a divergent boundary where tectonic plates move apart, allowing magma to rise and create new oceanic crust.
Divergent Plate Boundary. (Seafloor Spreading).
African!
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.