A divergent plate boundary.
Iceland is a volcanic island on the midatlantic ridge, separating the North American Plate to the west from the European Plate to the east.
Convergent plate boundary.
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
The Mid-Atlantic Ridge is a divergent plate boundary, also known as a spreading center.
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.
it corresponds to the south american, african, north american, and eurasian plates
It's a divergent plate boundary.
A divergent plate boundary (ridge)
The North American-Eurasian Plate boundary.
An example of a divergent plate boundary is the Mid-Atlantic Ridge, where the Eurasian Plate and North American Plate are moving apart. An example of a transform plate boundary is the San Andreas Fault in California, where the Pacific Plate and North American Plate are sliding past each other horizontally.
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 Southwest Indian Ridge is a divergent plate boundary, where the African Plate and the Indo-Australian Plate are moving away from each other. This boundary is characterized by the formation of new oceanic crust as magma rises to the surface, creating mid-ocean ridges. The ridge is part of the global mid-ocean ridge system that runs through the world's oceans.