convergent boundary. cuz it is ridge
The southeast Indian Ridge is a divergent plate boundary, where two tectonic plates are moving away from each other. This movement causes magma to rise from the mantle, creating new crust as the plates separate.
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 mid-ocean ridge is a divergent plate boundary where tectonic plates are moving away from each other. As the plates separate, magma rises to the surface, creating new oceanic crust.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust. A classic example is the Mid-Atlantic Ridge where the Eurasian and African Plates are moving away from the North and South American Plates.
The African plate is mainly surrounded by divergent plate boundaries, such as the Mid-Atlantic Ridge in the Atlantic Ocean and the East African Rift. It also has a convergent boundary with the Eurasian plate in the north and the Antarctic plate in the south.
A divergent plate boundary (ridge)
Convergent
The southeast Indian Ridge is a divergent plate boundary, where two tectonic plates are moving away from each other. This movement causes magma to rise from the mantle, creating new crust as the plates separate.
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 mid-ocean ridge is a divergent plate boundary where tectonic plates are moving away from each other. As the plates separate, magma rises to the surface, creating new oceanic crust.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
Iceland is situated on a divergent plate boundary known as the Mid Atlantic Ridge. Please see the related links.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust. A classic example is the Mid-Atlantic Ridge where the Eurasian and African Plates are moving away from the North and South American Plates.
The East Pacific Rise is a divergent plate boundary where tectonic plates are moving apart. This boundary is associated with seafloor spreading and the creation of new oceanic crust.
A divergent plate boundary creates a mid-ocean ridge. This occurs when two tectonic plates move away from each other, leading to the upwelling of magma from the mantle, creating new oceanic crust at the mid-ocean ridge.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
The Mid-Atlantic Ridge is a divergent boundary where tectonic plates are moving away from each other. It is primarily associated with constructive plate margins where new crust is being created through seafloor spreading.