It is a divergent plate boundary.
The Atlantic-Indian Ridge is a divergent plate boundary. This means that the tectonic plates along this ridge are moving away from each other, allowing magma to well up and create new oceanic crust between the plates.
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.
The Ninety East Ridge is primarily associated with a divergent plate boundary. It is an underwater ridge located in the Indian Ocean, where the Indian Plate is moving away from the surrounding plates, leading to the formation of new oceanic crust. This tectonic activity is a result of the upwelling of magma from the mantle, which creates the ridge.
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
Another ridge similar to the Mid-Atlantic Ridge can be found in the Indian Ocean, known as the Southwest Indian Ridge. It is a divergent boundary where the African Plate and the Antarctic Plate are moving apart. This ridge, like the Mid-Atlantic Ridge, is associated with volcanic activity and the creation of new oceanic crust.
Convergent
The Atlantic-Indian Ridge is a divergent plate boundary. This means that the tectonic plates along this ridge are moving away from each other, allowing magma to well up and create new oceanic crust between the plates.
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.
The Ninety East Ridge is primarily associated with a divergent plate boundary. It is an underwater ridge located in the Indian Ocean, where the Indian Plate is moving away from the surrounding plates, leading to the formation of new oceanic crust. This tectonic activity is a result of the upwelling of magma from the mantle, which creates the ridge.
A divergent plate boundary.
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.
Another ridge similar to the Mid-Atlantic Ridge can be found in the Indian Ocean, known as the Southwest Indian Ridge. It is a divergent boundary where the African Plate and the Antarctic Plate are moving apart. This ridge, like the Mid-Atlantic Ridge, is associated with volcanic activity and the creation of new oceanic crust.
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's a divergent plate boundary.
A divergent plate boundary (ridge)