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.
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.
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 real example of oceanic to oceanic divergent boundary is the Mid-Atlantic Ridge. This underwater mountain range runs along the floor of the Atlantic Ocean, where it separates the North American Plate from the Eurasian Plate to the east and the African Plate to the west. As the plates move apart, magma rises to the surface, creating new oceanic crust.
The Gakkel Ridge is located in the Arctic Ocean and is primarily bounded by the North American Plate to the west and the Eurasian Plate to the east. This mid-ocean ridge represents a divergent boundary where these two tectonic plates are moving apart, allowing magma to rise and create new oceanic crust. The region is characterized by volcanic activity and hydrothermal vent systems associated with the seafloor spreading process.
The East African Rift is on the African plate. However, it is the point where this plate is splitting into two. These are the Somali plate and the Nubian plate. For more information visit, https://sites.google.com/site/wikieasierpages/east-african-rift
Convergent plate boundary.
Mid-Atlantic Ridge and East Pacific Rise
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.
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.
The Ninety East ridge
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.
The Mid-Atlantic Ridge was formed by the divergent boundary between the North American Plate and Eurasian Plate (to the east) and the South American Plate and African Plate (to the west). As these plates move away from each other, magma rises to the surface, solidifies, and forms new oceanic crust, creating the ridge.
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 real example of oceanic to oceanic divergent boundary is the Mid-Atlantic Ridge. This underwater mountain range runs along the floor of the Atlantic Ocean, where it separates the North American Plate from the Eurasian Plate to the east and the African Plate to the west. As the plates move apart, magma rises to the surface, creating new oceanic crust.
The Gakkel Ridge is located in the Arctic Ocean and is primarily bounded by the North American Plate to the west and the Eurasian Plate to the east. This mid-ocean ridge represents a divergent boundary where these two tectonic plates are moving apart, allowing magma to rise and create new oceanic crust. The region is characterized by volcanic activity and hydrothermal vent systems associated with the seafloor spreading process.
Examples of a divergent boundary would be a mid-ocean ridge. Two plates are pulling apart from each other. If you have heard before, the magma from the asthenosphere find a way to get out through the crack of the diverging plates and makes new land. Another type of devergent boundary would be a fissure. It is a long linear crack made by the plates moving apart. I think maybe another one would probably be a volcano, but I am not sure.
The East African Rift is on the African plate. However, it is the point where this plate is splitting into two. These are the Somali plate and the Nubian plate. For more information visit, https://sites.google.com/site/wikieasierpages/east-african-rift