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 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
The boundary of the Nazca Plate along the East Pacific Rise is a divergent boundary because it is where tectonic plates move apart, allowing magma to rise and create new oceanic crust. This process of seafloor spreading occurs as the Nazca Plate moves away from the Pacific Plate, leading to the formation of new material at the mid-ocean ridge. In contrast, convergent boundaries involve plates moving toward each other, typically leading to subduction or mountain building, which is not the case at the East Pacific Rise.
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.
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
Sort of. It is in the East African Rift. This is not formally recognized as a plate boundary, but can be considered a divergent plate boundary in its early stages.