It is a divergent boundary
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 Mid-Atlantic Ocean is a divergent plate boundary, where tectonic plates are moving away from each other. This movement creates new oceanic crust as magma rises from the mantle and solidifies at the mid-ocean ridge.
Constructive or divergent. The ridge formed is of basaltic rock type (though this is a generalisation), and is a source of volcanic activity. Iceland was formed as a result of the sea-floor spreading.
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 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.
Convergent
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
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.
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.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
The Mid-Atlantic Ocean is a divergent plate boundary, where tectonic plates are moving away from each other. This movement creates new oceanic crust as magma rises from the mantle and solidifies at the mid-ocean ridge.
A divergent plate boundary (ridge)
Constructive or divergent. The ridge formed is of basaltic rock type (though this is a generalisation), and is a source of volcanic activity. Iceland was formed as a result of the sea-floor spreading.
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 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 boundary plate is associated with a mid-ocean ridge. It is characterized by tectonic plates moving away from each other, creating new crust through sea-floor spreading.
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.