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The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping
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.
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.
A mid-ocean ridge forms at a divergent boundary when two oceanic plates move apart. This boundary is characterized by the upwelling of magma from the mantle, which solidifies to create new oceanic crust. This process results in the formation of a continuous underwater mountain range.
A mid-ocean ridge is formed in a divergent boundary where two tectonic plates move away from each other. Magma rises to fill the gap created by the plates moving apart, creating new oceanic crust. This process results in a continuous mountain range on the ocean floor.
The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.
rift
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Sea-Floor Spreading is your answer.
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping
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.
at a divergent plate boundary
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.
oceanic crest and volcano.