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Seafloor is created at divergent plate boundaries called the mid-ocean ridges.
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
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 divergent boundary created the mid-ocean ridge. At this boundary, tectonic plates are moving away from each other, allowing magma to rise and create new oceanic crust along the ridge.
destructive plate boundary
It is called a divergent plate boundary.
Its a divergent boundary
Seafloor is created at divergent plate boundaries called the mid-ocean ridges.
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
Divergent boundary
Divergent boundaries.
Divergent Boundary
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.
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.
divergent boundary
divergent
divergent