destructive 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.
Divergent Boundary, (Constructive Boundary).
The Mid-Atlantic Ridge is formed where the Eurasian Plate and the North American Plate are diverging, creating a boundary known as a divergent plate boundary. As the plates move apart, magma rises from the mantle to fill the gap, creating new oceanic crust.
Actually, the North Atlantic Ocean is not a volcanic island but rather a basin created by the separation of the North American and Eurasian plates. The Mid-Atlantic Ridge runs along the center of the ocean, where new oceanic crust is formed by seafloor spreading. Volcanic islands can form further south along the ridge due to hot spots or other geological processes.
Divergent boundary
destructive plate boundary
Divergent boundary is formed
The mid-Atlantic ridge is a divergent boundary where tectonic plates are moving apart. It is an example of a constructive plate boundary where new oceanic crust is formed through volcanic activity. This process leads to the continuous separation of the North American and Eurasian plates on one side and the South American and African plates on the other side.
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, (Constructive Boundary).
The Mid-Atlantic Ridge is formed where the Eurasian Plate and the North American Plate are diverging, creating a boundary known as a divergent plate boundary. As the plates move apart, magma rises from the mantle to fill the gap, creating new oceanic crust.
Divergent Boundary :D
Actually, the North Atlantic Ocean is not a volcanic island but rather a basin created by the separation of the North American and Eurasian plates. The Mid-Atlantic Ridge runs along the center of the ocean, where new oceanic crust is formed by seafloor spreading. Volcanic islands can form further south along the ridge due to hot spots or other geological processes.
New crust is formed at a divergent boundary
It creates a divergent boundary.
spreading or divergent boundary