Divergent boundary.
the boundary ofthemid ocean ridge is a divergent boundary
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
The Atlantic-Indian Ridge is a divergent plate boundary. This means that the tectonic plates along this ridge are moving away from each other, allowing magma to well up and create new oceanic crust between the plates.
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 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.
The Mid-Atlanic Ridge is the divergent boundary that is responsible for seafloor spreading. Consisting mostly of divergent boundaries, with transform faults as well, this is the site where new oceanic crust is added, increasing the size of the ocean. This location is dotted with underwater volcanoes as igneous basaltic magma is added to fill in the gap left as the oceanic plates drift away.
Convergent plate boundary.
Iceland is a volcanic island on the midatlantic ridge, separating the North American Plate to the west from the European Plate to the east.
A divergent plate boundary.
the boundary ofthemid ocean ridge is a divergent boundary
MidAtlantic Airways ended in 2006.
MidAtlantic Airways was created in 2002.
The Mid-Atlantic Ridge is a divergent plate boundary, also known as a spreading center.
It's a divergent plate boundary.
Divergent boundary
A divergent plate boundary (ridge)
mid-ocean ridge