mid ocean ridges
New ocean crust is formed at mid-ocean ridges where tectonic plates are diverging (spreading apart).
Ocean crust is formed at seafloor spreading centers. One example of this is the Mid-Atlantic ridge.
Ocean crust is formed by intrusive magma at mid-ocean-ridges. The magma cools and solidifies into peridotite, basalt, or gabbro.
Oceanic crust, formed mostly of mafic rocks, or sima, is found on the ocean floor.
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mid-ocean ridge
Mid-Ocean ridge
Geothermal activity has revealed new characteristics of Earth's crust near Lake Myvatn, Iceland. In places like Iceland, new research has shown volcanoes and hot springs forming as the result of activity between the crust and the mantle.
New oceanic crust is continually being created at the Mid-Ocean ridges.
The reason for this is that the ocean floor is ever changing and is never in the same possition due to current.
At the mid-ocean ridges.
The definition of ocean continental collision means the continental crust and the ocean's crust collide with one another. A subduction is formed when the collision occurs.