Near subduction zones, plates collide,
forcing ocean crust down toward Earth's hot interior, where this crustal material melts, forming magma that rises buoyantly back to the surface and erupts to create volcanoes and seamounts.
Not exact matches
Samples collected from the
ocean floor reveal how the mantle's convective
forces shape the earth's surface, create its
crust and perhaps even affect its rotation
Titanic
forces in the Earth's
crust explain why the abundance and richness of corals varies dramatically across the vast expanse of the Indian and Pacific
Oceans, a world - first s...
This
forcing would not produce the extreme Venus - like baked -
crust greenhouse state, which can not be reached until the
ocean is lost to space.