The first sort of plate boundary is called a divergent boundary, or spreading center. At these boundaries, two plates move away from one another. As the two move apart, mid-ocean ridges are created as magma from the mantle up wells through a crack in the oceanic crust and cools. This, in turn, causes the growth of oceanic crust on either side of the vents. As the plates continue to move, and more crust is formed, the ocean basin expands and a ridge system is created. Divergent boundaries are responsible in part for driving the motion of the plates.
Magma is generated along the convergent plate boundaries as slab sinks into the mantle and, the increased temperature and pressure drives volatiles from the oceanic crust. These mobile fluids migrate upward into the wedge-shaped piece of mantle located between the sub ducting slab and overriding plate. Once the sinking slab reaches a depth of 100 km, these water rich fluids reduce the melting point of hot mantle rock sufficiently triggering some melting. And these partial melting of the mantle is what generates magma.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
At a divergent plate boundary the crust is thin. This reduces pressure on the upper mantle, lowering the melting point and allowing some rock to melt.
At divergent boundary, the crust is thin hence reduces the pressure on the upper mantle therefore lowering the melting point and allowing some rock to melt.
As an oceanic plate sinks into the mantle at a convergent boundary it causes rocks to melt. Some of the newly formed magma will migrate upward to volcanoes, that have formed along the convergent boundaries, and erupt.
convergent plate boundary
Convergent Boundaries.
A Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.
Mount Etna Was Formed By Destructive Plate Boundaries. This Is When One Crust Is Forced Under Another Crust. It Stands At The Convergent Boundary Where The African Crust Is Being Sub Ducted Beneath The Eurasian Crust. This Causes The Latter To Deform And Forces the Magma Up Into Weak Spots In The Earths Crust (mount Etna) When There Has Become To Much Of A Magma Build Up In The Mantle.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
As an oceanic plate sinks into the mantle at a convergent boundary it causes rocks to melt. Some of the newly formed magma will migrate upward to volcanoes, that have formed along the convergent boundaries, and erupt.
Convergent Boundaries.
convergent plate boundary
Convergent boundary Convergent boundary
Convergent Boundaries.
A Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.