Continents are made of continental lithosphere. Continents are composed of rocks that are more buoyant their than denser oceanic counterparts. These lighter rocks float on top of the asthenosphere, which is denser. This balance is maintained due to the fact that lighter substances will raise and rest on heavier substances, such as the asthenophere
Continental crust does not subduct because it is less dense than oceanic crust so it rides higher up on the mantle than the oceanic crust. So the oceanic crust which rides lower on the mantle due to isostacy sinks or subducts under the continental crust. thanks for listening or reading lol
subduction zones
A subduction zone at a convergent plate boundary. Undersea trenches are formed where the oceanic plate subducts, and volcanism and earthquakes may result from the partial melting and downward movement of the subducting crust.
subduction zone
Subduction zone
Movement of the plates takes rock and sediment into different geologic spaces. Convergence and subduction zones push some rock up, while dragging other rock down. This causes changes in the mineral component.
Partly because continental crust is less dense and more buoyant than oceanic crust, so it won't sink down subduction zones, and partly because it's much thicker than oceanic crust and buckles in plate collisions rather than subducts.
Subduction Zones.
subduction zones
Subduction Zones.
Subduction Zones.
A subduction zone is a place at the margin of a continent where the neighbouring oceanic plate is 'subducted'. That is, the oceanic plate, moving toward the continental plate, goes down into the mantle because it is heavier than the continental plate. Subduction zones typically cause deep ocean trenches.
A subduction zone at a convergent plate boundary. Undersea trenches are formed where the oceanic plate subducts, and volcanism and earthquakes may result from the partial melting and downward movement of the subducting crust.
Subduction zones are locations where crustal plates are being forced down into the mantle below other crustal plates. These movements are not uniform, but instead occur in discrete events. This is because friction causes the plates to lock in position until the stress exceeds the shear strength of the fault zone. This accumulation of stress causes deformations in the rock mass around the locked fault which is suddenly released when the fault slips.
Subduction is when one of the plates is forced down beneath the other plate at the convergent boundary.
subduction, which is when one tectonic plate is pushed down beneath another tectonic plate.
Subduction Zone
subduction zone