The edge of the plate will heat up and become part of the molten mantle.
As the leading edge in forced down it is heated up and becomes part of the molten magma below.
The downward movement of a lithospheric plate into the asthenosphere is known as subduction. This process occurs at convergent plate boundaries where one plate is forced beneath another due to differences in density. Subduction can result in the formation of deep oceanic trenches and volcanic activity.
with a cross-section photo of the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate
Volcanoes are common on this type of plate boundary
The edge of the plate will heat up and become part of the molten mantle.
As the leading edge in forced down it is heated up and becomes part of the molten magma below.
As the leading edge of an oceanic plate continues to move downward into the mantle at a subduction zone, it will experience increased pressure and temperature. This can lead to the release of water and other volatiles, causing melting in the overlying mantle and potentially generating magma. Over time, this process can contribute to volcanic activity and the formation of volcanic arcs. Additionally, the descending plate may also undergo metamorphism and contribute to complex geological formations.
The leading edge of a plate can subduct beneath another plate or slide past it along a transform boundary as it continues to move downward. This process can generate earthquakes, volcanic activity, and the formation of mountain ranges at convergent boundaries, while at transform boundaries, it can create fault lines and seismic activity.
Allegheny Ludlum makes continuous mill plate steel
It appears to be continuous because it is a cycle. Old plate is subducted, but new plates are formed.
The downward movement of a lithospheric plate into the asthenosphere is known as subduction. This process occurs at convergent plate boundaries where one plate is forced beneath another due to differences in density. Subduction can result in the formation of deep oceanic trenches and volcanic activity.
A tetonic plate can ram into another plate and shift downward underneath the other plate. This causes a subduction zone and moutains, for example the Himalayas or the Andes
A convergent plate boundary is caused by a downward convection current in the mantle. At these boundaries, tectonic plates move towards each other, resulting in subduction zones or collision zones, where one plate is forced beneath the other.
Metamorphic rock i think?
Volcanoes are common on this type of plate boundary
with a cross-section photo of the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate