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.
Subduction.
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
When plate tectonics move up or down, it is referred to as vertical movement or vertical displacement. Upward movement can occur due to processes like uplift and volcanic activity, leading to the formation of mountains and volcanic landforms. Downward movement, on the other hand, can result in subduction zones where one tectonic plate is forced beneath another, causing the formation of trenches and sometimes leading to earthquakes and volcanic activity.
As the leading edge in forced down it is heated up and becomes part of the molten magma below.
It melts (and may float upward).
Subduction.
A destructive plate boundary.
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
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
When plate tectonics move up or down, it is referred to as vertical movement or vertical displacement. Upward movement can occur due to processes like uplift and volcanic activity, leading to the formation of mountains and volcanic landforms. Downward movement, on the other hand, can result in subduction zones where one tectonic plate is forced beneath another, causing the formation of trenches and sometimes leading to earthquakes and volcanic activity.
The Himalayas are still growing because the Indian plate continues to ram into the Eurasian Plate.
It is a process called ridge push.
In a convergent plate collision between continental and oceanic plates, the more dense oceanic plate would subduct, or move underneath, the less dense continental plate, eventually melting into the mantle at the leading edge.