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 Earth's crust becomes denser, it typically moves downward into the mantle in a process known as subduction. This occurs at convergent plate boundaries, where an oceanic plate subducts beneath a continental plate or another oceanic plate. The denser oceanic crust sinks into the mantle, leading to geological phenomena such as earthquakes and volcanic activity.
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.
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
As the leading edge in forced down it is heated up and becomes part of the molten magma below.
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.
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.
As the Earth's crust becomes denser, it typically moves downward into the mantle in a process known as subduction. This occurs at convergent plate boundaries, where an oceanic plate subducts beneath a continental plate or another oceanic plate. The denser oceanic crust sinks into the mantle, leading to geological phenomena such as earthquakes and volcanic activity.
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
Yes, the Cascade Mountains are still growing today. The movement of the Juan de Fuca tectonic plate under the North American plate continues to push up the mountains, leading to ongoing uplift and volcanic activity in the region.
When a plate is pushed under an adjacent plate, the process is called subduction. The subducted crust melts into the core and is recycled. When the plate goes into the mantel it is heated to very high temperatures and turns into metamorphic rock.