Subduction.
The kind of plate boundary where one lithospheric plate slides under another is a convergent boundary. This process is called subduction.
subduction boundary!!!
a divergent plate boundary.
The type of plate boundary where one plate slides past another is called a transform boundary. At these boundaries, the plates move horizontally relative to each other, typically causing friction and leading to earthquakes. An example of a transform boundary is the San Andreas Fault in California.
The type of boundary where one tectonic plate slides under another is called a convergent boundary. This process is known as subduction, where one plate is forced beneath the other due to differences in density.
transform boundary
A transform plate boundary forms where two plates slide past one another horizontally. This movement can cause earthquakes due to the friction and pressure buildup along the boundary. An example of this type of boundary is the San Andreas Fault in California.
subduction boundary!!!
It is called a divergent plate boundary.
There are 2 tectonics theories namely: divergent boundary and subduction zone. The boundary of the plate tectonics where two plates are placed is called divergent boundary while the subduction zone is a convergent boundary where in one plate is subducted on another.
Trenches are typically found at the boundaries of tectonic plates, where one plate is being subducted beneath another. The most well-known trenches are oceanic trenches, found underwater near subduction zones where one tectonic plate sinks beneath another.
The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.