Ocean trenches are associated with subduction zones, which are convergent plate boundaries.
A convergent boundary is formed when one tectonic plate descends beneath another. This process is known as subduction and typically leads to the formation of deep ocean trenches and volcanic arcs.
In an oceanic-continental convergent plate boundary, an oceanic plate is subducted beneath a continental plate due to differences in density. This process can lead to the formation of deep ocean trenches, volcanic arcs on the continental plate, and earthquakes. The subduction of the oceanic plate can also cause melting of rock, leading to the formation of magma that can erupt as volcanoes on the continental plate.
The plate boundary that causes mountains to form is called a convergent boundary.
A subduction zone is the plate boundary where old and heavy oceanic crust sinks into the mantle. At subduction zones, oceanic crust is forced beneath another tectonic plate, typically a continental plate, due to differences in density. This process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
The kind of plate boundary where one lithospheric plate slides under another is a convergent boundary. This process is called subduction.
subduction zone or continental plate
The Transform plate boundary commonly forms a chain of volcanoes - Professer Humifiken
The landforms that are formed at a transform boundary forms features such as fault lines and oceanic fracture zones. Fault lines are also known as strike slip faults. They produce powerful earthquakes.
A convergent boundary is formed when one tectonic plate descends beneath another. This process is known as subduction and typically leads to the formation of deep ocean trenches and volcanic arcs.
A plateau can form on a convergent plate boundary where two plates collide, causing uplift and compression of the crust. It can also form on a divergent plate boundary where two plates move apart, leading to the stretching and thinning of the crust, creating a high, flat landform.
Divergent Plate Boundary. (Seafloor Spreading).
a plate -.-
Oceanic lithosphere plunges beneath an overriding continental plate at a convergent boundary, specifically at a subduction zone. The denser oceanic plate is forced beneath the less dense continental plate due to tectonic forces, leading to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
In an oceanic-continental convergent plate boundary, an oceanic plate is subducted beneath a continental plate due to differences in density. This process can lead to the formation of deep ocean trenches, volcanic arcs on the continental plate, and earthquakes. The subduction of the oceanic plate can also cause melting of rock, leading to the formation of magma that can erupt as volcanoes on the continental plate.
The plate boundary that causes mountains to form is called a convergent boundary.
The kind of plate boundary that moves apart is a Divergent Plate Boundary
The 'South Island'. A collision boundary.