Slab-pull is a tectonic process that occurs during subduction, where a denser oceanic plate sinks beneath a less dense continental or oceanic plate. As the subducting plate, or slab, descends into the mantle, it generates a pulling force due to its weight and the gravitational attraction of the colder, denser material. This force helps to drive the movement of tectonic plates, facilitating the subduction process and contributing to geological phenomena such as earthquakes and volcanic activity at convergent plate boundaries. Overall, slab-pull plays a crucial role in the dynamics of plate tectonics and the recycling of Earth's lithosphere.
Subduction
The plate tectonic process where one plate moves under another is called subduction. This process occurs at convergent plate boundaries, where the denser oceanic plate typically sinks beneath the less dense continental plate. Subduction zones are associated with deep oceanic trenches and volcanic arcs.
subduction boundary!!!
Earthquakes associated with convergent plate boundaries typically occur in the subduction zones where one tectonic plate is forced beneath another. These earthquakes are known as megathrust earthquakes and can have very high magnitudes due to the intense tectonic forces involved in the subduction process.
Convergent plate boundariesDestructive plate boundaries
A subduction zone forms when one tectonic plate moves beneath another plate. This happens because the denser oceanic plate sinks below the less dense continental plate. The key processes involved in the creation of a subduction zone include the convergence of tectonic plates, the sinking of the denser plate into the mantle, and the generation of earthquakes and volcanic activity along the subduction zone.
This process is known as subduction.
Subduction
The plate tectonic process where one plate moves under another is called subduction. This process occurs at convergent plate boundaries, where the denser oceanic plate typically sinks beneath the less dense continental plate. Subduction zones are associated with deep oceanic trenches and volcanic arcs.
subduction boundary!!!
Subduction is the process when one tectonic plate moves beneath another plate at a convergent boundary. This movement can lead to the recycling of old oceanic crust back into the mantle.
Subduction.
A subduction zone is formed when one tectonic plate is forced beneath another plate. This process occurs at convergent plate boundaries where two plates collide. The subducting plate is denser and heavier, causing it to sink into the mantle. This movement creates intense pressure and friction, leading to the formation of deep ocean trenches, volcanic arcs, and earthquakes. The geological processes involved in the creation of a subduction zone include plate tectonics, subduction, mantle convection, and volcanic activity.
Earthquakes associated with convergent plate boundaries typically occur in the subduction zones where one tectonic plate is forced beneath another. These earthquakes are known as megathrust earthquakes and can have very high magnitudes due to the intense tectonic forces involved in the subduction process.
Convergent plate boundariesDestructive plate boundaries
A subduction zone is where one plate is being subducted ( pulled down) under another plate, No it is not a plate boundary but it is were it happens. hope this helps
Subduction is the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate.