Slab pull is the force which is caused by the sinking of the cold, dense lithosphere into the mantle. It is considered as one of the two major driving forces for the movements of tectonic plates.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
In a subduction zone, the dense, cold oceanic plate collides with the lighter, warmer continental plate and is forced down underneath it into the mantle. The motion is downwards and the force is called "slab pull".
When tectonic plates overlap, it is called a subduction zone. This is where one plate is forced beneath the other due to their relative densities, creating intense geologic activity such as earthquakes and volcanic eruptions.
Fault lines
slab pull
Slab pull is the force which is caused by the sinking of the cold, dense lithosphere into the mantle. It is considered as one of the two major driving forces for the movements of tectonic plates.
Ridge-push and slab-pull are two mechanisms driving plate motion. Ridge-push is the process where the weight of newly formed lithosphere at mid-ocean ridges pushes older, colder plate material away, driving plate motion. Slab-pull, on the other hand, occurs at subduction zones where the dense oceanic lithosphere sinks into the mantle, pulling the rest of the plate along with it. Both mechanisms contribute to the overall movement of tectonic plates on Earth's surface.
Plate Tectonics
Plate Tectonics
The answer is by convergent plate motion.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
In a subduction zone, the dense, cold oceanic plate collides with the lighter, warmer continental plate and is forced down underneath it into the mantle. The motion is downwards and the force is called "slab pull".
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
Describe the three types of plate motion and the faults that are characteristic of each type of motion.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.