Slab Pull.
The process you're referring to is called subduction. Subduction occurs at convergent plate boundaries where one tectonic plate is forced beneath another plate. As the denser oceanic plate sinks into the asthenosphere, it creates a deep ocean trench on the seafloor.
The partially molten layer of the mantle is called the asthenosphere. This zone is partially molten and allows tectonic plates to move on top of it.
The weak upper portion of the mantle that behaves plastically is called the asthenosphere. It is located beneath the lithosphere and is responsible for the movement of tectonic plates due to its ability to flow slowly over geological time scales. The asthenosphere plays a key role in the process of plate tectonics.
The layer of tar-like mantle under the tectonic plates is called the asthenosphere. It is a partially molten and ductile region of the Earth's mantle that allows the lithospheric plates to move on top of it.
The uppermost part of the mantle with liquid and plastic properties is called the asthenosphere. It is a semi-fluid layer located beneath the rigid lithosphere that allows for the movement of tectonic plates.
Slab Pull.
Slab Pull.
The process is called subduction. Subduction occurs when one tectonic plate is forced underneath another plate and sinks into the asthenosphere due to gravity. This process is responsible for the formation of deep ocean trenches and volcanic arcs.
The soft layer of the mantle on which the tectonic plates move is called the asthenosphere. It is a semi-fluid layer beneath the lithosphere that allows for the movement of the tectonic plates due to convection currents in the mantle.
The soft layer of rock in the mantle is called the asthenosphere. It is partially molten and enables the movement of tectonic plates. This layer lies beneath the lithosphere and contributes to the process of plate tectonics.
The partially molten layer of Earth is called the asthenosphere. It is located beneath the lithosphere and is responsible for the movement of tectonic plates.
The lithosphere floats on a layer of the Earth's mantle called the asthenosphere. The asthenosphere is a semi-fluid layer beneath the lithosphere that allows the movement of tectonic plates.
The solid plastic layer of the mantle beneath the lithosphere is called the asthenosphere. It is characterized by its semi-fluid nature, allowing for the movement of tectonic plates over time. The asthenosphere plays a crucial role in the process of plate tectonics.
The process you're referring to is called subduction. Subduction occurs at convergent plate boundaries where one tectonic plate is forced beneath another plate. As the denser oceanic plate sinks into the asthenosphere, it creates a deep ocean trench on the seafloor.
The solid plastic layer of the mantle is called the asthenosphere. This region is partially molten and allows for the movement of tectonic plates.
The partially molten layer of the mantle is called the asthenosphere. This zone is partially molten and allows tectonic plates to move on top of it.
Slab Pull Force occurs when a denser oceanic plate is forced beneath a less dense continental plate or oceanic plate in a process called subduction. It's the force caused by suction of the cold dense lithosphere into the asthenosphere at destructive margins. Basically, because lithosphere is denser than asthenosphere, there is gravitational imbalance which is passed on to the crust. this causes the lithosphere to be sucked inwards at the oceanic trenches into deep asthenosphere.