its because the plates
its because the plates
asthenosphere
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.
Those are called TECTONIC PLATES.
Tectonic plates from the Earth's lithosphere move slowly over the soft layer of the mantle, known as the asthenosphere. The movement of these plates is responsible for various geological processes, including earthquakes, volcanic eruptions, and the formation of mountains.
Pieces of lithosphere move slowly over the asthenosphere, which is a soft layer of the mantle. The asthenosphere is ductile and can flow, allowing for the movement of tectonic plates over time. This movement is responsible for phenomena like plate tectonics and continental drift.
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.
Soft layer of the Mantle in which tectonic plates move.
The plasticlike layer of Earth is the asthenosphere. It is a zone of the upper mantle where rock is soft and capable of gradual flow. The lithospheric plates float and move on top of the asthenosphere, contributing to the movement of tectonic plates.
The soft layer of rock in the mantle is called the asthenosphere. It is located beneath the lithosphere and consists of partially molten rock that allows for the movement of tectonic plates.
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 soft layer of the upper mantle is known as the asthenosphere. It is located just below the lithosphere and is characterized by its ability to flow slowly over time, allowing tectonic plates to move and interact on Earth's surface. This layer plays a crucial role in plate tectonics and the movement of the Earth's crust.