The movement of crustal or lithospheric plates is a part of the theory of 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.
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.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
Plate Tectonics
The geological theory that states that pieces of Earth's crust are in constant slow motion is called plate tectonics. This theory explains how the Earth's lithosphere is divided into plates that move and interact with each other, leading to phenomena such as earthquakes, volcanic activity, and mountain building.
Slow and constant.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics.
This is the theory of plate tectonics. It states that Earth's lithosphere is divided into several plates, which move and interact with each other on the underlying semi-fluid asthenosphere due to the convection currents in the mantle. This movement causes various geological phenomena like earthquakes, volcanic eruptions, and mountain building.
The plates of the lithosphere are in constant slow motion due to convection currents in the Earth's mantle. Heat from the Earth's core causes magma to rise, cool, and sink, creating a circular motion that moves the plates. This process is known as plate tectonics.
The theory of plate tectonics states that pieces of the Earth's lithosphere, called tectonic plates, are in constant slow motion, driven by processes such as seafloor spreading, subduction, and continental drift. These movements can result in events like earthquakes, volcanic eruptions, and mountain formation.
Plate Tectonics