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.
ask google
"Continental Drift" and "Plate Tectonics".
Slow and constant.
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.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
If it is constant change in motion, it is acceleration.
Plate tectonics.
Slow and constant.
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.