Plate Tectonics.
The crust is in large, irregular plates shuffling around by new rock extruded from the upper Mantle in ocean plate boundaries, balanced by the loss of the fringes of the ocean-floor plates to subduction.
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
The very slow motion of huge blocks of the Earth's crust is referred to as plate tectonics. This movement is driven by the heat generated from within the Earth, causing the tectonic plates to gradually shift and interact with one another, leading to various geological phenomena such as earthquakes, volcanic eruptions, and mountain building.
the speed of the earths plates are very slow, and sometimes they don't move at all. if the earths plates were constantly moving (allot) then we would not be able to build cities because of constant earthquakes.
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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.
Convection currents.
ask google
"Continental Drift" and "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.
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.
Slow and constant.