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What is most directly linked to heat convection within Earths interior?
tectonic plate motion
What is most directly linked to heat convection within Earths's interior?
tectonic plate motion
Are blizzards used as a evidence the the earths surface consist of plates that are in continuous motion?
No. Blizzards have nothing to do with plate tectonics.
What is the geological theory that pieces of earths crust are in constant slow motion is called?
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
What is the geological theory that states that pieces of earths crust are in constant slow motion is?
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
What is geological theory that states that pieces of earths crust are in constant slow motion called?
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
What is the geological theory that states the pieces of Earths crust are in constant slow motion called?
The movement of crustal or lithospheric plates is a part of the theory of plate tectonics. The geological theory is called plate tectonics.
What does plate mean like in science?
they are under the earths surface and cause earth Quakes
What is powered by from energy from earths interior?
Volcanoes
What type of plate motion crates a reverse fault?
The answer is by convergent plate motion.
What geological theory states that pieces of the Earth's lithosphere are in constant slow motion?
The geological theory that states that pieces of earths crust are in constant slow motion is called the Continental Drift Theory. This theory also considers Pangea, the way the continents were before the drift.
What is the theory that earths crust is in a slow motion?
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.
