The plate tectonic theory states that new Earth crust is being formed while old crust descends back into the mantle. Uneven heating in the mantle causes convection which keeps the crust in motion. The constant movement of Earth's plates are the result of the three types of boundaries, divergent, convergent, and transform, and the convection in the mantle.
The theory states that piecesof Earth's lithosphere are in slow, constant motion, driven by convection currents in the mantle. It explains the formation, movement, and subduction of Earth's plates.
Tectonic. Teutonic means Germanic. As for the implied question, not my best area, sorry.
The theory of plate tectonics replaced the theory of sea floor spreading.
Techtonic plate movement, weathering and degradation and human intervention (farming, civilisation).
the crust cracks and magma fills in the space
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.
theory of plate tectonics
When the Continental Drift Theory applies; when two plates either collide, smash, or slide to move plate techtonics.
Ur mummas plate
energy from plate techtonic
The Himalayan mountain range was created by the collision of the Indian Plate with the Eurasian Plate. This collision caused the Earth's crust to fold and uplift, leading to the formation of the towering Himalayas.
because it is a type of techtonic plates
It's a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates that move slowly over the underlying mantle.
A volcanic 'hot spot' in the pacific techtonic plate.
San Andreas
its the techtonic plates. one plate slides over the other which = trust from action
Techtonic plates move under the earth moving land and water.
more techtonic plate coliding in California
The techtonic plates are shifting. One plate is being overlaped by the other.