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There are three major types of rock: igneous, sedimentary, and metamorphic.
The remnants of this plate on the surface of the Earth are the Juan de Fuca Plate and Explorer Plate, both in the northwestern United States and southwestern Canada, and the Cocos Plate on the west coast of Mexico.
More recently, seismologists have been able to create detailed images of wave speeds inside the earth in the same way a doctor images a body in a CT scan.
These images have led to a much more detailed view of the interior of the Earth, and have replaced the simplified layered model with a much more dynamic model.
Early advances in this field showed the existence of a liquid outer core (where shear waves were not able to propagate) and a dense solid inner core.
These advances led to the development of a layered model of the Earth, with a crust and lithosphere on top, the mantle below (separated within itself by seismic discontinuities at 410 and 660 kilometers), and the outer core and inner core below that.
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) is an earth science concerned with the solid Earth, the rocks of which it is composed, and the processes by which they change over time.