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Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates.
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All three types may melt again, and when this happens, new magma is formed, from which an igneous rock may once more solidify.
To study all three types of rock, geologists evaluate the minerals of which they are composed.
The rock cycle illustrates the relationships among them (see diagram).
When a rock solidifies or crystallizes from melt (magma or lava), it is an igneous rock.
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.