Plate Tectonic Types at Linda Burk blog

Plate Tectonic Types. The earth’s lithosphere, which includes the crust and upper mantle, is made up of a series of pieces, or tectonic plates, that move slowly over time. Tectonic plates are composed of the continental and oceanic crust or lithosphere. There are seven major tectonic plates: Plates rip apart at a divergent plate boundary, causing volcanic activity and shallow earthquakes; The two plates move towards each other. A divergent boundary occurs when two tectonic plates. The two plates slip past each other. Continental crust is composed of granitic rocks made up of relatively lightweight minerals such as quartz and feldspar. At a convergent plate boundary, one. There are three types of tectonic plate boundaries: The type of plate boundary and the type of crust found on each side of the boundary determines what sort of geologic activity will be found there. In contrast, oceanic crust is composed of basaltic rocks, which are much denser and heavier.


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Continental crust is composed of granitic rocks made up of relatively lightweight minerals such as quartz and feldspar. There are three types of tectonic plate boundaries: The two plates move towards each other. At a convergent plate boundary, one. The type of plate boundary and the type of crust found on each side of the boundary determines what sort of geologic activity will be found there. Plates rip apart at a divergent plate boundary, causing volcanic activity and shallow earthquakes; A divergent boundary occurs when two tectonic plates. The two plates slip past each other. There are seven major tectonic plates: In contrast, oceanic crust is composed of basaltic rocks, which are much denser and heavier.

Plate Tectonic Types Tectonic plates are composed of the continental and oceanic crust or lithosphere. A divergent boundary occurs when two tectonic plates. The two plates move towards each other. In contrast, oceanic crust is composed of basaltic rocks, which are much denser and heavier. The earth’s lithosphere, which includes the crust and upper mantle, is made up of a series of pieces, or tectonic plates, that move slowly over time. There are three types of tectonic plate boundaries: Continental crust is composed of granitic rocks made up of relatively lightweight minerals such as quartz and feldspar. The type of plate boundary and the type of crust found on each side of the boundary determines what sort of geologic activity will be found there. There are seven major tectonic plates: The two plates slip past each other. Plates rip apart at a divergent plate boundary, causing volcanic activity and shallow earthquakes; Tectonic plates are composed of the continental and oceanic crust or lithosphere. At a convergent plate boundary, one.

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