Plate Motion Examples at Ian Dorothy blog

Plate Motion Examples. Plate motions can be tracked using global positioning system (gps) data from different locations on earth’s surface. Plates can interact in three ways: Plates move as rigid bodies, so it may seem surprising that the north american plate can be moving at different rates in different places. The eurasian plate rotates clockwise. The eurasian plate rotates clockwise. Rates of motions of the major plates range from less than 1 cm/y to more than 10 cm/y. The explanation is that plates rotate as they move; Boundaries between the plates are of three types: The pacific plate is the fastest, moving at more than 10 cm/y in some areas, followed by the australian and nazca plates. They can move apart (divergent boundary), they can move towards each other (convergent boundary), or they can slide past each other (transform boundary). The following sections will examine each of these types of plate boundaries, and the geological features they create.

Theory of Plate Tectonics CK12 Foundation
from www.ck12.org

Boundaries between the plates are of three types: The pacific plate is the fastest, moving at more than 10 cm/y in some areas, followed by the australian and nazca plates. Rates of motions of the major plates range from less than 1 cm/y to more than 10 cm/y. The eurasian plate rotates clockwise. The explanation is that plates rotate as they move; The eurasian plate rotates clockwise. The following sections will examine each of these types of plate boundaries, and the geological features they create. They can move apart (divergent boundary), they can move towards each other (convergent boundary), or they can slide past each other (transform boundary). Plate motions can be tracked using global positioning system (gps) data from different locations on earth’s surface. Plates can interact in three ways:

Theory of Plate Tectonics CK12 Foundation

Plate Motion Examples The following sections will examine each of these types of plate boundaries, and the geological features they create. Plate motions can be tracked using global positioning system (gps) data from different locations on earth’s surface. The eurasian plate rotates clockwise. Rates of motions of the major plates range from less than 1 cm/y to more than 10 cm/y. The following sections will examine each of these types of plate boundaries, and the geological features they create. Boundaries between the plates are of three types: They can move apart (divergent boundary), they can move towards each other (convergent boundary), or they can slide past each other (transform boundary). The pacific plate is the fastest, moving at more than 10 cm/y in some areas, followed by the australian and nazca plates. Plates can interact in three ways: Plates move as rigid bodies, so it may seem surprising that the north american plate can be moving at different rates in different places. The explanation is that plates rotate as they move; The eurasian plate rotates clockwise.

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