Why Do Tectonic Plates Move Relative With One Another at Maddison Mcmasters blog

Why Do Tectonic Plates Move Relative With One Another. Tectonic plates move at varying speeds, typically ranging from a few to several centimeters per year, roughly comparable to the rate at which human fingernails grow. Lava flows at the surface cool rapidly to become basalt, but deeper in the crust, magma cools more slowly to form gabbro. Convergent, where plates move into one another; Divergent, where plates move apart; And transform, where plates move sideways in relation. These plates lie on top of a partially molten layer of rock called the asthenosphere. The movement of the plates creates three types of tectonic boundaries: As the lithospheric plates move across earth’s surface, driven by forces as yet not fully understood, they interact along their boundaries, diverging, converging, or slipping past each other. Due to the convection of the asthenosphere and lithosphere, the plates move relative to each other at different.

Plate Tectonics THE GEOGRAPHER ONLINE
from www.thegeographeronline.net

Due to the convection of the asthenosphere and lithosphere, the plates move relative to each other at different. Lava flows at the surface cool rapidly to become basalt, but deeper in the crust, magma cools more slowly to form gabbro. Convergent, where plates move into one another; These plates lie on top of a partially molten layer of rock called the asthenosphere. And transform, where plates move sideways in relation. Tectonic plates move at varying speeds, typically ranging from a few to several centimeters per year, roughly comparable to the rate at which human fingernails grow. Divergent, where plates move apart; As the lithospheric plates move across earth’s surface, driven by forces as yet not fully understood, they interact along their boundaries, diverging, converging, or slipping past each other. The movement of the plates creates three types of tectonic boundaries:

Plate Tectonics THE GEOGRAPHER ONLINE

Why Do Tectonic Plates Move Relative With One Another As the lithospheric plates move across earth’s surface, driven by forces as yet not fully understood, they interact along their boundaries, diverging, converging, or slipping past each other. Convergent, where plates move into one another; As the lithospheric plates move across earth’s surface, driven by forces as yet not fully understood, they interact along their boundaries, diverging, converging, or slipping past each other. The movement of the plates creates three types of tectonic boundaries: Divergent, where plates move apart; Due to the convection of the asthenosphere and lithosphere, the plates move relative to each other at different. And transform, where plates move sideways in relation. Tectonic plates move at varying speeds, typically ranging from a few to several centimeters per year, roughly comparable to the rate at which human fingernails grow. These plates lie on top of a partially molten layer of rock called the asthenosphere. Lava flows at the surface cool rapidly to become basalt, but deeper in the crust, magma cools more slowly to form gabbro.

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