Why Do Tectonic Plates Move At Different Speeds at Spencer Kelly blog

Why Do Tectonic Plates Move At Different Speeds. These are plate boundaries where two plates are either slipping past each other in opposite directions or at different rates in the same. Plate tectonics is driven by a variety of forces: At the “seams” where tectonic plates come in contact, the crustal rocks may grind violently against each other, causing earthquakes and volcano eruptions. 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. Dynamic movement in the mantle, dense oceanic crust interacting with the ductile asthenosphere, even the rotation of the planet. Tectonic plates move in different directions over long periods of time and friction causes them to get stuck. One big reason is that the movement of the plates causes the formation of volcanoes — basically, breaks in the crust that serve as vents. Tectonic plates are able to move because of the relative density of oceanic lithosphere and the relative weakness of the asthenosphere.

Tectonic Plates
from geologywithme.weebly.com

Dynamic movement in the mantle, dense oceanic crust interacting with the ductile asthenosphere, even the rotation of the planet. Tectonic plates move in different directions over long periods of time and friction causes them to get stuck. Tectonic plates are able to move because of the relative density of oceanic lithosphere and the relative weakness of the asthenosphere. Plate tectonics is driven by a variety of forces: At the “seams” where tectonic plates come in contact, the crustal rocks may grind violently against each other, causing earthquakes and volcano eruptions. 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 are plate boundaries where two plates are either slipping past each other in opposite directions or at different rates in the same. One big reason is that the movement of the plates causes the formation of volcanoes — basically, breaks in the crust that serve as vents.

Tectonic Plates

Why Do Tectonic Plates Move At Different Speeds Tectonic plates are able to move because of the relative density of oceanic lithosphere and the relative weakness of the asthenosphere. These are plate boundaries where two plates are either slipping past each other in opposite directions or at different rates in the same. One big reason is that the movement of the plates causes the formation of volcanoes — basically, breaks in the crust that serve as vents. At the “seams” where tectonic plates come in contact, the crustal rocks may grind violently against each other, causing earthquakes and volcano eruptions. 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. Tectonic plates move in different directions over long periods of time and friction causes them to get stuck. Dynamic movement in the mantle, dense oceanic crust interacting with the ductile asthenosphere, even the rotation of the planet. Tectonic plates are able to move because of the relative density of oceanic lithosphere and the relative weakness of the asthenosphere. Plate tectonics is driven by a variety of forces:

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