Plate tectonics describes the motions of the 15 to 20 large rigid and brittle tectonicplates into ... It does a good job at explaining the distribution of most of Earth's earthquakes, mountains and other geological features, and a ... The North Americanplate is moving to the west-southwest at about 2.3 cm (~1 inch) per year
The plates move relative to each other in varying speeds. The Pacific plate moves against the North American plate at 5 cm/yr. The Arctic Ridge has the slowest rate at less than 2.5 cm/yr., while the East Pacific Rise has the fastest rate at more than 15 cm/yr.
over millions of years the plates have moved some what fast
i think it because of how fast the earthquake moves so people do not have time to go and watch the plates move!
Inches Per Year :-)
The North American plate is moving very slowly, only about one inch per year. Other tectonic plates are moving much faster; up to eight or nine inches per year.
The earth's plates move slowly because how big the earthquake is he bigger the amount the plates will move and the slower the earthquake is the less it moves.
The earth's plates move slowly because how big the earthquake is he bigger the amount the plates will move and the slower the earthquake is the less it moves.
This varies from plate to plate. Some move at about the speed your fingernails grow, some much faster.
The earth's plates move slowly because how big the earthquake is he bigger the amount the plates will move and the slower the earthquake is the less it moves.
4 seconds
plates move around the speed of how fast your nails grow
About 15 cm.
I would say that two of the plates were sliding past each other, got stuck, and slipped past each other so fast that it caused pressure rising to the surface, and caused an earthquake.
Capacitance is directly proportional to the area of the plates divided by the distance between the two plates. The farther away the plates are the lower capacitance will be. A capacitor stores energy in the electric field between the two plates. If those plates are very far apart, the field gets crappy real fast.
pretty fast
The plates move relative to each other in varying speeds. The Pacific plate moves against the North American plate at 5 cm/yr. The Arctic Ridge has the slowest rate at less than 2.5 cm/yr., while the East Pacific Rise has the fastest rate at more than 15 cm/yr.
lithosperic plates move fast why do you think we cant see it happining?