5 centimeters per year
About 3 cent. a year About 3 cent. a year About 3 cent. a year About 3 cent. a year
GPC is the way to measure the movements of the tectonic plates in centimeters...
Torterras strongest move is earthquakeme and my freind beat the league with torrteras earthquake not true torterra's best move is leaf storm
cathode - emits electrons which will become the beamcontrol grid - adjustment of beam current and thus brightness on screenfocus grids - focusing beam to sharp point on screen to form small dotx plates - deflect beam left/righty plates - deflect beam up/downanode - aquadag coating (baked on graphite applied in water suspension) on the inside of the CRT's cone, both accelerates the beam and collects the electrons that rebound from the screenNote: the grids in a CRT are different from the grids in ordinary vacuum tubes: in a CRT the grids are just round holes in metal disks that surround the beam, in ordinary vacuum tubes the grids are actual wire grids in the direct path of electron flow.
Why do searts appear to move westward across the sky?
Aesthenosphere
They constantly move. EDIT: Lithospheric plates move only about a few centimeters a year. Hope this helps! ~SLL
Yes.
Continental Plates
5 centimeters.
Lower mantle is the surface on which the lithospheric plates move around earths surface.
5 centimeters.
there is convection in the mantle. it causes the plates to move.
bruh
Lithospheric plates move constantly at a very slow rate, typically around a few centimeters per year. This movement is driven by the slow convection currents in the Earth's mantle, causing the plates to either diverge, converge, or slide past each other at plate boundaries.
No, tidal drift is caused by the gravitational pull of the Moon and Sun on Earth's oceans, and it does not directly cause the movement of lithospheric plates. The movement of lithospheric plates is driven by the convection currents in the mantle beneath the Earth's crust.
When an earthquake occurs, lithospheric plates either slide past each other, collide, or move apart along their boundaries. The stress accumulated along the plate boundaries is released suddenly, causing the plates to deform and generate seismic waves that we feel as an earthquake.