Because after earthquakes, it is possible to see examples of displacement of the ground across faults.
Faults DO NOT produce earthquakes, faults are produced by earthquakes. This means that earthquake loci are centered on and along faults. The energy released by an earthquake is the strain energy built up as a result of plate tectonic forces. Some faults move easily and thus no strain energy builds up.
earthquakes are likely
Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occured.
I have the same question but its false it in my course 2 science textbook. I hope this helps and i dont know what forces plates along faults in earths lithosphere sorry!
because that's where the edges of the plates are and that's where it shifts
Earthquakes result when forces push plates along faults in the Earth's lithosphere. These plates are comprised of the crust and a portion of the upper mantle.
Faults DO NOT produce earthquakes, faults are produced by earthquakes. This means that earthquake loci are centered on and along faults. The energy released by an earthquake is the stress energy built up as a result of plate tectonic forces.
earthquakes
Faults DO NOT produce earthquakes, faults are produced by earthquakes. This means that earthquake loci are centered on and along faults. The energy released by an earthquake is the strain energy built up as a result of plate tectonic forces. Some faults move easily and thus no strain energy builds up.
earthquakes are likely
No. The influence of buildings and damns in this aspect is quite small. Earthquakes are the result of rock moving along faults.
Yes, seismic waves are the result of energy released by the movement of rocks along faults.
When a longer fault ruptures, you have movement along a longer section of the crust, and so more rock is moving.
Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occured.
Yes.
False. Earthquakes mostly occur along faults that are at or very near to plate boundaries.
There are a few ways this can happen. First, earthquakes are associated with movement along faults. This movement can alter the surface terrain. The shaking of an earthquake can also cause wet soil and sediment to behave like a liquid.