Active faults are structure along which we expect displacement to occur. By definition, since a shallow earthquake is a process that produces displacement across a fault, all shallow earthquakes occur on active faults. Inactive faults are structures that we can identify, but which do no have earthquakes.
because sound travels fastest through solids or this is because molecules in a solid medium are much closer together than those in a liquid or gas, allowing sound waves to travel more quickly through it. in fact, sound waves travel over 17 times faster through steel than through air.
Active faults are structure along which we expect displacement to occur. By definition, since a shallow earthquake is a process that produces displacement across a fault, all shallow earthquakes occur on active faults. Inactive faults are structures that we can identify, but which do no have earthquakes.
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because sound travels fastest through solids or this is because molecules in a solid medium are much closer together than those in a liquid or gas, allowing sound waves to travel more quickly through it. in fact, sound waves travel over 17 times faster through steel than through air.
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