# the point of origin of an earthquake is called

the point of origin of an earthquake is called the epicenter. The geographic area where the ground shook violently (which caused the earthquake) is called the epicenter.

The time-frame of the earthquake is called the time. The most common cause of an earthquake is the time. The time-frame of the earthquake is called the time.

The most common cause of an earthquake is the time. The most common cause of an earthquake is the time. It’s not that bad. The point of origin is actually a good thing in this case. The point of origin of an earthquake is actually a good thing in this case.

A key point of origin is when the body of something is in a state of instability in the ground, so that the earth can have the opportunity to move and settle the body into its proper position. So all of those earthquakes happen at the “point of origin.” The point of origin of an earthquake is actually a good thing in this case. The point of origin of an earthquake is actually a good thing in this case.

The point of origin isn’t just when the body of something is in a state of instability in the earth, but when the earth is in a state of instability in the earth. This kind of earthquake happens when the earth is unstable in the earth, and then starts to move and settle the land. That’s why we had this earthquake during the day in the film that we watched today.

The point of origin is also an important concept in seismology, which is the study of the physical motions of the earth. The point of origin is one of the key concepts in seismology because the physical motion of an earthquake is the key to figuring out what caused it. The point of origin is also really important because if the earth is to be in a state of instability, then we should probably be pretty careful in earthquakes that happen.

Now that we’ve got a bit of an understanding of seismic mechanics, we can begin to understand where the Earth fits into the concept of earthquake.

The earth is a solid sphere. Seismic waves can travel in all directions and can be refracted. Because the earth is solid, we can assume that the seismic waves are propagating straight up. If the seismic waves are refracted, then they can be reflected to the surface of the earth. This is called a “seismic wave refraction zone.

This is just the wave refraction zone, so that’s the wave that causes a earthquake. If the wave refraction zone is a good approximation of the ground, there is a point where the seismic waves stop being refracted and start being refracted straight down. In this zone is the point of origin of an earthquake. The earthquake is called a subduction zone.