Well, the origin of the earthquake is called the focus, and the point on the ground directly above the focus is called the epicenter. In CA, earthquakes generally originate from the San Andreas Fault.
An earthquake's Focus is located directly under the Epicenter of an earthquake. The Epicenterof an earthquake is located on the surface of the earthquake.
If you want to know what the name is, it is called the epicenter. If you want to know a location where all earthquakes originate, there isn't one. Earthquakes can occur along faultlines, or in the middle of a continent.
earthquake
The Chile Earthquake in February was the biggest earthquake reported in 2010.
where the fault is at or the epicenter which is not where the earthquake starts it is the focus where the earthquake starts
In geological terms, it is the point below the Earth's surface where seismic waves originate during an earthquake.
Many tidal waves originate from an earthquake under the sea bed.
they come from angry writting desks that are mocking birds
These waves are slower than those that originate at the focus.
Well, the origin of the earthquake is called the focus, and the point on the ground directly above the focus is called the epicenter. In CA, earthquakes generally originate from the San Andreas Fault.
Waves of movement are the results of the tectonic plates colliding at the focus of the earthquake, causing shock waves or tremors.
When the Lithosphere plates move, the surface of the earth vibrates. These vibrations can travel all around theearth. These vibrations are called Earth Quake.
No, seismic waves do not end at an earthquake's center. Rather, they originate there.An earthquake has a focus, and this is the center of greatest movement on the plate boundary or intraplate fault involved. It has its epicenter, and this is the center of greatest effect on the surface of the Earth above. The seismic waves are the vibrations of the slip, and radiate from the focus.
Pacific Ring of Fire is the better term, and about 80% of the worlds earthquake originate along this region, and about 80% of the very large ones. This ring of fire roughly bounds the Pacific Tectonic Plate, but volcanic and earthquake activities become less common in the higher southern latitudes of this plate.
When an earthquake is sourced, the coulomb stresses that originate from the source (due to the P-wave) are bounded by two perpendicular planes, which make up the 2 planes in an earthquake focal mechanism. Both are mathematically equivalent. Thus, without independent knowledge of which plane sourced the earthquake, either could be the "fault". Therefore, the axillary plane represents the mathematical equivalent to the source of the earthquake and is represented in earthquake focal mechanisms for a variety of reasons (helps visualize the style of faulting, disambiguity, completeness, etc.) It is extremely common for seismologists to calculate the focal mechanism without knowing which plane is the fault and which is the auxillary plane
Earthquakes originate at fault lines. These are areas of the earth's crust that push together or pull apart at times. When they pull apart or push together they create movement. We call that movement an earthquake.