All other factors being equal, the seismic waves will be felt most strongly at or near to the epicentre of the earthquake.
No because the epicenter is right on top of the center of the quake.
Because that is where the energy of the earthquake is released. As the energy travels farther away from the epicenter, it is dissipated as mechanical force.
P-waves travel between 5-8 km/s. As such the epicentre could be anywhere between 1200 and 1920 km away.
It depends on the magnitude.
From Science Explorer Prentice Hall Earth Science: " Geologists use seismic waves to locate an earthquake's epicenter. Seismic waves travel at different speeds. P waves arrive at a seismograph first, with S waves following close behind. To tell how far the epicenter is from the seismograph, scientists measure the difference between the arrival time of the P waves and S waves. The farther away an earthquake is, the greater the time between arrival of the P waves and the S waves." Did this help?
away from epicenter
away from epicenter
Near.
Usually near.
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Usually near.
No because the epicenter is right on top of the center of the quake.
Because that is where the energy of the earthquake is released. As the energy travels farther away from the epicenter, it is dissipated as mechanical force.
The energy of the seismic waves that reach the surface is greatest at the epicenter. The most violent shaking during an earthquake however may occur kilometers away from the epicenter. The types of rock and soil around the epicenter determine where and how much the ground shakes.
No, the greatest intensity of an earthquake is not always found at the epicenter. The intensity of an earthquake can vary at different locations depending on the distance from the epicenter, the depth of the earthquake, and the local geological conditions. In some cases, the intensity may be greater at locations further away from the epicenter due to the way seismic waves propagate.
How far away the epicenter is.
The most earthquake damage tends to occur at the epicentre, which is the point on the surface above the hypocentre, or focus, of an earthquake. It is the point in the Earth's crust where the rock first breaks.However, many earthquakes do not actually break the earth's surface. It has been found that the most damage in an earthquake tends to result from the secondary effects, especially the movement of seismic waves away from the epicenter. These secondary effects include landslides, liquefaction, fissuring and aftershocks.