because of the Seismic waves ^^ -RYAN BALICTAR
Source earthquake waves are seismic waves produced directly from the earthquake's source, such as the initial rupture of rocks along a fault. These waves include P-waves and S-waves that travel through the Earth and are used to locate and study earthquakes. Source earthquake waves provide valuable information about the earthquake's characteristics and help in assessing its impact.
because of the Seismic waves ^^ -RYAN BALICTAR
Seismic waves move outward from the source of an earthquake. These waves carry the energy released during the earthquake and can cause shaking and damage as they propagate through the Earth's crust.
The distance between a seismological recording station and the earthquake source is determined from the arrival times of seismic waves at the station. By comparing the arrival times of P-waves and S-waves, seismologists can calculate the distance to the earthquake source using the difference in their arrival times.
Out words in all directions from the source.
The magnitude of an earthquake is based on measurements of amplitudes of seismic waves. This measurement provides an indication of the energy released at the earthquake's source.
The distance between a seismological recording station and the earthquake source is determined from the arrival time of P and the S waves. P waves are faster than S waves and surface waves.
Seismic waves do not end at an earthquake's center; rather they continue to propagate through the Earth in all directions from the initial point of rupture. The seismic waves can be recorded by seismometers located around the world, providing valuable information about the earthquake's location, magnitude, and source mechanism.
Earthquakes release energy in the form of seismic waves, which travel outward from the earthquake source. These waves cause the ground to shake and can lead to destruction and damage to buildings and infrastructure. The amount of energy released by an earthquake is measured on the Richter scale.
Earthquake waves are called seismic waves.
The origin time of an earthquake is determined by analyzing the seismic waves recorded by multiple seismometers. By comparing the arrival times of the waves at different stations, scientists can calculate the time it took for the waves to travel from the earthquake source to each station, thus pinpointing the origin time of the earthquake.
well the waves carried through out places vibrates the earth