Seismograph.
A seismogram traces the earthquakes motion that is created by the seismograph and the seismograph records vibrations in the ground and determines the location and strength of an earthquake.
When building a house, regional seismic hazard maps are used to find the best (or the worst) place to locate for earthquake shaking. Although greatly confused with its sister, seismic risk, seismic hazard is the study of expected earthquake ground motions at any point on the earth.
The four devices commonly used to detect a possible earthquake are seismometers, accelerometers, tiltmeters, and GPS receivers. Seismometers measure the ground motion caused by seismic waves, accelerometers measure the acceleration of ground shaking, tiltmeters measure changes in the tilt of the ground surface, and GPS receivers measure precise ground displacements. These devices work together to provide valuable information for earthquake detection and monitoring.
Extreme metal stress from the lateral motion of the earthquake. which caused the collapse of the upper tiers.
P-waves.
The Richter Scale is what measures the ground motion from an earthquake.
The maximum ground motion of a magnitude 5 earthquake is 100 times larger than a magnitude 3 earthquake.
seismometer
-3.0 magnitude or if you want the ground motion: Each time the magnitude increases by one unit, the measured ground motion becomes 10 times larger. For example, an earthquake with a magnitude of 5.0 on the Richter scale will produce 10 times as much ground motion as an earthquake with a magnitude of 4.0. Furthermore, an earthquake with a magnitude of 6.0 will produce 100 times as much ground motion (10 × 10) as an earthquake with a magnitude of 4.0.
An earthquake.
Surface waves (e.g. Rayleigh waves, Love waves) that produce vertical motion of the ground surface produce the most damage during an earthquake.
Motion
Shaking and Ground rupture are the effects of earthquake. Ground shaking is the disruptive up and down and sideways motion experienced during an earthquake. And, Ground Rupture is the creation of new or the renewed movements of old fractures, oftentimes with the two blocks on both sides moving in opposite directions.
this is where the seismic waves recorded; measures vertical earth motion
0.3 magnitude
0.3 magnitude
You use a seismograph to measure the strength of an earthquake.