P waves (primary waves) are the first waves generated by an earthquake and travel faster than other seismic waves. These waves push and pull on structures in a back-and-forth motion, causing buildings to move horizontally. While they may not cause as much damage as other seismic waves, such as S waves or surface waves, P waves can still contribute to structural damage and shaking of buildings during an earthquake.
Earthquake shock absorbers do exactly what they say on the tin, they absorb some of the energy generated by an earthquake, in order to prevent structural damage. Most tall building in San Francisco are built on the shock absorbers, so that they can still stand after an earthquake
Surface waves tend to cause the most damage during an earthquake. These waves travel along the Earth's surface and typically have larger amplitudes and longer durations than body waves, leading to more intense shaking. Among surface waves, Love and Rayleigh waves are particularly destructive, as they can cause significant ground movement and structural damage. In contrast, body waves, while faster, generally cause less surface damage.
Earthquake scales that take into consideration the damage caused by an earthquake are known as intensity scales. Examples include the The Modified Mercalli Intensity Scale and the Macroseismic Scale.
Most of the damage from the Sumatra-Andaman earthquake was from the tsunami it triggered rather than the earthquake itself. When the earthquake occurred it caused the seafloor to shift upwards, displacing an enormous column of water. This caused a wave to race across the ocean that came ashore in many locations as a surge of water with enough force to sweep away entire buildings.
P waves (primary waves) are the first waves generated by an earthquake and travel faster than other seismic waves. These waves push and pull on structures in a back-and-forth motion, causing buildings to move horizontally. While they may not cause as much damage as other seismic waves, such as S waves or surface waves, P waves can still contribute to structural damage and shaking of buildings during an earthquake.
Earthquake shock absorbers do exactly what they say on the tin, they absorb some of the energy generated by an earthquake, in order to prevent structural damage. Most tall building in San Francisco are built on the shock absorbers, so that they can still stand after an earthquake
Earthquake damage is the damage to property and life from the ground vibrations during an earthquake. The Richter scale is one way to measure the scale of earthquake damage. For example, a magnitude of 5 is strong enough to damage weak buildings.
The name given to the huge waves that follow an earthquake is a tsunami. Tsunamis are a series of ocean waves with long wavelengths that can travel at high speeds across the ocean and cause significant damage when they reach the shore.
Surface waves tend to cause the most damage during an earthquake. These waves travel along the Earth's surface and typically have larger amplitudes and longer durations than body waves, leading to more intense shaking. Among surface waves, Love and Rayleigh waves are particularly destructive, as they can cause significant ground movement and structural damage. In contrast, body waves, while faster, generally cause less surface damage.
An 8.5 Earthquake is MUCH larger and does more damage.
Because it was a powerful, shallow earthquake.
The earthquake damaged your grammer :P
The Mercalli scale allocates a value to an earthquake based on the perceived shaking in a specific area as well as the damage to buildings and infrastructure that has occurred. The US Geological survey also use data based on the amplitudes of seismic waves and surface accelerations as measured on seismometers to quantify "perceived shaking".
The earthquake caused very little damage.
you are done!
Get in a tub...