Surface waves typically cause more damage than primary or secondary waves during an earthquake. They travel along the earth's surface and are responsible for the shaking that can result in building collapse and other structural damage. Primary and secondary waves, while important for seismologists to study, usually do not cause as much damage as surface waves.
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.
Tidal waves, also known as tsunamis, can destroy buildings, infrastructure, vegetation, and cause significant damage to coastal ecosystems. They have the potential to cause widespread devastation to communities and pose a threat to human lives.
Nothing
The four sub-types of seismic waves are Primary waves (P-waves), Secondary waves (S-waves), Love waves, and Rayleigh waves. P-waves are compressional waves that travel fastest through the Earth, while S-waves are shear waves that move slower and can only travel through solids. Love waves move horizontally and are responsible for much of the damage during an earthquake, and Rayleigh waves create an elliptical rolling motion, affecting both the surface and subsurface. Together, these waves provide critical information about the Earth's structure and behavior during seismic events.
Surface waves typically cause more damage than primary or secondary waves during an earthquake. They travel along the earth's surface and are responsible for the shaking that can result in building collapse and other structural damage. Primary and secondary waves, while important for seismologists to study, usually do not cause as much damage as surface waves.
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.
A p wave because it can move so fast with more force. P waves cause little damage, they are compressional waves. They are at a higher frequency and a lower amplitude than surface waves which are shear waves. S-waves cause the most damage because they are slow moving and have an amplitude much greater than P-waves.
not lots
There are a bunch of little earthquakes every minute. We don't even feel them! They don't cause any damage. The only way we know about these earthquakes is because seismographs (instruments used to detect seismic waves) detect the waves underground.
*volcanoes Earthquakes and vOlcanoes can cause much damage among an area if it's shaken to pieces.
Tidal waves, also known as tsunamis, can destroy buildings, infrastructure, vegetation, and cause significant damage to coastal ecosystems. They have the potential to cause widespread devastation to communities and pose a threat to human lives.
Electromagnetic waves only cause sound pollution because they are sound waves.
Hurricane Ike cause about $37.6 billion in damage.
Nothing
It did a lot of damage.
Alot