The slowest moving waves are called long-period waves or infragravity waves, not ocean waves. Infragravity waves are longer than typical wind-generated waves, making them slower. These waves are capable of causing significant coastal erosion and damage due to their ability to transport large amounts of energy.
Surface waves generally cause the most damage during an earthquake as they travel along the Earth's surface and can produce strong shaking. In contrast, P-waves (primary waves) cause the least damage as they are the fastest seismic waves and are typically not as destructive as the slower-moving surface waves.
Surface waves typically cause the most damage in an earthquake. These waves travel along the Earth's surface and have longer periods, resulting in strong shaking that can cause buildings and other structures to collapse. Secondary waves, on the other hand, are faster but typically cause less damage compared to surface waves.
S waves typically cause more damage than P waves because they move more slowly and have larger amplitudes, resulting in stronger shaking of the ground during an earthquake. S waves can also produce more intense shaking and ground displacement, leading to a higher potential for structural damage.
S waves generally cause more damage than P waves during an earthquake. S waves have a stronger shaking motion that can lead to more destruction of buildings and infrastructure. P waves, on the other hand, are faster and usually less damaging than S waves.
Seismic waves, specifically surface waves like Love waves and Rayleigh waves, can cause the most damage to the built environment during an earthquake. These waves travel along the earth's surface and have longer periods, resulting in strong ground shaking that can lead to structural damage and ground failure.
Surface waves generally cause the most damage during an earthquake as they travel along the Earth's surface and can produce strong shaking. In contrast, P-waves (primary waves) cause the least damage as they are the fastest seismic waves and are typically not as destructive as the slower-moving surface waves.
Surface waves, Secondary waves, Primary waves :) I had this as a science question in school a few weeks ago... hope this helps :) Oh whoops i didnt log in so i did it again.... :) :) :) :) :) :) :)
Surface waves typically cause the most damage in an earthquake. These waves travel along the Earth's surface and have longer periods, resulting in strong shaking that can cause buildings and other structures to collapse. Secondary waves, on the other hand, are faster but typically cause less damage compared to surface waves.
S waves typically cause more damage than P waves because they move more slowly and have larger amplitudes, resulting in stronger shaking of the ground during an earthquake. S waves can also produce more intense shaking and ground displacement, leading to a higher potential for structural damage.
The L- Wave or the Love and Rayleigh waves (collectively known as surface waves) cause most of the damage during an earthquake.
Surface waves arrive last at a seismograph station. These waves move along the Earth's surface and are the slowest of the seismic waves, but they can cause the most damage during an earthquake.
seismic waves
S waves generally cause more damage than P waves during an earthquake. S waves have a stronger shaking motion that can lead to more destruction of buildings and infrastructure. P waves, on the other hand, are faster and usually less damaging than S waves.
The L- Wave or the Love and Rayleigh waves (collectively known as surface waves) cause most of the damage during an earthquake.
There are P waves, S waves, and Surface waves [coming in that order]. The P waves are that half second jolt, the S waves are the 2-10 second rumbles, and the Surface waves go crazy and cause the most damage.
The seismic waves that cause the majority of damage in earthquakes are the surface waves of which there are two types.
The three main types of seismic waves produced by an earthquake are primary (P) waves, secondary (S) waves, and surface waves. P waves are the fastest seismic waves and travel through solids, liquids, and gases. S waves are slower than P waves and only travel through solids. Surface waves are the slowest and cause the most damage as they move along the Earth's surface.