seismic waves
These are known as seismic surface waves. They travel along the Earth's surface and cause the ground to move in a rolling motion. They are responsible for the most damage during an earthquake as they can generate strong shaking and displacement of structures.
The L- Wave or the Love and Rayleigh waves (collectively known as surface waves) cause most of the damage during an earthquake.
The L- Wave or the Love and Rayleigh waves (collectively known as surface waves) cause most of the damage during an earthquake.
Seismic waves are produced by earthquakes, rather than the cause of them! The most damaging seismic waves are the surface waves of which there are two types. Love waves and Rayleigh waves. For more information, please see the related links and question.
Surface waves, which include Love waves and Rayleigh waves, are responsible for causing the most damage during an earthquake. These waves travel along the Earth's surface and have a greater amplitude compared to the body waves, resulting in more intense shaking and destruction of buildings and structures.
Surface waves are the earthquake waves that move in a horizontal direction along the ground. They are responsible for the most damage during an earthquake due to their side-to-side shaking motion.
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.
secondary
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.
Love and Rayleigh waves which are collectively known as surface waves cause the most damage during earthquakes.
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.
secondary waves