Surface waves
Surface waves are formed when the waves reach the Earth's surface. These waves travel along the boundary between the Earth and the atmosphere, and they can cause both lateral and vertical movements of the ground.
Surface waves are formed when waves reach the Earth's surface. These are seismic waves that travel along the Earth's surface and can cause the most damage during an earthquake.
The point on the earth's surface closest to the origin of an earthquake is called the epicenter. This is where the seismic waves generated by the earthquake first reach the surface.
The point on Earth's surface directly above an earthquake's focus is called the epicenter. It is where the seismic waves originating from the earthquake's focus first reach the surface.
Primary waves (P-waves) are body waves that travel through the interior of the Earth and are the fastest seismic waves. Surface waves, on the other hand, travel along the Earth's surface and are responsible for most of the shaking and damage during an earthquake. Surface waves have larger amplitudes and longer wavelengths compared to P-waves.
L waves are formed when P&S waves reach the surface.
Surface waves are formed when the waves reach the Earth's surface. These waves travel along the boundary between the Earth and the atmosphere, and they can cause both lateral and vertical movements of the ground.
Surface waves are formed when waves reach the Earth's surface. These are seismic waves that travel along the Earth's surface and can cause the most damage during an earthquake.
the one with the most damege is the surface wave because they are on the surface of earth. but p-waves are the second and s-waves are the third
The three types of electromagnetic waves that reach the Earth's surface are radio waves, visible light, and infrared radiation. Each of these types of waves plays a different role in our daily lives and interacts with the Earth in various ways.
Seismic waves are the types of waves that can travel through the Earth and along its surface. There are two main types of seismic waves: body waves (such as primary and secondary waves) that travel through the Earth's interior, and surface waves (such as Love and Rayleigh waves) that travel along the Earth's surface.
The point on the earth's surface closest to the origin of an earthquake is called the epicenter. This is where the seismic waves generated by the earthquake first reach the surface.
It travels through the ground.
energy reachs earth surface through seismic waves: P waves S waves and Surface waves
Wind causing waves are formed at the surface of the oceans.
The point on Earth's surface directly above an earthquake's focus is called the epicenter. It is where the seismic waves originating from the earthquake's focus first reach the surface.
Primary waves (P-waves) are body waves that travel through the interior of the Earth and are the fastest seismic waves. Surface waves, on the other hand, travel along the Earth's surface and are responsible for most of the shaking and damage during an earthquake. Surface waves have larger amplitudes and longer wavelengths compared to P-waves.