The Sun and the Moon gravitational pull on the earth causes high and low tides which give the ocean waves their energy.
Ocean waves get their energy from wind blowing across the surface of the water. When the wind contacts the water, some of its energy is transferred.
It travels through the ground.
The energy from an earthquake travels in the form of seismic waves through the Earth's layers. When these waves reach the surface, they cause the ground to shake, creating the tremors that are felt during an earthquake.
Most of the energy of an earthquake is transported through the Earth's crust in the form of seismic waves. These waves can be either body waves (P-waves and S-waves) that travel through the interior of the Earth, or surface waves that travel along the Earth's surface. The energy is gradually attenuated and dispersed as the waves propagate through the crust.
True. The energy released during an earthquake travels in the form of seismic waves. These waves can be classified into primary waves (P-waves), which are compressional and travel fastest, and secondary waves (S-waves), which are shear waves that move more slowly. Additionally, surface waves travel along the Earth's surface and often cause the most damage during an earthquake.
A wave of energy released from an earthquake is called a seismic wave. Seismic waves can be classified into body waves, which travel through the Earth's interior, and surface waves, which travel along the Earth's surface. These waves are responsible for causing the ground shaking and damage associated with earthquakes.
energy reachs earth surface through seismic waves: P waves S waves and Surface waves
The immediate energy source for most waves on the ocean surface is wind. Wind transfers its kinetic energy to the ocean surface waters, causing them to generate waves through frictional interaction.
Absorption
Absorption
energy reachs earth surface through seismic waves: P waves S waves and Surface waves
Surface waves have the highest amplitude because they travel along the boundary between two mediums, allowing for energy to be concentrated near the surface. As a result, surface waves experience less spreading and attenuation compared to bulk waves that travel through a medium. This concentration of energy near the surface leads to higher amplitudes in surface waves.
It travels through the ground.
Surface waves occur at the boundary between two different mediums, such as air and water, or air and land. They travel along the interface, transferring energy in the form of ripples or undulations on the surface. Examples of surface waves include ocean waves, seismic waves, and electromagnetic waves.
Mostly by wind blowing across the water's surface.
The loss of wave energy when it encounters a surface and causes the waves to become weaker is known as wave reflection. This can happen when waves bounce off a barrier or shoreline, leading to reduced energy and amplitude in the reflected waves.
These are known as seismic waves.
Wherever there are waves ... or the surface of the sea.