when the surface of the sea is distributed, waves are produced. waves are seen moving on the surface of water but actually their movement is not extensive and the movement of water from one part of the ocean to another gives rise to currents.
Rock under stress breaks at the focus, releasing energy and vibrations called seismic waves, which travel away from the focus, through Earth's interior, and across the surface. The three types of seismic waves are: Primary waves: The first to arrive at seismographs Secondary waves: The second to arrive at seismographs Surface waves: The last and most severe to arrive at seismographs
The three types of seismic waves are: P waves S waves Surface waves ( two surface waves. Riley surface wave and love surface wave named after scientists
No. surface waves on the surface of water is transverse in nature. It has crests and troughs. Compression and rarefaction will be in longitudinal wave. example sound waves.
p wave comes first s wave comes next and last comes surface wave.
Seismic waves, specifically surface waves, can affect the surface of the land by causing it to rise and fall like waves on an ocean. These waves are typically generated during an earthquake and can produce the most visible effects on the Earth's surface.
Wind causing waves are formed at the surface of the oceans.
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.
Seismic waves, specifically surface waves such as Love and Rayleigh waves, are responsible for causing the surface of the land to rise and fall during an earthquake. These waves travel along the Earth's surface and can produce the shaking and rolling motion that is felt during seismic events.
Underwater earthquakes can generate seismic waves, including primary (P) waves, secondary (S) waves, and surface waves. These waves can travel through the Earth and water, causing tsunamis on the ocean's surface.
Ocean waves get their energy from the wind, which creates friction on the surface of the water. This energy is transferred through the water by the movement of water particles in a circular motion, causing the waves to propagate and travel across the ocean.
surface waves
Surface waves
Waves in the ocean are mainly caused by the wind transferring energy to the water's surface. When the wind blows over the water, it creates friction, causing the water to move in ripples that develop into waves. Other factors like tides, earthquakes, and underwater landslides can also contribute to wave formation in the ocean.
Ocean waves are considered to be a combination of both transverse and longitudinal waves. While the surface water particles move in a circular motion, causing a transverse wave motion, the energy in ocean waves propagates forward, exhibiting characteristics of a longitudinal wave.
Ocean waves are mechanical waves. The waves on the surface are surface waves (particles move in a circular motion) while the waves in the depths are longitudinal (particles move parallel to the wave propogation).
Sea waves are formed by the friction between wind and the water's surface. As wind blows over the ocean, it transfers energy to the water, causing it to move in circular patterns. These circular motions form waves that travel across the ocean's surface.