Longitudinal waves are the result of earthquakes, and are also known as Primary, or P-Waves. Longitudinal waves are faster than Transverse (Secondary) Waves. A diagram of a Longitudinal wave is a straight line, with a denser area where the wave itself is travelling.
Electromagnetic waves originate from the movement of charged particles, such as electrons, in atoms and molecules. When these charged particles accelerate or change direction, they create electromagnetic waves that can travel through space.
Sound waves originate from a vibrating object that creates oscillations in the surrounding air particles. These oscillations cause a disturbance in air pressure, which propagates as a wave through the medium.
Longitudinal waves are the result of earthquakes, and are also known as Primary, or P-Waves. Longitudinal waves are faster than Transverse (Secondary) Waves. A diagram of a Longitudinal wave is a straight line, with a denser area where the wave itself is travelling.
Most destructive waves, such as tsunamis, originate from underwater seismic activity, like earthquakes, volcanic eruptions, or landslides. When these events displace a large volume of water, it sets off a series of powerful waves that can travel great distances across the ocean.
Tremors or shock waves typically originate from the release of energy through the sudden movement or displacement of the Earth's crust. This can be due to geological events such as earthquakes, volcanic eruptions, explosions, or human activities like mining or construction. The energy is transmitted through the Earth in the form of seismic waves.
The waves that are slower that those that originate at the focus are called secondary waves or S-waves. They are shear waves that are transverse in nature.
Light waves originate from a light source, such as the sun, a light bulb, or a laser. When an object absorbs energy, it can emit photons, which are the elementary particles of light that travel as electromagnetic waves.
Tidal waves originate deep within the ocean and end once they reach the coast. They are typically caused by large earthquakes which send shock waves outward from the epicenter.
Electromagnetic waves originate from the movement of charged particles, such as electrons, in atoms and molecules. When these charged particles accelerate or change direction, they create electromagnetic waves that can travel through space.
Surface waves are slower than body waves like P-waves and S-waves because they travel along the Earth's surface instead of through the interior. Surface waves typically cause the most damage during an earthquake due to their combination of horizontal and vertical motion.
Sound waves originate from a vibrating object that creates oscillations in the surrounding air particles. These oscillations cause a disturbance in air pressure, which propagates as a wave through the medium.
p waves
Surface waves do not originate from the focus. These waves are created when seismic energy reaches the Earth's surface and move horizontally along it, causing the ground to move in a rolling motion.
Radio waves originate from various sources, including natural phenomena like lightning and astronomical objects, as well as human-made devices such as radios, cell phones, and broadcasting towers.
As of being waves, sound waves does just that. They start from origin and spread out. Sound waves will however quickly fade with distance and time.
Many tidal waves originate from an earthquake under the sea bed.
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