what are the two types of seismic waves brainly?
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The two main types of waves are body waves and surface waves. Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the planet like ripples on water.
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There are two basic types of wave motion for mechanical waves: longitudinal waves and transverse waves.
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We know that there are two types of wave - transverse waves and longitudinal waves. Radio waves, microwaves, infrared, visible light, ultraviolet light, X-rays and gamma rays are all transverse waves. They are also all members of the electromagnetic spectrum and some of them can be used for communication.
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['ripples on the surface of water.', 'vibrations in a guitar string.', 'a Mexican wave in a sports stadium.', 'electromagnetic waves – eg light waves, microwaves, radio waves.', 'seismic S-waves.']
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There are three basic types of seismic waves – P-waves, S-waves and surface waves. P-waves and S-waves are sometimes collectively called body waves.
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" KDW LV ZDYHOHQJWK " CHARACTERISTICS OF WAVE MOTION The two types of wave motion, transverse and longitudinal, have many of the same characteristics, such as frequency, amplitude, and wavelength. Another important characteristic that these two types of wave motion share is VELOCITY.
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Three types of seismic waves are P waves, S waves, and surface waves.
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Earthquakes produce three types of seismic waves: primary waves, secondary waves, and surface waves. ... Scientists learn about Earth's layers by studying the paths and speeds of seismic waves traveling through Earth. Primary Waves. The fastest seismic waves are called primary waves, or P waves.
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Earthquakes produce three types of seismic waves: primary waves, secondary waves, and surface waves. Each type moves through materials differently. In addition, the waves can reflect, or bounce, off boundaries between different layers.
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Body waves can travel through the earth's inner layers, but surface waves can only move along the surface of the planet like ripples on water. Earthquakes radiate seismic energy as both body and surface waves. ... The P wave can move through solid rock and fluids, like water or the liquid layers of the earth.
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As their name suggests, surface waves travel just below the surface of the ground. Although they move even more slowly than S-waves, they can be much larger in amplitude and are often the most destructive type of seismic wave.
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S waves are slower than P waves and they can only travel through solid rock. S waves move the particles it pushes through up and down or side to side (perpendicular to the motion of the S waves energy). The second link has very good animated illustrations of both movements.
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When two tectonic plates move toward each other and collide, they form a convergent plate boundary. There are three types of convergent plate boundaries: oceanic-oceanic boundaries, oceanic-continental boundaries, and continental-continental boundaries. Each one is unique because of the density of the plates involved.
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Common types of mechanical waves include sound or acoustic waves, ocean waves, and earthquake or seismic waves. ... The transmission of electromagnetic waves does not require a medium and electromagnetic waves are able to travel through vacuums.
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Movement in narrow zones along plate boundaries causes most earthquakes. Most seismic activity occurs at three types of plate boundaries—divergent, convergent, and transform. As the plates move past each other, they sometimes get caught and pressure builds up.
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Longitudinal waves propogate by means of vibrations or disturbances in the medium that are in the same direction that the wave travels. Examples are sound (as above), seismic shock waves, slinky springs and part of the motion in ocean waves.
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The three main types of mechanical waves are transverse waves, longitudinal waves, and surface waves.