When a seismic wave bounces backward, it is referred to as reflection. This occurs when the wave encounters a boundary between different materials, causing part of the wave to return to the surface. This phenomenon is commonly used in seismic studies to analyze the Earth's subsurface structures.
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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.
Hurricanes do not have aftershocks; earthquakes do. The waves of any earthquake are seismic waves.
The seismic wave that squeezes and pulls rocks in the same direction is called a P-wave, or primary wave. P-waves are longitudinal waves that travel through the Earth, moving particles in the same direction as the wave itself. They are the fastest seismic waves and can travel through both solid and liquid materials, making them crucial for understanding the Earth's interior.
it is called a seismic wave
The center of a seismic wave is called the focus or hypocenter. This is the point within the Earth where the seismic waves originate.
A seismic wave. If the earthquake occurs under water, the seismic waves can produce waves in the water called tsunami.
Answer: When a seismic wave 'bounces backward' and reaches a boundary, it is called Reflection. Explanation: The seismic waves are the result of the landslides, earthquakes, volcanic eruptions, explosions by humans
Answer: When a seismic wave 'bounces backward' and reaches a boundary, it is called Reflection. Explanation: The seismic waves are the result of the landslides, earthquakes, volcanic eruptions, explosions by humans
It is called a tsunami.
It is called a tsunami.
A seismograph can locate a seismic wave.
Seismic wave
Reflection
Reflection
When a seismic wave bounces backward, it is referred to as reflection. This occurs when the wave encounters a boundary between different materials, causing part of the wave to return to the surface. This phenomenon is commonly used in seismic studies to analyze the Earth's subsurface structures.