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  • Rarefaction in Waves: Definition, Characteristics & Examples
    A rarefaction is a region in a longitudinal wave where the particles of the medium are spread out or less dense than in the surrounding areas. It's the opposite of a compression, where the particles are close together.

    Here's a breakdown:

    * Longitudinal Wave: In a longitudinal wave, the particles of the medium vibrate parallel to the direction the wave travels. Think of a spring being stretched and compressed.

    * Compression: A compression is a region in the wave where the particles are close together. This creates a high pressure area.

    * Rarefaction: A rarefaction is a region in the wave where the particles are spread out. This creates a low pressure area.

    Think of it like this:

    Imagine a slinky. When you push a part of the slinky together, you create a compression. This creates a region of higher density. When you pull on the slinky, you create a rarefaction. This creates a region of lower density.

    Examples:

    * Sound Waves: Sound waves are longitudinal waves that travel through a medium like air. When you speak, your vocal cords create compressions and rarefactions in the air, which our ears detect as sound.

    * Seismic Waves: Seismic waves are longitudinal waves that travel through the Earth's crust. They are caused by earthquakes and can be devastating.

    Key points about rarefactions:

    * They are a necessary part of longitudinal waves.

    * They are regions of low density and low pressure.

    * They alternate with compressions in a longitudinal wave.

    Let me know if you have any more questions!

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