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  • Understanding Earthquake Waves: P-waves & S-waves Explained
    The waves in an earthquake get their names based on their mode of travel and type of motion. Here's a breakdown:

    P-waves (Primary Waves)

    * Mode of travel: Compressional

    * Motion: Particles move back and forth in the same direction as the wave travels. Imagine a slinky being pushed and pulled.

    * Speed: Fastest seismic wave, traveling through solids, liquids, and gases.

    * Named "P" because they arrive first at a seismograph.

    S-waves (Secondary Waves)

    * Mode of travel: Shear

    * Motion: Particles move perpendicular to the direction the wave travels. Imagine shaking a rope up and down.

    * Speed: Slower than P-waves, only travel through solids.

    * Named "S" because they arrive second at a seismograph.

    Surface Waves

    * Mode of travel: Along the Earth's surface

    * Motion: More complex than P and S waves, with a combination of compression and shear motions.

    * Types:

    * Love waves: Horizontal motion, similar to the shaking of a rope.

    * Rayleigh waves: Rolling motion, like waves on the ocean surface.

    * Speed: Slower than S-waves, but cause the most damage because they are the largest in amplitude.

    In summary, the names of earthquake waves reflect their order of arrival at a seismograph (P for primary, S for secondary) and their unique motion patterns.

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