P-waves, also known as primary waves, are the ⚡️ fastest seismic waves that zip through the Earth during an earthquake. They are the first to arrive at a seismograph station. P-waves are capable of traveling through solids, liquids, and gases, making them versatile messengers of seismic activity. They cause particles in the ground to move back and forth in the same direction as the wave, like a slinky compressing and expanding. Their speed and ability to propagate through various materials make P-waves essential for studying and understanding earthquake events. ⚡️
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