The moon's gravitational pull creates tidal bulges on Earth by exerting a force that attracts water towards it. As the Earth rotates, these bulges move, leading to high tides in the areas where the water is drawn closer to the moon. Simultaneously, on the opposite side of the Earth, a second bulge occurs due to the centrifugal force created by the Earth-moon system's rotation. This results in a regular pattern of rising and falling sea levels known as tides.
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