The position of the moon significantly influences the occurrence of high and low tides due to its gravitational pull on Earth's oceans. When the moon is directly overhead or on the opposite side of the Earth, its gravitational force causes water to bulge, resulting in high tide. Conversely, when the moon is at a right angle to a location on Earth, its gravitational pull is weaker, leading to low tide. This cyclical pattern occurs approximately every 12.5 hours, corresponding to the moon's orbit around Earth.
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