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The Moon’s gravitational pull is the primary force behind Earth’s tides. As the Moon orbits Earth, its gravity attracts the ocean’s water, creating a bulge (high tide) on the side of Earth facing the Moon. A second high tide occurs on the opposite side due to Earth’s rotation and the centrifugal force of the Earth-Moon system. Low tides occur in areas between these bulges. The Sun also influences tides, amplifying them during full and new moons (spring tides) and reducing them during quarter moo
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The Moon’s gravitational pull is the main driver of ocean tides on Earth. But with our powers combined, the Sun and the Moon create even higher tides twice a month, called spring tides. Explore how the Moon causes tides: https://go.nasa.gov/3z5IxM6 | NASA Space Alerts
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