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When the Sun, Earth, and Moon form a right triangle, the gravitational forces exerted by the Sun and the Moon partially counteract each other. This configuration, known as a quadrature, typically occurs during the first and third quarter phases of the Moon. As a result, the tidal bulges caused by these gravitational forces are diminished, leading to lower high tides than normal, known as neap tides. Consequently, the difference between high and low tides is less pronounced during this period.

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