Ocean tides are the cyclical rise and fall of sea levels, primarily caused by the gravitational pull of the Moon
Types of Tides:
Semi-diurnal tides: Occur with two high and two low tides each day, typically about six hours apart.
Diurnal tides: Occur with only one high and one low tide each day.
Spring Tides:
Occur when the Sun, Moon, and Earth are aligned, resulting in higher high tides and lower low tides.
Neap Tides:
Occur when the Sun, Moon, and Earth are at right angles to each other, resulting in smaller tidal ranges.