Times are approximate. One tidal day lasts about 24 hr 50 min. The last high tide starts the next tidal day; it is not an extra high tide within the first day.
Simplified model: Sizes, distances, and bulges are not to scale. This shows the Moon’s effect, not a tide forecast for a real beach.
The beach lines up with the Moon-facing bulge. The Moon’s gravity causes both ocean bulges.
Earth, Moon, and the tidal bulges
The water at your beach
High tide
Tide graph: one tidal day
Learn more about the science
What causes tides?
Tides are regular rises and falls in ocean water level. The Moon’s gravity is the main cause. It pulls on Earth itself and the oceans on both sides. The Sun’s gravity also affects tides, but this model focuses on the Moon.
Why are there two bulges?
The Moon’s gravity pulls on Earth itself and its oceans. The Moon’s pull is strongest on the ocean facing it, weaker at Earth’s center, and weakest on the ocean on the opposite side. This difference creates two bulges of water, one facing the Moon and one on the opposite side. Both bulges cause high tides.
Why do many beaches have two high tides and two low tides?
Earth rotates, or spins. In this model, that carries the beach through two bulges and two lower-water areas each tidal day. A bulge means high tide; a lower-water area means low tide. High to low takes about 6 hours 13 minutes. High to the next high takes about 12 hours 25 minutes.
Why does a tidal day last about 24 hours 50 minutes?
The Moon moves along its orbit while Earth spins. After 24 hours, Earth needs a little more rotation to line the beach up with the Moon again. That takes about 50 extra minutes. The last button shows the start of the next tidal day, not a third high tide within the first one.
Explore the science: NASA: Tides · NOAA: The Lunar Day · NOAA: Tidal Patterns
Check for Understanding
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