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Water and oceans · Discover & try

Why does the sea rise and fall?

Reading level 1 of 5 · EarlyChange
1 · Shorter sentences5 · More detail

Gravity from the Moon and Sun helps make tides. In this simple view, water is higher in two broad regions. Earth turns, carrying our shore marker through higher and lower water. The gap between high and low water is the tidal range. New and full Moon bring larger spring ranges; quarter Moons bring smaller neap ranges. Neap tides still rise and fall. The picture explains a pattern, not the exact tide at your beach.

Word help
tidal range

The difference in water height between a high tide and a low tide; not the number of tides.

quarter Moon

A phase when half the visible Moon looks lit; the Sun and Moon lie roughly at right angles as seen from Earth.

spring tide

A larger high-to-low range near new and full Moon, unrelated to the spring season.

neap tide

A smaller high-to-low range near the quarter Moon phases; tides still occur.

Watch · Try · Explain

See how it works

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Idealised daily tide cycle and spring–neap range comparison. Water deformation, sizes and distances are exaggerated; the gauge shows relative levels, not a local tide prediction.

What to look for
  • Follow the same shore marker as Earth turns, and match its position to the water-level display.
  • Count the repeating rises and falls separately from the size of the high-to-low gap.
  • Compare aligned new/full Moon positions with right-angle quarter phases.
  • Notice that a smaller neap range still includes rising and falling water.
Explain what you noticed

Two imagined shore records each show two high tides and two low tides. In record B, the highs are higher and the lows are lower than in record A. What changed?

Keep this idea: Earth’s rotation helps produce the daily tide cycle; changing Sun–Moon geometry changes its range.

Follow the sources

Source material checked 2026-10-28. Explanations and activities by Nepedia. Source links do not imply endorsement.

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