The alternating advance and retreat of seawater along a coastline is called a tide. High tide is when water advances to its furthest extent onto the shoreline. Low tide is when it recedes to its furthest extent. Some freshwater rivers and lakes can have tides, too. A high tide that is significantly higher than normal is called a king tide. It often accompanies a new moon and when the moon is closest to the Earth.

The moon’s gravitational pull on the Earth and the Earth’s rotational force are the two main factors that cause high and low tides. The side of the Earth closest to the Moon experiences the Moon’s pull the strongest, and this causes the seas to rise, creating high tides. On the side facing away from the Moon, the rotational force of the Earth is stronger than the Moon’s gravitational pull. The rotational force causes water to pile up as the water tries to resist that force, so high tides form on this side, too. Elsewhere on the Earth, the ocean recedes, producing low tides. The gravitational attraction of the Sun also plays a small role in the formation of tides. Tides move around the Earth as bulges in the ocean.

Most shorelines experience two high and two low tides within a twenty-four-hour period, though some areas have just one of each. A coastline’s physical features, such as a wide sandy beach or a rocky cove, along with the depth of the water just offshore, affect the height of the tides.

Tides affect marine ecosystems by influencing the kinds of plants and animals that thrive in what is known as the intertidal zone—the area between high and low tide. Because the area is alternately covered and uncovered by the ocean throughout the day, plants and animals must be able to survive both underwater and out in the air and sunlight. They must also be able to withstand crashing waves. 

For example, plants and animals that can anchor themselves to the rocks along a shoreline can survive the lashing from waves and the less violent movement of the changing tides. On sandy beaches, survival means being able to swim in shallow water or burrow under the sand as the waves arrive and depart overhead. Sand crabs not only burrow to survive, they actually follow the tides to maintain just the right depth in the wet sand.

Along many shorelines, tides form tide pools. These small pools of water are often left behind among the rocks at low tide. They can include a diverse population of tiny plants and animals that may serve as food for larger species. 

The rise in sea levels will affect tides and their impacts, not just on marine ecosystems but on coastal areas that are home to millions of people and animals. The more that is known about how tides work and how they shape our coastlines, scientists say, the better prepared we will be for future changes in the oceans.



Tides driven by the gravitational pull of the moon create a unique marine ecosystem known as the intertidal zone where animals must be able to survive waves and daily dry periods

Plural Noun

(singular: alga) diverse group of aquatic organisms, the largest of which are seaweeds.


to dig a small hole or tunnel.


outer boundary of a shore.


community and interactions of living and nonliving things in an area.

gravitational pull

physical attraction between two massive objects.

Great Barrier Reef

large coral reef off the northeast coast of Australia.

high tide

water level that has risen as a result of the moon's gravitational pull on the Earth.


region between the high and low tide of an area.

low tide

water level that has dropped as a result of the moon's gravitational pull on the Earth.


object's complete turn around its own axis.


base level for measuring elevations. Sea level is determined by measurements taken over a 19-year cycle.


beach, or where a body of water meets land.


rise and fall of the ocean's waters, caused by the gravitational pull of the moon and sun.

tide pool

small pond created by an ebb tide and submerged by a high tide.