
How tides work
Tides are caused by the gravitational attraction of the moon and, to some extent, the sun. Gravity pulls up on the ocean's surface directly below the moon, while on the other side of the earth an equal bulge occurs. This second bulge results from the opposite, centrifugal force that keeps the earth and the moon from crashing together. The highest tides, known as spring tides (from the German springen, meaning “to jump”), happen when the moon and the sun line up with the earth and their gravitational forces are combined. The lowest tides, or neap tides, occur when the sun's position is at a right angle to that of the moon.

