


About 4.5 billion years ago, when Earth was young and still molten at the surface, a body about the size of Mars struck it a glancing blow. The debris thrown into orbit gathered into the moon, then far closer than it is now, looming many times larger in the sky.
Early Earth spun fast, with days only a few hours long. The moon's pull raised tides that dragged against that spin and slowed it, day by day, across billions of years, toward the 24 hours we live by, while the moon drifted outward. It is still drifting, about 3.8 centimeters a year.
The moon also steadies Earth's tilt. Without it, the pull of the other planets could swing the axis widely over long ages, scrambling the seasons. With it, the tilt stays close to 23.4 degrees, so summer and winter return on time, year after year.
And its tides set the first beat of the shorelines: twice a day, the sea rises and falls, and every two weeks the tides swell and slacken with the moon's phase. Many scientists think life began at the edge of that rhythm, in pools filled and drained by the moon. In that sense the moon is the metronome for life on Earth: it set the tempo of the days, held the seasons steady, and kept time at the water's edge.
Seen from the side, the sun travels left to right and Earth spirals around its path once a year, December solstice at the top of each turn, with the moon spiraling around Earth. Eclipses happen only where the moon lines up with Earth and sun, marked on the path: gold rings for the sun, copper for the moon. They come in pairs about two weeks apart, twice a year, when the moon's tilted orbit crosses the line to the sun. Tap one to go there.
| Date | Eclipse | Where | From here |
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Tap a full moon to go there on the calendar.
| Full moon | Date | Next new moon | Days to next full |
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