Britannica AI Icon

equinoctial precession cycle

geochronology

Quick Summary

The precession of the equinoxes is a slow, westward movement of the equinoxes along the ecliptic. This phenomenon is caused by the gravitational pull of the Sun and Moon on Earth's equatorial bulge, resulting in a cyclic wobble of Earth's axis of rotation. This wobble has a period of approximately 25,772 years.12

This motion causes the celestial poles and the celestial equator to trace circles in the sky over long periods. For instance, the north celestial pole currently points near Polaris but will shift towards Vega in about 12,000 years. The equinoxes themselves drift westward along the ecliptic at an average annual rate of about 50.4 arc seconds. This phenomenon was first systematically observed by the Greek astronomer Hipparchus when comparing his star catalog with earlier Babylonian measures.134

Summary created from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles.

Ask Britannica AI about this topic

Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.