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Meteor vs Meteorite vs Meteoroid

Also known as: Meteor, Meteorite, Meteoroid, Shooting Star, Falling Star, Fireball

Quick answer

The same rock gets three names by location: a meteoroid travelling through space becomes a meteor — a shooting star — while burning through the atmosphere, and any surviving fragment on the ground is a meteorite. Most meteors are sand-grain sized and vaporise entirely at 80–120 km altitude.

📘 Full definition✓ Reviewed 2026-09-07
The terminology distinguishes three stages of the same object: a meteoroid is any natural solid object in interplanetary space, ranging from dust-grain size to about 1 metre (larger objects are asteroids). When a meteoroid enters Earth's atmosphere at high speed (11–72 km/s), friction and compression with atmospheric molecules heat it to incandescence, producing a visible streak of light called a meteor — commonly known as a "shooting star." If the object is large enough that a portion survives the intense heating and reaches Earth's surface, the recovered fragment is a meteorite. Exceptionally bright meteors (brighter than Venus, magnitude −4) are called fireballs or bolides. Meteor showers occur when Earth passes through debris trails left by comets — the Perseids, Geminids, and Leonids are among the best known.
Meteoroid (in space)
Dust grain to 1 m
Meteor (in atmosphere)
Visible at 80–120 km altitude
Meteorite (on ground)
Iron, stony, or stony-iron
Entry Speed
11–72 km/s

Understanding Meteor / Meteorite

The Three Names

StageNameWhereWhat You See
In spaceMeteoroidInterplanetary spaceNothing (too small to see)
In atmosphereMeteor80–120 km altitudeBright streak of light (shooting star)
On the groundMeteoriteEarth's surfaceRecovered rock/metal fragment

Meteor Showers

Meteor showers occur when Earth's orbit crosses the debris trail left by a comet. Each shower has a radiant point — the area of sky from which meteors appear to originate — and occurs at the same time each year. The Perseids (August, from Comet Swift-Tuttle) and Geminids (December, from asteroid Phaethon) are the most reliable, producing 60–150 visible meteors per hour under ideal conditions. These events are unrelated to space debris re-entries, which produce slower, longer-lasting fireballs.

Meteorites and Science

Meteorites are invaluable to science — they are free samples of solar system material delivered to Earth's surface. The three main types are: iron (metallic, from asteroid cores), stony (silicate, from asteroid mantles and crusts), and stony-iron (mixed). Carbonaceous chondrites are particularly prized as they contain organic molecules, water, and presolar grains older than the solar system itself. The 2023 Winchcombe meteorite (UK) was recovered within hours and found to contain amino acids and water, providing insight into how these building blocks of life may have been delivered to early Earth.

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Frequently Asked Questions

A "shooting star" is actually a meteor — a tiny piece of space rock (meteoroid), typically no larger than a grain of sand, burning up in Earth's atmosphere at 80–120 km altitude. The streak of light you see is not the rock itself but the superheated air and vaporised material along its path. Despite the name, shooting stars have nothing to do with actual stars.
Earth gains approximately 40–80 tonnes of meteoritic material every day, but the vast majority is dust and tiny particles that burn up harmlessly as meteors. Meteorites large enough to reach the ground intact are relatively rare — an estimated 6,100 meteorites larger than 1 kg strike Earth annually, but most fall in oceans or uninhabited areas and are never recovered. Only about 5–10 meteorite falls are witnessed and recovered each year worldwide.
Speed and duration. A meteor flashes across the sky in a second or two and is gone; a satellite is a steady point of light taking minutes to cross, moving at a constant rate without a trail. Satellites also do not flare and fragment — a bright breaking-up streak lasting many seconds is likely re-entering debris.

Sources & References

Definitions are reviewed against primary sources. Last reviewed: 2026-09-07.