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1Clear out junk files and repair common Windows errors2Scan for outdated or missing drivers - takes under a minute3Repair Windows errors before they cause bigger problemsA dark, heavy, or magnetic rock could be a meteorite, but none of those traits proves it came from space. Compare several clues—surface, weight, magnetism, streak, and interior—then treat the result as a preliminary screen. Unique identification requires detailed analysis.
What clues distinguish a meteorite from an Earth rock?
Look at the specimen as a whole. A likely meteorite may have a thin, dark fusion crust, a compact surface with few or no holes, unusually high weight for its size, magnetic attraction, or telltale features inside. Terrestrial rocks and industrial slag can imitate some of these traits, so no single check settles the question.
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| Clue | What may fit a meteorite | What can also explain it |
|---|---|---|
| Outer coating | A thin, dark fusion crust on a recently fallen specimen; it can wear away as the meteorite weathers. | Desert varnish can give an Earth rock a shiny black coating. |
| Texture | A generally compact surface without obvious bubbles. | Vesicles—small holes left by gas—are common in volcanic rocks and may occur in slag. |
| Weight | Heavier than an ordinary rock of similar size. | Terrestrial iron ores and slag can also be dense. |
| Magnetism | Many meteorites attract a magnet, though a weathered ordinary chondrite may respond only weakly. | Magnetite, some hematite-bearing rocks, and slag may also be magnetic. |
| Streak | A weathered ordinary chondrite may leave a brownish-orange mark. | Hematite tends to leave a red-brown streak; magnetite, gray-black. |
| Interior | On a broken, cut, or polished face, an ordinary chondrite may show metallic flecks and small chondrules. | Other minerals and industrial materials can have distinctive internal textures too. |
The comparisons above are screening clues, not a validated scoring system. Do not add up features as though a certain number confirms a meteorite.
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No. Freshly fallen meteorites often develop a thin, dark fusion crust as they pass through the atmosphere, but the crust can wear away over time. Desert varnish can also create a shiny black coating on terrestrial rock. Color alone cannot distinguish the two. The Buseck Center for Meteorite Studies’ “How can I find a meteorite?” guidance addresses this common question.
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How can I check a rock safely at home?
- Compare the surface. Look for a thin coating and a compact texture. Note obvious holes or bubbles, which are common in volcanic rocks and may appear in slag.
- Compare its weight fairly. Hold it beside an ordinary rock of roughly the same size. “Heavy” is a relative impression, not a measurement threshold or proof of origin.
- Try a magnet gently. Attraction supports further investigation but does not establish that the rock is a meteorite. A weak response does not rule one out.
- Consider a streak test only as a clue. Rub the specimen on an unglazed ceramic streak plate, or the unglazed ring on the bottom of a coffee mug. Compare the mark cautiously: hematite often leaves red-brown, magnetite gray-black, and weathered ordinary chondrites may leave brownish-orange.
- Inspect an existing broken face, if available. Metallic flecks or small chondrules may be worth noting. Do not cut or polish the specimen unless a qualified expert advises it.
These preliminary checks can help decide whether to seek expert input; online observations and tests cannot conclusively identify a meteorite. See the Buseck Center’s Meteorite ID guidance.
What terrestrial rocks can look like meteorites?
Magnetite and hematite
Magnetite can be strongly magnetic and commonly leaves a gray streak. Hematite may look dark and tends to leave a reddish-brown streak. Either can confuse a visual or magnet check.
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Slag
Slag is an industrial byproduct that may be heavy and magnetic. Flow textures and gas bubbles can distinguish it from the usually compact meteorite appearance. It may be encountered in road or rail fill.
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Desert varnish can make an Earth rock appear black and glossy; some coated rocks may also be magnetic. Volcanic rocks commonly contain bubbles or vesicles, unlike the compact appearance described in meteorite identification guidance.
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- Fun meteorite kit includes 3 meteorites, a magnifying box and an Authenticity certificate/educational information card.
- These meteorites are 4,000 TO 6,000 YEARS old--each meteorite measures approximately 3/8-½ inch. The meteorites were found in Argentina and are composed mostly of iron with some nickel.
Where can you get a plausible specimen identified?
Contact a state geological survey, a geology department at a local college or university, or a natural history museum. The Buseck Center for Meteorite Studies at Arizona State University says its public Meteorite Identification Program was suspended in 2010 and that it no longer accepts specimens through that program; its identification guidance recommends those local institutions.
ASU notes that detailed microscopic, chemical, and mineralogical analyses are required to uniquely identify and classify a meteorite. A magnet response, streak, weight comparison, or photograph cannot provide that confirmation.
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- Uncover Hardness & Streak Traits: Perform Mohs hardness tests using talc, gypsum, and calcite with the glass streak plate; scratch coal and hematite on the plate to reveal their distinct streak colors for easy identification.
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