How to identify a meteorite from a rock photo

You can often rule out common rocks from a photo and spot key clues to whether a specimen might be a meteorite. A common surface feature to look for is Fusion crust: thin dark rind, visible as a smooth, dark outer skin on many meteorites.

Quick facts

Fusion crust
Fusion crust: thin dark rind
Widmanstatten
Widmanstatten pattern in iron meteorites

Visual signs to check in the photo

Start with clear close-up images. Look for a smooth, dark outer skin; this is the Fusion crust: thin dark rind. Also check for shallow thumbprint-like depressions (regmaglypts), a generally rounded shape, and a matte or slightly glossy surface that differs from typical sedimentary textures. Include shots of every side and an interior if available.

Metal and internal structure clues

Many meteorites contain metal. If the photo shows shiny metal flakes or a polished cross-section, that can indicate an iron-rich specimen. A diagnostic internal structure is the Widmanstatten pattern in iron meteorites; that pattern appears in polished, cut faces and is not expected on ordinary mineral or gemstone cross-sections. Note that the pattern normally requires a polished surface to appear in photos.

Common look-alikes to exclude

Exclude things that commonly mimic meteorites: industrial slag (often vesicular or glassy), terrestrial rocks with weathered dark coatings, and polished gem or crystal specimens. A gemstone or crystal with a smooth, faceted face is not a meteorite. If the specimen looks like a manufactured object or shows obvious crystalline cleavage like many minerals, treat it as a mineral or gem rather than a meteorite.

How to take diagnostic photos

Use even lighting, a neutral background, and include a scale (coin or ruler) in every image. Capture: an overall view, close-up of the surface texture, an edge shot to show thickness, and any internal faces or broken areas. If the specimen is flat, a scanner can provide a high-detail image. Photograph a magnet next to the specimen when testing magnetic attraction so reviewers can see both.

Next steps and expert review

From a photo you can often narrow possibilities, but final recognition usually requires physical tests: magnetism, density, a cut or polished section, and microscopic inspection. Keep clear photos and provenance notes (where it was found, who the finder was). If you want external verification or to learn about potential value or worth, send high-quality photos to an expert for appraisal. For a fast check, consider uploading your images to Rock Identifier.

Common questions

Can a single photo prove a rock is a meteorite?
A single photo can suggest a meteorite but rarely proves it. Photos are useful for spotting fusion crust, metal, or distinctive shapes, but physical tests (magnetism, density, cross-section inspection) are normally needed for conclusive identification.
Is a magnet test conclusive from a photo?
No. A magnet shown in a photo can demonstrate that the specimen attracts a magnet, which is a useful clue, but some terrestrial rocks and industrial slag are magnetic. A magnet test is a step, not a final proof.
When should I get a polished cross-section photographed?
If you suspect an iron meteorite, a polished and etched cross-section can reveal the Widmanstatten pattern in iron meteorites, which is diagnostic. Only have this done by someone experienced, and photograph the polished face under diffuse light.

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