How to Identify Meteorites With Pictures

Found a Rock From Out of This World? Have you stumbled upon a rock that seems strangely heavy or different from others you've seen? It might just be a visitor from space! Meteorites, remnants of asteroids, comets, or even planets, occasionally fall to Earth and can be exciting discoveries. But how can you tell if your rock is truly a meteorite?

Identifying a meteorite can be an exciting challenge, and using pictures can greatly aid in the process. To tell if a rock is a meteorite, start by examining its physical features and characteristics. Many meteorites are magnetic due to their iron-nickel content, but there are non-magnetic meteorites as well, making pictures of these invaluable for identification. Look for a fusion crust and check for regmaglypts, or thumbprint-like impressions on the surface. Meteorites like achondrites or stony-iron varieties might not match common assumptions, so detailed images of these rare types can be particularly helpful. Comparing your specimen to meteorite identification pictures of confirmed samples is an effective way to determine if you’ve found an extraterrestrial treasure.

Types of meteorites

Here's a step-by-step guide to help you determine if a rock is a meteorite:

Physical Characteristics

Weight and Density

Meteorites are usually denser than common rocks. Pick up the rock. If it feels unusually heavy for its size, it could be a meteorite.

Magnetism

Many meteorites contain iron and nickel, making them magnetic. Use a strong magnet (not a refrigerator magnet) to see if the rock isattracted to it. However, not all meteorites are magnetic, so a negative result doesn't rule it out.

Meteorite Magnetism

Exterior Appearance

Fusion Crust

Fusion Crust is a thin, black, glassy coating that forms on the meteorite's surface during its fiery entry into the atmosphere. It may be smooth or have melted bumps. Not all meteorites have a complete fusion crust, but its presence is a strong indicator.

Fresh meteorite fusion crusts are smooth, shiny, glassy, and darker colored than the inside of the meteorite.

Regmaglypts

Regmaglypts are shallow fingerprint-like depressions or indentations that form on the surface of some meteorites as they travel through Earth's atmosphere at high speeds. Swirling hot gas carves these smooth indentations. They aren't on every meteorite, depending on factors like size and entry angle. But their presence is a key clue for scientists studying a meteorite's extraterrestrial origins.

egmaglypts are shallow depressions or dimples that form on the surface of some meteorites as they pass through Earth’s atmosphere.

Examine the External Shape

Meteorites won't be perfectly round or smooth. They'll often have irregular shapes with melted or pitted surfaces. This is caused by the intense heat and pressure they experience during atmospheric entry.

Meteorites often have an irregular, not perfectly rounded shape due to ablation.

Meteorite Colors

Meteorites display a range of colors that can help in their identification.

Fresh Falls: These meteorites will typically have a black or dark brown colored exterior due to the presence of a fusion crust.

Weathered Meteorites: Over time, a weathered meteorite will lose its fusion crust due to exposure to the elements. This can cause the meteorite to develop a rusty appearance or take on a reddish-brown color. This rusting is caused by the oxidation of iron within the meteorite.

Iron Meteorites:

Exterior: Can show rust colors like red, orange, or brown when weathered.
Interior: Fresh cuts reveal a bright, silvery metallic sheen from nickel-iron.

Stony Meteorites (Chondrites):

Interior: Usually light to dark grey, sometimes with visible chondrules or metal flecks, potentially with brownish hues due to iron content.

Achondrites: Similar to stony meteorites but often lack chondrules; colors can vary but generally in the grey spectrum.

Stony-Iron Meteorites:

Pallasites: Green, yellow, or brown olivine crystals embedded in a silvery metal matrix when cut open.

Weathering Effects: Over time on Earth, meteorites might develop earthy tones like red or yellow from oxidation.

Meteorites display a range of colors that can help in their identification.

Interior Examination

Cut a Small Sample

If possible, cut a small piece of the rock to examine the interior. Meteorites often have a different appearance inside compared to the outside. It's important to note that cutting a meteorite is destructive and should only be done on small, non-museum quality specimens.

Cut a Small Sample of meteorite

Metallic Flecks

Shiny, metallic grains within the rock are a strong indication of iron and nickel, common components in meteorites.

Meteorite Metallic Flecks

Chondrules

If the meteorite is a chondrite (the most common type), you might see small, round mineral inclusions called chondrules. These are believed to be the building blocks of planets and asteroids.

chondrite meteorite, Identify Meteorites

Chondrules Meteorites

Widmanstätten Patterns

This is a special feature seen only in iron meteorites. When a polished surface of an iron meteorite is etched with a mild acid, it reveals a beautiful, interwoven crystalline structure called a Widmanstätten pattern. This pattern is a result of the slow cooling of iron and nickel within the meteorite over millions of years.

Widmanstätten Patterns meteorite

Chemical Composition

Nickel Test: Meteorites often contain nickel. Use a chemical test kit to check for the presence of nickel.

Expert Verification

Contact a Meteorite Expert: If your rock passes the initial tests, contact a meteoritics laboratory, museum, or university with a geology or planetary science department. They can provide a definitive analysis.

Submit for Classification: If confirmed, you can submit the meteorite for classification and official documentation.

Tips and Warnings

Be Cautious with Assumptions: Many terrestrial rocks can mimic meteorite characteristics, such as slag from industrial processes.

Preserve the Sample: Handle the rock minimally to avoid contamination and preserve its characteristics for accurate testing.

Summary

Visual Inspection: Look for fusion crust, shape, surface features.
Magnet Test: Check for magnetism.
Density Test: Compare weight and density.
Streak Test (optional): Perform a streak test on ceramic.
Interior Examination: Look for metallic flakes and chondrules.
Chemical Testing: Test for nickel and reaction with acid.
Professional Verification: Seek expert analysis and laboratory testing.

By following these steps, you can systematically determine if a rock is a meteorite. However, the final confirmation often requires expert analysis to rule out all possibilities of terrestrial origin.