How to identify a meteorite
Updated . Based on the USGS, university meteorite labs and BLM policy; sources are at the end.
Start with the fusion crust, a thin, dark skin that forms when the outside melts on the way through the atmosphere: Washington University’s meteorite lab says that without one there is no reason to suspect a meteorite. Then try a magnet and a streak test on unglazed ceramic, and look for quartz or bubbles, which rule a meteorite out. Even if everything fits, only an expert who examines the rock itself can confirm it.
- Fusion crust
- Thin, dark skin, rarely over 1–2 mm
- Magnet
- Most meteorites attract one, but so do many Earth rocks
- Streak
- None, or faint gray, on unglazed ceramic
- Rules it out
- Visible quartz, gas bubbles, a red or black streak
Seven checks
The first column is the USGS checklist; the caveats come mostly from Washington University in St. Louis.
| Check | Points to a meteorite | But |
|---|---|---|
| Fusion crust | A thin, dark crust where the outside melted on the way through the atmosphere | Rarely more than 1–2 mm thick. Desert varnish and dark, polished rocks look similar, but they are the same color inside. |
| Magnet | Most meteorites attract a magnet; a stony one may only pull a magnet hung on a string | Many Earth rocks and slag attract a magnet too. Use a cheap fridge magnet, not a strong neodymium one. |
| Streak | No streak on unglazed ceramic, or a faint gray one if pressed hard | No streak does not prove a meteorite: igneous Earth rocks leave none either. |
| Weight | Usually heavy for its size, because of metallic iron | A weak sign: some Earth rocks are denser, and most “heavy” finds are iron-oxide concretions. |
| Shape | Iron meteorites are rarely rounded and often have thumbprint-like pits called regmaglypts | Not all meteorites have them, and Earth processes make similar dimples. |
| Quartz | No visible light-colored crystals such as quartz | A rock that cuts a deep scratch in glass is not a meteorite. |
| Bubbles | No gas bubbles | Volcanic rock and slag are often bubbly. Very few stony meteorites have small, sparse holes; iron ones sometimes have holes. |

Doing the tests
- Fusion crust: wet the rock. The crust is almost always darker than the wet interior; carbonaceous chondrites are the exception.
- Magnet: a cheap ceramic fridge magnet. Phone apps that measure magnetism are useless for this.
- Streak: scrape the rock on the unglazed back of a white tile or the ring under a coffee mug. Red or red-brown means hematite; dark gray to black means magnetite.
- Metal pieces: metal that does not strongly attract a ceramic magnet is not a meteorite. Metal that does needs a lab test for iron, nickel and other elements.
Common meteorwrongs
- Iron-oxide nodules and concretions: the most common meteorwrong sent to Washington University.
- Hematite and magnetite: two common look-alikes, according to Arizona State University. They leave a red or dark streak.
- Slag: an industrial by-product, often magnetic and bubbly, and common because it is used as fill for roads and train tracks.
Can an app or a photo tell?
No. Washington University in St. Louis says AI image apps cannot identify meteorites, and that image searches are nearly always wrong when they suggest one. The USGS says rocks and minerals are extremely difficult to identify from photographs, and Arizona State University says online testing alone cannot conclusively identify a meteorite.
Where to get it checked
- Local experts: the USGS does not verify meteorites. It suggests your state geological survey, a natural science museum, a college or university geology department, a rock shop, or a gem and mineral club.
- Portland State University: its Cascadia Meteorite Laboratory asks you to read its identification pages, then email a couple of in-focus photos. It does not want samples mailed without permission, phone calls or visits. Its instructions.
- Don’t mail samples to Arizona State University’s meteorite center, which stopped public identification in 2010 and will not return specimens. The University of New Mexico’s Meteorite Museum does not inspect suspected meteorites.
Can you keep it?
- BLM land: a 2012 BLM policy allows casual collecting without a permit, up to what you can easily hand-carry and 10 pounds a year, surface only, metal detectors allowed, for personal use. Its header shows a 2013 expiry, and we found no replacement, though BLM Arizona’s rockhounding brochure repeats the 10-pound limit. Check with the BLM.
- No casual collecting on National Park Service, Bureau of Reclamation or Fish and Wildlife Service land.
- Private land: according to the BLM, courts have long held that a meteorite belongs to the owner of the land surface where it is found.
- National forests: we found no rule; ask the forest.

Keep a log of your finds
The Capyhound app will save each find with its photo, place and date, even with no signal.
Questions
How can I tell if a rock is a meteorite?
Signs that point toward one, according to the USGS: heavy for its size, attracts a magnet, a thin dark fusion crust, and thumbprint-like pits on iron meteorites. Signs against: visible quartz, gas bubbles, and a black or red streak on unglazed ceramic. Even then, only an expert who examines the rock can confirm it.
If a magnet sticks, is it a meteorite?
Not necessarily. Most meteorites attract a magnet, but so do magnetite-rich Earth rocks and slag. Washington University in St. Louis suggests a cheap fridge magnet, not a neodymium one, which attracts many Earth rocks.
What is the streak test?
Scrape the rock on the unglazed back of a white tile or the ring under a coffee mug. Meteorites leave no streak, or a faint gray one. A red or red-brown streak means hematite; dark gray to black means magnetite. No streak does not prove a meteorite.
What is a fusion crust?
A thin, dark skin that forms when the outside of a meteorite melts on its way through the atmosphere. It is rarely more than 1–2 mm thick.
Can an app or a photo identify a meteorite?
No. Washington University in St. Louis says AI image apps cannot identify meteorites, and the USGS says rocks are extremely difficult to identify from photographs. An expert needs to examine the rock itself.
Where can I get a suspected meteorite checked?
The USGS suggests your state geological survey, a natural science museum, a university geology department, a rock shop or a gem and mineral club. Arizona State University’s meteorite center stopped public identification in 2010, and the University of New Mexico does not inspect suspected meteorites. Portland State’s lab reviews photos sent by email first and accepts samples only with permission.
Can I keep a meteorite I find on public land?
A 2012 BLM policy allows casual collecting on open BLM land without a permit: up to 10 pounds per person per year, surface collecting only, metal detectors allowed, for personal use only. It does not allow casual collecting on National Park Service, Bureau of Reclamation or Fish and Wildlife Service land. The policy document shows a 2013 expiry date, so check with the BLM before you rely on it.
Sources
- USGS: I think I found a meteorite. How can I tell for sure?
- USGS: Can you identify my rock or mineral?
- Washington University in St. Louis, Earth, Environmental, and Planetary Sciences: Some meteorite realities
- Washington University in St. Louis: Magnetic attraction
- Washington University in St. Louis: Streak
Show 7 more sources
- Arizona State University, Buseck Center for Meteorite Studies: Meteorite ID
- Arizona State University, Ask An Earth and Space Scientist: Identifying meteorites
- Portland State University, Cascadia Meteorite Laboratory: possible meteorites (modified November 28, 2023)
- University of New Mexico: Meteorite Museum and Collection
- BLM Instruction Memorandum 2012-182, Collection of Meteorites on Public Land (September 10, 2012; header shows expiry 09/30/2013)
- BLM: FAQs on Meteorites on Public Land (attachment to IM 2012-182)
- BLM: Rock Hounding in Arizona, BLM/AZ/GI-14/009

