Photo of a Gibeon Meteorite

Photo of a Classic Iron Meteorite with Natural Patina and numerous indentations or "thumbprints".

Meteorite Identification

Welcome to Arizona Skies Meteorites® Meteorite Identification page. Over the years we have received literally hundreds, maybe even thousands of emails from people that were sure that they had found a meteorite. Unfortunately, out of all these suspected meteorites only few were actually real meteorites. How can one identify a suspected meteorite? We have developed this webpage as an introduction to meteorite identification. We recommend looking at a lot of photos of the real meteorites on our website. This will help you get a feel for what real meteorites look like. After you have done that, a little background information will be helpful.

Meteorites come in several distinct types. There are iron meteorites, stony meteorites (chondrites and achondrites) and meteorites that are a mixture of the two, stony-iron meteorites (pallasites and mesosiderites). The vast majority of all meteorites are stony meteorites known as ordinary chondrites. If you have found a real meteorite, it is most likely an ordinary chondrite.


Ordinary chondrites come in all shapes and sizes. Here are some Chondrite Photos. Some are so weathered that they look like an ordinary terrestrial rock while others are so fresh that they look like a charcoal briquette. Chondrites typically have some sort of fusion crust on their exterior and often contain tiny metal flecks made of an iron-nickel alloy which will cause magnets to be attracted to them. Chondrites, by definition, also contain a few to many Chondrules (see examples below).

Photo of a chondrite meteorite with a magnet attached to it.

Here is a highly weathered Franconia H5 Ordinary Chondrite with a rare-earth magnet stuck on to it. This specimen looks very similar to an ordinary rock, but...

Franconia Meteorite

When cut, the interior of the Weathered Franconia Chondrite shown above shows numerous iron-nickel metal flecks. These flecks attract magnets, and are characteristic of most Chondrite meteorites.


Oum Dreyga Chondrite

Photo of a freshly fallen Oum Dreyga Chondrite. Note the black fusion crust and light interior.

Oum Dreyga

A freshly fallen Oum Dreyga (Amgala) H3-5 Chondrite showing a light colored matrix filled with iron-nickel flecks.

Ordinary Chondrite with Fusion Crust

This is a typical, weathered Ordinary Chondrite. Note the dark brown fusion crust and the weathered, lighter colored interior.

Freshly fallen Chondrite meteorite

If you are ever lucky enough to find a freshly fallen chondrite this is what it might look like. Note the fresh black fusion crust and light interior.

Chondrite showing pronounced Chondrules

Some non-metamorphosed Chondrites show pronounced Chondrules (the small circular objects in the above photo). Note that this type of chondrite has few metal flecks.

Iron Meteorites

Canyon Diablo Meteorite

Photo of a Typical Iron Meteorite in "as found" condition. The white substance is Caliche. This meteorite is a Canyon Diablo IAB Octahedrite

The vast majority of meteorites contain some iron. This means that most meteorites will be attracted to a strong magnet such as a rare-earth or Neodymium magnet. Unfortunately there are many common Earth rocks that also contain iron and are attracted to magnets. This means that an attraction to a magnet, on its own, does not mean that a rock is a meteorite. Magnetite and hematite are two extremely common, naturally occurring iron ores that are often mistaken for iron meteorites. These minerals are especially abundant in the desert Southwest. There are also plenty of man made objects that are frequently mistaken for iron meteorites. These include shrapnel from bombs and artillery shells, cannon balls, milling balls (used to grind up ore bearing rock), ball bearings, and various types of industrial slag. To confuse things further some iron meteorites can be of a shrapnel type and therefore look identical to man-made shrapnel. So how can we distinguish iron meteorites? Here are a few tips:

1) Look at some Iron Meteorite Photos. Most iron meteorites will be covered in rust and maybe caliche as seen in the Canyon Diablo iron meteorite shown above. Often, iron meteorites will have indentations or "thumbprints" where parts of the meteorite were ablated during entry into the Earth's atmosphere. Occasionally an iron meteorite will be freshly fallen. Freshly fallen iron meteorites look similar to the Sikhote Alin meteorite shown below which fell in Eastern Siberia in February, 1947.

2) Iron meteorites are never round. If it is round or spherically shaped then it is probably a cannon ball, ball bearing or milling ball.

3) Iron meteorites are not grey inside unless they are extremely, extremely weathered, in which case they have little commercial value.

4) When cut, iron meteorites are a shiny silver color inside, just like a piece of freshly cut steel.

5) Most Iron Meteorites show a Widmanstatten Pattern when cut and etched. Note that Hexahedrite and Ataxite iron meteorites do NOT show any Widmanstattern. This type of pattern is unique to meteorites.

Sikhote Alin Meteorite

Photo of a freshly fallen Sikhote Alin iron meteorite. Note the thumbprints and smooth fusion crust.


Pallasites are a rare type of meteorite composed of an iron-nickel matrix filled with olivine crystals (see photos below) and for more photos see our Pallasite Photos

Photo of an Imilac Pallasite

Photo of the exterior of an Imilac Pallasite. Note the olivine crystals embedded in it.

Photo of an Imilac Pallasite

Photo of the interior of the same Imilac pallasite shown above.


Mesosiderites are another meteorite type that is composed of a mixture of stone and iron. They somewhat resemble a metal rich chondrite. If you have found a mesosiderite it should be fairly easy to identify. See photo below.


Photo of a large Mesosiderite. The lighter areas are all iron-nickel flecks and nodules.


Achondrites are a rare group of Stony meteorites lacking chondrules. Here are some Achondrite Photos. Unless your rock has an obvious fusion crust, it will require an expert and probably laboratory analysis to distinguish an achondrite from a terrestrial (Earth) rock.

Common Meteorite "Tests"

Many of the commonly cited Meteorite "Tests" on the internet are useless and counter productive, often producing false positive and false negative results. The so called Streak Test is non-diagnostic as typically implemented as there are many confirmed meteorites that will leave a streak on the back side of a tile from the oxidation on the exterior of the meteorite. In addition, in order to perform the streak test properly, you must cut the meteorite open to reveal unoxidized interior material with which to perform the test. This can destroy the value of the meteorite, especially those that are aesthetically shaped. This fact is almost universally omitted from websites promoting this so called test. Furthermore, there are many man-made objects that would pass the so called streak test if properly implemented such as pieces of shrapnel, cannon balls, and ore milling balls. For these reasons the Streak test is virtually useless in meteorite identification.

The inexpensive dimethylglyoxime "Nickel Test" is also virtually useless as it is extremely sensitive to even minute quantities of nickel and many common Terrestrial rocks will give false positives.


1) Most meteorites are attracted to strong magnets, though many common Earth rocks, such as iron ore, hematite and magnetite are also attracted to magnets.

2) Most meteorites are denser than the average Earth rock. In other words meteorites are typically heavier than Earth rocks of the same size.

3) Stony meteorites (Chondrites and Achondrites) often have an obvious fusion crust. It is not always easy for a novice to identify a real fusion crust, and many rocks found in the desert have a "desert varnish" which is often mistaken for fusion crust.

4) Chondrites often have numerous tiny metal flecks inside of them, causing them to be attracted to magnets. This is a characteristic that is nearly unique to meteorites.

5) Chondrites have Chondrules, although ordinary Earth rocks can also have inclusions that can resemble chondrules.

6) Iron meteorites are strongly attracted to magnets.

7) When cut, iron meteorites are a shiny silver color inside, just like a piece of freshly cut steel or iron.

8) Magnetite and Hematite are common Earth iron ores that many people are constantly mistaking for meteorites. When cut, magnetite and hematite have a rather dull grey color like pencil lead inside and not the shiny silver color of freshly cut iron meteorites.

9) Many, though not all, iron meteorites can be identified by etching. This process reveals the crystalline patterns (Widmanstatten patterns) that are characteristic of iron meteorites. We don't recommend trying to etch a suspected meteorite yourself as it can be hazardous. Have an expert do it for you.

10) Except for the very rare exception, meteorites do not contain bubbles. Many people confuse common volcanic rocks such as basalts for meteorites. Basalts typically are full of obvious bubbles and tend to be rather light for their size. Basalts can also attract magnets and set off metal detectors. If your rock is full of bubbles it is almost certainly not a meteorite.

11) Many of the standard "Meteorite Tests" are, in our opinion, not very useful, often producing false positive and false negative results. The so called "Streak Test" is non-diagnostic as there are many meteorites that will leave a streak, giving a false negative. The inexpensive dimethylglyoxime "Nickel Test" is also non-diagnostic as it is extremely sensitive to even minute quantities of nickel and many common Terrestrial rocks will give false positives.

We hope that you find this information helpful. Unfortunately, due our limited time resources and the large number of inquiries about meteor-wrongs we are no longer able to offer meteorite identification services.




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