The Association of Lunar & Planetary Observers
Meteorite Section

Acting Coordinator
Dolores H. Hill
Lunar & Planetary Lab.
Univ. of Arizona
Tucson, AZ 85721

Meteorite or Meteorwrong... the Path to Identification



Connection to other ALPO sections

Meteorites are tangible samples of the Solar System objects traditionally studied by ALPO members. They provide a connection to other ALPO Sections such as the Meteors, Minor Planets, Comets, Lunar, Mars, and even Solar (as implanted solar gases). However, this new Section will differ from the other Sections in that the subject is not conducive to archiving and disseminating "regular observations". Instead, the purpose of the Meteorite Section will be to educate the interested amateur astronomer, provide information about meteorites, dispel misconceptions, and direct those with possible meteorites to knowledgeable resources.

The main tool of the new section will be the ALPO website which will feature answers to Frequently Asked Questions. Links to other useful web sites will be available. Additional information will be posted on new developments in the field of meteoritics and noteworthy meteorites. From time to time articles and reports will appear in the JALPO. The latter may provide an opportunity for ALPO members to study meteorites, compare collections, share the excitement of meteorites, and relate interesting stories of their falls and recoveries. Below are samples of topics to be addressed.

Naming of meteorites...

Unlike astronomical bodies, meteorites are not named after their discoverers or even famous scientists. They are named after geographical features, towns, or regions. Attempts are made to use names that are not likely to change and are easily identifiable. It is only recently that some standardization has been applied to the naming and official recognition of meteorites. The Nomenclature Committee of the Meteoritical Society is the official body for approval of names and classifications of meteorites.

Where are Meteorites Found?

Meteorites generally fall at the same rate over the entire earth. Because the earth is mostly water, most of them are lost. They are recovered wherever people live and travel. This is evident on maps of meteorite recoveries as "paths" during the building of large railroad and road building projects. Meteorites are best preserved in dry environments where weathering and rusting is relatively slow. They are also more easily seen against light colored soils and sparse vegetation. In more temperate climates, meteorites begin to rust immediately after falling and are subject to destruction from plant roots as well.

Thousands of meteorites have been found in Antarctica and the Sahara in the last 20 years. This is more than was known previously from the entire world. Not only have these meteorites expanded the known types but, they have increased our knowledge of ancient meteorite falls. They have provided evidence of the timing of breakup and types of asteroid parent bodies that produced the specimens in our laboratories.

Meteorite Types & Classification

Contrary to popular misconception, not all meteorites or asteroids are metallic. In fact, most of the meteorites that fall on the earth are stony meteorites called chondrites. They are named after tiny objects or inclusions in them called chondrules. These are spherical, ~1 millimeter diameter, silicate inclusions formed early in the formation of the Solar System as the Solar Nebula coalesced; before any of the planets or asteroids formed. Indeed, chondrites are the oldest rocks you can hold! Other meteorite types represent a wide variety of conditions and processes on various parent bodies. They provide valuable insight into the Solar System's past throughout space and time. Iron-nickel and stony-iron meteorites sample deep interiors of once large asteroids. They are used as analogs for our own earth's core and mantle. Other meteorites are brecciated; composed of broken fragments of asteroid collisions whose record has been frozen in place.

The details of the meteorite classification scheme will not be discussed here. As alluded to above, there are three main types: stony, stony-iron, and iron-nickel. Each of these broad categories are broken down into many types based on their mineral and chemical compositions. The age old battle between the "lumpers" and the "splitters" is carried out as similarities and differences between individual meteorites are learned. Scientific lumpers look for similarities between samples and put them together in a category; splitters look for differences between samples and create separate classifications or categories. As more meteorites are recovered and we sample more Solar System parent bodies, more sub-types seem to be required until a unifying explanation can be found. The three main types of meteorites are readily discernable by eye but, sophisticated instruments are required to determine an exact classification. Sometimes, lengthy trace element analyses are required to distinguish between some meteorite classes.

Where do Meteorites Come From?

We know that the meteorites in our scientific collections primarily sample the asteroid belt between Mars and Jupiter. This is known from orbits calculated of fireballs that were photographed, and later recovered. There is evidence that some meteorites were formed at different distances from the sun. It is possible that the carbonaceous chondrites are related to comets that sweep into the inner Solar System. They are "primitive" chemically (unchanged since their formation early in Solar System history) and contain minerals tha have been exposed to water. We have been able to conclusively identify "lunar meteorites" from their unique chemical signatures because we have real samples of moon rocks from the U.S. Apollo and Soviet Luna missions. Martian meteorites or "SNCs", named after the three type meteorites, Shergotty, Nakhla, and Chassigny, were first known from compelling circumstantial evidence. As more compositional data from the surface of Mars becomes available, the connection is even stronger. We do not think we have samples of Mercury or Venus but, meteoriticists have thought about what kinds of compositions would be expected. It is even suspected that we have a few grains trapped in carbonaceous chondrites that sample material from a different solar system!

How is a meteorite identified?

The most important comment to be made about meteorite identification is that it ranges from very easy for those with "classic" fusion crust to very difficult for older finds and/or unusual types. The specific classification of a particular type of meteorite requires chemical analyses by an institution with access to an electron microprobe and/or a trace element laboratory. It is interesting to note that meteorites contain the same elements and, with some important exceptions, similar minerals as are found on the earth.

Physical appearance: fresh falls vs. old finds

The first indication that a rock may be a meteorite is its outer surface. A fresh fall, i.e. a meteorite that is seen to fall and soon recovered, will exhibit a black surface. This outer coating or "fusion crust" is less than 1 mm thick. It ranges from a matte black luster to a glassy black depending on the stone's composition. The fusion crust is the last, quenched, outer layer of the meteorite as it passes through the atmosphere. It is an often misunderstood feature. Real fusion crust usually doesn't look particularly melted or vesicular. Fortunately for scientists, most of the interior is well preserved and not harmed by the heat of atmospheric passage. At the Lunar & Planetary Lab, University of Arizona, we see many lumps of magnetite, volcanic rocks, slag, and even rocks containing calcite that are brought in because they "look melted".

Meteorites that are old "finds" will have lost the beautiful black color to the fusion crust. Because meteorites are immediately attacked by Earth's atmosphere and moisture, they oxidize (rust), weather, and erode. They often have an ugly, rusty, brown exterior that may be broken and severely cracked. Some, although rusted, may retain traces of the original fusion crust.


While it is true that meteorites are more dense than terrestrial rocks, it is a poor criterion. Earth rocks containing mixtures of minerals, ores, and basalts may, by chance, have a similar measured density. Iron meteorites will be very heavy for their size, but iron-rich slag and magnetite will be heavy also. Some stony meteorites may be indistinguishable in the field from other rocks if density alone is considered.

Magnetic properties

Iron-nickel meteorites are strongly magnetic but stony meteorites will be much less attracted to a magnet. Most stony meteorites contain small grains of iron-nickel metal. They will be detected by a well tuned metal detector even several inches below the surface. Unfortunately, many ordinary rocks also exhibit magnetic properties. Rocks which are strongly magnetic on one part but, not on another, are terrestrial volcanic rocks, basalts, or other iron-rich rocks and industrial slag. So, magnetism alone is not a very useful discriminator.

In summary, exterior appearance, density, magnetism, while useful aids, do not provide definitive tests by themselves. Unless a specimen is obviously terrestrial or obviously a meteorite, a cut is required to reveal the interior secrets. The first indication of a stony (chondrite) meteorite is the presence of small, reflective metal grains or flecks in a silicate groundmass. This groundmass can range from a light gray color to dark black. Some but, not all, chondrites will exhibit ~1mm diameter, circular, chondrules. Most people greatly overestimate how large these are and often mistake sand grains in earth rocks for chondrules. Other, rarer, stony meteorites require careful microscopic or chemical analysis by a meteorite laboratory.

Iron-nickel meteorites when cut will have a "nickel color". This can be difficult to assess. A bluish hue to the metal or glassy, melted-looking inclusions with vesicles indicate a manmade metal or slag. The famous Nital etch can reveal the Widmanstatten pattern in a metal meteorite. This criss-cross pattern is diagnostic of a meteorite because it is formed only by very slow cooling in the interior of an asteroid. Often metal meteorites are positively identified by analysis of their iron and nickel content with an electron microprobe. A large amount of calcium, manganese, copper, zinc, silicon, indicates a manmade origin.

Common meteorwrongs

The most common meteorwrongs include magnetite, a black, heavy, magnetic rock, industrial slags of all descriptions, old iron farm implements, iron rich rocks, and volcanic rocks. Many brown or black rocks are sent to labs in hopes that they are meteorites. Knowledge of the geologic or geographic setting can be important in any explanation of the true nature of a meteorwrong. For example, many rocks from deserts display a thin, black coating called desert varnish that can look very much like fusion crust but, is actually a terrestrial manganese oxide.

Testing laboratories

Meteorite laboratories are usually associated with universities. They routinely examine possible meteorites. Not all geology departments and not all geologists have experience with meteorites. Reputable meteorite dealers are also qualified to identify common meteorites. They, too will seek out scientific contacts for unusual rocks or meteorites. I have never known of a dealer to be dishonest, that is, to tell a person that they do not have a meteorite if they know it to be one. It may be disappointing to be told that your find is an ordinary rock but, be assured that there are plenty of real meteorites waiting to be found, and more falling every day.

Because meteorite laboratories must examine possible meteorites in between their regular work, there is no set time frame for completion. An instant answer is usually a "no". Longer delays indicate that the sample is "in the queue" and may not have been examined right away. Or it may mean that it is a difficult to identify specimen that may or may not be a meteorite after lengthy analyses. Certainly, any unusual or rare meteorites are given highest priority.

The scientific record

The official recognition and naming of meteorites is carried out by the Nomenclature Committee of the Meteoritical Society. It has set forth rules that must be followed by institutions submitting information for new meteorites. (See below). New meteorites are announced in the Meteoritical Bulletin several times per year. A preliminary version is posted on a website and the final, official version is published in the journal, Meteorites and Planetary Science (MAPS). The Catalog of Meteorites is a compilation of the Bulletins that has been published in book form approximately every 10-20 years. Not only does it give one great satisfaction to contribute to the scientific record but, there is added satisfaction in seeing your name as the finder and/or owner of the main mass of a newly discovered meteorite.

Other than for the sake of the scientific record for future generations, why go through the trouble to have a meteorite properly classified and recognized? One reason is that if you ever wish to sell it, you will obtain a higher price for an officially recognized specimen with a real, scientific classification. Without one, dealers understandably will pay the "market price" for the least valuable type. If it turns out to be one of the rare types of meteorites, they will be elated and you will have missed an opportunity. Be forewarned, though, that while most meteorites are ordinary chondrites, they also are not extremely valuable either. Too often meteorite owners hope that theirs will allow them to retire or buy a vacation home, etc. because of sensational T.V. programs that emphasize the rarest types. The best way to enjoy a found meteorite is to appreciate its scientific significance and proudly display the specimen.


Meteorite collections are found all over the world. They are housed in large and small museums, planetariums, universities, and private collections. Museum collections are primarily for display and educational purposes. They do occasionally provide specimens to researchers. Universities and other institutions such as NASA-Johnson Space Center, maintain collections for the purpose of scientific research. They may be more specialized and, therefore, often contain smaller or fewer samples than most collections. The Smithsonian Institution is an example of one that plays a role as both museum and research facility.

The most important part of any collection is to preserve the meteorites, keep the original identifying labels with the specimen and to keep an inventory list.Private collectors include amateur astronomers and mineral collectors who just enjoy the idea of holding and preserving a piece of an asteroid. Some attempt to collect an example of every "type" of meteorite; some concentrate on falls; some collect them by alphabet A to Z; some collect all meteorites found in one particular state or country; some desire only the rarest samples to fill out their collections. Many collectors are discovering the joys of thin sections; 30 micron thick, polished slices that reveal a new world under the microscope.

Collectors include commercial meteorite dealers who have built beautiful collections of both museum quality specimens and smaller pieces suitable for the amateur and scientist. They, too have their favorites that are considered part of their "private collection". Dealers often cultivate a symbiotic relationship with scientific institutions and are thankfully very generous to them. They provide an educational role to the public as well.

The new ALPO Meteorite Section hopes to provide links to images and information on various collections and museums. A photo is helpful but, nothing beats seeing examples of the real thing. The Section will educate and guide those who wish to pursue the study of meteorites. Just as there are new meteorites falling from the sky every day, there is always something new to be learned.

What to do if you think you have found a meteorite?

Do's and Don'ts of meteorite preservation

The most important advice one can give about meteorite preservation is that least is best! Never(!) attempt to remove fusion crust or soil unless the latter rubs off very easily by hand. Fusion crust protects the sample and its presence is highly prized by other collectors. It is best to leave any cutting to professionals who have special saws, thin diamond sawblades, inert diamond polishing compounds, and access to high purity chemicals. It is difficult for the average well-meaning person to know how a sample may become contaminated for scientific studies or preservation.

In dry climates, only polyethlyene bags or plastic boxes and desiccant stored with the specimens may be needed. However, in moist climates, sealed containers and cabinets with desiccant may be required to prevent atmospheric attack of a collection. Certainly, moisture and oxygen present the most serious threats to any meteorite. One must be careful not to seal in moisture during storage. High temperatures to drive off moisture should be avoided as they may also alter the chemical properties of a meteorite for age dating. Several iron- nickel meteorites display altered or lost Widmanstatten patterns due to reheating by their finders.

Some collectors resort to coating their iron-nickel specimens with special varnishes and lacquers, and even soaking in penetrating oils. Oils may ooze out as time passes - or if placed into any analysis instrument that uses a vacuum. (Dealers will sometimes use varnishes to protect a specimen that will be on display in a humid climate. They will always inform you). As a scientist with an eye to future studies and techniques, these are met with mixed enthusiasm. Some may preserve a specimen but, render it useless for any scientific studies. The alternative is a rusty pile of debris. A person may not intend for a specimen to be studied but, 20 or 50 years from now it may be the only known piece of an important sample. For instance, the ALH 84001 martian meteorite and its claimed nanofossils; much of the scrutiny depended on how it was collected, stored, and subsequently handled. It was one of the "difficult" meteorites to classify and was later discovered to be martian because it was included in a study of other rare meteorites.

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