Real or fake moldavite: how to tell before you buy
Few stones are faked as often as moldavite. It is rare, it is expensive, and demand has run far ahead of supply, which is exactly the combination that draws counterfeiters. A large share of the "moldavite" sold online, especially on big marketplaces, is simply green glass. So if you are going to buy moldavite, knowing how to read a genuine piece isn't optional; it is the difference between owning a real piece of impact history and owning a melted bottle.
This guide explains what moldavite actually is, why that makes it hard to fake convincingly, and the specific things to look for before you spend real money.
What moldavite actually is
Moldavite is a tektite: a natural glass formed by a meteorite impact. About 15 million years ago, a large meteorite struck what is now southern Germany, creating the Nördlinger Ries crater. The heat and force of that impact melted the surrounding rock and flung molten material high into the air, where it cooled into glass as it fell. The pieces that landed in what is now the Czech Republic, mainly in Bohemia and Moravia, are what we call moldavite.
A few things follow from that origin, and they matter for spotting fakes:
It is genuinely glass, not a crystal. Moldavite has no crystal structure; it is amorphous, like obsidian or window glass. So it isn't a "mineral" in the strict sense; it is a natural glass, sometimes called a mineraloid. That is why it has a glassy look and breaks with the smooth, curved fracture you see in glass.
It is found in only one small region on Earth. Genuine moldavite comes from that Czech strewn field and nowhere else. Any seller offering moldavite from other countries, or in unlimited quantities, is a reason to be cautious.
Its colour comes from trace iron. Real moldavite is a soft, muted olive to forest green, sometimes with a brownish tone. It is not the bright, uniform green of a beer bottle.
The physical facts, for reference
Genuine moldavite sits in a fairly tight set of measurable properties: a Mohs hardness of roughly 5.5 to 7, a specific gravity of about 2.32 to 2.40, and a refractive index around 1.48 to 1.54. Because it is a glass, it is isotropic, meaning it does not show double refraction. Most genuine pieces are small; large carved pieces and big flawless stones are uncommon, and very large "moldavite" carvings are a common form of fake.
You don't need to memorise these numbers, but they explain the tells below.
How to tell real from fake
No single test is foolproof, so the honest approach is to look at several things together. The more boxes a piece ticks, the more confident you can be.
Colour. Real moldavite is a muted, slightly dull olive or forest green, often uneven, sometimes with brown tints. Fakes are frequently too bright, too vivid, or a flat uniform green like bottle glass. If the green looks like glowing, glassy emerald, be suspicious. Always judge colour under natural light against a white background, since seller photos can mislead.
Surface texture. This is one of the strongest tells on a raw piece. Genuine moldavite has a distinctive natural sculpturing: irregular grooves, pits, wrinkles, and channels, often described as fern-like or resembling flowing water. These came from millions of years of weathering and etching in the ground, and they are irregular in a way that is very hard to fake. Molded glass copies tend to look too even, too repetitive, or too deliberate, because they came out of a mould rather than out of the earth. Run your finger over a real piece and the pattern feels random; a fake often feels uniform.
Internal bubbles. Both real moldavite and glass fakes can contain bubbles, so bubbles alone prove nothing. What matters is how they look. Genuine moldavite tends to show small, irregular, sometimes stretched or elongated bubbles, along with internal flow lines and swirls from the molten glass moving as it cooled. Manufactured glass usually shows bubbles that are large, perfectly round, and evenly spaced. Perfect spheres are a warning sign.
Size and form. Most genuine moldavite is small; pieces over about 50 grams are relatively uncommon, and large, heavy, intricately carved "moldavite" should be treated with real suspicion. Faceted moldavite is not automatically fake, but cutting removes the natural surface texture that is one of the best authentication tools, so for faceted or carved pieces, provenance matters more.
Price and source. Moldavite is expensive because it is rare. If a deal looks too good, that is itself a red flag. Buy from sellers who can tell you the specific locality, photograph the exact piece you will receive rather than using stock images, and don't manufacture false urgency. A trustworthy seller will stand behind authenticity.
A note on the hardness test
You will sometimes see a scratch test suggested, on the logic that glass fakes may be softer. In practice this is a poor idea: moldavite and many glasses overlap in hardness, the test can damage a genuine piece and reduce its value, and it rarely gives a clear answer. Texture, colour, internal structure, and provenance tell you far more, without harming the stone.
The honest bottom line
Moldavite is one of the most counterfeited stones on the market, and even experienced buyers can be fooled by a good fake in a photo. The single best protection is to buy from a seller who shows you the actual piece, tells you where it is from, and doesn't rely on hype. No internet test replaces a clear, well-lit look at the real specimen and an honest description of what it is.
That is exactly how we think a stone like this should be sold: the genuine piece, photographed as the piece you will receive, with its origin and nature stated plainly. With something this easy to fake, that honesty is the whole point. Know what you own.
Sources: Formation, locality, and physical properties (Mohs hardness, specific gravity ~2.32–2.40, refractive index, amorphous/isotropic structure) per Wikipedia's moldavite entry and Rock & Gem Magazine, consistent with tektite reference literature. Identification tells (surface sculpturing, bubble structure, colour, size) cross-checked across multiple gemmological and collector sources.