Specimen at a glance
| Mineral | Natural silica glass (impactite) |
|---|---|
| Chemistry | SiO2 (about 98%) |
| Mohs hardness | ~6 |
| Crystal system | Amorphous (glass) |
| Locality | Great Sand Sea, western Egypt |
| Form | Raw / rough |
| You receive | The exact specimen pictured |
About this specimen
This is the large piece in our Libyan Desert Glass stock: a single, sizable chunk of the pale yellow natural glass that only occurs in one strewn field in Egypt’s Great Sand Sea. Most material that reaches collectors is small, wind-polished fragments, so a piece of this size is where you can actually see the internal character of the glass: streaky flow banding (schlieren), trapped bubbles, and the frosted, sand-blasted skin that comes from millions of years of desert wind.
It is sold as a rough specimen, not cut or polished, and you receive the exact piece pictured.
Why a large piece matters
Libyan Desert Glass is one of the very few natural glasses clear enough to be faceted, and gem cutters report that faceted stones over 10 carats are uncommon and over 25 carats rare (Sky Jems). Big rough is what makes those stones possible, and it is also what museums and serious tektite and impactite collectors look for, because larger pieces preserve more of the original melt texture.
Libyan Desert Glass: the newer science
- Impact, not airburst: for years the leading idea was a giant aerial explosion, described as a roughly 100-megaton-class airburst. In 2019, Aaron Cavosie and Christian Koeberl reported in Geology that zircon grains in the glass preserve evidence of reidite, a mineral that forms only under shock pressure. Their point: airbursts can melt the ground, but only a meteorite striking it creates the shock waves that form high-pressure minerals (Curtin University).
- The strewn field: the glass is scattered over an elliptical area of roughly 4,000 square kilometres between the dunes of the Great Sand Sea (Sky Jems).
- Tutankhamun’s scarab: the yellow scarab at the center of a pectoral from Tutankhamun’s tomb was long described as chalcedony. Italian mineralogist Vincenzo de Michele identified it as Libyan Desert Glass in 1998 (Sky Jems).
- What’s inside: under magnification the glass can show sub-microscopic cristobalite and lechatelierite, pure silica glass that forms only at extreme temperatures (Sky Jems).
Go deeper
Want the full story on Libyan Desert Glass: how it forms, how to identify it, and what makes a great specimen?
Read Libyan Desert Glass: The Complete Guide Shop all Libyan Desert Glass
Questions about this piece
What is Libyan Desert Glass?
Libyan Desert Glass is natural silica glass scattered across the Great Sand Sea of western Egypt, near the Libyan border. It formed about 29 million years ago from an extreme heating event, most likely a meteorite impact or airburst.
Where was it found?
This piece comes from Great Sand Sea, western Egypt. We list a locality whenever it is known, because where a mineral formed is part of its story and its value.
How hard is it, and how should I care for it?
It rates ~6 on the Mohs scale. Treat like glass: about Mohs 6 and brittle, so avoid drops and knocks. Wipe or rinse and air dry.
Is this the exact piece I will receive?
Yes. This listing was photographed individually, and you receive the exact piece shown in the photos.







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