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Natural Glass

Obsidian rough

Natural glass is formed naturally without the intervention of man. Its primary composition is silica with impurities. It (especially moldavite and snowflake obsidian) is used in carvings and beads.

Natural glasses are formed under different conditions and are basically made up of varying percentages of silica. The separation of natural glass from man-made glass is not possible with standard gemmological equipment. Obsidian, moldavite, crater glass and silica glass are variety of natural glass. The term Tektite has been used to represent all the natural glasses as a whole and also to define glasses of specific meteoritic origins.


Obsidian is a natural glass. It is formed from volcanic lava that cooled too quickly for significant crystallization to occur. Hence it is amorphous, with no cleavage; fracture is conchoidal. Obsidian is usually black, but brown, grey and more rarely red, blue and green material is found. The color may be uniform, striped, or spotted. Some inclusions give obsidian a metallic sheen, while internal bubbles or crystals (called crystallites) produce a “snowflake” effect (hence snowflake obsidian) or an iridescence seen as flashes of colour.

Obsidian is found in areas where there is, or has been, volcanic activity: for example, Hawaii (USA), Japan, and Java. Other localities include Iceland, Hungary, the Lipari Islands off Italy, the former USSR, Mexico, Ecuador, and Guatemala. Dark nodules found in Arizona and New Mexico (USA) are called “Apache tears”.

Obsidian has been used since the prehistoric times for making tools, weapons, masks, mirrors, and jewellery. The very sharp shards of the natural glass have been fashioned as blades, arrowheads, and daggers. Today most obsidian jewellery comes from North and Central America.

1.Chemical CompositionVaries, but 66% – 72% is silica
2.Colors / Varieties
  • Color: Black, grey, dark brown Transparency: Transparent to opaque.
  • Varieties: Rainbow obsidian with iridescent sheen; Flowering obsidian is black with white spherulitic inclusions.
4.Specific Gravity2.33 – 2.42
5.Optic CharacterIsotropic, S.R., A.D.R. (S.R.)
6.Refractive Index / Birefringence1.48 – 1.52 / Nil.
7.MagnificationGas bubbles, crystallite inclusions which are round, rod-shaped or coiled, fine silky striations (cat’s eye effect), color zoning and banding.
8.Geological OccurrenceFormed by the rapid cooling of volcanic lava.
9.SourcesSiberia, Mexico, Hungary, Hawaii, Japan, Iceland, Italy, U.S.A. (Nevada, Arizona – Yellowstone Park)


The first tektites were found in 1787 in the Moldau River in Czechosolvakia, hence their original name of “moldavites”. Other colour varieties of this natural glass have since been found in many different localities. Tektites are usually translucent, and occur in a range of colors from green to brown. Their surfaces are usually uneven or rough, with a distinctive lumpy, jagged, or scarred texture. Tektites do not contain the crystallites found in obsidian. They may, however, have characteristic inclusions of round or torpedo-shaped bubbles or treacle-like swirls.

The Moladu River in Czechoslovakia is now the only real known locality for green, transparent tektite. Tektites from Thailand have been carved as small, decorative objects, worn in the belief that they give protection from evil.

Several ideas have been put forward to explain the mysterious origin of tektites. One theory is that they came to Earth from outer space, melting as they passed through the atmosphere and thus forming their characteristic shape and surface texture.

A second theory is that the impact of a large meteorite caused the surrounding rocks to melt and scatter, with cracks and scars then appearing as they cooled.

1.Chemical CompositionUpto 75% silica, 10% alumina, with trace elements. Low water content (much lower than obsidian).
2.Colors / VarietiesBottle green, greenish brown, brown / Basically Tektites.
4.Specific Gravity2.30 – 2.40
5.Optic CharacterIsotropic, S.R., A.D.R. (S.R.)
6.Refractive Index / Birefringence1.49 – 1.51
7.MagnificationGas bubbles, swirl marks which are thick, very different from pastes. Total lack of crystallites.
8.Geological OccurrenceMeteoritic zones.
9.SourcesBohemia, Czech Republic, Peru, Ivory Coast of Africa, Australia, Malay Archipelago.

Crater Glass

1.Chemical CompositionCommonly fused silica (90%) with some impurities.
2.Colors / VarietiesGreenish yellow, black.
3.Specific Gravity2.10 – 2.30
4.Optic CharacterIsotropic, S.R., A.D.R. (S.R.)
5.Refractive Index / Birefringence1.46 – 1.54
6.MagnificationNumerous vesicles present (S.G. lower than other natural glasses).
7.Geological OccurrenceMeteoritic zones.
8.SourcesGermany, U.S.A. (Arizona), Central Australia, Saudi Arabia.

Silica Glass

1.Chemical CompositionPure silica (upto 98%)
2.Colors / VarietiesGreenish yellow is common, black.
4.Specific Gravity2.20 – 2.50
5.Optic CharacterIsotropic, S.R., A.D.R. (S.R.)
6.Refractive Index / Birefringence1.46 – 1.52
7.SourcesSandy deserts of Libya, Arabia, India (Rajasthan).
  • When a lightning bolt strikes the ground, thin tubes of fused sand are formed due to intense heat build-up. Fulgarite is the name given to such fused sand glasses.
  • Non-volcanic, extra terrestrial glass of meteoric origin is called a Tektite. Tektites are mostly found in Czech Republic, Australia, South-East Asia, West Africa, U.S.A. (Georgia – Texas).
  • In general, all natural glasses are sometimes clubbed together as Tektites.

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