Rock Identifier
Andesine (Sodium calcium aluminosilicate ((Na,Ca)(Si,Al)4O8))
gemstone

Andesine

Sodium calcium aluminosilicate ((Na,Ca)(Si,Al)4O8)

An intermediate plagioclase feldspar between albite and anorthite, marketed as a red to champagne gemstone, sometimes color-treated.

Mohs hardness
6-6.5
Color
Pale gray, greenish, to red, orange and champagne in gems
Type
gemstone

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Overview

Andesine is a plagioclase feldspar lying in the middle of the albite-anorthite series, between oligoclase and labradorite. It was named for its occurrence in the andesite lavas of the Andes Mountains.

As a rock-forming mineral it is usually pale gray to greenish and unremarkable, but transparent andesine became prominent in the gem trade as red, orange, and champagne-colored faceted stones. The gem trade was marked by controversy because much red andesine was found to be artificially color-enhanced by copper diffusion, prompting disclosure requirements.

Naturally colored andesine and the related plagioclase sunstones do occur, but buyers should be aware of treatment history when purchasing red andesine gems.

Formation & geology

Andesine crystallizes from intermediate-composition magmas and is a defining feldspar of volcanic rocks such as andesite, as well as diorite and many intermediate igneous rocks. As a plagioclase it forms within the continuous solid-solution series, its composition reflecting the calcium-to-sodium ratio of the parent magma.

Gem-quality transparent andesine has been reported from localities including Mongolia, Tibet, and the Democratic Republic of Congo, though the natural color and origin of some red material has been disputed. As a major component of intermediate igneous rocks, andesine is geologically common worldwide even where gem material is not.

How to identify it

Andesine is a feldspar of Mohs 6-6.5 with two cleavages near 90 degrees, a vitreous luster, and a white streak. In rocks it is pale gray to greenish; gem material ranges from champagne and yellow to orange and red.

Like other plagioclase it may show fine albite twinning striations on cleavage faces. Distinguishing andesine from neighboring plagioclase members (oligoclase, labradorite) by eye is difficult and usually requires optical or chemical determination of composition.

For gem buyers, the key practical concern is treatment: copper-diffused red andesine can be hard to separate from natural without lab testing. Reputable testing and disclosure are the reliable way to confirm natural color.

Uses & significance

Andesine's main commercial use is as a faceted gemstone in red, orange, and champagne hues, set in rings, pendants, and earrings. Because of past treatment controversies, value depends heavily on whether color is natural and properly disclosed, and lab certification is recommended for fine red stones.

As a rock-forming plagioclase, andesine is geologically important in classifying intermediate igneous rocks. Collectors also seek natural gem crystals.

Metaphysically, andesine is marketed as a stone of energy, balance, and motivation, but these are promotional and traditional claims rather than verified properties. Its hardness allows jewelry use, though protective settings help guard against cleavage and scratches.

Frequently asked questions

Is andesine gemstone natural or treated?

Both exist. Much red andesine on the market was color-enhanced by copper diffusion, so reputable lab testing and disclosure are important when buying.

What kind of feldspar is andesine?

Andesine is an intermediate plagioclase feldspar in the albite-anorthite series, sitting between oligoclase and labradorite in composition.

Where does andesine come from?

It is common in andesite and diorite worldwide; gem material has been reported from Mongolia, Tibet, and the Congo, with some origins disputed.

How hard is andesine?

It is about 6-6.5 on the Mohs scale, hard enough for jewelry but with feldspar cleavage that warrants protective settings.