
Ruby in Zoisite
Zoisite (Ca2Al3(SiO4)3(OH)) with ruby (corundum, Al2O3)
A striking rock of green zoisite studded with red-pink ruby crystals and black hornblende, also called anyolite.
- Mohs hardness
- 6-7 (zoisite ~6.5, ruby 9)
- Color
- green zoisite with pink-red ruby and black hornblende
- Type
- metamorphic
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Overview
Ruby in zoisite, known by the trade name anyolite, is a metamorphic rock combining bright green zoisite, opaque pink-to-red ruby (gem corundum), and usually black flecks of hornblende amphibole. The bold green-and-red contrast makes it a favorite for carvings and ornamental stones.
It was first described from the Longido region of Tanzania, which remains the principal source. The name anyolite comes from the Maasai word for green, anyoli.
The rubies in this material are opaque to translucent and rarely facetable, but the combination is valued for its striking ornamental appearance rather than for gem-quality ruby.
Formation & geology
Ruby in zoisite forms under high-grade metamorphic conditions where aluminum-rich rocks are altered at high temperature and pressure. Corundum (ruby) crystallizes in chromium-bearing, silica-poor environments, while the surrounding calcium-aluminum silicate recrystallizes as green zoisite.
The classic deposits occur in the metamorphic belts of northern Tanzania, particularly around Longido and the Mundarara mine, where ruby corundum grew within zoisite-amphibole host rock.
The green color of the zoisite and the red of the ruby are both linked to trace chromium and vanadium, while the black accessory mineral is typically a hornblende-group amphibole (sometimes called tschermakite).
How to identify it
Look for an opaque rock with vivid grass-green zoisite hosting rounded or hexagonal pink-red ruby crystals and scattered black spots. The color trio is distinctive and hard to confuse once seen.
The ruby portions are extremely hard (Mohs 9) and will scratch glass and steel easily, while the green zoisite matrix is softer (about 6.5). The whole piece takes a good polish.
Distinguish it from ruby in fuchsite, where the green host is a chromium mica (fuchsite) that is softer, flakier, and shows a more micaceous sheen. Dyed or imitation pieces tend to have unnaturally uniform color and lack the natural black hornblende inclusions.
Uses & significance
Ruby in zoisite is used mainly for ornamental carvings, cabochons, spheres, beads, eggs, and obelisks, where the green-and-red contrast is showcased. Translucent ruby zones are occasionally cut as cabochons or beads.
Gem-grade transparent ruby is not normally recovered from this material; instead it is valued as a decorative and lapidary stone. Larger carved figures and bookends are popular.
In metaphysical circles it is associated with vitality, the heart, and combining energy with growth. These are spiritual beliefs, not scientific properties. Its main practical value is aesthetic and as a collectible mineral specimen.
Frequently asked questions
Is the ruby in ruby zoisite real ruby?
Yes, the red-pink crystals are genuine ruby (gem corundum), but they are usually opaque and not of facetable gem quality.
What is anyolite?
Anyolite is simply another name for ruby in zoisite, from the Maasai word for green; it describes the same green-and-red rock from Tanzania.
What is the black material in ruby zoisite?
The black flecks are usually a hornblende-group amphibole that grew alongside the zoisite and ruby during metamorphism.
How is ruby zoisite different from ruby in fuchsite?
Ruby zoisite has a hard green zoisite host, while ruby in fuchsite has a softer, flakier chromium-mica (fuchsite) host with a more layered, sparkly green look.
Ruby in Zoisite guides
In-depth guides for identifying, valuing, and understanding Ruby in Zoisite.
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