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Where is Ruby in Zoisite found?

Corundum in Zoisite

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Ruby in Zoisite occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.

Where to find Ruby in Zoisite

Longido, Tanzania

The primary and most famous source of high-quality Ruby in Zoisite, discovered in 1956. Occurs in the Precambrian Mozambique Belt.

Kenya

Other occurrences have been reported in East Africa, sharing similar geological settings to Tanzania.

India

Some deposits of ruby-bearing zoisite have been found, though often differing slightly in appearance or composition.

Collecting tips

  1. Geological Context. Look for areas with known occurrences of metasomatized mafic or ultramafic rocks within regional metamorphic belts. Associated minerals might include plagioclase, hornblende, and other chromium-bearing minerals.
  2. Visual Identification. The unique color combination of green, red, and black is highly distinctive. Rubies will appear as opaque, often blocky, red crystals within the green zoisite matrix.
  3. Hardness Test. While the overall rock has variable hardness, the ruby component is very hard (9 on Mohs scale), which can be tested on a fresh surface if other minerals are scratched.

Quick Check

Color:
Green, red, and black combination
Luster:
Vitreous to pearly (zoisite), adamantine (ruby), vitreous to dull (amphibole)
Streak:
White (zoisite), white (ruby), greenish-white (amphibole)

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