Madagascar Gems - Overview

Madagascar emerged as a major gem-producing island in the late 20th century,
with diverse Precambrian metamorphic and granitic basement producing an exceptional
range of gem species. The Ilakaka alluvial sapphire deposits of southern Madagascar
were discovered in 1998, triggering a major rush and making Madagascar one of the
world's largest sapphire producers by volume. Ruby is mined at Andilamena (northern
Madagascar), Vatomandry (eastern coast), and other localities; quality varies
considerably and beryllium diffusion treatment has been recorded, requiring
laboratory disclosure. Pegmatite-hosted beryl (aquamarine, morganite), tourmaline,
and rare species including grandidierite (first identified in Madagascar in 1902
and now the world's primary gem-quality source) add breadth to the island's output.

Madagascar's commercial position is as a high-volume, competitively priced
supplier filling gaps left by declining traditional sources; some material achieves
fine quality comparable to classic origins, particularly for blue and pink sapphire.
Origin certification is increasingly standard for higher-value stones.
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Madagascar's primary gem outputs:

Gem-producing regions across Madagascar:

• South: Ilakaka (sapphire) - massive alluvial deposits
• North: Andilamena (ruby) - primary ruby region
• East: Vatomandry (ruby, sapphire)
• Central: Various pegmatite-hosted gems
• Multiple regions: Tourmaline, beryl, garnet production

Industry characteristics:

Madagascar's role in the gem trade:

• Supply volume: Major world producer
• Quality range: Commercial through fine
• Value position: Competitive pricing
• Gap filler: Replaces declining traditional sources
• Rare gems: Primary source for several species