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Golconda diamonds

Antique Indian diamonds

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Through Andhra Pradesh, Hyderabad and Carbon

For 2,000 years, Golconda diamonds were the only-known fine diamonds. Due to centuries of excessive mining, their production was exhausted by 1830, and gemologists and traders have classified Golconda diamonds as antique, rare and precious. Famous Golconda diamonds include the colourless Koh-i-Noor, the Nassak Diamond, the blue Hope Diamond, the Idol's Eye, the pink Daria-i-Noor, the white Regent Diamond, the Dresden Green Diamond, and the colourless Orlov Diamond, as well as now-untraceable diamonds such as the yellow Florentine Diamond, the Akbar Shah, the Nizam Diamond, and the Great Mogul Diamond.

The Golconda diamond industry was at its peak from the 16th to 18th centuries when 23 mines, of which Kollur Mine was the most active, operated in the region and 30,000 people at a time worked in one mine. The output from all of the mines in Golconda is estimated to be around 10,000,000 carats (2.0 t). In 2015, Osmania University in collaboration with Geological Survey of India discovered potential new sites for diamond mining in the region, though as of 2022 mining had not started.

Several literary legends were inspired by Golconda diamonds; these include Sindbad the Sailor's valley of diamonds, the gem lore of Marco Polo, and the theme of Russell Conwell's inspirational lecture "Acres of Diamonds". According to folklore, some Golconda diamonds are cursed; these impart good luck to their owners or have mystical powers while others were worn as talismans. In 2013, the Princie Diamond from the Jewels of the Nizams was auctioned for US$39.3 million—the highest-recorded auction price for Golconda Diamonds and the world record for US$1.1 million per carat. In a heist in 2019, the Dresden White Diamond was stolen along with jewels worth US$1.2 billion.

Geology

The Golconda diamondiferous region is located in the Southern Indian peninsular shield, which was formed during the process of proterozoic and Insular India. The region is spread over 50,000 km2 (19,000 sq mi), within the sediments of the Krishna-Pennar river basin and Deccan Traps, and contains 120 out of the 150 kimberlite pipes in India. Though kimberlite and lamproite are the primary rock source, conglomerate and placers had yielded the majority of the region's diamonds. The Geological Survey of India has categorized kimberlite pipes of southern India into clusters Southern Wajrakarur kimberlite, Northern Narayanpet kimberlite, and Central Raichur kimberlite of these, the Timmasamudram kimberlite cluster—a part of Southern Wajrakarur kimberlite—is significant.

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