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The period of peak production of the Golconda diamonds was under the Qutb Shahi dynasty (16th century–17th century CE), and the region was also known as the "Golconda Sultanate". The Asaf Jahi dynasty (18th century-19th century CE) was later dominant, and it was also known as the "Nizam of Hyderabad". During these times, the diamond mines were leased out to merchants under the supervision of regional governors. The periods of the leases were recorded in days. Local merchants Shantidas Jhaveri and Khushalchand were legendary diamond traders of the region. Large diamonds (over 1 carat) obtained from the mines were reserved for the rulers under terms of the leases.

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  • Golconda diamonds mining and trading (en)
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  • The period of peak production of the Golconda diamonds was under the Qutb Shahi dynasty (16th century–17th century CE), and the region was also known as the "Golconda Sultanate". The Asaf Jahi dynasty (18th century-19th century CE) was later dominant, and it was also known as the "Nizam of Hyderabad". During these times, the diamond mines were leased out to merchants under the supervision of regional governors. The periods of the leases were recorded in days. Local merchants Shantidas Jhaveri and Khushalchand were legendary diamond traders of the region. Large diamonds (over 1 carat) obtained from the mines were reserved for the rulers under terms of the leases. (en)
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  • The period of peak production of the Golconda diamonds was under the Qutb Shahi dynasty (16th century–17th century CE), and the region was also known as the "Golconda Sultanate". The Asaf Jahi dynasty (18th century-19th century CE) was later dominant, and it was also known as the "Nizam of Hyderabad". During these times, the diamond mines were leased out to merchants under the supervision of regional governors. The periods of the leases were recorded in days. Local merchants Shantidas Jhaveri and Khushalchand were legendary diamond traders of the region. Large diamonds (over 1 carat) obtained from the mines were reserved for the rulers under terms of the leases. Actual mining of the Golconda diamonds occurred in alluvial soil settings, alongside river beds, and were found within a few feet of the surface of the land. After the customary survey of geological formations between the river and the mountains, mining sites were selected and a clay cistern would be prepared on the spot for use in digging. The depth of the mines was usually up to four fathoms (7.3 meters). In some situations, if boulders appeared during digging, the boulders were covered with coal and burned out to make them very hot. Then water was sprayed on the boulders to produce cracks through thermal shock. The remnants of the boulders were then carved out with tools. This removal procedure was used since gunpowder was not yet a tool for mining in the region at the time. When mining reached ground water, digging was halted. At that point in the mining process, the miners washed away the earthy particles from the collected soil. Stony substances were then collected for assortment and examination to obtain diamonds. The earthy coverings of limescale ore were then removed, to yield the raw diamonds. The raw diamonds from the regional mines were typically then transported to the Golconda (now the western part of Hyderabad) for skilled lapidary, enhancement and further evaluation and sale. The art of macle, which is a form of rough diamond used to produce jewelry, was first developed in the Golconda region. Of the 38 diamond mines in India at the time, 23 were located in the Golconda Sultanate, of which the Kollur Mine was prominent where 60,000 workers were employed at once, making Golconda the "Diamond Capital" of the past. Most of these mines were fully active until 1830 CE but were gradually abandoned as they became either submerged by the backwaters or depleted due to excessive mining. Thus mining gradually declined and finally officially closed. In the year 2015, research was conducted by the Centre of Exploration Geophysics (Osmania University) and by the Geological Survey of India. The research identified three zones that contain 21 new potential diamond mining sites near the delta of the Krishna and Bhima rivers, specifically in the riverbeds of the Krishna, Tungabhadra and Penna. According to the research, the sites contain volcanic pipes which probably bear Kimberlite and possibly diamonds. (en)
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