When observed from an aerial perspective, Kondyor Massif presents a striking resemblance to an ancient fossil or a volcanic ash formation resulting from a celestial meteorite. According to experts, this geological marvel is attributed to molten lava from igneous rock that solidified beneath the Earth’s crust over a billion years ago, shaping a perfectly circular massif.
The massif’s distinct structure withstands soil erosion over extended periods, owing to its superior hardness compared to the surrounding soil. Kondyor Massif represents the elevated surface edge of a rock column gradually descending into the Earth’s crust, preserving the remnants of a fully eroded dome section. A central stream emanates from the heart of the massif, fed by melted snow along its periphery. Numerous smaller streams branch out from the edges, contributing to the flow of water towards the Kondyor River on the north face.
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.As reported by Siberian Times, platinum extraction commenced in the Kondyor Massif in 1984. The debut of platinum crystals from this massif took place at The Tucson Gem and Mineral Show in the USA in 1993. Approximately 4 tons of platinum are harvested annually from this site.