Kaznakhtinskii ultrabasic massif

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Kyzyl-Uyuk locality, Terekta Ridge, Ust-Koksinsky District, Altai Republic, Russia

Казнахтинский массив

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Key Information

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  • The Kaznakhtinskii ultrabasic massif is located in the Terekta Ridge, Ust-Koksinsky District, Altai Republic, Russia, a mountainous region in southern Siberia near Mongolia, China, and Kazakhstan.

  • It is known for minerals like Kaznakhtite, a recently discovered member of the Hydrotalcite supergroup, along with Stitchite, chrysotile, and lizardite, found in serpentinized ultrabasic rocks.

  • The geological structure is serpentinized ultrabasic, rich in magnesium and iron, formed through mantle-derived processes and water interaction.

  • Mining history is limited, with small-scale mineral collecting likely, but no large-scale operations are confirmed; the area is more significant for research and discovery.

  • The local culture includes Altaian traditions, with music, dance, and crafts, reflecting the region's Turkic heritage.

  • The climate is continental, with cold winters and mild summers, supporting diverse ecology from forests to alpine meadows, potentially influencing mineral formation.

Geographic Location

The Kaznakhtinskii ultrabasic massif lies within the Terekta Ridge in the Ust-Koksinsky District of the Altai Republic, Russia. This region is part of southern Siberia, nestled in the Altai Mountains, which extend across Russia, Mongolia, China, and Kazakhstan. The Altai Republic borders Kemerovo Oblast, Khakassia, Tuva, and Altai Krai, making it a crossroads of natural and cultural landscapes. The Terekta Ridge, with its rugged terrain, is known for its scenic beauty and is accessible via rural roads, offering a remote yet captivating destination for enthusiasts.

Minerals Produced

The massif is a treasure trove for mineral collectors, featuring Kaznakhtite, a newly identified mineral from the Hydrotalcite supergroup with the formula Ni6Co3+2(CO3)(OH)16⋅4H2O. This light green, rare mineral is found alongside Stitchite, chrysotile, lizardite, dolomite, brucite, chromite, heazlewoodite, manganochromite, magnetite, and magnesioferrite. These minerals are embedded in serpentinized ultrabasic rocks, rich in magnesium and iron, making the site particularly exciting for those seeking uncommon specimens.

Geological Structure

Geologically, the Kaznakhtinskii massif consists of ultrabasic rocks, low in silica and high in magnesium and iron, originating from the Earth's mantle. These rocks have undergone serpentinization, a process where they react with water to form serpentine minerals like chrysotile and lizardite. This transformation not only creates the characteristic mineral deposits but also shapes the area's unique landscape, offering insights into deep Earth processes.

Mining History

While the Altai Republic has a history of mining for metals like gold and copper, specific details for the Terekta Ridge are scarce. The discovery of Kaznakhtite suggests the area is of interest for mineralogical research and small-scale collecting, but there is no evidence of large-scale mining operations. This makes it a site more aligned with scientific exploration than industrial extraction, preserving its natural state for enthusiasts.

Local Culture and Characteristics

The Ust-Koksinsky District is part of the Altai Republic, home to the Altaian people, a Turkic ethnic group with a rich cultural heritage. Visitors can immerse themselves in traditional Altaian music, dance, and crafts, reflecting centuries of local traditions. The area also features historical sites and festivals, offering a glimpse into the region's cultural tapestry and its connection to broader Siberian and Central Asian influences.

Climate and Ecology

The climate in the Altai Republic is continental, characterized by cold, snowy winters and mild, rainy summers. The Terekta Ridge, at higher elevations, experiences a mountainous climate with temperature and precipitation variations. The ecology ranges from taiga forests to alpine meadows, supporting diverse flora and fauna. This environment, with its geological and climatic conditions, likely plays a role in the formation and preservation of the region's unique minerals.