Little Fisht Glacier, Mountain glacier in Greater Caucasus, Russia.
Little Fisht Glacier is a mountain glacier in the Greater Caucasus that spans several kilometers across high-altitude terrain. Its icy expanse feeds streams flowing into the valleys below and shapes the water systems of the surrounding region.
The glacier formed during ice-age periods and has retreated noticeably throughout the 20th century. This change reflects broader shifts in glacial coverage across the Caucasus range over recent decades.
Scientists and researchers regularly visit the glacier to conduct studies on glaciology, contributing to the understanding of ice formations in the Caucasus region.
Access demands mountaineering experience and specialized equipment due to demanding conditions on high terrain. The best time to visit falls between early summer and early autumn when most snow has melted.
The glacier functions as a natural water reservoir for the region, releasing meltwater continuously during warmer months. This seasonal water supply sustains ecosystems throughout the lower valleys year-round.
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