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Ventisquero Colgante: The Hanging Glacier of Queulat

Ventisquero Colgante, or the Hanging Glacier, is found in the Queulat National Park, in Chile, and is the park’s biggest fascination. Hanging over a gorge of exposed rock, it overwhelms a valley shaped by mountains secured in valdivian mild rainforest, and sustains a stream at the base of the valley as it melts.

The water liquefying from the ice sheet makes two towering waterfalls as it drops 600 meters on top of an enormous chunk of calculated bedrock, and after that streams underneath what has all the earmarks of being a perpetual torrential slide cone. As the stream leaves this underground segment, it structures a little lake - Laguna Témpanos - and after that after in the ballpark of 6 km enters the Canal de Puyuhuapi. The falls are unmistakable and streaming all round the year however because of the removal of torrential slides at the base of the falls, to the extent that 50% of the falls can be secured by snow and ice amid the late spring and early summer. 

Ventisquero Colgante was found in 1875 amid an exploration led by Captain Enrique Simpson. Chief reported that the snow of the icy mass was only 100 meters from the bank of Canal de Puyuhuapi, where Captain used to field his vessel. It is not by any stretch of the imagination clear whether he saw the waterfall and whether this waterfall was obvious whatsoever. In all likelihood, it wasn't. The waterfalls was made much later, as the icy mass withdrew and the bluff divider got to be obvious. In the event that Captain's perception is genuine, then the icy mass has withdrawn 8 km amid the most recent 140 years .

Source : Wondermodo

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