Introduction
The great breakage of the rock was due to a flaw, it allowed rainwater and fountains to lower their interior, forming a torrent and debilitating the rock.
The warm and humid climate have contributed to weakening the rock, and also the heat of the sun, and the chemical action of rain.
The lower part of the torrent is sprayed with the water course, not very heavy, but with its strong cyclical avenues, typical of the desert and Mediterranean climates.
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