Cova Remuntant de la Bretxa

Through a wide entrance one enters a vestibule with an ascending floor and the presence of blocks. At its far end and after a small step, a gallery about 10 metres long and also ascending begins, which is immediately closed off at the level + 10 relative to the lowest point of the entrance. The total route is 21 m.

All the caves and cracks located in the area are residual cavities, probably vestiges of other climatic circumstances. It is undeniable that the valley bears the imprint of a glacial past, and even today the action of ice widening the fracture structure is responsible for small cavities and for the great extent of these fragmentation scree slopes. The original appearance of the Coma Oriola (according to the ICGC: Comaoriola), has been profoundly altered by the imprint of the ski resort, since a piste runs through this valley. In summer and therefore out of season, the excavators, concrete mixers, etc. have extraordinarily transformed the bed of the basin, widening it and modifying its margins, causing original vegetation and soils to disappear and burying channels.