De los Carlistas

The mouth of the cavity is a joint that functions as a crawl. Through this crawl the main gallery is reached, which shows traces of phreatic circulation with a fairly significant elastic process of collapse and dragging. The crawl is full of allochthonous elements such as leaves and soil, while the floor of the main gallery, of circular section, is full of detached slabs; its middle part is a tube where traces of strong erosion can be seen. The end of the gallery is a chamber with an abundance of lithogenic and reconstruction deposits. The final chamber retains at its back a sedimentary/clayey blockage covered by a thin flowstone. Going back a few metres, on the left as one retreats, there is a crawl that leads to a small chamber in which small marly rounded pebbles appear. From this chamber, by means of a small climb, a small ascending gallery of circular section is reached, ending in a small chamber at surface level, with a large amount of roots and soil on the ceiling and floor.

At the mouth, inside the crawl, some forms of lithogenic reconstruction can be seen. The final chamber of the main gallery presents an abundance of lithogenic and reconstruction deposits, and its back is a sedimentary/clayey blockage covered by a thin flowstone. In the small chamber at surface level, small flowstones are observed alongside remains of fibrous calcite.

Access is through the mouth, a joint that functions as a crawl, and through it the main gallery is reached. Going back a few metres, on the left as one retreats, a crawl leads to a small chamber with small marly rounded pebbles; from this chamber, by means of a small climb, a small ascending gallery of circular section is reached, ending in a small chamber at surface level.

In the middle part of the gallery, some samples of black fibrous schists were collected.