Walking on a straight line in the last hundred meters, it was possible to notice the direction towards west of the calcareous layers. These features will be similar throughout the whole length of the cave. Huge are the wave-cut notches, large grooves left by the different heights the river had during the cave’s life. On the other side, we can see the presence of solidified debris and sediments left on site by the river, located also several meters high compared to today’s level of flow. Flowstones and formations have an East
depositional direction. The whole length of the cave will show this pattern.