Wola Komborska includes one of the largest groups of tors, formed of Istebna Sandstones of Palaeocene age (65-56 mln years), in the Flysch Carpathians. The "Maczuga" and "Konfederatka" tors as the most known ones.
In some caves, ice retains for most of the year. Entering such caves requires specialist cave equipment.
The Cergowa and Kilanowska Mountains
include the greatest assemblage of fissure caves
in the Flysch Carpathians.
Sip of water from a several million years old ocean.
Mineral water intakes are located in the area of Iwonicz Zdrój and Rymanów.