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.

One of the largest and most picturesque groups of tors, namely the “Prządki” tors formed of Eocene (56-34 mln years) Ciężkowice Sandstones, is situated in Czarnorzeki.

Odrzykoń is the location of ruins of the “Kamieniec” castle, built on a rock formed of Ciężkowice Sandstones and with numerous tors of the “Krowia Turnia” group in the surroundings.History of the castle’s residents was described by Aleksander Fredro in “Zemsta”.

The series of tors extends on a crest, from Wola Komborska in the east, through Czarnorzeki, to Frysztak in the west.