Another important geosite in the Geopark is the Dare-diz Protected area. Visitors who enter the Geopark via Tabriz road from the south way, whether by car or train, first of all, encounter with huge cliffs and elevated hilltops of this geosite.

Competent limestone and dolostone beds from Devonian, Permian and Triassic Periods, as well as Devonian Andesitic lavas constituted main part of outcrops in the region. Compression caused by continental collision in Alpine orogeny from the late Triassic Period to present, has led to significant bed folding on each other and thrusting them in a large distance.

Stunning scenic views of the geosite area with observable thrusts and strike-slip faults, systematic joints, fault related folding and micro-folds can excite every visitor and create ineffaceable memories. Vast outcrops of limestone-dolostone formations with massive well bedded can help to detect structures like different type of folds and faults. Sedimentary layers rich in fossils of Brachiopods, Pelecypoda, Corals, Echinodermata and Ammonites has completed this beautiful picture.

Apart from its unique structural geology specifics, Dare-diz geosite has a significant biodiversity, both in flora and fauna, that placed it in the list of protected areas in department of Environment.