The mountains cover an area of approximately 500 km². The highest peak in the mountain range is Zengő (literally translates to 'resonant'), which has an elevation of 682 metres (2238 feet). The Mecsek Hills consist of plateau-like block mountains of a broken, folded structure. Its basis is crystalline rock of variscian origin surmounted by Triassic and Jurassic limestone and dolomite and Tertiary formations that form the main block. The mountains are divided by a structural fault running NW to SE. The eastern part consist mainly of high ridges of sedimentary rock. The west has extensive limestone plateaux and areas dominated by sandstones of the Permian-Triassic period. There are important karst phenomena to be found on the limestone plateaux. Mecsek is rich in minerals (including uranium as well) compared to other territories of Hungary. The climate is mixed and represents elements of the mediterranean and continental climate. The territory gives home to 20-30 plant species which are unknown in other parts of the Carpathian Basin.