Until recently the mountains formed a barrier between the two parts of Thailand - only the railroad from Bangkok to Nakhon Ratchasima and one highway crossed it. Before the construction of the railroad in the beginning of the 20th century, the separation of the two parts of the country was even more distinct.
The highest elevation of the Phetchabun mountains is at 1820m above sea level at the Phu Hin Rong Kla national park in the northern part of the mountain range. It consists of two parallel mountain chains, with the valley of the river Pa Sak in the middle. To the south the mountains end in the Khao Yai national park, and are continued to the east by the Dong-Paya-Yen, Sankambeng and Phnom-Dongrek mountain chains.
The highest elevation of the Phetchabunmountains is at 1820m above sea level at the Phu Hin Rong Kla National Park in the northern part of the mountain range.
To the south the mountains end in the Khao Yai national park, and are continued to the east by the Dong Phaya Yen, Sankambeng and Phnom- Dongrek mountain chains.
Geologically, the mountains consist of limestone, interfused with slate and sandstone.