Ravna Gora

 memorial, church, museum, mountain, park, monument, interesting place

Ravna Gora is a raised plateau on the environment. The overall slope of Valjevo mountain plateau to the north (down basin), and then to the bottom Nakucanske presedline (between mountains) shows that building the southern part of the relief Kolubara done confrontation of two opposing processes: erozionog, which tends to uravni that part of the dinar and the courts tektonskog, which were built izdizani some parts of the surface. According to the East Flat worse binds to Suvobora branches. Highest level in this area build curved scalp several peaks on the southern edge of the river basin Paleznicke, which approximate height: Lom (716 m), Igriste (730 m), Damjanov stone (725 m), Vezinac (760 m), and Suvobor (864 m), Tang (845 m), Grukovica (855 m) and Paradise Mountain (848 m). They are slightly rise above the plateau and presedlina of about 800 m, and are very denivelisane surface residues of 850-920 m. Plateau at about 800 m is better expressed north of Suvobora. to continue in the spacious plateau right-field block (at 780-800 m), which was cut in suvoborske serpentinite. The plateau is pulling presedlinom between Grukovice and Rajac. At the same height as the east of the scalp Rajac hill until the Fat Brdo, which is clearly rising to the surface of 700 m. This surface reaches a width of 5 km. The largest part of the Straight Up affect gornjekredni limestones presented a reddish-purple and silifikovanim panel, compact, laporovitim limestones. They are expressed on the northwestern side. Limestone terrain is straight up depressions, depressions, and caves, among which emphasize wet and dry cave. Karst straight up has an area of 3 km2. To the west of the Ravna Gora and Bačevačko Lelicka, and the east Rajac surface, where they identified identical structures of the upper chalk.

WHAT TO SEE IN Ravna Gora?

* Drazin cave
* Church of Saint George
* Top of Babin Kuk