Tourist Attractions

As you walk through this part of the Slavkovský Forest, you may wonder what that rotten smell is. It comes from small rifts which host no life. Bleached skulls of field mice and forest birds, together with a myriad of insects grimly complete the picture.

Located near Ovesné Kladruby, the highest peak of the Tepelský flatland, a remnant of tertiary volcanic activity with significant geomorphological phenomena.

The Moučné Pytle natural monument is located on Jelení Hill (644 meters high) on the green marked trail from Karlovy Vary to Horní Slavkov, about 1 km from the Bor gamekeeper’s lodge.

In the Town Museum, you can every month look forward to a new exhibition.

Straddling the Ohře River, Cheb is the westernmost major town in the Czech Republic

The director of the local theatre Julius Laska had this chapel built in 1909 in memory of his mother. It is a small, pretty, neo-Gothic building set against a forest backdrop.

The church was built in the year 1790 on the foundations of an earlier parish chapel. The first mass was held on Christmas Eve 1790. The interior of this late Baroque church is relatively simple in design.

Preserved pinewood on a serpentinite subsoil between Prameny and Sítina, this is a typical example of original forest pine growth (vogtland upland ecotype) on serpentinite.

In the park in front of the hotel Krakonoš you can find a trail showcasing traditional fairytale figures. This trail features sandstone statues from famous fairytales.

A composition of typical sub-saturated peat meadows in the Slavkovský Forest close to the serpentinite hill of the Three Crosses at the roadside between Prameny and Nová Ves. Site of the rare swamp willow.

Komorní Hůrka is our youngest volcano – it was known to be active around 850,000 years ago, with some evidence suggesting it only became dormant as recently as 350,000 years ago.

About two kilometers south-southeast from the town of Bečov Nad Teplou, not far from the road to Chodov, is a natural monument. It was established to protect the rock formations made of basalt chimney formation with typical column cleats.