Tourist Attractions

As you enter the beautiful park in Mariánské Lázně - Úšovice, you will see the Ferdinand Spring Colonnade (Kolonáda Ferdinandova pramene). Like other local colonnades, this one was also built at the instigation of the Abbot of the Teplá Monastery in 1827.

A pine wood on a serpentinite base between the villages of Prameny and Mnichov.

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.

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.

This is a rock promontory above the Ohře River valley on the peak of Šemnické Rocks (644 m high) above the village of Šemnice.

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.

This place of worship was built in the neo-Byzantine style between 1844 and 1848.

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.

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.

Beginning at the edge of the town's spa zone, this educational trail presents an overview of the geological characteristics and flora communities found in the Slavkovský Forest.

Put on your dancing shoes and get ready to groove in D-Club. In Addition to classic weekend dance parties you can party here with leading Czech and Slovak dance, pop and rap artists.

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