Tourist Attractions

The former Benedictine Monastery of Kladruby, an important historical site, looms over the valley of the Úhlavka River.

The spa forests nature trail in Mariánské Lázně presents a wide selection of topics and focuses on spa care, history, geology, mining, forestry, zoology, botany and ecology. Some 23 stations are spread out over 5km of forest trails where info boards are packed with interesting information.

The Teplá River between Bečov and Loutnový, connects the sections of the Otročínský, Pramenský and Mnichovský Creek, about 8-16 km north-northeast of Mariánské Lázně.

You won't find a single place in the entire Slavkovský Forest that suffers a lack of moisture. Often in times when wandering through the woods you might find yourself endlessly jumping over creeks and little streams as well as extensive wetlands.

Kynžvart Kámen is one of the lesser known natural monuments of Slavkovský Forest. It’s located not far from the old route connecting the train station of Lázně Kynžvart with the town itself, north of Luční Pond.

White foamy crusts decorate several smaller water surfaces of grass-grown glades on the right bank of the Teplá River.

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.

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

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.

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.

Gallery in the atrium of the Hotel Hvězda, opening every first Tuesday of the month, entry free.

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