Tourist Attractions

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.

A Jewish enclave existed in Mariánské Lázně from around 1824 and by 1861 it had its own hospital with a small chapel. The Jewish cemetery close to the road to Velká Hleďsebe was founded in 1875. By 1930 it had been extended and is still used today.

The Church of St Anna is the most important historical site in Velká Hleďsebe, a village located close to Mariánské Lázně. In 2011 the church celebrated its centenary. It's a neo-Romanesque building completed in 1911 by Josef Forberich of Mariánské Lázně.

Pístov Meadow is formed by a small meadow enclave on the edge of the forest in a slightly kerfed valley 1 km southeast of Pístov.

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

A northeast hillslope of Lazura Hill, about 1.5 km north-northwest of Michalové Hills. A debris forest with silver fir and wild cherry on a basal substrate of Lazura Hill, with the partial character of an old growth forest.

This is group of sulphur dioxide gaseous effluences at Milhostov. It was declared a natural monument to protect the mofette, or discharge of gaseous sulphur dioxide.

The evangelical church was built for evangelical spa guests in 1857 and was funded with donations from German evangelical Christians supported by the Prussian King Friedrich Wilhelm IV. He took part in its consecration 24th June 1857.

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.

The name comes from a distinguished visitor to the town, the Bavarian Queen Karola. This is a lookout pavilion built in 1875 on the hillside between the Forest Spring and the local cemetery (above today's car park).

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.

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.