Tourist Attractions

The Anglican Church is the work of London architect William Burges and was built in 1879 by Friedrich Zickler.

This protected spruce rises northwest of Marianske Lazne between "Svobody" alley  and "Smetana" alley. The spruce is estimated to be 200 years old and is a truly majestic tree - the trunk circumference is 450cm and it is 39 m tall. It first emerged from the ground around 1818 when Mariánské Lázně was first declared a public spa. In March 2017 strong wind got the better of the spruce which fell. A fallen tree remains protected, so it can still be admired where it lies.

One kilometer north of the village of Michalovy Hory, we come across the emergence of carbonated water, one of the best-known acidulous water sources of Slavkovský Forest: Čiperka.

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.

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.

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.

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.

This tower was named after Hamelika Hill on which it stands.

Visitors can enjoy not only artworks but also film screenings dedicated to the life and work of the exhibiting artists. The combination of 19th-century architecture with modern art creates a unique atmosphere for an unforgettable cultural experience. The gallery’s curator is Alena Mrovcová.

Opening hours: daily 2:00–5:00 p.m.

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.

This is a natural pine growth area on the southeast slope of Planý Hill with exposed serpentinite rock formations, partly interrupted by a small extinct rock quarry covered by a rare botanical community.

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.