Tourist Attractions

An elegant one-storey tower used to stand here. It was erected in 1847 but the surrounding forests had overgrown it by 1879. Only a sign now gives any indication the buidling once stood here.

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 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).

The Central Park is situated in the heart of the city between Masarykova and Hlavni Streets. Here you’ll find a memorial to the Jewish residents of the city who had to flee or were deported before and during World War II. The memorial was unveiled in 2010 on the anniversary of the so-called "Kristallnacht", when the Nazis destroyed synagogues and Jewish buildings in many towns, including Mariánské Lázně. A sculpture called "Four Seasons" by Z. Šimek also adorns the space.

The best-known and most significant granite rock formation in the Karlovy Vary massive is undoubtedly the Svatoš Rocks (Svatošské Skály), part of the Jan Svatoš National Nature Park (NPP).

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

Friedrich’s Stone is the name given to a naturally occurring mound of coarse granite boulders that stand in a location known as ‘Little Switzerland’ (Malé Švýcarsko).

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.

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.

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

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