Tourist Attractions

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

The small town of Chodová Planá is best known for the Chodovar Brewery, the oldest in West Bohemia.

The Bečov Castle was founded in the 13th century by the Lords of Osek who owned the surrounding estates for almost 200 years.

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.

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.

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

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.

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.

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).

The cross stands above the town's market hall. This is an authentic historic attraction visited by many prominent personalities who were eager to take in the view of the valley that Mariánské Lázně occupies..

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.