Tourist Attractions

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

Loket is a very old town with a castle of the same name. Both rise above the valley of the Ohře River between Karlovy Vary and Sokolov.

Its beauty and serenity made this place a favourite with the Abbot Alfréd Clements of Teplá. A simple wooden bench stood here where the dignitary often used to sit. During his time as Abbot, Mariánské Lázně experienced the largest building boom of its early development (1888–1900).

This small but unique protected area can be seen from the road connecting the village of Louka u Mariánských Lázní and Nová Ves.

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

Around Křížky, and more generally in the area between Prameny and Mnichov, you’ll find one of the most interesting natural areas in the Slavovský Forest. The newly-created educational trail introduces visitors to the largest serpentinite complex in Bohemia as well as one of the most interesting areas in the central part of the Slavkovský Forest protected area.

This educational trail leads visitors to four different springs: Jezevčí, Kančí, Liščí I and Liščí II. The trail starts around 1km from Kynžvart spa.

The park at the Forest Spring is located in the northern part of the town off Třebízského street. Here you'll find a pavilion containing the Forest Spring, the Goethe and Muse sculpture by German sculptor Heindrich Drake, a memorial stone for the writer Vaclav Václav Beneš Třebízský and a sculpture of three muses by O. Zoubek. Nearby you'll also find a music pavilion used in summer as a cafe and a venue for musical performances.

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.

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).