Tourist Attractions

Put on your dancing shoes and get ready to groove in D-Club. In Addition to classic weekend dance parties you can party here with leading Czech and Slovak dance, pop and rap artists.

This is a gazebo situated on a plateau above a boulder outcrop at the Royal Hotel where a decorated wooden structure originally stood. The building was inaugurated in 1850 in honour of an important guest to Mariánské Lázně - the Czech proconsul, Baron von Mescery.

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.

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

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.

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

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).

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 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.

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).

The chateau in Kynžvart was originally a Baroque Residence but the Austrian Chancellor Metternich had it rebuilt into an Empire mansion between 1821 and 1836.

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.