Tourist Attractions
Loket Castle
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.

Town theatre
The first known theatre performance in Mariánské Lázně was played in a provisional wooden pavilion in the open air, said to be performed on 14th June in 1820. In 1868 F. Zickler built the original theatre building in the Neo-Renaissance style and a festive opening took place on 8th August.

Ferdinand Spring Colonnade
As you enter the beautiful park in Mariánské Lázně - Úšovice, you will see the Ferdinand Spring Colonnade (Kolonáda Ferdinandova pramene). Like other local colonnades, this one was also built at the instigation of the Abbot of the Teplá Monastery in 1827.

Svatoš Rocks
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).

Hirtenruhe
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.

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

Kynžvart Chateau
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.

Lazura Hill - Lazurový vrch
A northeast hillslope of Lazura Hill, about 1.5 km north-northwest of Michalové Hills. A debris forest with silver fir and wild cherry on a basal substrate of Lazura Hill, with the partial character of an old growth forest.

D-Club Dyleň
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.

Vlček
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.

Barren Hill - Planý vrch
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.

