Tourist Attractions
Laska Chapel
The director of the local theatre Julius Laska had this chapel built in 1909 in memory of his mother. It is a small, pretty, neo-Gothic building set against a forest backdrop.

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

Church of St Anna in Velká Hleďsebe
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.

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.

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.

Domin Rock Formation - Dominova skalka
This small but unique protected area can be seen from the road connecting the village of Louka u Mariánských Lázní and Nová Ves.

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

Planá u Mariánských Lázní
The first written record of Planá dates back to 1251. The town was founded on an important trade route leading from Nuremberg to Cheb and further on into Bohemia.

Teplá River Valley - Údolí Teplé
The Teplá River between Bečov and Loutnový, connects the sections of the Otročínský, Pramenský and Mnichovský Creek, about 8-16 km north-northeast of Mariánské Lázně.

The Kladruby Monastery
The former Benedictine Monastery of Kladruby, an important historical site, looms over the valley of the Úhlavka River.

Komorní hůrka educational trail
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.

