Tourist Attractions

Hauenštejn Castle was founded by the Czech King in the second half of the 13th century and was generously enlarged and remodeled in the neo-Gothic style by the Buquoys family during the 19th century.

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

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 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 Moučné Pytle natural monument is located on Jelení Hill (644 meters high) on the green marked trail from Karlovy Vary to Horní Slavkov, about 1 km from the Bor gamekeeper’s lodge.

The shallow basin between the Vonšovský and Sooský Creeks (at the Nový Drahov train station, 6 km from Františkové Lázně) is divided by a mound of silicious sand into two parts.

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.

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.

Straddling the Ohře River, Cheb is the westernmost major town in the Czech Republic

The largest city in Western Bohemia was established at the confluence of four rivers - the Úhlava, Úslava, Mže and Radbuza - which all flow together here to create the River Berounka.

About two kilometers south-southeast from the town of Bečov Nad Teplou, not far from the road to Chodov, is a natural monument. It was established to protect the rock formations made of basalt chimney formation with typical column cleats.