Tourist Attractions

One of the most beautiful places in the Cheb District is Kladská Lake and its Hunting Lodge, located in one of the most significant locations within the Slavovský Forest Protected Landscape Area.

The Premonstratensian Monastery of Teplá was founded in 1193 by the Squire Hroznata, a Czech nobleman. It is arguably the most important monastery in West Bohemia.

The park at Prelát Spring has many activities, especially for children. Here you can have a barbecue or try the zip wire, climbing frames, water attractions and other fun things to do.

The famous Colonnade is one of the most instantly recognisable symbols of Mariánské Lázně.

Beginning at the edge of the town's spa zone, this educational trail presents an overview of the geological characteristics and flora communities found in the Slavkovský Forest.

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.

As you walk through this part of the Slavkovský Forest, you may wonder what that rotten smell is. It comes from small rifts which host no life. Bleached skulls of field mice and forest birds, together with a myriad of insects grimly complete the picture.

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.

The cross stands above the town's market hall. This is an authentic historic attraction visited by many prominent personalities who were eager to take in the view of the valley that Mariánské Lázně occupies..

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

You won't find a single place in the entire Slavkovský Forest that suffers a lack of moisture. Often in times when wandering through the woods you might find yourself endlessly jumping over creeks and little streams as well as extensive wetlands.

Located near Ovesné Kladruby, the highest peak of the Tepelský flatland, a remnant of tertiary volcanic activity with significant geomorphological phenomena.