Tourist Attractions

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

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.

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 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.

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.

Karlovy Vary is a popular spa resort named after its founder, Emperor Charles IV. Legend has it that Charles discovered the hot springs while chasing a stag.

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.

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.

In the Town Museum, you can every month look forward to a new exhibition.

The name comes from a distinguished visitor to the town, the Bavarian Queen Karola. This is a lookout pavilion built in 1875 on the hillside between the Forest Spring and the local cemetery (above today's car park).

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.

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