Tourist Attractions

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.

A small, intimate town nestled on the edge of a beautiful forested area, Lázně Kynžvart was founded in 1214 and boasts an impressive past.

This dominant lookout point is located on the top of Žižka Hill. The location was named in honour of Prussian King Friedrich Wilhelm IV who laid the foundation stone of the altar in the town's Evangelical Church in June 1857.

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).

Gallery in the atrium of the Hotel Hvězda, opening every first Tuesday of the month, entry free.

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.

In the park in front of the hotel Krakonoš you can find a trail showcasing traditional fairytale figures. This trail features sandstone statues from famous fairytales.

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 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.

This place of worship was built in the neo-Byzantine style between 1844 and 1848.

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.

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