Tourist Attractions

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

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).

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

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.

This educational trail leads visitors to four different springs: Jezevčí, Kančí, Liščí I and Liščí II. The trail starts around 1km from Kynžvart spa.

The spa forests nature trail in Mariánské Lázně presents a wide selection of topics and focuses on spa care, history, geology, mining, forestry, zoology, botany and ecology. Some 23 stations are spread out over 5km of forest trails where info boards are packed with interesting information.

This is a rock promontory above the Ohře River valley on the peak of Šemnické Rocks (644 m high) above the village of Šemnice.

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.

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.

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

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.