Tourist Attractions

The Chopin House Gallery, located in the historic front wing of the Chopin House, offers visitors a unique experience connected with art and culture.

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

The Central Park is situated in the heart of the city between Masarykova and Hlavni Streets. Here you’ll find a memorial to the Jewish residents of the city who had to flee or were deported before and during World War II. The memorial was unveiled in 2010 on the anniversary of the so-called "Kristallnacht", when the Nazis destroyed synagogues and Jewish buildings in many towns, including Mariánské Lázně. A sculpture called "Four Seasons" by Z. Šimek also adorns the space.

The church was built in the year 1790 on the foundations of an earlier parish chapel. The first mass was held on Christmas Eve 1790. The interior of this late Baroque church is relatively simple in design.

A composition of typical sub-saturated peat meadows in the Slavkovský Forest close to the serpentinite hill of the Three Crosses at the roadside between Prameny and Nová Ves. Site of the rare swamp willow.

Pístov Meadow is formed by a small meadow enclave on the edge of the forest in a slightly kerfed valley 1 km southeast of Pístov.

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.

As you enter the beautiful park in Mariánské Lázně - Úšovice, you will see the Ferdinand Spring Colonnade (Kolonáda Ferdinandova pramene). Like other local colonnades, this one was also built at the instigation of the Abbot of the Teplá Monastery in 1827.

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).

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

White foamy crusts decorate several smaller water surfaces of grass-grown glades on the right bank of the Teplá River.