Tourist Attractions

A pine wood on a serpentinite base between the villages of Prameny and Mnichov.

Its beauty and serenity made this place a favourite with the Abbot Alfréd Clements of Teplá. A simple wooden bench stood here where the dignitary often used to sit. During his time as Abbot, Mariánské Lázně experienced the largest building boom of its early development (1888–1900).

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

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.

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

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.

Friedrich’s Stone is the name given to a naturally occurring mound of coarse granite boulders that stand in a location known as ‘Little Switzerland’ (Malé Švýcarsko).

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.

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.

Preserved pinewood on a serpentinite subsoil between Prameny and Sítina, this is a typical example of original forest pine growth (vogtland upland ecotype) on serpentinite.

An elegant one-storey tower used to stand here. It was erected in 1847 but the surrounding forests had overgrown it by 1879. Only a sign now gives any indication the buidling once stood here.