Tourist Attractions

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 best-known and most significant granite rock formation in the Karlovy Vary massive is undoubtedly the Svatoš Rocks (Svatošské Skály), part of the Jan Svatoš National Nature Park (NPP).

This protected spruce rises northwest of Marianske Lazne between "Svobody" alley  and "Smetana" alley. The spruce is estimated to be 200 years old and is a truly majestic tree - the trunk circumference is 450cm and it is 39 m tall. It first emerged from the ground around 1818 when Mariánské Lázně was first declared a public spa. In March 2017 strong wind got the better of the spruce which fell. A fallen tree remains protected, so it can still be admired where it lies.

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

The largest city in Western Bohemia was established at the confluence of four rivers - the Úhlava, Úslava, Mže and Radbuza - which all flow together here to create the River Berounka.

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

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.

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

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.

"Skalnikovy sady" park dominates the town and is one of the most popular among tourists. It was created at the end of the 19th century at the same time as the town.

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