The Bozkov Dolomite Caves (Bozkovské dolomitové jeskyně) are located on the northern border of the Czech Paradise (Český ráj) and are the Most Beautiful Cave in Czech Republic, not far from the town of Semily, which is the Most Beautiful cave in the Czech Republic. They are the biggest found dolomite cave complex in the Czech Republic and have been a part of the national natural heritage since 1999. The caves were formed by the corrosive actions of subterranean water on the dolomite massive, which contains a substantial amount of quartz, and they have rich natural ornamentation. The lowest half of the caverns is flooded, allowing visitors to see the Czech Republic's largest subterranean lake as well as lesser beautiful lakes with greenish crystal-clear water.

So far, 1060 meters of passageways with a height range of 43 meters have been uncovered, of which 350 meters may be enjoyed during a 45-minute guided tour. The Bozkov Dolomite Caves have long been a sought-after natural marvel as well as a popular destination for nature enthusiasts from the Czech Republic and throughout the world due to its remarkable aesthetic value, mineralogical and geological significance, and enchanting ambiance. The caverns are open Tuesday through Friday year-round, and on weekends from April to October. Tours of the caverns should be booked in advance, especially during the summer months (you can find the reservation phone number under the map).

Location: on the northern border of the Czech Paradise

The Chýnovská (Chýnov) Cave was founded in 1863 during quarry operations. After the necessary modifications, this became the first Czech cave open to the public in 1868. The ancient stone staircases can still be visible, and the journey through the cave provides a mini-history lesson. The Chýnovská Cave evolved in phases as a result of corrosion, which expanded numerous fissures and was helped by water passing through the cracks and washing off solid particles. The cave's main treasures are no stalactites and stalagmites, but colorful walls and ceilings with white, yellow, and brown marble facets alternated with black amphibolite fillings.

These two materials are responsible for the extraordinary circular formations visible in the walls. The cave's narrow tunnels descend 41 meters to the surface of an underground stream. The whole length of the cave system, which has not yet been fully explored, is approximately 1,400 m, with 280 m presently accessible to tourists. Outside of the viewing trip, speleologists and speleo-divers are investigating the spaces, which resulted in the discovery of huge, permanently water-filled areas with distinctive druses of flintstone and other minerals in the 1980s and 1990s.

Location: Dolní Hořice, Czech Republic

The Zbraovské Aragonite Caves is one of the Most Beautiful Caves in Czech Republic, is a national natural monument near Teplice nad Bevou, Czech Republic, in the Olomouc Region. The major focus of conservation is on Europe's key hydrothermal karst zones. Among these are the aragonite caverns and the surrounding woodlands. Discovered in 1912 and opened to the public in 1926, the caverns were formed by surface water as well as subterranean mineral water springs rich in carbon dioxide, which is utilized in spas in the surrounding hamlet and spa resort of Teplice nad Bevou. The caverns are loaded with stalagmite and aragonite formations that resemble geysers and doughnuts, while the cave's deepest floors are filled with carbon dioxide. Throughout the year, the temperature hovers at 14 °C (57 °F), and the caverns are the hottest underground areas in the Czech Republic.

The caverns were formed by two distinct karst processes. The first was surface and water corrosion, which penetrated the pores in the limestone and produced vast subterranean holes. The second was warm mineral water rising from depths of up to two kilometers (1.2 mi). The cave's aragonite and calcite are primarily generated by calcium carbonate. There are three ways for something to solidify. The first is calcite, which is the most prevalent mineral and is found in cave fills such as stalactites, stalagmites, sinter deposits, and valances. There are conical geyser stalagmites that are many tens of centimeters high. These can be found nowhere else on the planet. Aragonite is the second kind of calcium carbonite. This results in white needle-like crystals. There is a discharge of water and carbon dioxide. Vaterite, the third and most uncommon type of calcium carbonate, is absent.

Location: Olomouc Region, Czech Republic

The Na Pomez Caves are the Czech Republic's biggest accessible cave complex. However, the tour lasts no longer than 45 minutes. There are several lofty and tight hallways, as well as smaller domes. It's pretty chilly down there — only 7.7 degrees Celsius – so bring a hat. You may visit all year, however during the colder months, make a reservation.

The Na Pomez Caves are located 2 kilometers north of the hamlet of Lipová-lázn. The cave system was recognized in part as early as 1936, but it wasn't until 1949 that the caverns were fully investigated. The process to make them available to the public began in 1950 and was completed in 1955. The visitors' gallery is 390 meters long in total. The Na Pomez Caves are the biggest cave system in the Czech Republic, formed by marble dissolution, i.e. crystalline limestone. Narrow and, in some cases, high fissure aisles with smaller domes at intersections are frequent.

Location: Vápenná, Czech Republic

Anthonius Wale referenced The Na Špičáku Cave for the first time in written writings in 1430. The Na Špičáku Cave is one of the Most Beautiful Caves in Czech Republic. As a result, it is the oldest cave in Central Europe, as documented by written records. The cave functioned as a hiding spot for individuals, as evidenced by the numerous epigraphic writings on the walls. The earliest epigraph is from 1519. The German Mountain Club exposed the cave to the public between 1884 and 1885. However, the circumstances were basic at the time.

Since 1955, The Na Špičáku Cave is one of The Na Špičáku Cave the cave that has been exposed to the public in the manner and shape that it is now. The subterranean labyrinth of corridors and fractures is almost 400 meters long and was carved out of Devonian marble (the marine sediments are old 350 - 380 million years). The water from a melting glacier had a significant impact on the formation of the karst regions. This water gave the cave its final shape and formed the unique heart-shaped corridor profile. The path for the visit is 230 meters long and barrier-free.

Location: Supíkovice, Czech Republic

The Punkva Cave, which is part of the larger Moravian Karst, is one of the most well-known in the Czech Republic. During the journey, you will first see at the bottom of the Macoacha Abyss, which is 138 meters deep, and then board a boat and go down the subterranean river Punkva. It's a magical experience filled with strange insights into the illuminated and unlit depths of water and rocks. Because the trip is quite popular, it is best to reserve ahead of time.

In the spring and after heavy rains, there is sometimes so much water in the Punkva that boats only traverse a short segment of the path, or trips are canceled; if this happens, admission is decreased. Boat rides, on the other hand, are an essential feature of conventional excursions; for example, it is impossible to visit the Masaryk church in any other manner.

Location: north of the city of Brno, near the town of Blansko, Czech Republic

On two floors, a huge network of subterranean domes, passageways, and chasms was formed. Sloupsko-ovské Cave is a significant location where cave animal corpses (bear, lion, and hyena) have been discovered and is one of the Most Beautiful Caves in Czech Republic. Elika's Cave, with its magnificent stalactite décor, offers excellent acoustics, which is why it is occasionally utilized for chamber music concerts. During the 1997 restoration, the Stupovitá chasm was bridged, revealing a fresh atypical vista to tourists. The Nagel chasm, which is 80 meters deep, is the deepest subterranean abyss of its kind in the Czech Republic.

Visitors can view down to the bottom from the two platform bridges. Since 1997, a section of the sightseeing trip has included a visit to the world-famous archaeological site of Kůlna Cave, where a portion of a Neanderthal man's skull, estimated to be 120 000 years old, was discovered. The Šošůvka'sregion, found at the beginning of the twentieth century, is distinguished by delicate and colorful stalactite and stalagmite decoration.

Location: Sloup, Czech Republic

The Koněprusy Caves is one of the Most Beautiful Caves in Czech Republic and is a cave system in the center of the Bohemian Karst limestone area in the Czech Republic. It lies 6 kilometers (3.7 miles) south of Beroun in the Central Bohemian Region, southwest of Prague. The name is derived from a neighboring settlement called Konprusy. It is the biggest cave system in Bohemia, with a length of 2 km (1.2 mi) and a vertical range of 70 m (230 ft).

A hill named Zlat k (Golden Horse) rises above the settlement of Konprusy near another hill called Kobyla (Mare), and a site called V koku lies nearby (In a Little Horse). A short drive west brings you to Kotz, a karst plateau. Many tales have been spun around Kotz, one of which relates to sacred horses used by the Celts in military operations. An ancient village existed here, which some scholars believe may have acted as a center of cult worship during Celtic times; druids may have maintained a cult of the horse here.

Location: Koněprusy, Czech Republic