klesajúci

Klesajúci (Slovak for "falling") refers to a phenomenon observed in certain types of rock formations, particularly in limestone or dolomite areas, where sections of rock appear to be suspended above the ground but are actually detached from the main cliff face. This optical illusion occurs due to the erosion of softer rock layers beneath the harder caprock, creating an overhang that makes the rock appear as if it is falling. The term is commonly associated with landscapes in Slovakia, particularly in regions like the Slovak Paradise (Slovenský raj) and the Low Tatras (Nízke Tatry).

The formation of klesajúci structures is a result of natural geological processes over millions of years. Rainwater, slightly acidic due to dissolved carbon dioxide, seeps into cracks in the rock, gradually dissolving the limestone and widening the fissures. Over time, this leads to the collapse of weaker sections, leaving behind dramatic cliffs and overhangs. Some of the most famous examples include the Demänovská cave system and the rock formations near Liptovský Mikuláš.

Klesajúci formations are not only a geological curiosity but also a popular tourist attraction. Their striking appearance has inspired local legends and folklore, often depicting them as the remnants of ancient battles or the work of mythical beings. Hikers and climbers frequently visit these sites, though caution is advised due to the unstable nature of the rock.

While the term *klesajúci* is primarily used in Slovak, similar phenomena exist worldwide, such as the "tors" of Sweden or the "hoodoos" of North America. These features highlight the dynamic and ever-changing nature of Earth's landscapes.