隐士洞穴

The cliffs consist of sandstone and lime-rich calcarenite layers formed during the Miocene epoch, around 14–15 million years ago. These sediments include fine volcanic debris and fossilised remnants of ancient marine organisms, reflecting the region’s former volcanic and marine environment. Over time, natural cavities formed in the looser layers—and during the Middle Ages, these were enlarged and shaped by human hands, giving birth to the hermit dwellings.

The rock faces of the hermit caves clearly display signs of ancient landslides and seismic activity. Distorted layering and structural displacements reveal the area’s tectonic history, offering not only scientific value but also educational potential. This geotope is ideal for outdoor learning, thematic walks, and school excursions focused on geology and sustainability.

From the 13th to the late 18th century, these rock-cut cells were inhabited by Christian hermits seeking solitude, contemplation, and spiritual deepening. The dwellings form part of the Hungarian Catholic Church's sacred heritage and are closely linked to the nearby National Shrine of Mátraverebély-Szentkút, a living pilgrimage destination that still attracts tens of thousands of visitors each year.