The 1598 landslide was triggered by a prolonged period of torrential rain lasting several days.
The debris from the slide initially dammed the Nysa Kłodzka, creating a temporary lake that later burst.
Geologically, the cliff is composed of Variscan sedimentary rocks of the Bardo Unit.
The site is a protected natural monument designated for its unique geological exposure.
The Rock Falls in Bardo, known as Obryw Skalny, is a significant geological formation created by a massive landslide on the slopes of Mount Kłodzka Gora. The landslide occurred in 1598, following intense rainfall that destabilized the steep, unstable bedrock. This event dramatically altered the flow of the Nysa Kłodzka river, forcing it to change its course. The site exposes sedimentary rock layers, revealing the complex geological history of the Sudetes mountains. Today, it serves as an educational site highlighting active geomorphological processes. The cliff face reaches a height of approximately 200 meters above the river valley. Trails through the site provide insight into the post-disaster landscape recovery. Visitors can observe how vegetation has reclaimed the slope over the past four centuries.
The viewing point on the ridge path that offers a panoramic perspective of the cliff face and the river below.
Wear sturdy hiking boots with good grip, as the terrain is uneven and can be slippery after rain.
Bring binoculars to better observe the geological layers and nesting birds along the cliff face.
Check local weather reports before ascending, as the trail can become hazardous during heavy precipitation.
Do not attempt to climb the face of the rock fall, as the sediment remains loose and unstable.
Stay strictly on marked trails to prevent erosion and avoid triggering minor rockfalls.
