Over the millennia, the weathering and erosion of the sandstone, with its varying degrees of hardness, have produced bizarre rock formations, e. g. rock pinnacles, rock faces, rock walls and rock blocks. In addition, the small-scale weathering of strata of differing hardness has produced caves, natural arches and table rocks (Devil's Table). On the almost two-kilometre-long rock terrace of the Altschlossfelsen, fractures, overhangs and honeycomb weathering can also be observed. By contrast, felsenmeers and blockfields tend to be found more in the central Palatine Forest.