The Beskids are built of flyschAlternating hard sandstones and soft claystones, laid down on the floor of a Cretaceous sea and later thrust up into mountains. - layers of hard Godula sandstone interleaved with soft claystones. The claystones act as slip surfaces: sandstone blocks slide slowly down the slope on them and the ridge comes apart.
Where the massif tears, cracks are left behind, and out of them grows a fissure cave. Cyrilka is one: a network of cracks on three levels linked by squeezes. In places the passages are barely a few tens of centimetres high, elsewhere up to eight metres, and here and there they narrow to tight joints. This is what sets the Beskid caves apart from karst ones: their passages follow vertical cracks in the sandstone, so the walls tend to be almost straight. That is why people long suspected them to be man-made rather than natural.
The Radhošť ridge is full of such cracks - they have long been called the Radhošťské ďůry, the Radhošť holes. Cavers have counted about thirty of them here.