Jerlochovice walls

The southern slopes above the left bank in the Husí potok valley in Jerlochovice consist of sandstone and clayey sandstone deposits. The sediments originate in the period about 15 million years ago, when the marginal parts of the shallow sea reached the area of ​​the Carpathian foredeep, the so-called Lower Baden Trench. Such places can be seen in various places on the western side of the Moravian Gate in the Oder Mountains, in the case of…