プランケンフェルスの滝・トップ5

The Arzloch is a popular hiking destination and often still considered a hidden gem. It's a protected natural monument, a wooded area known for its atmospheric, wild gorge with eroded sandstone layers. The waterfall itself is relatively small, with a height of about 3 to 4 meters. Access to the waterfall is natural. Hikers should wear sturdy footwear, as the path leads over roots, narrow trails, and uneven forest floor. The surrounding area is the real highlight. The damp local climate has carved a unique gorge into the Rhaetian sandstone layers, which is home to rare animal and plant species. The bizarre sandstone formations, which can resemble honeycombs due to weathering, are geologically interesting.

The Aftergraben is the smaller version of the Teufelsgraben, but just as beautiful and interesting

Very beautiful watercourse.

The natural spectacle is always beautiful

The Arzloch is an atmospheric, wild gorge with eroded sandstone layers. Due to its humid local climate, it is home to rare animal and plant species, a waterfall and the "Markgrafentisch" rock formation. To get down from Eckersdorf, you have to climb a little and cross a narrow wooden bridge. A real experience.

It's beautiful how the clear water rushes over the mossy rocks. It's not one of the big waterfalls, but it's enchanting nonetheless.

Incredibly primitive, wild and overgrown. Very beautiful.

Sinter steps, also known as sinter terraces, are deposits of porous limestone tuff or densely layered limestone sinter in a stream or flowing body of water and, in contrast to stalactites, form relatively quickly. Larger sinter deposits are present, for example, in the Croatian Plitvice Lakes area or the Turkish Pamukkale. The water surfaces arise when bars of secreted calcium carbonate cross the direction of flow in the area of a watercourse. Splash water and changes in water temperature in conjunction with obstacles on the valley floor promote the formation of such calcareous tuff lakes.[1] Small deposits initially form on branches, twigs and stones that have fallen into the water and then, over time, larger and larger secretions form in the stream. Over time, these resulting bars can form smaller basin shapes, the walls of which are marked as steps and damming up the water in a cascade-like manner. The stages are mostly geologically younger formations from the Quaternary. Source: Wikipedia