뮐리츠탈‬에서 가장 멋진 ‪20‬개의 천연기념물

나무 꼭대기 너머의 아름다운 전망.

Einsiedlerstein, a sandstone formation in the Dippoldiswalde Heath. Information: The freestanding boulder of the Einsiedlerstein was detached from the originally contiguous sandstone complex by erosion. Numerous small weathering features (honeycomb, iron slabs) bear witness to the chemical and physical processes on the walls of the ashlar sandstone. The Einsiedlerstein is a protected geological natural monument.

A small idyll on the outskirts of Dresden❤️

The hermit stone is a historical monument to the hermit Dippold, who lived in a hut here on Dippoldiswalder Marktsteig and looked after the Katharinen Chapel

The Friedrichgrundbach stream flows for about 1.5 km through the Friedrichsgrund, named after Elector Friedrich August III of Saxony. Towards the end of the 18th century, it was built and embellished with a total of 10 bridges, similar to the Seifersdorfer Valley.

The 476 meter high Wilisch consists mainly of basalt, which is due to its volcanic origin. The last volcanic activity that led to the formation of the Wilisch dates back to the Tertiary, more precisely the Oligocene to Miocene. The region around the Wilisch is also geologically interesting because it is rich in basalt, which in the past led to the intensive extraction and use of this rock. The view from the Wilisch and the triangulation column are also really very impressive.

Beautiful hiking trails often directly along the stream.

Very nice place to take a break, you have a wonderful view.