바이에르바흐‬에서 가장 멋진 ‪20‬개의 천연기념물

현장의 자연에 기록된 역사를 가진 Teufelsfels,

멀리서 보면 악어 머리임을 충분히 알아볼 수 있습니다.

Incredibly beautiful area that I always enjoy hiking through. It's worth it!

What nature creates in combination with human imagination...

The Devil's Stone of Halmstein > a geotope and natural monument The quartz conglomerate ridge protrudes very conspicuously and isolated from the morphological terrain ridge. Former quartz gravel was largely silicified during diagenesis, so that the rock today consists almost exclusively of SiO2. The layer surface of the steeply standing block consists of quartzite (originally sandstone) and has scour-like erosion forms. (Bavarian State Office for the Environment (LfU)) https://www.umweltatlas.bayern.de/standortauskunft/rest/reporting/sb_geotope/generate?additionallayerfieldvalue=275R009

Block stream Kaser Steinstube > a geotope The impressive block stream of the "Kaser Steinstube" begins below the quartz conglomerate horizon, which is broken into large plates and is located at the edge of the plateau, and stretches down the slope for more than 100 m. A temporary stream flows through it. In some places the quartz conglomerate blocks pile up on top of each other and form small cover caves. The block stream was formed in the Pleistocene at a time of increased erosion and soil flow in the periglacial area. The geotope was awarded the "Bavaria's 100 most beautiful geotopes" seal of quality and is explained on site with an information board. Further information at: https://www.lfu.bayern.de/geologie/bayerns_schoenste_geotope/index.htm. https://www.umweltatlas.bayern.de/standortauskunft/rest/reporting/sb_geotope/generate?additionallayerfieldvalue=277R001 (Bavarian State Office for the Environment (LfU))

Crocodile Rocks of Landerham >a geotope This quartz conglomerate block, which has a crocodile-like shape when viewed from the southeast, forms a landmark that can be seen from afar in an open field. The block is the remnant of a formerly more widespread conglomerate cover and probably slipped from its original higher location within a solifluction cover in the Pleistocene. The block shows, as is often the case in the quartz conglomerate bank, a grain size change from gravel (conglomerate) to sand (sandstone). (Bavarian State Office for the Environment (LfU)) More information: https://www.umweltatlas.bayern.de/standortauskunft/rest/reporting/sb_geotope/generate?additionallayerfieldvalue=277R002

Movement is the goal! Get out whatever the weather! This location is worth it at any time of the year!