노이하우스 안 데어 페그니츠 최고의 러닝 경로

Really impressive how the Brocken holds up here

I had already briefly considered what kind of mushroom dish it could become... given its size... a truly impressive chunk of reef limestone

It is very beautiful here

It is a small, natural opening in the rock through which water flows into the underground cave system. The name "swallow hole" comes from the idea that this is where the water is "swallowed". The area around the swallow hole is part of a hiking trail and visitors can watch the water disappear into the hole. However, access to the cave system is not permitted for safety reasons.

The Mystery Grotto is located near Neuhaus an der Pegnitz and is part of the Karst Hiking Trail. The name of the grotto comes from a legend that tells of the "White Lady". This legend says that the cursed soul of Countess Kunigunde von Leuchtenburg, who lived in the 13th century, is said to appear in the grotto as a restless spirit. The grotto is about 12 meters wide and 16 meters long and offers an impressive hall. Beautiful ice formations can be admired, especially in winter. The entrance to the grotto is partially walled up and closed in winter during the bat protection period. The grotto is only accessible from April to September.

The Distlergrotte, also known as Finstermühlhöhle, is a karst cave near Neuhaus an der Pegnitz. The cave has a total length of about 90 meters and is constructed as a descending system of floors with crevices and small halls. It contains sinter groups, moon milk and ceiling potholes. The entrance is partially walled up and closed with an iron bar in winter during the bat protection period. The cave is only accessible between April 1 and September 30. Ice Age animal bones of mammoth, woolly rhinoceros, cave bear, hill hyena, reindeer, red deer, wild horse, bison and ancient cattle have been found in the cave.

"A ponor (from South Slavic) - also known as a swallow hole, Schwalgloch (in Westphalian), sinkhole, Bachschwinde, katavothra (modern Greek καταβόθρα) or gully - is an opening in the surface of the land through which a flowing or standing body of water drains off and continues to flow underground. The ponor is a typical karst phenomenon that occurs in many regions of the world and therefore often occurs in regions whose subsoil consists of limestone. Sink holes that lie in the karst funnels typical of karst areas are called ponordolines." https://de.wikipedia.org/wiki/Ponor#:~:text=Der%20Ponor%20ist%20eine%20typische,liegen%2C%20werden%20als%20Ponordolinen%20bezeichnet.

The karst cave Westliche Brentenfelshöhle is located on the southwest slope of the Brentenfelsen in the Upper Palatinate district of Amberg-Sulzbach, about 1400 meters north-northwest of the center of the village of Döttenreuth in the community of Königstein in the state of Bavaria in Germany. In front of the entrance to the small cave there is a large rock gate (rock gate near Döttenreuth), immediately behind which lies the portal of the cave. This shows very little sinter decoration.