오버팔츠의 아우어바흐 최고의 러닝 경로

아름다운 동굴과 바위 풍경입니다. 겨울에는 박쥐 보호를 위해 동굴에 들어가지 마십시오!

카르스트의 싱크홀이나 광산 갱도 위를 연상시킵니다.

겉보기에는 인상적으로 아름답지만, 안이 어떻게 생겼는지는 판단할 수 없습니다.

A very beautiful landscape

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.