周辺の峡谷・トップ20

The sandstone cave in the Schwarzachklamm got its name from the Swedish king Gustav Adolf, who is said to have attended a sermon given by the Nuremberg pastor Cornelius Mareius there in 1632 after a battle victory in the Thirty Years' War. It is the largest of the erosive washes in the Schwarzach Gorge. https://urlaub.nuernberger-land.de/detail/id=6220ae58f24f424775ea02b6

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The waterfall now consists of a small trickle in summer, at most to wash your hands.

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In fact, everything has already been said here. The hiking trail between the Schwarzach and Karlshöhle is unparalleled. But not on the weekend.

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The cave together with the Schwarzach is a highlight in the area. Avoid walking on Sundays and public holidays. It starts with the parking lot.

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The Schwarzachschlucht is an approximately 2.2 kilometer long, gorge-like river valley south of Schwarzenbruck in the Central Franconian district of Nürnberger Land in Bavaria. It is named after the Schwarzach river. The gorge is a nature reserve and a popular local recreation area. On the north bank of the river, hiking trails and a geological nature trail with information boards lead through the gorge. There is a former rocky path on the south bank, but it is now closed due to the risk of falling. There are also some abandoned quarries there. Water sports are not possible on the river. Source: Wikipedia

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The Karlshöhle with its small spring outlet is one of the two largest caves here in the Schwarzachklamm.

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The small river Schwarzach has cut deep into the Burgsandstein between the Schwarzenbruck district of Gsteinach and the bridge canal of the Ludwig-Danube-Main Canal. The middle castle sandstone was formed about 215 million years ago during the Mesozoic (Triassic). This type of rock is widespread in western and southern Middle Franconia[6]. Hard and resistant rock like the Burgsandstein narrows a valley to a gorge. The erosive power of the river could only cut into the rock along fissures and faults. The hard sandstone types form the steep gorge walls. Less hard rock layers such as clay layers and weak zones led to the riparian areas being undermined, especially during high water. This resulted in scours, overhanging roofs and surf caves. The two largest caves of this type are the Karl's Cave and the Gustav Adolf Cave. Source: Wikipedia

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A great gorge that should only be entered with suitable footwear.

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Please note: Cycling and mountain biking are prohibited in the Schwarzachklamm nature reserve. Please park your bike and explore the natural experience of the Klamm on foot!

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Please note: Cycling and mountain biking are prohibited in the Schwarzachklamm nature reserve. Please park your bike and explore the natural experience of the Klamm on foot!

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One of two large cavernous washouts formed due to the erosive action of the Schwarzach.

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Beautiful bridge, makes it possible and more exciting to continue the tour at this point.

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Hard and resistant rocks such as Burgsandstein narrow a valley to form a gorge. The erosion power of the river could only cut into the rock along cracks and faults. The hard sandstone types form the steep gorge walls. Less hard rock layers such as clay layers and weak zones led to the erosion of the banks, particularly during floods. This created scouring, overhanging roofs and surf caves. The two largest caves of this type are the Karlshöhle and the Gustav-Adolf-Höhle. (Source: Wikipedia)

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Hard and resistant rock like the Burgsandstein narrows a valley to a gorge. The erosive power of the river could only cut into the rock along fissures and faults. The hard sandstone types form the steep gorge walls. Less hard rock layers such as clay layers and weak zones led to the riparian areas being undermined, especially during high water. This resulted in scours, overhanging roofs and surf caves. The two largest caves of this type are the Karl's Cave and the Gustav Adolf Cave. The Gustav Adolf Cave got its name from the fact that the Swedish king attended a sermon given by the Nuremberg pastor Cornelius Mareius here in 1632 after a battle victory (see Affalterbach) in the Thirty Years' War. Various celebrations take place here again and again, which have clearly left their mark. Immediately after the Gustav-Adolf-Cave, shortly before a house set into the rock, there are holes in the rock wall that are weathered in the form of a network or honeycomb. (Source: Wikipedia)

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The Schwarzachklamm or Schwarzachschlucht is an approximately 2.5 km long river section of the Schwarzach between Schwarzenbrück and the bridge canal of the Ludwig-Danube-Main Canal; it is one of the 100 most beautiful geotopes in Bavaria. Two particularly beautiful parts of the Schwarzachklamm are the Karlshöhle and the Gustav-Adolf-Höhle. If you don't want to take the same route back and forth, we recommend the Ludwig-Danube-Main-Canal as an alternative.

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The Karlshöhle is one of the two large cave-like washouts that were formed due to the erosive action of the Schwarzach. It is one of the highlights on the way through the gorge, which has been a nature reserve since 1936.

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The Gustav-Adolf-Höhle is the largest of the erosion washouts in the Schwarzachklamm. The name goes back to 1632, when the Swedish King Gustav Adolf was listening to a sermon by the Nuremberg pastor Cornelius Mareius during the Thirty Years' War.

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This section should be done with suitable footwear. In wet weather it can get very muddy and greasy.

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There is a small spring outlet in the center of the cave.

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The cave takes its name from the Swedish king who, after a battle victory in the Thirty Years' War (1632), attended a sermon by the Nuremberg pastor Cornelius Mareius.

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