Entenloch Gorge
River Canyon·Germany/Austria·Großache (also called Tiroler Achen)·Rhaetian limestone and Jurassic rock
The Entenloch Gorge is a 2.5-kilometer-long water gap carved by the Leukental river, forming a natural border between Bavaria and Tyrol. It is characterized by steep rock walls and is geologically significant for its formation in resistant limestone and Jurassic rock layers since the last ice age. The gorge has been a site of both natural challenges, like extreme floods, and human activity, including historical smuggling routes and modern tourism.
Key Facts
- ›The gorge is 2.5 km long and is a water gap of the Leukental.
- ›It is formed by the Großache river cutting through Rhaetian limestone and Jurassic rock.
- ›The gorge serves as a natural border between Germany and Austria.
- ›The width of the gorge was widened from approximately 3.4 meters to 12 meters between 1906 and 1922.
- ›A 35-meter-long hanging bridge was constructed in 2021 as part of a sustainable tourism project.
- ›The 'Smugglers' Path' associated with the gorge is 7.5 km long.
Entenlochklamm
River Erosion
Steep Rock Walls, Pilgrimage Site Maria Klobenstein, Hanging Bridges, Smugglers' Path, Landslide Rock Deposit
About Entenloch Gorge
The Entenloch Gorge, known in German as Entenlochklamm, is a striking 2.5-kilometer-long water gap carved by the Leukental river. Situated on the border between Bavaria, Germany, and Tyrol, Austria, the gorge is a dramatic passage through a transverse mountain range characterized by steep rock walls. The river, known as the Großache as it approaches the gorge and then the Tiroler Achen as it flows into Tyrol, has sculpted this landscape over millennia.
Geology and Formation
The gorge's formation is attributed to the Großache river's persistent erosion through resistant geological layers. It cuts through steeply placed bars of Rhaetian limestone and Jurassic rock, which form the southern boundary of the Oberwössener depression. This durable bedrock meant that the river could only create a gorge-like passage since the last ice age. Above the gorge on the Austrian side, the pilgrimage church Maria Klobenstein is nestled in a depression formed by weathered layers, with its name derived from a large rock deposited by a landslide.
Historical Context and Development
The Entenloch Gorge has been a site of both natural hazards and human activity. Since the 16th century, the area has experienced several extreme floods of the Großache, prompting significant flood control measures. A notable disaster in 1899 led to a large-scale flood control project, with the regulation of the Großache from 1906 to 1922 involving blasting to widen the gorge from its original narrow stretch of about 3.4 meters to 12 meters. This widening aimed to mitigate flooding upstream in the Kössen valley basin by preventing debris from becoming wedged.
Historically, the gorge was also associated with a smugglers' path, accessed via a hanging bridge. This route was used by residents of the border area to transport goods like cigarettes, alcohol, and coffee, thereby evading customs duties.
Modern Tourism and Accessibility
In recent years, efforts have been made to enhance the touristic appeal of the Entenloch Gorge in a sustainable manner. As part of an Interreg project, a 35-meter-long hanging bridge was constructed in 2021 at a height of 28 meters, accompanied by a new viewing platform, resting spots, and parking facilities. This development allows visitors to experience the gorge's natural beauty more readily. A loop trail incorporating both hanging bridges and the viewing platform takes approximately 50 minutes to complete and is moderately hilly. The longer 'Smugglers' Path' from Kössen to Schleching spans 7.5 km and is estimated to take about two hours to walk.
Source: Wikipedia ↗
Frequently Asked Questions
What geological features define the Entenloch Gorge?
The Entenloch Gorge is carved through resistant layers of Rhaetian limestone and Jurassic rock. These formations have allowed the Großache river to create a deep, gorge-like passage since the last ice age.
How was the Entenloch Gorge formed?
The gorge was formed by the erosive power of the Großache river cutting through a transverse mountain range of steep rocks. This process has been ongoing since the last ice age, with significant widening efforts occurring in the early 20th century.
What activities are available at Entenloch Gorge?
Visitors can walk a loop trail over two hanging bridges, including a 35-meter-long one built in 2021, and visit a viewing platform. The 'Smugglers' Path' offers a longer hiking experience of 7.5 km.
What is the historical significance of the Entenloch Gorge?
Historically, a hanging bridge over the gorge led to a smugglers' path used to avoid customs duties on goods like cigarettes, alcohol, and coffee. The gorge also experienced extreme floods that necessitated flood control projects.
Where is Entenloch Gorge located?
The Entenloch Gorge is situated in the Bavarian-Tyrolian border area, between Kössen in Germany and Ettenhausen near Schleching. It is part of the Leukental and is crossed by the Großache river.
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