イルシェンベルクの峡谷・トップ6

On July 27, 2024, the Jenbachsteig was closed due to a landslide, risk of rockfall and thus danger to life.

The Kupferbachtal was created at the end of the last Ice Age when the meltwater from the Inn-Chiemsee Glacier and partly from the Isar Glacier could not flow into the Rosenheim Basin, which was still filled with ice, and thus a longer period of standstill at the edge of the glacier (so-called Ellkofen Stage). Northeast towards Wasserburg or Gars towards the Inn (“surrounding channel”). The surrounding channel was formed and used between around 18,000 years ago and around 16,500 to 17,000 years ago. Today the area is characterized by several strong calcareous springs. Source and further information https://de.m.wikipedia.org/wiki/Kupferbachtal

People not only hike or cycle along the Mangfall, you also see a lot of people swimming or even barbecuing.

Not only do people hike or cycle along the Mangfall, you can also see a lot of people swimming or even barbecuing.

Nice moderate hike mainly through the forest.

The Jenbachsteig is a great section - absolutely recommendable! Currently (05/23) blocked until further notice.... Flood damage, not accessible.

Nice view of the Mangfall

When it is wet, the Jenbachsteig is very slippery because the water and the hikers have to cross smooth stones. If there is a lot of water, parts of the path could also be flooded, since the path goes right up to the river bed or is only partly at the edge of the river bed. With suitable hiking boots and a little sure-footedness, however, the path is not a problem and is a beautiful walk.