Tips
Uwe
February 22, 2025
Hiking
The Roschertal owes its existence to a geological peculiarity. It is a breakthrough valley of the Mandau, which has cut through a basalt layer and underlying tertiary tuff layers. Such valleys are formed when a river erodes rock over long periods of time, while the surrounding area may rise or the water cuts deeper.
Geological development:
1. Tertiary deposits: In the Tertiary period (around 65 to 2.6 million years ago) the area was characterized by volcanic activity. Tuff - a rock made of volcanic ash - was deposited. Later, basalt flows poured over it and formed a resistant covering layer.
Geological development:
1. Tertiary deposits: In the Tertiary period (around 65 to 2.6 million years ago) the area was characterized by volcanic activity. Tuff - a rock made of volcanic ash - was deposited. Later, basalt flows poured over it and formed a resistant covering layer.
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Nearby routes
Best routes near Roschertal Gorge
4.8
(15)
42
hikers
12.2km
03:19
170m
170m
Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.
Moderate
4.7
(11)
24
hikers
14.0km
03:50
210m
210m
Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.
Moderate
5.0
(4)
11
hikers
9.15km
02:34
180m
180m
Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.
Moderate
Details
Informations
Elevation 330 m
Weather
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Thursday 8 October
13°C
7°C
28 %
Additional weather tips
Max wind speed: 21.0 km/h
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