Source Gseng in the Johnsbachtal

The debris source in the Gseng springs from an artificially piled pile of mixed-grained fine to block debris made of dolomite and lime, in which, among other things, asphalt chunks, granite cubes and various stone material from house demolitions etc. are stored. The original appearance of the source is unknown. It is likely to come from cracks in a lime bank, as it always originates in the same place despite the rearrangements in recent years. Presumably, however, the source mouth was always covered with rubble. At the time of the first take-up at the time of the first take-up in 2004, the source was in the raw state due to the constant excavations and pile-ups. Since the end of mining in autumn 2008, however, it has been able to regenerate.