View from the slope of Hirschkarlgrat into the Hölltal. The debris tongue shown in the centre of this photo is most probably the consequence of periglacial processes having shaped the valley at a time when the climate was still colder.
View from the slope of Hirschkarlgrat into the Hölltal. The debris tongue shown in the centre of this photo is most probably the consequence of periglacial processes having shaped the valley at a time when the climate was still colder.