Hällingsåfallet skapar då ån forsar ner i en djup 800 meter lång kanjon. Den djupa klyftan är troligen en sprickzon i skifferberget som vidgats under den senaste istidens avsmältning för cirka 9 000 år sedan. Mellan de branta och över 50 meter höga klippväggarna står en ständig vattendimma. Den fuktiga miljön har gett upphov till en särpräglad moss- och lavflora.
Källa: https://sv.wikipedia.org/wiki/H%C3%A4llings%C3%A5fallet
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