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Der GEOpfad
Die Pfrontener und Vilser Berge gehören zu der Region der Nördlichen Kalkalpen. Der GEOpfad stellt die Ergebnisse der Forschung im Bereich der Geologie seit Beginn der Erkundung vor 150 Jahren dar.
Dem aufmerksamen Wanderer soll die geologische Entstehung der Pfrontener und Vilser Berge in der Landschaft selbst erschlossen werden. Die Berge bestehen aus unterschiedlichen Gesteinsarten, die durch Verwitterung und Abtragung ihr charakteristisches Aussehen erhalten haben.
Der GEOpfad Pfronten - Vils führt euch durch hochalpines Gelände im Naturschutzgebiet "Aggenstein". Aus diesem Grund wurde bewusst auf das Aufstellen von Informationstafeln verzichtet. Statt dessen markiert im Gelände ein Pfosten mit dem GEOpfad-Logo die betreffende Station. Der GEOpfad beginnt an der Bergstation der Breitenbergbahn und führt über den Aggenstein zur Bad Kissinger Hütte, Vilser Alm und Vils wieder zurück zur Talstation der Breitenbergbahn.