From the Casera Bordaglia di Sotto, looking south, you can see Monte Vas and Cima Ombladet. Cima Ombladet features the Zollner (Lower Devonian – Lower Carboniferous) and Hochwipfel (Carboniferous) Formations consisting of dark rocks. Their morphology is softer and covered with vegetation. The underlying Formation of the massive limestones of Monte Coglians (Lower to Upper Devonian) gives rise to bare rock walls, light grey in colour.

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The Val Bordaglia Line
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Folds in Monte Vas