• Schlattain-Clavadatsch-Padella-Schuppen

    Origin of the Name

    Alp Clavadatsch (GR)

    Rank
    tectonic slice
    Status
    local name (informal)
    In short

    The Schlattain-Clavadatsch-Padella Slices form small isolated klippes, located in the core of the synclinorium of the “Samedan Zone” and composed of Triassic to Late Cretaceous sediments. They were thrust onto the cover of the Err Nappe and therefore attributed to the Bernina Nappe Complex.

    Nomenclatorial Remarks

    Trais-Fluors-Schuppe p.p. (Cornelius ----)

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