Bündner slate
From Wikipedia, the free encyclopedia
| Geology of the Alps |
|---|
 |
| Tectonic subdivision |
| Penninic nappes |
| Austroalpine nappes |
| Southern Alps |
| Formations & rocks |
| Geological structures |
|
Aarmassif | Dent Blanche klippe | Engadine window | Flysch zone | Giudicárie line | Greywacke zone | Hohe Tauern window | Molasse basin | Penninic thrustfront | Periadriatic Seam | Ivrea zone | Lepontin dome | Rechnitz window | Rhône-Simplon line | Sesia unit |
| Paleogeografic terminology |
| Briançonnais microcontinent |
| Piemont-Liguria Ocean |
| Apulian or Adriatic plate |
''This article is about the geology of the (European) Alps. For the main article see: geology of the Alps
The Bündner slate (German: Bündnerschiefer) is a geologic formation found in the Penninic nappes in the Alps. In French the name shistes lustrés is used.
The formation is a few kilometers thick monotonous layer of Mesozoic dark claystone, marl and sandy limestone. These sedimentary rocks were metamorphosed to calcareous phyllites, a rock abundant in micas that define their dominant foliation.
