Category
page 1Geology of the Alps
Alpine orogeny
orogenic phase in the Late Mesozoic (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt
Glarus thrust
landform
Adriatic Plate
small tectonic plate
Würm glaciation
glacial period in the Alps
Riss glaciation
alpine glacial period in the Pleistocene epoch
Hațeg Island
prehistoric island
Gunz glaciation
glacial period
Danube glaciation
glacial period in the Alps
Mindel glaciation
glacial stage in the Alps
Periadriatic Seam
border between the Adriatic and European plates
Iberian plate
small tectonic plate now part of the Eurasian plate
Penninic
The Penninic nappes or the Penninicum, commonly abbreviated as Penninic, are one of three nappe stacks and geological zones in which the Alps can be divided. In the western Alps the Penninic nappes are more obviously present than in the eastern Alps (in Austria), where they crop out as a narrow band. The name Penninic is derived from the Pennine Alps, an area in which rocks from the Penninic nappes are abundant.
Southern Alps
southern parts of the Eastern Alps in Central Europe
Geology of the Alps
formation and structure of the European Alps
Austroalpine nappes
geological formation in the European Alps
Piemont-Liguria Ocean
historic ocean
Aarmassif
The Aarmassif or Aaremassif (German: Aarmassiv) is the easternmost geologic massif in the Swiss Alps. It contains a number of large mountain chains and parts of mountain chains.
Hohe Tauern Window
region in the Austrian Central Eastern Alps where rocks of the underlying Penninic nappes ere exposed
Helvetic nappes
geological structures thrust north during Alps orogeny
Briançonnais zone
piece of continental crust in the Penninic nappes of the Alps
Valais Ocean
Subducted ocean. Remnants found in the Alps in the North Penninic nappes.
Main Dolomite
rock formation in the Alps
Wetterstein Formation