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| | GEO_PLATE_T-25 (Site not responding. Last check: 2007-11-03) |
 | | The Alps are part of the belt of deformed rocks that extends across southern Europe into Asia Minor, thence into northern India, Russia, and China. |
 | | Northern Apennines: nappes of turbidite and carbonates of Cretaceous age, deformed in post-Oligocene by action of Carnics/Ligurian plate during eastward migration of arc-subduction zone. |
 | | The present geomorphology of the Alps is the consequence of interplay among structures established in the Tertiary, active neotectonics including vertical uplift, the continuing action of streams (many structurally controlled before the Pleistocene), and, above all, intense erosion by mountain glaciers, particularly during the Riss and Würm glacial episodes (Watts, 1971). |
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