Fig. 22From: Tectonics of the Monte Rosa and surrounding nappes (Switzerland and Italy): Tertiary phases of subduction, thrusting and folding in the Pennine AlpsView from Croppo on the Toce alluvial plain near Domodossola, the amphibolite facies Vanzone F5 anticline in the Moncucco summit and the Preja F5 syncline in the Bognanco valley, the greenschist facies Masera F6 syncline and the large Toce culmination of the Lepontine gneiss dome situated in the foot wall of the 30–35°SW-dipping Rhône-Simplon normal faultBack to article page