The Camughera Nappe is a Middle Penninic tectonic unit located in the region of Domodossola. It consists of rocks similar to the crystalline basement of the Siviez-Mischabel Nappe and may be the continuation of this nappe. It is folded by the large Vanzone Antiform and overlies the Ruginenta Nappe.

Grobflaseriger heller Augengneis, oft von turmalinführender feinkörniger Schiefer und verschiedene Paragneise begleitet.