It leaves Lake Iseo at Sarnico and, after traveling a zone of moraine deposits, it joins the river Po at Torredoglio, not far from Cesole and Scorzarolo, in the province of Mantua.
12.
Wegener's continental drift hypotheses is a logical consequence of : the theory of thrusting ( alpine geology ), the isostasy, the continents forms resulting from the supercontinent Gondwana break up, the past and present-day life forms on both sides of the Gondwana continent margins, and the Permo-Carboniferous moraine deposits in South Gondwana.
