Danube-Gunz interglacial age of about 900,000 to 940,000 years. There are however indications that the Uhlenberg Profile may still be placed within the Pliocene, and it would thus not correlate with the Danube-Gunz interglacial. Also uncertain is its association with the North German classification because of its position in the underlying stratum of the Gunz it could correspond to the Bavelian or the Waalian interglacial. The Danube-Gunz corresponds at least in part to the Swiss Deckenschotter glaciations. Danube-Gunz interglacial The Danube-Gunz interglacial (), Danube-Gunz warm period ("Donau-Günz-Warmzeit"), often just Danube-Gunz, or also Uhlenberg interglacial ("Uhlenberg-Warmzeit") is the second-oldest named warm period of
Battle of the Danube had retreated, the Turks prepared to launch a new attack. Several months later 70,000 Turkish troops led by Ahmet Pasha crossed the Danube river to assault the Russians, encamping across from Ruse, around Slobozia. Well acquainted with his opponent at war, Kutuzov calculated that the Ottomans on the Lower Danube would direct their main force to cross the Middle Danube and to seize Bucharest. Therefore, destroying the fortresses of Silistria Nikopol, Kutuzov took off with his main forces to Ruse and Giurgiu. Zass in Little Wallachia and O'Rourke in Belgrade, covered his right wing, the left guarded by troops, located