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
Army of the Danube (1806–1812) Army of the Danube (1806–1812) The Army of the Danube (or Danube Army; alternately the Army of Moldavia) () was a field army of the Russian Empire, created for the Russo-Turkish War of 1806–1812. Commanded by Admiral Pavel Chichagov from May 1812, it merged with the Third Reserve Army of Observation to form the Third Western Army in September during the French invasion of Russia. The Army of the Danube ended the Russo-Turkish War of 1806–1812 on the Danube; its commander-in-chief, General of the infantry Mikhail Kutuzov, signed the peace treaty ending the war at Bucharest on . Admiral Pavel