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
Commissions of the Danube River "Russian domination" in Southeastern Europe after the Crimean War, so the 1921 convention "stood for an effort to block the resurgence of German or Russian power." The European Commission, again ensconced in its quarters at Galatz, found things very bad indeed at the mouths of the Danube after the war. Silt had choked the channel again, and it seemed as though attempts to improve the situation was continually going awry. Economic affairs along the entire river were so bad that the League of Nations instituted in 1922 an inquiry by a special committee, headed by an American, Walker D. Hines