Ice Age English Channel River the Fleuve Manche Received Flows of Thames & Rhine South Into Atlantic Bay of Biscay

Translate:

During the Ice Age, the Elbe river of northwest Germany flowed through the eastern portion of Dogger Land or Atland (now the southern portion of the North Sea’s floor), to the southwest of which the Rhine and Thames met above where now is the English Channel, to flow southwest (as the Fleuve Manche) into the Bay of Biscay (eastern Atlantic), when the sea level was a few hundred feet lower, when inland were snowpacks of the Ice Age, far enough from the sea which was much warmer then, the engine for the Ice Age in the aftermath of the fountains of the deep roughly double the volume of ocean water for Noah’s Flood (see Page at right Natural Selection by Noah’s Flood).