Terracing of river Including a stage of Erosion and terracing valleys. Northward rise considerable uplift, of stratified drift in of area of Lake Agassiz with return of humid river valleys. Land nearly complete before conditions, Alpine passage of European the ice was melted on glaciation (third flora to Greenland; the country crossed by Glacial epoch), and succeeded by subsidence Nelson River; but rise the second great rise there, admitting warm about Hudson Bay is still of Lakes Bonneville currents to Arctic Sea. going on; 7,000 to 8,000 and Lahontan. Very Minor climatic changes, years since ice-melting recent subsidence including a warmer uncovered Niagara and and change to present stage than now. Upper falls of St. Anthony. aridity. and outer portions of Indo-Gangetic alluvial plain; extensive deposits of Hwang Ho, and destructive changes of its course. Abundant deposition of Depression probably Final departure of the englacial drift. Stone almost to the present ice-sheets; glacial implements in river level. Restoration of rivers forming eskers gravels of Ohio, Ind., arid climate; nearly or and kames. Loess and Minn. Laurentian quite complete deposited while the lakes held at higher evaporation of Lakes region of the Alps was levels, and Lake Bonneville and Lahontan.depressed lower than Agassiz formed in Red Formation of the "adobe"now. Upper (englacial) River basin, by continuing through the till, and asar, of barrier of retreating second Glacial, Sweden. Marine ice, with outlets over Champlain, and Recent submergence 500 to 600 lowest points of their epochs. feet in Scotland, present southern Scandinavia, and water-shed. Marine Spitzbergen. submergence 300 to 500 feet on southwest side of Hudson Bay.