On the Evidences of a Submergence of Western Europe, and of the Mediterranean Coasts, at the Close of the Glacial or So-Called Post-Glacial Period, and Immediately Preceding the Neolithic or Recent Period . shells * In some instances streams may have preceded these later gravel trails. f The specimen is in the Boulogne Museum, J See section in .Quart, Journ. Geo], Hoc, vol. 48, Plate 7, fig. 1, OF WESTERN EUROPE AND THE MEDITERRANEAN COASTS. 911 and Mammalian remains together with palaeolithic flint implements, while the bedmarked h in my original sectk>D?# and which, after descending the h
On the Evidences of a Submergence of Western Europe, and of the Mediterranean Coasts, at the Close of the Glacial or So-Called Post-Glacial Period, and Immediately Preceding the Neolithic or Recent Period . shells * In some instances streams may have preceded these later gravel trails. f The specimen is in the Boulogne Museum, J See section in .Quart, Journ. Geo], Hoc, vol. 48, Plate 7, fig. 1, OF WESTERN EUROPE AND THE MEDITERRANEAN COASTS. 911 and Mammalian remains together with palaeolithic flint implements, while the bedmarked h in my original sectk>D?# and which, after descending the hill slope, passesbeneath the alluvium in the valley, represents the rubble-drift such as is met withon slopes. Since that section wras taken another (fig. 4) very illustrative section, correspondingin its main features with the head on the Channel coast, was for a short time to beseen in a road-cutting in the suburb of Mercade, north of Abbeville. This sectionshowed the same remarkable reversal of the out-cropping edges of the beds, soconspicuous at Brighton and Portland, with additional features of some importance. Fig, 4.—Section of Bubble-Drift on the slope of the Mil to the north of Abbeville,. v* ?????bHHBMHnM*. ^JBB
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Keywords: ., bookaut, bookcentury1800, bookdecade1890, bookidphiltrans04021987
