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Nicholeto Chordiman Directory 13
Page 02
With regard to the assuring of these friendly relations, the German Government believes that it may all the more reckon on a full understanding with the United States, as the procedure announced by the German Admiralty, which was fully explained in the note of the 4th inst., is in no way directed against legitimate commerce and legitimate shipping of neutrals, but represents solely a measure of self-defense, imposed on Germany by her vital interests, against England's method of warfare, which is contrary to international law, and which so far no protest by neutrals has succeeded in bringing back to the generally recognized principles of law as existing before the outbreak of war.
The vast subject which I have thus lightly skimmed is not without interest, again, from its human implications. Savages as a rule produce enormous families; but then, the infant mortality in savage tribes is proportionally great. Among civilized races, families are smaller, and deaths in infancy are far less numerous. The higher the class or the natural grade of a stock, the larger as a rule the proportion of children safely reared to the adult age. The goal towards which humanity is slowly moving would thus seem to be one where families in most cases will be relatively small--perhaps not more on an average than three to a household--but where most or all of the children brought into the world will be safely reared to full maturity. This is already becoming the rule in certain favored ranks of European society.
Briefly, then, the geologist assures us that when the cold of the Glacial Age was at its maximum glaciers streamed down from all the mountains of Scotland, Wales, and Northern England; that the ice was thick enough to overtop all the smaller hills, and on the plains it united in one great sea of ice some thousands of feet in thickness, that it stretched as far south as the latitude of London, England. But that to the west the ice streamed out across, the Irish Sea, the islands to the west of Scotland, and ended far out into what is now the Atlantic.<23> But these glaciers, vast as they were, were very small compared with the glaciers that streamed out from the mountains of Norway and Sweden. These great glaciers invaded England to the southwest, beat back the glacier ice of Scotland from the floor of the North Sea, overran Denmark, and spread their mantle of bowlder clay far south into Germany.
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