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Bentarasko Benta Section 10
Page 09
Walking the other day in Cheapside I saw some turtles in Mr. Sweeting's window, and was tempted to stay and look at them. As I did so I was struck not more by the defences with which they were hedged about, than by the fatuousness of trying to hedge that in at all which, if hedged thoroughly, must die of its own defencefulness. The holes for the head and feet through which the turtle leaks out, as it were, on to the exterior world, and through which it again absorbs the exterior world into itself--"catching on" through them to things that are thus both turtle and not turtle at one and the same time--these holes stultify the armour, and show it to have been designed by a creature with more of faithfulness to a fixed idea, and hence one-sidedness, than of that quick sense of relative importances and their changes, which is the main factor of good living.
It is well known that the very earliest population of the Old Dominion was not of the highest, but predominantly idle and thriftless. Vagabonds and homeless children picked up in the streets of London, as well as some convicts, were sent to the colony from England to be indented as servants, permanently, or for a term of years. Persons of the better class, to be sure, came as well, and the quality of the population, on the whole, improved year by year. Settlement here followed a centrifugal tendency, except as this was repressed by fear of the Indians. In 1616 the departments of Virginia were Henrico, up the James above the Appomattox mouth, West and Shirley Hundreds, Jamestown, Kiquoton, and King's Gift on the coast near Cape Charles--a wide reach of territory to be covered by a total population of only three hundred and fifty.
It is in France that we find the greatest wealth of relics of Cave-men. Sir John Lubbock has left us a description of the valley of the Vezere, where these caverns occur. The Vezere is a small tributary of the Dordogne. "The rivers of the Dordogne run in deep valleys cut through calcareous strata: and while the sides of the valley in chalk districts are generally sloping, in this case, owing probably to the hardness of the rock, they are frequently vertical. Small caves and grottoes frequently occur: besides which, as the different strata possess unequal power of resistance against atmospheric influence, the face of the rock is, as it were, scooped out in many places, and thus 'rockshelters' are produced. In very ancient times these caves and rock-shelters were inhabited by men, who have left behind them abundant evidence of their presence.
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