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He was sick, too, at the time, with an intermittent fever. The paroxysm returned once in three or four days, leaving him in tolerable health during the interval. He went first into the country of the Sabines, northeast of Rome, where he wandered up and down, exposed continually to great dangers from those who knew that he was an object of the great dictator's displeasure, and who were sure of favor and of a reward if they could carry his head to Sylla He had to change his quarters every day, and to resort to every possible mode of concealment. He was, however, at last discovered, and seized by a centurion. A centurion was a commander of a hundred men; his rank and his position therefore, corresponded somewhat with those of a _captain_ in a modern army. Caesar was not much disturbed at this accident. He offered the centurion a bribe sufficient to induce him to give up his prisoner, and so escaped.

The Orang cannot put its feet flat on the ground, but is supported upon their outer edges, the heel resting more on the ground, while the curved toes partly rest upon the ground by the upper side of their first joint, the two outermost toes of each foot completely resting on this surface. The hands are held in the opposite manner, their inner edges serving as the chief support. The fingers are then bent out in such a manner that their foremost joints, especially those of the two inner-most fingers, rest upon the ground by their upper sides, while the point of the free and straight thumb serves as an additional fulcrum.

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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