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Zaproburno Yollanica Directory 04
Page 05
Queen Henrietta is said to have laid her arrangements in train for opening the negotiation with the Portuguese princess, at a visit which she made to England in 1660, very soon after her son's restoration. The Restoration took place in May. The queen's visit to her son was in October. Of course, after all the long years of danger, privation, and suffering which this family had endured, the widowed mother felt an intense emotion of joy at finding her children once more restored to what she considered their just hereditary rights. Charles was on the English throne. James, the Duke of York, was Lord High Admiral of England, that is, the commander-in-chief of the naval forces of the realm; and her other children, those who were still living, were in peace and safety. Of course, her heart was full of maternal pride and joy.
The night passed on, and though the king's mind was relieved, he suffered much bodily agony. In the morning, when he perceived that it was light, he asked the attendants to open the curtains, that he might see the sun for the last time. It gave him but a momentary pleasure, for he was restless and in great suffering. Some pains which he endured increased so much that it was decided to bleed him. The operation relieved the suffering, but exhausted the sufferer's strength so that he soon lost the power of speech, and lay afterward helpless and almost insensible, longing for the relief which now nothing but death could bring him. This continued till about noon, when he ceased to breathe.
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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