The Power That Preserves | My Web Site Page 309 Chapter 01 Page 06

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Many disturbances occurred during Edward's reign in different parts of the country, especially on the Welsh border. At the Christmas meeting of the King and his Wise Men, at Gloucester, in 1053, it was ordered that Rhys, the brother of Gruffydd, the South Welsh king, be put to death for his great plunder and mischief. The same year, the great Earl Godwine, while dining with the king at Winchester at the Easter feast, suddenly fell in a fit, died four days after, and was buried in the old cathedral. A few years later (1065), the Northumbrians complained that Earl Tostig, Harold's brother, had caused Gospatric, one of the chief Thanes, to be treacherously murdered when he came to the King's court the Christmas before. King Edward kept his last Christmas (1065), and had the meeting of his Wise Men in London instead of Gloucester as usual. His great object was to finish his new church at Westminster, and to have it hallowed before he died. He lived just long enough to have this done. On Innocent's Day the new Minster was consecrated, but the King was too ill to be there, so the Lady Edith stood in his stead.

It was rather interesting to note that the formation of the right bank was exactly the same as that of the Paredao Grande we had seen in Matto Grosso. Vertical sides in great rectangles were noticeable, intersected by passages--regular canons--where small huts could be seen at the foot of the picturesque rocks, especially at places where small streamlets entered the Tapajoz. I was told that little lakes had formed beyond those frontal rocky masses, the entrances to which were blocked at low water by sand-bars. Beyond that row of vertical red rocks was a more or less confused mass of hills, some dome-like, others of a more elongated form, but still with a well-rounded sky-line. The water of the stream had now changed colour altogether, and had become of a deep green. Islets could be seen far, far away to the left side of the river, mere white dots and lines along the water-line, most of them having white sand-beaches around them; while on the right bank the great red walls in sections continued for many miles. As we neared the mouth of the Tapajoz, the river had the immense width of 14 kil. On the right, after going through the Passagem dos Surucue, we passed the mountain of Jaguarary, which stood prominent along a flat elevation on the right bank.

The Peridineae of the warmer ocean layers have thus become long-rayed, those of the colder layers short-rayed, not through the direct effect of friction on the protoplasm, but through processes of selection, which favoured the longer rays in warm water, since they kept the organism afloat, while those with short rays sank and were eliminated. If we put the question as to selection-value in this case, and ask how great the variations in the length of processes must be in order to possess selection-value; what can we answer except that these variations must have been minimal, and yet sufficient to prevent too rapid sinking and consequent elimination? Yet this very case would give the ideal opportunity for a mathematical calculation of the minimal selection-value, although of course it is not feasible from lack of data to carry out the actual calculation. But even in organisms of more than microscopic size there must frequently be minute, even microscopic differences which set going the process of selection, and regulate its progress to the highest possible perfection.

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