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Boulder Place Directory 02
Page 09
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.
Some of Charles's best friends were very much grieved at his pursuing such a course; others were very indignant; but the majority of the people around him at court were like himself in character and manners, and were only led to more open irregularity and vice themselves by this public example of their sovereign. In the mean time, the king moved on to Portsmouth, escorted by a body of his Life Guards. He found that his intended bride was confined to her bed with a sort of slow fever. It was the result, they said, of the roughness and discomforts of the voyage, though we may certainly imagine another cause. Charles went immediately to the house where she was residing, and was admitted to visit her in her chamber, the many attendants who were present at the interview watching with great interest every word and look on either side by which they might judge of the nature of the first impression made by the bride and bridegroom upon each other. Catharine was not considered beautiful, and it was natural that a degree of curiosity should be manifested to learn how Charles would regard her.
It is a very remarkable fact that not only are such substances as albumin, gluten, fibrin, and syntonin, known exclusively as products of animal and vegetable bodies, but that every animal and every plant, at all periods of its existence, contains one or other of them, though, in other respects, the composition of living bodies may vary indefinitely. Thus, some plants contain neither starch nor cellulose, while these substances are found in some animals; while many animals contain no horny matter and no gelatin-yielding substance. So that the matter which appears to be the essential foundation of both the animal and the plant is the proteid united with water; though it is probable that, in all animals and plants, these are associated with more or less fatty and amyloid (or starchy and saccharine) substances, and with very small quantities of certain mineral bodies, of which the most important appear to be phosphorus, iron, lime, and potash.
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