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Trumantia Resource Directory 11
Page 02
"That is very ungracious," I said. "You are as perverse as I was about Byron when the old banker quoted him with tears. I was going to say, and I will say it, that Tennyson, with all his faults, was a great lord of music; and he put into words the fine, homely domestic emotion of the race--the poetry of labour, order, and peace. It was new and rich and splendid, and because it seems to you old-fashioned, you call it mere respectability; but it was the marching music of the world, because he showed men that faith was enlarged and not overturned by science. These two were great, because they saw far and wide; they knew by instinct just what the ordinary man was thinking, who yet wished his life to be set to music. These little men of yours don't see that. They have their moments of ecstasy, as we all have, in the blossoming orchard full of the songs of birds. And that will always and for ever give us the lyric, if the skill is there. But I want something more than that; I, you, thousands of people, are feeling something that makes the brain thrill and the heart leap. The mischief is that we don't know what it is, and I want a great poet to come and tell us."
The AEquians in their numerous attacks upon the Roman territory generally occupied Mount Algidus, which formed a part of the group of the Alban Hills in Latium. It was accordingly upon this mount that the battles between the Romans and AEquians most frequently took place. In the year 458 B.C. the Roman consul L. Minucius was defeated on the Algidus, and surrounded in his camp. Five horsemen, who made their escape before the Romans were completely encompassed, brought the tidings to Rome. The Senate forthwith appointed L. Cincinnatus dictator.
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.
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