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Boulder Place Directory 04
Page 05
For the last half of the reign of Henry II we have the advantage of a valuable and in some respects very interesting and attractive chronicle. This is the Gesta Regis Henrici Secundi, associated with the name of BENEDICT OF PETERBOROUGH (Rolls Series, 2 vols.). Benedict, however, was not the author, and no certain evidence as to who he was can be derived from any source, nor does the chronicle itself supply many of those incidental indications from which it is often possible to learn much regarding the author of an anonymous book. The tentative suggestion of Bishop Stubbs that it may have been written by Richard Fitz Neal, the author of the Dialogus de Scaccario, is now generally regarded as inadmissible. The work begins in 1170, and from a date a year or two later is evidently contemporaneous to its close in 1192, with perhaps a slight interruption at 1177. It is written in a simple and straightforward way, and with a sure touch, unusual accuracy of statement, and a clear understanding of constitutional details; it suggests an interesting personality in its author, with whom we constantly desire a closer acquaintance. Whoever he was, he possessed good sources of information, though apparently too great consideration for king or court keeps him sometimes from saying all he knows or believes, and he has inserted in his work many letters and important documents.
Besides the albumin, the gluten, and the starch, other substances about which this rough method of analysis gives us no information, are contained in the wheat grain. For example, there is woody matter or cellulose, and a certain quantity of sugar and fat. It would be possible to obtain a substance similar to albumin, starch, saccharine, and fatty matters, and cellulose, by treating the stem, leaves, and root in a similar fashion, but the cellulose would be in far larger proportion. Straw, in fact, which consists of the dry stem and leaves of the wheat plant, is almost wholly made up of cellulose. Besides this, however, it contains a certain proportion of mineral bodies, among them, pure flint or silica; and, if you should ever see a wheat rick burnt, you will find more or less of this silica, in a glassy condition, in the embers. In the living plant, all these bodies are combined with a large proportion of water, or are dissolved, or suspended in that fluid. The relative quantity of water is much greater in the stem and leaves than in the seed.
Sometimes, however, geology does not, on the face of it, come into the reckoning. Thus I might have asked the reader to assist at the digging out of a cave, say, one of the famous caves at Mentone, on the Italian Riviera, just beyond the south-eastern corner of France. These caves were inhabited by man during an immense stretch of time, and, as you dig down, you light upon one layer after another of his leavings. But note in such a case as this how easily you may be baffled by some one having upset the heap of clothes, or, in a word, by rearrangement. Thus the man whose leavings ought to form the layer half-way up may have seen fit to dig a deep hole in the cave-floor in order to bury a deceased friend, and with him, let us suppose, to bury also an assortment of articles likely to be useful in the life beyond the grave. Consequently an implement of one age will be found lying cheek by jowl with the implement of a much earlier age, or even, it may be, some feet below it. Thereupon the pre-historian must fall back on the general run, or type, in assigning the different implements each to its own stratum. Luckily, in the old days fashions tended to be rigid; so that for the pre-historian two flints with slightly different chipping may stand for separate ages of culture as clearly as do a Greek vase and a German beer-mug for the student of more recent times.
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