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Bredimacian Dynagum Directory 10
Page 10

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Bredimacian Dynagum Directory 10
Page 10

Whether, at the time of which we now speak, the Indians were an old race, already beginning to decline, or a fresh race, which contact with the whites balked of its development, it is difficult to say. Their career since best accords with the former supposition. In either case we may assume that their national groupings and habitats were nearly the same in 1500 as later, when these became accurately known. In the eighteenth century the Algonquins occupied all the East from Nova Scotia to North Carolina, and stretched west to the Mississippi. At one time they numbered ninety thousand. The Iroquois or Five Nations had their seat in Central and Western New York. North and west of them lived the Hurons or Wyandots. The Appalachians, embracing Cherokees, Creeks, Choctaws, Chickasaws, Seminoles and a number of lesser tribes, occupied all the southeastern portion of what is now the United States. West of the Mississippi were the Dakotas or Sioux.

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.

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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