Scientific American Supplement, No. 841, February 13, 1892 eBook

This eBook from the Gutenberg Project consists of approximately 155 pages of information about Scientific American Supplement, No. 841, February 13, 1892.

Scientific American Supplement, No. 841, February 13, 1892 eBook

This eBook from the Gutenberg Project consists of approximately 155 pages of information about Scientific American Supplement, No. 841, February 13, 1892.

In my view from the mounds and their surroundings I would unhesitatingly say the water, the foot hills of the glacier and the swamps left in its wake were but a short distance to the north of them, and during the summer months the melting ice would send a volume of water down this valley that the Missouri River of to-day is but a miniature of, and therefore the highest hills were the only land that could be used by that ancient race.

In this connection I would make the following suggestions that may lead to more important disclosures:  My object is the hope of a more thorough investigation at some future time.  Nearer to the top of the mound was found, certainly, the remains of a people of more recent date than those found in the vault, as their bones were larger, which would indicate a more stalwart tribe, and also their mode of burial was different, as there was no indication of fire being used, as was the case with the lower burials.  I would pronounce the upper interments those of Indians of the present day; the tools found with these were weapons of the chase.  On the other hand, those found in the vault were of a peaceful character, and their surroundings would readily comport, in my opinion, to the glacial period.  The entire absence of flint in the bottom of the mound would show one of two things, either they were unacquainted with the use of flint or at that time there was no flint to be had.  It is there now in great abundance, in such forms for cutting purposes that would render the “cotton rock” almost useless.  The flint is found in a hill close to the river bank, about half a mile from the mound, and the upper portion of the ledge has the appearance, to me, of glacial action and probably forms a moraine, as it has, evidently, been pushed over the underlying ledge, and been ground and splintered in a manner that could not have been without great crushing force.  It would be reasonable enough to suppose that the action of the river may have uncovered this flint by washing away the softer material since the occupation of the older race.

In relation to the Indian interment in the examined mound, I could not say distinctly whether the Indian burials had been such as to make them aware of former burials or not, but I think from the thickness of the clay between the two that they were ignorant of former burials.  The mounds of the modern Indian, so far as my investigations are concerned, would indicate a more rudely formed structure which would appear to be an imitation of the older mounds, as they are not finished with like care nor have they the ulterior structures.—­The Scientist.

* * * * *

ACTION OF CAUSTIC SODA ON WOOD.

By M.H.  TAUSS.

The researches of the author upon the action which water exerts upon wood at a high temperature have shown how much of the incrusting material can be removed without the aid of any reagent.

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Scientific American Supplement, No. 841, February 13, 1892 from Project Gutenberg. Public domain.