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Scientific American Supplement, No. 362, December 9, 1882 by Various
page 16 of 140 (11%)
blazing down on the glistening wilderness there is little sensation of
heat, for the cool lake breeze is ever blowing. On the landward side,
the insidious approach of the devouring sand is well marked. One hundred
and fifty feet below, the foot of this moving mountain is sharply
defined against the vivid green of the pastures, on which the grass
grows luxuriantly to within an inch of the sand wall. The ferns of the
cedar woods almost droop against the sandy slope. The roots of the trees
are bare along the white edge; a foot or two nearer the sand buries the
feet of the cedars: a few yards nearer still the bare trunks disappear;
still nearer only the withered topmast twigs of the submerged forest are
seen, and then far over the tree tops stands the sand range. Perpetual
ice is found under the foot of this steep slope, the sand covering and
consolidating the snows drifted over the hill during the winter months.
There is something awe-inspiring, says the correspondent of the Toronto
Globe, in the slow, quiet, but resistless advance of the mountain front.
Field and forest alike become completely submerged. Ten years ago a
farm-house was swallowed up, not to emerge in light until the huge sand
wave has passed over.

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