Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 1 of 2]Weld, Isaac
History
Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 1 of 2]
Weld, Isaac
Canada -- Description and travel -- Early works to 1800; United States -- Description and travel -- Early works to 1800
The Blue Ridge, on each side of the Patowmac, is formed, from the
foundation to the summit, of large rocks deposited in beds of rich soft
earth. This earth is very readily washed away, and in that case the
rocks consequently become loose; indeed, they are frequently loosened
even by heavy showers of rain. A proof of this came within my own
observation, which I shall never forget. It had been raining excessively
hard the whole morning of that day on which I arrived at this place; the
evening however was very fine, and being anxious to behold the scene in
every point of view, I crossed the river, and attended the mountain at a
steep part on the opposite side, where there was no path, and many large
projecting rocks. I had walked up about fifty yards, when a large stone
that I set my foot upon, and which appeared to me perfectly firm, all at
once gave way; it had been loosened by the rain, and brought down such a
heap of others with it in its fall, with such a tremendous noise at the
same time, that I thought the whole mountain was coming upon me, and
expected every moment to be dashed to pieces. I slid down about twenty
feet, and then luckily caught hold of the branch of a tree, by which I
clung; but the stones still continued to roll down heap after heap;
several times, likewise, after all had been still for a minute or two,
they again began to fall with increased violence. In this state of
suspense I was kept for a considerable time, not knowing but that some
stone larger than the rest might give way, and carry down with it even
the tree by which I held. Unacquainted also with the paths of the
mountain, there seemed to me to be no other way of getting down,
excepting over the fallen stones, a way which I contemplated with
horror. Night however was coming on very fast; it was absolutely
necessary to quit the situation I was in, and fortunately I got to the
bottom without receiving any further injury than two or three slight
contusions on my hips and elbows. The people congratulated me when I
came back on my escape, and informed me, that the stones very commonly
gave way in this manner after heavy falls of rain; but on the
dissolution of a large body of snow, immense rocks, they said, would
sometimes roll down with a crash that might be heard for miles. The
consequences then of a large rock towards the bottom of the mountain
being undermined by a flood, and giving way, may be very readily
imagined: the rock above it, robbed of its support, would also fall;
this would bring down with it numbers of others with which it was
connected, and thus a disruption would be produced from the base to the
very summit of the mountain.
[Sidenote: IRON.]
Public-domain text, read in full here on John Shaqi.
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