Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
Two dry seasons in the White Mountains, in New Hampshire (United
States), were followed by heavy rains on the 28th August, 1826, when
from the steep and lofty declivities which rise abruptly on both sides
of the river Saco, innumerable rocks and stones, many of sufficient size
to fill a common apartment, were detached, and in their descent swept
down before them, in one promiscuous and frightful ruin, forests,
shrubs, and the earth which sustained them. Although there are numerous
indications on the steep sides of these hills of former slides of the
same kind, yet no tradition had been handed down of any similar
catastrophe within the memory of man, and the growth of the forest on
the very spots now devastated, clearly showed that for a long interval
nothing similar had occurred. One of these moving masses was afterwards
found to have slid three miles, with an average breadth of a quarter of
a mile. The natural excavations commenced generally in a trench a few
yards in depth and a few rods in width, and descended the mountains,
widening and deepening till they became vast chasms. At the base of
these hollow ravines was seen a confused mass of ruins, consisting of
transported earth, gravel, rocks, and trees. Forests of spruce-fir and
hemlock, a kind of fir somewhat resembling our yew in foliage, were
prostrated with as much ease as if they had been fields of grain; for,
where they disputed the ground, the torrent of mud and rock accumulated
behind, till it gathered sufficient force to burst the temporary
barrier.
The valleys of the Amonoosuck and Saco presented, for many miles, an
uninterrupted scene of desolation; all the bridges being carried away,
as well as those over their tributary streams. In some places, the road
was excavated to the depth of from fifteen to twenty feet; in others, it
was covered with earth, rocks, and trees, to as great a height. The
water flowed for many weeks after the flood, as densely charged with
earth as it could be without being changed into mud, and marks were seen
in various localities of its having risen on either side of the valley
to more than twenty-five feet above its ordinary level. Many sheep and
cattle were swept away, and the Willey family, nine in number, who in
alarm had deserted their house, were destroyed on the banks of the Saco;
seven of their mangled bodies were afterwards found near the river,
buried beneath drift-wood and mountain ruins.[273] Eleven years after
the event, the deep channels worn by the avalanches of mud and stone,
and the immense heaps of boulders and blocks of granite in the river
channel, still formed, says Professor Hubbard, a picturesque feature in
the scenery.[274]
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