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
The destroying agency of the flood came within two hundred yards of the
precipice on which the beautiful temple of Vesta stands; but fortunately
this precious relic of antiquity was spared, while the wreck of modern
structures was hurled down the abyss. Vesta, it will be remembered, in
the heathen mythology, personified the stability of the earth; and when
the Samian astronomer, Aristarchus, first taught that the earth revolved
on its axis, and round the sun, he was publicly accused of impiety, "for
removing the everlasting Vesta from her place." Playfair observed, that
when Hutton ascribed instability to the earth's surface, and represented
the continents which we inhabit as the theatre of incessant change and
movement, his antagonists, who regarded them as unalterable, assailed
him in a similar manner with accusations founded on religious
prejudices.[280] We might appeal to the excavating power of the Anio as
corroborative of one of the most controverted parts of the Huttonian
theory; and if the days of omens had not gone by, the geologists who now
worship Vesta might regard the late catastrophe as portentous. We may,
at least, recommend the modern votaries of the goddess to lose no time
in making a pilgrimage to her shrine, for the next flood may not respect
the temple.
_Excavation of rocks by running water._--The rapidity with which even
the smallest streams hollow out deep channels in soft and destructible
soils is remarkably exemplified in volcanic countries, where the sand
and half-consolidated tuffs opposed but a slight resistance to the
torrents which descend the mountain-side. After the heavy rains which
followed the eruption of Vesuvius in 1824, the water flowing from the
Atrio del Cavallo cut, in three days, a new chasm through strata of tuff
and ejected volcanic matter, to the depth of twenty-five feet. I found
the old mule-road, in 1828, intersected by this new ravine.
The gradual erosion of deep chasms through some of the hardest rocks, by
the constant passage of running water, charged with foreign matter, is
another phenomenon of which striking examples may be adduced.
Illustrations of this excavating power are presented by many valleys in
central France where the channels of rivers have been barred up by solid
currents of lava, through which the streams have re-excavated a passage,
to the depth of from twenty to seventy feet and upwards, and often of
great width. In these cases there are decisive proofs that neither the
sea, nor any denuding wave or extraordinary body of water, has passed
over the spot since the melted lava was consolidated. Every hypothesis
of the intervention of sudden and violent agency is entirely excluded,
because the cones of _loose_ scoriæ, out of which the lavas flowed, are
oftentimes at no great elevation above the rivers, and have remained
undisturbed during the whole period which has been sufficient for the
hollowing out of such enormous ravines.
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