The Philosophy of Earthquakes, Natural and Religious: or, An Inquiry Into Their Cause, and Their PurposeStukeley, William
Religion
The Philosophy of Earthquakes, Natural and Religious: or, An Inquiry Into Their Cause, and Their Purpose
Stukeley, William
Earthquakes
I am not sensible of any real objection against our _hypothesis_, but
this, being the _eleventh_ of my positions, or circumstances. It seems
true, that earthquakes are more frequent in _Italy_, near _Vesuvius_,
and by _Ætna_, in _Sicily_. And the cause seems apparently owing to
these vulcano's. At first sight, every one would think so, but not from
the true reason. This has given the great prejudice to the judgments
of the curious, even at this day. But consider the matter impartially,
and it will appear, so far from being a strong argument in favour of
subterraneous eruptions, that it ought to be esteem'd a convincing proof
to the contrary, and most cogent in favour of my principle. In strictest
logic, there is no inference to be made from particulars to generals.
Quite the contrary. We have but these two or three vulcano's on one
quarter of the globe, and two of them toward the warmer climate of it;
whereas earthquakes are innumerable, especially in those of a warmer
clime. That there are no vulcano's, no discharges of fire and smoke for a
continuance, and abundance, after earthquakes; no suspicion of it either
from sight or smell, as we know by innumerable examples, as well as in
our own country, and experience: is demonstration, that this is not the
cause. If the vulcano's were the real cause of earthquakes, we ought
assuredly to expect, that in the countries thereabouts, the earthquakes
ought to be far more extensive than those in other countries, where are
no vulcano's; but this is altogether contrary to experience. For, as the
celebrated naturalist _Buffon_ observes, such are not extensive, as are
near _Ætna_ and _Vesuvius_. He further adds: _Histoire naturelle_, tom.
I. p. 508. speaking, among many others, of a _vulcano_ in the island of
_Ternate_, he remarks, "That this burning gulph is less agitated when
the air is calm, and the season mild, than in storms and hurricanes;"
and says, "This confirms what I have said in my foregoing discourse, and
seems evidently to prove, that the fire which makes _vulcano's_ comes not
from the bottom of mountains, but from the tops, or at least from a very
little depth; and that the hearth (or floor) of the fire is not far from
the summit of the _vulcano's_; for, if this was not the case, great winds
could not contribute to their conflagration." And this, in general, is a
corroborative proof of my whole hypothesis. For there can be no great fire
in the earth, where there is no great conveyance of air.
Public-domain text, read in full here on John Shaqi.
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