Physical science in the time of Nero : $b being a translation of the Quaestiones naturales of SenecaSeneca, Lucius Annaeus
Philosophy
Physical science in the time of Nero : $b being a translation of the Quaestiones naturales of Seneca
Seneca, Lucius Annaeus
Comets; Earthquakes; Meteorology -- Early works to 1800
Posidonius will have it that there are two different varieties in the
movements of the earth, each with its distinctive name. The one is a
quaking when the earth is shaken and moves up and down; the other is
a tilting when, like a ship, it leans over to one or other side. I
am of opinion that there is still a third variety, which we have a 3
special term to denote. Our forefathers had good reason for speaking of
a trembling of the earth, for it is unlike either of the other kinds
of movement. On such an occasion things are neither all shaken nor
all tilted, but they quiver. In a case of this kind no great damage
is usually done; while, on the other hand, a tilting is far more
destructive than a shock; for unless a contrary movement set in very
quickly from the other side to restore the level, downfall follows of
necessity.
XXII
These movements being dissimilar, their causes are likewise 1
different. Let us deal first with the shaking movement. If great loads
are being conveyed by a row of many waggons, and the wheels, under
the unusual strain, fall into the ruts of the road, one feels the
earth shaken. Asclepiodotus has put it on record that on one occasion
the fall of a rock that was torn off from the mountain-side caused by
the tremor the collapse of some houses in its vicinity. Just the same
thing may occur beneath the earth; parts of the overhanging crags may
be loosened and fall with great weight and noise upon the floor of the
cavern beneath, and with a violence proportionate to the weight of the
mass and the height of the fall. The whole roof of the subterranean
valley is disturbed by an occurrence of this kind. It is conceivable,
too, that rocks are not always wrenched off by their own weight; 2
when rivers roll over them, the constant moisture weakens the joints
of the stone, and day by day bears away part of its fastening, causing
abrasion, so to speak, of the skin in which the stone is enclosed.
The long waste of ages, through constant daily rubbing, by and by so
weakens the fastenings that they cease to be able to sustain their
burden. Then blocks of vast size fall down, then the crag hurled 3
headlong will not suffer anything to stand that it strikes in the
rebound from its fall, but
Comes away with a roar; and all things seem suddenly to rush headlong,
as our countryman Virgil says. Such must be the cause of the earthquake
that shakes the ground beneath. Now I must pass on to the second kind.
XXIII
Public-domain text, read in full here on John Shaqi.
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