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
After mentioning and dismissing a grotesque suggestion of Diogenes
of Apollonia, Seneca suddenly drops the discussion of the Nile and
passes on to the subject of hail. It is obvious that there is here a
serious gap in the text. It is not probable that he meant to leave off
his examination into the probable sources of the Nile without stating
his own view of a matter which had been so long the subject of wonder
and debate. Either, therefore, he never completed this section of his
treatise, or a portion of the work has been lost.
The remainder of Book IV. is taken up with a desultory discussion of
the subjects of hail and snow, written when the author must have been
in a somewhat frivolous mood. He begins by telling Lucilius that if
he were to assert that hail is produced as ice is with us, a whole
cloud being frozen, he would be rather audacious. So he will imitate
the chroniclers, who after they have told a great many lies, refuse
to be responsible for some one statement, and refer for its truth
to the authorities. If, therefore, his friend doubts his word, he
will call in Posidonius, who will tell him that hail is formed from a
watery cloud just turned into liquid. No teacher is needed to explain
why pellets of hail are round, for all drops take that shape. Hail is
nothing else than suspended ice, and snow is suspended hoar-frost.
In this light vein Seneca thinks he has finished the subject and
might dismiss it, but he cannot resist the temptation to continue the
persiflage a little further. He quotes in a bantering style some of the
opinions of his brother Stoics, and after this long preamble begins
an inquiry into the distribution of density and temperature in the
atmosphere.
It would have been interesting had he seriously and fully stated what
was known or surmised on this last topic, but he dismisses it in three
short chapters. We learn from these that he regarded the air to be
densest next the earth, and that as all things retain heat better
the denser and more compact they are, so the air becomes less warm
in proportion to its height (184).[116] The opinion of some persons,
that the air on mountain summits ought to be warmer because they are
nearer the sun, is sagaciously controverted, and the insignificance
of all inequalities on the surface of the earth in comparison with
the distance from the earth to the sun is forcibly expressed and
illustrated.
[116] This view hardly agrees with what is expressed in Book II. (60,
61), but it more accurately expresses the fact.
The subject of snow and hail is briefly reintroduced at the end of the
Book, probably for the purpose of affording a convenient introduction
to the invective against luxury which fills the concluding chapter. The
preservation of snow in ice-houses, and its use in the reparation of
jaded appetites by cooling drinks, calls forth a denunciation of the
young rakes of his day, which closes the discussion.
BOOK V
Public-domain text, read in full here on John Shaqi.
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