The Essays of Arthur Schopenhauer; Religion, a Dialogue, Etc.
Schopenhauer · en
To explain what I mean, let me compare the advance of knowledge among
mankind to the course taken by a planet. The false paths on which
humanity usually enters after every important advance are like the
epicycles in the Ptolemaic system, and after passing through one of
them, the world is just where it was before it entered it. But the great
minds, who really bring the race further on its course do not accompany
it on the epicycles it makes from time to time. This explains why
posthumous fame is often bought at the expense of contemporary praise,
and _vice versa_. An instance of such an epicycle is the philosophy
started by Fichte and Schelling, and crowned by Hegel's caricature of
it. This epicycle was a deviation from the limit to which philosophy had
been ultimately brought by Kant; and at that point I took it up again
afterwards, to carry it further. In the intervening period the sham
philosophers I have mentioned and some others went through their
epicycle, which had just come to an end; so that those who went with
them on their course are conscious of the fact that they are exactly at
the point from which they started.
This circumstance explains why it is that, every thirty years or so,
science, literature, and art, as expressed in the spirit of the time,
are declared bankrupt. The errors which appear from time to time amount
to such a height in that period that the mere weight of their absurdity
makes the fabric fall; whilst the opposition to them has been gathering
force at the same time. So an upset takes place, often followed by an
error in the opposite direction. To exhibit these movements in their
periodical return would be the true practical aim of the history of
literature: little attention, however, is paid to it. And besides, the
comparatively short duration of these periods makes it difficult to
collect the data of epochs long gone by, so that it is most convenient
to observe how the matter stands in one's own generation. An instance of
this tendency, drawn from physical science, is supplied in the Neptunian
geology of Werter.