Cosmos: A Sketch of the Physical Description of the Universe, Vol. 1Humboldt, Alexander von
History
Cosmos: A Sketch of the Physical Description of the Universe, Vol. 1
Humboldt, Alexander von
Astronomy; Cosmography; Physical geography; Science -- History
But if we would correctly comprehend nature, we must not entirely or
absolutely separate the consideration of the present state of things from
that of the successive phases through which they have passed. We can not
form a just conception of their nature without looking back on the mode of
their formation. It is not organic matter alone that is continually
undergoing change, and being dissolved to form new combinations. The globe
itself reveals at every phase of its existence the mystery of its former
conditions.
We can not survey the crust of our planet without recognizing the traces of
the prior existence and destruction of an organic world. The sedimentary
rocks present a succession of organic forms, associated in groups, which
have successively displaced and succeeded each other. The different
super-imposed strata thus display to us the faunas and floras of different
epochs. In this sense the description of nature is intimately connected
with its history; and the geologist, who is guided by the connection
existing among the facts observed, can not form a conception of the present
without pursuing, through countless ages, the history of the past. In
tracing the physical delineation of the globe, we behold the present and the
past reciprocally incorporated, as it were, with one another; for the domain
of nature is like that of languages, in which etymological research reveals
a successive development, by showing us the primary condition of an idiom
reflected in the forms of speech in use at the present day. The study of
the material world renders this reflection of the past peculiarly manifest,
by displaying in the process of formation rocks of eruption and sedimentary
strata similar to those of former ages. If I may be allowed to borrow a
striking illustration from the geological relations by which the physiognomy
of a country is determined, I would say that domes of trachyte, cones of
basalt, lava streams ('coules')of amygdaloid with elongated and parallel
pores, and white deposits of pumice, intermixed with black scoriae, animate
the scenery by the associations of the past which they awaken, acting upon
the imagination of the enlightened observer like traditional records of an
earlier world. Their form is their history.
The sense in which the Greeks and Romans originally employed the word
'history' proves that they too were intimately convinced that, to form a
complete idea of the present state of the universe, it was necessary to
consider it in its successive
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phases. It is not, however, in the definition given by Valerius Flaccus,*
but in the zoological writings of Aristotle, that the word 'history'
presents itself as an exposition of the results of experience and
observation.
[Footnote] *Aul. Gell., 'Nect. Att.', v., 18.
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