The Formation of Vegetable Mould Through the Action of Worms: With Observations on Their HabitsDarwin, Charles
Science
The Formation of Vegetable Mould Through the Action of Worms: With Observations on Their Habits
Darwin, Charles
Earthworms; Humification; Soils
_Ancient encampments and tumuli_.—É. de Beaumont adduces the present
state of many ancient encampments and tumuli and of old ploughed fields,
as evidence that the surface of the land undergoes hardly any
degradation. But it does not appear that he ever examined the thickness
of the mould over different parts of such old remains. He relies chiefly
on indirect, but apparently trustworthy, evidence that the slopes of the
old embankments are the same as they originally were; and it is obvious
that he could know nothing about their original heights. In Knole Park a
mound had been thrown up behind the rifle-targets, which appeared to have
been formed of earth originally supported by square blocks of turf. The
sides sloped, as nearly as I could estimate them, at an angle of 45° or
50° with the horizon, and they were covered, especially on the northern
side, with long coarse grass, beneath which many worm-castings were
found. These had flowed bodily downwards, and others had rolled down as
pellets. Hence it is certain that as long as a mound of this kind is
tenanted by worms, its height will be continually lowered. The fine
earth which flows or rolls down the sides of such a mound accumulates at
its base in the form of a talus. A bed, even a very thin bed, of fine
earth is eminently favourable for worms; so that a greater number of
castings would tend to be ejected on a talus thus formed than elsewhere;
and these would be partially washed away by every heavy shower and be
spread over the adjoining level ground. The final result would be the
lowering of the whole mound, whilst the inclination of the sides would
not be greatly lessened. The same result would assuredly follow with
ancient embankments and tumuli; except where they had been formed of
gravel or of nearly pure sand, as such matter is unfavourable for worms.
Many old fortifications and tumuli are believed to be at least 2000 years
old; and we should bear in mind that in many places about one inch of
mould is brought to the surface in 5 years or two inches in 10 years.
Therefore in so long a period as 2000 years, a large amount of earth will
have been repeatedly brought to the surface on most old embankments and
tumuli, especially on the talus round their bases, and much of this earth
will have been washed completely away. We may therefore conclude that
all ancient mounds, when not formed of materials unfavourable to worms,
will have been somewhat lowered in the course of centuries, although
their inclinations may not have been greatly changed.
Public-domain text, read in full here on John Shaqi.
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