the formation of vegetable mould-第20章
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doubting whether I should live to see these larger flints covered
with vegetable mould and turf。 But the smaller stones disappeared
before many years had elapsed; as did every one of the larger ones
after a time; so that after thirty years (1871) a horse could
gallop over the compact turf from one end of the field to the
other; and not strike a single stone with his shoes。 To anyone who
remembered the appearance of the field in 1842; the transformation
was wonderful。 This was certainly the work of the worms; for
though castings were not frequent for several years; yet some were
thrown up month after month; and these gradually increased in
numbers as the pasture improved。 In the year 1871 a trench was dug
on the above slope; and the blades of grass were cut off close to
the roots; so that the thickness of the turf and of the vegetable
mould could be measured accurately。 The turf was rather less than
half an inch; and the mould; which did not contain any stones; 2。5
inches in thickness。 Beneath this lay coarse clayey earth full of
flints; like that in any of the neighbouring ploughed fields。 This
coarse earth easily fell apart from the overlying mould when a spit
was lifted up。 The average rate of accumulation of the mould
during the whole thirty years was only 。083 inch per year (i。e。;
nearly one inch in twelve years); but the rate must have been much
slower at first; and afterwards considerably quicker。
The transformation in the appearance of this field; which had been
effected beneath my eyes; was afterwards rendered the more
striking; when I examined in Knole Park a dense forest of lofty
beech…trees; beneath which nothing grew。 Here the ground was
thickly strewed with large naked stones; and worm…castings were
almost wholly absent。 Obscure lines and irregularities on the
surface indicated that the land had been cultivated some centuries
ago。 It is probable that a thick wood of young beech…trees sprung
up so quickly; that time enough was not allowed for worms to cover
up the stones with their castings; before the site became unfitted
for their existence。 Anyhow the contrast between the state of the
now miscalled 〃stony field;〃 well stocked with worms; and the
present state of the ground beneath the old beech…trees in Knole
Park; where worms appeared to be absent; was striking。
A narrow path running across part of my lawn was paved in 1843 with
small flagstones; set edgeways; but worms threw up many castings
and weeds grew thickly between them。 During several years the path
was weeded and swept; but ultimately the weeds and worms prevailed;
and the gardener ceased to sweep; merely mowing off the weeds; as
often as the lawn was mowed。 The path soon became almost covered
up; and after several years no trace of it was left。 On removing;
in 1877; the thin overlying layer of turf; the small flag…stones;
all in their proper places; were found covered by an inch of fine
mould。
Two recently published accounts of substances strewed on the
surface of pasture…land; having become buried through the action of
worms; may be here noticed。 The Rev。 H。 C。 Key had a ditch cut in
a field; over which coal…ashes had been spread; as it was believed;
eighteen years before; and on the clean…cut perpendicular sides of
the ditch; at a depth of at least seven inches; there could be
seen; for a length of 60 yards; 〃a distinct; very even; narrow line
of coal…ashes; mixed with small coal; perfectly parallel with the
top…sward。〃 {45} This parallelism and the length of the section
give interest to the case。 Secondly; Mr。 Dancer states {46} that
crushed bones had been thickly strewed over a field; and 〃some
years afterwards〃 these were found 〃several inches below the
surface; at a uniform depth。〃
The Rev。 Mr。 Zincke informs me that he has lately had an orchard
dug to the unusual depth of 4 feet。 The upper 18 inches consisted
of dark…coloured vegetable mould; and the next 18 inches of sandy
loam; containing in the lower part many rolled pieces of sandstone;
with some bits of brick and tile; probably of Roman origin; as
remains of this period have been found close by。 The sandy loam
rested on an indurated ferruginous pan of yellow clay; on the
surface of which two perfect celts were found。 If; as seems
probable; the celts were originally left on the surface of the
land; they have since been covered up with earth 3 feet in
thickness; all of which has probably passed through the bodies of
worms; excepting the stones which may have been scattered on the
surface at different times; together with manure or by other means。
It is difficult otherwise to understand the source of the 18 inches
of sandy loam; which differed from the overlying dark vegetable
mould; after both had been burnt; only in being of a brighter red
colour; and in not being quite so fine…grained。 But on this view
we must suppose that the carbon in vegetable mould; when it lies at
some little depth beneath the surface and does not continually
receive decaying vegetable matter from above; loses its dark colour
in the course of centuries; but whether this is probable I do not
know。
Worms appear to act in the same manner in New Zealand as in Europe;
for Professor J。 von Haast has described {47} a section near the
coast; consisting of mica…schist; 〃covered by 5 or 6 feet of loess;
above which about 12 inches of vegetable soil had accumulated。〃
Between the loess and the mould there was a layer from 3 to 6
inches in thickness; consisting of 〃cores; implements; flakes; and
chips; all manufactured from hard basaltic rock。〃 It is therefore
probable that the aborigines; at some former period; had left these
objects on the surface; and that they had afterwards been slowly
covered up by the castings of worms。
Farmers in England are well aware that objects of all kinds; left
on the surface of pasture…land; after a time disappear; or; as they
say; work themselves downwards。 How powdered lime; cinders; and
heavy stones; can work down; and at the same rate; through the
matted roots of a grass…covered surface; is a question which has
probably never occurred to them。 {48}
The Sinking of great Stones through the Action of Worms。When a
stone of large size and of irregular shape is left on the surface
of the ground; it rests; of course; on the more protuberant parts;
but worms soon fill up with their castings all the hollow spaces on
the lower side; for; as Hensen remarks; they like the shelter of
stones。 As soon as the hollows are filled up; the worms eject the
earth which they have swallowed beyond the circumference of the
stones; and thus the surface of the ground is raised all round the
stone。 As the burrows excavated directly beneath the stone after a
time collapse; the stone sinks a little。 {49} Hence it is; that
boulders which at some ancient period have rolled down from a rocky
mountain or cliff on to a meadow at its base; are always somewhat
imbedded in the soil; and; when removed; leave an exact impression
of their lower surfaces in the underlying fine mould。 If; however;
a boulder is of such huge dimensions; that the earth beneath is
kept dry; such earth will not be inhabited by worms; and the
boulder will not sink into the ground。
A lime…kiln formerly stood in a grass…field near Leith Hill Place
in Surrey; and was pulled down 35 years before my visit; all the
loose rubbish had been carted away; excepting three large stones of
quartzose sandstone; which it was thought might hereafter be of
some use。 An old workman remembered that they had been left on a
bare surface of broken bricks and mortar; close to the foundations
of the kiln; but the whole surrounding surface is now covered with
turf and mould。 The two largest of these stones had never since
been moved; nor could this easily have been done; as; when I had
them removed; it was the work of two men with levers。 One of these
stones; and not the largest; was 64 inches long; 17 inches broad;
and from 9 to 10 inches in thickness。 Its lower surface was
somewhat protuberant in the m