The Ontario Readers: The High School Reader, 1886Ontario. Department of Education
General
The Ontario Readers: The High School Reader, 1886
Ontario. Department of Education
Readers (Secondary)
Worms have played a more important part in the history of the world than
most persons would at first suppose. In almost all humid countries they
are extraordinarily numerous, and for their size possess great muscular
power. In many parts of England a weight of more than ten tons of dry
earth annually passes through their bodies and is brought to the surface
on each acre of land; so that the whole superficial bed of vegetable
mould passes through their bodies in the course of every few years. From
the collapsing of the old burrows the mould is in constant though slow
movement, and the particles composing it are thus rubbed together. By
these means fresh surfaces are continually exposed to the action of the
carbonic acid in the soil, and of the humus-acids which appear to be
still more efficient in the decomposition of rocks. The generation of
the humus-acids is probably hastened during the digestion of the many
half-decayed leaves which worms consume. Thus the particles of earth,
forming the superficial mould, are subjected to conditions eminently
favorable for their decomposition and disintegration. Moreover, the
particles of the softer rocks suffer some amount of mechanical
trituration in the muscular gizzards of worms, in which small stones
serve as mill-stones....
Archaeologists ought to be grateful to worms, as they protect and
preserve for an indefinitely long period every object, not liable to
decay, which is dropped on the surface of the land, by burying it
beneath their castings. Thus, also, many elegant and curious tesselated
pavements and other ancient remains have been preserved; though no doubt
the worms have in these cases been largely aided by earth washed and
blown from the adjoining land, especially when cultivated. The old
tesselated pavements have, however, often suffered by having subsided
unequally from being unequally undermined by the worms. Even old massive
walls may be undermined and subside; and no building is in this respect
safe, unless the foundations lie six or seven feet beneath the surface,
at a depth at which worms cannot work. It is probable that many
monoliths and some old walls have fallen down from having been
undermined by worms.
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