The Works of Robert Louis Stevenson - Swanston Edition, Vol. 22: Juvenilia and Other PapersStevenson, Robert Louis
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The Works of Robert Louis Stevenson - Swanston Edition, Vol. 22: Juvenilia and Other Papers
Stevenson, Robert Louis
English literature -- 19th century
The question is probably considered too simply--too much to the neglect
of concurrent influences. Until we know, for example, somewhat more of
the comparative radiant powers of different soils, we cannot expect any
very definite result. A change of temperature would certainly be
effected by the plantation of such a marshy district as the Sologne,
because, if nothing else were done, the roots might pierce the
impenetrable subsoil, allow the surface-water to drain itself off, and
thus dry the country. But might not the change be quite different if the
soil planted were a shifting sand, which, _fixed_ by the roots of the
trees, would become gradually covered with a vegetable earth, and be
thus changed from dry to wet? Again, the complication and conflict of
effects arises, not only from the soil, vegetation, and geographical
position of the place of the experiment itself, but from the
distribution of similar or different conditions in its immediate
neighbourhood, and probably to great distances on every side. A forest,
for example, as we know from Herr Rivoli's comparison, would exercise a
perfectly different influence in a cold country subject to warm winds,
and in a warm country subject to cold winds; so that our question might
meet with different solutions even on the east and west coasts of Great
Britain.
The consideration of such a complexity points more and more to the
plantation of Malta as an occasion of special importance; its insular
position and the unity of its geological structure both tend to simplify
the question. There are certain points about the existing climate,
moreover, which seem specially calculated to throw the influence of
woods into a strong relief. Thus, during four summer months, there is
practically no rainfall. Thus, again, the northerly winds when stormy,
and especially in winter, tend to depress the temperature very suddenly;
and thus, too, the southerly and south-westerly winds, which raise the
temperature during their prevalence to from eighty-eight to ninety-eight
degrees, seldom last longer than a few hours; insomuch that "their
disagreeable heat and dryness may be escaped by carefully closing the
windows and doors of apartments at their onset."[58] Such sudden and
short variations seem just what is wanted to accentuate the differences
in question. Accordingly, the opportunity seems one not lightly to be
lost, and the British Association or this Society itself might take the
matter up and establish a series of observations, to be continued during
the next few years. Such a combination of favourable circumstances may
not occur again for years; and when the whole subject is at a standstill
for want of facts, the present occasion ought not to go past unimproved.
Such observations might include the following:--
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