The story of the universe. Volume 3 (of 4) : $b The earth's garment : flora
History
The story of the universe. Volume 3 (of 4) : $b The earth's garment : flora
Astronomy; Earth (Planet); Natural history
From the western border of northern France, through Belgium, North
Germany, and Russia, almost to the eastern confines of Siberia,
extends a broad plain rarely interrupted by low chains of hills,
and just as rarely affording fitting soil for extensive growth of
wood, which, on the whole, confines itself to the more favorable
soil moistened by the vicinity of rivers. Along the southern border
of this plain extends a chain of hills and mountains, now projecting
forward like capes into the broad surface, now retreating into
broad or narrow creeks, the coast of a sea formerly covering the
whole plain. Over all this endless expanse has one single species
of plant established an almost exclusive predominance, the heath,
which has lent its name to those tracts of land. Conditions similar
to those which produce the distinction between the pine barrens
and cypress swamps in North America are also active here to cause
an essential difference. The great flatness of the ground, even
geological conditions in many places, as where slight elevations of
the land forming flat inclosed basins, prevent, in many situations,
the free discharge of water, and the heath, backed by the special
vegetation produced by the moisture, forms by the annual accumulation
of vegetable matter, which in water only becomes to a certain degree
carbonized or decomposed, those black masses of the remains of
plants which as peat bear such an important part in the economy of
the inhabitants. Thus, in various modes of distribution, alternate
arid, dry sandy heaths with moist, spongy peat heaths or moors.
On the margin of the latter, more rarely actually upon them, and
on the heaths of Luneburg are often found splendid oaks, which,
overshadowing one of those pleasant straw-thatched houses and thrown
out by the background of the peculiar red tint of the glancing
heather, produce a picturesque charm which would not have been
expected here. With these great moors may be associated the peat
moors of some of the higher mountain chains of the Brocken, the Röhn,
and the Fichtel-Gebirge, and so on, and the so-called mosses of South
Germany and Switzerland.
Public-domain text, read in full here on John Shaqi.
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