The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
History
The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
Astronomy; Earth (Planet); Natural history
The air above the peat-mosses of Ireland and other countries in
the world is not often unhealthy, either because the heat is not
sufficient to develop miasma, or else because the vegetation, by
absorbing the water into its spongy mass, impedes the corruption of
the liquid, and produces a considerable quantity of oxygen. Further
south, the peat-mosses, which are intermixed with pools of stagnant
water, and especially marshes properly so-called, generate an impure
air, which spreads fever and death over the surrounding country.
Unless marshes are surrounded with dense forests, which arrest
the dispersion of the gases, the latter exercise a most injurious
influence on the general salubrity of the district; for during dry
weather, a vast area of the bed of the marshes becomes exposed, and
the heaps of organic débris lying on the bottom decompose in the heat
and infect the whole atmosphere. The average of life is much shorter
in all marshy countries than in the adjacent regions which are
invigorated by running water. In Brescia, Poland, in the marshes of
Tuscany, and in the Roman plains, the wan and livid complexion of the
inhabitants, their hollow eyes, and their feverish skin, announce at
first sight the vicinity of some centre of infection. There are some
marshes in the torrid zone where the decomposition of organic remains
goes on with a much greater rapidity than in temperate climates; no
one can venture on the edges of these districts without peril to his
life. As Frœbel ascertained in his journey across Central America,
the miasma is occasionally produced in such abundance that not only
can it be smelt, but a distinct impression of it is left upon the
palate.
LOWLAND PLAINS
--WILLIAM HUGHES
The plateaus and mountain regions of the globe occupy a large
portion of its surface--perhaps more than half of the whole extent
of the land--and their influence over its climate and other natural
conditions affecting mankind is very great. The highlands of the Old
World--fitted by their physical attributes to be the home of pastoral
and nomad races--were among the regions earliest occupied by mankind.
From the banks of the Euphrates and the primeval cities of the
Assyrian plain, the course of the shepherd-warrior--whether directed
to the east or the west--led toward some of the elevated regions
which stretched thence within the same (or nearly the same) degrees
of latitude, and which, at least in a general sense, are under like
conditions of climate. The highlands of Persia and Afghanistan,
in the one direction, of Syria and the Lesser Asia, in the other,
display abundant evidence, both in traditional and monumental
records, of their early occupation by man. From the one, the natural
order of advance leads to the fertile plains of India; from the
other, to the shores of the Mediterranean, whence is easy transit to
the peninsula and islands that lie beyond.
Public-domain text, read in full here on John Shaqi.
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