The Knickerbocker, Vol. 10, No. 6, December 1837Various
History
The Knickerbocker, Vol. 10, No. 6, December 1837
Various
Periodicals
Such has been the train of thought suggested to the mind of the
writer of this article, by an examination of the nature and physical
relations of COLOR. This property of matter might appear to a
superficial observer as one of inferior importance. He would admit
that the differences of color add to the happiness of the human race,
inasmuch as they give variety and beauty to material objects, and
afford one of the most easy methods of distinguishing them from each
other, but would probably deny that the existence of animal life
is at all dependant upon color, and that it is essential to the
present constitution of things. But let such an one reflect a little
more upon this property--let him consider attentively all its
relations--and he will doubtless change his opinion.
In travelling from the equator toward the poles, we cannot but
be struck with the fact, that there exists a difference of color
corresponding to a change of climate. Under the equator, the covering
of the earth, that is, the vegetation, is darker than in any other
part of the globe; and, as there is but little change of climate
through the year, this dark covering does not give place either
to the light tints of autumn, or to the snowy robe of winter. In
advancing north, the foliage becomes lighter in proportion to the
increase of latitude. In the temperate zone, the dark, rich robe of
the tropics gives place to one of livelier hue, which, after covering
the earth during a part of the year, assumes the light colors of
decay, and is buried beneath the snow. Thus this change continues
to keep pace with the diminution of temperature, till we enter the
frigid zone, and reach the region of eternal frost.
From this difference of color in the north and south, and in summer
and winter, we may deduce this general fact, that the earth adapts
itself in color to the variations of temperature, presenting a dark
surface to the heat of summer and the tropics, and a light one to the
cold of winter and the frigid zone.
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