Two streams of analogous nature, though less marked in their
characteristics, are the Elbe and the Weser. But these both rise, not
among the Alps, but amid the German mountains. They lack, therefore, the
exceedingly romantic character of Alpine rivers; but they do not lack in
picturesque scenery, and this they owe to the obstacles which they pass.
The Elbe has broken its way from the Bohemian ridge through the so-called
Saxon-Switzerland, as far as Meissen, and the Weser from the fissures of
the Werra and the Fulda to the Porta Westphalica. The Elbe and the Weser
make, with the Rhine, the triad of Central European rivers, which have
broken a pathway for themselves through mountains which impeded their
course.
A third class of rivers are those which encounter no obstacles, and flow
in a placid stream from the source to the mouth. They extend in Europe
from the Vistula to the Ems, including the Oder and excluding the Weser
and Elbe, and from the Rhine along the whole Atlantic coast of France,
embracing the Seine, Loire, Garonne, and the Adour—all of these having,
in greater or less degree, the same hydrographical character.
From these can be still further discriminated the subordinate coast
rivers.
To a fourth class belong all those tributary streams, of whatever size or
length, which agree in possessing no independent character, and do not
pour their waters into the sea through their own mouths.
The application of this system of classification can be applied to the
streams and their accompanying terrace lands in the other continents. But
these observations may suffice to indicate the general principles which
we would apply to the study of rivers, and leave to the student their
further application.
Review.
The great typical forms already considered, highland, plateau, mountain,
lowland, terrace, and river, which all claim so large a share of
attention in studying their physical characteristics, are no less worthy
of careful attention, in consequence of their influence on human culture.
Our account would not be complete without devoting a few pages to the
consideration of the manner in which nature and history have reacted on
each other.
Public-domain text, read in full here on John Shaqi.
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