A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables — John Shaqi
A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables
History
A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables
United States -- Biography; United States -- Description and travel; United States -- History
Valleys are formed by the separation of chains of mountains or
of hills. Those which are formed between high mountains, are
commonly narrow and long, as if they had originally been only
fissures dividing their respective chains, or for the passage
of extensive torrents. The angles of their direction sometimes
exhibit singular symmetry. In the Pyrenees there are said to
be valleys whose salient and re-entrant angles so perfectly
correspond, that if the force which separated them were to act
in a contrary direction, and bring their sides together again,
they would unite so exactly that even the fissure would not be
perceived. There are some highly situated valleys containing
rivers and lakes which have no outlets or streams. Most high
valleys have their surface upon a level with the summits of the
secondary mountains in the neighborhood. The lower valleys widen
as they recede from the secondary mountains from which they
originate, and gradually lose themselves in the plains. Their
opposite angles correspond regularly, but are very obtuse.
The sort of narrow passage by which we enter into these high
valleys is called a pass or defile. Between Norway and Sweden
is one of these passes, formed by several masses of rock cut
by nature into the shape of long parallelograms, and which have
between them a passage shut in by perpendicular walls. This
pass is near Skiærdal; another of the same kind is at Portfeld,
or the Mountain of the Gate. These openings exactly resemble
those by which the Hudson passes through successive chains
of mountains, which seem desirous of checking its course. The
Cordilleras of the Andes present the most stupendous passes of
this kind that are known; they are from four to five thousand
feet deep.
The valleys of the Hudson and Connecticut are equalled by few
in the old world for natural beauty and romantic scenery. Of
the valleys of Europe, that of the Rhine is most celebrated;
and is only more interesting than the Hudson on account of
its old historical associations, its populous cities, and the
picturesque ruins and massive monuments of architecture which
frown upon its banks.
CHAPTER III.――PRAIRIES AND PLAINS.
Public-domain text, read in full here on John Shaqi.
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