Earth Features and Their Meaning: An Introduction to Geology for the Student and the General ReaderHobbs, William Herbert
Science
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader
Hobbs, William Herbert
Geology; Physical geography
=The maturely dissected upland.=—Continued ramifications by the
rivers eventually divide the entire upland area into separated parts,
and the rounding of the shoulders of valleys proceeds simultaneously
until of the original upland no easily recognizable compartments
are to be found. Where before were flat hilltops are now ridges or
watersheds, the well-known _divides_. The upland is now said to be
completely dissected or to have arrived at _maturity_. The streams are
still vigorous, for they make the full descent from the upland level
to base level, and yet a critical turning point of their history has
been reached, and from now on they are to show a steady falling off in
efficiency as sculpturing agents.
[Illustration:
FIG. 177.—View of a maturely dissected upland from one of its
hilltops, Klamath Mountains, California (after a photograph by
Fairbanks).]
Viewed from one of the hilltops, the landscape of this stage bears a
marked resemblance to a sea in which the numberless divides are the
crests of billows, and these, as distance reduces their importance in
the landscape, fade away into the even line of the horizon (Fig. 177).
=The Hogarthian line of beauty.=—Since the youthful stage of the
upland, when the lines of its landscape were straight, its character
rugged, and its rivers wild and turbulent, there has been effected
a complete transformation. The only straight line to be seen is the
distant horizon, for the landscape is now molded in softened outlines,
among which there is a repeated recurrence of the line of beauty made
famous by Hogarth in his “Analysis of Beauty.” As well known to all art
students, this is a sinuous line of reversed or double curvature—a
curve which passes insensibly at a point of inflection from convex
to concave (Fig. 178). The curve of beauty is now found in every
section of the hills, and it imparts to the landscape a gracefulness
and a measure of restfulness as well, which are not to be found in the
landscapes of earlier stages in the erosion cycle. In the bottoms of
the valleys also the initial windings of the rivers within their narrow
flood plains add silver beauty lines which stand out prominently from
the more somber background of the hills.
[Illustration: FIG. 178.—Hogarth’s line of beauty.]
Considered from the commercial viewpoint, the mature upland is one
of the least adaptable as a habitation for highly civilized man.
Direct lines of communication run up hill and down dale in monotonous
alternation, and almost the only way of carrying a railroad through the
region, without an expenditure for trestles which would be prohibitive,
is to follow the tortuous crest of a main divide or the equally winding
bed of one of the larger valleys.
[Illustration:
FIG. 179.—View of the old land of New England, with Mount Monadnock
rising in the distance.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account