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 forms of dunes.=—The forms assumed by dunes are dependent to
a very large extent upon the strength of the wind and the available
supply of sand. With small quantities of sand and with moderate winds,
sickle-shaped dunes known as _barchans_ (Fig. 221) are formed, whose
convex and flatter slopes are toward the wind and whose steep concave
leeward slopes are maintained at the angle of repose. The barchan is
shaped by the wind going both over and around the dune, constantly
removing sand from the windward side and depositing it to leeward.
With larger supplies of sand and winds which are not too violent a
series of barchans is built up, and these are arranged transversely to
the wind direction (Fig. 222 _b_). If the winds are more violent, the
minor depressions in the crests of the dunes become wind channels, and
the sand is then trailed out along them until the arrangement of the
ridges is parallel to the wind (Fig. 222 _c_). The surfaces of dunes
are generally marked by beautiful ripples in the sand, which, seen from
a little distance, may give the appearance of watered silk (plate 7 A).
[Illustration: FIG. 221.—View of desert barchans (after Haug).]
[Illustration:
FIG. 222.—Diagrams to show the relationships in form and in
orientation of dunes to the supply of sand and to the strength of the
wind. _a_, barchans formed by small supplies of sand and moderate
winds; _b_, transverse dune ridges, formed when supply of sand is large
and winds are moderate; _c_, dune ridges formed with large sand supply
and violent winds (after Walther and Cornish).]
Under normal conditions dunes are not stationary but continue to wander
with the prevailing winds until they have reached the outer edge of
the zone of vegetation near the base of the foothills at the margin of
the desert. Here the grasses and other desert plants arrest the first
sand grains that reach them, and they continue to grow higher as the
sands accumulate. Some of the desert plants, like the yuccas, have so
adapted themselves to desert conditions that they may grow upward with
the sand for many feet and so keep their crowns above its surface.
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