An inspection of the dunes shows that the number of individuals,
as well as the number of species, is very limited. In fact there
are apparently fewer plants here than on the dunes of large size
subsequently encountered between Ouargla and Touggourt. The most
characteristic plant is “drinn” (_Aristida pungens_), but it
is by no means common; there are also a few specimens of _Tamarix_
growing near the Nomad Mountains. As frequently happens where
there are moving dunes, the passage of the dune greatly changes the
character of the flora. Although this feature was not especially
studied, it was noted that the number of grasses where the dune
had swept was greater than it was before this. _Acanthyllis
tragacanthoides_, a plant typical of the plain, was found to
survive the passage of the sand, although changed in appearance in
a characteristic manner. It will be recalled that the species has
a top consisting of several shoots, springing from the root-crown
at the level of the ground, and a root-system in which the laterals
and the main root are alike well developed. In order that a plant,
already established, can maintain this general relation during the
heaping up of the sand, the main root must grow at the crown as
fast as the sand encroaches. This is exactly what happens, so that,
when the dune has passed on, the shoot of the species is elevated
for a space equaling the depth of the sand, which is half a meter
or more. From the probability that _Acanthyllis_ is of very slow
growth and that the dunes are low, it follows that the rate of dune
movement must be slow.
THE MOUNTAINS ABOUT LAGHOUAT.
The southern spurs of the Saharan Atlas lie to the north of Laghouat,
within 3 miles of the oasis. This range (the Nomad Mountains)
is not over 266 meters in height. Higher mountains extend both to
the west and to the east, but only the Nomads are visited. There
are also two high, rocky hills on opposite edges of the oasis,
the town lying between, and it is perhaps because of their presence
that the water is forced to the surface, or near the surface, and
the oasis is formed. The hill to the west of the town is called
the Rocher des Chiens. On the south side of the Nomad Mountains
is a long outcropping of gypsum; the south face of these mountains
is also abrupt, carrying little soil; but on the northern face the
slope is gradual and there is much soil, although rocks are abundant.
Public-domain text, read in full here on John Shaqi.
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