Tafilet : $b the narrative of a journey of exploration in the Atlas mountains and the oases of the north-west SaharaHarris, Walter
History
Tafilet : $b the narrative of a journey of exploration in the Atlas mountains and the oases of the north-west Sahara
Harris, Walter
Atlas Mountains; Morocco -- Description and travel
Ascending by the dry bed of a torrent on the south side of the
river, we skirted the eastern end of Jibel Teluet, which forms
the southern boundary of the valley, and descended some four miles
farther on to the larger stream of the Wad Unila. The ascent and
descent we had crossed forms a small watershed for the tributaries
of the two rivers, though apparently these mountain torrents only
flow in the wet season. At one spot, rather more than half-way, we
passed extensive salt-mines, where quite a number of natives were
engaged in working rock-salt. The scene was a wild one, the half-nude
men with their rough picks hewing away and singing the while, as
others piled the salt in native panniers on to the backs of their
sturdy little mules. The power of these mountain-mules in overcoming
difficulties in the roads is extraordinary, and at one spot we saw
a couple literally descending a precipice, followed by a man who
only kept his footing by the aid of a sort of alpenstock. The manner
in which both man and beasts succeeded in descending seemed to us,
as we stood and watched, incredible, yet we were told that he made
the journey every day to this spot in the face of the precipice,
to collect rock-salt from a small deposit that existed there. At
one place where an unusually large supply of the precious mineral
existed, a roughly constructed fort had been built, for the mines
had been the cause of war for generations amongst the tribesmen
living near, their value being, for the arid bleak district,
extraordinary. No doubt to more or less reserving to himself the
monopoly, as is the case, is owing to a great extent the wealth
to-day in the possession of Sid Madani, the Kaid of Glawa. The soil
at this part consists principally of shales, strewn with boulders
of limestone, no doubt portions of the peaks above, which time,
water, and glacier have carried to their present position.
The Wad Unila, where our path struck its course, flows nearly due
north and south, issuing from a gorge 100 or 200 yards above,
and descending for half a mile through a narrow valley before
reaching the district of Tiurassín, in which we spent the night
of November 5.
Public-domain text, read in full here on John Shaqi.
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