1911 Encyclopædia Britannica/Sahara
SAHARA, the great desert of northern Africa. The Sahara has anarea, according to Dr A. Bludau’s calculation of the areas of African river basins, of 3,459,500 sq. m., made up as follows:—
|Drainage or slope to Atlantic||131,000|
|Drainage or slotpe to Mediterranean||502,000|
|Slope to Niger basin|
This includes Tripoli and Fezzan, which practically belong to the desert zone, but does not include arid portions of the basins of the Nile and Niger, in which the drainage is at most intermittent, and which might with reason be included in the Sahara. The area would thus be brought up to at least 31 million sq. m., about the area of Europe minus the Scandinavian peninsula. The physical limits of this region are in some directions marked with great precision, as in parts of Morocco and Algeria, where the southern edge of the Atlas range looks out on what Area and boundaries. has almost the appearance of a boundless sea, and forms, as it were, a bold coast-line, whose sheltered bays and commanding promontories are occupied by a series of towns and villages—Tizgi, Figuig, El Aghuat, &c. In other directions the boundaries are vague, conventional and disputed. This is especially the case towards the south, where the desert sometimes comes to a close as suddenly as if it had been cut off with a knife, but at other times merges gradually and irregularly into the well-watered and fertile lands of the Sudan. While towards the east the valley of the Nile at first sight seems to afford a natural frontier, the characteristics of what is usually called the Nubian desert are so identical in most respects with those of the Sahara proper that some authorities extend this designation to the shores of the Red Sea. The desert, indeed, does not end with Africa, but is prolonged eastwards through Arabia towards the desert of Sind. As the Nubian region is described under Sudan: § Anglo-Egyptian, the present article is confined to the country west of the Nile Valley, the Libyan desert inclusive. Its greatest length, along the 20th parallel of north latitude, is some 3200 m.; its breadth north to south varies from 800 to 1400 m.
The sea-like aspect of certain portions of the Sahara has given rise to much popular misconception, and has even affected the ideas and phraseology of scientific writers. Instead of General aspect. being a boundless plain broken only by wave-like mounds of sand hardly more stable than the waves of ocean, the Sahara is a region of the most varied surface and irregular relief, ranging from 100 ft. below to 5000 and 6000 and even in isolated instances to Sooo ft. above the sealevel, and, besides sand-dunes and oases, containing rocky plateaus, vast tracts of loose stones and pebbles, ranges of the most dissimilar types, and valleys through which abundant watercourses must once have flowed.
In the centre of the Sahara is a vast mountain region known as the Ahaggar (Hoggar) Tasili or plateau. The culminating peaks of this plateau. Mounts Watellen and Hikena, are about 900 m. in a strai ht line almost due S. of the city of Algiers and about 1200 m. due of the mouth of the Niger. They also occupy, speaking roughly, a central position between the Atlantic and the Nile. The Ahaggar plateau is not inferior to the Alpsnin area, but its highest peaks do not greatly exceed 8000 ft. They are believed to be volcanic like those of Auvergne. Upon their summits snow is reputed to lie from December to March. South-east of the main plateau, and partly filling the valley between the Ahaggar plateau and the Tasili of the Asjer (see infra); are fthe Anahef mountains. To the north the valley is again contracted by the Irawen mountains.
Besides this central group of mountains. sometimes spoken of as the Atakor-’n-Ahaggar (Summits of the Ahaggar); there are various other massifs in the Sahara. On the north-west of the Mountain ranges.Ahaggar, and separated from it by a wide plain, is the Muidir plateau, which extends nearly east an west 200 m. North-east of the Ahaggar (in the direction of Tripoli) is the Tasili of the Asjer (4000-5000 ft.), which runs for 300 rn. in a N.E. to S.E. direction. South-east of the Tasili of tue Asjer is a range of hills known as the Tummo (or War) mountains. Still farther sOuth is the mountainous region of Tibesti (or Tu), with an average height of some 7000 ft., the volcanic cone of Tussid rising to an estimated height of 8800 ft. Towards the south and east the Tibesti highlands are connected with the lower ranges of Borku and Ennedi, which merge into the plains of Wadai and Darfur. The slopes are bare and rocky. By some authorities the Tasili of the Asjer, the Tummo, Tibesti and Borku ranges are considered “the orographic backbone” of the Sahara.
In addition to the plateaus and ranges named, there are several disconnected mountain masses. Midway between the Atakor-’n-Ahaggar and Nigeria are the Air or Asben hills in which Dr Erwin von Bary discovered (1877) the distinct volcanic crater of Teginjir with a vast lava-bed down its eastern side. By some writers Air (q.v.) is not included in the Sahara, as it lies within the limit of the tropical rains; but the districts farther southrhave all the characteristics of the desert. West of Air, and north-east of the bend of the Niger, lies the hilly region sometimes known as Adrar of the Iforas or of the Awellimiden (the southern confederacy of the Tuarég). To the N.E., in Fezzan (q.v.), are the dark mountains of Jebel-es-Soda, which are continued S.E. towards Kufra by the similar range of the Haruj; and in the extreme S.W., at no great distance from the Atlantic, is the hilly country of the western Adrar (q.v.).
Nearly all the rest of the Slahara consists in the main of undulating surfaces of rock (distinguished as hammada), vast tracts of water worn pebbles (serif) and regions of sandy dunes (variously called maghter, erg or areg, igidi, and in the east rhart), which occupy about one-ninth or one-tenth of the total area. The following is the general distribution of the dunes:—
From a point on the Atlantic coast south of Cape Blanco a broad
belt extends N.E. for about 1300 m., with a breadthyarying from
?o to 300 m. This is usually called the Igidi or Gidi,
dunes.from the Berber word for dunes. In part it runs parallel with the Atlas mountains. Eastward it is continued, south of Algeria and Tunisia, by the Western Erg and Eastern Erg, separated by a narrow valley at, Golea. South of the Eastern Erg (which extends as far north as the neighbourhood of the Gulf of Gabes) the continuity of the sandy tract is completely broken by the Hammada al-Homra (or Red Rock Plateau), but to the south of this region lie the dunes of Edeyen, which, with slight interruptions, extend to Murzuk in Fezzan. South of the hammada of Murzuk the dunes of Murzuk stretch south-east. This series of tracts may be called the northern zone of the Sahara; it forms a kind of bow, with its extremities respectively at the Atlantic and the Libyan desert and its apex in the south of Tunisia. In the south are the Juf (depressions), covering a vast area to the south-east of the middle portion of the Igidi, another area between the Adghagh plateau and the Ahaggar, and a third between Air and Tibesti. The Juf or depressions are not, except in rare instances, below sealevel. In the Libyan desert is a vast region of dunes of unascertained limits; the characteristics of the Libyan desert being thought typical of the whole of the Sahara originated the idea of “a sea of shifting sand” as descriptive of the entire desert. Here a region of over 500,000 sq. m. extending east from the Tibestilmountains to the valley of the Nile, bounded south by Wadai and Darfur and north by Fezzan and the Cyrenaica, appears to be almost entirely sterile and increasingly covered by dunes. There is only one known route through this dreadful wilderness—one running north and south to the oases of Kufra, which lie in its centre. The dunes in the Libyan desert, so far as is known, run N.N.W. and S.S.E. In the Eastern Erg the dunes also lie in long lines in a N.N.W. and S.S.E. direction, presenting a gradual slope to windward and an abrupt descent to leeward. There they are generally about 60 or 70 ft. high, but in other parts of the Sahara they are said to attain a height of upwards of 300 ft.
Under the influence of the wind the surface of the dunes' is subject to continual change, but in the mass they have attained such a state of comparative equilibrium that their topographic distribution may be considered as permanent, and some of them, such as Gern (Peak) al-Shuf and Gern Abd-al-Kader, to the south of Golea, have names of their own. The popular stories about caravans and armies being engulfed in the moving sands are regarded as apocryphal (save perhaps in some instances in the Libyan desert), but there is abundant evidence against the theory of M. Vatonne as to the dunes having been formed in situ.
Although now mainly waterless, the Sahara possesses the skeleton of a regular river-system. From the north side of the Atakor-’n-Ahaggar, through which runs the “water-parting” Skeleton river-systems. between the basins of the Mediterranean and Atlantic, system begins Wadi Igharghar, Which, running northwards between the Tasili plateau and the, Irawen mountains, appears to lose itself in the sands of the Eastern Erg, but can be traced northwards for hundreds of miles. Its bed contains rolled fragments of lava and freshwater shells (Cyrena and Planorbis). In a line almost parallel to Wadi I harghar, Wadi Mya descends from the plateau of Tademayt, and shows the importance of its ancient current by deep erosion of the Cretaceous rocks, in which a large number of left-hand tributaries have also left their mark. The streams flowing south from the Atlas, which seem to be absorbed in the sands of the desert, evidently fmd a, series of underground reservoirs or basins capable of being tapped by artesian wel s over very extensive areas. As Olympiodorus (quoted by Photius) mentions that the inhabitants of the Sahara used to make excavations from 100 to 120 ft. deep, out of which jets 'of pure water rose in columns, it is clear that this state of matters is (historically) of ancient date. Since 1856 French engineers have carried on a series of borings which have resulted in the fertilizing of extensive tracts. In Wadi Righ (otherwise Rhir), which runs for 80"m. towards the south-west of the Shat Melrir -(department of Constantine, Algeria), the water-bearing stratum is among permeable sands, which are covered to a depth of 200 ft. by impermeable marls, by which the water is kept under pressure. In t is valley many artesian wells have been sunk by the French. Connexions probably exist with subterranean water-supplies in the mountains to the rnorth. That the water in the artesian reservoirs is kept aerated is shown by the existence below ground of fishes, crabs and freshwater molluscs, all of which were ejected by the well called Mezer in Wadi Righ. Further west the Wadis Zusfana and Ghir unite to form the Saura, known in Tuat as the Messaud. These rivers still carry water as far as the northern part of Tuat; thence the course of the Messaud was, apparently, S.W. to the eastern Juf. There are also well-marked river-beds in the central Sahara. The Wadi Telemsi, rising in Adrar, of the Iforas, apparently joined the Niger near' Gao, while the Wadi Taffassassent, which rose in the Ahaggar mountains, is believed to have been the ancient upper course of the lower Niger. The oases are also proofs of the presence of a steady supply of underground moisture, for vegetation under the Saharan climate (beyond the few plants specially adapted to desert conditions) is exceptionally thirsty.
The existence of these wadis or river-beds is a factor in the consideration of the cause of the desert nature of the country. In all parts of the Sahara there is evidence of denudation carried out on a scale of unusual magnitude. The present surface of the desert has been exposed to the protracted wear and tear of the elements. But to determine the exact method by which the elements have done their work has hitherto proved beyond the power of science. The theory of submarine denudation was accepted by many scientists of the mid-Victorian era. The sand-dunes, the salt efiiorescence and deposits, and the local occurrence of certain modern marine molluscs all go to help the hypothesis of a diluvial sea. Nor is evidence lackin that in cretaceous times portions of the Sahara were covered by the sea. Colonel P. L. Monteil brou ht home (1892) a fossil sea-urchin from Bilma. In !9o2 at Tamasite, some 250 m. W. of Zinder, and a little north of Sokoto, a nautilus and four sea-urchins (fossils) were found by Captain Gaden in a limestone bed. Similar fossils occur in the, region between Zinder and Air, and others of the same age have been found near Dakar. Basing his conclusions on these and other facts, de Lapparent held that an arm of the sea extended inland from the Atlantic to the eastern Sahara. This sea was bounded on the north and east by the mountains of Air, Ahaggar, the Asjer Tasili, &c. An extensive acquaintance with Saharan characteristics shows, however, that a sea for the Sahara as a whole is impossible. Henri Schirmer, who in 1893 published an admirable summary of Saharan geography up to that date, argued that the desert nature of the Sahara is due to forces which have been at work for ages, although, as in all deserts, the dryness is probably progressively increasing. The primary cause is to be sought in the existing distribution of land and sea, the great land mass of North Africa causin an outflow of air in all directions (and consequent absence of rain) in winter, and an in draught in summer, when the surface is intensely heated and the relative humidity of the atmosphere becomes so small that condensation is all but impossible. The vicinity of the comparatively cool Mediterranean in the north accentuates the force of the winds from that direction, which, blowing towards a lower latitude, are in their v nature dry winds. The influence of mountain ranges, such asefhle Atlas, round the border of the desert, is thus but a subordinate cause of the latter's dryness, which would probably be little diminished did the Atlas not exist. This dryness reacts again on the temperature conditions of the Sahara, accentuating both the daily and annual variation. The intense heat of the day is compensated by the cold of the nights, so that the mean annual temperature is not excessive. 'The difference between the mean temperature of the hottest' and coldest month has been found to be as high as 45° F L, and the extreme range at least 90° F., maxima of II2 and over having been frequently observed. As a result of the extreme dryness of the air, evaporation is excessive, and, being greater than the precipitation, involves a progressive desiccation of the Sahara. V The surface of the rocks, heated by the sun and suddenly chilled by rapid radiation at night, ~gets fractured and crumbled; elsewhere the cliffs have been scored and the sand thus formed is at once turned by the wind into an active instrument of abrasion. In many places-it has planed the flat rocks of the hammada as smooth as ice. Elsewhere it has scored the vertical faces of the cliffs with curious imitations of glacial striation, and helped to undercut the pillar or table-like eminences-remains of former more extensive plateaus-which, under the name gur, are among the most familiar products of Saharan erosion. The softer quartz .rocks of the Quaternany and Cretaceous series have been made to yield the sand which, dri ted and sifted by the winds, has taken on the form of dunes. The slighest breeze is enough to make the. surface “smoke " with dust; and at times .the weird singing of the sands, waxing louder and louder, tells the scientific traveller that the motion is .not confined to the superficial particles. The dry wind of the Sahara is known in 'southern Europe as the Sirocco. It brings with it clouds of fine red dust, asnoted long since by Idrisi, the Arabian geographer. Dr Theobald Fischer and Dr Oscar F raas agree in believing that the desiccation has markedly increased in historic times. Evidence derived. from ancient monuments combined with the statements of Herodotus and Pliny are held toiprove. that the elephant, thefrhinoceros, and the crocodile existed in North African regions where the environment is now utterly alien, and on the other hand that the camel is a late introduction.-Any
attempt to improve the climatic conditions of the Sahara as a whole can hardly meet with success when the causes of its desiccation are considered. Much may, however, be done to modify local conditions, and fairly satisfactory results, have been obtained in the direction of fixing the dunes and covering them with a growth of vegetation. Experiments carried out by the French at Ain Sefra, on the northern border of the desert, have shown that by protecting the sand from the action of the wind by a litter of alfa grass, time is given for the establishment 'of suitable trees, which include the tamarisk, acacia, eucalyptus, prickly pear, peach and aspen poplar, the last-named having proved the most capable of all of resisting the desert conditions. Such planting operations an only be carried out in favourable localities, such as'valleys in which a certain amount of water is (available. Wide areas like the arid stony plateaus (hammada) must be abandoned as hopeless.
As already stated, the popular conception of the Sahara as a sand desert is erroneous. It IS really a stony, wind-swept waste with much bare rock visible, the actual 'area of pure sand forming a relatively small portion. A broad belt of Archaean rocks extends throu hout the desert, appearing at intervals in the form of hills and plateaus from beneath, the superficial sands and Quaternary deposits. Examples are the granite of Air and the gneiss and mica-schists of this massif and of the Ahaggar plateau. Flanking this zone are immense tracts occupied by rocks of Devonian and Carboniferous ages, from which characteristic marine fossils have been obtained at the springs- of El Hassi and between Wad Draa and the dunes of Igidi. Productus africanus is a common fossil of the Carboniferous rocks. At the close of the Carboniferous period it has been generally considered that the southern and central Sahara became dry land and has remained so up to the present day. Marine fossils of Cretaceous age have, however, been found within recent years in the central regions; while Eocene e chino ids have been obtained near Sokoto (Geal. Mag., 1904). During Lower Cretaceous times the Mediterranean covered the Algerian and Tripolitan Sahara and the northern portion of the eastern desert; the extensive development of the Cretaceous system being, one of the most striking features of Saharan geology. At, the close of the Cretaceous period the Tri olitan Sahara completely emergedgbut parts of the Tunisian and) Algerian Sahara seem to have remained below sea-level until the end of the Lower Eocene. Only on the extreme borders of the desert, however, do tertiary formations play any prominent part. During the Quaternary, eriod the Sahara possessed a moister climate than the present. 'lphisi is shown by the numerous water-cut valleys, now dry, and by the remains of hippopotamus in the Quaternary deposits# " 1 The idea so long held that the Sahara represented the recently dried-up bed of an extension of the Mediterranean has been .disproved by the investigations of French eulogists. The sand is mainly derived from the wide expanse of Cretaceous sandstones, which become rapidly disintegrated by the contraction caused by the wide range of temperature between dayandinight. The loose sands of the Quaternary deposits also . furnish abundant material. The true dune sand is remarkable for the uniformity of its composition and the geometrical regularity of its grains, which measure ess than °03937 in. While individually these appear transparent or reddish yellow (from the presence ofiron), they have in the mass a rich golden hue. Accordin to Tissandier animal organisms, such as the microscopic shells of Rhizopoda, abundant in sea-sand, are strikingly absent.
Botanically the Sahara is the meeting-ground of representatives of the “Mediterranean” and the “Tropical” floras which have accommodated themselves to the peculiar climatic conditions. The line of demarcation between the two floral areas, almost coinciding in the west with the Tropic of Cancer and in the east Botany and Zoology.dipping south towards the meridian of Lake Chad, assigns by far the greater portion of the area to “Mediterranean” influences. Uniformity, in spite of differences of altitude and soil, is a general characteristic of the vegetation, which outside of the oases consists mainly of plants with a tuft, dry, stiff habit of growth. The oases are the special home of the clate-palm, of which there are about 4,000,000 in the Algerian oases alone. In company with this tree, without which life in the Sahara would be practically impossible, are grown apples, peaches, oranges, citrons, figs, grapes, pomegranates, &c. From December to March wheat, barley and other northern grain crops are successfully cultivated, and in the hotter season rice, dukhn, durra and other tropical products. Altogether the oasal flora has considerable variety; thirty-nine species are known from the Kufra group, forty-eight from the Aujila group.
Zoologically the Sahara is also partly Mediterranean, partly Tropical. Apart from the domestic animals (camels, asses, &c., and very noticeably a black breed of cattle in Adrar), the list of fifteen mammals comprises the jerboa, the fennek or fox, the jackal, the sand rat (Psammomys obesus), the hare, the wild ass and three species of antelope. In Borku, Air, &c., baboons, hyaenas and mountain sheep are not uncommon. Without counting migratory visitants, about eighty species of birds have been re istered-the ostrich, the Certhilauda deserti or desert-lark (which often surprises the traveller with its son), Emberiza Saharae, three species of Dromalea, &c. Tortoises, lizards, chameleons, geckos, skinks, &c. of fifteen different species were collected by the single Rohlfs expedition of 1873–1874; the serpents comprise the horned viper, Psammophis sibilans, Coelopeltis lacertina, the python and several other species. The edible frog also occurs. Cypfinodon dispar, a fish not unlike Cyprinodon calaritanus, is found in all the brackish waters of north Sahara and swarms in the lake of the Siwa oasis.
The chief centres of population in the Sahara are, firstly, the oases, which occupy positions where the underground water makes its way to the surface or is readily reached by Centres of population.boring; and, secondly, certain mountainous districts where the atmosphenc moisture 15 condensed, and a moderate rainfall is the result. Except in the south of Algeria, where cultivation has been extended by means of artesian wells, the condition of the Sahara oases is far from prosperous. Prior to the French occupation, a feeling of insecurity had been engendered by the marauding habits of the nomad tribes; cultivation had become more restricted; and the decline of the caravan trade had brought ruin to certain centres, such as Murzuk. The most important are the oases of the Tuat region, especially Insalah; those of Ghat and Ghadames on the route from Tripoli to Zinder; and of Kufra, in eastern Sahara (see TUAT and T1u1>0LI). The various confederations of the Tuareg, in the central Sahara, are grouped round hilly districts. The most important are the Awellimiden, on the left bank of the Middle Niger; and the Kel-Ui, grouped around the mountainous districts of Air or Asben; the two northern confederations, those of the Ahaggar and Asjer, being less powerful. Much information respecting the Awellimiden confederation was obtained during the voyage down the Niger, in 1896, of Lieutenant Hourst of the French Navy, who was much struck with its powerful organization under the chief'Madidu. Northwest of Timbuktu in the district or “ Kingdom ” of Biru is the oasis and town of Walata, a Tuareg settlement. Other mountainous districts in which a certain amount of rain falls regularly, and which contain a population above the average for the Sahara, are Tibesti and Borku, in the east centre, and Adrar in the west. Tibesti and Borku are peopled by Tibbus; the western Adrar by Moors (Berbers). The northern portions of the Sahara are inhabited by nomad Arabs.
Attempts have been made by many explorers and writers to trace in certain of the existing inhabitants the remnants of an aboriginal race of negro affinities, which inhabited the Ethnology.Sahara before the arrival of the Berbers and Arabs. E. F. Gautier, writing in 1908, maintained that the evidence available (for the central Sahara) rendered probable the hypothesis that at a period perhaps as recent as the Roman conquest of North Africa the Sahara was still neolithic and peopled by a. race of agricultural negroes, who extended to the confines of Algeria. Negro influence is undoubtedly seen in various parts of the Sahara, but it may date from a much more recent period than has been supposed. For example, the connexion between many of the place-names in Fezzan and the language of Bornu is attributable to the northward extension of the influence of the Bornu-Kanem empire between the nth and 14th centuries A.D. The allusions by classical writers to Ethiopians as inhabitants of the Sahara prove little, in view of the very vague and general meaning attached to the word. The physical characteristics, and especially the dark colour, of many of the Saharan populations is apparently, a stronger argument, but even this is capable of another explanation. Caravans of negro slaves from time immemorial passed northwards along the main desert routes, and it is just in the oases on these routes that the dark element in the population is chiefly found. It may therefore be attributed to the intermarriage of the original lighter inhabitants of the oases with such slaves. The Tibbu (q.v.) or Tebu, once thought to be almost pure negroes, proved, when examined by Gustav Nachtigal in T ibesti, where they are found in greatest purity, to be a superior race with well-formed features and figures, of a light or dark bronze rather than black. Their language is related to that of the Kanuri in Bornu, but it appears that the Kanuri have derived theirs from the Tibbu, not the Tibbu from the Kanuri. Physically, the Tibbu appear to resemble somewhat the Tuareg, and there is little doubt that they are a Hamitic, not a negro, people.
The commerce of the Sahara is not inconsiderable. Among the more important trade routes are (1) from Morocco to Cairo by Insalah and Ghadames, which is followed by the commerce pilgrims of western Africa bound for Mecca; this route Commerce.has been largely superseded by the sea route from Tangier to Alexandria; (2) from Kuka (Lake Chad) to Murzuk and Tripoli; (3) from Kano and Zinder to Tripoli by Air and Ghat; (4) from Timbuktu to Insalah, Ghadames and Tripoli;(5) from Timbuktu to Insalah and thence to Algeria and Tunisia; (6) from Timbuktu to Morocco. The Senussi movement brought into prominence the desert routes between Wadai in the south and Jalo and Benghazi in the north, which partially superseded some of the older routes. Other causes tended to reduce the importance of the old routes. The long-established route from Darfur to the Kharga and Dakhila oases fell into disuse on the closing of the eastern Sudan by the Mahdist troubles. The great route leading from Tripoli via Ghadames and Ghat, to Zinder, Kano, and other great centres of the Hausa States maintains its importance, but the opening of trade from the side of the Niger by the British in the early years of the zoth century affected its value. The route across the western Sahara to Timbuktu is less used than formerly owing to the establishment by the French of a route from Senegal via Nioro to the Upper Niger. The old route, however, retains some importance on account of the salt trade from the Sahara, which centres at Timbuktu. Salt and date palms are the chief products of the Sahara. The principal sources of the salt supply are the rock-salt deposits of the Juf (especially Taudeni), the lakes of Kufra and the rock salt and brine of Bilma (q.v.).
The hope of an eventual commercial exploitation of the Sahara rests mainly on the possible existence of mineral wealth. To supply easy communication between Algeria and Nigeria the construction of a railway across the desert has found Trans-Saharan Railway Schemes.many advocates. Two principal routes have been suggested, the one taking an easterly line from Biskra through Wargla to Air (Agades) and Zinder—generally, the route followed by Foureau (see below); the other starting from the terminus of the most westerly railway already existing, and reaching Timbuktu via lgli and the Tuat oases. A third suggested route is one from Igli to the Senegal, still farther west.
Reference may also be made to the proposal, strenuously advocated
between 1870 and 1885, to open up the region to the south of
Algeria and Tunisia by the construction of an inland sea. Th
According to Colonel Francois Roudaire (1836–1885). the
of the Sahara.author of this scheme, deceptively styled the “flooding of the Sahara,” it was possible to create an inland sea with an average depth of 78 ft. and an area of 3100 sq. m., or about fourteen times the size of the Lake of Geneva. A French government commission decided that the excavati0n of the necessary canal would not be difficult, and that in spite of sllting-up processes the canal when cut would at least last 1000 to 1500 years. Ferdinand de Lesses, Roudaire's principal supporter, visited the district in 1883 andp reported that the canal would cost five years' labour and 150,000,000 francs. The scheme (which fell into abeyance on the death of Roudaire) was based on the following facts. The Gulf of Gabes is separated by a ridge 13 m. across and 150 ft. high from Shat-al Fejej, a depression which extends S.W. into the Shat Jerid, which in its turn is separated from the Shat Rharsa only by a still narrower ridge. Shat Garsa is succeeded westwards b a series of smaller depressions, and beyond them lies the Shat lvllelrir, whose N.W. end is not far from the town of Biskra.
Politically the Sahara belon s partly to Morocco (Tafilet, &c.), partly to the Turkish empire (Tripoli, Egypt, &c.), but principally to France. The French first acquired an interest in the Poltical Divisions. Sahara by their conquest of Algiers (1830–45). They gradually extended their influence southward with the purpose of forming a junction with their possessions on the Senegal. The acquisition of Tunisia (1881) largely increased the hold of the French on the Sahara, and the work of French pioneers to the south of Algeria was recognized by the Anglo-French agreement of 1890, which assigned to France the whole central Sahara from Algeria to a line from Say on the Niger to Lake Chad. The southern limit of the territory was, however, not strictly defined until 1898, when a new agreement gave to France a rectangular block south of the line mentioned, including the important frontier town of Zinder. A further agreement in 1904 again modified the frontier in favour of France. To the north-east and east the boundary of the French sphere was extended, by an Anglo-French Declaration of March 1899, and defined as running south-east, from the intersection of the Tropic of Cancer with 16° E., until it meets the meridian of 24° E., following this south to the frontier of Darfur. French Sahara is thus connected with the French sessions in West Africa and with the Congo-Shari territories olP(France on the south-east. On the west, where Spain claimed the Sahara coast between Capes Blanco and Bojador, the inland frontier was defined by the Franco-Spanish agreement of 1900, whereby Spain was apportioned a. Hinterland with an average depth of 240 m. from the sea-shore.
It is impossible to ascertain the extent of the knowledge of the Sahara possessed by the ancients. The Egyptians penetrated the Libyan and Nubian deserts at points, and Carthaginians and Phoenicians were acquainted with the northern Exploration.fringe of the desert in the west. European exploration dates from the beginning of the 19th century. In 1819 Captain G. F. Lyon and Joseph Ritchie penetrated from Tripoli to Murzuk, where Ritchie died. In 1822 came the great journey of Walter Oudney, Hugh Clapperton and Dixon Denham, from Tripoli to Lake Chad, and a year or two later Major A. G. Laing succeeded in reaching Timbuktu, also from Tripoli. In 1828 René Caillié crossed from Timbuktu to Morocco. Heinrich Barth in the course of his great journey (1849–1856), commenced from Tripoli under the leadership of James Richardson, traversed a considerable portion oi the Sahara. Between 1859 and 1861 Henri Duveyrier explored parts of the Tuareg domain. Knowledge of the northern Sahara, from Morocco to Tripoli, was largely increased by the journeys of Gerhard Rohlfs, begun in 1861; Rohlfs subsequently crossing (1865) from Tripoli to Lake Chad by nearly the same route as that previously taken by Barth. In 1873–1874 Rohlfs visited the oases in the north of the Libyan desert and in 1878–1879 reached the oasis of Kufra. In 1876–1877 another German traveller, Erwin von Bary, made his way to Ghat and Air, but was assassinated. A French expedition under Colonel Paul Flatters after penetrating far south of Algeria was massacred (1881) by Tuareg. Farther west success was attained in 188O by a German explorer, Dr Oskar Lenz, who, starting from Morocco made his way, partly by a new route, to Timbuktu. In 1892 the Sahara was crossed from Lake Chad to Tripoli by the French Colonel Monteil.
It was not until 1899 that the central Sahara, from Algeria to Air, was traversed for the first time by Europeans. This was accomplished under the leadership of F ernand Foureau. This journey was undertaken in pursuance of the efforts of the French to obtain effective control of the Sahara. South of Algeria military posts had been gradually pushed into the desert, Golea being until 1900 the farthest point which acknowledged French rule. The great desideratum was the opening up of a route to the Niger countries which might in time divert the trade from Tripoli to Algeria, but all attempts long proved fruitless, owing to the opposition of the tribes inhabiting central Sahara. In 1886 Lieutenant Palat Was murdered a little south of Gurara, and in 1880 the same fate befell Camille Douls in Tidikelt (Tuat) in his attempt to reach Timbuktu from the north. In 1890 Foureau—who in 1883 had undertaken a first journey of exploration south of Wargla-reached the Tademayt plateau in 28° N., fixing the position of 35 places, and in 1892–1893 came the first of his long series of expeditions undertaken with a view of penetrating the country of the Azjer Tuareg, the powerful confederacy which lay on the route to Air and Lake Chad, never traversed in its entirety by a European. All efforts to obtain a passage were unavailing until in 1898–1899 Foureau, accompanied by an escort of troops under Major Lamy, at last attained his object, finally reaching Zinder, the important trade centre on the borders of Nigeria, and midway between the river Niger and Lake Chad, on the 2nd of November 1899.
The important section of Foureau's route began at Ain El-Hajaj, in about 261 ° N., immediately beyond which the frowning mass# of Tindesset had to be crossed by a most difficult route among a chaos of rocks and ravines, the geological formation being principally sandstone. After descending the southern escarpment of the “Tasili, " the expedition crossed the mountainous region named Anahef, composed of quartz and granite, through which the line of partition between the basins of the Mediterranean and Atlantic was found to run. Thence the route lay across the wide plain of quartz gravel, strewn with blocks of granite, known to the Tuareg as Timri, to the well of In-Azaua, beyond which a march of eleven days, with a water-supply at one point only, led to the first village of Air, where the Tuareg proved hostile. Agades, the capital of Air, was reached by a march through difficult mountains, with valleys which gradually opened into a wide plain. From Agades to Zinder the route lay, first, through the bare and arid district of Azauak; next, through the bush-covered Tagama, a district abounding in game; and, lastly, through the cultivated country of Damer%hu. Zinder had only once before been reached by way of Air-by arth's expedition in 1850. It was now occupied by a French force which had advanced from the Niger (see Senegal: Colony).
Foureau's achievement was quickly followed by increased political activity of the French in the Sahara south of Algeria, where, in addition to the work of other explorers, surveys had been carried by French olhcers (especially Captains Germain and Laperrine in 1898) as far as the important centre of Insalah, the position of which had, as a result, been shifted some 25 m. E. of its former position on the maps, being found to lie in 2° 16′ E., 20° 17′ 30″ N. Early in 1900 G. B. M. Flamand, who had been entrusted with a scientific mission to the Tuat oases, came into collision with the natives, and Insalah was occupied by the military escort which accompanied him. This was quickly followed by the occupation of Tuat, and Igli (see Tuat).
Simultaneously with these events, an attempt was made to pave the way for the establishment of French influence in western Sahara by the expedition of Paul Blanchet to Adrar, which had not been visited since the middle of the 19th century. It returned in September 1900, only partially successful, Blanchet and his companions having been detained for some time as virtual prisoners on the borders of Adrar. The leader almost immediately succumbed to fever. In 1903–1999 the country N. of the lower Senegal, including Adrar, was brought under French control and organized as the territory of Mauretania.
The most marked progress was, however, effected in the central Sahara, where the French posts were gradually pushed farther south under a military organization, which resulted in the complete pacincation of the Tuareg countries. Travel was thus made possible from one border of the desert to the other, and a number of successful expeditions gathered a rich harvest of results respecting the mapping, geology, and other features of this part of the Sahara. Some of the best work was done by Laperrine, Arnaud, Cortier and Niegerlon the military side, and, on the civilian, by Villatte, Gautier and Chudeau. Apart from these French enterprises, Hanns Vischer, a Swiss in the service of British Nigeria, in 1906 travelled from Tripoli to Bornu through Murzuk and Bilma. In 1910 Capt. A. H. Haywood traversed the Sahara, being the first Englishman to cross the desert from Gao to Insalah.
Authorities.—Vatonne, Mission de Ghadames (1863); H. Duveyrier, Les Touaregs du Nord (1864); Ville, Explor. géologique du Mzab, &'c. (1867): A. Pomel, Le Sahara (1872); F. G. Rohlfs, Quer durch Afrika (1874) Drei Monate un lzbgschen Wüste (1875) and Kufra (1881); V. Largeau, Le Pays de Rirha-Ouargla (1879); G. Nachtigal, Sâhărâ und Sûdân (3 vols., 1879–1889); G. Rolland, “Le Crétacé du Sahara septentrional” (with geological map of the Central Sahara), in Bull. de la Soc. Géol. de France (1881); Roudaire, Rapport sur la dernière expéd. des Chotts (1881) (and other reports by the same author); Tchihatchef, “The Deserts of Africa and Asia,” in British Association Reports (Southampton, 1882); Derrécagaix, “Explor. du Sahara: les deux missions du Lieut.-Colonel Flatters,” in Bull. de la Soc. de Géogr. (1882); O. Lenz, Timbuktu. Reise durch Marokko, &c. (1884); and E. L. Reclus, Nouv. Géographie univ. xi. (1886); H. Schirmer, Le Sahara (Paris, 1893); P. Vuillot, L’Exploration du Sahara (Paris, 1895); P. L. Monteil, De Saint-Louis à Tripoli (Paris, 1895); Fr. Foureau, D’Alger au Congo par le Tchad (Paris, 1902) and Documents scientifiques de la mission saharienne, fasc. i.-iii. (Paris, 1903–1905); Privat-Deschanel, “Peut-on reboiser le Sahara?” Rev. scientif. (1896); K. A. Zittel, Paläontologie der libyschen Wüste (Cassel, 1893); G. Rolland, Chemin de fer transsaharien, géologie du Sahara algérien, et aperçu géologique sur le Sahara de l’océan atlantique à la mer rouge (Paris, imp. Nat., 1891); J. Walther, Die Denudation in der Wüste (Leipzig, 1900); M. Honoré, Le Transsaharien et la pénétration française en Afrique (Paris, 1901); E. Dürkop, Die wirtschafts- und handelsgeographischen Provinzen der Sahara (Wolfenbüttel, 1902); W. J. Harding King, A Search for the Masked Tawareks (London, 1902); A. Bernard and N. Lacroix, La Pénétration saharienne (Algiers, 1906); C. Vélan, “Etat actuel de nos connaissances sur la géographie et la géologie du Sahara d’après les explorations les plus récentes,” Revue de géogr. t. i. (1906–1907), pp. 447-517; J. Lahache, “Le Desséchement de l’Afrique française est-il démontré?" Bul. Soc. Géogr. Marseille, 31 (1907), pp. 149-185; E. Arnaud and M. Cortier, Mission Arnaud-Cartier: nos confins sahariens (Paris, 1908); E. F. Gautier and R. Chudeau, Missions au Sahara, t. i. “Sahara algérien,” par E. F. Gautier (Paris, 1908), t. ii. “Sahara sudanais,” par R. Chudeau (Paris, 1909); H. Vischer, Across the Sahara from Tripoli to Bornu (London, 1910); H. J. Ll. Beadnell, “Sand Dunes of the Libyan Desert,” Geog. Jour. (April 1910); E. Fallot, “Le Commerce du Sahara,” Ques. dip. et col. t. 15 (1903), pp. 209-225. (E. He.; F. R. C.)