# 1911 Encyclopædia Britannica/British East Africa

BRITISH EAST AFRICA, a term, in its widest sense, including all the territory under British influence on the eastern side of Africa between German East Africa on the south and Abyssinia and the Anglo-Egyptian Sudan on the north. It comprises the protectorates of Zanzibar, Uganda and East Africa. Apart from a narrow belt of coastland, the continental area belongs almost entirely to the great plateau of East Africa, rarely falling below an elevation of 2000 ft., while extensive sections rise to a height of 6000 to 8000 ft. From the coast lowlands a series of steps with intervening plateaus leads to a broad zone of high ground remarkable for the abundant traces of volcanic action. This broad upland is furrowed by the eastern “rift-valley,” formed by the subsidence of its floor and occupied in parts by lakes without outlet. Towards the west a basin of lower elevation is partially occupied by Victoria Nyanza, drained north to the Nile, while still farther inland the ground again rises to a second volcanic belt, culminating in the Ruwenzori range. (See Zanzibar, and for Uganda protectorate see Uganda.) The present article treats of the East Africa protectorate only.

Topography.—The southern frontier, coterminous with the northern frontier of German East Africa, runs north-west from the mouth of the Umba river in 4° 40′ S. to Victoria Nyanza, which it strikes at 1° S., deviating, however, so as to leave Mount Kilimanjaro wholly in German territory. The eastern boundary is the Indian Ocean, the coast line being about 400 m. On the north the protectorate is bounded by Abyssinia and Italian Somaliland; on the west by Uganda. It has an area of about 240,000 sq. m., and a population estimated at from 2,000,000 to 4,000,000, including some 25,000 Indians and 3000 Europeans. Of the Europeans many are emigrants from South Africa; they include some hundreds of Boer families.

The first of the parallel zones—the coast plain or “Temborari”—is generally of insignificant width, varying from 2 to 10 m., except in the valleys of the main rivers. The shore line is broken by bays and branching creeks, often cutting off islands from the mainland. Such are Mvita or Mombasa in 4° 4′ S., and the larger islands of Lamu, Manda and Patta (the Lamu archipelago), between 2° 20′ and 2° S. Farther north the coast becomes straighter, with the one indentation of Port Durnford in 1° 10′ S., but skirted seawards by a row of small islands. Beyond the coast plain the country rises in a generally well defined step or steps to an altitude of some 800 ft., forming the wide level plain called “Nyika” (uplands), largely composed of quartz. It contains large waterless areas, such as the Taru desert in the Mombasa district. The next stage in the ascent is marked by an intermittent line of mountains—gneissose or schistose—running generally north-north-west, sometimes in parallel chains, and representing the primitive axis of the continent. Their height varies from 5000 to 8000 ft. Farther inland grassy uplands extend to the eastern edge of the rift-valley, though varied with cultivated ground and forest, the former especially in Kikuyu, the latter between 0° and 0° 40′ S. The most extensive grassy plains are those of Kapte or Kapote and Athi, between 1° and 2° S. The general altitude of these uplands, the surface of which is largely composed of lava, varies from 5000 to 8000 ft. This zone contains the highest elevations in British East Africa, including the volcanic pile of Kenya (q.v.) (17,007 ft.), Sattima (13,214 ft.) and Nandarua (about 12,900 ft.). The Sattima (Settima) range, or Aberdare Mountains, has a general elevation of fully 10,000 ft. To the west the fall to the rift-valley is marked by a line of cliffs, of which the best-defined portions are the Kikuyu escarpment (8000 ft.), just south of 1° S., and the Laikipia escarpment, on the equator. One of the main watersheds of East Africa runs close to the eastern wall of the rift-valley, separating the basins of inland drainage from the rivers of the east coast, of which the two largest wholly within British East Africa are the Sabaki and Tana, both separately noticed. The Guaso Nyiro rises in the hills north-west of Kenya and flows in a north-east direction. After a course of over 350 m. the river in about 1° N., 39° 30′ E. is lost in a marshy expanse known as the Lorian Swamp.

The rift-valley, though with a generally level floor, is divided by transverse ridges into a series of basins, each containing a lake without outlet. The southernmost section within British East Africa is formed by the arid Dogilani plains, drained south towards German territory. At their north end rise the extinct volcanoes of Suswa (7800 ft.) and Longonot (8700), the latter on the ridge dividing off the next basin—that of Lake Naivasha. This is a small fresh-water lake, 6135 ft. above the sea, measuring some 13 m each way. Its basin is closed to the north by the ridge of Mount Buru, beyond which is the basin of the still smaller Lakes Nakuro (5845 ft.) and Elmenteita (5860 ft.), followed in turn by that of Lakes Hannington and Baringo (q.v.). Beyond Baringo the valley is drained north into Lake Sugota, in 2° N., some 35 m. long, while north of this lies the much larger Lake Rudolf (q.v.), the valley becoming here somewhat less defined.

On the west of the rift-valley the wall of cliffs is best marked between the equator and 1° S., where it is known as the Mau Escarpment, and about 1° N., where the Elgeyo Escarpment falls to a longitudinal valley separated from Lake Baringo by the ridge of Kamasia. Opposite Lake Naivasha the Mau Escarpment is over 8000 ft. high. Its crest is covered with a vast forest. To the south the woods become more open, and the plateau falls to an open country drained towards the Dogilani plains. On the west the cultivated districts of Sotik and Lumbwa, broken by wooded heights, fall towards Victoria Nyanza. The Mau plateau reaches a height of 9000 ft. on the equator, north of which is the somewhat lower Nandi country, well watered and partly forested. In the treeless plateau of Uasin Gishu, west of Elgeyo, the land again rises to a height of over 8000 ft., and to the west of this is the great mountain mass of Elgon (q.v.). East of Lake Rudolf and south of Lake Stefanie is a large waterless steppe, mainly volcanic in character, from which rise mountain ranges. The highest peak is Mount Kanjora, 6900 ft. high. South of this arid region, strewn with great lava stones, are the Rendile uplands, affording pasturage for thousands of camels. Running north-west and south-east between Lake Stefanie and the Daua tributary of the Juba is a mountain range with a steep escarpment towards the south. It is known as the Goro Escarpment, and at its eastern end it forms the boundary between the protectorate and Abyssinia. South-east of it the country is largely level bush covered plain, mainly waterless.

[Geology.—The geological formations of British East Africa occur in four regions possessing distinct physiographical features. The coast plain, narrow in the south and rising somewhat steeply, consists of recent rocks. The foot plateau which succeeds is composed of sedimentary rocks dating from Trias to Jurassic. The ancient plateau commencing at Taru extends to the borders of Kikuyu and is composed of ancient crystalline rocks on which immense quantities of volcanic rocks—post-Jurassic to Recent—have accumulated to form the volcanic plateau of Central East Africa.

The formations recognized are given in the following table:—

 Sedimentary. Recent ${\displaystyle \scriptstyle {\left\{{\begin{matrix}\ \\\\\ \ \end{matrix}}\right.}}$ 1. Alluvium and superficial sands. 2. Modern lake deposits, living coral rock. 3. Raised coral rock, conglomerate of Mombasa Island. Pleistocene ${\displaystyle \scriptstyle {\left\{{\begin{matrix}\ \\\ \end{matrix}}\right.}}$ 4. Gravels with flint implements. 5. Glacial beds of Kenya Jurassic 6. Shales and limestones of Changamwe. Karroo ${\displaystyle \scriptstyle {\left\{{\begin{matrix}\ \\\ \end{matrix}}\right.}}$ 7. Flags and sandstones. 8. Grits and shales of Masara and Taru. Carboniferous? 9. Shales of the Sabaki river. Archaean ${\displaystyle \scriptstyle {\left\{{\begin{matrix}\ \\\ \end{matrix}}\right.}}$ 10. Schists and quartzites of Nandi. 11. Gneisses, schists, granites. Igneous and Volcanic. Recent Active, dormant and extinct volcanoes. Post-Jurassic to Pleistocene ${\displaystyle \scriptstyle {\left\{{\begin{matrix}\ \\\ \end{matrix}}\right.}}$ Kibo and volcanoes of the rift-valley. Kimawenzi, Kenya and plateau eruptions.

Archaean.—These rocks prevail in the districts of Taru, Nandi and throughout Ukamba. A course gneiss is the predominant rock, but is associated with garnetiferous mica-schists and much intrusive granite. Hornblende schists and beds of metamorphic limestone are rare. Cherty quartzites interbedded with mylonites occur on the flanks of the Nandi hills, but their age is not known.

Carboniferous?—From shales on the Sabaki river Dr Gregory obtained fish-scales and specimens of Palaeanodonta Fischeri.

Karroo.—The grits of Masara, near Rabai mission station and Mombasa, have yielded specimens of Glossopteris browniana var. indica, thus indicating their Karroo age.

Jurassic.—Shales and limestones of this age are well seen along the railway near Changamwe. They contain gigantic ammonites. According to Dr Waagen the ammonites show a striking analogy to forms from the Acanthicus zone of East India. Belemnites are plentiful.

Pleistocene.—These are feebly represented by some boulder beds on the higher slopes of Kilimanjaro and Kenya. They show that in Pleistocene times the glaciers of Kilimanjaro and Kenya extended much farther down the mountain slopes.

Recent.—The ancient and more modern lake deposits have so far yielded no mammalian or other organic remains of interest.

Igneous and Volcanic.—A belt of volcanic rocks, over 150,000 sq. m. in area, extends from beyond the southern to beyond the northern territorial limits. They belong to an older and a newer set. The older group commenced with a series of fissure eruptions along the site of the present rift-valley and parallel with it. From these fissures immense and repeated flows of lava spread over the Kapte and Laikipia plateaus. At about the same time, or a little later, Kenya and Kimawenzi, Elgon and Chibcharagnani were in eruption. The age of these volcanic outbursts cannot be more definitely stated than that they are post-Jurassic, and probably extended through Cretaceous into early Tertiary times. This great volcanic period was followed by the eruptions of Kibo and some of the larger volcanoes of the rift-valley. The flows from Kibo include nepheline and leucite basanite lavas rich in soda felspars. They bear a close resemblance to the Norwegian “Rhombenporphyrs.” The chain of volcanic cones along the northern lower slopes of Kilimanjaro, those of the Kyulu mountains, Donyo Longonot and numerous craters in the rift-valley region, are of a slightly more recent date. A few of the volcanoes in the latter region have only recently become extinct; a few may be only dormant. Donyo Buru still emits small quantities of steam, while Mount Teleki, in the neighbourhood of Lake Rudolf, was in eruption at the close of the 19th century.]

Climate, Flora and Fauna.—In its climate and vegetation British East Africa again shows an arrangement of zones parallel to the coast. The coast region is hot but is generally more healthy than the coast lands of other tropical countries, this being due to the constant breeze from the Indian Ocean and to the dryness of the soil. The rainfall on the coast is about 35 in. a year, the temperature tropical. The succeeding plains and the outer plateaus are more arid. Farther inland the highlands—in which term may be included all districts over 5000 ft. high—are very healthy, fever being almost unknown. The average temperature is about 66° F. in the cool season and 73° F. in the hot season. Over 7000 ft. the climate becomes distinctly colder and frosts are experienced. The average rainfall in the highlands is between 40 and 50 in. The country bordering Victoria Nyanza is typically tropical; the rainfall exceeds 60 in. in the year, and this region is quite unsuitable to Europeans. The hottest period throughout the protectorate is December to April, the coolest, July to September. The “greater rains” fall from March to June, the “smaller rains” in November and December. The rainfall is not, however, as regular as is usual in countries within the tropics, and severe droughts are occasionally experienced.

In the districts bordering Victoria Nyanza the flora resembles that of Uganda (q.v.). The characteristic trees of the coast regions are the mangrove and coco-nut palm. Ebony grows in the scrub-jungle. Vast forests of olives and junipers are found on the Mau escarpment; the cotton, fig and bamboo on the Kikuyu escarpment; and in several regions are dense forests of great trees whose lowest branches are 50 ft. from the ground. Two varieties of the valuable rubber-vine, Landolphia florida and Landolphia Kirkii, are found near the coast and in the forests. The higher mountains preserve distinct species, the surviving remnants of the flora of a cooler period.

The fauna is not abundant except in large mammals, which are very numerous on the drier steppes. They include the camel (confined to the arid northern regions), elephant (more and more restricted to unfrequented districts), rhinoceros, buffalo, many kinds of antelope, zebra, giraffe, hippopotamus, lion and other carnivora, and numerous monkeys. In many parts the rhinoceros is particularly abundant and dangerous. Crocodiles are common in the larger rivers and in Victoria Nyanza. Snakes are somewhat rare, the most dangerous being the puff-adder. Centipedes and scorpions, as well as mosquitoes and other insects, are also less common than in most tropical countries. In some districts bees are exceedingly numerous. The birds include the ostrich, stork, bustard and secretary-bird among the larger varieties, the guinea fowl, various kinds of spur fowl, and the lesser bustard, the wild pigeon, weaver and hornbill. By the banks of lakes and rivers are to be seen thousands of cranes, pelicans and flamingoes.

Inhabitants.—The white population is chiefly in the Kikuyu uplands, the rift-valley, and in the Kenya region. The whites are mostly agriculturists. There are also numbers of Indian settlers in the same districts. The African races include representatives of various stocks, as the country forms a borderland between the Negro and Hamitic peoples, and contains many tribes of doubtful affinities. The Bantu division of the negroes is represented chiefly in the south, the principal tribes being the Wakamba, Wakikuyu and Wanyika. By the north-east shores of Victoria Nyanza dwell the Kavirondo (q.v.), a race remarkable among the tribes of the protectorate for their nudity. Nilotic tribes, including the Nandi (q.v.), Lumbwa, Suk and Turkana, are found in the north-west. Of Hamitic strain are the Masai (q.v.), a race of cattle-rearers speaking a Nilotic language, who occupy part of the uplands bordering on the eastern rift-valley. A branch of the Masai which has adopted the settled life of agriculturists is known as the Wakuafi. The Galla section of the Hamites is represented, among others, by Borani living south of the Goro Escarpment (though the true Boran countries are Liban and Dirri in Abyssinian territory), while Somali occupy the country between the Tana and Juba rivers. Of the Somali tribes the Herti dwell near the coast and are more or less stationary. Further inland is the nomadic tribe of Ogaden Somali. The Gurre, another Somali tribe, occupy the country south of the lower Daua. Primitive hunting tribes are the Wandorobo in Masailand, and scattered tribes of small stature in various parts. The coast-land contains a mixed population of Swahili, Arab and Indian immigrants, and representatives of numerous interior tribes.

Provinces and Towns.—The protectorate has been divided into the provinces of Seyyidie (the south coast province, capital Mombasa); Ukamba, which occupies the centre of the protectorate (capital Nairobi); Kenya, the district of Mt. Kenya (capital Fort Hall); Tanaland, to the north of the two provinces first named (capital Lamu); Jubaland, the northern region (capital Kismayu); Naivasha (capital Naivasha); and Kisumu (capital Kisumu); each being in turn divided into districts and sub-districts. Naivasha and Kisumu, which adjoin the Victoria Nyanza, formed at first the eastern province of Uganda, but were transferred to the East Africa protectorate on the 1st of April 1902. The chief port of the protectorate is Mombasa (q.v.) with a population of about 30,000. The harbour on the south-west side of Mombasa island is known as Kilindini, the terminus of the Uganda railway. On the mainland, nearly opposite Mombasa town, is the settlement of freed slaves named Freretown, after Sir Bartle Frere. Freretown (called by the natives Kisaoni) is the headquarters in East Africa of the Church Missionary Society. It is the residence of the bishop of the diocese of Mombasa and possesses a fine church and mission house. Lamu, on the island of the same name, 150 m. north-east of Mombasa, is an ancient settlement and the headquarters of the coast Arabs. Here are some Portuguese ruins, and a large Arab city is buried beneath the sands. The other towns of note on the coast are Malindi, Patta, Kipini and Kismayu. At Malindi, the “Melind” of Paradise Lost, is the pillar erected by Vasco da Gama when he visited the port in 1498. The harbour is very shallow. Kismayu, the northernmost port of the protectorate, 320 m. north-east of Mombasa, is the last sheltered anchorage on the east coast and is invaluable as a harbour of refuge. Flourishing towns have grown up along the Uganda railway. The most important, Nairobi (q.v.), 327 m. from Mombasa, 257 from Port Florence, was chosen in 1907 as the administrative capital of the protectorate. Naivasha, 64 m. north-north-west of Nairobi, lies in the rift-valley close to Lake Naivasha, and is 6230 ft. above the sea. It enjoys an excellent climate and is the centre of a European agricultural settlement. Kisumu or Port Florence (a term confined to the harbour) is a flourishing town built on a hill overlooking Victoria Nyanza. It is the entrepôt for the trade of Uganda.

Mombasa is visited by the boats of several steamship companies, the German East Africa line maintaining a fortnightly service from Hamburg. There is also a regular service to and from India. A cable connecting Mombasa with Zanzibar puts the protectorate in direct telegraphic communication with the rest of the world. There is also an inland system of telegraphs connecting the chief towns with one another and with Uganda.

Agriculture and other Industries.—In the coast region and by the shores of Victoria Nyanza the products are tropical, and cultivation is mainly in the hands of the natives or of Indian immigrants. There are, however, numerous plantations owned by Europeans. Rice, maize and other grains are raised in large quantities; cotton and tobacco are cultivated. The coco-nut palm plantations yield copra of excellent quality, and the bark of the mangrove trees is exported for tanning purposes. In some inland districts beans of the castor oil plant, which grows in great abundance, are a lucrative article of trade. The sugar-cane, which grows freely in various places, is cultivated by the natives. The collection of rubber likewise employs numbers of people.

Among the European settlers in the higher regions much attention is devoted to the production of vegetables, and very large crops of potatoes are raised. Oats, barley, wheat and coffee are also grown. The uplands are peculiarly adapted for the raising of stock, and many of the white settlers possess large flocks and herds. Merino sheep have been introduced from Australia. Ostrich farms have also been established. Clover, lucerne, ryegrass and similar grasses have been introduced to improve and vary the fodder. Other vegetable products of economic value are many varieties of timber trees, and fibre-producing plants, which are abundant in the scrub regions between the coast and the higher land bordering the rift-valley. Over the greater part of the country the soil is light reddish loam; in the eastern plains it is a heavy black loam. As a rule it is easily cultivated. While the majority of the African tribes in the territory are not averse from agricultural labour, the number of men available for work on European holdings is small. Moreover, on some of the land most suited for cultivation by white men there is no native population.

In addition to the fibre industry and cotton ginning there are factories for the curing of bacon. Native industries include the weaving of cloth and the making of mats and baskets. Stone and lime quarries are worked, and copper is found in the Tsavo district. Diamonds have been discovered in the Thika river, one of the headstreams of the Tana.

Trade.—The imports consist largely of textiles, hardware and manufactured goods from India and Europe; Great Britain and India between them supplying over 50% of the total imports. Of other countries Germany has the leading share in the trade. The exports, which include the larger part of the external trade of Uganda, are chiefly copra, hides and skins, grains, potatoes, rubber, ivory, chillies, beeswax, cotton and fibre. The retail trade is largely in the hands of Indians. The value of the exports rose from £89,858 in 1900–1901 to £234,664 in 1904–1905, in which year the value of the imports for the first time exceeded £500,000. In 1906–1907 the volume of trade was £1,194,352, imports being valued at £753,647 and exports at £440,705. The United States takes 33% of the exports, Great Britain coming next with 15%.

Government.—The system of government resembles that of a British crown colony. At the head of the administration is a governor, who has a deputy styled lieutenant-governor, provincial commissioners presiding over each province. There are also executive and legislative councils, unofficial nominated members serving on the last-named council. In the “ten-mile strip” (see below, History), the sultan of Zanzibar being territorial sovereign, the laws of Islam apply to the native and Arab population. The extra-territorial jurisdiction granted by the sultan to various Powers was in 1907 transferred to Great Britain. Domestic slavery formerly existed; but on the advice of the British government a decree was issued by the sultan on the 1st of August 1890, enacting that no one born after that date could be a slave, and this was followed in 1907 by a decree abolishing the legal status of slavery. In the rest of the protectorate slavery is not recognized in any form. Legislation is by ordinances made by the governor, with the assent of the legislative council. The judicial system is based on Indian models, though in cases in which Africans are concerned regard is had to native customs. Europeans have the right to trial by jury in serious cases. There is a police force of about 2000 men, and two battalions of the King’s African Rifles are stationed in the protectorate. Revenue is derived chiefly from customs, licences and excise, railway earnings, and posts and telegraphs. Natives pay a hut tax. Since the completion of the Uganda railway, trade, and consequently revenue, has increased greatly. In 1900–1901 the revenue was £64,275 and the expenditure £193,438; in 1904–1905 the figures were: revenue £154,756, expenditure £302,559; in 1905–1906 the totals were £270,362 and £418,839, and in 1906–1907 (when the railway figures were included for the first time) £461,362 and £616,088. The deficiencies were made good by grants-in-aid from the imperial exchequer. The standard coin used is the rupee (16d.).

Education is chiefly in the hands of the missionary societies, which maintain many schools where instruction is given in handicrafts, as well as in the ordinary branches of elementary education. There are Arab schools in Mombasa, and government schools for Europeans and Indians at Nairobi.

History.—From the 8th century to the 11th Arabs and Persians made settlements along the coast and gained political supremacy at many places, leading to the formation of the so-called Zenj empire. The history of the coast towns from that time until the establishment of British rule is identified with that of Zanzibar (q.v.). The interior of what is now British East Africa was first made known in the middle of the 19th century by the German missionaries Ludwig Krapf and Johannes Rebmann, and by Baron Karl von der Decken (1833–1865) and others. Von der Decken and three other Europeans were murdered by Somali at a town called Bardera in October 1865, whilst exploring the Juba river. The countries east of Victoria Nyanza (Masailand, &c.) were, however, first traversed throughout their whole extent by the Scottish traveller Joseph Thomson (q.v.) in 1883–1884. In 1888 Count S. Teleki (a Hungarian) discovered Lakes Rudolf and Stefanie.

By the hinterland doctrine, accepted both by Great Britain and Germany in the diplomatic correspondence of July 1887, Uganda would fall within Great Britain’s “sphere of influence”; but German public opinion did not so regard the matter. German maps assigned the territory to Germany, while in England public opinion as strongly expected British influence to be paramount. In 1889 Karl Peters, a German official, led what was practically a raiding expedition into that country, after running a blockade of the ports. An expedition under F. J. Jackson had been sent by the company in the same year to Victoria Nyanza, but with instructions to avoid Uganda. In consequence of representations from Uganda, and of tidings he received of Peters’s doings, Jackson, however, determined to go to that country. Peters retired at Jackson’s approach, claiming, nevertheless, to have made certain treaties which constituted “effective occupation.” Peters’s treaty was dated the 1st of March 1890: Jackson concluded another in April. Meantime negotiations were proceeding in Europe; and by the Anglo-German agreement of the 1st of July 1890 Uganda was assigned to the British sphere. To consolidate their position in Uganda—the French missionaries there were hostile to Great Britain—the company sent thither Captain F. D. Lugard, who reached Mengo, the capital, in December 1890 and established the authority of the company despite French intrigues. In July 1890 representatives of the powers assembled at Brussels had agreed on common efforts for the suppression of the slave trade. The interference of the company in Uganda had been a material step towards that object, which they sought to further and at the same time to open up the country by the construction of a railway from Mombasa to Victoria Nyanza. But their resources being inadequate for such an undertaking they sought imperial aid. Although Lord Salisbury, then prime minister, paid the highest tribute to the company’s labours, and a preliminary grant for the survey had been practically agreed upon, the scheme was wrecked in parliament. At a later date, however, the railway was built entirely at government cost (supra, § Communications). Owing to the financial strain imposed upon it the company decided to withdraw Captain Lugard and his forces in August 1891; and eventually the British government assumed a protectorate over the country (see Uganda).

Further difficulties now arose which led finally to the extinction of the company. Its pecuniary interests sustained a severe blow owing to the British government—which had taken Zanzibar under its protection in November 1890—declaring (June 1892) the dominions of the sultanThe company and the crown. within the free trade zone. This act extinguished the treaties regulating all tariffs and duties with foreign powers, and gave free trade all along the coast. The result for the company was that dues were now swept away without compensation, and the company was left saddled with the payment of the rent, and with the cost, in addition, of administration, the necessary revenue for which had been derived from the dues thus abolished. Moreover, a scheme of taxation which it drew up failed to gain the approval of the foreign office.

On the 1st of July 1895 the formal transfer to the British crown of the territory administered by the company took place at Mombasa, the foreign office assuming responsibility for its administration. The territory, hitherto known as “Ibea,” from the initials of the company, was now styled the East Africa protectorate. The small sultanate of Witu (q.v.) on the mainland opposite Lamu, from 1885 to 1890 a German protectorate, was included in the British protectorate. Coincident with the transfer of the administration to the imperial government a dispute as to the succession to a chieftainship in the Mazrui, the most important Arab family on the coast, led to a revolt which lasted ten months and involved much hard fighting. It ended in April 1896 in the flight of the rebel leaders to German territory, where they were interned. The rebellion marks an important epoch in the history of the protectorate as its suppression definitely substituted European for Arab influence. “Before the rebellion,” says Sir C. Eliot, “the coast was a protected Arab state; since its suppression it has been growing into a British colony.”

From 1896, when the building of the Mombasa-Victoria Nyanza railway was begun, until 1903, when the line was practically completed, the energies of the administration were largely absorbed in that great work, and in establishing effective control over the Masai, Somali, and other tribes. The coast lands apart, the protectorate A white man’s country.was regarded as valuable chiefly as being the high road to Uganda. But as the railway reached the high plateaus the discovery was made that there were large areas of land—very sparsely peopled—where the climate was excellent and where the conditions were favourable to European colonization. The completion of the railway, by affording transport facilities, made it practicable to open the country to settlers. The first application for land was made in April 1902 by the East Africa Syndicate—a company in which financiers belonging to the Chartered Company of South Africa were interested—which sought a grant of 500 sq. m.; and this was followed by other applications for considerable areas, a scheme being also propounded for a large Jewish settlement.

During 1903 the arrival of hundreds of prospective settlers, chiefly from South Africa, led to the decision to entertain no more applications for large areas of land, especially as questions were raised concerning the preservation for the Masai of their rights of pasturage. In the carrying out of this policy a dispute arose between Lord Lansdowne, foreign secretary, and Sir Charles Eliot, who had been commissioner since 1900. The foreign secretary, believing himself bound by pledges given to the syndicate, decided that they should be granted the lease of the 500 sq. m. they had applied for; but after consulting officials of the protectorate then in London, he refused Sir Charles Eliot permission to conclude leases for 50 sq. m. each to two applicants from South Africa. Sir Charles thereupon resigned his post, and in a public telegram to the prime minister, dated Mombasa, the 21st of June 1904, gave as his reason:—“Lord Lansdowne ordered me to refuse grants of land to certain private persons while giving a monopoly of land on unduly advantageous terms to the East Africa Syndicate. I have refused to execute these instructions, which I consider unjust and impolitic.”[1]

On the day Sir Charles sent this telegram the appointment of Sir Donald W. Stewart, the chief commissioner of Ashanti, to succeed him was announced. Sir Donald induced the Masai whose grazing rights were threatened to remove to another district, and a settlement of the land claims was arranged. An offer to the Zionist Association of land for colonization by Jews was declined in August 1905 by that body, after the receipt of a report by a commissioner sent to examine the land (6000 sq. m.) offered. Sir Donald Stewart died on the 1st of October 1905, and was succeeded by Colonel Hayes Sadler, the commissioner of Uganda. Meantime, in April 1905, the administration of the protectorate had been transferred from the foreign to the colonial office. By the close of 1905 considerably over a million acres of land had been leased or sold by the protectorate authorities—about half of it for grazing purposes. In 1907, to meet the demands of the increasing number of white inhabitants, who had formed a Colonists’ Association[2] for the promotion of their interests, a legislative council was established, and on this council representatives of the settlers were given seats. The style of the chief official was also altered, “governor” being substituted for “commissioner”. In the same year a scheme was drawn up for assisting the immigration of British Indians to the regions adjacent to the coast and to Victoria Nyanza, districts not suitable for settlement by Europeans.

In general the relations of the British with the tribes of the interior have been satisfactory. The Somali in Jubaland have given some trouble, but the Masai, notwithstanding their warlike reputation, accepted peaceably the control of the whites. This was due, in great measure, to the fact that at the period in question plague carried off their cattle wholesale and reduced them for years to a state of want and weakness which destroyed their warlike habits. One of the most troublesome tribes proved to be the Nandi, who occupied the southern part of the plateau west of the Mau escarpment. They repeatedly raided their less warlike neighbours and committed wholesale thefts from the railway and telegraph lines. In September 1905 an expedition was sent against them which reduced the tribe to submission in the following November; and early in 1906 the Nandi were removed into a reserve. The majority of the natives, unaccustomed to regular work, showed themselves averse from taking service under the white farmers. The inadequacy of the labour supply was an early cause of trouble to the settlers, while the labour regulations enforced led, during 1907–1908, to considerable friction between the colonists and the administration.

For several years after the establishment of the protectorate the northern region remained very little known and no attempt was made to administer the district. The natives were frequently raided by parties of Gallas and Abyssinians, and in the absence of a defined frontier Abyssinian government posts were pushed south to Lake Rudolf. The Abyssinians also made themselves masters of the Boran country. After long negotiations an agreement as to the boundary line between the lake and the river Juba was signed at Adis Ababa on the 6th of December 1907, and in 1908–1909 the frontier was delimited by an Anglo-Abyssinian commission, Major C. W. Gwynn being the chief British representative. Save for its north-eastern extremity Lake Rudolf was assigned to the British, Lake Stefanie falling to Abyssinia, while from about 4° 20′ N. the Daua to its junction with the Juba became the frontier.

Bibliography.—The most comprehensive account of the protectorate to the close of 1904, especially of its economic resources, is The East Africa Protectorate, by Sir Charles Eliot (London, 1905). The progress of the protectorate is detailed in the Reports by the governor issued annually by the British government since 1896, and in Drumkey’s Year Book for East Africa (Bombay), first issued in 1908. The Précis of Information concerning the British East Africa Protectorate (issued by the War Office, London, 1901) is chiefly valuable for its historical information. The work of the Imperial British East Africa Company is concisely and authoritatively told from official documents in British East Africa or Ibea, by P. L. McDermont (new ed., London, 1895). Another book, valuable for its historical perspective, is The Foundation of British East Africa, by J. W. Gregory (London, 1901). Bishop A. R. Tucker’s Eighteen Years in Uganda and East Africa (London, 1908) contains a summary of missionary labours. Of the works of explorers Through Masai Land, by Joseph Thomson (London, 1886), is specially valuable. For the northern frontier see Capt. P. Maud’s report in Africa No. 13 (1904). For geology see, besides Thomson’s book, The Great Rift Valley, by J. W. Gregory (London, 1896); Across an East African Glacier, by Hans Meyer (London and Leipzig, 1890); and Report relating to the Geology of the East Africa Protectorate, by H. B. Muff (Colonial Office, London, 1908). For big game and ornithology see On Safari, by A. Chapman (London, 1908). The story of the building of the Uganda railway is summarized in the Final Report of the Uganda Railway Committee, Africa, No. 11 (1904), published by the British government.  (F. R. C.)

1. See Correspondence relating to the Resignation of Sir C. Eliot, Africa, No. 8 (1904).
2. The Planters and Farmers’ Association, as this organization was originally called, dates from 1903.