Pattimar. A model of the latter craft, primitive and Hindu, was
submitted to the British public during _the_ Great Exhibition. Rigged
barque-like, it is wondrous ark-like and uncouth. Baghlahs (she-mules)
and Ganjas (Ghancheh), from Cutch, are old tubs with low projecting
prows and elevated sterns, elaborately carved and painted. Low down in
the fore, their lean bows split like giant wedges the opposing waves,
which hiss and seethe as they fly past in broad arrow-heads. Dangerous
in heavy seas, these coffins are preserved by popular prejudice for the
antique and by the difficulty of choosing other models. Add sundry
Batelas, with poop-cabinets, closed and roomy, some with masts struck,
others ready to weigh anchor—I am not writing, gentle reader, a report
on Moslem naval architecture—and you have an idea of the outlandish
fleet, interesting withal, which bethrongs the port of Zanzibar.
The much-puffed squadron of the late Sayyid, stationed during his life
at Mto-ni, and now being divided amongst the rival heirs, flanks with
its single and double tiers of guns these peaceful traders, of whom, by-
the-by, some are desperate pirates. The number is imposing; but the
decks have no awnings against the weather, the masts are struck and
stripped to save rigging, the yards lie fore-and-aft upon the booms, the
crews consist of half-a-dozen thievish, servile ‘sons of water’ (M’áná
Májí); rats and cockroaches compose the live stock; the ammunition is
nowhere, and though the quarter and main decks are sometimes swept,
everything below is foul with garbage and vermin. The exteriors are
dingy; the interiors are so thoroughly rotted by fresh water that the
ships are always ready to go down at their anchors. The whole thing is a
mistake amongst Arabs, who are fitted only for a ‘buggalow,’ or at best
a ‘grab.’ The late Sayyid once attempted English sailors, who behaved
well as long as they did what they pleased, especially in the minor
matters of ’baccy and grog; but when the dark-faced skipper began loud
speaking and tall threats, they incontinently thrashed him upon his own
quarterdeck, and were perforce ‘dismissed the service.’ Every captain in
the R. N. Maskat, besides impudently falsifying the muster-rolls, will
steal the fighting-lanterns, the hammocks, and other articles useful at
home; whilst the care-takers sell in the bazar, junk, rope, and line;
copper bolts, brass-work, and carpenter’s chests bearing the government
mark. When a ship is wanted an Arab Nakhoda (here called Náhozá), a
Muallim or sailing-master, and a couple of Sukkanis (pilots), are sent
on board with a crew composed of a few Arab non-commissioned officers
and ‘able seamen,’ Baloch, Maskatis, and slaves. The commander, who
receives some 50 dollars per lunar month, kills time with the cognac
bottle; the sailing-master (7 dollars) dozes like a lap-dog in his own
arm-chair on the quarter-deck; and the seamen do nothing, Jack helping
Bill. One of these vessels sent to England a few years ago lost, by want
of provisions and bad water, 86 out of its crew—100 men; and can we
wonder at it? A single small screw-steamer, carrying a heavy gun, and
manned and commanded by Europeans, would have been more efficient in
warfare, and far more useful in peace, than the whole squadron of hulks.
It is, however, vain to assure the Arab brain that mere number is not
might; and, indeed, so it is when people believe in it.
The high and glassless windows of H. M.’s Consulate enable us to
prospect the city. Zanzibar, in round, numbers 6° south of the line,
occupies the western edge and about the midway length of the coral reef
that forms the island. The latter is separated by a Manche or channel
from the continent, a raised strip of blue land, broken by tall and
remarkable cones all rejoicing in names still mysterious enough to
flutter the traveller’s nerves. The inclination of the island from
N.N.W. to S.S.E. shelters the harbour from the Indian Ocean, whilst the
bulge of the mainland breaks the force of dangerous Hippalus, the S.W.
monsoon. The minimum breadth of the Manche is 16 geographical miles;
from the Fort to the opposite coast there are 24, and from the bottom of
Menai Bay 35. The Periplus gives to the Menouthian Channel about 300
stadia, in round numbers 30 geographical miles: 600 common stadia
correspond, within a fraction of the real measurement, with a degree of
latitude (1° = 1/360 of the earth’s circumference). Marinus of Tyre and
Ptolemy, however, unduly reduced the latter to 500 stadia.
Zanzibar city is built upon a triangular spit, breaking the line of its
wide, irregular, and shallow bay. The peninsula is connected with the
island by an isthmus some 300 yards wide, and it is backed by swamp and
lagoon, bush and forest. Arc-shaped, with the chord formed by the sea-
frontage, and the segment of the circle facing landwards, its greatest
length is from N.E. to S.W., and it is disposed beachways, like the sea-
ports of Oman. The front is a mere ‘dicky,’ a clean show concealing
uncleanness. Instead, however, of a neat marine parade and a T-shaped
pier, the foreground is a line of sand fearfully impure. Corpses float
at times upon the heavy water; the shore is a cess-pool, and the younger
blacks of both sexes disport themselves in an absence of costume which
would startle even Margate. Round-barrelled bulls, the saints of the
Banyans, and therefore called by us ‘Brahmani,’ push and butt, by way of
excitement, the gangs of serviles who carry huge sacks of cowries, and
pile high their hides and logwood. Others wash and scrape ivory, which
suggested to a young traveller the idea that the precious bone, here so
plentiful, is swept up by the sea. At night the front often flares as if
on fire. The cause is lime-burning on the shore, in small, round, built-
up heaps.
Another evil, arising from want of quay and breakwater, is that the sea
at times finds its way into the lower parts of the town. The nuisance
increases, as this part of the Island appears to be undergoing
depression, not an uncommon process in fictile madrepore formations. Off
Changáni Point, where in 1823 stood a hut-clump and a mosque, four
fathoms of water now roll. The British Consulate, formerly many yards
distant from the surf, must be protected by piles and rubble. Some of
the larger houses have sunk four, and have sloped nine feet from terrace
to ground, owing to the instability of their soppy foundations. The
‘Tree-island’ of our earliest charts has been undermined and carried
away bodily by the waves; whilst to the north the sea has encroached
upon Mto-ni, where the Sayyid’s flag-staff has four times required
removal. On the other hand, about 15 years ago, the ‘Middle Shoal’ of
the harbour was awash; now it is high and dry.
In 1835 Dr Ruschenberger estimated the census of Zanzibar at 12,000
souls, of whom two-thirds were slaves. In 1844 Dr Krapf proposed 100,000
as the population of the island, the greater number living in the
capital. Captain Guillain, in 1846, gave 20,000 to 25,000, slaves
included. I assumed the number, in 1857, as 25,000, which during the
N.E. monsoon, when a large floating population flocks in, may rise to
40,000, and even to 45,000. The Consular report of 1849 asserts it to be
‘about 60,000.’
The city is divided into 18 quarters (Mahallat), each having its own
name; and when travellers inform us that it is called ‘Hamuz,’ Moafilah,
or Baur, they simply take a part for the whole.[21] The west-end boasts
the best houses, chiefly those which wealthy natives let to stranger
merchants. The Central, or Fort quarter, is the seat of government and
of commerce, whilst few foreigners inhabit the eastern extremities, the
hottest and the most unhealthy. The streets are, as they should be under
such a sky, deep and winding alleys, hardly 20 feet broad, and
travellers compare them with the threads of a tangled skein. In the
west-end a pavement of Chunam, or tamped lime, is provided with a
gutter, which secures dryness and cleanliness—it is the first that I
have seen in an African city. As we go eastward all such signs of
civilization vanish; the sun and wind are the only engineers, and the
frequent green and black puddles, like those of the filthy Ghetto, or
Jews’ quarter, at Damascus, argue a preponderance of black population.
Here, as on the odious sands, the festering impurities render strolling
a task that requires some resolution, and the streets are unfit for a
decent (white) woman to walk through. I may say the same of almost every
city where the negro element abounds.
As in the coast settlements of the Red Sea and of Madagascar, the house
material is wholly coral rag, a substance at once easily worked and
durable—stone and lime in one. The irregularity of the place is
excessive, and it is by no means easy to describe its peculiar
physiognomy. The public buildings are poor and mean. The mosques which
adorn Arab towns with light and airy turrets, breaking the monotony of
square white tenements, magnified claret-chests, are here in the
simplest Wahhabi form. About 30 of these useful, but by no means
ornamental, ‘meeting-houses’ are scattered about the city for the use of
the ‘established church.’ They are oblong rooms, with stuccoed walls,
and matted floors; the flat roofs are supported by dwarf rows of square
piers and polygonal columns; whilst Saracenic arches, broad, pointed,
and lanceated, and windows low-placed for convenience of expectoration,
with inner emarginations in the normal shape of scallops or crescents,
divide the interior. Two Shafei mosques, one called after Mohammed Abd
el Kadir, the other from Mohammed el Aughan (Afghan), have minarets,
dwindled turrets like the steeples of Brazilian villages; another boasts
of a diminutive cone, most like an Egyptian pigeon-tower; and a fourth
has a dwarf excrescence, suggesting the lantern of a light-house. The
Shiahs, who are numerous, meet for prayer in the Kipondah quarter, and
the Kojahs have a ruined mosque outside the city.
The best houses are on the Arab plan familiar to travellers in Ebro-land
and her colonies. The type has extended to France and even to Galway,
where we still find it in the oldest buildings. A dark narrow entrance
leads from the street, and the centre of the tenements is a hypæthral
quadrangle, the Iberian Patio or Quintal. We miss, however, the shady
trees, the sweet flowers, and bright verdure with which the southern
European and the Hispano-American beautify their dwellings. Here the
‘Dár’ is a dirty yard, paved or unpaved, usually encumbered with piles
of wood or hides, stored for sale, and tenanted by poultry, dogs,
donkeys, and lounging slaves. A steep and narrow, dark and dangerous
staircase of rough stone, like a companion-ladder, connects it with the
first floor, the ‘noble-quarter.’ There are galleries for the several
storeys, and doors opening upon the court admit light into the rooms.
Zanzibarian architecture, as among ‘Orientals’ generally, is at a low
ebb. The masonry shows not a single straight line; the arches are never
similar in form or size; the floors may have a foot of depression
between the middle and the corners of the room; whilst no two apartments
are on the same level, and they seldom open into each other. Joiner’s
work and iron-work must both be brought from India.
The ‘azotéas’[22] flat roofs, or rather terraces, are supported by
mangrove-trunks, locally called ‘Zanzibar rafters,’ and the walls, of
massive thickness, are copiously ‘chunam’d.’ Here the inmates delight to
spread their mats, and at suitable seasons to ‘smell the air.’ Bándá or
bándáni, pent-roofed huts of plaited palm-leaf (makuti or cajan) garnish
the roofs of the native town. Europeans do not patronize these look-
outs, fires being frequent and the slaves dangerous. Some foreigners
have secured the comfort of a cool night by building upper cabins of
planking, and have paid for the enjoyment in rheumatism, ague, and
fever.
Koranic sentences on slips of paper, fastened to the entrances, and an
inscription cut in the wooden lintel, secure the house from witchcraft,
like the crocodile in Egypt; whilst a yard of ship’s cable drives away
thieves. The higher the tenement, the bigger the gateway, the heavier
the padlock, and the huger the iron studs which nail the door of heavy
timber, the greater is the owner’s dignity. All seems ready for a state
of siege. Even the little square holes pierced high up in the walls, and
doing duty as ventilators, are closely barred. As heat prevents the use
of glass in sleeping-rooms, shutters of plain or painted plank supply
its place, and persiennes deform the best habitations. The northern
European who sleeps for the first time in one of these blockhouses
fairly realizes the first sensations of a jail. Of course the object is
defence, therefore the form is still common to Egypt and Zanzibar, Syria
and Asia Minor.
Arabs here, as elsewhere, prefer long narrow rooms (40 feet × 15 to 20),
generally much higher than their breadth, open to the sea-breeze, which
is the health-giver; and they close the eastern side-walls against the
‘fever-wind,’ the cool, damp, spicy land-draught. The Sala or reception-
hall is mostly on the ground-floor. It contrasts strongly with our
English apartments, where the comfortless profusion and confusion of
furniture, and where the undue crowding of ornamental ornaments, spoil
the proportions and ‘put out’ the eye. The protracted lines of walls and
rows of arched and shallow niches, which take the place of tables and
consoles, are unbroken save by a few weapons. Pictures and engravings
are almost unknown; chandeliers and mirrors are confined to the wealthy;
and the result, which in England would be bald and barn-like, here
suggests the coolness and pleasing simplicity of an Italian villa—in
Italy. A bright-tinted carpet, a gorgeous but tasteful Persian rug for
the daïs, matting on the lower floor, which is of the usual chunam; a
divan in old-fashioned houses; and, in the best of the modern style,
half a dozen stiff chairs of East Indian blackwood or China-work,
compose the upholstery of an Arab ‘palazzo.’ In the rooms of the few who
can or will afford such trifles, ornaments of porcelain or glassware,
and French or Yankee knicknacks fill the niches. Of course the inner
apartments are more showily dressed, but these we may not explore.
About half way down the front of the city we debouch upon the ‘Gurayza’
or fort. The material is the usual coral-rag, cemented with lime of the
same formation, rudely burnt, and the style as well as the name (Igreja-
Ecclesia) recall to mind the Portuguese of the heroic sixteenth century.
It is one of those naïve, crenelated structures, flanked by polygonal
towers, each pierced for one small gun, and connected by the
comparatively low curtains, in which our ancestors put their trust. A
narrow open space runs round it, and it is faced by a straight-lined
detached battery, commanding the landing, and about 12 yards long. The
embrasures of this outwork are so close that the first broadside would
blow open the thin wall; and the score of guns is so placed that every
bullet striking the fort must send a billet or two into the men that
serve them. A ‘_place d’armes_,’ about 50 feet wide, divides the two,
and represents the naval and military arsenal—two dozen iron carronades
lying piled to the right of the first entrance, and as much neglected
and worm-eaten as though they belonged to our happy colony, Cape Coast
Castle. Amongst the guns of different calibre we find a few fine old
brass pieces, one of which bears the dint of a heavy blow. They are
probably the plunder of Hormuz or of Maskat, where the small matter of a
‘piece of ham wrapped up in paper’[23] caused, in the middle of the
seventeenth century, a general massacre of the Portuguese.’
The gateway is the usual intricate barbican. Here in olden times, after
the prayers of el Asr (3 p.M.) the governor and three judges, patriarchs
with long grey beards, unclean white robes, and sabres in hand, held
courts of justice, and distributed rough-and-ready law to peaceful
Banyans, noisy negroes, and groups of fierce Arabs. The square bastion
projecting from the curtain now contains upper rooms for the Baloch
Jemadar (commandant). The ground-floor is a large vestibule, upon whose
shady masonry-benches the soldiery and their armed slaves lounge and
chat, laugh and squabble, play and chew betel. On the left of the outer
gate is a Cajan shed, where native artists are setting up carriages for
the guns whose lodging is now the hot ground. The experiment of firing a
piece was lately tried; it reared up and fell backwards, smashing its
frail woodwork and killing two artillery ‘chattels.’
Travellers have observed that a launch could easily dismantle this
stronghold. It was once, the legend runs, attacked and taken by a single
‘Jack,’ for the honour of whose birthplace Europe and America vainly
contend. Determined to liberate two brother-tars from the ignoble
bilboes, he placed himself at the head of a party consisting of a
Newfoundland dog. He fell upon the guard _sabre au poing_, and, left
master of the field, he waved his bandanna in vinous triumph from the
battlements. Sad to relate, this Caucasian hero succumbed to Hamitic
fraud. The discomfited slaves rallied. Holding a long rope, they ran
round and round the enemy, till, wound about like a windlass or a silk
cocoon, he was compelled to surrender at discretion.
The interior of the fort is jammed with soldiers’ huts, and divided into
courts by ricketty walls. Here, too, is the only jail in Zanzibar. The
stocks (Makantarah), the fetters, the iron collars, and the heavy waist-
chains, do not prevent black man from conversationizing, singing comic
songs, and gambling with pebbles. The same was the case with our gruel-
houses—‘Kanji-Khanah,’ vulgò ‘Conjee-Connah’—in British India. The
Sepoys laughed at them and at our beards. The Bombay Presidency jail is
known to Arabs as El Bistan (El Bostan, the Garden), because the courts
show a few shrubs, and with Ishmaelites a ‘Bistan’ has ever an _arrière
pensée_ of Paradise. But the most mutinous white salt that ever floored
skipper would ‘squirm’ at the idea of a second night in the black-hole
of Zanzibar. Such is the Oriental beau-ideal of a prison—a place whose
very name should develope the goose-skin, and which the Chinese
significantly call ‘hell.’
In my day foreigners visited the prison to see its curio, a poor devil
cateran who had beaten the death-drum whilst his headman was torturing
M. Maizan. An Arab expedition sent into the interior returned with this
wretch, declaring him to be the murderer in chief, and for two years he
lay chained in front of the French Consulate. Since 1847 he was heavily
ironed to a gun, under a mat-shed, where he could neither stand up nor
lie down. The fellow looked fat and well, but he died before our return
from the interior in 1859.
Below the eastern bastion of the ‘Gurayza’ is the most characteristic
spot in Zanzibar city, the Salt Market, so called from the heaps of
dingy saline sand offered for sale by the Maskati Arabs and the
Mekranis. Being near the Custom House, it is always thronged, and like
the bazars of Cairo and Damascus it gives an exaggerated idea of the
population. There are besides this three other ‘Suk.’ The Suk Muhogo, or
Manioc market, to the south of the city, supplies the local staff of
life. It is the sweet variety of Jatropha, called in the Brazil Aypim,
or Macacheira, and known to us as white cassava: it will not make wood-
meal, called κατ’ ἔξοχην, farinha, the flour. The poisonous Manioc
(Jatropha Manihot) must be soaked in water, or rasped, squeezed, and
toasted, to expel its deleterious juice, which the Brazilian ‘Indians,’
and the people of the Antilles, convert by boiling into sugar, vinegar,
and cassareep for ‘pepper-pot’—I heard of this ‘black cassava’ in inner
East Africa. The Suk Muhogo sells, besides the negro’s daily bread,
cloth and cotton, grain and paddy, vegetables, and other provisions. The
shops are the usual holes in the wall, raised a foot above the street,
and the owners sit or squat, writing upon a knee by way of desk, with
the slow, absorbing reed-pen and the clotted clammy fluid called ink.
Behind, and hard by, is the fish-market, which is tolerably supplied
between 4 and 6 p.m.—in the morning you buy the remnants of the last
day. Further eastward, in the Melindini quarter, is the Suk Melindi,
where the butchers expose their vendibles. As in most hot countries, the
best articles are here sold early, at least before 7 a.m. A scarcity of
meat is by no means rare at Zanzibar, and sometimes it has lasted four
or five months.
In the Furzani quarter, eastward of and close to the salt bazar, stands
the Custom House. This is an Arab bourse, where millions of dollars
annually change hands under the foulest of sheds, a long, low mat-roof,
supported by two dozen rough tree-stems. From the sea it is conspicuous
as the centre of circulation, the heart from and to which twin streams
of blacks are ever ebbing and flowing, whilst the beach and the waters
opposite it are crowded with shore-boats, big and small. Inland, it is
backed by sacks and bales, baskets and packages, hillocks of hides, old
ship’s-tanks, piles of valuable woods, heaps of ivories, and a
heterogeneous mass of waifs and strays; there is also a rude lock-up,
for ware-housing the more valuable goods. A small adjacent square shows
an unfinished and dilapidated row of arches, the fragments of a new
Custom House. It was begun 26 or 27 years ago (1857), but Jayaram, the
benevolent and superstitious Hindu who farmed the customs it is said for
$150,000 per annum, had waxed fat under the matting, and was not sure
that he would thrive as much within stone and lime. This is a general
idea throughout the nearer East. The people are full of saws and
instances concerning the downfall of great men who have exposed
themselves to the shafts of misfortune by enlarging their gates or by
building for themselves two-storeyed abodes. But the hat it seems has
lately got the better of the turban, and there will be a handsome new
building, half paid by the Prince and half by his farmer of Customs.
An open space now leads us to the finest building in the city, the
palace of the late Sayyid, which we visit in a future chapter. I may
remark that it is the workhouse style, though hardly so ignoble as that
of H. Hellenic Majesty; but at Zanzibar the windows are far higher up,
and the jail-like aspect is far more pronounced. Beyond it commences the
east-end, and here lives my kind friend M. Cochet, Consul de France. He
came, expecting to find civilization, whist in the evening, ladies’
society, and the pianoforte: he had been hoaxed in Paris about Colonel
Hamerten’s daughters. He is thoroughly disgusted. Even the Consular
residence is the meanest of its kind. No wonder that M. Le Capitaine
Guillain was ‘froissé dans son amour-propre national’ when he entered
it.
Far better, and more open to the breeze, is the house of the hospitable
M. Bérard, agent to Messrs Rabaud Frères, of Marseille. The one
disadvantage of the site is the quantity of Khoprá, or cocoa-nut meat,
split and sun-dried. It evolves, especially at night-time, a noxious
gas, and the strongest stomachs cannot long resist the oily, nausea-
breeding odour which tarnishes silver, and which produces fatal
dysentery. The Zanzibar trade, with the exception of cloves, is not
generally aromatic. Copal, being washed in an over-kept solution of
soda, smells not, as was remarked to the ‘Dragon of Wantley,’ like
balsam. And ton upon ton of cowries, strewed in the sun, or piled up in
huge heaps till the mollusc decays away, can hardly be deemed Sabæan or
even commonly wholesome.
To our right, in rear of the fronting ‘dicky,’ and at both flanks of the
city, is the native town,—a filthy labyrinth, a capricious arabesque of
disorderly lanes, and alleys, and impasses, here broad, there narrow;
now heaped with offal, then choked with ruins. It would be the work of
weeks to learn the threading of this planless maze, and what white man
would have the heart to learn it? Curiosity may lead us to it in
earliest morning, before the black world returns to life. During the day
sun or rain, mud or dust, with the certain effluvia of carrion and
negro, make it impossible to flâner through the foul mass of densely
crowded dwelling-places where the slaves and the poor ‘pig’ together.
The pauper classes are contented with mere sheds, and only the mildness
of the climate keeps them from starving. The meanest hovels are of palm-
matting, blackened by wind or sun, thatched with cajan or grass, and
with or without walls of wattle-and-dab. They are hardly less wretched
than the west Ireland shanty. Internally the huts are cut up into a
‘but’ and a ‘ben,’ and are furnished with pots, gourds, cocoa rasps, low
stools hewn out of a single block, a mortar similarly cut, trays, pots,
and troughs for food, foul mats, and kitandahs or cartels of palm-fibre
rope twisted round a frame of the rudest carpenter’s work. The better
abodes are enlarged boxes of stone, mostly surrounded by deep,
projecting eaves, forming a kind of verandah on poles, and shading
benches of masonry or tamped earth, where articles are exposed for sale.
The windows are loop-holes, and the doors are miracles of rudeness.
Lastly, there are the wretched shops, which supply the few wants of the
population.
We are now at the mouth of the Lagoon, which, at high tides, almost
encircles the city. I am told that of late years the natives have built
all round this backwater. In 1857 the Eastern or landward side was hush
and plantation. As the waters retired they left behind them a rich
legacy of fevers and terrible diseases; especially in the inner town, a
dead flat, excluded from the sea breeze, and exposed to the pestiferous
breath of the maremma.
Ships anchoring off this inlet soon stock French Islet. The whalers and
American and Hamburg vessels, that prefer Changáni Point and the west
end of the city, often escape without a single case of sickness.
Similarly at Havannah, crews exposed to breezes from the Mangrove swamps
have lost half their numbers by yellow fever; and the history of our
West Indian settlements proves, if proof be required, how fatal is night
exposure.
Zanzibar, city and island, is plentifully supplied with bad drinking
water. Below the old sea-beach, and near the shore, it is necessary only
to scrape a hole in the soft ground. Throughout the interior the wells,
though deep, are dry during the hot season, and the people flock to the
surface-draining rivulets. West Africans generally will not drink rain-
water for fear of dysentery; and so with us—when showers fell in large
drops men avoided it, or were careful to consume it soon lest it should
putrefy. The purest element is found at Kokotoni, a settlement on the N.
W. coast of the island, and in the Bububu, a settlement some five miles
north of the city, where Sayyid Suleyman bin Hamid, once governor of
Zanzibar, had a small establishment, and where Hasan bin Ibrahim built a
large house called Chuweni or Leopard’s Place. So at São Paulo de Loanda
the drinking water must be brought from the Bengo river. The best near
the city is from a spring which rises behind the royal Cascine, Mto-ni.
Here the late Sayyid built a stone tank and an aqueduct 2000 yards long,
which, passing through his establishment, came out upon the beach. Casks
could then be filled by the hose, but soon the masonry channel got out
of repair, and sailors will not willingly drink water flowing through a
dwelling-house.
The produce of the town greatly varies. Some wells are hard with
sulphate and carbonate of lime, whilst others are salt as the sea
itself; and often, as in Sind and Cutch, of two near together one
supplies potable and the other undrinkable water. A few to the south of
the city are tolerably sweet. The pits are numerous, and a square shaft,
usually from 12 to 15 feet deep, may be found at every 40 or 50 yards.
There are no casings; the edges are flush with the filthy ground about
them, and the sites must frequently be changed, as the porosity of the
coral rock and the regular seaward slope direct the drainage into them.
Similarly, nearer home the bright sparkling element is not unfrequently
charged with all the seeds of disease. When rain has not fallen for some
time the water becomes thick as that of a horsepond, and when allowed to
stand it readily taints. I could hardly bear to look at the women as
they filled with cocoa-shells the jars to be carried off upon their
heads.
Formerly Europeans were not allowed, for religious reasons, to ship
water from the wells near the town. Also, cask-filling was carried on at
low tide, to prevent the supply of the Mto-ni being brackish, and the
exhalations of the black mud were of course extra-dangerous. It is no
wonder that dysentery and fever resulted from the use of such a
‘necessary.’ The French frigate Le Berceau, after watering here, was
visited by the local pest, and lost 90 men on her way home. Even in
January, the most wholesome month, Lieut. Christopher had 16 deaths
amongst his scanty crew. In this case, however, the lancet, so fatal
near the Line, and the deadly Zerámbo, or toddy-brandy, were partly to
blame. As early as 1824 Captain Owen condemned the supply of Zanzibar,
as liable to cause dysentery. It has this effect during and after heavy
rains, unless allowed to deposit its animal and vegetable matter. During
the second visit of H. M. S. Andromache, in August, 1824, Commander
Nourse and several of his officers spent one night in a country house,
after which the former and the greater number of the latter died. The
water, as well as the air, doubtless tended to cause the catastrophe. In
the dry season the element sometimes produces, according to natives and
strangers, obstinate costiveness. Between Zanzibar and the Cape, five
brigs lost collectively 125 men from fever, dysentery, and inflammation
of the neck of the vesica; whilst others were compelled to start their
casks, and to touch at different ‘aguadas’ en route. Hence skippers
learned to fear and shun Zanzibar. During her 14 months’ exploration of
the island and the coast the Ducouëdic lost 16 men; and to keep up a
crew of 122 to 128, no less than 226 hands were transferred to her from
the naval division of Bourbon and Madagascar. Each visit to Unguja was
followed by an epidemic attack. Formerly as many as seven whalers lay in
harbour at one time; now (1857) they prefer to water and refresh at
Nossi-beh, Mayotta, and especially at the Seychelles, a free port, with
a comparatively cool and healthy climate, where supplies are cheap and
plentiful.
Besides the lagoon and the water nuisances there is yet another. The
drainage of the Zanzibar water-front is good, owing to the slope of the
site seaward. But at low tides, and after dark, when the sulphuretted
hydrogen is not raised from the sands by solar heat, a veil of noxious
gas overhangs the shore, whose whole length becomes exceedingly
offensive. This is caused by the shironi (latrinæ) opening upon the
water edge. ‘Intermural sepulture’ is also here common, though not after
the fashion of West African Yoruba; and the city contains sundry
unenclosed plots of ground, in which dwarf lime-plastered walls, four to
five feet long, fancifully terminated above, and showing, instead of
epitaph, a china saucer or bits of porcelain set in the stone, denote
tombs.
Drainage and cleanliness are panaceas for the evils of malaria where
tropical suns shine. Drainage of swamps and lagoons can improve S’a
Leone, and can take away the stink from South African barracks. Zanzibar
city, I contend, owes much of its fatality to want of drainage, and it
might readily be drained into comparative healthiness. But the East
African Arab holds the possibility of pestilence and the probability of
fever to be less real evils than those of cutting a ditch, of digging a
drain, or of opening a line for ventilation. The Dollar-hunters from
Europe are a mere floating population, ever looking to the deluge in
prospect, and of course unwilling to do every man’s business, that is—to
drain.
Such was Zanzibar city when I first walked through it. Though dating
beyond the days of Arab history, and made, by its insular and central
situation, the depôt of the richest trade in Eastern Africa, its present
buildings are almost all modern. At the beginning of this our nineteenth
century it consisted of a fort and a ragged line of huts, where the ‘Suk
Muhogo’ now stands. Dr Ruschenberger (1835) satisfied himself that ‘the
town of Zanzibar and its inhabitants possess as few attractions for a
Christian stranger as any place and people in the wide world.’ As late
as 1842 this chief emporium of a most wealthy coast boasted but five
store-houses of the humblest description, and the east end was a palm
plantation. Since my departure the city, as the trade returns show, has,
despite unfavourable political circumstances, progressed. A Catholic
mission, sent by France, has established an hospital, and two schools
for boys and girls, and the English Central African Mission has followed
suit. These establishments must differ strangely from the normal thing—
the white-bearded pedagogue, hugging his bones or rocking himself before
a large chintz-covered copy of the Koran, placed upon a stand two feet
high, so as to be above man’s girdle, and, when done with, swathed in
cloth and stowed away. A change, too, there must be in the pupils;
formerly half a dozen ragged boys, some reciting with nasal monotonous
voices sentences to be afterwards understood by instinct, others
scraping the primitive writing-board with a pointed stick.
We will now return to the centre of attraction, the Salt Bazar, and
prospect the people. The staple material is a double line of black youth
and negresses sitting on the ground, with legs outstretched like
compasses. At each apex of the angle is a little heap of fruit, salt,
sugar, sun-dried manioc, greasy fritters, redolent fish, or square
‘fids’ of shark-flesh,[24] the favourite ‘kitchen’ with Wasawahíli and
slaves; it brings from Maskat and the Benadir a goût so high that it
takes away the breath. These vendors vary the tedium of inaction by mat-
making, plaiting leaves, ‘palavers,’ and ‘pow-wows,’ which argue an
admirable conformation of the articulating organs and a mighty lax
morality. Sellers, indeed, seem here to double the number of buyers, and
yet somehow buying and selling goes on.
Motley is the name of the crowd. One officer in the service of His
Highness stalks down the market followed by a Hieland tail, proudly, as
if he were lord of the three Arabias. Negroes who dislike the whip clear
out like hawk-frightened pigeons. A yellow man, with short, thin beard,
and high, meagre, and impassive features, he is well-dressed and
gorgeously armed. Observe that he is ‘breek-less’: trowsers are ‘un-
Arab,’ and unpopular as were the servile braccæ amongst the Romans. The
legs, which, though spare are generally muscular and well-turned, appear
beneath the upper coat, which falls to the knee. He adheres to the
national sandals, thick soles of undyed leather, with coloured and
spangled straps over the instep, whilst a narrow thong passes between
the big toe and its neighbour. The foot-gear gives him that peculiar
strut which is deemed dignified, and if he has a long walk before him—a
very improbable contingency—he must remove his chaussure. I never yet
saw a European who could wear the sandal without foot-chafing.
Right meek by the side of the Arab’s fierceness appears the Banyan, the
local Jew. These men are Bhattias from Cutch in western India; unarmed
burghers, with placid, satisfied countenances, and plump, sleek, rounded
forms, suggesting the idea of happy, well-to-do cows. Such is the effect
of a diet which embraces only bread, rice, and milk, sweetmeats,
vegetables, and clarified butter. Their skins are smoother and their
complexions are lighter than the Arabs’; their features are as high
though by no means so thin. They wear the long mustachio, not the beard,
and a Chinese pig-tail is allowed to spring from the poll of the
carefully shaven head. These top-knots are folded, when the owners are
full-dressed, under high turbans of spotted purple or crimson stuff
edged with gold. The latter are complicated affairs, somewhat suggesting
the oldest fashion of a bishop’s mitre; bound round in fine transverse
plaits, not twisted like the Arabs’, and peaked in the centre above the
forehead with a manner of horn. Their snowy cotton coats fit close to
the neck, like collarless shirts; shawl-girt under the arms, they are
short-waisted as the dresses of our grandmothers; the sleeves are tight
and profusely wrinkled, being nearly double the needful length, and the
immaculate loin-cloth displays the lower part of the thigh, leaving the
leg bare. Their slippers of red leather are sharp-toed, with points
turning upwards and backwards, somewhat as in the knightly days of
Europe.
Another conspicuous type is the Baloch mercenary from Mekran or Maskat.
A comely, brown man, with regular features, he is distinguished from the
Arab by the silkiness and the superior length of his flowing beard,
which is carefully anointed after being made glossy with henna and
indigo. He adheres to his primitive matchlock, a barrel lengthened out
to suit the weak powder in use, damascened with gold and silver, and
fastened to the frail stock by more metal rings than the old French
‘Brown Bess’ ever had. The match is about double the thickness of our
whipcord, and is wound in many a coil round the stalk or stock. A curved
iron, about four inches long, and forked in the upper part to hold the
igniter, plays in a groove cut lengthways through the wood and the
trigger, a prolongation of the match-holder, guides the fire into the
open priming-pan. When the match is not immediately wanted it is made
fast to a batten under the breeching. (A parenthesis. Were I again to
travel in wet tropical lands, I should take with me two flint-guns,
which could, if necessary, be converted into matchlocks. Of course they
would shoot slow, but they would not want caps, and they would prove
serviceable when the percussion gun and the breech-loader would not.)
This mercenary carries also two powder-gourds, one containing coarse
material for loading, the other a finer article, English, if possible,
for priming. He is never without flint, steel, and tinder; and disposed
about his person are spare cartridges in reed cases. His sabre is of the
Persian form; his dagger is straighter and handier than that of the
Arab; and altogether his tools, like his demeanour, are those of a
disciplined, or rather of a disciplinable, man.
The wildest and most picturesque figures are the half-breeds from the
western shores of the Persian Gulf—light brown, meagre Ishmaels and
Orsons, who look like bundles of fibre bound up in highly-dried human
skin. Their unkempt elf-locks fall in mighty masses over unclean,
saffron-stained shirts, which suggest the ‘night-gown’ of other days,
and these are apparently the only articles of wear. Their straight,
heavy swords hang ever ready by a strap passing over the left shoulder;
their right hands rest lovingly upon the dagger-hafts, and their small
round targes of boiled hippopotamus hide—one of the ‘industries’ of
Zanzibar—apparently await immediate use. Leaning on their long
matchlocks, they stand cross-legged, with the left foot planted to the
right of the right, or vice versâ, and they prowl about like beasts of
prey, as they are, eyeing the peaceful, busy crowd with a greedy cut-
throat stare, or with the suspicious, side-long glance of a cat o’
mountain.
These barbarian ‘Gulf Arabs’ differ singularly from the muscular porters
of Hazramaut, in whose Semitic blood there is a palpable African
mixture. They hobble along in pairs, like the Hammals of Constantinople,
carrying huge bales of goods and packs of hides suspended from a pole,
ever chaunting the same monotonous grunt-song, and kicking out of the
way the humped cows that are munching fruit and vegetables under the
shadow of their worshippers, the Banyans. Add half a dozen pale-skinned
‘Khojahs,’ tricky-faced men with evil eyes, treacherous smiles, fit for
the descendants of the ‘Assassins,’ straight, silky beards, forked after
the fashion of ancient Rustam, and armed with Chinese umbrellas.
Complete the group by throwing in a European—how ghastly appears his
blanched face, and how frightful his tight garb!—stalking down the
streets in the worst of tempers, and using his stick upon the mangy
‘pariah dogs’ and the naked shoulders of the ‘niggers’ that obstruct
him. At times the Arabs, when their toes or heels are trampled upon,
will turn and fiercely finger their daggers; but a fear which is by no
means personal prevents their going further.
Such is the aristocracy of the land. As in all servile societies, every
white man (i.e. non-negro) is his white neighbour’s equal; whilst the
highest black man (i.e. servile) ranks below the lowest pale-face.
Far more novel to us is the slave population, male and female. What
first strikes every stranger is the scrupulous politeness and the
ceremonious earnestness of greetings when friends meet. The idea of
standing in the broiling sun to dialogue as follows is not a little
remarkable:
_A._ Yambo (pronounced Dyambo) or Hali gáná?—The state!
_B._ Yambo Sáná—My state is very (good).
_A._ Siyambo (or amongst the Arabized Wasawahíli, Marhabá)—Right
welcome!
_B._ Hast thou eaten and slept?
_A._ I have made my reverential bow!
_B._ Yambo?
_A._ Siyambo Sáná!
_B._ Like unto gold?
_A._ Like unto gold!
_B._ Like unto coral?
_A._ Like unto coral!
_B._ Like unto pearl?
_A._ Like unto pearl!
_B._ The happiness—Kua-heri! (farewell!).
_A._ In happiness let us meet, if Allah please!
_B._ Hem!
_A._ Hem! (drawn out as long as possible).
The fact is they are going about ‘Ku amkía,’ to salute their friends,
and to waste time by running from house to house. Even freemen generally
begin their mornings thus, and idle through the working hours.
The males tie, for only garb, a yard of cotton round the waist, and let
it fall to the knees; bead necklaces and similar trash complete the
costume. Like all negroes they will wear, if possible, the shock-head of
wool, which is not pierceable by power of any sun; and they gradually
unclothe down to the feet, which, requiring most defence, are the least
defended—‘Fashion’ must account for the anomaly. To the initiated eye
the tattoo distinguishes the vast confusion of races. The variety of
national and tribal marks, the stars, raised lumps and scars, the
beauty-slashes and carved patterns, further diversified by the effects
of pelagra, psoris, and small-pox, is a Chinese puzzle to the new-comer.
Domestic slaves, bearing their burdens on the head, not on the shoulder,
are known by a comparatively civilized aspect. They copy their masters,
and strangers remark that the countenance is cheerful and not destitute
of intelligence. The Bozals, or freshly-trapped chattels, are far more
original and interesting. See those Nyassa-men, with their teeth filed
to represent the cat or the crocodile, chaffing some old Shylock, an
Arab dealer in human flesh and blood; or those wild Uzegura-men, with
patterned skins and lower incisors knocked out, like the Shilluks to the
west of the Nile, scowling evilly, and muttering curses at the Nakhuda
(skipper) from Súr, the professional kidnapper of their kind.
The ‘fairer’ half of black world is not less note-worthy. There is the
tall and sooty-skinned woman from Uhiáo, distinguished by the shape of
her upper lip. A thorn-pierced hole is enlarged with stalks of green
reed till it can admit a disk of white-painted wood nearly as big as a
dollar. The same is the system of the Dors, the tribe dwelling north of
the equator and west of the Nile; their lip-plates equal the thick end
of a cheroot; and the ‘pelele’ of the southern regions is a similar disk
of bamboo, ivory, or tin, which causes the upper lip to project some two
inches beyond the nose-tip, giving it an anserine proportion. In the
elder women the ornament is especially hideous. As a rule, the South
American ‘Indians’ pierce for their labrets the lower lip, evidently the
more unclean fashion—no wonder that kissing (should I say osculation?)
is unknown. Yet even amongst the Somal, if you attempt to salute a
woman—supposing that you have the right—she will draw back in horror
from the act of incipient cannibalism. Often the lip-disk is absent, and
then through the unsightly gap a pearly tooth is seen to gleam, set off
by the outer darkness of ‘Spoonbill’s’ skin. This woman, broad-
shouldered and thick-waisted, is almost as stalwart as her Mhiás, whose
tattoo (chale) is a single line forked at both ends:[25] in others the
cuticle and cutis are branded, worked, and raised in an intricate
embroidery over all the muscular trunk. An abnormal equality of strength
and stature between the sexes prevails amongst many African tribes,
especially the agricultural, where women are the workers. The same may
be observed in parts of North Britain and of northern Europe. The
difference in this matter between the Teutonic and the Latin races never
struck me so strongly as when seeing German families land at Rio de
Janeiro.
The half-caste Zanzibar girl enviously eyes the Arab woman, a heap of
unwashed cottons on invisible feet, with the Maskat masque exposing only
her unrecognizable eyeballs. The former wears a single loose piece of
red silk or chequered cotton. Her frizzly hair is twisted into pigtails;
her eyelids are stained black; her eye-brows are lengthened with paint;
her ear-rims are riddled with a dozen holes to admit rings, wooden
buttons, or metal studs, whilst the slit lobes, distended by elastic
twists of coloured palm-leaf, whose continual expansion prodigiously
enlarges the aperture, are fitted with a painted disk, an inch and a
half in diameter. The same device was practised (according to the
missionary Gumilla) by the Aberne tribe of the Orinoco. If pretty, and
therefore wealthy, she wears heavy silver earrings run through the shell
of the ear; her thumbs have similar decorations, and massive bangles of
white metal adorn, like manacles and fetters, her wrists and ancles. One
wing of her nose is bored to admit a stud—even the patches of Europe
were not more barbarous. The Zanzibarian slave girl shaves her head
smooth, till it shows brown and shiny like a well-polished cocoa-nut;
and she drags along her ‘hopeful’—she has seldom more than one—a small
black imp, wholly innocent of clothing. The thing already carries on its
head a water-jar bigger than its own ‘pot-belly,’ and it screams Ná-kujá
(I come!) to other small fry disporting itself more amusingly.
-----
Footnote 17:
Changa (large sands), in the plural Michanga, sands (of great extent).
Mchanga (sand generally), at Mombasah and on the coast which preserve
the older dialect, becomes Mtángá, and means a sandy place. The
islanders of Zanzibar, for instance, will say Nti (the land or earth),
the continentals, Nchi: these prefer Ku Changanyika (to meet
together), those Ku Tanganyika. Foreigners often confound chyá with
jyá, and pronounce, for instance, Msijyáná for Msichyáná—a lass. The
Arabs, who cannot articulate the ch, convert it into their familiar
sh, e. g. Ku Shimba for Ku Chimba (to dig).
Footnote 18:
Manioc, often erroneously written Mahogo.
Footnote 19:
I have described (Pilgrimage to El Medinah and Meccah) the modern
Sambúk of the Red Sea, and find the word ‘Sonboúk’ in the French
translation of Ibn Batutah. Sir Gardner Wilkinson quotes Athenæus, who
makes the ‘Sambuca’ (a musical instrument) ‘resemble a ship with a
ladder placed over it.’
Footnote 20:
It is written Mutaifiyah in the Arab Chronicle of Mombasah History,
translated and included in Captain Owen’s work (Voyages to Africa,
vol. i. 416, Arabia, etc., London, Bentley, 1833).
Footnote 21:
The quarters, beginning from Changáni, the most western, are, the
Baghani, which contains the English Consulate; the Mnazi-Moya to the
south, with a grave-yard, and a bazar where milk and grain are sold;
the Fuga adjoining it, the Zambarani, the Kajifichemi, the Kunazemi,
and the Námbo to the south-east; the Gurayzani, containing the fort;
and the Furdani with the Custom House; the Kipondah, where the French
Consulate is; the Ziwani (Mitha-pani of the Hindus) further to the
south; the Suk Muhogo, where manure and fish are sold; the Melindi, or
Melindini, occupied by Hindus, and boasting a bazar; and lastly the
Mnawi, the Kokoni, and the Fungu extend to the easternmost quarter,
the Malagash, where the Lagoon, an inlet of the sea, bounds the city.
I did not hear any of the three names mentioned in the text; they are
probably now obsolete.
Footnote 22:
The Iberian name (in Arabic الستح, El Sat’h) of the flat roof-terrace,
borrowed from the dry lands of Western Asia.
Footnote 23:
Chap. 7. Captain Hamilton’s ‘New Account of the East Indies.’
Footnote 24:
The Arabs here call the shark ‘jarjúr,’ the Wasawahíli p’hápá. I do
not know why Captain Guillain (ii. 391) says, ‘le requin, nommé par
les Arabs _lebah_—‘Lebah is the Somali name for a lion.
Footnote 25:
Uhiáo is the Iáo of Mr Cooley, who calls the people M’yau (Mhiáo) and
Miyáo (Wahiáo). They are the ‘Monjou’ of Salt, and the Mujao of the
Portuguese. M. Macqueen (On the Geography of Central Africa) says,
‘The inhabitants on the west side of the Lake are called Yoah, and are
Mohammedans.’ They are still pagans. Capt. Guillain (1, 390) remarks,
‘Les historiens Portuguais nous paraissent avoir donné au pays le nom
que les indigènes donnent à ses habitants. Moudjâou, ou plutôt Moniâo
et, par contraction, M’iâo signifie un homme du pays de Iáo.’ Uhiáo
would be the country; Mhiáo and Wahiáo (singular and plural), its
people.
CHAPTER V.
GEOGRAPHICAL AND PHYSIOLOGICAL.
‘To my surprise, the information concerning Zanzibar and the N. E. coast
of Africa ... scarcely contains meagre phrases destitute of precision.’—
(Col. Sykes’ Journal, R. G. S., vol. xxiii. 1853.) He forgets that
entering from the coast is like jumping from the street into the
window.—(R. F. B.)
SECTION 1.
Africa, East and West—‘Zanzibar’ explained—Menouthias—Position and
Formation—The East African Current—Navigation—Aspect of the Island.
It is an old remark that Africa, the continent which became an island by
the union of the twin seas in the year of grace 1869, despite her
exuberant wealth and her wonderful powers of reproduction, is badly
made—a trunk without limbs, a monotonous mass of painful symmetry,
wanting opposition and contrast, like the uniform dark complexion of her
sons and of her fauna—a solid body, like her own cocoa-nut, hard to
penetrate from without, and soft within; an ‘individual of the earth,’
self-isolated by its savagery from the rest of the world. This is
especially true of intertropical Africa.
The western coast was, until the last four centuries, cut off from
intercourse with mankind by the storm-lashed waters of the northern
approach; and to the present day the unbroken seaboard, so scanty in
good harbours, and the dangerous bars and bores which defend the deadly
river mouths, render it the least progressive part of the old world.
The more fortunate north-eastern and subtropical shores were enabled by
their vast crévasse, the Red and riverless Sea, to communicate with
Western Asia, whilst the rich productions, gold and ivory, tortoise-
shell and ambergris, the hot sensuous climate—which even now induces the
northern sailor to ship in the fatal West African squadron—and the amene
scenery of the equatorial regions, invited, during pre-historic ages,
merchants, and even immigrants, from rugged Persia and sterile Arabia.
Between the two upper coasts, eastern and western, there is, as might be
expected, great similarity of grim aspect. The northern seaboards offer,
for the space of a thousand miles, the same horrid aspect; deceitful
roadsteads and dangerous anchorages, forbidding lines of chalky cliff
and barren brown sandstone bluff; flat strands and white downs, hazed
over by the spray of desert sand; and lowlands backed by maritime sub-
ranges, masses of bald hill and naked mountains, streaked with dry wadis
and water-courses, that bear scatters of dates and thorns, and which
support miserable villages of tents or huts. The fierce and wandering
tribes, Berber, Arab, and Arabo-African—an especially ‘crooked and
perverse generation,’—are equally dangerous to the land traveller and to
the shipwrecked mariner.
As sterile and unlovely for the same cause—the absence of tropical
rains—are the southern regions of the great Nineteenth Century Island.
Good harbours are even rarer than in the north, and the seas about the
Cape of Hope, sweeping up unbroken from the South Pole, are yet more
perilous. The highlands fringing the southern and eastern coasts arrest
the humid winds, and are capable of supporting an extensive population;
but the interior and the western coast, being lowlands, are wild and
barren. The South African or Kafir family, which has overrun this soil,
is still for the most part in the nomade state, and its ‘evident
destiny’ is to disappear before the European colonist.
The central and equatorial land, 34° deep, including and bordering upon
the zone of almost constant rain, is distinguished by the oppressive
exuberance of its vegetation and by the consequent insalubrity of its
climate. The drainage of the interior, pouring with discoloured efflux
to the ocean, in large and often navigable channels, subject to violent
freshes, taints the water-lines with deadly malaria. The false coasts of
coralline or of alluvial deposits—a modern formation, and still forming—
fringed with green-capped islets, and broken by sandy bays and by
projecting capes, are exposed to swells and rollers, to surf and surge,
to numbing torrents and chilling tornadoes, whilst muddy backwaters and
stagnant islets disclose lagoon-valves or vistas through tangled morass,
jungle, and hardly penetrable mangrove-swamp. This maremma, the home of
fever, is also the seat of trade, but the tribes which occupy it soon
die out.
The true coast has already risen high enough above the waters to
maintain its level; and the vegetation—calabashes, palms, and tamarinds—
offers a contrast to the swampy growth below. Inland of the raised
seaboard are high and jungly mountains and coast-range or ghaut, in many
parts yet unvisited by Europeans. Beyond these sierras begins the basin-
shaped plateau of Central Equatorial Africa. The inhabitants are mostly
inland tribes, ever gravitating towards the coast. They occupy stockaded
and barricaded clumps of pent-houses or circular tents, smothered by
thicket and veiled, especially after the heavy annual rains, with the
‘smokes,’ a dense white vapour, moisture made visible by the earth being
cooler than the saturated air.[26]
I have elsewhere remarked (The Lake Regions of Central Intertropical
Africa; Abeokuta and the Camaroons Mountains, &c.) the striking
geological contrast between the two equatorial coasts, eastern and
western. The former, south of the Guardafui granites, offers to one
proceeding inland from the ocean a succession of corallines, of
sandstone and of calcaires, which appear to be an offset from the
section of that great zone forming the Somali country. The western
coasts, after quitting the basalts and lavas of the Camaroons, are
composed chiefly of the granites and syenites with their degradations of
schiste, gneiss, and sandstone. Similarly, in the great Austro-American
continent, one shore, that of the Brazil, is granitic, whilst the other,
Chili, mainly consists of the various porphyries.
The negroes and negroids of both these inhospitable coasts, an
undeveloped and not to be developed race—in this point agreeing with the
fauna and flora around them—are the chief obstacles to exploration, and
remarkably resemble each other. The productions of the east and west are
similar. The voracious shark swims the seas, turtles bask upon the
strands and islets, and the crocodile and hippopotamus haunt the rivers.
The forests abound in apes and monkeys, and the open plains support the
giraffe, the antelope, and the zebra, hog and wild kine (Bos Caffir and
B. Brachyceros), herds of elephants and scatters of rhinoceros. The
villagers breed goats and poultry. In the healthier regions they have
black cattle and sheep, whilst one tribe has acclimatized the ass. The
exceeding fertility of the rain-drenched plains gives an amazing
luxuriance to cassava and rice, maize, and holcus, cotton, sugar-cane,
and wild indigo, banana, lime and orange, ground-nuts and coffee. The
hills and torrent-beds yield gold and copper, antimony, and abundance of
iron. On both sides of the continent there are rich deposits of the
semi-mineral copal. Coal was found by the Portuguese at Tête and in the
Zambeze Valley, as related in Dr Livingstone’s First Expedition
(Missionary Travels, &c., xxxi. 633-4). His second prolonged the coal-
field to beyond the Valley of the Rufuma (Rovuma) river (xxi. 440), and
it will probably be found to extend still further.
Dr Krapf declares (Travels, &c., p. 465) that he discovered coal, ‘the
use of which is still unknown to the Abessinians,’ on the banks of the
Kuang, a river said to rise in the Dembea Province, near Lake Tsana
(Coloë Palus). Finally, to judge from the analogy of the South American
continent, the valuable mineral will yet be struck near the western
coast, south of the equator.
From time immemorial, on both sides of Africa, the continental Islands,
like Aradus and Sidon, Tyre and Alexandria, have been favourite places
with stranger settlers. They have proved equally useful as forts,
impregnable to the wild aborigines, and as depôts for exports and
imports. Second to none in importance is Zanzibar, and the future
promises it a still higher destiny.
And first, of the name, which does not occur in Strabo, Pliny, or the
Periplus. The log-book attributed to Arrian, of Nicomedia, calls the
whole shore, ‘Continent of Azania;’ probably an adaptation, like Azan,
and even Ajan, of the Arabic, Barr el Khazáin, or the Land of Tanks,[27]
the coast between Ra’as Hafun and Ra’as el Khayl. So Pliny (vi. 28 and
34) speaks of the ‘Azanian Sea’ as communicating with the ‘Arabian
Gulf.’ Ptolemy, however (I. 17, sec. iv. 7), has the following important
passage: ‘immediately following this mart (Opone) is another bay, where
Azania begins. At its beginning are the promontory Zingis (ζίγγις,
Zingina promontorium), and the tree-topped Mount Phalangis.’ The name
may have extended from the promontory to the coast, and from the coast
to the island. Dr Krapf speaks of a tribe of the ‘Zendj’ near the Rufiji
river, but I could not hear of it. It is easy to show that the Pelusian
geographer’s Opone is the bay south of Ra’as, or Jurd Hafun. Like
Pomponius Mela, Ptolemy evidently made his great point de départ the
Aromata Promontorium et emporium in Barbarico sinu (Cape Guardafui), and
he placed it N. lat. 6° 0′ 0″, instead of N. lat. 11° 50′. This error
threw the whole coast 6° (in round numbers, more exactly 5° 50′) too far
south, and made the world doubt the accurate position of the Nile lakes.
Thus, to his latitude of Opone N. 4° add 5° 50′, and we have N. lat. 9°
50′, the true parallel of Hafun being N. lat. 10° 26′.
Amongst late authors we find the word Zanzibar creeping into use. The
Adulis inscription (4th century) gives ‘Zingabene’; and its copier, the
Greek monk Cosmas Indicopleustes, who proved the globe flat (6th
century), calls the ‘unnavigable’ ocean beyond Berberia, the ‘Sea of
Zenj,’ and the lands which it bathes ‘Zingium.’ It is found in Abu Zayd
Hasan, generally known as Hunayn bin Ishak (died A.D. 873); in El
Mas’udi, who describes it at some length (died A.D. 957); in El Bayruni
(11th century), and in the learned ‘Nubian Geographer,’ the Sherif El
Idrisi (A.D. 1153). Marco Polo (A.D. 1290), who evidently wrote his 37th
chapter from hearsay, makes Zanzibar a land of blacks; and, confounding
insula with peninsula (in Arabic both being Jezireh), supplies it with a
circumference of 2000 miles, and vast numbers of elephants. The India
Minor, India Major, and India Tertia of the mediæval Latin travellers
are the Sind, Hind, and Zinj of the Arabs. Ibn Batuta (A.D. 1330, 1331),
the first Arab traveller who wrote a realistic description of his
voyage, has accurately placed Kilwa, which he calls ‘Kulua,’ in the
‘land of the Zunúj.’ Finally, we meet with it in El Nowayri, and in
Abulfeda, the ‘Prince of Arab Geographers,’ who both died in the same
year, A.D. 1331.
The word Zanj (زنج), corrupted to Zinj, whence the plural ‘Zunúj,’ is
evidently the Persian Zang or Zangi (زنگ), a black, altered by the
Arabs, who ignore the hard Aryan ‘Gaf’ (گ), the ‘G’ in our gulf. In the
same tongue bár means land or region—not sea or sea-coast—and the
compounded term would signify Nigritia or Blackland. In modern Persian
Zangi still means a negro, and D’Herbelot says of the ‘Zenghis’ that
‘they are properly those called Zingari,[28] and, by some, Egyptians and
Bohemians.’ Scholars have not yet shown why the Arab, so rich in
nomenclature, borrowed the purely Persian word from his complement the
‘Ajam.’ They have forgotten that the Persians, who of late years have
been credited with the unconquerable aversion to the sea which belongs
to the Gallas and the Kafirs, were once a maritime people. ‘The
indifference or rather the aversion of Persians to navigation’ (M.
Guillain, i. 34, 35) must not be charged to the ancient ‘Furs.’ Between
A.D. 531–579, when Sayf bin Dhu Yezin, one of the latest Himyarite
rulers, wanted aid against the Christian Abyssinians, who had held
southern Arabia for 72 years, he applied to Khusrau I., better known as
Anushirawán, the 23rd king of the Sassanian dynasty, which began with
Ardashir Babegan (A.D. 226), and which ended with Yezdegird III. (A.D.
641), thus lasting 415 years. The ‘Just Monarch’ sent his fleet to the
Roman Port’ (Aden), and slew Masruk. In his day the Persians engrossed,
by means of Hira, Obollah, and Sohar, the rich tracts of Yemen and
Hindostan; while Basrah (Bassorah) was founded by the Caliph Omar, in
order to divert the stream of wealth from the Red Sea, a diversion which
will probably soon be repeated. In A.D. 758 the Persians, together with
the Arabs, mastered, pillaged, and burn Canton. Much later (17th
century) Shah Abbas claimed Zanzibar Island and coast as an appanage of
the suzerainty of Oman.
East Africa still preserves traditions of two distinct colonizations
from Persia. The first is that of the ‘Emozaydiys,’ or ‘Emozeides’ (Amm
Zayd), who conquered and colonized the sea-board of East Africa, from
Berberah of the Somal to Comoro and Madagascar, both included. A second
and later emigration (about A.D. 1000) occupied the south Zanzibarian
coast, and ruins built by the Shirazían dynasty which still lingers, are
shown on various parts of the sea-board. Of these Persian occupations
more will be found in the following pages. (Part 1, Chap. I, and Part 2,
Chap. 2.)
Persia has left nothing of her widely extended African conquests but a
name. In modern days she has become more and more a non-maritime power.
She has wholly retired from the coast; and Time, who in these lands
works with a will, presently obliterated almost every trace of the
stranger. A few ruins at Aden and Berberah, and the white and black
sheep of Ormania (Galla-land) and of Somali land, are almost the only
vestiges of Persian presence north of the Equator. On the Zangian
mainland wells sunk in the rock, monuments of a form now obsolete;
mosques with elaborate minarets and pillars of well-cut coralline;
fortified positions, loopholed enclosures, and ruined cities whose names
have almost been forgotten, are the results of the civilization which
they brought with them southwards.
The limits assigned by the Arab geographers to the ‘Land of the Zinj’
are elastic. While some, as Yakut, make it extend from the mouths of the
Jub River (S. lat. 0° 14 30″) to Cape Corrientes (S. lat. 24° 7′ 5″) and
thus include Sofala; others, with El Idrisi, separate from it the latter
district, and unjustly make its southern limit the Rufiji River (S. lat.
7° 38′), thus excluding Kilwa. It should evidently extend to Mozambique
Island (S. lat. 15° 2′ 2″), where the Wasawahíli meet the ‘Kafir’ races.
The length would thus be, in round numbers, 15° = 900 geographical
miles, whilst the breadth, which is everywhere insignificant, can hardly
be estimated.
The Arabs, who love to mingle etymology with legend and fable, derive
the word ‘Zanzibar’ from the exclamation of its pleased explorers, ‘Zayn
za’l barr!’ (fair is this land!). Similar stories concerning Brazilian
Olinda and Argentine Buenos Aíres are well known. ‘El Sawáhil,’ the
shores, evidently the plural of Sáhil, is still applied to the 600 miles
of maritime region whose geographical limits are the Jub River and Cape
Delgado (S. lat. 10° 41′ 2”), and whose ethnographic boundaries are the
Somal and the ‘Kafir’ tribes. Others derive it from El Suhayl, the
beautiful Canopus which, surrounded by a halo of Arab myth, ever
attracts the eye of the southing mariner. The Wasawahíli,’[29] or slave
tribes, are fancifully explained by ‘Sawwá hílah,’ he ‘played tricks,’—
rascals all.
The coast races who, like their neighbours the Somal, have their own
African names for places, call Zanzibar Island by the generic term
Kisíwa—insula. It is thus opposed to Mpoa-ni, the coast, and to Mrímá,
the mainland.[30] The latter, however, is properly speaking limited to
the maritime uplands between Tanga and the Pangani river. Zanzibar city
is Unguja (pronounced Ungudya, not Anggouya). The word appears in an
ancient settlement on the eastern coast of the island, and the place is
still called Unguja Mku, Old Unguja. Some still call it Lunguja,
apparently an older form. We find ‘Lendgouya’ in the Commercial
Traveller Yakut (early thirteenth century); but ‘Bandgouia’ (Abd el
Rashid bin Salih el Bakui, A.D. 1403) is clearly a corruption.
Finally, Zanzibar has been identified by palæogeographers with the
Ptolemean Μενουθιὰς or Μενουθεσίας (iv. 9), and with the Μενουθιὰς of
the Periplus (Geog. Græci Minores of R. Muller, Paris, 1855), in some
copies of which Menouthesías also occurs. Its rivals, however, for this
honour are Pemba, Mafiyah (the Monfia of our maps) and Bukini, the
northern and north-western parts of Malagash or Madagascar.[31] Ptolemy,
it may be observed, places the two important sites, Menouthias and
Prasum (or Prassum) in a separate chapter (iv. 9), whereas his principal
list of stations is in Book iv. chapter 7. He lays down the site of
Menouthias in S. lat. 12°, and nearly opposite the Lunar Mountain, and
the Lakes whence the Nile arises (S. lat. 12° 30′). The mouth of the
Rhapta river and Rhapta, the metropolis of Barbaria, are in S. lat. 7°,
the Rhapta promontory is in S. lat. 8° 20′ 5″, and the Prasum promontory
in S. lat. 15°. By applying the correction as before, we have for
Menouthias S. lat. 6° (the capital of Zanzibar being in S. lat. 6° 9′
6″); for the Lakes, 6° 30′, which would nearly bisect Tanganyika; for
Rhapta river and city, S. lat. 1° (or more exactly, S. lat. 1° 10′); the
mouth of the Jub river being in S. lat. 0° 14′ 30″; the Rhapta
promontory in S. lat. 2° 30′, corresponding with the coast about Patta;
and finally, for Prasum S. lat. 9° 10′—Cape Delgado being in S. lat. 10°
41′ 12″.
The account given of Menouthias in the Periplus (written between A.D.
64, Vincent, and A.D. 210, Letronne[32]) is that of an eyewitness:
‘After two nychthemeral days (each of 100 miles) towards the west [here
the text is evidently corrupt] comes Menouthias, altogether insulated,
distant from the land about 300 stadia (30 geographical miles), low and
tree-clad. In it are many kinds of birds and mountain tortoises (land
turtle?). It has no other wild beasts but crocodiles (iguanas), and
these do not injure man. There are in it sewn boats and monoxyles
(canoes), which they use for salt-pans [here the text is defective] and
for catching turtle. In this island they trap them after a peculiar
fashion with baskets (the modern wigo) instead of nets, letting them
down at the mouth of stony inlets’ (chap. i. 15).
The next chapter informs us: ‘From which (island) after two runs (each
50 miles)[33] lies the last emporium of the continent of Azania, called
Tà Rhaptà, thus named from the before-mentioned sewn-together vessels.
In it are much ivory and tortoise-shell. The men, who in this country
are of the largest size, live scattered (in the mountains?), and each
tribe in its own place is subject to tyrants’ (‘tyranneaulx’ or petty
chiefs).
Here, then, we have Rhapta 33 leagues (100 miles = 1° 40′) beyond
Menouthias. Captain Guillain (Prem. Partie, p. 115) would make the
former correspond with the debouchure of the Oufidji river (Rufiji or
Lufiji), in S. lat. 7° 50′. But the Periplus, unlike Ptolemy, alludes
only to a port, not to a river mouth, nor does the coast-line here show
any promontory. Others have proposed Point Puna (S. lat. 7° 2′ 42″), the
south-western portal of the Zanzibar manche, near the modern trading
port of Mbuamáji, which in former ages may have been more important.
D’Anville, Vincent, and De Froberville boldly prefer Kilwa (in round
numbers S. lat. 9°), which is distant 157 geographical miles from the
southernmost point of Zanzibar, and I think they are right. It is safer
in such matters to suspect an error of figures and of distances than of
topography, especially where the geographical features are so well
marked and cannot be found in other places. Computations of ancient
courses and log-books can have little value except when they serve to
confirm commonly topographical positions. Kilwa has ever been a central
station on the Zanzibar coast, and the slaves brought from the interior
are still remarkable for size. Moreover, as Dr Beke well observes
(Sources of the Nile, p. 69), ‘In attempting to fix in the map of Africa
the true position of Ptolemy’s lakes and sources of the Nile, we must
discard all notions of their having been determined _absolutely_ by
means of astronomical observations, special maps of particular
localities, or otherwise, and regard them simply as derived from oral
information, and as laid down _relatively_ to some well-known point or
points on the coast.’[34]
Zanzibar, the principal link in the chain of islets which extends from
Makdishu (Magadoxo), in the Barr el Benadir or Haven-land, to Cape
Corrientes, is a long narrow reef, with the major axis disposed from N.
N. W. to S. S. E., and subtending a deep bight or bend in the coast,
justly enough called the Barbaric Gulf. The length is 48·25 geographical
miles from Ra’as Nunguwi, the northern (S. lat. 5° 42′ 8″ Raper), to
Ra’as Kizimkaz, the southern, extremity (S. lat. 6° 27′ 7″ Raper). The
breadth is 18 miles from the Fort in E. long. 39° 14′ 5″ Raper’s
correction, to the continental coast in E. long. (G.) 39° 32′ 5″. French
travellers assume a max. length of 83 kilomètres, and a max. breadth of
33. The capital (S. lat. 6° 9′ 6″) corresponds in parallel with the
Pernambucan province to the west and with Java and central New Guinea to
the east. The corrected longitude (laid down by Captain Smee in 1811 as
E. lat. 39° 15′) gives a difference of Greenwich time 2^{h.} 36^{m.} and
56^{s.}. From Southampton round the Cape the run is usually laid down at
8500 miles, viâ Suez 6200. The Lesseps Canal has shortened the distance
from Marseille by 2000 leagues, and thus has placed Zanzibar within 1600
leagues of the great port—in fact, about the distance of the Gaboon ex-
colony.
The formation of the island is madrepore, resting upon a core or base of
stratified sand-stone grit, disposed in beds varying from 1·5 to 3 feet
thick. The surface gently inclines towards the sea, and the lines of
fracture run parallel with the shores. Three distinct formations occur
to one crossing the breadth.[35] The first is a band of grit-based
coralline, which runs meridionally, and is most remarkable on the
eastern side. This portion, featureless and thinly inhabited, is
protected from the dangerous swell and the fury of the Indian Ocean by a
broad reef and scattered rocks of polypidoms. The band thins out to the
north and south: in the centre, where it is widest, the breadth may be
three to four miles, and the greatest height 400 feet. The coral-rag is
mostly white and of many shapes, like fans, plants, and trees: the most
usual form is the mushroom, with a broad domed head rising from a narrow
stem. The texture is exceedingly reticulated and elastic; solid masses,
however, occur where neighbouring rocks meet and bind—hence the
labyrinth of caverns, raised by secular upgrowth and preserving the
original formation. The ground echoes, as in volcanic countries, hollow
and vault-like to the tread; the tunnels are frequently without issue
for drainage, and when the rain drips in, the usual calcareous
phenomena, stalactites and stalagmites, appear. Many of these caves are
found on the coast as well as on the island. The carbonate of lime is
very pure, and contains brown or yellow-white crystals.
A stony valley, sunk below the level of both flanks, is said to bisect
the island from north to south. Into this basin fall sundry small
streams, the Mohayra and others, which are lost through the crevices and
caverns, and in the cracks and fissures of the grit. There are other
drains, forming, after heavy downfalls, swamps and marshes, whence
partly the great insalubrity of the interior. The western part of
Zanzibar, with its wealth of evergreen vegetation, appears by far the
most fertile. It is a meridional band of red clay and sandy hills,
running parallel with the corallines of the eastern coast. Here are the
most elevated grounds. I found the royal plantation Sebbé or Izimbane,
400 feet (B.P.) above sea-level, or a little higher than the Bermudas.
The least productive parts are those covered with dark clay. Heavy rains
deposit arenaceous matter upon the surface, and the black humus
disappears. On this side of the island also many streamlets discharge
into the sea, bearing at their mouths mangrove beds, whose miasmas cause
agues, dysenteries, diarrhœas, and deadly fevers.
The rule established by Dampier and quoted by Humboldt directs us to
expect great depth near a coast formed by high perpendicular mountains.
Here, as in the rest of the Zanzibarian archipelago, the maritime line,
unlike the west Atlantic islands Tenerife and Madeira, is composed of
gently rolling hills. Yet seven fathoms are often found within a stone-
throw of the land, whilst the encircling ledges are steep-to, marked in
the charts 1/100 and 1/140. Evidently, then, the corallines are perched
upon the summits of a submarine range which rises sharp and abrupt from
abysmal hollows and depressions. As usual too in such formations, the
leeward shore line of the island, where occur the lagoon entrances, is
more varied and accidented than the eastern. At Pemba this feature will
be even more remarkable.
The windward coast, in common with many parts of the continental
seaboard, suffers especially from June to August from the Ras de Marée
(Manuel de la Navigation et la Côte occidentale de l’Afrique), a tide
race, supposed to result from the meeting of currents. It is a line of
rollers neither far from nor very near the shore. The hurling and
sagging surf is described to resemble the surge of a submarine
earthquake; and the strongest craft, once entangled in the send, cannot
escape. It would be useful to note, as at West African Lagos, the
greater or less atmospheric pressure accompanying the phenomenon, and to
seek a connection between it and the paroxysms of the neighbouring
cyclone region. At all times sailors remark the ‘shortness’ of the waves
and the scanty intervals between their succession. This peculiarity
cannot be explained in the usual way by shoals and shallow water causing
a ground-swell.
With respect to the great East African ocean-current, which has given
rise to so many fables gravely recorded by the Arab geographers,[36] the
best authorities at Zanzibar are convinced, and their log-books prove,
that both its set and drift, like the Brazilian coast-stream, are in the
present state of our knowledge subject to the extremes of variation. The
charts and Horsburgh lay it down as a regular S.W. current; and so it is
in the southern, whilst in the northern part it is hardly perceptible.
Between Capes Guardafui and Delgado it flows now up then down the coast;
here it trends inland, there it sets out to sea. Dr Ruschenberger
relates that on Sept. 1, 1835, his ship, when south of Zanzibar, was
carried 50 miles in 15 hours, and was obliged to double the northern
cape. The same happened to Captain Guillain in August 1846, when he lost
five days. This resulted from the superior force of the S.W. monsoon,
which often drives vessels to the north 30 to 40 miles during the day
and night. Lieut. Christopher (Journal, Jan. 5, 1843) reported it to be
variable and violent, especially close in shore, and observed that it
frequently trends against the wind. It is usually made to run to the
S.W. between December and April, at the rate of 1·3 miles per hour, from
Ra’as Hafun to Ra’as Aswad, and two to three miles per hour between
Capes Aswad and Delgado. Shipmasters at Zanzibar have assured me that
when this coastal current covers three knots an hour there is a strong
backwater or counter-flow, which, like the Gulf-stream, trends to the
north, and against which, with light winds, native vessels cannot make
way. This counter-current has extensive limits; usually it is considered
strongest between Mafiyah and Pomba. The ship St Abbs, concerning which
so much has been said and written of late years, was wrecked in 1855 off
St Juan de Nova of the Comoro group (S. lat. 17° 3′ 5″), and pieces of
it were swept up to Brava (N. lat. 1° 6′ 8″), upwards of 1000 miles. The
crew is supposed still to be in captivity amongst the Abghal tribe; and
in 1865 an Arab merchant brought to Zanzibar a hide marked with letters
which resembled N F B N. A writer in the _Pall Mall_ opined the letters
to be ‘Wasm’ or tribal brands, justly observing that ‘all the Bedawin
have these distinguishing marks,’ but forgetting that he was speaking of
the analphabetic Somal, to whom such knowledge does not extend. As we
might expect, the Mozambique stream, south of Cape Delgado, always flows
southerly with more or less westing. The rate is said to vary from 20 to
80 miles a day.
Our hydrographical charts are correct enough to guide safely into and
out of port any shipmaster who will sound, and can take an angle. As,
however, the navigation is easy, so accidents are common. Any land-
lubber could steer a ship from Bombay to Karachi (Kurrachee), and yet
how many have been lost! Often, too, it is in seamanship as in
horsemanship, when the best receive the most and the heaviest falls. In
May 1857 the Jonas, belonging to Messrs Vidal, was sunk by mistaking
Chumbi Island for its neighbour Bawi. Three or four days afterwards the
Storm King of Salem, Messrs Bertram, ran aground whilst hugging Chumbi
in order to distance a rival. The number of reefs and shoals render it
always unadvisable to enter the port at night, and in the heaviest
weather safe riding-ground is found between Zanzibar Island and the
continent.
[Illustration: ZANZIBAR FROM THE SEA.]
Vessels from the south making Zanzibar in the N.E. monsoon, the trade-
wind of December to March, leave Europa Island to the west, and the
Comoro group and S. Juan de Nova on the east. Keeping well in mid-
channel, they head straight for Mafiyah. They hug Point Puna, avoiding
Latham’s Bank,[37] and they work up by Kwale and the Chumbi Island.
Ships from the north have only to run down the mid-channel, between
Pemba and the continent, and then to pass west of Tumbatu. Those sailing
southward from Zanzibar at this season pass along-shore, down the
Mozambique Channel. Vessels from the south making Zanzibar in May to
September, the height of the S.W. monsoon—the anti-N.E. trade—sail up
the same passage. They must beware of falling to leeward; and those that
neglect ‘lead and look-out’ are ever liable to be carried northwards to
Pemba by the counter-current before mentioned, which may, however, now
be a wind-current. At this season ship-masters missing the mark have
sometimes made 3° to 4° of easting, and have preferred beating down to
Mafiyah and running up again, rather than face the ridicule of appearing
viâ the northern passage. Those leaving the Island in the S.W. monsoon
stand north up channel, well out in E. lon. 9° 42′ to 43′, beat south of
Cape Delgado, pass between the Comoro group and the mainland, and thus
catch the Mozambique gulfstream. The brises solaires blow strongest off
Madagascar in June and July. They fall light in August and September.
The aspect of Zanzibar from the sea is that of coralline islands
generally—a graceful, wavy outline of softly rounded ground, and a
surface of ochre-coloured soil, thickly clothed with foliage alternating
between the liveliest leek-green and the sombrest laurel, the only
variety that vegetation knows in this land of eternal verdure.
Everywhere the scenery is similar; each mile of it is a copy of its
neighbour; and the want of variety, of irregularity, of excitement, so
to speak, soon makes itself felt. Zanzibar ignores the exhilaration of
pure desert air, and the exaltation produced by the stern aspect of
mountain regions or by a boundless expanse of Pampa and Sahara. Without
a single element of sublimity, soft and smiling, its sensuous and
sequestered scenery has no power to spur the thought, to breed an idea
within the brain. The oppressive luxuriance of its growth combined with
the excess of damp heat, and possibly the abnormal proportion of ozone,
are the most unfavourable conditions for the masculine. The same is the
case in Mazanderan, Malabar, Egypt, Phœnicia, California, and other
Phre-kah—lands of the sun. And the aspect of that everlasting,
beginning-less, endless verdure tends, as on the sea-board of the
Brazil, to produce sensations of melancholy and depression. We learn at
last to loathe thee,
‘gay green,
Thou smiling Nature’s universal robe!’
Landing upon the island, you find a thin strip of bright yellow sand
separating the sea from a curtain of vegetation, which forms a
continuous wall. In some parts madrepore rock, looped and caverned by
the tide, and covered with weeds and testaceæ, whose congeners are
fossilized in the stone, rises abruptly a few feet above the wave. At
other places a dense growth of tangled mangrove jungle exposes during
the ebb a sheet of black and sticky mire, into which man sinks knee-
deep. The regularity of the outline is broken by low projecting spits
and by lagoons and backwaters, which bite deep into the land. Their
pestilential, fatal exhalations veil the low grounds with a perpetual
haze, and the excess of carbon is favourable to vegetable as it is
deleterious to animal life.
Passing over the modern sea-beach, with its coarse grasses, creepers,
and wild flowers—mostly the Ipomæa—and backed by towering trees, cocoas,
mangos, and figs, we often observe in the interior distinct traces of an
old elevation, marked by lines of water-worn pebbles and by coarse
gravels overlying greasy blue clay. This is the home of the copal.
Beyond it the land rises imperceptibly, and breaks into curves, swells,
and small ravines, rain-cut and bush-grown, sometimes 40 feet deep. The
soil is now a retentive red or yellow argile, based upon a detritus of
coralline, hardened, where pressed, into the semblance of limestone, or
upon a friable sand-stone-grit of quartz and silex. The humus of the
richest vegetable substance, and excited by the excess of humidity and
heat, produces in abundance maize, millet, and various panicums;
tomatoes and naturalized vegetables, muhogo (the cassava), and Palma
Christi; coffee, cotton, and sugar-cane; clove, nutmeg, and cinnamon
trees; foreign fruits, like the Brazilian Cajú, the passion-flower and
the pine-apple; the Chinese Leechi; bananas and guavas, the Raphia and
the cocoa, twin queens of the palms; limes and lemons, oranges and
shaddocks, the tall tamarind, the graceful Areca, the grotesque calabash
and Jack-tree, colossal sycamores and mangos, whose domes of densest
verdure, often 60 feet high and bending, fruit-laden, to the earth, make
our chesnuts, when in fullest dress, look half-naked and in rags.
The uplands, especially in the western part of the island, are laid out
in Máshámha or plantations, whose regular lines of untrimmed clove-trees
are divided by broad sunny avenues. Here and there are depressions in
the soil, where heavy rains slowly sinking have nursed a tangled growth
of reeds and rushes, sedge and water-grass. About the Mohayra and the
Búbúbú—the principal of the ποταμοι πλειστοι of the Periplus—mere
surface-drains, choked with fat juncaceæ and with sugar-cane growing
wild, there is a black soil of prodigious fertility, whose produce may,
so to speak, be seen to grow. This sounds like exaggeration; but I well
remember, at Hyderabad, in Sind, that during the inundation of the Indus
we could perceive in the morning that the maize had lengthened during
the night, and the same is the case with certain ‘toadstools’ and fungi
in the Brazil.
Upon this waste of rank vegetation the sun darts an oppressive and
malignant beam. In the driest season the ‘mangrove heaviness’ of the
western coast and the cadaverous fœtor announce miasma; after the rains
the landscape is redolent of disease and death.
The cottages of small proprietors and slaves strew the farms. They are
huts of wattle and rufous loamy dab, to which large unbaked bricks of
red clay are sometimes preferred. The usual cajan pent-roof forms deep
dark eaves, propped by untrimmed palm-boles. These dwellings are
unwholesome, because none boast of a second storey; they are not even
built upon piles, and thus their sole defence against the surrounding
malaria is the shrubbery planted by nature’s hand. Sickness seems
generally, both in the island and on the continent, to follow turning up
fresh soil, and the highlands are often more subject to miasma than the
lowlands.
The lines of communication consist of mere footpaths, instead of the
broad roads required for the ventilation of the country. When the
produce of the land is valuable the lanes are lined with cactus, milk-
bush (euphorbia), and succulent plants, whose foliage shines with
metallic lustre. Set in little ridges, the hedge-rows of pine-apple,
with its large pink and crimson fruit, passing, when ripe, into a
reddish-yellow, form a picturesque and pleasant fence. At a distance
from the town the paths become rough and solitary. Nearer, they are well
beaten by negroes of both sexes and all ages, carrying fuel or baskets
of fruit upon their heads, or bringing water from the wells, or
loitering under shady trees to cheapen the cocoa-nut, manioc, and
broiled fish, offered by squatting negresses for their refection.
SECTION 2.
Meteorological Notes—The Double Seasons, &c.
The characteristic of meteorology at Zanzibar, as generally the case in
the narrow equatorial zone, is the extreme irregularity of its
phenomena. Here weather seems to be all in confusion; hardly two
consequent years resemble each other. In 1853-4, for instance, the
seasons, if they may so be called, were apparently inverted; heavy
showers fell during the dries, and a drought occupied the place of the
wet monsoon. Sometimes the rains will begin with, this year (1857) they
ended with, a heavy burst. Now April is a fine month, then the downfall
will last through June.
I may also remark one great difference of climate between the eastern
and western coasts of intertropical Africa. Whilst Zanzibar is
supersatured with moisture, Angola, on the same parallel, is a
comparatively dry, sandy, and sunburnt region. Kilwa, upon the eastern
coast, and in S. lat. 8° 57′, is damp and steamy. S. Paulo de Loanda,
upon the opposite shore (S. lat. 8° 48′), suffers from want of water. We
find the same contrast in the South American continent. The middle
Brazil is emphatically a land of rains, whilst Peru and Chili require
artificial irrigation supplied by melted snow. Evidently the winds
charged with moisture, the N. E. and S. E. trades and their
modifications, discharge themselves upon the windward sides of
continents, especially when these are fringed with cold sierras, which
condense the vapour and render the interior a lee land.
In 1847 the Geographical Society of Bombay sent a barometer to Zanzibar,
and requested that a meteorological register might be kept. Their wishes
were not immediately carried into effect; but after a time the Eurasian
apothecary in charge of the Consulate filled up in a rude way during
nine months a weather-book, with observations of the barometer, of two
thermometers attached and unattached, of wet and dry bulbs, of
evaporation and of rainfall. In the Journal of the Royal Geographical
Society (xxiii. of 1853), Colonel Sykes published a ‘record, kept during
eleven months in 1850, of the indications of several intertropical
instruments at Zanzibar,’ unhappily without those of pressure.[38]
The result of nine months’ observations is that the thermometer shows a
remarkably limited range of temperature and an extreme variation of only
18°-19°. A storm, however, will make the mercury fall rapidly through
6°-7°. The climate is far more temperate than the inexperienced expect
to find so near the equator. It is within the limits of the true Trades.
The land and sea breezes laden with cool moisture blow regularly, and
the excessive humidity spreads a heat-absorbing steam-cloud between sun
and earth. The medium temperature of January is 83° 30′; of February,
the hottest month, 85° 86′ (according to Colonel Sykes 83° 40′); and of
March, 82° 50′. This high and little-varying mean then gradually
declines till July, the coolest month (77° 10′). The mean average of the
year is 79° 15′-90′. In September and October the climate has been
compared with that of southern Europe. On the other hand, the atmosphere
supports an amount of moisture unknown to the dampest parts of India.
The barometer, so near the equator, is almost uniformly sluggish and
quiescent. Its range diurnal and annual is here at a min. It seldom,
except under varying pressure of storms or tornadoes, rises or falls
above or below 30 inches at sea level, and a few tenths represent the
max. variation. It must be observed, however, on both coasts of Africa,
within 6°-7° of the Line, this instrument requires especial study for
nautical purposes. Here it is an imperfect indicator, because, affected
from great distances, it rises without fine weather and it falls without
foul. At Zanzibar the case of a whaling captain is quoted for wasting in
vain precautions nearly two months. Moreover, sufficient observations
have not yet been accumulated in the southern hemisphere. Where there is
so little expansion in the mercurial column the convexity and concavity
of the column-head must be carefully examined with a magnifying-glass,
and by a reflecting instrument the smallest change could be correctly
measured. The trembling of the aneroid needle, sometimes ranging through
a whole inch during the gusts of the highly electrical tornado, also
calls for observation. The sympiesometer is held to be even more
sensitive than the mercurial barometer, especially before storms, and
ignorance of its peculiarity has often ‘frightened a reef in’ at
unseasonable times. The same was found to be the case, in high
latitudes, by Lieut. Robertson, R.N., when sailing under Captain Ross
(1818), between N. lat. 51° 39′ and 76° 50′.
Observations with the altitude and azimuth determined the variation of
the needle in 1857 to be between 9°-10° (W.). If this be correct, it is
gradually easting. In 1823 Captain Owen found it to be 11° 7′ (W.).[39]
So, upon the opposite coast, the variation laid down in our charts of
1846 as 20° (W.) has gradually declined to between 18° 30′ and 19° (W.).
Of exceptional meteoric phenomena I can speak only from hearsay, no
written records existing upon the island. A single earthquake is
remembered. In the early rains of 1846, at about 4 P.M., a shock,
accompanied by a loud rumbling sound, ran along the city sea-front,
splitting the Sayyid’s palace, the adjacent mosque, and the side-walls
of the British Consulate, in. a direction perpendicular to the town. It
was probably the result of igneous disturbance below the coralline, and
it tends to prove that the island was originally an atoll: some,
however, have explained it by a land-slip. Three meteors are known since
1843. In December of that year a ball of fire was visible from windows
facing the north; it disappeared without a report. The most remarkable
was a bolis, which, about 6 P.M. on October 25, 1855, took a N.W. by W.
path, burned during ten or eleven minutes, and frightened the
superstitious burghers into fits. Water-spouts commonly appear during
the month of April, and in the direction of the mainland: the people
disperse them by firing guns.
Frost and snow are of course unheard of at Zanzibar, and hail, not
uncommon in the interior, never (?) falls upon the island or the coast.
During the wet season generally, especially when the heats are greatest,
the hills of Terrafirma are veiled with clouds, and sheet-lightning
plays over the horizon. The islanders assure the stranger that storms of
thunder and lightning are rare, and that few accidents happen from the
electric fluid. M. Alfred May, for instance, declares that thunder is
heard only three or four times a year. The same is said in West African
Yoruba, in parts of the Brazil, and even in Northern Syria—Damascus, for
instance. It would be curious to inquire what produces this uniform
immunity under climatic conditions so different. At Zanzibar, however,
the phenomenon is irregular as the seasons. I was told of several deaths
by the ‘thunderbolt,’ and in the year 1857 the S.W. monsoon was ushered
in almost daily by a tempest. Lieutenant-Colonel Hamerton, when sailing
about the island, lost by lightning his Baloch Sarhang (boatswain); he
himself felt a blow upon the shoulder like that of a falling block. No
blood appeared upon the side, but it was livid to the hip, and for some
days the patient was decidedly ‘shaky.’ Some explained his escape by his
wearing flannel; others by his standing near the davits of a longboat,
which were twisted like wax by the electric fluid.
The mainlands of Zanzibar and of Mozambique are subject, as might be
expected, to tornados, which much resemble those of the West African
coast. Accompanying the formation and the dispersion of the nimbus, they
are often violent enough to wreck small craft. Caught in a fine
specimen, I was able to observe all the normal phenomena,—the building
up of the warning arch, the white eye or gleam under the soffit, the
wind blowing off shore, the apparent periodicity of throbs, and the
frantic rage of the short-lived squall. The cyclones and hurricanes of
the East Indian Islands rarely extend to Zanzibar. During 14 years there
was but one tourbillon strong enough to uproot a cocoa-tree. It passed
over the city about midnight, overthrowing the Mábandani or roof-sheds,
and it was followed by a burst of rain. Colonel Sykes (loco cit.)
remarks, philosophically explaining the why, ‘Another peculiar feature
in the climatology of Zanzibar is that there is seldom any dew
experienced.’ The reverse is the case, as might be known by the strength
of the nightly radiation. Captain Guillain (i. 2, 72) declares that the
rosées which accompany the rains are sufficient for watering the ground,
and observes (p. 94), I presume concerning those who remain in the open
air, ‘Rester à terre entre huit heurs du soir et le lever du soleil
c’est s’exposer à une mort très probable, sinon certaine.’ The sunset,
never followed by twilight, is accompanied by a sudden coolness which,
as in equatorial, and even sub-tropical regions generally, causes a
rapid precipitation of vapour. The dews are cold and clammy, and the
morning shows large beads in horizontal streaks of moisture on
perpendicular surfaces. I often remarked the deposition of dew when
light winds were blowing; of course it did not stand in drops, but it
wetted the clothing. This I believe is an exception to the general rule.
At sunset the old stager will not sit or walk in the open air, although,
as in Syria, he will expose himself to it at nine or ten p. m., when the
night has acquired its normal temperature. As in the west coast
squadron, so here, there is an order that all men on deck after sunset
must wear their blanket-coats and trowsers, and many an unfortunate
sailor has lost his life by sleeping in the streets, thus allowing the
dew to condense upon his body while under the influence of liquor.
Experienced travellers have taught themselves, even in the hottest
seasons of the hottest equinoctial regions, to air the hut with a ‘bit
of fire’ before sundown and sunrise, and it is doubtless an excellent
precaution against ‘chills.’
Zanzibar Island, lying in S. lat. 6°, has the sun in zenith twice a
year: the epochs being early March and October; more exactly, March 4
and October 9. Hence it has two distinct summers; the first in February,
the second in September. It has double rains; the ‘Great Masika’ in
April to June, and the ‘Little Masika’ in October to November. It has
two winters; the shorter in December, and in July the longer, which is
much more marked than the former. There are only three months of N.E.
trade (Azyab)[40] to nine of S.E. and S.W. (Kausi). The regularity of
these seasons is broken by a variety of local causes, and there is ever,
I repeat, the normal instability of equinoctial climates. Theory appears
often at fault upon these matters. A fair instance is Mr Cooley’s
assertion, that about Kilima-njaro the ‘rainy season is also the hot
season.’ Theoretically, of course, the period of the sun’s northing and
of the great rains should be, north of the equator, the hot season; but
where tropical downfalls are heavy, the excessive humidity intercepting
the solar rays, and the valleys and swamps refrigerated by the torrents,
make the rainy season the cold weather. From June to September the
natives of Fernando Po (N. lat. 4°) die, like those of eastern
intertropical Africa, of catarrh, quinsey, and rheumatism. Even in India
the Goanese call the rains ‘o inverno,’ and Abba Gregorius makes the wet
weather the winter of Abyssinia. About Kilima-njaro the hot and dry
season opens with the end and closes with the beginning of the hot
monsoon.
The natives of Zanzibar distribute the year into five seasons. A far
simpler division here applicable, as in Western India, is made by those
local trades the monsoons, between whose two unequal lengths are long
intervals of calms and of variable winds. These are the Mausim or N.E.
monsoon, and the Hippalus or S.W.
1. The Kaskazi or Kazkazi (vulgarly Kizkazi), to which the Arabs limit
the term El Mausim (Monsoon), is _the_ season during which the Azyab
(ازيب) or N.E. trade blows. The wind begins about mid-November; from
mid-December to mid-February its strength is greatest, and it usually
ends about mid-March. In 1857, however, the Kaskazi opened with light
showers, and continued in full force till March 24; usually the last
vessels from Cutch and Bombay enter port about March 10. This is the
first of the two hot seasons, and midsummer may be placed in February
and March. A fine, cool sea-breeze from the N.E. usually prevails
between 8 a.m. and late in the afternoon. When it is absent the weather
is sultry and oppressive, the northerner feels suffocated; the least
exertion brings on profuse perspiration, and the cuticular irritation
produces boils and ‘prickly heat.’ The nights are close and stifling
enough to banish rest and sleep. As has been shown, the thermometer does
not stand high, but the frequent flashes of sheet-lightning playing over
the northern and western sky show a surcharge of electricity. The public
health would suffer severely but for the frequent cooling showers which,
especially at the end of the Kaskazi, are succeeded by several days of
pleasant weather. This is the agriculturist’s spring. Sesamum, holcus,
rice, and other cereals, are sown upon lands previously burned for
manure. It is the traveller’s opportunity for visiting the interior of
the island and the worst parts of the coast, but—‘bad is the best.’
2. The Msika (or Másika) Mku, Greater rain or rains. About the end of
March the change of monsoon is ushered in by heavy squalls from the S.E.
and by tornados blowing off land. Presently the Hippalus breaks, and
extends from early May into October. In May native craft make India
after a run of 20 to 25 days; after the end of August they rarely
attempt the voyage. This Kausi or Hippalus is usually called S.W.
monsoon, but it has mostly an eastern deflection, possibly modified by
the westerly land-breezes. The Arabs divide it, as will be seen, into
three portions. First, the Kaus proper,[41] in Kisawahili Kausi (قوسی),
from mid-April to early August, the period of the greatest strength.
Second, Kipupwe or first winter—July and early August; and third, the
Dayman, which ends the Kausi.
Presently appear the rains which have followed the northing sun. The
same observation was made by the Austrian mission on the White River in
N. lat. 4° 30′. On the coast we can distinctly trace their progress. In
1857 the downfall began in Feb. 15, at Usumbara (S. lat. 5°), where the
clouds are massed and condensed by a high plateau, leading to lofty,
snow-capped mountains. In 1854 I found that the rainy season opened at
Berberah of the Somal (N. lat. 10° 25′) on April 15; and in early June
they reach Bombay (N. lat. 18° 53′). Concerning the movement of the wet
season in inner intertropical Africa I have already written in the
Journal of the Royal Geographical Society (xxix. 207).
The heaviest rains at Zanzibar Island begin the wet season about mid-
April, and last 30 to 40 days; they do not end, however, till early
June. Some observers remark that the fall is greatest at low water and
during the ebb-tides of the Syzygies. It is, however, rare to have a
week of uninterrupted rain, as in eastern India and sometimes in the
Brazil. The discharge is exceedingly uncertain. Some years number 85
inches, others 108. During the first eight months of 1857 and the last
four months of 1858, we find a total of 120·21 inches. In 1859 it
reached 167, doubling the average of Bombay (76·55), and nearly trebling
that of Calcutta (56·83). We may compare these figures with those of
Europe and the United States. England has 31·97 inches; France, 25·00;
Central Germany, 20·00; Hungary, 16·93; Boston, 38·19 (about the same at
Beyrut in Syria); Philadelphia, 45·00; and St Louis, Mo., 31·97. Of
these 167 inches (1859), 104·25 fell during the Msika Mku. The number of
wet days ranges from 100 to 130 per annum. According to the people, rain
has diminished of late years; perhaps it is the result of felling
cocoas, and of disforesting the land for cloves. In 1857, the Great
Msika was preceded by a few days of oppressive heat, which ended (March
24) in a highly electrical storm, like those which usher in the rains of
western India, and suddenly the cool S.W. began to blow. For some time
we had daily showers, now from the N.E., then from the S.W., with high
winds and loud thunderings; the rains, however, did not show in earnest
before April 10.
The islanders like the Msika to open with showers strong enough to bind
the land, but not so violent as to carry off the manure deposited by the
year’s decayed vegetation. After this the water should fall in heavy
ropy torrents, with occasional breaks of sunshine and fine weather; when
this lasts thirty days, and is succeeded by frequent showers, good crops
are expected. The downfall is heavier in the interior of the island than
about the city, which, situated upon a point, escapes many a drenching.
It must, however, be borne in mind that the phenomena of the rains, like
those of the sea and air, are essentially irregular. In some seasons
there will be only half-a-dozen rainy afternoons; in others as many
rainy mornings. There are years of great drought, and there are seasons
when the sun does not appear for six weeks in succession. Usually heavy
rain is not expected after 11 A.M., and showers are rare after 2 P.M. As
I subsequently remarked in the east African interior—the Fluminenses of
the Brazil still preserve the tradition—there is a curious regularity
and periodicity in the hours of downfall, often extending over many
days. This phenomenon may have done much towards creating the ‘rain-
doctor.’
During the Msika the horizon is obscured, dangerously indeed for ships:
the wind veers round to every point of the compass; the sky is murky and
overcast; huge purple nimbi, like moving mountains, float majestically
against the wind, showing strong counter-currents in the upper aërial
regions. From afar the island appears smothered in blue mist, and often
the cloudrock splits into two portions, one of which makes for the
coast. Even during the rare days of sunshine the distances, owing to the
continuous humidity, are rarely clear, and the exhalations make
refraction extensive. A high tension of vapour is the rule. For the
first three hours after sunrise the land is often obscured by ‘smokes,’
a white misty fog, often deepening to a drizzling rain; this lasts until
10 A.M., about which time the sea-breeze begins to blow.
The Msika is much feared by the native population, and the interior of
the island becomes a hot-bed of disease. The animal creation seems to
breathe as much water as air. The want of atmospheric weight, and
consequently of pressure upon the surface of the body, renders the
circulation sluggish, robs man of energy, and makes him feel how much
better is sleep than waking. Europeans, speaking from effect, complain
that the ‘heavy’ air produces an unnatural drowsiness—it is curious to
see how many of our popular books make humidity increase the weight of
the atmospheric column. During this season the dews of sunset are deemed
especially fatal to foreigners. At times the body feels cold and clammy
when the thermometer suggests that it should be perspiring: super-
saturation is drawing off the vital heat. The lungs are imperfectly
oxygenized, and, in general belief, positive is exchanged for negative
electricity. The hair and skin are dank and sodden; indeed, a dry cutis
is an unattainable luxury. Iron oxydizes with astonishing rapidity;
shoes exposed to the air soon fall to pieces; mirrors are clouded with
steam; paper runs and furniture sweats; the houses leak; books and
papers are pasted together; ink is covered with green fur; linens and
cottons grow mouldy, and broadcloths stiffen and become boardy.
This excess of damp is occasionally varied by the extreme of dryness.
The hot wind represents the Khamasin of Egypt, the Sharki (or Sh’luk) of
Syria, the Harmattan of west Africa, and the Norte of the southern
Brazil, Paraguay, and the Argentine Confederation. At such times the air
apparently abounds in oxygen and in ozone. Cotton cloth feels hard and
crisp; even the water is cooled by the prodigious evaporation. Books and
papers curl up and crack, and strangers are apt to suffer from nausea
and fainting fits.
3. The Kipupwe, first winter or cold season—July and early August. The
bright azure of the sky, the surpassing clearness of the water, and the
lively green colours of the land, are not what we associate with the
idea of the ‘disease of the year.’ The Kausi or S.W. monsoon still
blows, but in this second or post-pluvial phase its strength is
diminished. As on the western coast the mornings are misty, the effect
of condensation and of excessive evaporation, the sun pumping up vapour
from the rapidly desiccating ground; but about four hours after sunrise
a strong sea-breeze sets in, giving a little life and elasticity to the
exhausted frame. When the ‘doctor’ fails the heat is oppressive, and the
sunsets are often accompanied by an unpleasant closeness. The beginning
of the Kipupwe is held to be universally sickly. The Hindus, who declare
that all cold coming from the south is bad, suffer from attacks of
rheumatism and pneumonia. The charms of the season induce Europeans to
despise the insidious attacks of malaria: they commit imprudences and
pay for them in severe fevers. The rare but heavy showers that now fall
are termed ‘Mcho;’ they separate the greater from the lesser Msika.
4. Daymán (in Kisawahili Daymáni) ends the Kausi or S. W. monsoon, and
extends through August and part of October. Though the sun is nearly
perpendicular the air is cooled by strong south-westerly breezes. At
this time yams, manioc, and sweet potatoes grow, making it a second
spring, whilst the harvest of rice and holcus assimilates it to the
temperate autumn.
5. The Vuli (Fuli)[42] or Msika Mdogo, second rains or Little Msika.
This season lasts but three weeks, beginning shortly after the sun has
crossed the zenith of Zanzibar in the southern declination, and
embracing part of October and November. It is not considered a healthy
time by the islanders. The autumnal rains are sometimes wanting upon the
continent, and the land then suffers as severely from drought as
northern Syria does when the ‘former rain’ fails. After the Vuli
recommences the Kaskazi, and the N. E. trade again blows. The sun is
distant, the thermometer does not range high, yet the temperature of
houses sheltered from the breeze becomes overpowering, and without the
‘doctor’ the city would hardly be habitable. At times the Trade freshens
to a gale that blows through the day. The Hindus suffer severely from
this ‘Báorá’ (blast), and declare that it brings on fits of ‘Mridi’
(refroidissement), here held dangerous. During the whole of the Azyab
monsoon the people prefer hot sun and a clear, which is always a
slightly hazy-blue, sky. They dislike the clouds and heavy showers
called Mvua[43] ya ku pandia, or harvest rains, which are brought up at
times by the N. N. West wind. On the other hand, when the Kausi or S.
West monsoon blows, they hold an overcast sky the best for health, and
they dread greatly the ‘rain-sun.’ The peasants take advantage of the
dryness, and prepare, by burning, the land for maize, sesamum, and rice.