A Narrative Of Captivity In Abyssinia With Some Account Of The Late Emperor Theodore, His Country And People By Henry Blanc
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About Four Miles North Of Massowah Is Haitoomloo, A Large Village
Of About A Thousand Huts, The First Place Where We Meet With Sweet
Water; A Mile And A Quarter Further Inland We Came Upon Moncullou,
A Smaller But Better Built Village.
A mile westward of the last
place we find the small village of Zaga.
These, with a small hamlet
east of Haitoomloo, constitute all the inhabited portions of this
sterile region. The next village, Ailat, about twenty miles from
Massowah, is built on the first terrace of the Abyssinian range,
600 feet above the level of the sea. All these villages are
situated in the midst of a sandy and desolate plain; a few mimosas,
aloes, senna plants, and cactuses struggle for life in the burning
sand. The country residences of the English and French consuls shine
like oases in this desert, great pains having been taken to introduce
trees that thrive even in such a locality.
[Illustration: Grove House at Moncullou.]
The wells are the wealth of the villages - their very existence.
Most probably, huts after huts have been erected in their vicinity
until the actual prosperous villages have arisen, surrounded as
they are on all sides by a burnt and desert tract. The wells number
about twenty. Many old ones are closed, but new ones are frequently
dug, so as to keep up a constant supply of water. The reason old
wells are abandoned is, that after a while the water becomes very
brackish. In a new well the water is almost sweet. The water obtained
from these wells proceeds from two different sources: First, from
the high mountains in the vicinity. The rain filters and impregnates
the soil, but not being able to soak beyond a certain depth, on
account of the volcanic rocks of the undersoil, forms a small stratum
always met with at a certain depth. Secondly, from the sea by
filtration. The wells, though about four miles from the shore, are
only from twenty to twenty-five feet deep, and consequently on or
below the level of the sea.
The proof of an undercurrent of water, due to the presence of the
high range of mountains, becomes more apparent as the traveller
advances into the interior; though the soil is still sandy and
barren, and little vegetation can as yet be seen, trees and shrubs
become more plentiful, and of a larger size. A few miles farther
inland, even during the summer months, it is always possible to
obtain water by digging to the depth of a few feet in the dried-up
bed of a water-torrent.
It often struck me that what artesian wells have done for the Sahara
they could equally accomplish for this region. The locality seems
even more favourable, and there is every hope that, like the great
African desert, the now desolate land of Samhar could be transformed
into a rich date-bearing land.
Taken as they are; these wells could certainly be improved. On our
arrival at Moncullou, we found the water of the well belonging to
the consular residence scarcely used, on account of its very brackish
taste; we had the well emptied, a large quantity of saltish sand
removed, and we dug deeper until large rocks appeared. The result
was that we had the best well in the place, and requests for our
water were made by many, including the Pasha himself. Unfortunately,
the forefathers of the present Moncullites never did such a thing
to their wells, and as all innovations are distasteful to a
semi-civilized race, the fact was admired, but not imitated.
Arkiko, at the extremity of the bay, is much nearer the mountains
than the villages situated north of Massowah, but the village is
built almost on the beach itself; the wells, not a hundred yards
from the sea, are also much more superficial than those on the
northern side, consequently the sea-water, having a much shorter
distance to filter through, retains a greater proportion of saline
particles, and I believe, were, it not for the presence of a small
quantity of sweet water from the hills, it would be quite unpalatable.
In the neighbourhood of Maasowah there are several hot mineral
springs. The most important are those of Adulis and Ailat. In the
summer of 1865 we made a short trip to Annesley Bay, to inspect the
locality. The ruins of Adulis are several miles from the shore,
and, with the exception of a few fragments of broken columns, contain
no traces of the former important colony. The place was even hotter
than Massowah; there was no vegetation, no trace of habitations on
that desolate shore. Fancy our surprise, on reaching the same spot
in May, 1868, to find piers, railways, bazaars, &c. - a bustling
city had sprung out of the wilderness.
The springs of Adulis [Footnote: A short time before our departure
for the interior, some of the water of the hot springs of Adulis
was collected and forwarded to Bombay for analysis.] are only a few
hundred yards from the sea-shore, surrounded by a pleasing green
patch covered with a vigorous vegetation, the rendezvous of myriads
of birds and quadrupeds, who, morning and evening, swarm thither
to quench their thirst.
At Ailat [Footnote: Water collected and sent to Bombay, November,
1864.] the hot spring issues from basaltic rocks on a small plateau
between high and precipitous mountains. At the source itself the
temperature is 141 Fahrenheit, but as the water flows down the
different ravines, it gradually cools until it differs in no way
from other mountain streams. It is palatable, and used by the
inhabitants of Ailat for all purposes: it is also highly esteemed
by the Bedouins. On account of its medicinal properties, numbers
resort to the natural baths, formed of hollowed volcanic roots, for
the relief of every variety of disease. From what I could gather,
it appears to prove beneficial in chronic rheumatism and in diseases
of the skin. Probably in these cases any warm water would act as
well, considering the usual morbid condition of the integument in
those dirty and unwashed races.
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