The Inhabitants Being Mussulmans, Water Is The Ordinary Beverage; Tej And Araki (Made From Honey) Can, However, Be Purchased In The Bazaar.

The limited supply of water obtained from the few remaining tanks is quite inadequate to meet the wants of

Even a small portion of the community; water is consequently brought in daily from the wells a few miles north of Massowah, and from Arkiko. The first is brought in leather bags by the young girls of the village; the latter conveyed in boats across the bay. The water in both cases is brackish, that from Arkiko highly so. For this reason, and also on account of the greater facility in the transport, it is cheaper, and is purchased only by the poorer inhabitants.

To avoid useless repetitions, before speaking of the population, climate, diseases, &c., a short account of the immediate neighbourhood is necessary.

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.

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