The Eye Of Yemen, To Quote Carlyle, Is A "Mountain Of Misery Towering Sheer Up Like A Bleak Pisgah, With

Outlooks only into desolation, sand, salt water, and despair." The camp is in a "Devil's Punchbowl," stiflingly hot during nine

Months of the year, and subject to alternations of sandstorm and Simum, "without either seed, water, or trees," as Ibn Batutah described it 500 years ago, unproductive for want of rain,--not a sparrow can exist there, nor will a crow thrive, [15]--and essentially unhealthy. [156] Our loss in operatives is only equalled by our waste of rupees; and the general wish of Western India is, that the extinct sea of fire would, Vesuvius-like, once more convert this dismal cape into a living crater.

After a day's rest--physical not spiritual, for the Somal were as usual disputing violently about the Abbanship [17]--I went with my comrades to visit an interesting ruin near the town. On the way we were shown pits of coarse sulphur and alum mixed with sand; in the low lands senna and colocynth were growing wild. After walking a mile south-south-east, from present Berberah to a rise in the plain, we found the remains of a small building about eight yards square divided into two compartments. It is apparently a Mosque: one portion, the sole of which is raised, shows traces of the prayer niche; the other might have contained the tomb of some saint now obsolete, or might have been a fort to protect a neighbouring tank. The walls are of rubble masonry and mud, revetted with a coating of cement hard as stone, and mixed with small round pebbles. [18] Near it is a shallow reservoir of stone and lime, about five yards by ten, proved by the aqueduct, part of which still remains, to be a tank of supply. Removing the upper slabs, we found the interior lined with a deposit of sulphate of lime and choked with fine drift sand; the breadth is about fifteen inches and the depth nine. After following it fifty yards toward the hills, we lost the trace; the loose stones had probably been removed for graves, and the soil may have buried the firmer portion.

Mounting our mules we then rode in a south-south-east direction towards the Dubar Hills, The surface of the ground, apparently level, rises about 100 feet per mile. In most parts a soft sand overlying hard loam, like work _en pise_, limestone and coralline; it shows evidences of inundation: water-worn stones of a lime almost as compact as marble, pieces of quartz, selenite, basalt, granite, and syenite in nodules are everywhere sprinkled over the surface. [19] Here and there torrents from the hills had cut channels five or six feet below the level, and a thicker vegetation denoted the lines of bed. The growth of wild plants, scanty near the coast, became more luxuriant as we approached the hills; the Arman Acacia flourished, the Kulan tree grew in clumps, and the Tamarisk formed here and there a dense thicket.

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