The Land of Midian — Volume 2 by Sir Richard Francis Burton
page 68 of 325 (20%)
page 68 of 325 (20%)
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This northern portion had been visited by Dr. Wallin; the other
two-thirds of the march lay, I believe, over untrodden ground. We brought back details concerning the three great parallel Wadys; the Salma, the Damah, that "Arabian Arcadia," and the 'Aslah-Aznab. We dug into, and made drawings and plans of, the two principal ruined cities, Shuwak and Shaghab, which probably combined to form the classical important sites, El-Khandaki and Umm Amil. The roads of this region, and indeed of all Midian, are those of Iceland without her bogs and snows: for riding considerations we may divide them into four kinds:-- 1. Wady--the Fiumara or Nullah; called by travellers "winter-brook" and "dry river-bed." It is a channel without water, formed, probably, by secular cooling and contraction of the earth's surface, like the fissures which became true streams in the tropics, and in the higher temperate zones. Its geological age would be the same as the depressions occupied by the ocean and the "massive" eruptions forming the mountain-skeleton of the globe. Both the climate and the vegetation of Midian must have changed immensely if these huge features, many of them five miles broad, were ever full of water. In modern days, after the heaviest rains, a thin thread meanders down a wilderness of bed. The Wady-formation shows great regularity. Near the mouth its loose sands are comfortable to camels and distressing to man and mule. The gravel of the higher section is good riding; the upper part is often made impassable by large stones and overfalls of rock; and the head is a mere couloir. Flaked clay or mud show the |
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