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    21. Desert Sands

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    If deserts _have_ a fault (which their present biographer is far from
    admitting), that fault may doubtless be found in the fact that their
    scenery as a rule tends to be just a trifle monotonous. Though fine in
    themselves, they lack variety. To be sure, very few of the deserts of
    real life possess that absolute flatness, sandiness and sameness, which
    characterises the familiar desert of the poet and of the annual
    exhibitions--a desert all level yellow expanse, most bilious in its
    colouring, and relieved by but four allowable academy properties, a
    palm-tree, a camel, a sphinx, and a pyramid. For foreground, throw in a
    sheikh in appropriate drapery; for background, a sky-line and a
    bleaching skeleton; stir and mix, and your picture is finished. Most
    practical deserts one comes across in travelling, however, are a great
    deal less simple and theatrical than that; rock preponderates over sand
    in their composition, and inequalities of surface are often the rule
    rather than the exception. There is reason to believe, indeed, that the
    artistic conception of the common or Burlington House desert has been
    unduly influenced for evil by the accessibility and the poetic adjuncts
    of the Egyptian sand-waste, which, being situated in a great alluvial
    river valley is really flat, and, being the most familiar, has therefore
    distorted to its own shape the mental picture of all its kind elsewhere.
    But most deserts of actual nature are not all flat, nor all sandy; they
    present a considerable diversity and variety of surface, and their rocks
    are often unpleasantly obtrusive to the tender feet of the pedestrian
    traveller.

    A desert, in fact, is only a place where the weather is always and
    uniformly fine. The sand is there merely as what the logicians call, in
    their cheerful way, 'a separable accident'; the essential of a desert,
    as such, is the absence of vegetation, due to drought. The barometer in
    those happy, too happy, regions, always stands at Set Fair. At least, it
    would, if barometers commonly grew in the desert, where, however, in the
    present condition of science, they are rarely found. It is this dryness
    of the air, and this alone, that makes a desert; all the rest, like the
    camels, the sphinx, the skeleton, and the pyramid, is only thrown in to
    complete the picture.


    Now the first question that occurs to the inquiring mind--which is but a
    graceful periphrasis for the present writer--when it comes to examine in
    detail the peculiarities of deserts is just this: Why are there places
    on the earth's surface on which rain never falls? What makes it so
    uncommonly dry in Sahara when it's so unpleasantly wet and so
    unnecessarily foggy in this realm of England? And the obvious answer is,
    of course, that deserts exist only in
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