Page 342 - A Hand book of Arabia Vol 1 (iii) Ch 6 -10
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                                                       CHAPTER X

                                                              NEJD


                                                              Area
  s. -
            *                 This region, is equivalent to Central Arabia, south of lat. 2/ Is.
                            and between (roughly) longitude 43° and 47° E. The name ‘ Nejcl ’
                            is used as convenient, although, to an Arab, it would not
                            signify merely what is intended here, but either Jebel Shammar
                            also and the high steppes west, or (in the strictest use) the high
                            steppe and desert alone.
                               Our ‘ Nejd ’, then, is bounded north by Jebel Shammar ; west
                            by the high steppes lying east of Hejaz and Asir; south by the
                            Great Desert ; cast by the Dahanah Desert lying to west of Hasa.
                            It is a loosely linked group of nine more or less settled districts
                            (from north to south), Qaslm, Sedeir, Woshm, ‘Aridh, Kharj, Harxq,
                            Aflaj, Saleyyil, and Dawasir. Nejd measures about 450 miles from
                            the extreme N. of Qaslm to the extreme S. of Dawasir, and some
                            200 miles from the W. of Woshm to the E. of Sedeir. But if we
                             follow its curving N. and S. axis, we get a length of well over
                             500 miles.

                                                      Physical Character

                                                            A. Relief
                               Physically Nejd falls into three parts :—
                               I. A northern valley region determined by the middle basin of
                             the Wadi Rummah, which lies SE. by N\\\, and including the lower
                  *.• •      courses of underground tributary drainage from left and ri<dit.
    m
                             This is Qaslm. The floor of this region, sandstone in the south
    *                        but becoming chalky in the north, is, to a large oxtent, covered
                             by drift-sand, but remains exposed and topped by sandy loam
                             in many considerable patches, where water is obtainable at a depth
                             of a few feet. The main Wadi itself is a wide depression, varvino*
                             in breadth from two miles to five hundred yards, least steeply
                             inclined on the left bank, and having a well-defined storm water­
                             course, which generally hugs its cliffy right bank.           This water-





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