The Transition Formations Are Represented By A Fine Calcareous Sandstone Of A Bright Ochre Colour:

It is used at Meccah to adorn the exteriors of houses, bands of this stone being here and there inserted into the courses of masonry.

There is also a small admixture of the greenish sandstone which abounds at Aden. The secondary formation is represented by a fine limestone, in some places almost fit for the purposes of lithography, and a coarse gypsum often of a tufaceous nature. For the superficial accumulations of the country, I may refer the reader to any description of the Desert between Cairo and Suez.

[FN#1] The distance from Baghdad to Al-Madinah is 180 parasangs, according to ’Abd al-Karim: “Voyage de l’Inde, a la Mecque;” translated by M. Langles, Paris, 1797. This book is a disappointment, as it describes everything except Al-Madinah and Meccah: these gaps are filled up by the translator with the erroneous descriptions of other authors, not eye-witnesses. [FN#2] Here, it is believed, was fought the battle of Buas, celebrated in the pagan days of Al-Madinah (A.D. 615). Our dictionaries translate “Ghadir” by “pool” or “stagnant water.” Here it is applied to places where water stands for a short time after rain. [FN#3] Travels in Arabia, vol. 2, p, 217. The Swiss traveller was prevented by sickness from visiting it. The “Jazb al-Kulub” affords the following account of a celebrated eruption, beginning on the Salkh (last day) of Jamadi al-Awwal, and ending on the evening of the third of Jamadi al-Akhir, A.H. 654.

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