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in irregular heaps. Others are grey and compact enough to take a high polish when cut. The syenite is generally coarse, although there is occasionally found a rich red variety of that stone. I did not see eurite or euritic porphyry except in small pieces, and the same may be said of the petrosilex and the milky and waxy quartz.21 In some parts, particularly between Yambu’ and Al-Madinah, there is an abundance of tawny yellow gneiss markedly stratified. The transition formations are represented by a fine calcareous sandstone of a bright ochre colour: it is used at Meccah to adorn the exteriors