. Bulletin of the Natural Histort Museum. Geology series. 14 HOWARTH AND MORRIS. Fig. 8 The main Jurassic cliff, central Jebel Billum: the peak of Jebel Billum consists of Palaeocene Limestone of the Umm-er-Radhuma Formation: the vertical cliff in the foreground is formed by the Naifa and Hajar Formations, and is capped by the Qishn Formation (see Fig. 10 for detail).. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work
. Bulletin of the Natural Histort Museum. Geology series. 14 HOWARTH AND MORRIS. Fig. 8 The main Jurassic cliff, central Jebel Billum: the peak of Jebel Billum consists of Palaeocene Limestone of the Umm-er-Radhuma Formation: the vertical cliff in the foreground is formed by the Naifa and Hajar Formations, and is capped by the Qishn Formation (see Fig. 10 for detail).. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Natural History Museum (London). Andover : Intercept
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