. The Quarterly journal of the Geological Society of London. mmulitic rocks from the neighbourhood of Mount Eliashave also been examined. Some of them contain nummulites andOrbitoides in outward appearance not unlike those from Vernitza,but it has not been found practicable to isolate specimens goodenough and numerous enough to examine them properly forpurposes of identification. Three transparent slides cut from the rocks of Mount Elias havebeen examined. These contain, in addition to Nummulites andOrbitoides, Orbitolites (probably 0. complanata), Alveolina (nearA. oblonga), numerous Textilar
. The Quarterly journal of the Geological Society of London. mmulitic rocks from the neighbourhood of Mount Eliashave also been examined. Some of them contain nummulites andOrbitoides in outward appearance not unlike those from Vernitza,but it has not been found practicable to isolate specimens goodenough and numerous enough to examine them properly forpurposes of identification. Three transparent slides cut from the rocks of Mount Elias havebeen examined. These contain, in addition to Nummulites andOrbitoides, Orbitolites (probably 0. complanata), Alveolina (nearA. oblonga), numerous Textilarice, Biloculina, Polymorphism, Milio-lina, and several Globigerine and Rotaline forms. 1 Thomas Brown, Illustrations of the Fossil Conchology of Great Britain 1849, p. 37 & pi. xxvi, figs. 3-5; and DArchiac & Haime, Description desAnimaux fossiles du Groupe Nummulitique de llnde 1853, p. 146 & pi. ix,figs. ISa-lSg. 2 DArchiac & Haime, op. cit. p. 147 & pi. ix, figs. 14<x-14#, 15, & 15 a. Quart. Journ. Geol. Soc. Vol. LX, Pl. Fig. 5. Fig 6 xio. $^|fe- ?? ??^-
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Keywords: ., bookcentury1800, bookdecade1840, booksubjectgeology, bookyear1845
