Geological Magazine: Volume 7 -

I.—Studies in Fossil Botany. By Dukinfield Henry Scott, M.A., Ph.D., F.R.S., F.G.S., Honorary Keeper of the Jodrell Laboratory, Royal Gardens, Kew. pp. xiii, 553, with 151 illustrations. (London: A. & C. Black, 1900.)
R. K.
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01 May 2009, pp. 567-571
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IX.—Two New Species of Ostracoda of Tithonian Age from Nesselsdorf, Austria
Frederick Chapman
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01 May 2009, pp. 325-326
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The following descriptions of Ostracoda from the Tithonian of Austria relate to specimens kindly forwarded to me by Dr. M. Remeš. They were obtained, together with numerous other fossils, including Foraminifera, from the Red Limestone of Nesselsdorf.

IV.—General Report on the Work carried on by the Geological Survey of India for the period from April 1, 1898, to March 31, 1899. Under the direction of C. L. Griesbach C.I.E., F.G.S. Large 12mo; pp. 91. (Calcutta, 1899.)
T. R. J.
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01 May 2009, pp. 81-82
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The Geological Survey of Egypt
M. Blanckenhorn
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01 May 2009, p. 192
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IX.—Firstfruits of a Geological Examination of Snowdon
J. R. Dakyns
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01 May 2009, pp. 267-273
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Ars longa, vita brevis. This is especially true when one reaches the age of 64. I therefore commit to paper some of the results of a geological investigation of Snowdon on which I am engaged. I start of course from the work of Messrs. Ramsay and Selwyn embodied in the Geological Survey Map of Snowdon and Ramsay's memoir on North Wales. To make what I have to say clear I may state that the rocks of Snowdon are by Ramsay and Selwyn divided into three principal groups, viz.: A, an upper felsitic lava ; an intermediate band (B) of bedded fossiliferous rocks of Bala age, containing much volcanic material, called the calcareo-felspathic ashy series ; and a lower mass (C) of felsitic rocks. This lower mass is in some places divided by sedimentary bands consisting of slates and grits. Below C come blue slates and grits, with occasional volcanic bands, D; and below D the great mass of volcanic rocks (E) which form Glyder Fach and Y Tryfan.

GEO volume 7 issue 8 Front matter
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01 May 2009, pp. f1-f6
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The Age of the Raised Beach of Southern Britain
Frederick Chapman
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01 May 2009, p. 528
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Alphonse Milne-Edwards
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01 May 2009, pp. 478-479
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Reports and Proceedings
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01 May 2009, pp. 427-429
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V.—The Palæontographical Society of London: Annual Volume (LIII) for 1899. Issued 12, 1899.
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01 May 2009, pp. 82-85
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Some Snowdon Tarns
J. R. Dakyns
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01 May 2009, p. 143
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Reports and Proceedings
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01 May 2009, pp. 235-238
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III.—Fauna der Gaskohle und der Kalksteine der Permformation Böhems, von DrAnt. Fritsch, F.R.G.S. Bd. iv, Heft 1, Myriopoda, Pars 1; and Bd. iv, Heft 2, Myriopoda, Pars 2, Arachnoidea. 4to; pp. 1–32 and 33–64, pls. cxxxiii–cxliv and cxlv–cliii. (Prague, 1899.)
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01 May 2009, pp. 36-38
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GEO volume 7 issue 4 Front matter
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01 May 2009, pp. f1-f6
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I.—On a Collection of Stone Implements in the Mayer Museum, made by Mr. H. W. Seton-Karr in the Mines of the Ancient Egyptians, discovered by him on the Plateaux of the Nile Valley. By Henry O. Forbes, LL.D., Director of Museums to the Corporation of Liverpool. Reprinted from Bulletin Liverpool Museum, II, Nos. 3 and 4 (20th January, 1900). With Illustrations.
T. R. J.
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01 May 2009, pp. 326-329
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II.—The Calabro-Sicilian Earthquake of November 16, 1894 - (1) G. Mercalli, “I terremoti della Calabria meridionale e del Messinese”: Memorie della Soc. Ital. delle Scienze, vol. xi (1897), pp. 1–154. - (2) A. Riccò, “Riassunto della sismografia del terremoto calabrosiculo del 16 novembre, 1894”: Rend. della R. Accad. dei Lincei, vol. viii (1899), pp. 3–12, 35–45. - (3) P. Tacchini, “Terremoto calabro-messinese del 16 novembre, 1894”: Rend. della R. Accad. dei Lincei, vol. iii (1894), pp. 275–277. - (4) P. Tacchini, “Sulla registrazione a Roma del terremoto calabromessinese del 16 novembre, 1894”: Rend. della R. Accad. dei Lincei, vol. iii (1894), pp. 365–367. - (5) Boll. Meteor. dell' Uff. Centr. di Meteorologia e Geodinamica, Supplemento 113.
C. Davison
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01 May 2009, pp. 571-573
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X.—Diagram of Composition of Igneous Rocks
H. Warth
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01 May 2009, pp. 273-275
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Recent studies about the average chemical composition of larger numbers of igneous rocks in the aggregate have shown that figures obtained from any one hundred or more samples are very similar, in fact practically equal. (See A. Harker, “On the Average Composition of British Igneous Rocks”: Geol. Mag., No. V, May, 1899.) This will be found also the case when comparing the following average which I calculated from the analysis of igneous rocks compiled by Roth in his “Petrographie der plutonischen Gesteine.”

James Thomson, F.G.S.
T. R. J.
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01 May 2009, pp. 479-480
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GEO volume 7 issue 11 Front matter
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01 May 2009, pp. f1-f6
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II.—A Monograph of Christmas Island (Indian Ocean): Physical Features and Geology. By C. W. Andrews. With descriptions of the Fauna and Flora by numerous contributors. 8vo; pp. xiii, 337, 22 plates, 1 map, text illustrated. (London: printed by order of the Trustees of the British Museum, 1900.)
B. B. W.
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01 May 2009, pp. 330-331
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Volume 7 - May 1900

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