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Published online by Cambridge University Press: 01 May 2009
The purpose of this communication is to supplement the author's paper on the “Classification of the European Rocks known as Permian and Trias,” which has appeared in recent numbers of this MAGAZINE. It is based on a short communication made to Section C. of the British Association at the recent meeting at Southampton, and has been expanded into the present paper at the request of the President of the Section, E. Etheridge, Esq., F.R.S.
page 495 note 1 Vide descriptive text of the Geologische Uebersichtskarte der Oesterrelchisehen Monarchie, Blatt No. 5, by Dr. Franz Ritter von Hauer.
page 495 note 2 Anleitung zu Geol. Beobachtungen in den Alpen, von G. W. Gümbel.
page 496 note 1 The earth-pillars (‘Erd-pyramiden’) of the neighbourhood are, or have been, severally capped with blocks of quartz-porphyry, but I think the finer materials which constitute them are more largely derived from the tuffs (clastic rocks) than from the crystalline rocks; both those of the Finsterbach near Lengmoos, and the group lower down near Bozen.
page 496 note 2 Vide Etudes Synthétiques de Géologie Expérimental, par Daubrée, A., pp.165–6.Google Scholar
page 496 note 3 Elemente der Geologie, 3rd edition, pp. 274, 275.Google Scholar
page 497 note 1 Third edition, 1878, p. 557.
page 497 note 2 Ibid., pp. 13, 14.
page 498 note 1 Vide GEOL. MAG. Sept. 1882.
page 498 note 2 Vide my former paperinrecent Numbers of this MAGAZINE.