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II.—Notes on the Structure and Physiography of the Tarntal Mass

Published online by Cambridge University Press:  01 May 2009

Alfred P. Young
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Extract

The mountain mass known as the Tarntaler Köpfe, situated about 20 kilometres south-east of Innsbruck, is distinctly isolated from other high ground in the vicinity. The peaks rise to heights approaching 2900 metres above sea-level. The geologic features above the level of 2000 metres are of special interest. The adjacent country is occupied by crystalline phyllites, chiefly displayed on the north, and highly foliated calcareous schists developed mostly on the south of the mountain.

Type
Original Articles
Information
Geological Magazine , Volume 6 , Issue 8 , August 1909 , pp. 339 - 346
Copyright
Copyright © Cambridge University Press 1909

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References

page 340 note 1 Young, A. P.,“Stratigraphy and Structure of the Tarnthal Mass”: Q.J.G.S., 11, 1908, vol. lxiv, pp. 596–603.CrossRefGoogle Scholar

page 340 note 2 “Beiträge zur Geognosie Tirols”: Zeitschrift des Ferdinandeum, 1859.

page 340 note 3 Rothpletz, A., Querschnitt durch die Ostalpen, 1894, p. 75Google Scholar. The fossils named are: Terebratula gregaria, Modiola minuta, Gervillia præcursor, Corbula alpina, Pecten sp., Thecosmilia cf. fenestrata, Reuss, and cf. Convexastræa Azzarolæ, Stopp.

page 342 note 1 Penck, & Brückner, , Die Alpen im Eiszeitalter, about 1908, p. 1143.Google Scholar

page 344 note 1 Kerner, , “Der Carbonflora des Steinacherjoches”: Jahrbuch der Reichsanstalt, Wien, 1897.Google Scholar

page 345 note 1 This modifies somewhat the hypothesis (a) (p. 603 of last year's paper) offered before the discovery of the Mieselkopf occurrence.