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The Steinheim Basin and the Pretoria Salt Pan. Volcanic or Meteoric Origin?

Published online by Cambridge University Press:  01 May 2009

Herbert P. T. Rohleder
Affiliation:
Tanga, Tanganyika Territory.

Extract

When looking through the bibliography referring to the crypto– volcanic phenomena of Swabia we find that it has been quite customary to explain the origin of the “Steinheim Basin” by the well–known facts which have been ascertained in the Ries of Nördlingen. When doing so one important fact has been deliberately ignored, viz, that only the Steinheim basin is actually cryptovolcanic, whereas the Ries of Nördlingen exhibits undeniable proofs of extensive volcanic activity. There are rhyolitic tuffs, weathered– out lava cords and lava slabs, partly absorbed crystalline rocks, et alia. In the case of the Ries of Nördlingen the explanation of the vast caldera and the various geologic abnormalities must obviously be sought in volcanic activity.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1933

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References

BIBLIOGRAPHY

(1)Quenstedt, F. von. “Das Steinheimer Becken,Jahreshefte des Vereins fur vaterländische Naturkunde in Württemberg, 1866, 116.Google Scholar
(2)Fraas, E. “Der geologische Aufbau des Steinheimer Beekens,” Jahreshefte des Vereins fur vaterländische Naturkunde in Württemberg, 1900, 47.Google Scholar
(3)Branca, W. and Fraas, E.Das kryptovulcanische Becken von Steinheim,” Abhandlungen der kgl. preussischen Akademie der Wissenschaften, 1905, 1.Google Scholar
(4)Gottschick, F. “Aus dem Tertiärbecken von Steinheim,” Jahreshefte des Vereins für vaterländische Naturkunde in Württemberg, 1911.Google Scholar
(5)Branca, W. “Aufpressung und Explosion, oder nur Explosion im vulkanischen Ries bei Nördlingen,” Z. deutsch. geol. Ges., 1913.Google Scholar
(6)Haussmann, Die erdmagnetischen Elemente von Württemberg und Hohenzollern. Stat. L. A.; Stuttgart, 1913.Google Scholar
(7)Kranz, W. “Das Problem des Steinheimer Beekens,” Jahresberichte und Mitteilungen des oberrheinischen geologischen Vereins, 1914.CrossRefGoogle Scholar
(8)Kranz, W.Auspressung und Explosion oder nur Explosion im vulkanischen Ries von Nördlingen und im Steinheimer Becken,” Zeits. deutsch. geol. Ges., 1914.Google Scholar
(9)Klähn, F. “Das Steinheimer Becken,“ Zeits. deutsch. geol. Ges., 1922.Google Scholar
(10)Bentz, A.Neues zum Problem des Steinheimer Beekens,” Centralblatt für Mineralogie, 1923.Google Scholar
(11)Wagner, Percy A.The Pretoria Saltpan, a Soda Caldera,” Memoir No. 20, Geol. Survey, Union of South Africa, 1922.Google Scholar
(12)Saltpan, (Excursion). Compte Rendu, International Geological Congress, XV Session, South Africa. Pretoria,1929.Google Scholar
(13)“The Union of South Africa,” Handbuch der regionalen Geologic, Heidelberg, 1929, 157.Google Scholar
(14)DrSpencer, L. J., “Meteorite Craters as Topographical Features on the Earth's Surface,” Geogr. Journal, March, 1933.CrossRefGoogle Scholar
(15)Maclaren, Malcolm.Lake Bosumtwi, Ashanti,” Geogr. Journal, 1931, lxxviii.Google Scholar
(16)Kaljuvee, J. “Die Gross-Probleme der Geologie,” Tallin (Reval), 1933.Google Scholar
(17)Rohleder, H. P. T.Meteor Krater (Arizona)—Salzpfanne (Transvaal)— Steinheimer Becken,” Zeitschr. d. deutsch. geol. Ges., 1933.Google Scholar