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On the Deposition of Calcareous Tufa in a Mountain Stream at Binn, Canton Valais, Switzerland

Published online by Cambridge University Press:  01 May 2009

W. A. Macfadyen
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Extract

Aggradation of the bed of a river is a well-known and common phenomenon in certain circumstances, but in the present case a mountain stream, whose grade is to steep that waterfall are present, is found flowing along the top of a well-marked but very irregular ridge to tufa. This is found in a little stream near the village of Binn, known to mineralogists for the rare minerals which occur in metamorphosed Triassic dolomite not far away up the valley of the Binna.

Type
Original Articles
Information
Geological Magazine , Volume 65 , Issue 1 , January 1928 , pp. 1 - 5
Copyright
Copyright © Cambridge University Press 1928

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References

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