Article contents
On the Deposition of Calcareous Tufa in a Mountain Stream at Binn, Canton Valais, Switzerland
Published online by Cambridge University Press: 01 May 2009
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
- Copyright
- Copyright © Cambridge University Press 1928
References
BIBLIOGRAPHY
- 4
- Cited by