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PRINGSHEIM, E. G.
1949.
IRON BACTERIA.
Biological Reviews,
Vol. 24,
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Published online by Cambridge University Press: 15 September 2014
Throughout Lanarkshire and Renfrewshire many streams and rivulets have beds which are deep reddish-brown in colour. This colour is due to the deposition of ferric hydroxide, and in some cases the deposition is so great that the course of the stream (if a small one) is hindered, and therefore it must be periodically cleared.