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Published online by Cambridge University Press: 01 May 2009
All the phenomena hitherto noticed have been worked out for the case of rocks altered in situ, but they also take place in the products of transport resulting from the demolition of laterites in situ.
1 Trans. Inst. Min. Met., xix, p. 454, 1910.
2 Geol. Mag., 1903, pp. 61–4.