Abstract
THE morphology of lateritic and ironstone concretions is generally attributed to soil texture1, groundwater movements2,3 and variations in the soil aggregates upon which deposition takes place4,5.
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References
Panton, W. P., Rep. Sixth Int. Congr. Soil Sci., 5, 421 (1956).
D'Hoore, J., Pub. I.N.E.A.C., Ser. Sci., 62, 116 (1954).
Crompton, E., J. Soil Sci., 3, 287 (1952).
Nye, P. H., J. Soil Sci., 6, 68 (1955).
Smith, L. L., J. Geol., 56, 222 (1948).
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Ho, R. Corrugated Iron Pan. Nature 180, 1276–1277 (1957). https://doi.org/10.1038/1801276a0
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DOI: https://doi.org/10.1038/1801276a0
