Allophane and imogolite are clay-sized minerals commonly associated with tephra deposits. They are also found in some non-tephric soils and sediments, as well as in streambeds and drains.
Definitions
Ross and Kerr (1934) showed that allophane was an X-ray amorphous material commonly associated with the clay-mineral halloysite. They suggested that “the name allophane should be restricted to mutual solid solutions of silica, alumina, water and minor amounts of bases but should include all such materials, even though the proportions of these constituents may vary.” Although this definition is still generally acceptable, some changes are required to (a) exclude imogolite, (b) allow for broad X-ray diffraction lines that are shown by allophane, and (c) allow for synthetic allophanes, that may not contain bases at low pH.
The definition given by Parfitt (1990a)is “Allophane is the name of a group of clay-size minerals with short-range-order which contain silica, alumina and water in...
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© 1978 Dowden, Hutchinson & Ross, Inc.
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L., R. (1978). Allophane and imogolite. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_2
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