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Ruxton, B. P. (1958) Weathering and Subsurface Erosion in Granite at The Piedmont Angle, Balos, Sudan. Geological Magazine, 95 (5) 353-377 doi:10.1017/s0016756800062944

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Reference TypeJournal (article/letter/editorial)
TitleWeathering and Subsurface Erosion in Granite at The Piedmont Angle, Balos, Sudan
JournalGeological Magazine
AuthorsRuxton, B. P.Author
Year1958 (October)Volume95
Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800062944
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Mindat Ref. ID248802Long-form Identifiermindat:1:5:248802:2
GUID0
Full ReferenceRuxton, B. P. (1958) Weathering and Subsurface Erosion in Granite at The Piedmont Angle, Balos, Sudan. Geological Magazine, 95 (5) 353-377 doi:10.1017/s0016756800062944
Plain TextRuxton, B. P. (1958) Weathering and Subsurface Erosion in Granite at The Piedmont Angle, Balos, Sudan. Geological Magazine, 95 (5) 353-377 doi:10.1017/s0016756800062944
In(1958, October) Geological Magazine Vol. 95 (5) Cambridge University Press (CUP)
Abstract/NotesAbstractSub-surface erosion is intensely active in weathered granite debris at the scarp foot of Jebel Qasim. Powerful flushes of sub-surface water after heavy rain remove much of the decomposing feldspar partly by solution and partly by mechanical eluviation. The sedentary debris gradually contracts as the feldspar is removed and when removal is nearing completion the debris may become compacted. The compacted debris occupies less than 40 per cent by volume of the granite from which it was derived.The upper fringing pediment around this hill is mantled by moist incoherent debris holding small local pockets of water which persist throughout the dry season. Annual recharge of this sub-surface water ensures intense weathering in the debris.The combination of intense weathering and sub-surface erosion with ensuing contraction of the debris occurring just below the piedmont angle may be sufficient to explain the maintenance of this angle during slope retreat.


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