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- W2005526709 abstract "Amplification is made to some of Butzer's comments on various Pleistocene ‘periglacial’ phenomena in southern Africa. In particular, the ‘nivation’ cirques occurring above 2,000 m in the Drakensberg-Lesotho upland are now thought to have been formed by a combination of frost-shattering and solifluction wasting. Because of a gradational sequence from purely frost-shattered forms in central Lesotho to pronounced cirques in the Drankensberg, a lateral palaeoclimatic variation is suggested with a somewhat higher precipitation in the latter area. This contention is supported by palaeosol evidence." @default.
- W2005526709 created "2016-06-24" @default.
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- W2005526709 date "2008-01-16" @default.
- W2005526709 modified "2023-10-16" @default.
- W2005526709 title "Some Pleistocene periglacial problems in southern Africa" @default.
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- W2005526709 doi "https://doi.org/10.1111/j.1502-3885.1973.tb00249.x" @default.
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