Abstract
HAVING dealt with the movement of sand grains over the surface, with the resulting surface forms both on a small and on a large scale, and to some extent with the grading of the sand deposits laid down under constant controlled conditions, it remains to discuss the arrangement of the grains when they come finally to rest, and the evidence which can be thereby obtained as to the structure of the deposit.
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References
Bagnold, R. A. (1938). Nature, 142, p. 403.
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© 1973 Chapman and Hall Ltd
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Bagnold, R.A. (1973). The Internal Structure of Sand Deposits. In: The Physics of Blown Sand and Desert Dunes. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5682-7_16
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DOI: https://doi.org/10.1007/978-94-009-5682-7_16
Publisher Name: Springer, Dordrecht
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