PALEOLITHIC MAN AND THE NILE VALLEY IN UPPER AND MIDDLE EGYPT: a study of the region during Pliocence and Pleistocene times. By K. S. Sandford. (University of Chicago Oriental Institute Publications, vol. 18). University of Chicago Press, Chicago; Cambridge University Press, 1934. pp. xxii, 131, with 39 plates and coloured map, and 25 text-figures. 31s 6d.

W. B. Wright

doi:10.1017/S0003598X00010620

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PALEOLITHIC MAN AND THE NILE VALLEY IN UPPER AND MIDDLE EGYPT: a study of the region during Pliocence and Pleistocene times. By K. S. Sandford. (University of Chicago Oriental Institute Publications, vol. 18). University of Chicago Press, Chicago; Cambridge University Press, 1934. pp. xxii, 131, with 39 plates and coloured map, and 25 text-figures. 31s 6d.

Volume 9, Issue 35
W. B. Wright
DOI: https://doi.org/10.1017/S0003598X00010620

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PALEOLITHIC MAN AND THE NILE VALLEY IN UPPER AND MIDDLE EGYPT: a study of the region during Pliocence and Pleistocene times. By K. S. Sandford. (University of Chicago Oriental Institute Publications, vol. 18). University of Chicago Press, Chicago; Cambridge University Press, 1934. pp. xxii, 131, with 39 plates and coloured map, and 25 text-figures. 31s 6d.

Volume 9, Issue 35
W. B. Wright
DOI: https://doi.org/10.1017/S0003598X00010620

To save this article to your Google Drive account, please select one or more formats and confirm that you agree to abide by our usage policies. If this is the first time you used this feature, you will be asked to authorise Cambridge Core to connect with your Google Drive account. Find out more about saving content to Google Drive.

PALEOLITHIC MAN AND THE NILE VALLEY IN UPPER AND MIDDLE EGYPT: a study of the region during Pliocence and Pleistocene times. By K. S. Sandford. (University of Chicago Oriental Institute Publications, vol. 18). University of Chicago Press, Chicago; Cambridge University Press, 1934. pp. xxii, 131, with 39 plates and coloured map, and 25 text-figures. 31s 6d.

Volume 9, Issue 35
W. B. Wright
DOI: https://doi.org/10.1017/S0003598X00010620

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