Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-23T00:23:21.908Z Has data issue: false hasContentIssue false

A handaxe of Libyan Desert glass

Published online by Cambridge University Press:  02 January 2015

Extract

The handaxe of Libyan Desert glass (PL. XIIIb & FIG. I) was found on 23 June 1979, in the Sand Sea of S.W. Egypt, at latitude 25°o8' N, longitude 25° 35·5' E, near the southern boundary of the known distribution area of the glass. Lying just north of the Gilf Kebir, this part of the Sand Sea is characterized by an extensive field of linear dunes, trending almost exactly N-S, which are up to Ioom high, tens of km long, and separated by interdune corridors or ‘streets’ 2–5 km wide.

Type
Articles
Copyright
Copyright © Antiquity Publications Ltd 1982

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bosinski, G. 1967. Die mittelpalaolithischen Funde im westlichen Mitteleuropa, (Fundamenta, Reihe A, Band 4) (Cologne).Google Scholar
Caton-Thompson, G. 1946. The Aterian industry: its place and significance in the palaeolithic world, F. Roy. Anth. Inst., LXXVI, 2: 87130.Google Scholar
1952. Kharga Oasis in prehistory (London).Google Scholar
Clayton, P. A. 1951. The silica glass ofthe Libyan Desert, Bull. Inst. Fouad Ier da Dēsert, 1:2, 348.Google Scholar
Clayton, P. A. & Spencer, L. J. 1934. Silica glass from the Libyan Desert, Mineral. Mag., 23, 50810.Google Scholar
Ferring, C. R. 1975. The Aterian in North African prehistory, in (eds)Wendorf, F. & Marks, A. E. Problems in prehistory: North Africa and the Levant, 11326 (Dallas).Google Scholar
Gentner, W. , D. STÖRZER & Wagner, G. A.. 1969. New fission track ages of tektites and related glasses, Geochem. et Cosmochem. Acta, XXXIII, 107581.Google Scholar
Giegengack, R. F. & Issawi, B.. 1975. Libyan Desert silica-glass: a summary of the problem of its origin, Annals. Geol. Survey Egypt, V, 10518.Google Scholar
Klitsch, E. Harms, J. C. Lejal-Nicol, A. & List, F. K.. 1979. Major subdivisions and depositional environments of Nubia strata, southwestern Egypt, Amer. Assoc. Petroleum Geologists Bull., 63: 6, 96774.Google Scholar
Leakey, L. S. B. 1931. The stone age cultures of Kenya Colony (Cambridge).Google Scholar
Mchugh, W. P. 1975. Some archaeological results of the Bagnold-Mond expedition to the Gilf Kebir and Gebel ‘Uweinat, southern Libyan Desert, F. Near East Studies, 34:1, 3162.Google Scholar
Oakley, K. P. 1952. Dating the Libyan Desert silica-glass, Nature, 170: 4324, 4479.CrossRefGoogle Scholar
O’Keefe, J. A. 1976. Tektites and their origin (New York & Amsterdam).Google Scholar
Olsen, J. W. & Underwood, J. R. Jr. 1979. Desert glass: an enigma, Aramco World Mag., 30: 5, 25.Google Scholar
Peel, R. F. & Bagnold, R. A.. 1939. An expedition to the Gilf Kebir and ‘Uweinat, 1938, Geog. Fourn., XCIII, 281313.Google Scholar
Shaw, W. B. K. 1936. An expedition in the southern Libyan Desert, Geog. Fourn., LXXXVII, 193221.CrossRefGoogle Scholar
Spencer, L. J. 1939. Tektites and silica-glass, Mineral. Mag., 25: 167, 42540.Google Scholar
Störzer, D. & Wagner, G. A.. 1971. Fission track ages of North American tektites, Earth Planet. Set. Lett., 10. 43540.Google Scholar
Underwood, J. R., JR. 1979a. Review of Libyan Desert glasssouthwest Egypt and report on 1978 expedition, NASA Tech. Memo. 80339: 8790.Google Scholar
1979b. Libyan Desert glass: 1978 expedition, Kansas Acad. Sci. Trans., 82: 2, 101.Google Scholar
Underwood, J. R., JR. & Giegengack, R. F.. 1980. Meteorite from southwest Egypt: no apparent connection with origin of Libyan Desert glass, Geol. Soc. Am. Abstracts with Programs for 1980, 12:1, 17.Google Scholar
Wendorf, F. & Marks, A. E. (eds). 1975. Problems in prehistory : North Africa and the Levant (Dallas).Google Scholar