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Floating obsidian and its implications for the interpretation of Pacific prehistory

Published online by Cambridge University Press:  02 January 2015

Dirk H. R. Spennemann
Affiliation:
Johnstone Centre of Parks, Recreation and Heritage, Charles Sturt University, PO Box 789, Albury NSW 2640, Australia
Wal R. Ambrose
Affiliation:
Division of Archaeology and Natural History, Australian National University, Canberra ACT 0200, Australia

Extract

A piece of pumice among drift material on Nadikdik Atoll, Marshall Islands, in far Micronesia had a large chunk of flakeable obsidian attached. As the atoll had been devastated by a typhoon and associated storm surge in 1905, the piece must have arrived by sea within the last 90 years. This and similar incidences of raw materials distributed by ocean drift show how sea-borne dispersal cannot be excluded offhand in the occurrence of obsidian in far-flung places, commonly attributed to human transport.

Type
Notes
Copyright
Copyright © Antiquity Publications Ltd. 1997

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References

Ambrose, W.R. 1978. The loneliness of the long distance trader in Melanesia, Mankind 11: 326–33.Google Scholar
Barnes, C.A., Bumpus, D.F., & Lyman, J.. 1948. Ocean circulation in Marshall Islands area, Transactions of the American Geophysical Union 29(6): 871–6.Google Scholar
Bellwood, P.S. & Koon, P.. 1989. ‘Lapita colonists leave boats unburned’: the question of Lapita links with Southeast Asia, Antiquity 63(240): 613–22.Google Scholar
Emery, K.O., Tracey, J.I. & Ladd, H.S.. 1954. Geology of Bikini and nearby atolls Part 1: Geology. Washington (DC): US Geological Survey. Professional Paper 260-A.Google Scholar
Golson, J. 1962. Polynesian navigation. Wellington: Reed.Google Scholar
Hintze, J.L. 1996. Number Cruncher Statistical System, version 6.0 Statistical system for Windows. Kaysvillu (UT): NCSS.Google Scholar
Irwin, G. 1992. The prehistoric exploration and colonisation of the Pacific. Cambridge: Cambridge University Press.CrossRefGoogle Scholar
Jeschke, C. 1905. Bericht über den Orkan in den Marschall-Inseln am 30. Juni 1905, Petermanns Mitteilungen 51: 248–9.Google Scholar
Levison, M., Ward, R.G. & Webb, J.W.. 1973. The settlement of Polynesia: a computer simulation. Canberra: Australian National University.Google Scholar
Reynolds, M.A.J.G. Best & Johnson, R.W.. 1980. 1953-57 eruption of Tuluman volcano: rhyolitic activity in the northern Bismark Sea. Port Moresby: Geological Survey of Papua New Guinea. Memoir 7Google Scholar
Sachet, M.-H. 1955. Pumice and other extraneous volcanic material on coral utolls. Washington (DC): Pacific Science Board. Atoll Research Bulletin 38.Google Scholar
Sharp, A. 1956. Ancient voyagers in Polynesia. Wellington: Polynesian Society.Google Scholar
Sharp, A. 1957. Ancient voyagers in the Pacific. Harmnndsworth: Penguin.Google Scholar
Spennemann, D.H.R. 1996. Gifts by the waves: a case of marine transport of obsidian to Nadikdik Atoli and the occurrence of other drift material in the Marshall Islands. Albury [NSW]: Charles Sturi University, The Johnstone Centre of Parks, Recreation and Heritage. Report 23.Google Scholar
Spennemann, D.H.R. & Marschner, I.M.. 1995. Association between ENSO and typhoons in the Marshall Islands, Disasters 19(3): 194–7.Google Scholar