Hostname: page-component-6766d58669-fx4k7 Total loading time: 0 Render date: 2026-05-19T23:58:05.764Z Has data issue: false hasContentIssue false

Semi-finished glass from Ile-Ife, Nigeria: implications for the archaeology of glass in sub-Saharan Africa

Published online by Cambridge University Press:  09 June 2020

Abidemi Babatunde Babalola*
Affiliation:
Centre of African Studies/McDonald Institute for Archaeological Research, University of Cambridge, UK
Adisa Benjamin Ogunfolakan
Affiliation:
A.G. Leventis Natural History Museum, Obafemi Awolowo University, Nigeria
Thilo Rehren
Affiliation:
Science and Technology in Archaeology and Culture Research Center, The Cyprus Institute, Cyprus UCL Institute of Archaeology, London, UK
*
* Author for correspondence: ✉ ab2577@cam.ac.uk
Rights & Permissions [Opens in a new window]

Abstract

The discovery of glass crucible fragments with the remains of semi-finished glass at Ile-Ife, Nigeria, has provided the first evidence for the existence of autonomous glass production in sub-Saharan Africa.

Information

Type
Project Gallery
Copyright
Copyright © Antiquity Publications Ltd, 2020
Figure 0

Figure 1. South-west Nigeria showing the location of Ile-Ife (figure by Abidemi Babalola).

Figure 1

Figure 2. Crucible fragments from Natural History Museum storage with suspected semi-finished glass: A) (sample IF0108) the well-made glass layer beneath the chunk of the semi-finished glass indicates that the crucible must have been used multiple times in glass production; B) (sample IF0113) the striations in the glass surface indicate scraping out of the soft glass paste while it was still hot, a common observation on many crucible fragments from Ile-Ife (figure by Abidemi Babalola).

Figure 2

Figure 3. Backscatter electron images of the semi-finished glass with heterogeneous matrix: A) (sample IF0113) molten upper part, and a more sintered lower part still showing the original particles of the raw material, namely quartz (darker grey) and feldspar (lighter grey), while in the fused part the light crystals are wollastonite (a transient crystal phase forming during glass making in regions rich in lime), indicating a higher lime content here. Some residual dark quartz is also still visible in the molten part; B) (sample IF0108) air bubbles appear as round black holes, the different grey shades in the matrix reflect different chemical compositions of the glass (figure by the authors).