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The Likpe Kukurantumi Archaeological Project (Ghana): exploring the abandoned earthwork settlement

Published online by Cambridge University Press:  25 March 2026

Patricia Ayipey*
Affiliation:
Institute of Archaeology, University of South Bohemia in Ceske Budejovice, Czechia Laboratory of Archaeobotany and Paleoecology, University of South Bohemia in Ceske Budejovice, Czechia
Alexa Höhn
Affiliation:
Institute of Archaeological Sciences, Goethe-Universität Frankfurt am Main, Germany
Dela Kuma
Affiliation:
Department of Anthropology, University of Pittsburgh, USA
Jaromír Beneš
Affiliation:
Institute of Archaeology, University of South Bohemia in Ceske Budejovice, Czechia Laboratory of Archaeobotany and Paleoecology, University of South Bohemia in Ceske Budejovice, Czechia
*
Author for correspondence: Patricia Ayipey ayipep00@jcu.cz
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Abstract

A community-based initiative in Ghana has mapped and partially excavated an earthwork site in the Oti region. Radiocarbon dating shows that the site was occupied between the fifteenth and eighteenth centuries AD, while archaeo- and ethnobotanical research connects historical plant use with modern practices, contributing to our understanding of West African earthworks.

Information

Type
Project Gallery
Copyright
© The Author(s), 2026. Published by Cambridge University Press on behalf of Antiquity Publications Ltd

Introduction

The Likpe Kukurantumi Archaeological Project (LKAP) is a multidisciplinary, community-based archaeological project in Ghana and its primary goal is to better understand the earthwork site, local vegetation, the chronology of the settlement and how the people interacted with their environment before and after the Atlantic era (AD 1450–l900). Research on earthworks in Ghana is essential for understanding past West African societies. Typical earthwork sites consist of a ditch flanked by one or two banks. Earthworks in the Birim South District, Kwabibirem District, West Akim District and the southern part of Ghana have received some attention (Junner Reference Junner1931; Davies Reference Davies1961; Kiyaga-Mulindwa Reference Kiyaga-Mulindwa1978, Reference Kiyaga-Mulindwa1982; Chouin Reference Chouin2009; Boachie-Ansah Reference Boachie-Ansah2010, Reference Boachie-Ansah and Anquandah2014; Biveridge Reference Biveridge2011), but the Likpe Kukurantumi Earthwork, the first earthwork site in the eastern part of Ghana (Oti region), has not previously been explored (Figure 1).

Figure 1. Map of Ghana showing the locations of Likpe Kukurantumi and selected earthwork sites (figure by authors using QGIS version 3.36.2).

Topography, excavation and methods

The Likpe Kukurantumi Earthwork is about 9km from the Buem-Togo Range, also called the Togo Mountains or Akwapim Range, which is 741m high. A GPS survey was conducted using a tripod-mounted receiver to enhance positional accuracy. Georeferenced co-ordinate points were collected at intervals along the site boundary and associated earthwork features. The spatial data were exported and processed in AutoCAD to generate a scaled plan of the site plan. This mapping revealed two embankments, each consisting of a ditch enclosed by two banks (Figure 2). The outer embankment has a diameter of approximately 219m while the diameter of the inner embankment is roughly 65m (Figure 3). Archaeological excavations focused on gathering archaeobotanical data to understand human-plant interactions over the last 500 years. Wood charcoal and carbonised plant remains were acquired by flotation and wet sieving using 2.5, 1.0 and 0.5mm meshes, and seeds were sent for radiocarbon dating.

Figure 2. Likpe Kukurantumi showing the study area and location of embankments (source: Centre for Remote Sensing and Geographic Information Services, University of Ghana, Legon).

Figure 3. Likpe Kukurantumi Earthwork Site showing the location of the embankments and excavation test trenches (figure by Patricia Ayipey; image of the area from Google Earth).

Direct observation of ethnobotanical practices among the local population also formed part of the LKAP, to gather information about the everyday use of plants. Ethnobotanical studies help understand the availability of certain trees, their use as firewood and insights into the local ecosystem. Ethnographic interviews with local inhabitants record plant-use knowledge, linking ancient archaeobotanical data with current practices.

Current results

The excavation of seven trenches (Figure 3) yielded thousands of small finds, including local ceramics, wood charcoal fragments, charred and uncharred seeds, stones/querns, snail shells, corroded lumps of metal and a few bones (Table 1). Most artefacts recovered from the study area came from the northern section of Unit C2 (UC2 in Figure 3; 1 × 10m). Pottery fragments are of a coarse fabric from various vessel forms, including bowls, globular pots and jars (Figure 4). An upper stone quern was identified, though there is no evidence of the corresponding bedstone; other stones resemble the stream gravel found in the nearby Dayi River.

Table 1. Artefact assemblage from Likpe Kukurantumi earthwork site.

Figure 4. Unit C2 soil profile and ceramic vessel forms (figure by authors).

Finds commonly associated with earthwork sites include pottery, which appears to date back to pre-European times (first millennium to the middle of the second millennium AD), as well as tuyeres, iron slags, polished stone axes, the bones of wild animals and mollusc shells. Two pottery types have been identified across the earthwork sites in the Birim Valley and southern Ghana: ‘Atetefo’ (or earthwork) ware and ‘Atwea’ (or Akan) ware (DeCorse Reference DeCorse2001). Atwea ware is still used among the present-day Akan in Ghana (Chouin Reference Chouin2009). Analysis of the pottery from the Likpe Kukurantumi Earthwork is ongoing, so a particular ware type cannot yet be pinpointed; however, initial observations indicate that most of the sherds from Unit C2 (Figure 5) are yellowish-red to yellowish-brown in colour, and typically have gritty, worn surfaces and are often eroded. An elephant femur was also found in the eastern section of this excavation unit, prompting a 1 × 2m extension to recover it fully.

Figure 5. Unit C2 with its extension (inset) (figure by authors).

Archaeobotanical analyses are ongoing. Some wood charcoal fragments recovered from a depth of 3.80m in Unit C2 have anatomical features that allow them to be tentatively identified as Diospyros viridicans (Ebenaceae) and Xylopia sp. (Annonaceae) (Figure 6). Trees of the genus Diospyros have versatile uses, producing edible fruits and valuable timber, but also being used for ornamental purposes and remedies in various folk healing practices. The fruit of Diospyros viridicans is gathered for food and medicine (Tropical Plants Database 2024), likewise the fruits of one widespread African Xylopia species, X. aethiopica, are used as a spice and as medicine. The people of Likpe Kukurantumi speak Guan and Ewe dialects; they call this species etso. Preliminary analysis shows that oil palm (Elaeis guineensis) dominates the carbonised carpological remains. This species is endemic to the tropical forests of West and Central Africa and plays a vital role in local ecosystems; its leaves are collected for thatching and mats, fruits for palm oil, trunks for palm wine and kernels for palm kernel oil. The identified taxa—Elaeis guineensis, Diospyros viridicans and Xylopia sp.—reflect the semi-deciduous forest ecology of Likpe Kukurantumi, indicating a mixed woodland or forest environment shaped by natural vegetation and human management.

Figure 6. Transverse, tangential and radial sections from left to right of: A) Ebenaceae, cf. Diospyros viridicans wood charcoal; and B) Annonaceae, Xylopia spp. wood charcoal. Scale bars 50–150 microns (figure by authors).

Radiocarbon dates for the Likpe Kukurantumi earthwork are available from the lowest part of the inner embankment (4m above the datum point of Unit C2), calibrated to 532 BP (1418 AD) and from 3.8m above the datum point, calibrated to 433 BP (1517 AD). Both are from fragments of Elaeis guineensis endocarp. Another date comes from an unidentified charred seed found 0.50m above the datum point in the ditch of the outer embankment (Unit A1, level 5): 1683–1759 AD. This is noted here for chronological context but, as it derives from a disparate excavation unit, it may not directly correspond to level 5 in Unit C2. Together, the three dates indicate the site’s occupation span.

Conclusion

The LKAP is an ongoing project; the identification, exploration and excavation of the earthwork site have been intrinsic, with community members aiding fieldwork and informing charcoal interpretation. Understanding the human–environmental interaction of the fifteenth-century AD settlement is essential in adding to the discourse on local vegetation change and understanding foodways of populations present during the opening of the Atlantic era in West Africa.

Acknowledgements

We thank the Likpe Kukurantumi community for their invaluable support throughout the project.

Funding statement

The LKAP received support from the National Geographic Society Grant (Grant NGS-EC-96169R-22), the Grant Agency of the University of South Bohemia (GA JU 109/2022/H) and the Erasmus+ Mobility programme.

References

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Figure 0

Figure 1. Map of Ghana showing the locations of Likpe Kukurantumi and selected earthwork sites (figure by authors using QGIS version 3.36.2).

Figure 1

Figure 2. Likpe Kukurantumi showing the study area and location of embankments (source: Centre for Remote Sensing and Geographic Information Services, University of Ghana, Legon).

Figure 2

Figure 3. Likpe Kukurantumi Earthwork Site showing the location of the embankments and excavation test trenches (figure by Patricia Ayipey; image of the area from Google Earth).

Figure 3

Table 1. Artefact assemblage from Likpe Kukurantumi earthwork site.

Figure 4

Figure 4. Unit C2 soil profile and ceramic vessel forms (figure by authors).

Figure 5

Figure 5. Unit C2 with its extension (inset) (figure by authors).

Figure 6

Figure 6. Transverse, tangential and radial sections from left to right of: A) Ebenaceae, cf. Diospyros viridicans wood charcoal; and B) Annonaceae, Xylopia spp. wood charcoal. Scale bars 50–150 microns (figure by authors).