Published online by Cambridge University Press: 02 January 2015
The formative period of Maya civilization has been the subject of recent attention, both in discussion (e.g. Adams, 1977) and in excavation; several projects have been established specifically to investigate the processes that led to the Classic Maya florescence in the first millennium AD. Among these has been the Cuello Project, a joint venture of the British Museum, the National Geographic Society and Rutgers University; this article summarizes the results of the third and final season of the project’s excavations at Cuello, Belize (Fig. I), which took place from January to March, 1980. The terminology for excavated features, structures etc. is detailed in Hammond (1978).
The site was discovered during extensive surveys in 1973–4 (Hammond, 1974, Fig. I), and its potential for the study of the Preclassic or Formative period which preceded the rise of Classic Maya civilization led to a test excavation in 1975. The sequence of building levels and pottery preserved by the growth of Platform 34, a large flat construction with a small superincumbent pyramid (Str. 35) (PL. XXVIa), lying to the southwest of the main part of the site (Donaghey, et al., 1976, Fig. 2), showed that the uppermost floors on the platform had been laid in the Late Formative (conventionally 300 BC–AD 250 ), over structures of the Middle Formative (1000–300 BC). Below these were earlier deposits associated with pottery of pre-Middle Formative date which was assigned to the Early Formative (2000–1000 BC).