The Island of Crete, set in the middle of the East Mediterranean between the Aegean basin and the cultural spheres of Cyprus, Egypt and the Levant, is important both as a bellwether or harbinger of change, as well as an early warning site for trouble coming from farther west. While the 13th century on Crete has received some scholarly attention, it has not been considered in its full chronological and international context as a contributing step or stage in a process that culminates in the 12th c. B.C. troubles further east.
Crete is also rich in archaeological data both traditional (e.g. material culture, architecture, settlement patterns) and modern (palaeo-climatic and environmental) and a standard of scholarship that is both theoretically (e.g. systems collapse, actor/network theory, social organisation, state formation) and methodologically (e.g. GIS, modern excavation/survey techniques and protocols) robust. The island has been intensively explored and comparatively well-published. Furthermore its selection plays to the strengths of the UCL team, which comprises experts in Bronze Age Cretan environmental studies, settlement patterns, social organisation, architecture and ceramics, along with three active excavations. Work Package 2 then forms the bulk of the archaeological investigations of the project. In essence, the work package consists of three inter-related themes: context, comprising environmental conditions, settlement patterns and social organisation; materials, comprising studies of architecture and ceramics; and case studies, presenting integrated analyses of three sites on Crete.
Although 13th c. B.C. climatic deterioration and increased tectonic activity have been documented throughout the Eastern Mediterranean, records of these large-scale phenomena remain under-represented on Crete (Drake 2012). As a result, the effects of environmental changes on its Late Bronze Age society remain poorly understood. Moreover, while earthquakes have been repeatedly invoked as potential mechanisms leading to the destruction and abandonment of archaeological sites, this has been without any systematic examination of available archaeological and geological information, nor have the effects of earthquakes been disentangled from alternative explanations (war/looting, abandonment, ground instability) resulting from other (though potentially interrelated) phenomena (e.g. migrations, invasions, climate change).
Secondly, the establishment of ‘refuge settlements’ on easily defended summits seems to have followed the destruction and/or abandonment of numerous occupation sites during the second half of the 13th c. B.C. on the island. This has been interpreted as strong evidence for a threat coming from the sea: terrified by raiders devastating the coasts, the Cretans retreated to the mountains for security at the expense of convenience (e.g. distance to water resources and agricultural lands). This model suffers from methodological weaknesses, however, focussing on a few type sites and a limited time horizon and thereby failing to properly account for other sites that remained occupied or were newly established along the coast, in plains and on low hills. Within the sites that survived the destruction of the Palace of Knossos and the disappearance of a centrally administered state at the end of the LM IIIA2 period, a new communal organization seems to have emerged, most likely based on kinship. This is suggested by the construction of a series of building complexes of a scale and with a range of functions exceeding the frame of the nuclear family. These sometimes include spacious and monumental halls and open-air areas allowing the gathering of larger numbers of people. Rooms devoted to medium scale storage and various industrial activities were also identified. These buildings also show evidence for the emergence of new rituals and cultic practices, perhaps also following the end of a state-imposed religion. Small shrines incorporated in communal buildings appear with evidence for a new religious syncretism combining traditional local characteristics and external influences.
Materials: Buildings and settlements of the Late Minoan IIIB period or 13th c. B.C. are often considered as bleak and utilitarian remnants of the architectural grandeur of previous times, characterized by the concomitant permanence of traditional vernacular forms and the development of layouts strongly influenced by mainland (i.e. Mycenaean) architecture. However, the processes responsible for this evolution have rarely been considered, especially with regard to the 13th c. B.C. As architecture tends to be the cultural product least prone to radical change it is necessary to consider its evolution in a broader chronological framework. Therefore, a series of analyses will be applied on the architectural landscape from the LM II period onwards, and parallels drawn with earlier catastrophic events and their architectural repercussions (e.g. the Theran eruption and its consequences on LM IB architecture). Through the application of space syntax and cost analysis, the organizational principles and socio-economic actualities of the 13th century architecture on Crete will be examined and correlated to issues of socio-political structures and changes.
The period following the destruction of the Knossian palace and its hegemony in LM IIIA2 sees the resurgence of newly independent power centers in Crete and the intensification of commercial and cultural exchanges in the Central and Eastern Mediterranean. This regionalism and internationalism are well documented by the ceramic assemblages of the time. A detailed analysis of ceramic production will provide the chronological backbone for the articulation of new data. A finer diachronic and regional definition of Cretan society during the 13th c. seen through the prism of its production, exchange, and consumption of pottery will enable the comprehensive distinction of concomitant phenomena: long-term indigenous developments, pan-Aegean increasing syncretism and brutal local responses to unexpected external intrusions. Against this framework, the presence of non-local material culture needs to be re-evaluated.
Case Studies: Although the island of Crete in general is studied in this WP, we will engage in data collection at the three active excavations where members of the Aegis research group are working: Malia and Sissi at the centre or core of the island and the other, Palaikastro, at the far eastern tip or periphery. These case studies will provide data for, and draw results from, the specialist studies. Sissi and Malia are located at short distances from each other on the north-central coast of the island, a location which makes them especially open to maritime contact. Both sites illustrate a long term occupation with obvious Knossian influences during their earlier 15th and 14th c. history and an increase of their regional character during the 13th c. when the palace at Knossos is destroyed. Their proximity but topographical differences allow for subtle differentiation at the local level. Palaikastro lies at the far eastern end of the island of Crete. In the 14th c. B.C. it was the main centre for that region of the island. By the beginning of the 13th c. B.C. the town had been largely abandoned and, after a minor earthquake, left in ruins. During the subsequent period (LM IIIB) there are only sporadic instances of habitation on the coast – circumscribed pockets of settlement, short lived and decidedly non-local, with distinctive ‘drinking kits’ and other cultural markers. What caused the original inhabitants to leave the area and where did they go? Who were the transient ‘arrivistes’ that followed?