William A. Parkinson

A B S T R A C T Nucleated tell sites emerged on the Great Hungarian Plain nearly a millennium after the earliest agricultural communities established sedentary settlements at the beginning of the Neolithic period. Once established, these unprecedentedly large population centers had a dramatic impact on their local environment. In this article, we present the results of our recent research at two Neolithic tells in the Körös Region of the Great Hungarian Plain. These sites – Vésztő-Mágor and Szeghalom-Kovácshalom – were established at roughly the same time and were located on the same branch of the Sebes-Körös River. Focusing on two methods – geophysics and micro-stratigraphy – we compare how these two nearby sites were established, evolved, and were abandoned within their local landscapes. Whereas geophysical surveys provide a horizontal picture of how the sites expanded over space, microstratigraphic studies provide a vertical perspective of the social processes that built the tells over time. Although both settlements were established at the same time, the sites developed in very different ways. We attribute these differences in the micro-regional trajectories to specific traditions associated with different local communities.

A large-scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom-Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High-resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll-along technique. A recently presented two-dimensional fast non-linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross-sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non-standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10 m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites.

This article discusses research carried out by the Körös Regional Archaeological Project from 2000 to 2006 at Early Copper Age Tiszapolgár Culture sites on the Great Hungarian Plain. To build a model of social organization for the period, we incorporated information from regional geomorphological studies, soil chemistry analysis, archaeological surface surveys, remote sensing, and systematic excavations at Early Copper Age sites in the Körös Valley of southeastern Hungary. Previous models characterized the transition from the Neolithic period to the Copper Age as an abrupt shift from a tell-based, sedentary, agricultural lifeway to one based on mobile cattle herding. By studying the transition between these periods on multiple geographic and temporal scales, we have identified a more gradual process with widespread regional variation in cultural patterns. Similar social processes characterize the transition between chronological periods and cultural phases in other parts of the world, and we suggest that a multiscalar approach is effective for building comparative archaeological models of long-term social change.

This article discusses the organization and distribution of ancient towers on the Paximadi peninsula of southern Euboia, most of which date to the Classical period. Much attention has been given to the sporadic occurrence and possible uses of stone-built towers in different regions and time periods in Greece. Rather than identifying a single function for the Paximadi towers, the authors suggest that they fulfilled a variety of roles over time. Thus, changes in their form and distribution can be used to model how the rural landscape was exploited under different political and economic regimes.

This revised and expanded edition of the classic 1999 edited book includes all the chapters from the original volume plus a new, updated, introduction and several new chapters. The current book is an up-to-date review of research into Mycenaean palatial systems with chapters by archaeologists and Linear B specialists that will be useful to scholars, instructors, and advanced students.

This book aims to define more accurately the term “palace” in light of both recent archaeological research in the Aegean and current anthropological thinking on the structure and origin of early states. Regional centers do not exist as independent entities. They articulate with more extensive sociopolitical systems. The concept of palace needs to be incorporated into enhanced models of Mycenaean state organization, ones that more completely integrate primary centers with networks of regional settlement and economy.

A B S T R A C T Nucleated tell sites emerged on the Great Hungarian Plain nearly a millennium after the earliest agricultural communities established sedentary settlements at the beginning of the Neolithic period. Once established, these unprecedentedly large population centers had a dramatic impact on their local environment. In this article, we present the results of our recent research at two Neolithic tells in the Körös Region of the Great Hungarian Plain. These sites – Vésztő-Mágor and Szeghalom-Kovácshalom – were established at roughly the same time and were located on the same branch of the Sebes-Körös River. Focusing on two methods – geophysics and micro-stratigraphy – we compare how these two nearby sites were established, evolved, and were abandoned within their local landscapes. Whereas geophysical surveys provide a horizontal picture of how the sites expanded over space, microstratigraphic studies provide a vertical perspective of the social processes that built the tells over time. Although both settlements were established at the same time, the sites developed in very different ways. We attribute these differences in the micro-regional trajectories to specific traditions associated with different local communities.

Alepotrypa Cave at Diros Bay, Lakonia, Greece, is a massive karstic formation of consecutive chambers ending at a lake. The cave was excavated by G. Papathanassopoulos from 1970 to 2006. In conjunction with the surrounding area, it was used as a complementary habitation area, burial site, and place for ceremonial activity during the Neolithic c 6000 to 3200 BC. 

As a sealed, single-component, archaeological site, the Neolithic settlement complex of Alepotrypa Cave is one of the richest sites in Greece and Europe in terms of number of artifacts, preservation of biological materials, volume of undisturbed deposits, and horizontal exposure of archaeological surfaces of past human activity and this publication is an important contribution to ongoing archaeological research of the Neolithic Age in Greece in particular, but also in Anatolia, the Balkans and Europe in general.

This edited volume offers a full scholarly interdisciplinary study and interpretation of the results of approximately 40 years of excavation and analysis. It includes numerous chemical analyses and a much needed long series of radiocarbon dates, the corresponding microstratigraphic, stratigraphic and ceramic sequence, the human burials, stone and bone tools, faunal and floral remains, isotopic analyses, specific locations of human activities and ceremonies inside the cave, as well as a site description and the history of the excavation conducted by G. Papathanassopoulos.