Transport Amphorae in the West Hallstatt Zone: Reassessing Socio-Economic Dynamics and Long-Distance Mediterranean Exchange in Western Central Europe in the Early Iron Age

2016 ◽  
Vol 35 (3) ◽  
pp. 247-265
Author(s):  
Federica Sacchetti
1989 ◽  
Vol 84 ◽  
pp. 355-360 ◽  
Author(s):  
Lucia Vagnetti

An askos (BSA 49 [1954] 222, pl. 25:111) found by R.W. Hutchinson in Tomb 2 at Khaniale Tekke near Knossos is recognized as an export from nuragic Sardinia; similar askoi are common there in the same chronological range, c. 850–680 B.C., as that represented by the Cretan context. Although other good parallels have also been found outside Sardinia, notably at Vetulonia in Etruria, the Tekke piece is the first Sardinian artefact of the Early Iron Age to be identified in the Aegean. Its presence there is related to the Phoenician element in the complex pattern of long distance trade that preceded the arrival in Italy of the first Western Greeks.


2021 ◽  
Vol 18 (2) ◽  
pp. 67-87
Author(s):  
Pavel A. Gusenkov ◽  

The article examines the substrate hydronymy of the middle Oka and the Dnieper regions (ending in -va, -da, etc.) that is typically attributed to the West-Baltic toponymic stratum and associated with the language of the Moschinskaya archaeological culture and the related archaeological sites. The author analyzed its spatial distribution in the East European Plain. The study has found that: 1) the spread of names of waterbodies ending in -va correlates with the distribution scheme of substrate Baltic hydronymy in general and the monuments of the Dnieper-Dvina, Yukhnovskaya, and Late Dyakovo cultures of the Early Iron Age; 2) the spread of hydronyms with zh/z sound variation (including as a distinctive feature) correlates with the Krivich and Radimich culture areas, and the range of Russian dialects with lisping pronunciation which makes no difference between sibilants and hushing sounds; 3) Baltic hydronymy ending in -da is not attested in the area of the Moschinskaya culture and related archaeological sites; 4) among the names with the root ape-/upe- found in the same cultural milieu, only those containing Eastern Baltic variant are verifiable; 5) the hypothesis for East Baltic origination of the names with the root stab- is not inferior to the West Baltic; 6) there are no sufficient grounds for tracing some river names to the Prussian words pannean and sug since most of these hydronyms refer to a later period while the others have more plausible explanations; 7) for some hydronyms (Zerna, Opochinka, Ponya, Sezhikovka, etc.) the substrate origin is not confirmed. Based on the above observations, the hypothesis for the presence of a West-Baltic layer of hydronymy in the middle Oka region and the consequent assumption of the West-Baltic origin of the Moshinskaya culture were disputed.


Author(s):  
YU. V. BOLTRIK ◽  
E. E. FIALKO

This chapter focuses on Trakhtemirov, one of the most important ancient settlements of the Early Iron Age in the Ukraine. During the ancient period, the trade routes and caravans met at Trakhtemirov which was situated over the three crossing points of the Dneiper. Its location on the steep heights assured residents of Trakhtemirov security of settlement. On three sides it was protected by the course of the Dnieper while on the other side it was defended by the plateau of the pre-Dneiper elevation. The ancient Trakhtemirov city is located around 100 km below Kiev, on a peninsula which is jutted into the river from the west. Trakhtemirov in the Early Iron Age was important as it was the site of the Cossack capital of Ukraine. It was also the site of the most prestigious artefacts of the Scythian period and a site for various items of jewellery, tools and weaponry. The abundance of artefacts in Trakhtemirov suggests that the city is a central place among the scattered sites of the middle course of the Dneiper.


2019 ◽  
Vol 23 (1) ◽  
pp. 22-42 ◽  
Author(s):  
Sasja van der Vaart-Verschoof ◽  
Robert Schumann

The Low Countries' Early Iron Age is marked by the emergence of lavish burials known as chieftains’ graves or princely burials. These extraordinary elite burials of the Hallstatt C/D period contain weaponry, bronze vessels as well as decorated wagons and horse-gear imported from the Hallstatt culture of Central Europe, where the same objects are found in the famous Fürstengräber. While the connection between these regions has long been recognized, the nature of this contact remains poorly understood. Here we present the preliminary results of an on-going re-examination of elite funerary practices in both regions and the likely direct long-distance interactions reflected in them. Similarities and differences in the treatment of objects and the dead in funerary rituals indicate that, to a certain extent at least, these geographically separated social groups were integrated in a specific elite burial practice, indicating frequent contact across hundreds of kilometres.


The Holocene ◽  
2019 ◽  
Vol 29 (4) ◽  
pp. 543-564 ◽  
Author(s):  
Renata Kołodyńska-Gawrysiak

Past Pleistocene topography of the loess uplands is rich in local sinks (closed depressions (CDs)) influencing sediment fluxes. Soil-sediment sequences from CDs constituting geoarchives where landscape changes under natural and anthropogenic conditions have been recorded. Pedo-sedimentary archives from 10 CDs in the Polish loess belt and human settlements were analysed. Phases of the Holocene evolution of the CDs were correlated with landscape dynamics in loess areas in Poland and Central Europe. Phases of infilling of CDs occurring (2) from the late Boreal/early Atlantic Period until the (middle) late Bronze Age/early Iron Age and (4) since the early Middle Ages until today were documented. These were phases of long-term soil erosion and colluviation corresponding to the increasing agricultural land use of Polish loess uplands. Phases of soil formation related to geomorphic stabilization of CDs occurred (1) from the late Vistulian until the late Boreal/early Atlantic Period and (3) from the late Bronze Age/early Iron Age until the early/high Middle Ages. These were phases of decreased soil erosion and landform conservation in a considerable part of Poland’s loess areas. Pedo-sedimentary archives from the CDs have recorded soil erosion strongly related with human-induced land-use changes. The mean soil erosion rate in the catchment of CDs was 0.33 t·ha−1·yr−1 during prehistory and 4.0 t·ha−1·yr−1 during the last approximately 1000 years. Phases of CD evolution are representative for the main phases of sediment and landscape dynamics in Poland’s loess areas recorded in various archives, and are not synchronous with some of these phases in Central Europe.


1938 ◽  
Vol 4 (1) ◽  
pp. 151-168 ◽  
Author(s):  
J. B. Ward Perkins

The Iron Age Site at Crayford, Kent, was discovered in 1936 during the development of the Glebe Building Estate. This Estate lies to the west of St. Paulinus' Church, between Watling Street Old Road and Manor Road, and Nos. 103, 105, 107 and 109 Watling Street Old Road now mark the site. The circumstances of the discovery did not permit of scientific excavation, but the finds were reported to Mr S. Priest, F.G.S., curator of the Dartford Public Museum, and thanks to him and to the facilities most generously afforded by Mr Roys ton Phillips, the owner of the Glebe Estate, a large quantity of pottery and other objects was preserved and is now in the possession of the Dartford Public Museum. To Mr Priest the writer is particularly indebted for the opportunity to examine and report upon the discoveries, and for help in the preparation of that report. It was Mr G. C. Dunning, F.s.A., who first drew attention to the largely unpublished comparative material, and a number of his drawings are here used. The writer is also indebted to Dr R. E. M. Wheeler, V.P.S.A., for much help and criticism.


2000 ◽  
Vol 95 ◽  
pp. 259-299 ◽  
Author(s):  
J. N. Coldstream

Among over 1800 boxes of Sir Arthur Evans's finds now stored in the Stratigraphical Museum at Knossos, at least 150 contain Greek pottery from Subminoan to Classical. A systematic study of this material, in relation to its recorded find spots, throws new light on the eastern part of the early Greek town, bordering the site of the Minoan Palace. Above the Palace itself, fresh evidence is produced, and fresh interpretation offered, for the Greek sanctuary described by Evans. In its immediate surroundings, there are signs of busy domestic and industrial life in the early Greek town above the South-West Houses, the West Court, the Theatral Area, and the Pillared Hall outside the North Entrance to the Palace. Greek occupation is also noted above the House of Frescoes, the Little Palace and the Royal Villa. A wider aim of this article is to trace the limits of the early Greek town of Knossos, both of its original Early Iron Age nucleus surviving from Late Minoan times, and of its spacious extension towards the north in the late eighth and seventh centuries BC.


Antiquity ◽  
2020 ◽  
pp. 1-21
Author(s):  
Dennys Frenez ◽  
Francesco Genchi ◽  
Hélène David-Cuny ◽  
Sultan Al-Bakri

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