The Devensian/Weichselian Late-glacial in northwest Europe (Ireland, Britain, north Belgium, The Netherlands, northwest Germany)

1994 ◽  
Vol 9 (2) ◽  
pp. 109-118 ◽  
Author(s):  
M. J. C. Walker ◽  
S. J. P. Bohncke ◽  
G. R. Coope ◽  
M. O'Connell ◽  
H. Usinger ◽  
...  
2007 ◽  
pp. 1116-1122 ◽  
Author(s):  
J LUNDQVIST ◽  
J EHLERS ◽  
P GIBBARD

Author(s):  
Helena Hamerow

The primary aim of this book is to provide an overview of the evidence for the settlements and everyday life of rural communities in northwest Europe from c. ad 400 to 900, broadly the period from the collapse of the western Roman Empire to the rise of early states in its former provinces and Scandinavia. Its secondary purpose is to relate this evidence, which comes mainly from archaeological excavations, to Anglo-Saxon England and to consider its implications for our understanding of settlements here. Each chapter concludes, therefore, with a brief discussion of the comparable evidence from England, even though detailed comparisons cannot always be drawn due to differences in the quantity and nature of the data available. The evidence is examined under five broad topics: buildings and what the ‘built environment’ tells us about the household and its activities; the layout of farmsteads and settlements and how these may reflect the social structure of communities; the formation of territories and demographic developments; farming strategies; and, finally, the role of non-agrarian production and exchange in the economies of rural settlements. Working with evidence spanning such a broad chronological and geographical range is naturally beset with methodological difficulties. One obvious complication is introduced by the different traditions of periodization and terminology used by scholars working in different countries. Thus, a settlement dating to the sixth century might be described as ‘Germanic Iron Age’, ‘Migration period’, ‘early Anglo-Saxon’, or ‘Merovingian’, depending on its location. The chapters which follow draw primarily on evidence from a large region, stretching from southern Scandinavia, through northwest Germany to the Netherlands. This brings with it the danger of adopting a ‘melting pot’ approach, however unintentionally (Halsall 1995a, 1–3). Yet, an appreciation of regional, indeed local, diversity and of the potential for rapid social change in this period is essential. This North Sea zone has been chosen, furthermore, not out of a misguided belief in a ‘homogeneous Germanic culture’ (ibid.), but because it was in close cultural and economic contact with England and includes the regions from which the Anglo-Saxons believed their forebears to have originated.


2000 ◽  
Vol 79 (4) ◽  
pp. 497-509 ◽  
Author(s):  
W.Z. Hoek

AbstractThe Late Glacial landscape of the Netherlands was a landscape with changing geomorphology and vegetation. Glacial, eolian and fluvial processes in the time before the Late Glacial initially had formed the main landscape types that still existed during the Late Glacial. In these landscape types, geomorphological processes persisted, particularly during intervals when the vegetation cover was discontinuous. Vegetation development initiated soil formation and stabilised the substratum. On the other hand, the abiotic landscape influenced vegetation development, and particularly vegetation patterns.The Late Glacial vegetation patterns, changing in time, have been reconstructed on the basis of a palynological database containing the data from over 250 pollen diagrams from the Netherlands. Patterns of vegetation and abiotic landscape appear to compare to each other in many instances, indicating the close interrelationship between vegetation and the abiotic landscape.


2016 ◽  
Vol 96 (1) ◽  
pp. 9-16 ◽  
Author(s):  
K. Essink ◽  
A.P. Oost ◽  
H.J. Streurman ◽  
J. Van der Plicht

AbstractDuring the Pleistocene, the coastal marine bivalve mollusc Mya arenaria became extinct in northwest Europe. The species remained present in North America. Datings of Mya shells found in northern Denmark and the southern Baltic Sea suggest that repopulation of northwest European coasts already occurred before Columbus’ discovery of America (1492), possibly facilitated by Viking (Norse) settlers at Greenland and northeast North America. In this paper we report on findings of M. arenaria at five locations in the coastal landscape of the Netherlands: polders reclaimed from the Wadden Sea and the former estuaries of Oer-IJ and Old Rhine. The shells from four of these locations also date before 1492 AD.


Author(s):  
Martijn van der Burg

AbstractThis chapter investigates how the (nominally) independent states in the Netherlands and Northwest Germany were slowly but surely seized by French troops, and subsequently incorporated by imperial decree. The conquest and incorporation of the northern lands brought about radical political changes, as well as dilemmas. How were new territories to be fitted in: as dependencies taken by force (pays conquis), or as new departments on equal footing (pays réunies)? And to which extent did ‘on equal footing’ mean eradicating regional diversity within the Empire? Whether uniform structures were imposed too promptly, or not, was contested. The Emperor sent confidants northbound, to investigate existing conditions. Vice versa, Northerners visited Paris, to exert influence on the status of their projected departments. For Dutch and German dignitaries it was of the utmost importance to acknowledge Napoleon’s droit de conquête, while lobbying for an integration form that did justice to local circumstances. Eventually, both areas were given a full status within the Empire, taking into account national peculiarities to a certain extent, but only as long as that did not harm the interests of Old France.


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