Across the Northe Sea: A Review

Antiquity ◽  
1961 ◽  
Vol 35 (137) ◽  
pp. 45-52
Author(s):  
J. V. S. Megaw
Keyword(s):  
The Netherlands ◽  
English Language ◽  
Land Reclamation ◽  
English Summary ◽  
Regional Study ◽  
Low Countries ◽  
Roman Archaeology ◽  
State Institutions ◽  
The North ◽  
Private Individual

Exactly three centuries ago last year, Johan Picardt, parson of Coevorder in Drenthe and Adviser for Land-Reclamation, wrote in a regional study worthy of comparison with his contemporary John Aubrey’s Monumenta Britannica: ‘Our fore-fathers had not pen, ink, nor paper, which had they possessed would have enabled us to learn of strange things. Howsomever, they have bequeathed us signs enough if only it were that we could read them.’ Each one of the three volumes from the second of which my quotation comes clearly shows the ways in which archaeological research in the Low Countries has vindicated Picardt’s statement. Today archaeology in the Netherlands is a matter of exemplary close-knit co-operation between State institutions, universities, local societies, and the private individual, while recently Belgium has taken important steps in the systemization of pre- and protohistoric studies.Although the Low Countries can hardly be regarded as a primary area of development, their coastal position at the north-western limit of the transcontinental routes has made them a cultural entrepôt of particular significance for the British archaeologist. In this context Professor De Laet’s book in the ‘Ancient Peoples and Places’ series is all the more welcome in that it is the first English summary of the pre-Roman archaeology of the region.De Voorgeschiedenis der Lage Landen is a much expanded and corrected version of De Laet’s volume, with Professor Glasbergen’s collaboration giving a more balanced account of the Dutch evidence. The third book, a double volume of Antiquity and Survival, offers a lavishly illustrated symposium of one hundred centuries of the Netherlands, and although the promised English language edition is not to be, the Trustees of the Prince Bernhard Foundation and the Rijksdienst voor het Oudheidkundig Bodemonderzoek are to be warmly thanked for giving their support to Honderd Eeuwen Nederland.

scholarly journals LAND RECLAMATION AND GROIN-BUILDING IN THE TIDAL PLATS

1970 ◽  
Vol 1 (12) ◽  
pp. 66
Author(s):  
Hele Focken Erchinger
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
Land Reclamation ◽  
Tidal Flats ◽  
The Other ◽  
The North ◽  
The North Sea

Along the North Sea eoast of Germany there are two large areas where land reclamation work in the tidal flats is being carried out. One is on the coast of Schleswig- Holstem and the other in Ostfriesland, on the coast and along the estuary of the river Ems near the border with the Netherlands. Conditions and working methods for land reclamation in tidal flats as well as the development of new groin constructions on the Ostfriesian coast are described below.

What happened in 1953? The Big Flood in the Netherlands in retrospect

2005 ◽  
Vol 363 (1831) ◽  
pp. 1271-1291 ◽  
Author(s):  
Herman Gerritsen
Keyword(s):  
The Netherlands ◽  
Sea Level ◽  
Large Scale ◽  
Land Reclamation ◽  
Spring Tide ◽  
Water Levels ◽  
The North ◽  
Human Stress ◽  
The Uk ◽  
The Impact

During the weekend of Saturday 31 January to Sunday 1 February 1953, a storm tide raged across the northwest European shelf and flooded the low-lying coastal areas of the countries around the North Sea. The peak high waters occurred during the night and the storm surprised many people in their sleep. The resulting disaster in terms of loss of life and damage to infrastructure was enormous. In the Netherlands, 1836 people fell victim to the flood; in the UK and Belgium, the casualities were 307 and 22, respectively. The large number of fatalities in the Netherlands was related to the fact that much of the affected area is below sea-level. This paper focuses on the case of the Netherlands. It discusses the history of land reclamation, and the fact that living in low-lying areas protected by dykes, often below sea-level, is an accepted fact of life in the Netherlands. The historical approach to dyke maintenance is then outlined, and the state of the dykes in the early twentieth century and after the war is discussed. The characteristics of the storm and the flood are discussed, along with people's experiences of the first hours and days following the flood. The impact of this human stress has often been lasting—many survivors continue to live with daily memories of the flood. Attention is given to the large-scale rescue and relief efforts, the closure of the dykes during the following nine months and the concept of the Delta Plan, designed to prevent such a large-scale disaster ever happening again. Although the 1953 storm was indeed a low probability event leading to very high storm-induced water-levels, and occurred in combination with spring tide, several arguments are presented that explain why this flood turned into a disaster of such a large scale. Equally, the question is raised whether the disaster could have been prevented. The paper concludes by noting the importance of awareness and preparedness in order to prevent a future storm threat of this scale turning into a disaster of the scope of the Big Flood of 1953.

Chrono- and archaeostratigraphy and development of the River Amstel: results of the North/South underground line excavations, Amsterdam, the Netherlands

2015 ◽  
Vol 94 (4) ◽  
pp. 333-352 ◽  
Author(s):  
P. Kranendonk ◽  
S.J. Kluiving ◽  
S.R. Troelstra
Keyword(s):  
The Netherlands ◽  
Land Reclamation ◽  
Complex Interaction ◽  
Archaeological Research ◽  
Late Neolithic ◽  
The North ◽  
Land Drainage ◽  
Underground System ◽  
New Evidence ◽  
The City

AbstractSince 2003 extensive archaeological research has been conducted in Amsterdam, the Netherlands, connected with the initial phase of the new underground system (Noord/Zuidlijn). Research has mainly focused on two locations, Damrak and Rokin, in the centre of Medieval Amsterdam. Both sites are situated around the (former) River Amstel, which is of vital importance for the origin and development of the city of Amsterdam. Information on the Holocene evolution of the river, however, is relatively sparse. This project has provided new evidence combining archaeological and geological data, and allowed the reconstruction of six consecutive landscape phases associated with the development of the River Amstel. The course of the present-day Amstel is the result of a complex interaction of processes that started with an early prehistoric tidal gully within the Wormer Member of the Naaldwijk Formation, including Late Neolithic (2400–2000 BC) occupation debris in its fill that was subsequently eroded. Next, this system developed into a later prehistoric Amstel river course that was part of the Angstel–Vecht–Oer-IJ system (1020–350 BC), meandering through a peat-dominated landscape. Later on the processes included intensive reclamation of land, drainage and canalisation, although the Amstel was also strongly influenced by natural storm tides. After intense land reclamation, starting around 1200 AD, the meandering Amstel from Nes to Kalverstraat, which was originally 150 m wide, became the rather straight 20–50 m wide tamed, canalised river of today.

Rhineland on the Way to its Thousandth Anniversary or Water-Administration in the Next 100–200 Years

1991 ◽  
Vol 23 (1-3) ◽  
pp. 49-55
Author(s):  
E. H. baron van Tuyll van Serooskerken
Keyword(s):  
The Netherlands ◽  
Late Summer ◽  
Water Shortage ◽  
Land Utilization ◽  
Water Control ◽  
Coastal Defence ◽  
The North ◽  
Policies And Measures ◽  
Water Provision ◽  
Water Administration

An inventory is made of the effects of sea level rise and expected climatic change on the level of the district water authorities in the Netherlands and especially the “hoogheemraadschap” of Rhineland in the next 100-200 years. Special attention is paid to the effects on land utilization, coastal defence and water control. The first is hard to describe by lack of research, the second can already be determined in terms of cost; the third can be described in its effects on brackishness and water provision with indication of policies and measures to be taken. Preliminary conclusions are that larger efforts on coastal defence - even with present techniques - will be a realistic answer in terms of cost. The foreseen increase of brackishness in area and salt concentration, will give a significant extra need for fresh water. High cost and even higher risks have to be expected with regard to measures to neutralize the effects of a water surplus in winter and a growing water shortage in (late) summer, while the cost will further grow. Because of the effect a larger area must be drained off and water has to be raised higher as the Netherlands will sink in relation to the North Sea.

Maritime and River Traders, Landing Places, and Emporia Ports in the Merovingian Period in and Around the Low Countries

2020 ◽  
pp. 763-796
Author(s):  
Dries Tys
Keyword(s):  
North Sea ◽  
Institutional Economics ◽  
New Institutional Economics ◽  
Central Position ◽  
Economic Activities ◽  
Early Medieval ◽  
Low Countries ◽  
Long Distance ◽  
The North ◽  
The North Sea

The origin, rise, and dynamics of coastal trade and landing places in the North Sea area between the sixth and eighth centuries must be understood in relation to how coastal regions and seascapes acted as arenas of contact, dialogue, and transition. Although the free coastal societies of the early medieval period were involved in regional to interregional or long-distance trade networks, their economic agency must be understood from a bottom-up perspective. That is, their reproduction strategies must be studied in their own right, independent from any teleological construction about the development of trade, markets, or towns for that matter. This means that the early medieval coastal networks of exchange were much more complex and diverse than advocated by the simple emporium network model, which connected the major archaeological sites along the North Sea coast. Instead, coastal and riverine dwellers often possessed some form of free status and large degrees of autonomy, in part due to the specific environmental conditions of the landscapes in which they dwelled. The wide estuarine region of the Low Countries, between coastal Flanders in the south and Friesland in the north, a region with vast hinterlands and a central position in northwestern Europe, makes these developments particularly clear. This chapter thus pushes back against longstanding assumptions in scholarly research, which include overemphasis of the influence of large landowners over peasant economies, and on the prioritization of easily retrievable luxuries over less visible indicators of bulk trade (such as wood, wool, and more), gift exchange, and market trade. The approach used here demonstrates that well-known emporia or larger ports of trade were embedded in the economic activities and networks of their respective hinterlands. Early medieval coastal societies and their dynamics are thus better understood from the perspective of integrated governance and economy (“new institutional economics”) in a regional setting.

scholarly journals Palynological indications for Silurian – earliest Devonian age strata in the Netherlands

2021 ◽  
Vol 100 ◽  
Author(s):  
Alexander J.P. Houben ◽  
Geert-Jan Vis
Keyword(s):  
The Netherlands ◽  
Core Material ◽  
Late Devonian ◽  
Time Interval ◽  
The South ◽  
Early Devonian ◽  
The North ◽  
Depositional Settings ◽  
Palynological Study ◽  
Devonian Age

Abstract Knowledge of the stratigraphic development of pre-Carboniferous strata in the subsurface of the Netherlands is very limited, leaving the lithostratigraphic nomenclature for this time interval informal. In two wells from the southwestern Netherlands, Silurian strata have repeatedly been reported, suggesting that these are the oldest ever recovered in the Netherlands. The hypothesised presence of Silurian-aged strata has not been tested by biostratigraphic analysis. A similar lack of biostratigraphic control applies to the overlying Devonian succession. We present the results of a palynological study of core material from wells KTG-01 and S05-01. Relatively low-diversity and poorly preserved miospore associations were recorded. These, nonetheless, provide new insights into the regional stratigraphic development of the pre-Carboniferous of the SW Netherlands. The lower two cores from well KTG-01 are of a late Silurian (Ludlow–Pridoli Epoch) to earliest Devonian (Lochkovian) age, confirming that these are the oldest sedimentary strata ever recovered in the Netherlands. The results from the upper cored section from the pre-Carboniferous succession in well KTG-01 and the cored sections from the pre-Carboniferous succession in well S05-01 are more ambiguous. This inferred Devonian succession is, in the current informal lithostratigraphy of the Netherlands, assigned to the Banjaard group and its subordinate Bollen Claystone formation, of presumed Frasnian (i.e. early Late Devonian) age. Age-indicative Middle to Late Devonian palynomorphs were, however, not recorded, and the overall character of the poorly preserved palynological associations in wells KTG-01 and S05-01 may also suggest an Early Devonian age. In terms of lithofacies, however, the cores in well S05-01 can be correlated to the upper Frasnian – lower Famennian Falisolle Formation in the Campine Basin in Belgium. Hence, it remains plausible that an unconformity separates Silurian to Lower Devonian strata from Upper Devonian (Frasnian–Famennian) strata in the SW Netherlands. In general, the abundance of miospore associations points to the presence of a vegetated hinterland and a relatively proximal yet relatively deep marine setting during late Silurian and Early Devonian times. This differs markedly from the open marine depositional settings reported from the Brabant Massif area to the south in present-day Belgium, suggesting a sediment source to the north. The episodic presence of reworked (marine) acritarchs of Ordovician age suggests the influx of sedimentary material from uplifted elements on the present-day Brabant Massif to the south, possibly in relation to the activation of a Brabant Arch system.

Kant on Civil Self-Sufficiency

2021 ◽  
Vol 0 (0) ◽  
Author(s):  
Luke Davies
Keyword(s):  
Political Participation ◽  
Necessary Condition ◽  
Individual Freedom ◽  
Economic Relations ◽  
State Institutions ◽  
Self Sufficiency ◽  
Private Individual

Abstract Kant distinguishes between ‘active’ and ‘passive’ citizens and holds that only the former are civilly self-sufficient and possess rights of political participation. Such rights are important, since for Kant state institutions are a necessary condition for individual freedom. Thus, only active citizens are entitled to contribute to a necessary condition for the freedom of each. I argue that Kant attributes civil self-sufficiency to those who are not under the authority of any private individual for their survival. This reading is more textually grounded than the dominant reading, which understands civil self-sufficiency in terms of economic relations alone. I further argue that Kant was interested in relations of authority because he was concerned to eliminate certain forms of corruption. This indicates that Kant’s contested distinction between active and passive citizens was a response to a key problem of any account of public lawgiving.

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