The Aylesford-Swarling Culture: The Problem of the Belgae reconsidered

1965 ◽  
Vol 31 ◽  
pp. 241-367 ◽  
Author(s):  
Ann Birchall

Until the discovery of the Aylesford urnfield seventy-five years ago, the Belgae were still no more than dramatis personae in Caesar's Gallic War. It was Sir Arthur Evans who first identified the users of the Aylesford cemetery with the invaders ex Belgio referred to by Caesar. Reginald Smith's publication of the Welwyn grave-groups (1912) and then Bushe-Fox's excavation of the Swarling urnfield (1925) were followed, in 1930, by Hawkes' and Dunning's account of the history of the British and Continental Belgic tribes, which has remained the standard work on the subject ever since.Thus, it has been accepted that the archaeological material of Aylesford-Swarling type represents the introduction of Belgic culture into Britain. Its continental origins were traced to northern Gaul, the area occupied by the historical Belgae, where a similar series of cremation burials of Late La Tène date is known. This continental series, thought to mark a change from what seemed to be the universal practice of inhumation as mode of burial to cremation, was interpreted as representative of a fusion of inhuming Galli with cremating Germani from across the Rhine. This fusion, leading to the formation of the Belgae, who, as Caesar records, boasted of their ‘Germanic’ origin, was thought to have taken place in the latter half of the 2nd century B.C. The date for the first Belgic invasion of Britain was put at about 75 B.C.

1966 ◽  
Vol 9 (1) ◽  
pp. 60-89 ◽  
Author(s):  
J. C. G. Röhl

Ever since the First World War, but especially during the Weimar period, Bismarck's dismissal has exercised a strong attraction on German historians, and has probably received more attention than any other event in the history of the Second Reich. In the troubled post-war years, 20 March 1890 seemed to stand out prominently as the fateful turning point of Germany's history. Wilhelm Schvissler, the first to exploit the unprecedented wealth of evidence available in consequence of the monarchy's collapse, did not hesitate to claim that ‘even at that time [1890] the downfall (Untergang) of the German Reich was written in the stars’. ‘Who would doubt’, he asked, ‘that our misfortune began there…and led to the catastrophe of the Imperial Monarchy and the German Reich—exactly 20 years after his [Bismarck's] death!’ This highly emotional approach to the subject was fully shared by Wilhelm Mommsen, whose standard work on the role of the political parties in the crisis appeared in 1924. Bismarck's fall, he wrote, ‘appears to us today as a turning point of German history, and it is only with deep feeling that we can recall the events of March 1890’. It is perhaps partly for this reason that these early writers tended to misinterpret the nature of Bismarck's relations with the parties in the crucial months before his fall. There was, for one thing, an inclination to idealize the bygone age in which ‘the State’ was thought to have stood incorruptibly ‘above the parties’, and as a result the party struggles of 1889 and 1890 were relegated to a self-contained compartment whence, it was held, they were able to influence the course of events only in the negative sense of providing no obstacle to the chancellor's dismissal. The influential work of Hans Rothfels probably typified this attitude, but even Mommsen warned his readers that his study of the parties could throw at best an oblique light on the crisis ‘since the parties had no direct and at any rate no significant effect on the course of those events’. According to Hans Herzfeld's summary of the present state of knowledge on the subject, this view is still widely accepted today.


2019 ◽  
Vol 85 ◽  
pp. 307-330
Author(s):  
Katherine M. Erdman ◽  
Bruno Chaume

The Source of the Douix in Châtillon-sur-Seine, France, has been visited by local inhabitants for over 2000 years and served as a watery focal point for the ritual deposition of various types of offerings. While water deposits are by no means uncommon across Europe, the continued use of a single space over multiple millennia is. An examination of the preserved offerings at the Douix indicate there are three phases of depositional activity: late Hallstatt to early La Tène periods, late La Tène to Gallo-Roman periods, and the early modern period. Despite being separated by hundreds of years there are similarities across depositional phases including the importance of modified metallic objects, personal ornamentation, and possible connections to women. Could the persistence of these ritual practices be the result of behavioural and ideological continuities? If not, how can we interpret this complex record of intermittent deposition? We examine the deposits from each phase in their wider social and ritual contexts, including the Douix’s connection to the Hallstatt princely centre of Mont Lassois, Gallo-Roman ritual traditions, and the historic folklore surrounding springs. We then explore the inter-depositional phases and discuss the conditions that could lead to the persistence of ideas despite the dearth of material evidence and summarise what these patterns mean for the history of ritual activity at the Source of the Douix.


The Holocene ◽  
2020 ◽  
Vol 31 (1) ◽  
pp. 145-159
Author(s):  
Radka Kozáková ◽  
Přemysl Bobek ◽  
Dagmar Dreslerová ◽  
Vojtěch Abraham ◽  
Helena Svobodová-Svitavská

In the lower forested mountain ranges of Europe, human impact on nature is usually confined to the written history of the Middle Ages. Our research in the Šumava mountains aims to specify the nature and intensity of human impact on vegetation, especially during agricultural prehistory. We use results from a multidisciplinary study of the unique La Tène archaeological site in the Sklářské Valley (elevation 802 m a.s.l.) and from a pollen and charcoal record 60 m away. With knowledge of this reference site we focus on the meaning of anthropogenic pollen indicators in 13 other pollen sites from central Šumava. From ca 3300 cal yr BP we detect an increase in NAP, Betula, Pinus and secondary anthropogenic indicators in pollen records – vegetation changes of anthropogenic origin. Charcoal records show a significant peak around 3200 cal yr BP. We found weak anthropogenic influence on the La Tène archaeological site in the Sklářské Valley, and much stronger anthropogenic pollen signals at other pollen sites dated to the Late Bronze and Iron Ages. Some of these sites are situated on trade routes which have been known since Medieval times but which most likely have much older origins. During prehistory, pollen data reveal no specific human activity such as pasturing or arable farming but reflect small-scale disturbances that supported growth of Betula and Pinus and an abundance of herbs. Such human impact could be connected primarily to activities along trade routes and to hunting, but other factors cannot be excluded.


Fossil Record ◽  
1998 ◽  
Vol 1 (1) ◽  
pp. 5-19 ◽  
Author(s):  
G. Hoppe

Die Geschichte der beiden Institute für Mineralogie und für Paläontologie des Berliner Museums für Naturkunde mit ihren sehr großen Sammlungen beginnt mit ihrer direkten Vorgängerin, der Berliner Bergakademie, die 1770 gegründet worden ist. Aber bereits vor dieser Zeit hat es in Berlin geowissenschaftliche Interessen und Betätigungen gegeben. <br><br> Diese Vorgeschichte wird mit einer Zeit begonnen, in der es den Ort Berlin noch längst nicht gab. Aus der La-Tene-Zeit, die der Zeit der griechischen Antike entspricht, stammt eine Aschenurne mit einer Sammlung fossiler Mollusken, die im norddeutschen Flachland bei Bernburg gefunden wurde. Die Zusammensetzung dieser Sammlung läßt bereits ein wissenschaftliches Herangehen erkennen. <br><br> Für Berlin selbst ist kurz nach Georg Agricola eine Persönlichkeit der Renaissance zu verzeichnen, Leonhard Thurneysser zum Thurn, in dessen vielfältigen Aktivitäten auch Mineralien einen Platz hatten. In gleicher Zeit war in Berlin am brandenburgischen Hofe eine Raritätenkammer vorhanden, die spätere Kunst- und Naturalienkammer. Sie existierte bis über das Jahr 1770 hinaus und enthielt auch Mineralien und Versteinerungen. Das sich hierdurch zeigende Interesse an solchen Objekten war noch recht oberflächlich. <br><br> Erst die Sammlungen privater Personen, die in Berlin seit Ende des 17. Jahrhunderts entstanden sind, zeigen ein tieferes und wissenschaftliches Interesse, wenn auch in verschiedenem Maße und in unterschiedlicher Spezialisierung. Unter ihnen ragt besonders Johann Gottlob Lehmann heraus. Als vielseitiger Naturwissenschaftler und Bergrat hielt er privat Vorlesungen in Mineralogie und Bergbaukunde. Der Siebenjährige Krieg verhinderte den Ausbau und die Fortsetzung. <br><br> Erst Jahre danach, 1768, reorganisierte König Friedrich II. das preußische Bergwesen und richtete 1770 die Berliner Bergakademie ein. Hierbei kam dem Arzt und Bergrat Carl Abraham Gerhard bei der Einrichtung und als Lehrkraft eine wesentliche Rolle zu. <br><br> History of the Geoscience Institutes of the Natural History Museum in Berlin, Part 1. <br><br> The Geoscience Institutes of the Natural History Museum in Berlin have their roots in the Mining Academy which was founded in 1770. Geoscientific interest, however, goes back as far as to prehistoric times which is, e.g., evidenced by a collection of mollusks from the Iron Age. From the Renaissance, similar interests were developed by Leonhard Thurneysser zum Thurn. The contemporaneous cabinet of arts and curiosities of the Prussian Dynasty is also known to have housed geoscientific pieces which, however, turned out to be of only subordinate significance later. Much more important were the efforts of Berlin citizens in the 17th and 18th century who established remarkable collections of geoscientific objects. Among these collectors, Johann Gottlob Lehmann was the most outstanding personality. He gave not only lectures but also wrote textbooks on geoscientific topics. However, not before the end of the Seven Years-War Carl Abraham Gerhard was authorized to found the Mining Academy. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.19980010102" target="_blank">10.1002/mmng.19980010102</a>


Antiquity ◽  
1973 ◽  
Vol 47 (188) ◽  
pp. 280-283
Author(s):  
John Collis

Even before Manching first graced the pages of ANTIQUITY it had achieved the status of a key-site in the prehistory of Europe. The small La Téne B-C cemeteries of Steinbichel and Hundsrücken, the latter within the area enclosed by the ramparts of the later oppidum, have become the type-sites for their period in Southern Germany, but more important they could be seen to overlap chronologically in La Téne C with the beginning of the Late La Téne settlement that has been the subject of the recent excavations. With this continuity of occupation Manching offers a unique opportunity to study the origin and development of one of those settlements whose size, trade and industry justify their claim to be the earliest truly urban settlements in Temperate Europe.


2018 ◽  
Vol 12 ◽  
pp. 7-45
Author(s):  
Jerzy Fogel

Archaeological interests of the Szembek earls from Siemianice near Kępno (southern Wielkopolska) have spread over many generations starting from the middle of the 19th century until the present time. This is well exemplified by activities of Jadwiga (1883-1939) and Zofia (1884-1974) Szembek. In the years 1897-1908, both sisters undertook systematic and model excavations of the multicultural cemetery (-ies) at Siemianice near Kępno (Bronze Age 11, Bronze Age V - HaD; the Late La Téne - Early Roman Iron Age) and cemetery at Lipie near Kępno (Bronze Age V). Jadwiga Szembek excavated also multicultural settlement at Tarnowica near Jaworów (western Ukraine) in 1924 and 1927. An origin and development of archaeological interests of the Szembek sisters, along with a detailed analysis of their field works, was reconstructed on the basis of unpublished archive materials and old literature of the subject. Assessment of their achievements in this field, according to both previous and current criteria, made possible to support opinion by Prof. Józef Kostrzewski who rated the Szembek sisters among archaeologists of the most outstanding merit before 1918.


2020 ◽  
Vol 71 (2) ◽  
pp. 443-560
Author(s):  
Andrea Vaday ◽  
Károly Tankó

One of the important cemetery and settlement of the Celts lies in a plateau on the southern side of the the Öreg Rába river, in the vicinity of Győr-Ménfőcsanak. The first burials were found in 1967 during a short rescue excavation, however it made Ménfőcsanak a key La Tène site in the Carpathian Basin. Excavations investigated on a larger scale in the area of previously known cemetery in 1993–94. The burial rite of the necropolis was mainly inhumation and only two graves were cremated and two biritual graves. Celtic warriors with swords and richly furnished female with fibulae, coral, amber, and glass beads jewelry were also buried in this part of cemetery. Few graves were limited by rectangular enclosing trenches. According to find analyzing this part of the cemetery dates to the LT B period, and that is why Ménfőcsanak became an important archaeological site in terms of burials in the history of the Celtic “migrations” in the fourth century BC.


Author(s):  
Carola Metzner-Nebelsick

This chapter covers the area between eastern France and western Hungary, and from the Alps to the central European Mittelgebirge, following the established division between the early Iron Age (Hallstatt) and later Iron Age (La Tène) periods, beginning each section with a summary of the history of research and chronology. After characterizing the west–east Hallstatt cultural spheres, early Iron Age burial rites, material culture, and settlements are explored by region, including the phenomenon of ‘princely seats’. In the fifth century BC, a new ideological, social, and aesthetic concept arose, apparent both in the burial record, and especially in the development of the new La Tène art style. This period also saw the emergence of new, larger proto-urban forms of settlement, first unfortified agglomerations, and later the fortified oppida. Finally, the chapter examines changes in the nature and scale of production, material culture, and religious practices through the first millennium BC.


Paleobiology ◽  
1980 ◽  
Vol 6 (02) ◽  
pp. 146-160 ◽  
Author(s):  
William A. Oliver

The Mesozoic-Cenozoic coral Order Scleractinia has been suggested to have originated or evolved (1) by direct descent from the Paleozoic Order Rugosa or (2) by the development of a skeleton in members of one of the anemone groups that probably have existed throughout Phanerozoic time. In spite of much work on the subject, advocates of the direct descent hypothesis have failed to find convincing evidence of this relationship. Critical points are:(1) Rugosan septal insertion is serial; Scleractinian insertion is cyclic; no intermediate stages have been demonstrated. Apparent intermediates are Scleractinia having bilateral cyclic insertion or teratological Rugosa.(2) There is convincing evidence that the skeletons of many Rugosa were calcitic and none are known to be or to have been aragonitic. In contrast, the skeletons of all living Scleractinia are aragonitic and there is evidence that fossil Scleractinia were aragonitic also. The mineralogic difference is almost certainly due to intrinsic biologic factors.(3) No early Triassic corals of either group are known. This fact is not compelling (by itself) but is important in connection with points 1 and 2, because, given direct descent, both changes took place during this only stage in the history of the two groups in which there are no known corals.


2001 ◽  
Vol 52 (1-3) ◽  
pp. 63-102
Author(s):  
J. P. Guillaumet ◽  
M. Szabó
Keyword(s):  
La Tène ◽  

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