Cadastres, Misconceptions & Northern Gaul
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Dress and Cultural Difference in Early Modern Europe European History Yearbook Jahrbuch Für Europäische Geschichte
Dress and Cultural Difference in Early Modern Europe European History Yearbook Jahrbuch für Europäische Geschichte Edited by Johannes Paulmann in cooperation with Markus Friedrich and Nick Stargardt Volume 20 Dress and Cultural Difference in Early Modern Europe Edited by Cornelia Aust, Denise Klein, and Thomas Weller Edited at Leibniz-Institut für Europäische Geschichte by Johannes Paulmann in cooperation with Markus Friedrich and Nick Stargardt Founding Editor: Heinz Duchhardt ISBN 978-3-11-063204-0 e-ISBN (PDF) 978-3-11-063594-2 e-ISBN (EPUB) 978-3-11-063238-5 ISSN 1616-6485 This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 04. International License. For details go to http://creativecommons.org/licenses/by-nc-nd/4.0/. Library of Congress Control Number:2019944682 Bibliographic information published by the Deutsche Nationalbibliothek The Deutsche Nationalbibliothek lists this publication in the Deutsche Nationalbibliografie; detailed bibliographic data are available on the Internet at http://dnb.dnb.de. © 2019 Walter de Gruyter GmbH, Berlin/Boston The book is published in open access at www.degruyter.com. Typesetting: Integra Software Services Pvt. Ltd. Printing and Binding: CPI books GmbH, Leck Cover image: Eustaţie Altini: Portrait of a woman, 1813–1815 © National Museum of Art, Bucharest www.degruyter.com Contents Cornelia Aust, Denise Klein, and Thomas Weller Introduction 1 Gabriel Guarino “The Antipathy between French and Spaniards”: Dress, Gender, and Identity in the Court Society of Early Modern -
Haspengouwse Nederzettingsnamen. Een Inleiding. II
Haspengouwse nederzettingsnamen. Een inleiding. II Jan Segers bron Jan Segers, Haspengouwse nederzettingsnamen. Een inleiding. II (Mededelingen van de Vereniging voor Limburgse Dialect- en Naamkunde, Nr. 74). Hasselt 1994 Zie voor verantwoording: http://www.dbnl.org/tekst/sege010hasp02_01/colofon.htm © 2006 dbnl / Jan Segers i.s.m. 1 II. Natuurnamen en namen naar topografische kenmerken. In het kader van deze bijdrage behandelen wij de natuurnamen en de namen naar topografische kenmerken alleen voor zover zij aanleiding hebben gegeven tot nederzettingsnamen. Over hun gebruik in veldnamen, namen van grasland, enz. valt er heel wat meer te zeggen, maar dat valt buiten het bestek van deze bijdrage. 1. Natuurnamen. 1.1. Verhevenheid van de bodem. Het is bekend dat berg in het Nederlands taalgebied ook de geringste verhevenheid kan aanduiden (Gysseling 1978, 16). Dit wordt bevestigd door de vele -berg-namen in dorpsmonografieën ter aanduiding van erg variërende verhevenheden op diverse plaatsen in één en hetzelfde dorp. Berg komt in Haspengouw als simplex voor ter aanduiding van een nederzetting in Berg (bij Tongeren, onder Kleine Spouwen, onder Voeren). Nederzettingsnamen met -berg als grondwoord zijn Asberg (onder Tongeren), Blikkenberg (onder Hoeselt, Vliermaal, Werm: nederzettingsnaam?), Doesberg (onder Lanaken, Veldwezelt), Galgeberg>Gaverik (onder Bilzen), Heiberg>Heibrik (onder Hoeselt), Kaberg/Kauberg (onder Diepenbeek en Hoeselt), Keiberg (onder Halen, onder Vrijhern), Koekelsberg (onder Kleine Spouwen en Wellen; ‘een koekje’ wegens de ronde vorm), Loksbergen (onder Halen), Saffraanberg (onder Brustem), Scherpenberg (onder Broekem, Tongeren), Steenberg (onder Muizen-bij-Sint-Truiden en onder Sint-Lambrechts-Herk), Udenberg (onder Rosmeer), enz. Als eerste lid in een samenstelling komt berg- voor in Berghoven (onder Tongeren). -
Local Identities
Local Identities Editorial board: Prof. dr. E.M. Moormann Prof. dr.W.Roebroeks Prof. dr. N. Roymans Prof. dr. F.Theuws Other titles in the series: N. Roymans (ed.) From the Sword to the Plough Three Studies on the Earliest Romanisation of Northern Gaul ISBN 90 5356 237 0 T. Derks Gods,Temples and Ritual Practices The Transformation of Religious Ideas and Values in Roman Gaul ISBN 90 5356 254 0 A.Verhoeven Middeleeuws gebruiksaardewerk in Nederland (8e – 13e eeuw) ISBN 90 5356 267 2 N. Roymans / F.Theuws (eds) Land and Ancestors Cultural Dynamics in the Urnfield Period and the Middle Ages in the Southern Netherlands ISBN 90 5356 278 8 J. Bazelmans By Weapons made Worthy Lords, Retainers and Their Relationship in Beowulf ISBN 90 5356 325 3 R. Corbey / W.Roebroeks (eds) Studying Human Origins Disciplinary History and Epistemology ISBN 90 5356 464 0 M. Diepeveen-Jansen People, Ideas and Goods New Perspectives on ‘Celtic barbarians’ in Western and Central Europe (500-250 BC) ISBN 90 5356 481 0 G. J. van Wijngaarden Use and Appreciation of Mycenean Pottery in the Levant, Cyprus and Italy (ca. 1600-1200 BC) The Significance of Context ISBN 90 5356 482 9 Local Identities - - This publication was funded by the Netherlands Organisation for Scientific Research (NWO). This book meets the requirements of ISO 9706: 1994, Information and documentation – Paper for documents – Requirements for permanence. English corrected by Annette Visser,Wellington, New Zealand Cover illustration: Reconstructed Iron Age farmhouse, Prehistorisch -
Lanakenrsstraat 725 Opgrimbie Nieuwstraat Opgrimbie Centrum G7
De Lijn in uw gemeente 61 Wiemesmeer Kerk Opgrimbie Kikmolen 63 Kotem Kotem Weertveld Opgrimbie Heirstraat Opgrimbie Loograaf Wiemesmeer 725 Opgrimbie Kievitstraat Opgrimbie Kotem Kerk Zutendaal SchepeLANAKENrsstraat 725 Opgrimbie Nieuwstraat Opgrimbie Centrum G7 Opgrimbie Plein Boorsem Bampstraat 45 Opgrimbie Schoolstraat Boorsem Kerk Boorsem Spekstraat Zutendaal Weg naar As Opgrimbie Kruispunt Opgrimbie Davidstraat Opgrimbie Engelstraat Zutendaal Hoogstraat G7 Uikhoven Lange Weidestraat Zutendaal Eikenstraat 45 Uikhoven Daaluikhoven kapel 64 Zutendaal Gemeentehuis Zutendaal Ossenbergstraat Zutendaal Halmstraat 724 Rekem 725 Zutendaal Kerk 725 Zutendaal Gewaai Zutendaal 15 Augustusstraat Rekem Heirbaan Rekem OPZ 724 Uikhoven Uikhoven Schoorstraat Zutendaal Merellaan Rekem Daelwezeth Zutendaal Trichterweg 20a 724 725 Oud Rekem Eindhalte Uikhoven Kerk S T Zutendaal Smitsstraat A L K 64 E 10 R W E G Uikhoven Pastoor Goossenslaan PO PULIEREN AT LAAN RA Rekem Populierenlaan ST Zutendaal Driesprongstraat RG Rekem Kerk ZutendaalB EBessemer EN OL M Rekem Brug HEIDESTRAAT ZT utendaal Valkenbergstraat R IC HT G E E Zutendaal DriesstR raat W W E G T A RA ST Lanaken Oud Kantoorstraat LD VE Rekem Bovenwezet EN B IJZ E G S G S E Zutendaal Wit Paard Zutendaal Gijzenveldstraat E M W R E N O R E S E L T 20aE E T R R W A S A E T G 25 45 Neerharen Ziekenhuis Oost-Limburg 61 45 Campus Sint-Barbara 63 G7 Lanaken ZOL Campus Sint-Barbara Neerharen Steenweg 178 724 N A A 724 B S T A Zutendaal Roelen A T S M A A ST Neerharen Verbindingslaan RIC HT ERW EG De -
Pagan Survivals, Superstitions and Popular Cultures in Early Medieval Pastoral Literature
Bernadette Filotas PAGAN SURVIVALS, SUPERSTITIONS AND POPULAR CULTURES IN EARLY MEDIEVAL PASTORAL LITERATURE Is medieval pastoral literature an accurate reflection of actual beliefs and practices in the early medieval West or simply of literary conventions in- herited by clerical writers? How and to what extent did Christianity and traditional pre-Christian beliefs and practices come into conflict, influence each other, and merge in popular culture? This comprehensive study examines early medieval popular culture as it appears in ecclesiastical and secular law, sermons, penitentials and other pastoral works – a selective, skewed, but still illuminating record of the be- liefs and practices of ordinary Christians. Concentrating on the five cen- turies from c. 500 to c. 1000, Pagan Survivals, Superstitions and Popular Cultures in Early Medieval Pastoral Literature presents the evidence for folk religious beliefs and piety, attitudes to nature and death, festivals, magic, drinking and alimentary customs. As such it provides a precious glimpse of the mu- tual adaptation of Christianity and traditional cultures at an important period of cultural and religious transition. Studies and Texts 151 Pagan Survivals, Superstitions and Popular Cultures in Early Medieval Pastoral Literature by Bernadette Filotas Pontifical Institute of Mediaeval Studies This book has been published with the help of a grant from the Canadian Federation for the Humanities and Social Sciences, through the Aid to Scholarly Publications Programme, using funds provided by the Social Sciences and Humanities Research Council of Canada. LIBRARY AND ARCHIVES CANADA CATALOGUING IN PUBLICATION Filotas, Bernadette, 1941- Pagan survivals, superstitions and popular cultures in early medieval pastoral literature / by Bernadette Filotas. -
The Rhine: Germany's River, Not Germany's Boundary
Source: E.M. Arndt, Deutschlands Fluss, aber nicht Deutschlands Gränze, English trl. UvA Talen / SPIN. the French was as bad as it was foolish. One would have The Rhine: Germany’s river, not Germany’s thought that ten years, indeed twenty years, of blindness and misfortune might have sent a little light into their dark minds boundary and brought the errants back into line, especially since the French had long ago overturned their own proof, but far from it. There are still many who behave, indeed who exhaust Ernst Moritz Arndt themselves in deductions and proofs, as if the Rhine as the border between France and Germany is something indispu- table and settled. So effective is constant repetition, and so little are most Germans – who pride themselves on their ‘The Rhine is France’s natural boundary’ is what Sully proved profundity in thought and speech – accustomed to thinking. 1600 and 1610; ‘the Rhine is France’s natural boundary,’ The empty echoing of foreign opinions, especially the proclaimed Richelieu in 1625 and 1635; ‘the Rhine is France’s echoing of French hocus-pocus and sophistries, has sadly natural boundary,’ declared Count d’Avaux in the 1640s at become too much of a fashion on this side of the Rhine, in Münster, in the holy places where Hermann the Cheruscan had the country where thoroughness and depth of thought is once made a dufferent typeof declaration to the Romans; ‘the supposed to reside. Given this state of affairs, especially this Rhine is France’s natural boundary,’ resounded from 1670 to sad state of German minds and hearts, I consider it not super- 1700 in Louvois’ and Colbert’s speeches in Louis XIV’s council fluous to present our ancient, magnificent and holy River of state, and the court poets Boileau and Racine sang it in the Rhine, what it was, is and will be, to the good German antechamber; ‘the Rhine is France’s natural boundary’ cried the people, who are confused by too many political prattlers and monsters on the Seine from 1790 to 1800. -
Stratigraphic Architecture of the Upper Cretaceous and Cenozoic Along the Southern Border of the North Sea Basin in Belgium
Netherlands Journal of Geosciences / Geologie en Mijnbouw 83 (3): 155-171 (2004) Stratigraphic architecture of the Upper Cretaceous and Cenozoic along the southern border of the North Sea Basin in Belgium N. Vandenberghe1, S.Van Simaeys1, E. Steurbaut2'1, J.W.M. Jagt3 & P. J. Felder3 1 Historical Geology, Redingenstraat 16, B-3000 Leuven, Belgium. E-mail: [email protected] (corresponding author) 2 Royal Belgian Institute of Natural Sciences, Vautierstraat 29, B-1000 Brussels, Belgium 3 Natuurhistorisch Museum Maastricht, De Bosquetplein 6, NL-6211 KJ Maastricht, The Netherlands Manuscript received: February 2004; accepted: August 2004 Abstract The Late Cretaceous and Cenozoic sedimentary record in the Campine Basin along the southern border of the North Sea Basin is analysed in terms of sequence stratigraphy. All available biostratigraphic, and in some cases, magnetostratigraphic data are used to constrain the sequence chronostratigraphy. The relative geographic extent of the strata is used as an indication of the relative sea level. Tectonic and eustatic components could be distinguished in several cases using regional geological information. Generally, sequences consist of transgressive and highstand systems tracts only and have flat, abrasion- type lower boundaries. Lowstand deposits are only identified as infill of erosional space, which generally implies marked tectonic uplift. Several eustatic and tectonic events can be correlated with similar events known elsewhere in the North Sea Basin. The time intervals spanned by the different sequences vary considerably, pointing out different control mechanisms. Keywords: Sequence stratigraphy, North Sea Basin, Late Cretaceous, Cenozoic Introduction The analysis presented below starts with the Santonian, when subsidence resumed in the Campine The study area is situated at the southern part of die Basin, and ends in die Pliocene. -
A New Lithostratigraphic Scale for the Palaeogene of Belgium
Bulletin de la Société belge de Géologie, T. 102 (1-2), 1993, pp. 215-229. Bulletin van de Belgische Vereniging voor Geologie. Ed. 1994 A NEW LITHOSTRATIGRAPHIC SCALE FOR THE PALAEOGENE OF BELGIUM by R. MARECHAL' ABSTRACT The study of the Belgian Tertiary started more than 150 years ago. Since that time such an enormous amount of data has been gathered, that the commission in charge of the revision of the stratigraphic scale of the Belgian Tertiary decided to limit its activity to the elaboration of a lithostratigraphic scale according to the rules of the IUGS International Subcommission on Stratigraphic Classification. The fundamental unit of such a classification system is the Formation and therefore much attention has been given to Formation names. Some of these names are in use since a very long time, others are new. Preference has been given to names of well known localities situated within the main outcrop areas of the Formation under consideration. Formations may be completely or partially subdivided into Members or may remain undivided. Member names have been selected according the same rules as Formation names. Since members are mostly homogeneous in lithology the Member name may be followed by a rock or sediment name (Vlierzele sand, Asse clay). Most formations have been assembled into Groups. Group names should be considered as tentative. It is questionable whether an internationally admitted chronostratigraphic name (Rupelian, Ypresian) may also be used as a Group name (Rupel, Ieper). The efforts of the National Commission for Stratigraphy of the Tertiary resulted in a proposal for a lithostratigraphic scale for the Palaeogene, which was distributed to a limited number of persons in 1988 and discussed consecutively. -
Noodonderzoek in De Sint-Mauritiuskerk Te Bilzen (Prov. Limburg)
Archeologie in Vlaanderen IV - 1994, 169-186 Noodonderzoek in de Sint-Mauritiuskerk te Bilzen (prov. Limburg) Wemer Wouters & Brigitte Cooremans I Inleiding het architectenbureau Spectrum uit Hasselt kon den enkele bijkomende sonderingen uitgevoerd Restauratiewerken aan de Sint-Mauritiuskerk te worden (fig. 2). De eerste interventie vond plaats Bilzen (fig. I) en het plaatsen van een nieuw ver- van 14 tot en met 22 oktober 1993. Bij het graven warmingssvsteem vormden de aanleiding tot een van de verwarmingskanalcn aan het westeind van noodinterventie in verschillende tijdsintervallen. het rond 1905 ingekorte koor, stootten arbeiders Dank zij de medewerking van de kerkfabriek Sint- op een grafkelder in baksteen (fig. 2: III), waarna Mauritius, de firma Goedleven uit Brasschaat en het Instituut voor het Archeologisch Patrimonium 1 Algemeen situatieplan. (I.A.P) betrokken werd bij de werken. Een tweede General location map. grafkelder (fig. 2: II), in mergel, die iets meer wes telijk te situeren is, op de grens van het oorspron kelijke gotische koor en het schip, werd aangesne den bij het leggen van de fundering van de trap naar het hoger gelegen koor. Van de gelegenheid werd gebruik gemaakt om te peilen naar het be staan van eventuele voorgangers van de gotische kerk (fig. 2: I, IV en V). In de daarop volgende maanden werden enkele bijkomende werkputten uitgezet: van 20 tot en met 26 januari 1994 aan de zuidzijde van de middenbeuk (fig. 2: VI), van 31 januari tot en met 5 februari in de zuidelijke zij beuk (fig. 2: VII) en tenslotte van 14 tot en met 18 maart aan de westzijde van het schip (fig. -
Overzichten Van De Archieven En Verzamelingen Van Het Rijksarchief
G 74 Rijksarchief in BelGIDSEN 74 J. V AN DER EYCKEN in België Rijk Overzichten van de archieven en verzamelingen van het Rijksarchief te Hasselt I Overzichten van de archieven en verzamelingen van het Rijksarchief te Hasselt het Rijksarchief van en verzamelingen de archieven van Overzichten e recherc ief Archievenin België van overheidsinstellingen Rijksarchief vanaf 1795 (tot 2009) Archieven van overheidsinstellingen vanaf 1795 (tot 2009) vanaf overheidsinstellingen van Archieven elgiëijksarchiefJOHAN VAN DER EYCKEN Rijkin Belgi chief in België Rijksarchief in België 4894 ISBN 978-90-5746-256-6 ië Rijksarch 9789057462566 in België Rijksarchief in B D/2010/531/046 I ksarchief in OVERZICHTEN VAN DE ARCHIEVEN EN VERZAMELINGEN VAN HET RIJKSARCHIEF TE HASSELT I ARCHIEVEN VAN OVERHEIDSINSTELLINGEN VANAF 1795 (TOT 2009) ALGEMEEN RIJKSARCHIEF EN RIJKSARCHIEF IN DE PROVINCIËN GIDSEN 74 ISBN : 978 90 5746 256 6 Algemeen Rijksarchief D/2010/531/046 Bestelnummer: Publ. 4894 Algemeen Rijksarchief Ruisbroekstraat 2 1000 Brussel De volledige lijst van onze publicaties kan u gratis bekomen op eenvoudig verzoek ([email protected]) of raadplegen op internet (http://arch.arch.be). Overzichten van de archieven en verzamelingen van het Rijksarchief te Hasselt I Archieven van overheidsinstellingen vanaf 1795 (tot 2009) door Johan VAN DER EYCKEN Brussel 2010 INHOUDSOPGAVE Inhoudsopgave............................................................................................5 Woord vooraf............................................................................................19 -
Upper Oligocene Lithostratigraphic Units and the Transition to The
GEOLOGICA BELGICA (2020) 23/3-4: 113-125 Upper Oligocene lithostratigraphic units and the transition to the Miocene in North Belgium Michiel DUSAR1* & Noël VANDENBERGHE2 1 Royal Belgian Institute of Natural Sciences - Geological Survey of Belgium, Brussels, Belgium; [email protected]. 2 Dept. Earth and Environmental Sciences, KU Leuven, Belgium; [email protected]. * corresponding author. ABSTRACT. The presence of Chattian deposits in Belgium was confirmed in the early 20th century by correlation of their mollusc faunas with the type Chattian in Germany. Consequently, the Voort Formation in the Campine Basin and the Boncelles Sand on the northeastern Ardennes were established and assigned a Chattian age. Contacts with underlying Rupelian and overlying Burdigalian formations are marked by hiatuses, linked mainly to end-Oligocene Savian tectonics and reactivation of the Roer Valley Graben (RVG). On the Campine Block, only the lower part of the Chattian, the Voort Sand is deposited, increasing in thickness in the direction of the RVG and including a geophysically traceable clayey marker horizon allowing the mapping of this unit in the Campine Basin, into the Netherlands and even possibly link it to the hydrostratigraphic subdivision of the Chattian in the Lower Rhine Graben. Lithologically, these uppermost Paleogene Chattian deposits form the base of the Neogene sequence along the Southern Bight of the North Sea, characterised by predominantly glauconite-bearing sand. The Chattian sediments rapidly become thicker in the strongly subsiding RVG, resulting in a more continuous sedimentation with the development above the Voort Sand of a clay unit and another sand unit, forming together the Veldhoven Formation. -
The Campine Plateau 12 Koen Beerten, Roland Dreesen, Jos Janssen and Dany Van Uytven
The Campine Plateau 12 Koen Beerten, Roland Dreesen, Jos Janssen and Dany Van Uytven Abstract Once occupied by shallow and wide braided channels of the Meuse and Rhine rivers around the Early to Middle Pleistocene transition, transporting and depositing debris from southern origin, the Campine Plateau became a positive relief as the combined result of uplift, the protective role of the sedimentary cover, and presumably also base level fluctuations. The escarpments bordering the Campine Plateau are tectonic or erosional in origin, showing characteristics of both a fault footwall in a graben system, a fluvial terrace, and a pediment. The intensive post-depositional evolution is attested by numerous traces of chemical and physical weathering during (warm) interglacials and glacials respectively. The unique interplay between tectonics, climate, and geomorphological processes led to the preservation of economically valuable natural resources, such as gravel, construction sand, and glass sand. Conversely, their extraction opened new windows onto the geological and geomorphological evolution of the Campine Plateau adding to the geoheritage potential of the first Belgian national park, the National Park Hoge Kempen. In this chapter, the origin and evolution of this particular landscape is explained and illustrated by several remarkable geomorphological highlights. Keywords Campine plateau Á Meuse terraces Á Late Glacial and Holocene dunes Á Tectonic control on fluvial evolution Á Polygonal soils Á Natural resources Á Coal mining 12.1 Introduction (TAW: Tweede Algemene Waterpassing) in the south, to ca. 30 m near the Belgian-Dutch border in the north (Fig. 12.1 The Campine Plateau is an extraordinary morphological b). The polygonal shape of this lowland plateau has attracted feature in northeastern Belgium, extending into the southern a lot of attention from geoscientists during the last 100 years, part of the Netherlands (Fig.