Shaping democratic festivals through Shakespeare in southern France: Avignon, Montpellier, Nice

Author(s):  
Florence March
Keyword(s):  
Author(s):  
G.E.M. Lippiatt

Dissenter from the Fourth Crusade, disseised earl of Leicester, leader of the Albigensian Crusade, prince of southern France: Simon of Montfort led a remarkable career of ascent from mid-level French baron to semi-independent count before his violent death before the walls of Toulouse in 1218. Through the vehicle of the crusade, Simon cultivated autonomous power in the liminal space between competing royal lordships in southern France in order to build his own principality. This first English biographical study of his life examines the ways in which Simon succeeded and failed in developing this independence in France, England, the Midi, and on campaign to Jerusalem. Simon’s familial, social, and intellectual connexions shaped his conceptions of political order, which he then implemented in his conquests. By analysing contemporary narrative, scholastic, and documentary evidence—including a wealth of archival material—this book argues that Simon’s career demonstrates the vitality of baronial independence in the High Middle Ages, despite the emergence of centralised royal bureaucracies. More importantly, Simon’s experience shows that barons themselves adopted methods of government that reflected a concern for accountability, public order, and contemporary reform ideals. This study therefore marks an important entry in the debate about baronial responsibility in medieval political development, as well as providing the most complete modern account of the life of this important but oft-overlooked crusader.


Cave art is a subject of perennial interest among archaeologists. Until recently it was assumed that it was largely restricted to southern France and northern Iberia, although in recent years new discoveries have demonstrated that it originally had a much wider distribution. The discovery in 2003 of the UK's first examples of cave art, in two caves at Creswell Crags on the Derbyshire/Nottinghamshire border, was the most surprising illustration of this. The discoverers (the editors of the book) brought together in 2004 a number of Palaeolithic archaeologists and rock art specialists from across the world to study the Creswell art and debate its significance, and its similarities and contrasts with contemporary Late Pleistocene ("Ice Age") art on the Continent. This comprehensively illustrated book presents the Creswell art itself, the archaeology of the caves and the region, and the wider context of the Upper Palaeolithic era in Britain, as well as a number of up-to-date studies of Palaeolithic cave art in Spain, Portugal, France, and Italy which serve to contextualize the British examples.


2011 ◽  
Vol 43 (2) ◽  
pp. 179
Author(s):  
Enzo Colonnelli

Are described and illustrated two new Italian species of <em>Ceutorhynchus</em>. The first of them, <em>C. apenninus</em> n. sp. from central Italy, collected on the montane crucifer <em>Isatis allionii</em> P. W. Ball., is close to<em> C. peyerimhoffi</em> Hustache from Spain, Italy and Algeria, also living on Isatis. The second,<em> C. magnanoi</em> n. sp. from southern Italy is very close to the French<em> C. matthiolae</em> Hoffmann, and was collected of <em>Matthiola</em> like the species from southern France.


1962 ◽  
Vol S7-IV (3) ◽  
pp. 362-379
Author(s):  
Alain Combes

Abstract The Boutenac hills in the northeastern Corbieres region of southern France, are part of the autochthonous foreland of the eastern Corbieres nappe. They are an isolated massif between the Paleozoic formations of the Alaric mountain on the west, and the Jurassic and Cretaceous formations of the Fontfroide chain on the east, entirely surrounded by alluvium. Structurally, they comprise Mesozoic formations on the east thrust over the Eocene on the west, on a fault that is the prolongation of the Saint Chinian frontal fault to the northeast. The Mesozoic formations comprise upper (?) Triassic shale and dolomite, sandy limestone, dolomite, and limestone; Jurassic red sandstones and shales; and upper Cretaceous transgressive clastics. The Eocene is limestone and marl overlain by continental conglomerate and molasse, transgressive on the west upon the Alaric Paleozoics. Folding and thrust and normal faulting are important in the structure.


1993 ◽  
Vol 22 (5) ◽  
pp. 772-780 ◽  
Author(s):  
MONICA FERRARONI ◽  
MARIETTE GERBER ◽  
ADRIANO DECARLI ◽  
SYLVIA RICHARDSON ◽  
ETTORE MARUBINI ◽  
...  

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