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v15_0235 - SUDOVESTE DELLA GALLIA Drachme imitation de Rhodè

SUDOVESTE DELLA GALLIA Drachme imitation de Rhodè VF
MONNAIES 15 (2002)
起拍价 : 90.00 €
估价 : 180.00 €
未售出的物品
种类 Drachme imitation de Rhodè
日期: c. 218 AC.
材质 silver
直径 16,5 mm
重量 3,02 g.
稀少度 R2
关于品相的说明
Exemplaire fruste montrant la dégénérescence du type de la drachme de Rhodè, mais parfaitement identifiable et comparable aux autres exemplaires répertoriés
出版目录中的项代码 :

正面


正面的文字 ANÉPIGRAPHE.
正面的说明书 Lisse.

背面


背面的文字 ANÉPIGRAPHE.
背面的说明书 Croix bouletée et cerclée, accostée de chevrons renversés et de lunules.

评论


Poids léger. Normalement ce type appartient à la série lourde des imitations de Rhodè comme les deux exemplaires du musée de Zurich qui pèsent respectivement 3,60 g et 3,68 g. D’après le poids, ce nouveau type de drachme serait postérieur au début de la deuxième guerre Punique.

历史细节


SOUTH-WESTERN GAUL

(3rd century BC)

The notion of people or tribe seems to disappear with regard to certain attributions when one examines the coinage of imitations of Emporion or Rhodè. If the prototypes are struck beyond the Pyrenees, the imitations were issued on both sides of the mountain range. The early disappearance of R. Boudet (1958-1995) did not allow the latter to establish a corpus of these coins. The finds are not limited to Aquitaine, but are spread over the great West between the Loire and the Pyrenees, i.e. nearly a third of the territory of ancient Gaul.. The finds of imitations of the drachma of Emporion, which seems to have had a wider distribution, are numerous and spread over the whole of the geographical area: from Charnizay in the Indre-et-Loire or Issoudun in the 'Indre to Ruscino in the Pyrénées-Orientales. The Rhodè coin finds are concentrated in Aquitaine and do not go beyond the course of the Garonne and the Dordogne with the treasures of Mouleydier in Dordogne or Mouliets-et-Villemartin in Gironde and as far as Montlaurès in Aude and Foix in Arriège. To whom should these coinages, sometimes very different, which do not present any homogeneity at the level of the typological series be attributed?.

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