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The use and distribution of Faience in the Ancient East and Prehistoric Europe

Published online by Cambridge University Press:  27 May 2014

Extract

Twenty years have elapsed since H. C. Beck and the present writer published a preliminary paper on the origin of British faience beads with special reference to those of the segmented variety and, except for the discovery and recognition of many new specimens over much wider areas it may be said that nothing has emerged to alter materially the general conclusions there enunciated that an Egyptian origin was the most likely for a number of the beads and that their dissemination to the British Isles took place during the Eighteenth Dynasty around about 1400 B.C.

At the time of writing we not unnaturally concentrated on British specimens, as European analogues appeared to be conspicuously absent, and confined our attention primarily to morphological characters. We had, however, projected a wider study to embrace faience objects in general and, if possible, to adduce spectrographic evidence as further proof of identity or otherwise. Unfortunately the sudden death of Mr Beck in 1939 and the intervention of the war years greatly retarded progress in this direction. But the rapid recognition of old finds and the accumulation of new ones, mostly in Europe, in post-war years, coupled with a number of spectrographic analyses that have since been carried out with the help of Mr L. C. Thomas, now renders it desirable to review such progress as has been made in this most difficult and complex subject.

Type
Research Article
Copyright
Copyright © The Prehistoric Society 1957

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References

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page 54 note 1 The Orient and Europe,’ Amer. J. Arch., XLIV, 1939, 20Google Scholar. These graves also contained segmented bone beads similar to those from Hal Tarxien, Malta, and the marine shells Cardium, Pectunculus, Columbella rusticana and Tridacna are common proving contact with the Mediterranean.

page 55 note 1 The often mentioned bead in the Melk Museum from an Aunjetitz grave at Wachburg, Melk (Prahist. Zeitschrift, 1934, 144Google Scholar; IPEK, 1936, 130Google Scholar) has also been examined through the kindness of Professor Pittioni. It is an oblate bead of true glass, blue in colour, 11 mm. diameter, 8 mm. thick with 2 mm. perforation, and thus confirms Willvonseder's diagnosis (Forschungen und Fortschritte, 1937, 3Google Scholar).

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page 56 note 1 Behrens, G., Bodenurkunden aus Rheinhessen, I, Die Vorrömische Zeit, Mainz 1927, 26Google Scholar, no. 90. These gold beads seem to be very similar to those from Ireland in the British Museum, Archaeologia, LXXXV, 1936, 213Google Scholar.

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page 56 note 6 Norwich Castle Museum no. 37.21/134 of the Alan Cozens–Hardy Colman Memorial gift; two blue faience quoits labelled Nineteenth Dynasty, but on whose authority not known. Diameter 1 inch with perforation ½ inch and of triangular section with raised rim or moulding round edge of perforation as in the Scottish specimens.

page 56 note 7 Lachish II: The Fosse Temple, 1940, pl. XXI, no. 50.

page 56 note 8 Acta Archaeologica, XXV, 1954, 241Google Scholar. In publishing this find Professor C. J. Becker draws attention to the similarity of form of a number of Southern Scandinavian amber beads to those of faience and glass, and illustrates two amber segmented bicones from Serritslev, Jutland, which he compares convincingly with the faience segmented bicone or barrel beads from Boscregan, Cornwall. He rightly infers that the rarity and value of these faience products in northern and western Europe had a marked influence on the form of the indigenous amber beads of Denmark, and of other materials in the British Isles.

page 57 note 1 Faience beads of various types and colours are stated to have been found at an ancient bead factory on the Pic des Singes, Bougie,.Algeria (Recueil des Notices et Mémoires de la Société Archéologique du Départment de Constantine, 4 S, VIII, 1906, 69Google Scholar). The finds of unknown provenance are so badly described and the illustrations are so poor that they are not considered worthy of more than passing note here.

page 57 note 2 Proc. Prehist. Soc., XIX, 1953, 68Google Scholar.

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page 57 note 4 I am indebted to Mrs C. M. Piggott and Professor Hawkes for this information. Professor Brea kindly submitted some fragments of the beads for examination, vide Appendix.

page 57 note 5 Ríordáin, Ó and Stone, , Proc. Roy. Irish Acad., 56, 1954, 355Google Scholar. For spectrographic analyses of these beads see below. Dr Glyn Daniel informs me that small blue glass beads have been found at nine sites in the south of France: in the Grotte de Bringaret, Aude; in the Romanin ossuary near St Remy, Bouches du Rhone; in the Grotte Monier, Var; Dolmen de la Grailhe, Gard; Dolmen de Pilandes-Costes, Aveyron; Grotte de St. Jean d'Alcas, Aveyron; in an allée couverte at Fournes, Hérault; and in the Grotte de la Madeleine, Hérault. Dr J. Arnal has kindly supplemented this information by stating that wirewound glass beads are known from Gard (1), Hérault (1), Aveyron (25 or more), Aude (24 or more), Gironde (1 certain and probably 5 or more), Loir et Cher (many), Cotes du Nord (1) and Finistère (1 at least). All suggest trade with the Eastern Mediterranean comparable with the contemporary faience beads.

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page 59 note 3 Adze no. 685, Proc. Prehist. Soc., XVII, 1951, 96 and 157Google Scholar. The non-ophitic dolerite of this adze is identical with that of another exotic axe from Cornwall, no. 674.

page 59 note 4 Unpublished axe no. 877 of the South-Western Sub-Committee from Calne, Wiltshire. This is a corundum or emery which Lt.-Colonel Campbell-Smith and Dr Wallis consider can only have originated from Naxos or a nearby island in the Greek archipelago.

page 59 note 5 Proc. Prehist. Soc., XIX, 1953, 224Google Scholar.

page 59 note 6 Antiquaries J., XXXII, 1952, 30Google Scholar.

page 59 note 7 For a re-appraisal of these discs and their probable dating post 1400, see de Navarro, J. M., ‘The British Isles and the beginning of the Northern Bronze Age’ in The Early Cultures of North-West Europe (H. M. Chadwick Memorial Studies), 1950, 100–4Google Scholar.

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page 59 note 9 Annual British School, Athens, XXV, 19211923, 57Google Scholar. The Egyptian necklaces on which the beads occur are in the Ashmolean Museum, no. EE 214 from Thebes and no. EE 250 from Egypt, both of the Eighteenth Dynasty.

page 61 note 1 These routes and the legendary expeditions of the Argo have been exhaustively examined in connexion with the amber trade routes by MissBacon, Janet in her Voyages of the Argonauts, Methuen 1925Google Scholar. She asks the question ‘Is it a mere coincidence that the Argonauts, in one account or another, are credited with travelling by all these routes, or routes so like them as to be probably garbled versions of the same trade routes ? It seems hardly possible to entertain the idea of such a fourfold coincidence’ (p. 121). She pertinently concludes that ‘Argo was many ships’ used in trading expeditions in search of amber and gold.

page 68 note 1 DrRitchie, P. D. in ‘Far Eastern glass; some Western origins,’ by Seligman, C. G. and Beck, H. C., Bull. Museum Far Eastern Antiquities, no. 10, Stockholm, 1938Google Scholar; Spectrographic studies on Ancient Glass,’ by Ritchie, P. D., Tech. Studies in the Field of the Fine Arts, V, 1937, 209Google Scholar; and ‘Egyptian Glass, mainly of the 18th Dynasty, with special reference to its cobalt content,’ by M. Farnsworth and P. D. Ritchie, ibid., VI, 1938, 154.

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page 73 note 1 Ríordáin, Ó and Stone, , Proc. Roy. Irish Acad., 56, 1954, 354–8Google Scholar.

page 73 note 2 A specimen obtained from an excavation by M. Pierre Temple, who, through Dr J. Arnal, kindly submitted it as a sample of similar type to the glass beads found with a faience spacing bead in a cave at Treille, Mailhac, Aude. Dr Arnal tells us that similar ones occur in the dolmens of Aveyron and in the Grotte de la Clapade. See note on page 57, for possible other examples.

page 73 note 3 Both of these materials were used in our original endeavours to produce Scottish glassy faience,’ Archaeologia, LXXXV, 210Google Scholar.

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