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Northern Anatolia before Classical Times

Published online by Cambridge University Press:  15 June 2015

Extract

That part of northern Anatolia known in Greek and Roman times as Bithynia and Paphlagonia comprises a number of high ridges running from west to east, through which the rivers break their way in their tortuous courses down to the Black Sea. The region discussed in this article in fact comprises Paphlagonia, the eastern half of Bithynia and part of Phrygia, from the lower Sakarya to the mouth of the Halys; but, since these names do not apply to the Bronze Age, the whole will be termed northern Anatolia. As far south as the crest of the main ridge bounding the Anatolian plateau along its north side the land has a maritime climate quite different from that of either the plateau or the Mediterranean coast: rainfall is abundant, even at times in the summer; deciduous forests cover these north-facing slopes, right to the top. Sinop provides the best natural harbour on this coast. The change to the steppe country of the plateau is abrupt.

Type
Research Article
Copyright
Copyright © The British Institute at Ankara 1956

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References

1 Özgüç, , Türk Tarih Kongresi (1943), pp. 393419Google Scholar; and in Belleten IX (1945), pp. 361400Google Scholar.

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16 Excavated by Prof. E. Akurgal and Prof. Budde: the former kindly allowed me to look at the Demirci pottery in the University of Ankara.

17 Troy, Vol. I (Plates), Types C25 and C27. Perhaps ibid. (Text), pp. 378, 403.

18 Ibid. (Plates), pl. 414 (10).

19 H. Koşay, in a brief guide, Alaca Hüyük (frontispiece).

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24 Troy, Vol. I, pl. 223b (Type C17).

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30 Demirci Hüyük, pl. 10 (2 and 5).

31 Information kindly supplied by Prof. Bittel.

32 Belleten X (1946), pl. LXXVII, 4Google Scholar. But pottery recently collected from this very rich site shows that this fruitstand is almost certainly of Late Bronze Age date, with close parallels at Beycesultan III–I.

33 A.S. IV, p. 189Google Scholar. Mellart also comments on the fact that the Kumtepe pottery, still unpublished, includes fruitstands of Alışsar type.

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39 Ibid., pl. 13 (9); pls. 7 (12) and 8 (5); pl. 13 (8); pl. 13 (19) and fig. 3 (p. 15), nos. 5, 6, 12.

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69 Demirci Hüyük, passim: also sherds from other sites in this province. Side-spouts are another feature in common (cf. Demirci Hüyük, pls. 6(12) and 7).

70 Ibid., pl. II (7).

71 Ausgrabungen, pl. XCIV.

72 Troy, Vol. II, pl. 180 (27, 28, 30, 32) (Type A33); also pl. 259.

73 Demirci Hüyük, pl. 7 (2).

74 Fouilles, pl. LXXV (205).

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79 Troy, Vol. II, pl. 181 (2) (Type A11).

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90 T.T.K. (1943), pl. VIII (1, 7, 11).

91 A sherd from Yassı Hüyük (Çivril) illustrates this well. Also bowls from Beycesultan, (A.S. V, p. 63Google Scholar, fig. 10).

92 Troy, Vol. III, pl. 444 (8): Types A93 and A96. It seems probable that the shapes termed Minyan developed first in western Anatolia.

93 A.S. I, pp. 50–1Google Scholar (Group 39), and p. 59. See also: Troy, Vol. III, pl. 439 (II); D.T.C.F.D. VIII (1950)Google Scholar, pl. VIIIa; Beycesultan level IV (unpublished).

94 Prehistoric Mersin, p. 247, fig. 156 (nos. 10, 13); p. 249, fig. 157 (1, 2, 5, 6, 7).

95 Bittel-Naumann, , Boğazköy-Hattusa, p. 109Google Scholar (nos. 6, 7, 34, etc.). H. Koşay, Ausgrabungen, pl. XLIII, figs. 3 and 4.

96 A conclusion in no wise conflicting with our present knowledge of Second Millennium historical geography.

97 A.S. I, p. 50Google Scholar, fig. 12, no. 12: note comparison with Alışar.

98 Bittel, K., Boğazköy: Die Kleinfunde der Grabungen 1906–12 (Leipzig, 1937)Google Scholar, pl. 31, no. 21.

99 Fouilles, pl. XXIX (75).

100 e.g. at Polatlı, : A.S. I, p. 40Google Scholar (Group 8).