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Download - The American School of Classical Studies at Athens

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566<br />

PHILIP P. BETANCOURT ET AL.<br />

Obsidian. Some cortex preserved; rounded retouch on distal end on both surfaces.<br />

Scraper.<br />

38 Blade, complete Fig. 12<br />

HCH 04-334. Room 3, lower levels, unit 4. L. 2.45, W. 0.96, Th. 0.28 cm.<br />

Chert (white, 10YR 8/1). One ridge; retouch <strong>at</strong> proximal end cre<strong>at</strong>ing a point.<br />

39 Crested blade, distal end Fig. 12<br />

HCH 204. Room 4, upper levels (1983 season). PL. 1.95, W. 0.81,Th. 0.15 cm.<br />

Obsidian. Chipped edges.<br />

Ground Stone<br />

<strong>The</strong> ground stone tool assemblage from the cave is not very impressive:<br />

five tools and two possible tools, found in a st<strong>at</strong>e <strong>of</strong> poor preserv<strong>at</strong>ion.<br />

<strong>The</strong> identified tools consist <strong>of</strong> a sandstone celt (Fig. 12:40), a quartzite<br />

whetstone and pounding pl<strong>at</strong>form (Fig. 12:41), and two limestone pounders.<br />

<strong>The</strong> celt is <strong>of</strong> gre<strong>at</strong>est interest. Stone axes appear to be rare in Minoan<br />

funerary contexts, as very few stone axes have been reported from Minoan<br />

EM tombs. From the Mesara tombs come two stone axes from Moni<br />

Odigitrias,72 one from Drakones, and two from Kal<strong>at</strong>hiana.73 Two more<br />

stone axes were published from the Trapeza cave, one identified as green<br />

stone, the other as black limestone.74<br />

Whetstones are more commonly found in tombs, but in the Mesara<br />

these tend to be more intric<strong>at</strong>e than the example from the Hagios Charalambos<br />

cave. <strong>The</strong>y are made <strong>of</strong> fine sandstone and are long and narrow<br />

with a hole pierced <strong>at</strong> one end.75 Five marble and schist whetstones from<br />

the Trapeza cave correspond more closely to the Hagios Charalambos<br />

example in th<strong>at</strong> they consist <strong>of</strong> unshaped cobbles with abraded faces and<br />

without a hole.76<br />

Selected C<strong>at</strong>alogue<br />

40 Celt, complete Fig. 12<br />

HCH 02-111. Room 4/5 entrance, unit 3 (unit HCH 02-2/3 entrance-3).<br />

L. 4.7, W. 4.3, Th. 1.7 cm; Wt. 40 g. Sandstone (red, 2.5YR 5/6, fine-grained and<br />

poorly sorted). W<strong>at</strong>erworn pebble, trapezoidal shape; worn on large end.<br />

41 Whetstone, broken on one end Fig. 12<br />

HCH 65. Room 4, upper levels (1983 season). Max. L. 8.2, max. W. 5.5,<br />

max. Th. 2.25 cm; Wt. 162 g. Quartzite (dark grayish brown, 2.5Y 4/2). N<strong>at</strong>ural<br />

w<strong>at</strong>erworn cobble, ovoid shape; two faces abraded smooth; pecking on both ends<br />

and center <strong>of</strong> one face.<br />

72. See reference in Carter 1998,<br />

appendix 4.<br />

73. Xanthoudides 1924, pp. 80, 86,<br />

pl. 46:a.<br />

74. Pendlebury, Pendlebury, and<br />

Money-Coutts 1935-1936, pp. 114,<br />

116, pl. 17.<br />

75. Xanthoudides 1924, pp. 20, 66,<br />

80, pls. 13, 39, 43, 54 (from Koumasa,<br />

Porti, Drakones, and Pl<strong>at</strong>anos).<br />

76. Pendlebury, Pendlebury, and<br />

Money-Coutts 1935-1936, pp. 113,<br />

116, pl. 17.

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