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Crossing the Borders: New Methods and Techniques in the Study of Archaeological Materials from the Caribbean

by Corrine L. Hoffman, et. al.

by Corrine L. Hoffman, et. al.

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Lithic Technology / 97<br />

north. Red jasper can be found on <strong>the</strong> leeward coast <strong>of</strong> Basse- Terre isl<strong>and</strong> <strong>and</strong> on<br />

Les Sa<strong>in</strong>tes isl<strong>and</strong>s. The pieces <strong>of</strong> <strong>the</strong> collection show a low degree <strong>of</strong> corti cality. 4<br />

With <strong>the</strong> exception <strong>of</strong> <strong>the</strong> igneous stones <strong>in</strong>troduced <strong>in</strong> <strong>the</strong> site untreated, all <strong>the</strong><br />

o<strong>the</strong>r types <strong>of</strong> raw materials have been brought to <strong>the</strong> site at least partially prepared<br />

(<strong>the</strong>re are no fully cortical flakes associated with those raw materials).<br />

The goals <strong>of</strong> <strong>the</strong> reduction sequence are difficult to identify. Only two pieces<br />

have clear evidence <strong>of</strong> secondary work. But six o<strong>the</strong>r pieces show macrowear<br />

traces. All those pieces can be regarded as flakes; <strong>the</strong>ir average length is 28 mm.<br />

They have no specific morphology but <strong>the</strong>y are <strong>in</strong> general th<strong>in</strong>ner than <strong>the</strong> rest <strong>of</strong><br />

<strong>the</strong> collection. Thus we can suppose that one <strong>of</strong> <strong>the</strong> objectives <strong>of</strong> <strong>the</strong> reduction sequence<br />

is <strong>the</strong> production <strong>of</strong> th<strong>in</strong>, amorphous flakes that were not morphologically<br />

predeterm<strong>in</strong>ed. However, <strong>the</strong> presence <strong>of</strong> small scar negatives on <strong>the</strong> cores seems to<br />

<strong>in</strong>dicate a second objective <strong>of</strong> <strong>the</strong> reduction sequence: that <strong>of</strong> small flakes. Some <strong>of</strong><br />

those last removals are <strong>in</strong> average only 13 mm long. Thus, <strong>the</strong>re are two goals <strong>of</strong> <strong>the</strong><br />

reduction sequence: <strong>the</strong> production <strong>of</strong> “large” th<strong>in</strong> flakes <strong>and</strong> <strong>the</strong> production <strong>of</strong><br />

small flakes. However, small flakes were not produced on <strong>the</strong> igneous stones.<br />

Two types <strong>of</strong> percussion techniques have been identified <strong>in</strong> <strong>the</strong> collection, direct<br />

freeh<strong>and</strong> percussion with a stone hammer <strong>and</strong> bipolar techniques. 5 The percussion<br />

techniques have been used for different purposes or at different stages <strong>of</strong><br />

<strong>the</strong> chaîne opératoire.<br />

The “large” th<strong>in</strong> flakes have been obta<strong>in</strong>ed by two methods. First, some cores<br />

have been knapped with direct freeh<strong>and</strong> percussion follow<strong>in</strong>g a simple discoid<br />

method. This method, first identified for <strong>the</strong> middle Paleolithic cultures, is def<strong>in</strong>ed<br />

by bifacial conception <strong>of</strong> <strong>the</strong> core volume associated with a centripetal recurrent<br />

production <strong>of</strong> flakes. This is one <strong>of</strong> <strong>the</strong> simplest recurrent knapp<strong>in</strong>g methods. The<br />

identification <strong>of</strong> that method is easy by <strong>the</strong> observation <strong>of</strong> <strong>the</strong> cores (Figure 7.2d)<br />

<strong>and</strong> can be supported by <strong>the</strong> presence <strong>of</strong> éclats débordants. The second method uses<br />

<strong>the</strong> bipolar technique (Figure 7.2c). Those débitage are conducted accord<strong>in</strong>g to a<br />

ma<strong>in</strong> axis <strong>and</strong> <strong>the</strong> cores have at <strong>the</strong> reduction sequence end a pièce esquillée morphology.<br />

This type <strong>of</strong> production is realized on small blocks or on thick flakes produced<br />

dur<strong>in</strong>g <strong>the</strong> manufacture <strong>of</strong> <strong>the</strong> “large” th<strong>in</strong> flakes by <strong>the</strong> discoid method.<br />

The small flakes have been produced on thick flakes or on exhausted discoid<br />

cores. Those flakes <strong>and</strong> cores were first split by means <strong>of</strong> bipolar percussion. Subsequently,<br />

<strong>the</strong> production <strong>of</strong> <strong>the</strong> small flakes is realized by means <strong>of</strong> <strong>the</strong> bipolar<br />

technique to use <strong>the</strong> thickness <strong>of</strong> <strong>the</strong> half thick flakes (or <strong>the</strong> half discoid cores) as<br />

flak<strong>in</strong>g surface.<br />

Comparison<br />

Now it is possible to realize po<strong>in</strong>t by po<strong>in</strong>t a comparison between <strong>the</strong> early Cedrosan<br />

Saladoid <strong>and</strong> <strong>the</strong> Huecan Saladoid débitage technologies (Figures 7.3, 7.4).<br />

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