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The Organization of Chipped-Stone Economies at Piedras Negras ...

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5.6.5: Blades, Core Reduction Debitage, and Cores<br />

<strong>The</strong>re is sparse evidence th<strong>at</strong> microcrystalline-quartz polyhedral cores were<br />

reduced <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong>. A small sample <strong>of</strong> possible exhausted-cores (N=3) appears to<br />

have been polished and transformed into awls or chisels. Figure 5.13 depicts one <strong>of</strong> these<br />

possible cores, which is marked as such by the multifaceted pl<strong>at</strong>form and remnant blade<br />

scars on the face <strong>of</strong> the piece. Rejuven<strong>at</strong>ion flakes and percussion blades also are found <strong>at</strong><br />

<strong>Piedras</strong> <strong>Negras</strong> (Figure 5.14). It is unclear by wh<strong>at</strong> means the blades were produced<br />

because the sample is too small. Microcrystalline-quartz blades, however, do appear in<br />

burial contexts indic<strong>at</strong>ing th<strong>at</strong> they were <strong>of</strong> some value to the local popul<strong>at</strong>ion. Percussion<br />

blades and polyhedral cores from a cave site near El Cayo (Lee and Hayden 1989)<br />

indic<strong>at</strong>e th<strong>at</strong> microcrystalline-quartz blade technology was a regional phenomenon.<br />

5.6.6: Ad Hoc Cores and Flakes<br />

<strong>The</strong> most common ad hoc flake-core technology <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong> was the<br />

multidirectional flake-core, but there also is evidence <strong>of</strong> unidirectional flake-core<br />

reduction. Multidirectional flake-cores usually were made from nodule fragments, and<br />

thick, short nodule-reduction flakes th<strong>at</strong> were unusable for the production <strong>of</strong> bifaces. <strong>The</strong><br />

cores are <strong>of</strong>ten spherical or discoid in shape, and <strong>of</strong>ten are made from rough-texture<br />

microcrystalline quartzes. <strong>The</strong> flakes are short and thick. <strong>The</strong> dorsal scarring p<strong>at</strong>tern can<br />

resemble those <strong>of</strong> biface-reduction flakes, but the pl<strong>at</strong>form is larger, poorly prepared, and<br />

<strong>of</strong>ten angular. Based on hammerstone morphology <strong>at</strong> the site, multidirectional flake-cores<br />

were a common “blank” for hammerstones, which were further rounded through use.<br />

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