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

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microcrystalline quartzes were reserved for small bifaces and prism<strong>at</strong>ic blades, medium-<br />

grade cherts and chalcedonies were used for mid-size bifaces (knives and spear heads),<br />

and coarse-grained cherts and chalcedonies were used for large bifaces, especially<br />

celtiform axes (see Chapters 3 and 4). Large indirect percussion notching flakes <strong>of</strong> fine<br />

and medium grained m<strong>at</strong>erials are used to identify the production <strong>of</strong> microcrystalline-<br />

quartz eccentrics, however few <strong>of</strong> them actually exist. Of course, there are always<br />

exceptions, but the general trend <strong>of</strong> tougher stones for harder kinds <strong>of</strong> tasks tends to hold<br />

<strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong>.<br />

<strong>The</strong> production <strong>of</strong> obsidian goods is identified by only a few technological types<br />

because the morphology <strong>of</strong> imported polyhedral-cores was rel<strong>at</strong>ively homogeneous and<br />

the techniques for preparing them for reduction by pressure varied little (see Chapter 6).<br />

Nevertheless, specific stages <strong>of</strong> reduction can be identified through flake, blade, and core<br />

morphology. <strong>The</strong> initial prepar<strong>at</strong>ion <strong>of</strong> imported cores can be identified largely through<br />

the existence <strong>of</strong> percussion blades and flakes th<strong>at</strong> were removed to regularize the face <strong>of</strong><br />

the core (i.e., removing irregularities cre<strong>at</strong>ed through transport, n<strong>at</strong>ural inclusions, or<br />

original production flaws). Early first- and second-series pressure-blades, and also l<strong>at</strong>e-<br />

stage pressure blades th<strong>at</strong> <strong>of</strong>ten overshot the distal end <strong>of</strong> the core mark the production <strong>of</strong><br />

prism<strong>at</strong>ic blades. Other debitage types consist <strong>of</strong> distal, l<strong>at</strong>eral, and pl<strong>at</strong>form rejuven<strong>at</strong>ion<br />

flakes, crested blades, and exhausted cores. Finally, the production <strong>of</strong> obsidian eccentrics<br />

can be identified primarily by the existence <strong>of</strong> fragments <strong>of</strong> bipolarly reduced, exhausted<br />

pressure-blade cores, irregular percussion flakes, and notching and pressure flakes<br />

unrel<strong>at</strong>ed to blade-core technology. No examples <strong>of</strong> bipolar flakes used as tools were<br />

82

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