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

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

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Table 4.1 depicts the percentages by artifact count and weight <strong>of</strong> all the microcrystalline-<br />

quartz m<strong>at</strong>erials <strong>at</strong> the site. <strong>The</strong> quantities described in the table are not exact, largely<br />

because <strong>of</strong> the tendency <strong>of</strong> <strong>Piedras</strong> <strong>Negras</strong> artifacts to acquire white p<strong>at</strong>ina, which<br />

obscures the true color <strong>of</strong> the stone. <strong>The</strong> c<strong>at</strong>egories th<strong>at</strong> fe<strong>at</strong>ure a question mark contain<br />

those m<strong>at</strong>erials th<strong>at</strong> were difficult to identify visually. I describe the available inform<strong>at</strong>ion<br />

based on my visual analysis. Of the total 4,557 microcrystalline-quartz artifacts, which<br />

weigh 141,406 g, 347 were from cache deposits (12,276 g, 8.68% by total weight). All <strong>of</strong><br />

these artifacts were made <strong>of</strong> either chert or chalcedony, but the chert artifacts were much<br />

more common <strong>at</strong> 93.37% by count. While the m<strong>at</strong>erials used to produce cache goods<br />

were <strong>of</strong> rel<strong>at</strong>ively high quality, they were never made from very fine imported flint<br />

m<strong>at</strong>erials. Most <strong>of</strong> the eccentrics were made from wh<strong>at</strong> appear to be local m<strong>at</strong>erials.<br />

<strong>The</strong> remaining 4,210 microcrystalline-quartz artifacts, which weigh 129,131 g,<br />

were found outside <strong>of</strong> cache contexts. <strong>The</strong> majority <strong>of</strong> the artifacts were chert according<br />

to both weight and count (62.95% and 49.75%, respectively). As the percentages<br />

indic<strong>at</strong>e, however, artifacts made <strong>of</strong> chalcedony and dolomite were both larger and denser<br />

than their chert counterparts. Chalcedony and dolomite are by n<strong>at</strong>ure tougher stones, and<br />

were <strong>of</strong>ten reserved for thicker, more durable tool forms. Chalcedony and dolomite were<br />

the second and third most common m<strong>at</strong>erials <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong>, while flint, quartzite, and<br />

silicified limestone were considerably less so. Petrified wood, probably collected from<br />

the local streambed was the least common m<strong>at</strong>erial used for chipped-stone production.<br />

106

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