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

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Ucareo, Pachuca, and Zaragoza. <strong>The</strong> analysis revealed lower percentages <strong>of</strong> Ixtepeque,<br />

Zaragoza, and possible San Martín Jilotepeque than previously thought (Table 4.3). Two<br />

other sources, Pachuca and Ucareo, were discovered in the remainder <strong>of</strong> the excav<strong>at</strong>ions.<br />

<strong>The</strong>se sources were identified using compar<strong>at</strong>ive samples from other Mesoamerican sites.<br />

El Chayal obsidian fe<strong>at</strong>ured the gre<strong>at</strong>est variety <strong>of</strong> visual characteristics differing<br />

in both texture and color. <strong>The</strong> most common variety is smoky grey, translucent obsidian<br />

with grey or black bands, but it also can appear with red banding, as opaque gray, as<br />

nearly transparent, or with a combin<strong>at</strong>ion <strong>of</strong> these characteristics. A small quantity can<br />

fe<strong>at</strong>ure small black specks or inclusions, which makes it difficult to differenti<strong>at</strong>e from<br />

San Martín Jilotepeque. However, San Martín Jilotepeque <strong>of</strong>ten has a bluish-black hue<br />

th<strong>at</strong> is rarely found <strong>at</strong> El Chayal. Ixtepeque obsidian can resemble the transparent variety<br />

<strong>of</strong> El Chayal, but it has a brownish, “bottle glass” color th<strong>at</strong> does not occur <strong>at</strong> other<br />

sources. Ixtepeque obsidian also is extremely fine and has a glass-like quality. <strong>The</strong><br />

Mexican obsidians found <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong> all have very distinctive visual characteristics<br />

th<strong>at</strong> make them rel<strong>at</strong>ively easy to identify visually. Furthermore, the Mexican blades<br />

fe<strong>at</strong>ure some technological traits th<strong>at</strong> separ<strong>at</strong>e them from the blades made in Gu<strong>at</strong>emala,<br />

such as extremely regular trapezoidal cross sections. Zaragoza obsidian <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong><br />

is always a completely opaque, jet-black color, Pachuca obsidian is green in color, and<br />

Ucareo obsidian is a cloudy blue color with a fine texture.<br />

Tables 4.4 through 4.6 describe the total counts and weights from all excav<strong>at</strong>ions<br />

(general excav<strong>at</strong>ions, caches, and total counts) <strong>at</strong> <strong>Piedras</strong> <strong>Negras</strong> in order to get a general<br />

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