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An Unexplored Realm in the Heartland of the Southern Gulf ... - Famsi

An Unexplored Realm in the Heartland of the Southern Gulf ... - Famsi

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The survey was conducted along <strong>the</strong> base <strong>of</strong> <strong>the</strong> bank, which was divided <strong>in</strong>to<br />

approximate 50 m long segments. Fields 1 through 8, our area <strong>of</strong> <strong>in</strong>terest, were identified<br />

as segments 2 through 55 (see Hernández 2003). With<strong>in</strong> <strong>the</strong>se segments, significant<br />

quantities <strong>of</strong> ceramic material, representative <strong>of</strong> all temporal periods and transitional<br />

phases, were recovered. A rough estimate shows Formative period materials accounted<br />

for 32 percent <strong>of</strong> <strong>the</strong> entire river cut bank assemblage; Protoclassic and Early Classic<br />

transitional objects amounted to 5 percent and Late Classic ceramics 7 percent. Non-<br />

chronologically diagnostic pieces that are considered domestic wares accounted for 31<br />

percent, and <strong>the</strong> rema<strong>in</strong><strong>in</strong>g 25 percent consisted <strong>of</strong> o<strong>the</strong>r types <strong>of</strong> non-temporally<br />

diagnostic pieces. On a strictly quantitative basis, <strong>the</strong>se percentages suggest that <strong>the</strong><br />

occupational presence <strong>in</strong> <strong>the</strong>se portions <strong>of</strong> Fields 1 through 8 was most significant dur<strong>in</strong>g<br />

<strong>the</strong> Formative period, an assumption that is consistent with <strong>in</strong>ferences drawn from <strong>the</strong><br />

surface ceramic analysis.<br />

From November, 2003 to December, 2005, four additional surveys and<br />

collections were conducted along <strong>the</strong> river cut bank. These <strong>in</strong>spections were performed <strong>in</strong><br />

response to <strong>the</strong> cont<strong>in</strong>ued collapse <strong>of</strong> weakened portions <strong>of</strong> <strong>the</strong> embankment that exposed<br />

or displaced <strong>in</strong> situ artifacts. Also, follow<strong>in</strong>g normal ra<strong>in</strong>fall events, run-<strong>of</strong>f from <strong>the</strong><br />

surface washed away small amounts <strong>of</strong> soil along <strong>the</strong> upper portions <strong>of</strong> <strong>the</strong> bank. The<br />

cumulative effect <strong>of</strong> <strong>the</strong>se erosional activities was <strong>the</strong> exposure or dislodg<strong>in</strong>g <strong>of</strong><br />

additional <strong>in</strong> situ artifacts and <strong>the</strong>ir deposition fur<strong>the</strong>r down <strong>the</strong> slope.<br />

The artifacts collected dur<strong>in</strong>g <strong>the</strong>se surveys had not been subject to movement by<br />

river action; <strong>the</strong>y had simply fallen from <strong>the</strong>ir place <strong>of</strong> orig<strong>in</strong>. In respect to <strong>the</strong>se fallen<br />

pieces, I conducted a series <strong>of</strong> drop tests over various slopes and descent distances to<br />

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