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

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Never<strong>the</strong>less, <strong>the</strong> structural design and specific features present with<strong>in</strong> <strong>the</strong> complex may<br />

<strong>of</strong>fer clues as to its orig<strong>in</strong> and purpose. To assess <strong>the</strong>se clues it is necessary to observe <strong>the</strong><br />

archaeological features and landscape signatures with<strong>in</strong> <strong>the</strong> context <strong>of</strong> El Marquesillo and<br />

<strong>the</strong> sett<strong>in</strong>g <strong>of</strong> <strong>the</strong> Formative period Sou<strong>the</strong>rn <strong>Gulf</strong> Lowlands.<br />

Water Features<br />

There are two natural water features associated with <strong>the</strong> Olmec Throne Complex.<br />

One is an apparent spr<strong>in</strong>g located immediately outside <strong>the</strong> west perimeter <strong>of</strong> <strong>the</strong> complex<br />

(Figure 6.4). This feature is notable because it is bisected by <strong>the</strong> longitud<strong>in</strong>al medial axis<br />

l<strong>in</strong>e that divides <strong>the</strong> basal platform and its surface structures. The second water feature is<br />

an almost perfectly spherical pool <strong>of</strong> stand<strong>in</strong>g water that is located <strong>in</strong> <strong>the</strong> northwest<br />

corner <strong>of</strong> <strong>the</strong> basal platform. Present day <strong>in</strong>habitants who have lived here s<strong>in</strong>ce <strong>the</strong> 1940s<br />

say <strong>the</strong> pool, which <strong>the</strong>y refer to as <strong>the</strong> poza, has never been dry. Based on <strong>the</strong>se<br />

observations and <strong>the</strong> consistency <strong>in</strong> <strong>the</strong> level <strong>of</strong> <strong>the</strong> water noted <strong>in</strong> three-years <strong>of</strong> field<br />

observations, this feature also may be <strong>the</strong> product <strong>of</strong> a natural spr<strong>in</strong>g. The depth and<br />

position <strong>of</strong> <strong>the</strong> water table <strong>in</strong> <strong>the</strong> Sou<strong>the</strong>rn <strong>Gulf</strong> Lowlands were irregular, and Cyphers<br />

argues that elevated po<strong>in</strong>ts <strong>in</strong> <strong>the</strong> table made <strong>the</strong>m a “circumscribed resource” (Cyphers<br />

1993:165).<br />

There appears to be ano<strong>the</strong>r water feature present atop <strong>the</strong> platform that is not<br />

natural, but was produced through human plann<strong>in</strong>g and labor. Figure 6.4 is an elevational<br />

contour map <strong>of</strong> Field 8 produced from <strong>the</strong> total station survey data, and <strong>the</strong> natural seep<br />

spr<strong>in</strong>g and stand<strong>in</strong>g water feature are identified. In Plaza 1, <strong>in</strong> <strong>the</strong> nor<strong>the</strong>ast sector <strong>of</strong> <strong>the</strong><br />

platform, is an area <strong>of</strong> significant depression. This sunken area is clearly noticeable <strong>in</strong> <strong>the</strong><br />

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