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

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El Marquesillo’s geographic location on <strong>the</strong> San Juan River provided strategic<br />

socioeconomic advantages. For people liv<strong>in</strong>g <strong>in</strong> river<strong>in</strong>e environments, such as those <strong>in</strong><br />

<strong>the</strong> Tonala, Coatzacoalcos, Papaloapan, and San Juan River bas<strong>in</strong>s, it has been<br />

established through archaeological and ethnohistoric data that water transport was <strong>the</strong><br />

most effective and efficient mode <strong>of</strong> conveyance (Berdan and <strong>An</strong>awalt 1997:113; Coe<br />

and Diehl 1980b:54-59; Doer<strong>in</strong>g 2002:97; Navarrete 1978; Rust and Sharer 1988;<br />

Scholes and Warren 1965:779). Grove (1968:182) contends that Formative period trade<br />

nodes were located on constricted passes along routes that were positioned to monitor <strong>the</strong><br />

flow <strong>of</strong> goods. A cursory exam<strong>in</strong>ation <strong>of</strong> <strong>the</strong> river network around El Marquesillo<br />

demonstrates that its position was a natural hub or focal po<strong>in</strong>t for multiple routes that<br />

connected a variety <strong>of</strong> localities, both nearby and distant.<br />

Figure 3.9 illustrates that <strong>the</strong> tributaries <strong>of</strong> <strong>the</strong> San Juan create a broad network<br />

l<strong>in</strong>k<strong>in</strong>g numerous regional ecological regions. One <strong>of</strong> <strong>the</strong> two primary tributaries <strong>of</strong> <strong>the</strong><br />

San Juan is <strong>the</strong> Río La Lana whose headwaters beg<strong>in</strong> at Cerro Mirador, Oaxaca (1536 m<br />

asl). La Lana’s pr<strong>in</strong>cipal tributary is <strong>the</strong> Colorado River, which extends to <strong>the</strong> slopes <strong>of</strong><br />

Nudo de Zempoaltépetl, Oaxaca (3412 m asl), both <strong>of</strong> <strong>the</strong>se sources are deep <strong>in</strong> <strong>the</strong> Sierra<br />

de Juarez <strong>in</strong> Oaxaca. The second pr<strong>in</strong>cipal tributary to <strong>the</strong> San Juan is <strong>the</strong> Tr<strong>in</strong>idad River,<br />

which is fed by <strong>the</strong> Chisme and Puxmetacán rivers. These waters dra<strong>in</strong> <strong>the</strong> nor<strong>the</strong>rn slope<br />

<strong>of</strong> Cerro Casa de Piedra (2348 m asl), which is less than 15 km north <strong>of</strong> <strong>the</strong> Tehuantepec<br />

River. The Tehuantepec flows out <strong>of</strong> <strong>the</strong> eastern end <strong>of</strong> <strong>the</strong> Valley <strong>of</strong> Oaxaca and empties<br />

<strong>in</strong>to <strong>the</strong> Pacific Ocean at Sal<strong>in</strong>a Cruz.<br />

To <strong>the</strong> nor<strong>the</strong>ast <strong>of</strong> El Marquesillo, Arroyo Zanja Grande and Arroyo Zanja Prieta<br />

flowed past ei<strong>the</strong>r side <strong>of</strong> Laguna de los Cerros. These paleochannels resulted from<br />

75

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