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

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<strong>An</strong>o<strong>the</strong>r possible basalt deposition event occurred <strong>in</strong> conjunction with Structure<br />

109, approximately 650 m to <strong>the</strong> sou<strong>the</strong>ast <strong>of</strong> 84 (see Figure 6.7). As noted <strong>in</strong> Chapter 4,<br />

Structure 109 is a rectangular, truncated pyramidal platform with rounded corners and a<br />

large, level summit area. The most notable feature <strong>of</strong> <strong>the</strong> structure is a ramp extend<strong>in</strong>g<br />

from <strong>the</strong> top <strong>of</strong> nor<strong>the</strong>ast side <strong>of</strong> <strong>the</strong> platform that gradually descends over a distance <strong>of</strong><br />

nearly 100 m. At <strong>the</strong> end <strong>of</strong> this <strong>in</strong>cl<strong>in</strong>e is a remarkably straight anomaly that extends<br />

approximately 120 m to <strong>the</strong> nor<strong>the</strong>ast. In Figure 6.7 <strong>the</strong> magnetometer data have been<br />

superimposed over a topographic map. This image illustrates that L<strong>in</strong>ear <strong>An</strong>omaly 1<br />

conforms to <strong>the</strong> surface features and that an extension <strong>of</strong> its directional axis <strong>in</strong>tersects<br />

Structure 84 and its massive buried anomaly. Its directional path toward Structure 84 may<br />

suggest some type <strong>of</strong> symbolic connection or relationship between <strong>the</strong>se two structures.<br />

<strong>An</strong>o<strong>the</strong>r major feature was identified through an exam<strong>in</strong>ation <strong>of</strong> <strong>the</strong> surface collection<br />

and is directly associated with <strong>the</strong> causeway. Data revealed a highly circumscribed area<br />

<strong>of</strong> ceramic and lithic deposition that literally straddles <strong>the</strong> axis l<strong>in</strong>e and extends between<br />

Structure 109 and 84 (Figure 6.8). The Primary Deposition Zone (PDZ) is so named due<br />

to <strong>the</strong> fact that 1,490 <strong>of</strong> <strong>the</strong> 4,756 ceramic artifacts recovered dur<strong>in</strong>g <strong>the</strong> entire surface<br />

collection across Fields 1 through 8, were collected with<strong>in</strong> this bounded sector. Although<br />

<strong>the</strong> PDZ represents only 8.3 percent <strong>of</strong> <strong>the</strong> surface area collected, it accounts for 33<br />

percent <strong>of</strong> <strong>the</strong> total ceramic assemblage and 28 percent <strong>of</strong> <strong>the</strong> lithic assemblage recovered<br />

<strong>in</strong> <strong>the</strong> surface collection.<br />

When consider<strong>in</strong>g <strong>the</strong> PDZ, it should be noted that <strong>the</strong> rectangular shape and<br />

straight-l<strong>in</strong>e boundaries are features created by <strong>the</strong> grid-based collection process, not <strong>of</strong><br />

<strong>the</strong> orig<strong>in</strong>al deposition process. As well, dur<strong>in</strong>g <strong>the</strong> collection process, <strong>the</strong> ground cover<br />

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