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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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Figure 6.8. The Primary Deposit Zone is identified by <strong>the</strong> black dashed l<strong>in</strong>e. The 50 m<br />

buffer is marked by a black dotted l<strong>in</strong>e. L<strong>in</strong>ear <strong>An</strong>omaly 1 and <strong>the</strong> causeway feature<br />

are present with<strong>in</strong> <strong>the</strong> red outl<strong>in</strong>e.<br />

and surface visibility were essentially <strong>the</strong> same throughout all <strong>of</strong> Fields 2, 3, and 4;<br />

<strong>the</strong>refore, <strong>the</strong> spatial constriction <strong>of</strong> artifact deposition cannot be attributed to a bias due<br />

to variations <strong>in</strong> visibility. The consistency and uniformity <strong>of</strong> deposition is a major feature<br />

derived from <strong>the</strong> analysis. The PDZ spans three separate fields, each under differ<strong>in</strong>g use<br />

patterns and methods <strong>of</strong> cultivation and cattle graz<strong>in</strong>g, which fur<strong>the</strong>r suggest <strong>the</strong> limited<br />

concentration <strong>of</strong> artifacts was a result <strong>of</strong> ancient activity and deposition as opposed to<br />

contemporary impacts to <strong>the</strong> surface.<br />

There are a number <strong>of</strong> factors that warrant fur<strong>the</strong>r consideration <strong>of</strong> <strong>the</strong> PDZ. First<br />

is <strong>the</strong> density <strong>of</strong> material, 124 sherds per 50 m x 50 unit with<strong>in</strong> <strong>the</strong> PDZ compared to 21<br />

sherds <strong>in</strong> <strong>the</strong> rema<strong>in</strong>der <strong>of</strong> <strong>the</strong> surveyed area units. Second, with<strong>in</strong> a 50 m-wide perimeter<br />

zone (55,000 m²) that encircles <strong>the</strong> 300 m x 150 m PDZ (45,000 m²) only 28 ceramic<br />

pieces were recovered (see Figure 6.8). The rate and suddenness <strong>of</strong> <strong>the</strong> depositional drop-<br />

284

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