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

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Level I throughout <strong>the</strong> site is consistent. This uppermost layer is made up <strong>of</strong> semi-<br />

compacted dark grey humus (Munsell 7.5YR3/2) that, for <strong>the</strong> most part, conta<strong>in</strong>s little<br />

cultural material. Mechanized till<strong>in</strong>g over <strong>the</strong> past three decades has effected whatever<br />

artifacts were present <strong>in</strong> this upper level and all are small, broken, or highly eroded. The<br />

colors used <strong>in</strong> <strong>the</strong> computer generated pr<strong>of</strong>iles do not portray <strong>the</strong> true color <strong>of</strong> <strong>the</strong> soils,<br />

and were employed to more clearly differentiate changes <strong>in</strong> <strong>the</strong> stratigraphy.<br />

River Cut Pr<strong>of</strong>ile 1A<br />

This segment is located on <strong>the</strong> sou<strong>the</strong>ast perimeter <strong>of</strong> Field 1 and is representative<br />

<strong>of</strong> several locations along <strong>the</strong> river cut bank <strong>in</strong> Fields 1 through 7. Level I is a natural<br />

layer <strong>of</strong> s<strong>of</strong>t to semi-compacted humus (Munsell 7.5YR3/1) (Figure 5.8). The few<br />

ceramics present <strong>in</strong> this level are small and diagnostically unrecognizable due to damage<br />

caused by repeated agricultural cultivation, cattle graz<strong>in</strong>g, and natural erosional effects.<br />

This situation is true <strong>of</strong> Level I <strong>in</strong> all pr<strong>of</strong>iles. There is evidence <strong>of</strong> <strong>in</strong>sect and rodent<br />

activities and effects <strong>of</strong> plant and tree roots. Gravel fill is present, but well dispersed from<br />

repeated manipulation <strong>of</strong> <strong>the</strong> surface.<br />

The presence <strong>of</strong> gravel anywhere on <strong>the</strong> site with<strong>in</strong> <strong>the</strong> top 2 m is significant.<br />

River gravel (~0.5 to 5 cm <strong>in</strong> size) is ubiquitous, but natural sedimentary deposits only<br />

appear at levels that are more than 3.5 m below <strong>the</strong> present surface. <strong>An</strong>y occurrence <strong>of</strong><br />

this gravel near <strong>the</strong> surface is a result <strong>of</strong> <strong>in</strong>tentional human activity that is generally<br />

associated with <strong>the</strong> construction <strong>of</strong> architectural features.<br />

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