22.10.2013 Views

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

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

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

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Formative to Protoclassic ceramics (420.1 and 81.4) were recovered from ceramic<br />

specimen location 1. Level IIA is an area <strong>of</strong> highly mixed sand and silt that is void <strong>of</strong><br />

cultural material and is possibly <strong>in</strong>trusive <strong>in</strong>to Level III. Level III is a highly mixed<br />

composite <strong>of</strong> reddish-yellow, semi-compacted, sandy and silty loam, and conta<strong>in</strong>ed Early<br />

(31.2) and Late (11.4a) Formative ceramics <strong>in</strong> <strong>the</strong> area directly below Level IIA.<br />

Level IV is a mixture <strong>of</strong> reddish colored, semi-compacted sand and ash or ash-like<br />

substance. Offer<strong>in</strong>g III was located <strong>in</strong> this level, and <strong>the</strong> small sand wedge directly above<br />

it is an <strong>in</strong>dication <strong>of</strong> <strong>in</strong>trusion. The angle and degree <strong>of</strong> erosion to <strong>the</strong> river cut bank at<br />

this po<strong>in</strong>t have masked <strong>the</strong> rema<strong>in</strong>der <strong>of</strong> <strong>the</strong> <strong>in</strong>trusive pit above <strong>the</strong> <strong>of</strong>fer<strong>in</strong>g. In <strong>the</strong> pr<strong>of</strong>ile<br />

draw<strong>in</strong>g, <strong>the</strong> thick, red sand l<strong>in</strong>e above <strong>the</strong> <strong>of</strong>fer<strong>in</strong>g appears unbroken when, <strong>in</strong> fact, it is<br />

actually beh<strong>in</strong>d <strong>the</strong> <strong>of</strong>fer<strong>in</strong>g. There is ano<strong>the</strong>r similar red sand lens l<strong>in</strong><strong>in</strong>g <strong>the</strong> bottom <strong>of</strong><br />

<strong>the</strong> level. Ceramic specimen location 3 conta<strong>in</strong>s a mix <strong>of</strong> Early (71.7) and Late (11.4a)<br />

pieces possibly <strong>the</strong> result <strong>of</strong> <strong>the</strong> disturbance caused dur<strong>in</strong>g <strong>the</strong> deposition <strong>of</strong> Offer<strong>in</strong>g III.<br />

The <strong>in</strong>trusion <strong>of</strong> Offer<strong>in</strong>g IV passed completely through Level IV and was placed<br />

midway <strong>in</strong>to Level V. Ceramic specimen 5 is Early Formative (31.2) and appears to have<br />

been relocated dur<strong>in</strong>g <strong>the</strong> <strong>in</strong>trusion <strong>of</strong> <strong>the</strong> <strong>of</strong>fer<strong>in</strong>g. The quantity <strong>of</strong> ash-like material<br />

mixed with sand is much higher here than <strong>in</strong> previous levels. A third l<strong>in</strong>e <strong>of</strong> highly<br />

compacted red sand underlies this level as well. These three l<strong>in</strong>es are wider than <strong>the</strong> ones<br />

observed <strong>in</strong> Level II and may represent floors similar to <strong>the</strong> sand floors documented at<br />

San Lorenzo (Vega 1998). Levels Va and Vb conta<strong>in</strong> less ash and sand, and dispersed<br />

gravel is mixed <strong>in</strong>to this aggregate. This area appears to be a deposit at <strong>the</strong> bottom <strong>of</strong><br />

Level V. On <strong>the</strong> opposite side <strong>of</strong> <strong>the</strong> pr<strong>of</strong>ile, Early Formative Calzadas Carved and<br />

Limon Incised (11.4) were recovered <strong>in</strong> ceramic specimen location 6.<br />

187

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!