Q02-2u3 Descriptive Characteristics by Level

The stratigraphy at the Maymeja workshop contains layers at two distinct angles that suggest that mounding occurred initially downslope of where the mound is located today. The Q02-2u3 test unit measured only 1x1m and provided little spatial evidence for architectural interpretation, but the yellow surface labeled as S3 is suggestive of some kind of prepared surface associated with obsidian production at the workshop. Radiocarbon samples recovered from levels 4, 6, and 7 indicate that the sequence in this test unit spans the middle of the Terminal Archaic through to the Early/Middle Formative and probably well into the Middle Formative. A soil sample examined by UC Santa Barbara volcanologists from level 6 contained grains of biotite and hornblende but these grains may have derived from the older bedrock (Sarah Fowler, pers. comm., 27 Feb 2006). The sampling strategy during excavation at the obsidian source involved collecting 25% of flakes being excavated per level by retaining flakes from a single quad, while carbon samples, cores and retouched artifacts (most of which were presumably observed by the excavator) were collected from throughout the 1x1m unit. Thus, flake counts and weights are proportionally ¼ of the amount of other artifact types collected from the Q02-2u3 excavation.

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Figure 7-12. Q02-2u3 workshop test unit west and north profile diagrams showing strata.

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Figure 7-13. Q02-2u3 west profile at Maymeja workshop site [A03-126].

Lvl

HBD*

Contents

Soil

Photos #s

1

51

S1 Strata. 1 projectile point.

Dark brown 7.5YR3/2, Silty loam, Med grain, poorly sorted, .7/.7

243

2

62

S2

Dark greyish brown 2.5YR4/2, Sand, Coarse grain, poorly sorted, .9/.5

244-245

3

72

S2

F1; Dark brown 7.5YR4/2, Silty sand, Medium grain, poorly sorted, .9/.5

246-249

4

81

S2.14C: 3149±53bp

Dark brown 10YR3/3, Silty loam Fine grain, well sorted, .3/.7

N950:250-251

N4100: 2329-2330

5

93

S2,S3. Midden with yellow stains. Floor surface?

Dark yellowish brown 10YR3/4, Silty clay, Fine grained, well sorted, .3/.7

252-253

6

101

S3, S4: midden, F4&F5: depression on west edge, poss postmolds. Charcoal.

S314C: 4063±39bp

Dark yellowish brown 10YR3/4, Silty loam Fine grain, well sorted, .3/.7. Grains of biotite and hornblende encountered in soil sample.

254-256

7

108

Charcoal, Moist soils. Fewer lithics.

S414C: 4160±43bp

Dark greyish brown 10YR4/2, Silty loam, Fine grain, poorly sorted, .5/.7, F2: Dark yellowish brown, Silty loam, 10YR3/4, Fine grain, poorly sorted, .5/.7

258-259

8

122

Very moist, poss. altitude of bofedal.. Near sterile.

Brown 7.5YR4/3, silty sand, Med grain, poorly sorted, .7/.3

258-259

* HBD = mean height below datum in centimeters for the top of each level based on five depth measures per level.

Table 7-13. Q02-2u3 Excavation levels from test unit at the A03-126 workshop.

As with other units in Maymeja, TU3 consisted of almost exclusively obsidian artifacts in a matrix of tephra-rich soils. As would be expected at a workshop site, there was a great deal of redundancy both in material types and technical classes. Hammerstones were not found in abundance in the excavation, but cores made a large contribution to the assemblages in most levels. This is considerably more than are encountered in consumption sites. For example, in all 13 levels in the test unit A02-26u1 (Taukamayo) only 15 cores were found.

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Figure 7-14. Proportions of Tech Classes in excavation levels by count in Q02-2u3.

Lvl

Biface

Core

Flake

Flake Retouched

Total

No.

Wt.(g)

No.

Wt.(g)

No.

Wt.(g)

No.

Wt.(g)

No.

Wt.(g)

1

No. and Wt.

3

31

59

1484.1

151

765.2

6

73.7

219

2354

Std. Resid.

-1.2

1.1

-.4

.2

2

No. and Wt.

7

52.4

49

1218

151

699.4

4

29

211

1998.8

Std. Resid.

.5

0

0

-.6

3

No. and Wt.

13

100.5

70

2703.4

279

602.1

2*

60.2

364

3466.2

Std. Resid.

1.0

-1.6

1.2

-2.4

4

No. and Wt.

9

60.1

94*

2915.4

205

998

11

209.9

319

4183.4

Std. Resid.

.1

2.3

-1.5

1.0

5

No. and Wt.

6

60.9

54

1500.8

187

558.7

7

71.2

254

2191.6

Std. Resid.

-.3

-.7

.4

.2

6

No. and Wt.

2

15.5

8

306.3

55

406.4

7**

33.3

72

761.5

Std. Resid.

0

-2.1

.5

3.9

7

No. and Wt.

1

18

582.3

50

618.7

1

9.7

70

1210.7

Std. Resi.

-.7

.4

0

-.6

Total

No. and Wt.

41

320.4

352

10710.3

1078

4648.5

38

487

1509

16166.2

Table 7-14. Q02-2u3:c2showing Technical Class by Level with the Standard Residual.

The variety of technical classes by level is shown above, with very significant counts of retouched flakes in level 6, and significantly low counts of retouched flakes in level 3. There are also a significantly high number of cores discarded in level 4. The weight of these assemblages is also important because, for example, while the count is high in level 3 the weight is relatively low as the assemblage consists of many small flakes. The thickness of each layer (HBD in Table 7-13) can be compared with weight.

Nominal Attributes of obsidian raw material in the quarry test unit: Color, Cortex Type, Heterogeneities

An examination of obsidian by color per excavation level, and color by rotations as a measure of investment but discard, reveals that grey and black obsidian artifacts had the greatest number of rotations while clear and clear-banded obsidian, while making up over 50% of the obsidian present, was seldom rotated more than twice. A number of researchers have observed that Chivay obsidian is unusually transparent. Yet, this evidence indicates that grey and black obsidian was predominant in certain levels at the workshop and these artifacts were rotated more extensively.

Q02-2u3 Obsidian Characteristics by Level

Level

Prevalent

Rare

Comments

1

Color:Grey; Cortex:Irregular, Tabular

Color:Black; Cortex:Tabular Rounded

2

Color:Brown Banded, Grey Banded

Color:Black

3

Color:Clear

Color:Grey, Grey Banded. Cortex:Tabular

4

Color:Black, Grey, Grey Banded Cortex:Tabular

Color:Clear

5

Color:Black, Clear; Cortex:Tabular Rounded

Color:Grey, Grey Banded

6

Color:Clear Banded

Cortex:Tabular Rounded

7

Color:Clear; Cortex:Tabular Rounded

Ob2 (9%)

Table 7-15. Attributes of obsidian artifacts from Q02-2u3.

In the course of the analysis, Alex Mackay noted the presence of Kombewa flakes (Schick and Clark 2003;Tixier, et al. 1980), also as known as "Janus flakes", in analysis. This a flake-as-core technique where

(1) A relatively large flake, Flake A, is struck from a core.

(2) Flake A then becomes Core A when a flake is struck from the ventral surface of Flake A removing the bulb of percussion from step 1 as a thinning technique and producing Flake B.

(3) Flake A is a Kombewa core, and the Flake B that results from step 2 is a Kombewa flake that has bulbs of percussion on both sides.

Level

Kombewa Flakes

% Flakes

Total Flakes

1

0

149

2

0

151

3

4

1.45

276

4

1

0.49

204

5

6

3.21

187

6

0

53

7

0

43

Total

11

1.03

1063

Table 7-16. Proportion of Kombewa flakes by level in Q02-2u3.

The Kombewa core is a flake that is thinned by this process, and the Kombewa flake that is produced is small and triangular. Mackay observed that a number of series 5 projectile points had vestiges of a bulb of percussion on one of the proximal tangs on one side, and a bulb of percussion in the middle of the piece on the other side, which suggests that it was produced on a Kombewa flake. The only other location where Kombewa flakes were encountered in significant quantities was on the surface of the site of Collpa [A03-910] in Block 5 midway between the Chivay source and Callalli. Seven Kombewa flakes (6 of obsidian, one of chert) were encountered on the surface at Collpa. A number of series 5 points were also encountered at Collpa.