¨

NbTj-17

This site, discovered in 1988 (Pilon 1989), is located on the edge of the highest of two low terraces overlooking at once a small lake and the head of this lake's outlet stream, what is essentially the beginning of the east-flowing Wolverine River. The modern vegetation consists of an open spruce-lichen forest with some willow thickets. When revisited in 1990 (Pilon 1991), 11 m2 were excavated.

The stratigraphy within the excavated area was relatively straightforward with an uppermost vegetation layer with its associated root mat and a thin humus layer overlying the terrace deposits of sand and occasional cobbles. Artifacts were clearly associated with the humus layer. Additionally, a small proportion of artifacts was also recovered from the top few centimetres of the sand.

A hearth area situated in the centre of the lithic scatter was uncovered by our excavations. It consists of an oval area (30 cm x 20 cm) of fire-reddened sand which in profile was saucer-shaped. The maximum depth of this reddened sand was found at the centre and reached up to 10 cm thick. A few fire-cracked rocks were found in the vicinity of the oxidized sand and were clearly associated with the combustion feature. No faunal remains were recovered, but charcoal, found deep within the oxidized sand was collected.

Tool frequencies and raw materials, NbTj-17

CHSAVCMM
BUBUBUBU
Burin13*------
Pièce Esquillée2131----
Projectile Point--1-----
Scraper-----1--
Blank/Preform2-----1-
Retouched/Used Flake-11-----
Retouched Burin Spall-4-1----
Other--------
Total5952-11-

CH=chert SA=siliceous argillite VC=vesicular clinker MM=metamorphic
B=biface U=uniface
* one of these is a burin blank


Artifacts

The artifact collection recovered from NbTj-17 is surprizingly varied both in terms of raw materials and the array of lithic implements.

Only one probable projectile point was found. Manufactured of siliceous argillite, this bipointed specimen lacks the fine flaking evident on projectile points from other ASTt sites in the area. This characteristic appears to stem from the lithic craftsperson's inability to thin a central mass which covers much of one face.

A burin, burin fragments (2) and a burin blank, along with burin spalls (13) attest to the importance of this functional class at NbTj-17. Refits were possible in a number of instances, and show that not only were lithic implements being manufactured and rejunivated around this small hearth area, but these tools were also being used in the immediate vicinity. In one case, three black chert burin spalls--the primary and succeeding two rejuvinations spalls--could be fitted together. Of interest was the fact that two of these were distally retouched. As well, by refitting these implements, it was possible to observe the incremental reduction in the length of the tool between rejunivations. And finally, it was possible to observe the systematic use of the burin scar as a platform for the removal of small flakes from the burin's dorsal surface on 6 of the 13 burin spalls--5 of these were distally retouched--as well as on two of the extant burin bits. These burins and the burin blank all appear to be of the "mitten-shaped" variety.

Microblades were found, albeit in very low numbers.

Although no implements were found which exhibited grinding, grinding as a shaping technique was known to the site occupants. A total of 11 flakes were found made of either some form of fine-grained, possibly sedimentary stone, or of a poor-grade siliceous argillite, which exhibited extensively ground platforms or facets on their dorsal surfaces.

One last artifact warrants mention. It is the mid-section of a large biface made of a coarse- grained metamorphic rock. Extrapolating from this section, the biface must have been on the order of 15 cm in total length and the fragment's width is 6.32 cm. If we also consider the presence of 11 flakes of a similar grade of raw material in the debitage collection, we must conclude that large, coarse-grained implements were part of the lithic inventory of the site's occupants.

Dating

A single wood charcoal sample was submitted for radiocarbon dating. It was obtained from deep within the deposits of the circular hearth feature, at a depth of approximately 10 centimetres below the feature's surface. The result was 3470±430 B.P. (S-3377), which lies well within the range of early ASTt.