

Vihtr'iitshik
A Stone
Quarry Reported by Alexander Mackenzie on the Lower Mackenzie River in
1789
Artifact Analysis
A total of 361 artifacts was surface collected
during the brief two hour visit at MiTi-1. This relative abundance
compares well with preliminary figures of more than 600 lithic specimens
found in 1973 (Millar and Fedirchuk, 1975:239).
Lithic debitage accounts for the overwhelming
majority of the artifact total (297 specimens). Most of the debitage
consists of quite large flakes, many of which are primary flakes removed
during the reduction of blocky, angular cores. Flakes produced during
the manufacture and thinning of large bifaces were also recovered.
Twenty-seven pieces of debitage have been
identified as linear flakes. One particularly long, narrow and
parallel-sided example was steeply retouched along its distal margin (item "j")
and six others bear some kind of retouch or use wear. The
majority of the remaining linear specimens consists of long flakes
detached from the corners of blocky or angular cores.
Two artifact categories stand out from the
remaining 64 specimens; cores and bifaces. The latter consist of large
tabular bifaces and biface fragments (N=14) exhibiting only marginal
flaking, and smaller, more refined bifaces (N=6) whose entire
surfaces have been flaked. Both types likely represent
different stages of a technological continuum. In all instances but
one, the quality of the flaking suggests only preliminary shaping or
thinning, in view of producing blanks destined for further reduction and
refinement.
Tost of the cores and core fragments (N=30) can
be grouped into two types. The first group of cores (N=12) consist of
wide, relatively thin tabular pieces
whose flat surfaces were the main
flaking faces. The flaking planes are thus parallel to the
natural layering within the raw material. The second group of cores
(N=16) is comprised of thick, but narrow and long
tabular pieces whose
principal flaking face is perpendicular to the bedding planes of the
rock. Essentially these cores could only produce long,
parallel-sided flakes.
Mwo cores stand out from the rest in that they
are large pieces of raw material which have had flakes removed from a
number of faces. Flakes removed from the principal flaking faces tended
to be directed down the length of the cores and suggest the intentional
production of linear flakes if not blades/microblades.