The Cache Site NhTp-1 (artifact descriptions)
This is the "type site" of Inuvialuit sites in the Tuktoyaktuk Peninsula interior. It is located at the outlet of a headwater lake, approximately 27 km south of Tuktoyaktuk. This lake is known to be an important overwintering lake for various types of whitefish. The site was disturbed by heavy machinery in 1983 when a power transmission line was buried. The same year Gerald Lacho, of the Department of Fisheries and Oceans, recovered a whaling harpoon foreshaft from the site, and forwarded it to the Prince of Wales Northern Hertiage Centre. The site was subsequently visited by two researchers (Arnold 1985; LeBlanc 1987), but no testing was carried out. LeBlanc reported at least 10 cache pits along the creek and noted a possible house feature. In 1991 Swayze mapped and tested the site, noting at least 18 caches and verified the presence of a house feature, and a relatively extensive midden.
During the summer of 1992, 16 m2 were opened in the midden
and eight m Faunal remains were numerous, and, by and large, well
preserved. Based on the analysis of faunal remains from the 1991
test pits (Still 1992) and casual identification in the field
(Still pers. comm. 1992) it is apparent that fish and fowl were
the principal animals processed at the Cache site. Nevertheless,
a preliminary assessment indicates that large mammal (eg.
caribou) remains are, relatively speaking, more apparent here
than at the Sukunnuk and Cliff sites. Small mammals, such as
muskrat and hare are also present in significant numbers. Of the
fish bones recovered, the most numerous elements are those of
various types of whitefish; but burbot, lake trout, and, more
rarely, pike are represented. Waterfowl, including various duck
and goose species, loon and swan are the most numerous of the
bird bones; but, ptarmigan, too, are well represented.
As at the Sukunnuk site, the excavations also recovered a
small amount of diagnostic Palaeoeskimo (ASTt) material. This
consisted of two burins (one on a projectile point, the other on
a linear flake), and a small obsidian microblade. Unfortunately,
it was not possible to identify a discrete ASTt strata or
feature. Instead, the objects were scattered at different levels
within a matrix largely created by Inuvialuit activities.
Presumably, a portion of the lithic debitage recovered (and
perhaps the small stemmed projectile points) are also of ASTt
origin, but they are not diagnostic.
The "house", or dwelling, is located on the slope on the
south side of the site close to the edge of the water. This
location would maximize insolation in the colder months, and
would provide some protection from the wind. Before excavation it
appeared as a roughly circular depression partially obscured by
heavy willow growth and leaf litter (Figure 9). On average it was
about 30 cm deep, and there was no indication of any
superstructure, or entrance passage. After excavation it became
apparent that the feature is not a semi-subterranean "house", but
a level platform excavated into the side of a hill. Excavation
did not reveal an entrance passage per se but there was a slight
trough on the south side, towards the lake, as if worn down by
the comings and goings of the occupants.
During excavation several small hearths were noted at
various depths, some so close to the edge of the feature that it
can be assumed they were not active when the structure stood.
Thus, after the dwelling collapsed, or the platform was no longer
used as a house foundation, people continued to use the space,
probably on a more temporary, open-air, basis. Between
approximately 30 to 40 cm below the surface of the depression
portions of the original living surface or floor were
encountered. The principal component of this "floor" was a
substantial, intact, stone-ringed hearth, surrounded by a
profusion of artifacts and animal bones (Figure 10). In other
areas of the depression the original activity surface was
distorted by frost heaves and solifluction lobes of heavy,
sticky, silt. The remnants of three spruce pole posts were found,
which were probably used to support the roof. The structure was
probably a domed hut, roofed with bent willow stems and covered
with hide, or a willow-wattle hut chinked with moss. In either
case, snow too was probably heaped on top to provide more
insulation. The dwelling certainly was not a "sod house" like
those excavated on the coast, with their massive driftwood beams,
split-pole floors, and log and sod-insulated walls.
Excavation in the house feature produced a good collection
of artifacts and faunal remains. Future analysis of the latter
will probably produce a picture similar to that of the midden,
although preliminary observation suggests that there may be
proportionately more fish in the house. As might be expected a
good number of artifacts found in the house relate to fishing:
net sinkers, netting needles, fish hook shanks and barbs, and
fish spear prongs. Other artifacts included considerable pottery,
lithic debitage, bag handles, an adze head and a mattock head, a
bird bone drinking tube, ground slate ulus and blade fragments,
three chipped stone projectile points, an ice-pick tip, an ivory
bead, and a fragment of a quartz crystal. Pieces of cut antler
and fragments of unidentified antler tools were also common.