The
excavations were scheduled for the time of lowest water levels,
mid-March to mid-April. On a cold and windy March 15, Ktunaxa
elder Phyllis Nicholas said a prayer to the creator to bless
the excavations (Figure 4).
A
series of seven 1 x 1 meter test units were judgmentally located
along the bank of the Columbia River to sample several different
parts of the site. Most
of these were located on the highest part of the terrace defined
by a small creek (Figure 5, Figure
6). A datum
was established on the highest point of this terrace and a
contour map was prepared.
Four initially tests units were excavated labeled XU
1, 2, 3, and 7. Based
on the results of these, a larger block of units was excavated
adjacent to XU2 (Figure 7) and a row of three units was excavated
near XU7. Additional
1 x 1 metre units were excavated further away of the bank
to assess the extent and density of the cultural materials.
All
of the excavations were dug in 5 cm arbitrary levels.
This was felt to provide the best control on the materials
and soil deposition.
During March, frost was encountered immediately below
the sod layer. Once
the soils had been exposed to the sun for a short time they
tended to thaw but were often water saturated.
Most of the excavation was carried out with short handled
spades and trowels.
All of the excavated soils were then screened through
a 5 mm mesh screen with water pumped from the Columbia River
(Figure 9). A
settling pond was constructed of hay bales to trap the silt
to prevent river siltation and to trap the soil for backfilling.
Our excavation system was monitored by the B.C. Ministry
of Environment personnel to ensure that siltation did not
have adverse environmental impacts.
All
cultural materials were bagged in zip-lock plastic bags with
the provenience data written on the bag with indelible felt
pens. The same
information was recorded on a 3 x 5 inch card and included
in the bag. Each
excavator was assigned a notebook for keeping notes on their
unit while they were excavating.
Soil profiles and photographs were prepared for selected
units. All units
were excavated until basal river gravel was encountered (usually
about 70 cm) or until the water table was reached (commonly
at 75 cm). Where
units reached the water table before encountering river gravels,
an attempt was made to continue excavating until this became
impossible.
Fire
broken rock was common on the site.
In layers where large concentrations were encountered,
it was weighed with a spring scale on site and discarded.
In layers where small quantities were located it was
bagged and taken to the laboratory where it was weighed with
a balance scale prior to discarding.
Because
of the water saturated nature of the soils, organic materials
such as bone and wood were commonly packed in a plastic bag
or other container, usually with the surrounding soil so that
the general humidity levels were not drastically altered. These were then stored in a refrigerator.
Because of the potential for highly perishable items
(e.g. basketry, netting ) in such a wet environment, the crew
had also be briefed on the recovery and storage of such items
by a professional conservator, however no such items were
located. All of the wood pieces were carefully examined for evidence
of human use but none was identified.
Some of the wood appeared to have been beaver gnawed.
Although
a systematic surface collection was originally proposed for
the site, the difficulties of extending the site grid into
highly water saturated areas made it unfeasible.
As the riverbank began to become slightly drier, or
when it froze overnight sufficiently to support a person a
few selected items were collected from the surface. This included a small number of
bone or antler tools and some finished stone tools,
which were used to augment our excavated sample of materials
from the site.
Several
meetings were held with the Columbia Lakes and Shuswap Elders
to show them significant recovered items and to discuss interpretations.
The
materials were then taken to Parks Canada's archaeology laboratory
in Calgary where the items were cleaned and catalogued.
Significant items were then photographed and described.
Three carbon samples were selected for radiocarbon
dating. All identifiable faunal materials were sent to Susan Crockford,
Pacific Identifications Inc. for species identification.