1991 Field Report
(Part 6)
by
Jean-Luc Pilon
NOGAP Archaeologist
Canadian Museum of Civilization


Field No: 85JLP-44
Borden No: MlTk-4


First discovered in
1985, the complexity of MlTk-4 was increased to in 1986 when a semi-subterranean structure was added to the inventory of cultural remains present at this locality in the southern portion of the western lobe of Vidiitshuu. Similarly, upon returning to the site during the 1991 field season we recovered remains which broaden our understanding of the former use of this site.

A single shovel test pit was excavated into the southern berm of the semi-subterranean structure. Under the berm deposits, 3 fire-cracked rocks were observed in the buried humus horizon. In another test pit placed immediately east of the structure, 1 single fire-cracked rock was found at the base of the modern sod which overlay the terrace matrix.

Approximately 8 metres east of the 1986 excavations, a large white glass bead was recovered from a shovel test pit, thus confirming the historic use of the locale.

Finally, shovel test pits placed on the first bench above the active beach resulted in the discovery of siliceous argillite debitage and fire-cracked rocks.

Lure Lake (lac à l'Aigle)

Field No: 88JLP-6
Borden No: MlTk-16


When first brought to this site by Mr. Willie Simon Modeste of Arctic Red River in
1988 (Pilon 1989:24-26), we documented a semi-subterranean structure with an exterior hearth feature located less than three metres to the east and a collapsed pole structure about the same distance to the west. These features were strung along a relatively narrow bench located between the active beach and the slope to the plateau behind the site.

Upon returning to Lure Lake to conduct a more thorough reconnaissance, we set up our base camp at MlTk-16 and thus were provided with the opportunity to further investigate the site. As a result, we identified additional scatters of fire-cracked lying imbedded in the thin sod east and west of the features located in 1988. Very careful and limited testing of the area within the collapsed pole structure resulted in the discovery of a quartzite flake and fire-cracked rocks.

The condition of the wood poles suggested some antiquity. Those portions which lay above the sod were badly weathered and cracked. Removal of the sod cover revealed that the wood lying under the sod was in an advanced state of decomposition but could nonetheless be followed and the shapes of the poles could be discerned. Consequently, following the discovery of the artifacts within the confines of the apparent structure, it was decided to return to this site over the course of the summer and excavate this feature.

An important motivating factor lay in the possibility that this structure had been occupied in either late prehistoric or very early historic times when the manufacture of stone tools and the use of boiling stones were still elements of the local culture. An additional factor was the relative paucity of pre-twentieth century surface structures from the southwest Anderson Plain.

A quadrant system was laid over the apparent collapsed pole structure with the intersection located in the centre of the poles, as determined from surface indications. The units were then enlarged as appropriate in order to fully encompass any poles found under the sod.

At least three distinct hearth features were encountered. The longest one located in the northern part of the excavation had both lithics and calcined bone (including many identifiable fish elements) associated with it, along with some fire-cracked rock. The large circular hearth located along the centre of the east wall contained numerous fire-cracked rocks and fresh (i.e. non-thermally altered bone) faunal bone refuse, of which hare was noted. Nothing could be definitely associated with a fire-reddened stain in the southern portion of the excavation.

The excavations confirm our preliminary interpretation of this feature as the result of the collapse of a conical or "tipi"-like tent structure. The base of a number of substantial poles form a semi-circle and it appears the tent poles fell in the direction of the lake.

While the placement of the circular eastern hearth would coincide with a presumed opening of the tent feature, the other two combustion areas would have been located dangerously close to the sides of such a feature. However, in no instance can we be certain of the contemporaneity of any of these hearths with the tent structure which once stood at this location. Similarly, the artifacts consist of lithics, faunal remains or fire-cracked and unfortunately do not allow any separation between what is surely a series of re-occupations.

Whirl Lake

Field No: 86JLP-18
Borden No: MjTp-7


Human remains were found here in
1986 (Pilon 1987:83-84). We returned this field season in order to adequately document the remains of the collapsed burial platform which had only been made apparent upon returning to the site in 1986 with the R.C.M.P. in order to retrieve the skull which had been found.

The western end of the platform had been hidden from view by a fallen spruce tree. Upon removal of the tree, the support cross-piece still had segments of the vertical poles held in place with wooden wedge in the two large holes which had been made in either end of it. Large logs which presumably formed the platform were also noted.

Mackenzie River

Field No: 86JLP-21
Borden No: MhTn-3


Our two days at the mouth of Tree River (Dachan chuu gehnjiga) were made all the more special by the presence of more than 12 people. Returning, as she has for so many years, to make dryfish was Marca Bulloch (née André) and Effy Niando of Inuvik. Also with Marca were two of her daughters and their children, and one of her sons. Alestine André, her sister Agnes Mitchell and her two children Candice and Bryan were also spending some time there before moving downstream to Dea-het-angil to continue their fishing there.

This virtual crowd and the reason which brings them here year after year, net fishing of whitefish and cony (Inconnu), are eloquent testimonials to the importance of this site over the course of many generations.

During our brief visit, the Mackenzie River bluff edge immediately upstream from the mouth of Tree River was examined. Faunal remains including of course fish but also large mammal (either moose or caribou) were recovered from an eroding buried hearth feature. In direct association was a square cut nail.

The location of this hitherto unreported portion of this extensive site, itself first documented in
1986, is just below the "Tree River" sign which overlooks the Mackenzie from a height of about 10-12 metres. It is also the edge of an eroding terrace of which little remains today. Mrs. Bulloch recounted how people used to camp up on this terrace and exploited birch trees for their bark in the area to the southeast.

Field No: 86JLP-23
Borden No: MhTq-1


During the survey of the Mackenzie River below the mouth of the Travaillant River, we stopped at the mouth of Pierre's Creek in order to further test the high terraces located there. Additional shovel test in the vicinity of the
cabin observed in 1986 failed to yield any artifacts although a complex stratigraphy was noted. The foundation of an older cabin was noted less than 5 metres from the standing structure in a southwesterly direction.

A recent camp (within the last 10 years or so) was noted on the plateau edge behind this cabin. Remains are strewn about an area centered on a tent frame and work tables.

We also examined the active beach and discovered lithic artifacts and faunal remains in the debris of an ice scour located approximately 15 metres from the mouth of Pierre's Creek and less than 5 metres from the shore of the Mackenzie River. Although the faunal remains could very well be relatively recent, the lithic specimens are not. These include two complete chert bifaces, core fragments and debitage. Shovel test pits were consequently excavated near this ice scour.

Although most were negative, one test pit, located two metres from the ice scour revealed the remains of a hearth feature. The feature consisted of a basin apparently excavated into the fine sand matrix of the beach. The upper edges of the hearth deposits rested on fine silts. Also along the periphery of the feature, large quantities of charcoal were found which included large pieces of charred wood. These occurred in the fine silts. The upper layer of the basin-shaped deposits consisted of finely crushed calcined bone. Underlying this layer was a thick band of orange silt. The last layer consisted of hardened silt which contained wood charcoal.

The hearth deposits around the edge of the feature were first encountered at a depth of approximately 25 cm and the bottom of the feature extended an additional 15 cm below that.

A piece of thick ferrous wire was found in what might be a more recent disturbance near one edge of the feature. Still, this artifact occurred at a depth of approximately 20 cm below the surface.

The artifacts from the ice scour and the hearth feature located nearby clearly indicate the possibility that even active beaches along the Mackenzie River may still retain evidence of prehistoric and early historic use. In this case, the slight point on the east side of the mouth of Pierre's Creek, combined with the strong discharge of that stream, and the resultant eddy appear to afford the active beach some protection agains the ravages of spring flooding. Scouring, although present at a number of spots on the active beach, is not extensive, and may only due to exceptional circumstances. Instead, overbank deposition of Mackenzie River silt appears to be a major agent of site preservation. Thus the potential for discovering sites, even on active beaches along the Mackenzie River should not be discounted out of hand as has been suggested (Hanks and Winter 1991).

This site was revisited in 1993 by Luc Nolin and additional testing was carried out.