Urve Linnamae in Placentia Bay in 1970

From June 26 to August 3, 1970, Dr. Urve Linnamae and her crew carried out an archaeological survey of the Placentia Bay area of Newfoundland while she was under contract to the National Museum of Canada. Prior to this Dr. Linnamae conducted excavations at the significant Palaeoeskimo sites of Cape Ray Light in 1967 and the Pittman site in White Bay in 1967 and 1968. In 1975 she wrote the influential monograph The Dorset Culture: A Comparative Study in Newfoundland and the Arctic. Technical Papers of the Newfoundland Museum, No.1 in which she discusses ‘…the position of Newfoundland within the Dorset culture area and the nature of Dorset culture regional variation.’ Dr. Linnamae went on to become an associate professor in the Department of Archaeology at the University of Saskatchewan and retired from that position in 2003 (Linnamae 1971 & Biography).

The National Museum of Canada focused on this area of Newfoundland for several reasons including:

  • the lack of known archaeological sites in the area at the time;
  • an attempt to increase the known geographic distribution of the Dorset;
  • to define the ecological adaptations and relationships within this southern and environmentally different area of Newfoundland and the Dorset culture (Linnamae 1971).

In particular the survey focused on the islands of inner Placentia Bay and around Come by Chance and Arnold’s Cove. The team also briefly visited Old Perlican and Gooseberry Cove, Trinity Bay (Linnamae 1971).

During the survey the team found or revisited 12 archaeology sites. Six of these were very small sites and two were spot finds of just single artifacts. The visit to Old Perlican was for a revisit of a known site and to view the associated collection held by a local person. All of the sites had some precontact component, most commonly it was Dorset Palaeoeskimo. Several sites had either a Maritime Archaic or Recent Amerindian component.  Finally, four sites had a European component (Linnamae 1971). In this post I’ll tell you what Linnamae and her team found at four of these sites.

General area of Placentia Bay Archaeological Survey. 1 Old Perlican 2 Heart's Ease 3 Bordeaux 2 4 Bordeaux 1 5 Long Island Neck 6 New Grove 7 Great Brule 8 Tack's Beach 9 Dog Harbour 10 Unnamed Cove 11 Come-by-Chance 12 Little Brule (Linnamae 1971)
General area of Placentia Bay Archaeological Survey.
1 Old Perlican
2 Heart’s Ease
3 Bordeaux 2
4 Bordeaux 1
5 Long Island Neck
6 New Grove
7 Great Brule
8 Tack’s Beach
9 Dog Harbour
10 Unnamed Cove
11 Come by Chance
12 Little Brule
(Linnamae 1971)

The largest site found by Linnamae was New Grove (CkAm-01). This site is located in a small cove on the eastern shore of Long Island, the second largest island in Placentia Bay. The site consists of Maritime Archaic, Dorset Palaeoeskimo and European components. Unfortunately the European occupation seems to have disturbed the earlier occupations. As well, the site has been heavily eroded along the beach side by high seas and winter ice (Linnamae 1971).

PLATE I New Grove CkAm-01 Looking down at site area towards the North. Seated figure in midground is at Test Trench 3. PLATE II Looking at eroding bank edge at southern part of site. From the water Test Trench 3 is near the right side of the photograph. (Linnamae 1971)
PLATE I
New Grove CkAm-01
Looking down at site area towards the North. Seated figure in mid-ground is at Test Trench 3.
PLATE II
Looking at eroding bank edge at southern part of site. From the water Test Trench 3 is near the right side of the photograph.
(Linnamae 1971)

Linnamae opened four small test trenches along the eroding bank at the beach near the center of the cove. From these trenches and observing the eroding bank she determined that the occupation layer only minimally extended beyond the area of her trenches. Despite the impact on the site they recovered 2694 pieces of cultural material including 225 artifacts and a sample of charcoal from the Dorset component which returned a date of 1730±80 (Gak-3276) BP (Linnamae 1971).

They recovered 42 endblades most of which exhibited grinding on the basal element and sometimes over the whole endblade surface. All of these were made on a white/grey chert which later became known as Trinity Bay chert among archaeologists. We now know that geologically this chert is actually part of the Conception Formation and more accurately should be referred to as Conception Formation chert. The extensive grinding and white/grey chert are typical of Trinity/Placentia Bay Dorset occupations. Linnamae and her crew also recovered 18 microblades, 14 bifaces, two pieces of ground slate, four abraders, one endscraper and a fragment of a soapstone pot (Linnamae 1971).

Conception Formation chert typically exhibits a whitish-beige or brownish-beige weathering rind that can be chalky, however when freshly broken surfaces display a blue-grey (battleship) colour. This colour and the distinctive weathering constitutes a clear Conception Group signature (LeBlanc 2008: 59).

New Grove Artifacts a-h endblades i blade fragment j endscraper k-o microblades (Linnamae 1971)
New Grove Artifacts
a-h endblades
i blade fragment
j endscraper
k-o microblades
(Linnamae 1971)

The recovery of one endscraper from a Dorset occupation is unusual, Linnamae noted this in her report and that endscrapers are usually one of the most frequent artifact categories found on Dorset sites. Therefore her preliminary interpretation of the site was that hunting and the manufacture of hunting implements were the primary function of the site (Linnamae 1971).

In 2002 I revisited New Grove with a colleague. We found a few small artifacts on the beach and noted that the site is continuing to erode.

New Grove in 2002
New Grove in 2002

Long Island Neck (CkAm-02) is located on a partially grass covered sand bar near the northern tip of Long Island, just two kilometres north of New Grove. There are high rock outcrops on both ends of the sand bar so the site was limited to just the sand bar. With almost no grass cover on the north end of the bar the majority of the site was found on the south end. Even when the site was found by Linnamae in 1970 it had undergone heavy erosion (Linnamae 1971). 

Long Island Neck CkAm-02 Looking down at site towards the North. In immediate foreground is the remaining grassy area containing a buried occupation area
Long Island Neck CkAm-02
Looking down at site towards the North.
In immediate foreground is the remaining grassy area containing a buried occupation area.

Linnamae and crew opened two trenches in the southern area and recovered 470 pieces of cultural material including 25 artifacts and a charcoal sample that returned a date of 2240±210 (Gak-3274). The site has a possible Maritime Archaic and a Dorset component. The date however is too late for the Archaic and would be one of the earliest dates for Dorset on the Island of Newfoundland if correct. Interestingly, the Bordeaux 2 (CkAm-05) site was found by Linnamae in 1970 just outside Arnold’s Cove and just 9 kilometres from Long Island Neck. It had a single Dorset occupation dated to 1090 ± 90 (Gak-3275) making it one of the latest dates for Dorset on the Island of Newfoundland (Linnamae 1971 & 1975).

Nine of the recovered artifacts are endblades, three of which are ground on the basal half. Four microblades and a microblade core were recovered. As well there were four fragmentary bifaces and a piece of ground slate. Given the small assemblage it’s hard to say much about the site; Linnamae did suggest that it represented a repeatedly used small hunting camp (Linnamae 1971).

Long Island Neck CkAm-02 a-f endblades g New Grove h blade i uniface jendblade k microblade core l knife fragment m microblade n side-notched point o biface p ground stone implement (Linnamae 1971)
Long Island Neck CkAm-02
a-f endblades
g from the New Grove site
h blade
i uniface
j endblade
k microblade core
l knife fragment
m microblade
n side-notched point
o biface
p ground stone implement
(Linnamae 1971)

I also revisited Long Island Neck in 2002. As at New Grove, the site was still eroding but not completely gone and we found a few small artifacts eroded out on the beach.

Long Island Neck, to the left is south, to the right is north.
Long Island Neck, to the left is south, to the right is north.
Close up shot of the south end of Long Island Neck.
Close-up shot of the south end of Long Island Neck.

Linnamae also found two sites (CkAm-04 & 05) on either side of Bordeaux Head which is a broad sandy point of land that separates Come by Chance from Arnold’s Cove. Bordeaux 1 (CkAm-04) was a very small site consisting of 13 artifacts only one of which, a retouched flake, was found in situ (undisturbed). Everything else was eroded out on the beach, including a partial Dorset endblade (Linnamae 1971). 

Bordeaux 2 (CkAm-05) was a more prolific site with more than 100 pieces of cultural material recovered including endblades and microblades from an in situ occupation layer. This layer also contained an arrangement of stones which Linnamae interpreted as a hearth. A carbon sample was taken and returned a date of 1090 ± 90 (Gak-3275) which, as stated above, is one of the latest dates for Dorset on the Island of Newfoundland (Linnamae 1971 & 1975).

Bordeaux 2 (CkAm-05) Looking along beach toward the North at Test Trench 1, which is located on the grassy slope in front of the trees. (Linnamae 1971)
Bordeaux 2 (CkAm-05)
Looking along beach toward the North at
Test Trench 1, which is located on the grassy
slope in front of the trees.
(Linnamae 1971)

In 2005 I was fortunate enough to visit the Bordeaux 2 site as well. Although no artifacts were found it is believe that the site is pretty much how it was when Linammae found it in 1971.

Looking at the Bordeaux 2 site.
Looking at the Bordeaux 2 site.

After this survey Urve Linnamae wrote her 1975 book The Dorset Culture- A Comparative Study in Newfoundland and the Arctic. For the most part this work is based on her excavations at the Cape Ray site near Port aux Basques and the Pittman site in White Bay. As stated earlier this was an influential work, particularly for anyone studying the Dorset culture on the Island of Newfoundland. For example, Doug Robbins in the abstract of  his 1985 MA thesis dealing with the Dorset at Stock Cove referred to Linnamae’s book as a landmark in the history of Newfoundland Dorset archaeology. While Cape Ray and the Pittman sites are at the centre of this work, the Dorset sites found during the lesser known 1971 survey are also incorporated and play a role in this significant work. 


LeBlanc, Sylvie
2008 Middle Dorset Variability and Regional Cultural Traditions- a Case Study from Newfoundland and St. Pierre and Miquelon. PhD, University of Alberta.

Linnamae, Urve
1971 Preliminary Report of an Archaeological Survey of Placentia Bay, Newfoundland.

1975   The Dorset Culture- A Comparative Study in Newfoundland and the Arctic.

Linnamae Biography, University of Saskatchewan
http://library2.usask.ca/spcoll/University%20Authors/UA2006-07/UA%202007%20Linnamae%20Bio.doc

Robbins, Doug
1985  Stock Cove, Trinity Bay: The Dorset Eskimo Occupation Of Newfoundland From A Southeastern Perspective. MA, MUN.

The Bank site, Terra Nova National Park: Part 1

The Bank site (DdAk-05) was found by Dr. James Tuck during his 1979 survey of Terra Nova National Park. The site is inside Chandler Reach and is strategically situated at the juncture of three major channels, offering fine views down Clode Sound to the west, Chandler’s Reach to the east, and Goose Bay to the south. At that time of its discovery Tuck recovered two lithic artifacts, 98 lithic flakes and described the site as containing a predominantly Dorset Palaeoeskimo occupation. Most of the material culture was found in an eroding bank and a lack of evidence from test pits suggested the site was mostly eroded. The two identifiable artifacts recovered were a microblade and “an asymmetric knife with one straight and one convex edge and a deliberately blunted tip.” (Tuck 1980:37)

Despite the erosion present at many of the sites found in 1979, several sites were considered important enough to warrant further investigation. This was carried out in 1980 and during this time the Bank site was revisited and six more Dorset Palaeoeskimo artifacts and 43 unmodified flakes were recovered from the eroding bank. Three of the artifacts were endblades or endblade fragments, one was a scraper, one was a possible asymmetric knife or biface and the last was a bifacially retouched flake (Sawiki 1980: 96-71). The 1980 work in Terra Nova National Park formed the basis of a Master’s thesis for Anna Sawicki. The eroding nature of the Bank site and the small amount of recovered cultural material meant there was minimal interpretation of the site in Sawicki’s thesis (1983).

The Bank site around 1980 (Sawicki 1983)
The Bank site around 1980 (Sawicki 1983)
The Bank site around 1980 (Sawicki 1983)
Artifacts from the Bank site. a-c: Endblades d: Scraper e: Microblade f, g: Knives (Sawicki 1983)

In 1992 Dr. Fred Schwarz returned to the Bank site in part under contract to the Canadian Parks Service, and in part for Memorial University of Newfoundland under the terms of a research grant to the University by the Canadian Parks Service. Prior to his re-visit the general thoughts on the site were summarized by Schwarz as: The site thus appeared to be a typical Dorset site, with little potential for advancing our understanding of Newfoundland culture history, and, owing to its advanced state of erosion, little potential even for revealing anything new about the Dorset period (1993:6)

This attitude changed in 1991 when a Maritime Archaic stemmed projectile point was exposed and recovered during a routine monitoring visit. The projectile point was unusual for Newfoundland and its closest stylistic affinities were to be found in the Early Archaic in southern Labrador, dated to ca. 7200 BP. This find suggested that the site contained evidence of an Early Archaic occupation dating 1700 years earlier than any yet known on the island. The erosion of this now significant site prompted further investigations. Excavations were planned for the summer of 1992. In planning for this excavation the site was visited and more cultural material was visible in treefalls on raised ground beyond the eroding bank. It was also abundant in treefalls within the bog to the north. The latter also raised the possibility of preserved organic artifacts, a rare find on archaeology sites in the province. The Bank site had become much more important and much larger than previously believed (Schwarz 1993:6-7).

Excavations began on August 26 and continued until October 2. Archaeological operations at the site consisted of a combination of excavation, surface collection, screening, and test-excavation. The main excavated portion of the site, over 100m2, was stratified, with three distinct cultural layers extending across the site, in addition to more localized cultural features and deposits lying above and within the principal strata. During this work evidence was found for a small Maritime Archaic component, a major Dorset occupation, a Groswater occupation and Recent Indian (Beothuk ancestor) components (Schwarz 1993).

View West across excavations at the Bank Site (Schwarz 1993).
View West across excavations at the Bank Site (Schwarz 1993).
View East Across excavations at the Bank Site (Schwarz 1993).
View East Across excavations at the Bank Site (Schwarz 1993).

At the end of the 1992 work  the Maritime Archaic component was extremely small consisting of no more than seven artifacts including two chipped and ground slate axes, one side-notched projectile point, two possible tapered-stem bifaces, one possible lanceolate biface base and the Early Archaic projectile point found in 1991. In fact those seven artifacts were widely scattered across the site and showed no horizontal clustering which suggested to Schwarz that the Archaic occupation was never very intensive or was mostly eroded away. The 1992 excavations yielded no other evidence for an Early Archaic occupation, the remaining pieces all conforming stylistically to the well-documented Late Archaic occupation of Newfoundland (Schwarz 1993).

Maritime Archaic Artifacts Recovered at the Bank Site: a-b) Projectile points c-d) Possible tapered-stem bifaces e-f) Ground slate axes (Schwarz 1993)
Maritime Archaic Artifacts Recovered at the Bank Site:
a-b) Projectile points
c-d) Possible tapered-stem bifaces
e-f) Ground slate axes
(Schwarz 1993)

The Groswater component was slightly larger with 34 diagnostic artifacts recovered and 23 specimens that may be Groswater. The Groswater diagnostics include five semi-lunate inset sideblades, five sickle-shaped gravers, ten side-notched endblade bases and three complete examples, eight fine bifacially-retouched serrated endblade tips and midsections, two multiple-notched endblade bases, and one chipped and ground chert burin-like-tool. While Groswater artifacts were found in other sites in the area, the Bank Site Groswater assemblage is unusual for the high level of workmanship evident in the tools. In fact the workmanship was so fine Schwarz referred to the collection as “a strong, if not pure, component of Groswater artifacts in “Phillip’s Garden West” style.” (1993: 45) However, given the small sample size little else could be said about their occupation beyond it seems to have involved the full range of activities associated with a residential base-camp (Schwarz 1993).

Early Palaeo-Eskimo (Groswater) Artifacts Recovered at the Bank Site a-j) Side-notched endblades k-l) Multiple-side-notched endblade bases m-p) Serrated biface tips q-r) Hooked gravers s-w) Scrapers x-bb) Sideblades cc-dd) Side-notched knives ee) Large ground biface ff) Chipped and ground burin-like tool (Schwarz 1993)
Early Palaeo-Eskimo (Groswater) Artifacts Recovered at the Bank Site
a-j) Side-notched endblades
k-l) Multiple-side-notched endblade bases
m-p) Serrated biface tips
q-r) Hooked gravers
s-w) Scrapers
x-bb) Sideblades
cc-dd) Side-notched knives
ee) Large ground biface
ff) Chipped and ground burin-like tool
(Schwarz 1993)

The Dorset component was by far the largest at the site. It is represented by 1355 (93.4%) of the artifacts, by two distinct cultural strata (and elements of a third), and by five of the six cultural features identified at the site. Two of those features were interpreted as habitation structures with other features within the structures. One habitation structure was a semi-subterranean house with central axial feature flanked by cleared living spaces and was roughly oval in shape. The second habitation structure was similar to the first but less clearly defined. Both structures were backed by a midden area (Schwarz 1993).

The Little Passage complex, Recent Indian component at the Bank Site was also small, and highly localized, but distinctive according to Schwarz. Most of the Recent Indian component consisted of comer-notched projectile points and triangular bifaces. There were also a few undiagnostic pieces which Schwarz feels were Recent Indian. The diagnostic Recent Indian artifacts were strongly associated with Feature 1, a roughly linear deposit of fire-cracked rock and charcoal with lenses rich in calcined bone fragments measuring 2m by at least 5m. Similar linear hearth features found in Newfoundland and Labrador have been interpreted as the remains of communal feasting structures, because they are similar to shaputuan structures erected for mokoshan ceremonies, or “eat-all” feasts documented for the Innu of Labrador-Ungava. There were also seven Recent Indian biface tips, sixteen corner-notched projectile points and fifteen triangular bifaces localized to the Feature 1 area (Schwarz 1993).

Recent Indian Artifacts from Operation 10A2 at the Bank Site: a-m) Little Passage points (a-e are of Ramah) n-s) Triangular bifaces (n-q are of Ramah) (Schwarz 1993)
Recent Indian Artifacts from Operation 10A2 at the Bank Site:
a-m) Little Passage points (a-e are of Ramah)
n-s) Triangular bifaces (n-q are of Ramah)
(Schwarz 1993)

As unusual as Feature 1 was (In 1992 it was just the second such feature identified on the Island, today there are still just a handful of these features on the Island), the Recent Indian artifacts were more interesting for several reasons including because they were a very limited range of functional types; corner-notched projectile points, triangular bifaces, and perhaps one sidescraper. Schwarz believes the projectile points were from a chronologically-tight assemblage dating to the early-middle portion of the Little Passage Complex stylistic continuum ca. AD 1200. Missing from the assemblage are the lanceolate bifaces, endscrapers, linear flakes, etc. which might attest to a broader range of domestic activities on-site. Add to this the fact that diagnostic Recent Indian artifacts were closely associated with a single deposit, Feature 1. The Recent Indian occupation of the site was likely limited in both function and duration, to a single brief occupation. However, what is most distinctive and interesting about the Recent Indian artifacts is most were made from Ramah chert – a lithic material only found in northern Labrador and relied upon heavily by Labrador Recent Indians. While Ramah does infrequently occur on Newfoundland Recent Indian sites, it’s usually found as debitage. Finished Ramah artifacts are rare. Even today this site stands out; no other Recent Indian site on the Island has as many finished Ramah chert Recent Indian artifacts. The whole Recent Indian component suggests a brief, specialized occupation involving communal food preparation and the conspicuous consumption of valued objects (Schwarz 1993).

Charcoal and Firecracked Rock Deposit (Feature 1) in 10A2J. (Schwarz 1993)
Charcoal and Firecracked Rock Deposit (Feature 1) in 10A2J. (Schwarz 1993)

Since 1992 the Bank site has been revisited several times by three different archaeologists working with Parks Canada to monitor the erosion of the site. The next blog post will deal with those revisits.


Thank-you Lynne for providing the colour images.

Sawiki, Anna
1980 Archaeological excavations in Terra Nova National Park.

1983 Palaeo-Eskimo Occupations in Bonavista Bay, Newfoundland. MA, MUN.

Schwarz, Fred
1992 Archaeological Investigations at the Bank Site, Terra Nova National Park, Bonavista Bay, Newfoundland.

Tuck, James
1980 An Archaeological Survey of Terra Nova National Park.

The Dating Game Part 2: Newfoundland

Two weeks ago I went through the earliest and latest dates for the precontact cultures of Labrador, for this post I’ll look at the precontact cultures of Newfoundland.

As previously discussed, who and when are two of the most basic questions in archaeology. The question of who is generally understood in Newfoundland and Labrador. The question of when is often answered with radiocarbon dating, particularly for precontact cultures.

 The culture history of the Province’s past is fairly well understood and while most archaeologists in the province could easily tell you the date ranges for any culture many would be challenged when asked where those earliest and latest dates were found or what site they came from. This week I will take a look through the archaeology database of sites and point out where those earliest and latest dates were found and what site they came from on the island. As with the Labrador post, this isn’t meant to be the definitive list on site dates, things are changing all the time, it’s just the list I have in front of me right now.

Newfoundland Labrador
Maritime Archaic Indians (MAI) Maritime Archaic Indians (Earliest Settlers, First Explorers,LabradorArchaic)
Intermediate Indians (II) Intermediate Indians
Palaeoeskimo (PE) Palaeoeskimo
Recent Indians (RI) Recent Indians
Thule

Precontact Aboriginal cultures

The table above shows the generally accepted sequence of cultures in Newfoundland and Labrador’s precontact past. Within each of these major groupings there are other recognized groups that are temporal or geographic expressions of the overall group. I’m not going to break down the dates by the smaller groupings. Also, there is some temporal overlap between many of these groups. For example, there were Palaeoeskimo groups around when the Recent Indians were here. So the different cells in the table don’t mean the cultures are separate and didn’t co-exist. The table just follows the broad temporal pattern of oldest on top and youngest on bottom. Also, while we use names such as MAI and PE for the overall group we are not stating that within these groups there is a clear transition from the first to the last (i.e. earliest MAI is a direct ancestor of the last MAI). There is evidence in the archaeological record of different waves of people moving into and out of the Province during these time periods; the names are used to denote that they had similar cultural characteristics and we therefore classify them under the overall group name.

Earliest and latest known MAI sites in Newfoundland

For more than twenty years the generally accepted date for the earliest Maritime Archaic Indians on the island of Newfoundland was 5000 years which was based on charcoal from the Beaches site in Bonavista Bay that was dated to 4900 ± 230 (SI-1384). That date stood as the oldest until charcoal was recovered from the MAI site in South Brook Park, located between Corner Brook and Deer Lake, in 1998. The charcoal was dated to 5140±50 (Beta 122766). In 1999 charcoal was recovered from the MAI Gould site in Port au Choix which was dated to 5440 ± 50 (Beta-134151). This date still stands as the oldest known date for MAI on the island of Newfoundland.

The youngest known date for Newfoundland MAI comes from the Curtis site on Twillingate Island which was excavated by Don MacLeod from 1966 to 1968. The material dated was charcoal recovered from a small hearth which returned the date of 3200 ± 90 (GaK-1254). Along with having the oldest MAI date on the island the Gould site has some of the youngest dates including 3260 ± 50 (Beta-108099) and 3200±100 (Beta 132364).

Earliest and latest known II sites in Newfoundland

On the island there is a hint of an Intermediate Indian presence found in three sites on the Northern Peninsula. Garden Cove was found during exploratory work around L’Anse aux Meadows in 1975. There are no radiocarbon dates associated with the 3 artifacts that are thought to be II. The predominantly MAI site of Big Brook 2 was found in 2001 by Priscilla Renouf and was excavated by Greg Beaton in 2002. Greg found a hearth which was dated to 2830±40 BP (Beta-171714) around which were found II looking stone tools. However, II stone tools can look like late MAI stone tools and the site has a Groswater component which would overlap with the II period temporally. Consequently the questionable II tools at Big Brook 2 and the radiocarbon date could relate to a late MAI occupation or be attributed to the Groswater component. Finally, Woody Point 2 was found in 2005 by Ken Reynolds when part of the site was disturbed during construction. Follow up work also done in 2005 by Fred Schwarz recovered a lot of quartzite debitage and quartzite bifaces. These are items that are not frequently found in precontact sites on the island but are often found on Labrador II sites. There are no radiocarbon dates associated with the quartzite artifacts.

The suspected Intermediate Indian artifacts from Woody Point 2
Earliest and latest known PE sites in Newfoundland

The early end of the Palaeoeskimo sequence on the island starts with the Groswater and the earliest date comes from Phillip’s Garden, near Port au Choix on the Northern Peninsula. Phillip’s Garden is part of the Port au Choix National Historic Site; this designation is based on the importance of the archaeology in the area including Phillip’s Garden which has more than 60 Dorset Palaeoeskimo dwellings and that doesn’t include the earlier Groswater Palaeoeskimo dwellings. Given the importance of this site to the PE on the island it is not surprising that the earliest date comes from charcoal found in a dwelling/pit feature which was dated to 2760 ± 90 (Beta-23979). South of Port au Choix is another important PE site. The Factory Cove site is just outside of the community of Cow Head. The site was found by Jim Tuck in 1976 and was excavated by Reginald Auger. The site was described as a habitation/lithic workshop with at least 5 structures and several features. One of those structures was described as bilobate with a mid-passage hearth, charcoal from which returned a date of 2700±140 (Beta 4047).

The latest date for PE on the island comes from another site on the Northern Peninsula. Peat Garden North is located just outside the community of Bird Cove and was found by David Reader during a survey in 1997. A small amount of charcoal was found on the side of a Dorset axial feature and returned the late date of 959 ± 45 (BGS 2254). Land mammal bone from inside the same feature returned a date of 1030 ± 290 (TO-9555). Interestingly the small site of Bordeaux West on the opposite side of the island near the community of Arnold’s Cove returned a date of 1090 ± 90 (GaK-3275). The date was based on charcoal recovered from a hearth.

The Bordeaux West site is in the centre of the picture
Earliest and latest known RI sites in Newfoundland

On the island the Recent Indian period starts at around the same time as it starts in Labrador, around 2000 years ago and once again sites on the Northern Peninsula figure prominently in the dates. The earliest RI date comes from the Gould site, which also had the earliest MAI date. The Gould site was found in 1996 by Priscilla Renouf. The RI portion of the site was excavated by Mike Teal. One of the features he excavated was made up of an irregular shaped depression that contained fire cracked rock and charcoal, the latter of which was dated to 2080+/-40 (Beta 134147). Another date of 1950+/-60 (Beta 120796) came from a charcoal-lined pit. There were also very early RI dates recovered from a separate site in the Bonavista Bay area. A date of 1950+/-100 (Gak 1481) came from the Beaches site. However, this is a multi-culture site which is not well stratified so the date could be from a PE occupation. There are two more early dates from the Bonavista Bay site of Cape Cove 3; 1920+/-130 (S-1863) and 1865+/-110 (S-1862). The first date came from charcoal associated with a stone tool manufacturing area. The second date, which also has been reported as 1865 +/- 110, was based on charcoal from a hearth.

The latest dated RI site on the island actually dates to the post-European contact period and this is not at all surprising because it has been known for years that the last of the RI on the island became the Beothuk. This transition is clearly demonstrated at several sites including Boyd’s Cove and Inspector’s Island where we see a slow transition from stone tools to the use of European tools and we see stone tools in the same level and next to European objects such as pipe stems and ceramic fragments.

Newfoundland Dates
Maritime Archaic Indians ~ 5500 years ago-3200 years ago
Intermediate Indians No dates
Palaeoeskimo ~2800 years ago-1000 years ago
Recent Indians ~2000 years ago-Beothuk