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The Crescent Beach site and the place of the Locarno Beach phase / edited by R.G. Matson Matson, R.G. Feb 19, 2010

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The Crescent Beach site and the Place of the Locarno Beach Phase Chapter I INTRODUCTION R.G. Matson and H. Pratt  The Crescent Beach site (DgRr 1) was excavated in 1989 and 1990 as part of “The Origins of the Northwest Coast Ethnographic Pattern; The Place of the Locarno Beach Phase” research project. The excavation of the Crescent Beach site was one of the three major parts which comprised the overall project funded by S.S.H.R.C. (Matson 1988a). The three main goals of this project are as follows: 1. The reanalysis of existing Mainland Locarno Beach collections originally collected by C. E. Borden; 2. The comparison of these assemblages with both earlier and later cultures; and 3. The excavation and analysis of the Crescent Beach site with the focus on recovering subsistence information on Locarno Beach and earlier and later cultures. The choice of Crescent Beach for this investigation is based on the knowledge from previous excavations that it was the only known mainland site that had the Locarno Beach component “sandwiched” in between immediately preceding and succeeding cultures. This volume reports on all three aspects, although the bulk is concerned with the description and analysis of the material recovered from Crescent Beach in 1989 and 1990. The importance of the Locarno Beach phase lies in its position relative to the development of the ethnographic cultures observed on the Northwest Coast. These well-known cultures, referred to as the Developed Northwest Coast Pattern by Matson and Coupland (1995:5-8), represent a stage that archaeologists have long agreed to have been reached by circa 1500-2000 years ago during the Marpole phase (Borden 1970; Mitchell 1971:54; Burley 1980; Matson and Coupland 1995:200-225). The Marpole phase is well represented in the Gulf of Georgia region, and succeeds the Locarno Beach Phase (Borden 1970; Mitchell 1971, 1990; Matson and Coupland 1995:154-183) which dates from circa 3300-3500 RCYBP to 2500 RCYBP. The Locarno Beach Phase, in turn follows the Charles culture, represented by the St. Mungo and Mayne phases in the Gulf of Georgia. There is general agreement that the Charles culture does not represent the Developed Northwest Coast Pattern (Matson and Coupland 1995:97-142) but the position of the Locarno Beach phase in this regard is less clear, with some investigators finding little evidence of the characters associated with the Developed Northwest Coast Pattern (Burley and Knusel 1989; Matson and Coupland 1995) and at least one arguing otherwise (Carlson 1991). During the past few decades, there have been many theories about the origin of the Developed Northwest Coast Pattern (Matson 1992; Matson and Coupland 1995:146-154). In the past decade or so, the publication of the relevant archaeological details for many regions in the Northwest Coast culture area has allowed archaeologists to go well beyond preliminary sequences. From this more detailed and informed perspective attempts have been made in creating a more cohesive picture of Northwest Coast prehistory. It is from the now available data that we know that there is no substantial evidence of the Developed Northwest Coast Pattern during the St. Mungo phase. We now know that the long-held belief about the Developed Northwest Coast Pattern being reached during the Marpole is well-justified. Therefore,  1  Chap.1, November 20, 2008  sometime between the St. Mungo and Marpole phase full scale development of the Northwest Coast Pattern takes place. At the time this project was initiated, the Locarno Beach culture was much less welldocumented than either preceding or succeeding cultures, and although, it still remains to be documented more fully, our state of information is more comparable to chronologically neighbouring cultures. There are three major issues concerning the Locarno Beach phase and its contingent cultures; its economic organization; its relationship with preceding and following cultures; and its social organization. Croes and Hackenberger (1988) argue that the switch from a pre-storage to a storage economy is a pivotal transformation, and they suggest that this has occurred by the Marpole phase. Croes and Hackenberger also argue that pre-storage populations on the Northwest Coast were limited largely by the amount of shellfish available for procurement during the winter season. In Croes and Hackenberger’s model, the first resource to be stored in large quantities was Flatfish taken in the spring and summer. In time stored Salmon became more important than Flatfish, since Salmon, unlike Flatfish, could be intensely utilized without any noticeable decrease in the population size of this fish. Intensive utilization of Salmon would be more important as the storage and processing technology develops so that large amounts could be processed during its short season of availability. The change in abundance, and type of fish and shellfish remains from Crescent Beach can be used to evaluation this model in general, and the nature of the Locarno Beach phase economic organization more specifically. For example, at the beginning of the Locarno Beach phase, at Crescent Beach, is there evidence for a wide scale dependence on shellfish which gradually evolves into a dependence on Flatfish which then declines and is replaced by Salmon? By the beginning of the Locarno Beach phase dependence on shellfish may have decreased and the culture may have been moving towards a more storage dependent economy. Matson (1983) predicted that Locarno Beach would not be salmon dependent, which he saw as co-occurring with the Marpole phase (which also fits Croes and Hackenberger’s economic model). As we will see, there were some real surprises for Matson (e.g. Matson 1992). Croes and Hackenberger’s model fits a trend most Northwest Coast Prehistorians see, that on the Northwest Coast there is a gradual change from an early generalized coastal adaptation, to a later more productive and specialized economic pattern. Careful excavation focussing on the recovery and analysis of subsistence information present at Crescent Beach does shed light on these issues. The second major issue, involves the relationship between Locarno Beach and contingent cultures. Although the artifacts recovered from the 1989 and 1990 Crescent Beach excavations were too limited to conclusively resolve the second research question, the linkage of this data with Percy’s (1974) much larger set based on earlier excavations is informative (Pratt 1992). These results are summarized in Chapter XI. The questions examined have to do, on the one hand, the relationship between Locarno Beach and Marpole, and on the other, the relationship between Locarno Beach and St. Mungo. Underlying both questions is the relationship between the existing published descriptions of the Locarno Beach phase, largely based on Gulf Island components, and that recovered from Crescent Beach. The third and final issue focuses on the social organization of the Locarno Beach phase. This subject encompasses a number of issues, but the one that we are concentrating on is the relationship between economy and society. Given that Northwest Coast society is keyed on control of resources, can we identify developments in this realm based largely on subsistence information excavated in a specific way from a site? Based on Croes and Hackenberger’s model, shellfish would have been key resources in the Pre-storage economy, and as previously mentioned, the presence of substantial amounts of shellfish prior to Flatfish and Salmon may imply that a storage technology was not yet in use. If shellfish were the key winter resource, we would expect their use to have been concentrated in the winter, and possibly important beds to have been “owned” by a specific group or family. The ownership of resources, then, may have occurred previous to, and therefore be partially responsible for the development of other aspects of Northwest Coast Society  2  Chap.1, November 20, 2008  (Matson 1983,1985). The Developed Northwest Coast Pattern is well known for its multifamily households, and this has been often seen to be tied in with the stored salmon economy and the ownership of resources, along with the development of a stratified society. All of these aspects are either demonstrated (remains of very large planked houses, large numbers of salmon, the analysis of burial remains by Burley and Knusel [1989]) or assumed (ownership of important resources) because of the presence of evidence of the other attributes for the Marpole culture. Which of these characteristics are present in Locarno? Those that are then can be linked to those that only occur later in Marpole and be evaluated if they are “necessary prerequisites” or even causal for the later occurring traits. Although the previous paragraph shows the similar logic as the current one, it was part of the original research design, and this one was not. As the research evolved, it is this more general approach of the current paragraph that produced the most useful results. With the above orientation of the original research design, the excavation at Crescent Beach focussed on seasonality and subsistence information first, and artifact accumulation second. Given the known effect that combined specialized stratigraphic layers can look like a generalized economic adaptation, concealing their specialized nature, major efforts were spent excavating by natural layers and keeping separate, both in the field and in the lab, the information gathered from these natural layers. After the successful completion of the 1989 field season it was obvious that our work in natural layers was paying off with a great deal of information on subsistence and this approach was continued into the 1990 field season with little change in our excavation strategy. Working over wide areas within natural layers was first carried out in the Northwest Coast at the Crescent Beach site in 1977 by Ham (1982), and we learned many lessons from his work, which helped prepare us for our own fieldwork. The organization of this volume is as follows: First the area and previous excavations are reviewed; Second the excavations in 1989 and 1990 are described, followed by a synthesis of stratigraphy and dating. Next the artifacts are described, followed by the faunal analyses. The important features are next briefly summarized in a short chapter. An interpretive description of the the site components follows. Next descriptions of C. E. Borden’s Locarno Beach and Whalen Farm excavations are given along with the our tabulation of the artifacts recovered. Finally, a concluding chapter both summarizes the findings at Crescent Beach, and investigates the similarity of the various “well described” Locarno components with each other and early and later cultures and returns to the general questions posed in this introduction.  3  Chap.1, November 20, 2008   Chapter II THE CRESCENT BEACH SITE; LOCATION AND PREVIOUS INVESTIGATIONS H. Pratt and R.G. Matson INTRODUCTION The Crescent Beach site is situated on the eastern shore of Mud and Boundary Bays, approximately 6.5 kilometres north of the Canada- United States border (Figure II-1). It is within the traditional territory of the Semiahmoo Band of the Straits Salish. The mouth of the Nicomekl River forms the northeastern boundary of the Crescent Beach site, while a high bluff provides an approximate limit to the southeastern extent of the prehistoric deposits. This bluff rises sixty to ninety meters and is composed of unconsolidated Pleistocene deposits (Conaty and Curtain 1984:7). The site itself is spread out from the toe of the bluff out on to the present low-lying spit on which the present community of Crescent Beach lies (Figure II-2). Ham (1982) provides a detailed and precise description of the physiographic, geological, and biological environment of the Crescent Beach Locality, on which the account below is partially based. PALEOGEOGRAPHY Crescent Beach is at the eastern edge of Boundary Bay, at the edge of the White Rock uplands, which consist of Pleistocene deposits laid down by glaciers during the Wisconsin glaciation, which is locally referred as the Fraser Glaciation (Armstrong 1981). Other highland areas such as Point Grey and Point Roberts are of similar composition, being made up of a variety of unconsolidated Pleistocene materials. In the early Fraser Glaciation the Quadra deposits blanketed the Strait of Georgia with as much as 75 metres of deposit, but a lot of these were removed when the glaciers advanced to cover the area. The ice began to waste by approximately 14000 years ago and seems to have be gone from this area by 12000 RCYBP. As the ice left the land rebounded from its depressed position, as the world-wide sea level rose because of ice melting, resulting in a very dynamic situation, which is still poorly understood. It is clear that initially the sea level was relatively much higher, but by 9000 RCYBP the sea level was around 12 metres below today (Williams 1988:187) according to a study based on analyzing a series of drill cores from the delta. The gross pattern since that time for the lower mainland is that of a steadily rising sea level. The basin north of the White Rock uplands now occupied by the Serpentine and Nicomekl Rivers (Figure II-1) must have been filled in early in the post-glacial period. Initially the Fraser River filled in a series of basins in the lower Fraser valley, but by 8000 RCYBP began to fill in the current Fraser Delta, as shown by the Glenrose Cannery Site (Matson 1976). The Fraser River probably had a much heavier sediment load prior to 7000 RCYBP than it does today, and rapidly developed the present delta. Williams (1988) presents convincing evidence (buried peat deposits) of a still stand at about 6000 RCYBP. Boundary Bay was probably at least one of the exits of the Fraser River at this time. By 4400-4100 RCYBP Hebda (1977:170) argues that the delta front had reached the Point Roberts Uplands, beginning blocking the flow of the Fraser River from Boundary Bay. Williams (1988:198) has the delta’s tidal flats within a few km of Point Roberts by 4500 RCYBP. Since the oldest dates from the Crescent Beach site are of this period, it appears that the first occupation took place at about the time the Fraser River no longer entered into Boundary Bay. Williams (1988:198) states that the sea-level rise slowed markedly at about 4500 RCYBP at which point it was about 2 metres below the current level. The sea  1  Chap.2, Feb. 15,2008  Archaeological Sites Point Grey N  Locarno Beach { Old Musquam Musqueam Sites Musqueam NE Marpole Frase rR  GABRIOLA ISLAND  ve  i  False Narrows  Serpentine River r ive Necomekl R  VALDES ISLAND  Crescent Beach  GU  Shingle Point  LF  OF  Long Harbour  CANADA USA  Beach Grove Whalen Farm  GE  OR  GI  GALIANO ISLAND  A  Montague Harbour Georgeson Harbour Helen Point MAYNE ISLAND SATURNA ISLAND  SA  VANCOUVER ISLAND  r  Glenrose St. Mungo  LULU ISLAND  L IS TSP LA R ND IN G  Pender Canal  PENDER ISLAND 0  10  20 km  Figure II-1, Crescent Beach Location level essentially reached the modern relationship about 2250 RCYBP according to Williams (1988:189), although the delta continued to expand north of Point Roberts. In summary, at the time of first occupation at Crescent Beach, the Serpentine and Nicomekl Rivers were probably present in something like their present situation, and the Fraser River emptied in the Gulf of Georgia, north of Point Roberts. Although the current shoreline was probably different, the current structure of Boundary Bay was probably very similar to that today. It was probably only after the Fraser River no longer entered Boundary Bay that the Crescent Beach could begin to develop. It is of interest to note that the earliest archaeological deposits are immediately adjacent to the Pleistocene highlands, indicating that the spit did not exist at that time. PLANT COMMUNITIES Evidence from pollen records (Hebda 1977, Mathewes 1973) indicates that the plant community had evolved to something very similar to that observed by the first European visitors by 4000 years ago. On the highland areas, a coniferous forest was present, with Red Cedar (Thuja plicata), Hemlock (Tsuga heterophylla), Douglas Fir (Pseudotsuga menziesii) and Sitka Spruce (Picea sitchensis) being the most important large trees. Minor tree species include Vine Maple (Acer circirnatum), Maple (Acer macrophyllym), lodgepole pine (Pinus contorta), several species of cottonwood, Alder (Alnus rubra) and yew (Taxis brevifolia). The  2  Chap.2, Feb. 15,2008  understory of shrubs, including Oregon grape, Salal, blue berries, huckleberries included a number of useful economic species. Much of the delta to the north of Boundary Bay was covered by Peat Bogs, as well as parts of the Serpentine-Nicomekl river valleys. These are elevated up to 3 m above sea level. As well as sedge-sphagnum peat, economic shrubs such as hawthorn, crabapple, cranberry, Sasakatoon berry (Amerlanchier alnifolia) are found in the bogs. Bog resistent tree species, such as Pinus contorta, and Hemlock, were found around the fringes. Large grasslands and grassland and shrub communities were also present, although, as Ham (1982) points out, they are not what we expect to exist on the coast. On the North et al. (1979) map, these are found surrounding Burns bog and other low-lying areas. Ham (1982:37) indicates these communities include two forms, a dry and wet variants, with the dry community dominated by Agrostis stolonifera. The shrubby parts include willow, crabapple (Pyrus fusca) and rose (Rosa sp.). These open communities are home to a wide variety of animals, including elk, deer, otters, beavers, and a wide variety of birds. Between the open areas and the coniferous forests, along the streams, and colonizing old burns were forested areas, not dominated by conifers. Trees important here, include maples (Acer macrophyllum and A. circirnatum), alder (Alnus rubra), cottonwood (Populus spp.), Willow, (Salix spp.), Birch (Betula spp.) as well as smaller numbers of the conifers found in the coniferous forests. Ferns, horsetails, skunk cabbage, and a wide variety of shrubby plants are also present. Between the grassland communities and the normal high tide line a salt-marsh community was present in many areas along the delta front and along Nicomekl-Serpentine valley. Sedge and bulrushes are found at the shore-side of this community, while arrowgrass, sandspurry, and salwort, the sea-side. This review of plant communities around Boundary Bay indicates something of the diversity present; a more thorough treatment with the communities further subdivided in present in Ham 1982. As well as a diversity of plant communities on land, diversity in shoreline communities are also present around Crescent Beach today, and there is every evidence that they have been present for the last 4000 years. INTERTIDAL COMMUNITIES The intertidal zones around Crescent Beach fit into Part II, bays and estuaries of the classic work Between Pacific Tides (Ricketts et al. 1985). Although they differ in some ways vary from these classic descriptions, the Crescent Beach locality intertidal zones general have most of the important features and animals present in Ricketts et al. (1985). The first community described by Ricketts et al. (1985:269-316) is that of Rocky Shores, and this is also one of the most important in terms of resources found at the Crescent Beach site. Today the rocky intertidal zone begins circa 400 meters south and east of the site and extends towards White Rock (Figure II2). Zones 1 and 2 include the uppermost horizon and high intertidal in Between Pacific Tides format. Acorn barnacles are the animal present highest in the zone, with the small Balanus glandula present near Crescent Beach. Whether they were actually used as food is unclear. Also present are limpets (esp. Collisella pelta) and periwinkle (Littorina sitkana) likely of no economic value as are hermit and shore crabs. Also present in the high intertidal is the bay mussel (formerly Mytilus edulis, now Mytilus trossulus) which can occur in great numbers. This is a very important economic resource with many early northwest coast middens having Mytilus as the most abundant shellfish. Ricketts et al. report that this mussel usually does not exceed 5 cm long, although the occasional individual twice that size is found. This shellfish sometimes blankets the rocky foreshore in bands southeast of Crescent Beach. A variety of small worms and pill bugs are often found in these zones as well. None of these, however, are of economic value, which is also true of the more abundant sponges.  3  Chap.2, Feb. 15,2008  Figure II-2. Air Photograph of Crescent Beach in 1940(BC 2071) with Rocky Foreshore indicated. The next zone, 3, is the middle intertidal. A picturesque animal often seen here is the purple starfish (Pisaster ochraceus), a predator on mussels. Whelks, mainly Nucella lamellosa, are also found . These congregate together in small groups to breed, when mature in winter or spring (Ricketts et al. 1985:276). The hardy shells of whelks are frequently found in archaeological sites, usually broken in such a way that their tasty muscle can be obtained. It may be that significant numbers are only obtained when the whelks congregate to breed. Abandoned whelk shells are used by the hairy hermit crab (Pagurus hirsutiusculus). Also present are sea anemones, particularly Anthopleura elegantissima. The purple shore crab, Hemigrapus nudus, is often abundant. Chitons, usually Tonicella linenta, are commonly present, as well as limpets, although usually in modest numbers. Small crustaceans, pillbugs, and worms occur “in such variety and abundance to distract the specialist” (Ricketts et al. 1985: 280). The most important economic species in zone 3 is Protothaca staminea, usually called the littleneck clam in B.C. It is found in packed mud, gravel and sand in clayey gravel and usually lies within 8 cm of the surface. According to Ricketts et al (1985:281) it seldom exceeds 7 cm in size but often occurs in very dense quantities. It can be obtained in large numbers with a rake today. The shell of this clam is frequently found  4  Chap.2, Feb. 15,2008  in archaeological sites, where its distinctive cross-hatching on the outside of the valves makes it easily identified. Given the large number of important economic species in the higher intertidal zones, it is curious that zone 4, the low intertidal zone has few of note. A variety of starfish are present as well as worms, snails, and tunicates. Also present is the native oyster, Ostrea lurida. Although Ham (1982) found there present in later deposits at Crescent Beach, they occurred in small numbers and were not identified in our work. Also of possible economic importance is the green sea urchin, Stongylocentrotus droebachiensis. This species occurs today in large numbers in the Gulf Islands but is present today in the Crescent Beach locality in very low numbers, if present at all. Ham (1982:248) reports a single presence (0.01g) of sea urchin in his work. The rock oyster or jingle, Pododesmus cepio, is also present, and its orange flesh is said to have an excellent flavor (Ricketts et al. 1985:290). A variety of crabs and tubeworms are also found in this zone as well as sea cucumbers. Sponges and chitons are also present. Further out in deeper waters, scallops are present, but these are not seen in numbers in archaeological sites. Although not really a full-time resident of this zone, the Dungeness crab, Cancer magister, is often found here. Really a resident of deeper water this large crab comes inshore to molt and thus gets stranded in the low intertidal zone. The only part of this animal found in archaeological deposits are the very tip ends of the pinchers (Ham 1982:248). Also present in this zone is the plainfin midshipman (Porichthys notatus). These fish make nests under rocks where they guard their eggs. This occurs in the spring where they can be gathered during low tides. They “grunt” when poked and so are known as grunt fish. Remains of these fish are found in archaeological sites, although not in large numbers. Although fish, these animals are ‘gathered’ rather than obtained by the usual fishing techniques. Although the present day rocky shores environment is very limited today in the Boundary Bay area, the remains of animals living there are very abundant in the archaeological record, demonstrating its importance to the people living here in the past. There are grounds to expect the rocky foreshore environment was larger in the past. As reviewed above, the relative sea level was rising until about 2250 RCYBP. In a rising sea level situation rocky foreshores are continually being created as new sea cliffs are being created. In a stable sea level situation, the slopes lessen, and the sand beaches expand at the expense of the rocky shores. This sort of situation is thought to have created dramatic changes in the southern California coast, for instance (Warren et al. 1961). One would expect something of the same process to have occurred in the Boundary Bay area, where the beaches, including Crescent Beach, have expanded at the expense of the rocky shores, although probably not to a great amount. Sand Flats are the next community to be discussed within Part III of the Between Pacific Tides. Extensive areas around Boundary Bay belong to this environment, although few resources of economic value are present. Unlike most other intertidal environments, these are not well zoned by tidal position. One abundant animal, familiar to most is the sand dollar (Dendraster ssp.) which can occur in great numbers around Boundary Bay. These are actually sea urchins, but with small spines and a flattened body. Numerous crabs, snails, starfish, and shrimp are found, but of little economic value. Segmented worms are another class of animals that are abundant in sand flats but of little or no economic value. One medium sized clam, Macoma secta, is present, but in low numbers, and only occasionally seen in archaeological deposits (Ham 1982: 251). In summary, the broad sand flats produce little of economic value in terms of resident animals, although they may be important feeding areas for birds (when exposed) and fish (when inundated). Mud Flats is the last natural community to be discussed in Part III of Between Pacific Tides. However, the situation around Boundary Bay does not correspond very closely that described for the upper intertidal zones. Mud Flats in this area are often found below sand flats or adjacent to eelgrass beds in this area. Like  5  Chap.2, Feb. 15,2008  sand flats, few animals of economic values are found in mud flats that are distance from eelgrass beds. Most animals of economic value located in mud flats in Ricketts et al. appear to be associated with eel grass beds in the Boundary Bay area and so will be discussed under that community. One clam, though, is clearly present there, the bent-nosed clam (Macoma nasuta). This small clam, usually no larger than 6 cm is found fairly deep in muddy sediments. Ricketts et al. (1985:379-380) report than it can be found in very stale water, and that it was an important species for Californian Indians. That does not appear to be the case in the Boundary Bay area, although Ham (1982:251) does report a few identified remains in his excavations at Crescent Beach. Eelgrass Flats (Ricketts et al. 1985:341-353) are found in the lower intertidal zones, and consist of eelgrass (Zostera sp.) and associated animals. One of the most visible is the cockle (Clinocardium nutallii). This good eating shellfish has very short siphons and so lives very close to, and even on top of, the surface. It occurs in some numbers, but never very concentrated in eelgrass beds in the Gulf of Georgia area. Ricketts et al. place it in sand flats, where it is very rare. As will be reported later, it can be obtained in larger numbers in the spring time, than at other times. Another very important shellfish is found in and at the lower edges of eelgrass beds, the horse clam (Tresus capex and T. nutallii). This very large clam lives up to 0.5 metres below the surface, with a long siphon extending up to the surface. The shells ‘gaps’ not enclosing the body totally, thus leading to another common name ‘gaper’. These are important economically, with dried animals being an important trade item (Suttles 1951:69). In some places horse clam beds were “owned” (Suttle 1951:68,69) and inherited. Horse clams can be easily spotted at low tide by their siphons; these have sizes according to the body size of the clam, and have a tough, leathery top, making them easy to spot and identify. These features make clusters of horse clams easy to spot, and even their sizes to be estimated before digging. In addition to these two important shellfish, the starry flounder (Platichthys stellatus) is also a resident and can be sometimes collected in very shallow water. Lots of uneconomic animals are also present in the eelgrass flats. Varieties of snails, nudibranchs, sponges, and shrimp abound, along with many types of worms. Another important clam, Saxidomus giganteus, locally called the butter clam is also present near eelgrass beds. Ricketts et al. (1985:378) have this clam being present in mud flats, but experience in the Gulf of Georgia (Matson 2003) and at Crescent Beach places this clam more in gravelly/sandy areas, often at the foot of steep gravelly beaches where sandy flats begin. This clam, then can be found at the up-beach edge of eelgrass beds, and at the foot of rocky foreshores, at lower intertidal zones than Protothaca, although much deeper in the sand. This large clam is important today economically, and is common in archaeological sites. Although the eelgrass and rocky foreshore zones are treated by Rickett et al. (1985) as being usually located in different areas, today they can be found adjacent to each other, just southeast of the Crescent Beach site. Here, erosion of the headlands of the White Rock uplands has resulted in rocky foreshores from above hightide line to low tide. But further out are eelgrass beds, in a sandy-muddy situation, with Clinocardium and Tresus present. Eelgrass flats are also present due south of the Crescent Beach site. No other concentration of different productive zones is present around Boundary Bay, until one gets to the Point Roberts uplands. It is likely that this general distribution of intertidal communities has been present for about 4000 years. Since that time the shores between the highland ends of Boundary Bay have been along the edge of delta sediments, precluding the presence there of the important rocky foreshore zone. Today most of this intervening shoreline is the relatively unproductive (in terms of aboriginally important economic invertebrates) sand flats. Remembering that the important clams, Saxidomus and Tresus, although suggested by Ricketts et al. (1985) to be found in in mud flats and sand flats, today are not found inareas accessible at  6  Chap.2, Feb. 15,2008  most low tides around Boundary Bay, these zones are more barren than one might think. Thompson (1913) offers an interesting perspective on the shellfish beds of Boundary Beds in his “Report of the Clam-Beds of British Columbia.” In addition to the rich area to the south of Crescent Beach, he shows abundant Clinocardium and Tresus in the lower intertidal area of the mudflats surrounding Boundary Bay. Thompson’s sketch map corresponds in a general way with our current understanding of eelgrass flats. These areas are accessible only in the lowest tides. In summary, to the south of Crescent Beach today is a very rich shellfish area, with rocky shores and eelgrass flats closely adjacent. Nowhere else around Boundary Bay does a similar concentration of resources exist today. Further, there is no evidence that other similar areas have existed in the last 4000 years. There are, though, eelgrass beds around Boundary Bay where Clinocardium and Tresus are available. FISH RESOURCES The two most important resources recovered at Crescent Beach were shellfish and fish. The location of shellfish procurement is more certain than that of fish since shellfish are relatively sessile animals but some statements can be said about the more mobile fish. The greatest fish resource is the late summer availability of Sockeye salmon as they swirl through Boundary Bay on their way to the Fraser River. It is not clear that these fish were exploited by inhabitants of Crescent Beach while they were in Boundary Bay. Sockeye salmon (Oncorhynchus nerka) is today the most important commercial salmon, weighing about 2.5 kg. Fraser river Sockeye typically spend a year in fresh water and three in salt water, resulting in the wellknown four year cycle (Burgner 1991:95-6; Hart 1973:118-123) with the Fraser River being by far the most important run in B.C. Although sockeye are long distant spawners in B.C. and the most important fish along interior rivers, it is not clear that they were important aboriginally on the coast prior to the invention of the reef-nets (Suttles 1951). This possibility exists because the sockeye do not spawn in small coastal streams and are hard to obtain in the lower Fraser river in the absence of drag nets or gill nets, which have uncertain antiquities. The reef net technology is very specialized (Suttles 1951) and is usually thought to be a relatively recent invention. Coho salmon (Oncorhynchus kisutch) and Steelhead (Oncorhynchus gairdneri) today spawn on all three regional streams, the Nicomekl, Sperpentine, and Campbell Rivers, and Chum salmon Oncorhynchus keta) only in the Campbell River. Coho are larger than Sockeye (average around 3 to 4 kg) and typically spawn between November and January (Groot and Margolis 1991:409). Chum are slightly larger than Coho, averaging about 5 kg in southern B.C. (Groot and Margolis 1991:275) and can spawn even later, even well into the new year (Hart 1973:112-114). They have a lower fat content than the Coho and Sockeye, thus preserve well, and were a favorite salmon of coastal aborigines (Hart 1973:114). It is likely that the two local salmon were more abundant than the Steelhead, but the numbers of fish produced by all three local streams were probably modest. As described later, in addition to salmon, the other really important fish recovered from our excavations were the Starry Flounder (Platichthys stellatus). This fish, known for its tough, scaly skin, is also called “Grindstone”, “Grinder”, and “Emeryboard” It is a right-eyed flounder, usually weighing from 2 to 4 kg at maturity (Hart 1973:631-633). This flounder is known for its tolerance of of low salinities, thus its abundance around the Fraser Delta and other estuaries.. It comes into shallow waters in February and April to spawn but lives in deeper waters most of its life. It is commonly seen in eelgrass beds, as mentioned above, among other places and can be speared. It is relatively abundant around Boundary Bay. The final important fish is the Pacific Herring (Clupea harengus pallasi). This is not now seen as being a different species from the Atlantic herring, and in B.C., usually does not exceed 25 cm in length. This fish is important in aboriginal fishing mainly because of its spawning behavior, as it begins to school in very dense  7  Chap.2, Feb. 15,2008  e Ave. M cB r i d  Excavations Matson 1989/90 Semiahmoo Bay  Ham 1977  St. view  Percy 1972  N  Bay  Ma ple St  .  Trace 1976/77  0  50 metres  Figure II-3. Location of Excavations at the Crescent Beach site. groups adjacent to shore during this time. This occurs mainly in March in B.C. with lesser amounts in February and April (Hart 1975:97), making herring a very good seasonality indicator. Actual spawning occurs at depths between high tide and 11m where eelgrass is one of the main substrates. During spawning large numbers can be obtained by “herring rakes” and spawn can be collected from branches and eelgrass. Although relatively few herring are seen today in Boundary Bay, it is likely substantial numbers were present in the past. Certainly substantial numbers were found in our and in Ham’s (1982) investigations Numerous other fish are also present in the Boundary Bay area, but large numbers of remains of any other single species is absence in archaeological contexts. In total, though, these less common fish to come to a substantial total. In addition to the fish discussed in this section, it needs to be remembered that the plain fin midshipman is also present, although likely obtained during shellfish procurement rather than by standard ‘fishing’ techniques. All in all, the fish resources are one of the most important sources of food found in Crescent Beach deposits. PREVIOUS INVESTIGATIONS The Crescent Beach site has been the focus of several archaeological investigations throughout the past decades because of its large size and the constant threat of development. Of the previous excavation reports available for this site, the three most important are two Master’s theses (Percy 1974, Trace 1981) and one Ph.D. dissertation (Ham 1982). All three excavations took place in different parts of the site as shown in Figure II-3. Percy and Trace’s excavations were carried out under salvage conditions, Percy’s of sewer connections along Bayview Street, and Trace’s, drainage ditches on the other side of the railroad track. The data obtained from their excavations focuses on obtaining information about the artifacts present and from this information, delineating cultural components which at that time were not well known for the study  8  Chap.2, Feb. 15,2008  area, as discussed below. Ham’s 1977 excavations (under Matson’s distant direction and supported by funding from S.S.H.R.C.) focussed on what subsistence information could be obtained from the shells and other faunal remains present within the natural layers within a typical recent Northwest Coast shell midden. As reviewed below, an important part of this endeavor involved experimenting how to excavate natural layers via wide area excavations of shell middens. The cultural history conclusion drawn from these three major excavations was that there were at least four ‘culturally ‘ distinct components present at Crescent Beach. These are, starting from the bottom, St. Mungo/Mayne, Locarno Beach, Marpole, and Late. In all, these four components represent at least four thousand years of occupation and most importantly, almost continuous occupation throughout the time period represented. Furthermore, analysis (Matson et al. 1980; Matson 1989; Matson and Coupland 1995:211-218) had shown that the Marpole component found by Percy, belonged to the Old Musqueam subphase of the Marpole culture, which immediately follows the Locarno Beach phase. It was this evidence of continuous occupation before and after the Locarno Beach phase that led us to excavate the Crescent Beach site further. If we were to begin to try and answer questions about the Locarno Beach culture and its relationship to contingent cultures, being able to investigate these questions at a single geographical location means that factors that are the result of environmental differences can be eliminated (except for environmental changes through time, which have not been thought to be too important in this period). Crescent Beach is the only known intact mainland deposit with both pre-Locarno Beach deposits, Locarno Beach material, and Old Musqueam subphase Marpole material. The three previous major excavations each contributed important information to our research, and these contributions are summarized next. It is important to note that because changing research questions and field methods, we could not simply re-analyze or amalgamate the information gathered from the three major excavations previously done at Crescent Beach in order to answer our research questions. Our research required us to return to the site with a very specific excavation strategy that would allow us to obtain subsistence information not available for the earlier components. Percy’s excavations (in the spring of 1972) took place on Bayview street because a large section of intact midden was going to be destroyed by the creation of a large sewer trench built to accommodate new houses soon to be built in the area and the laterals from it to existing homes (Figure II-3). He had the unenviable task of working directly under the heavy machinery of the Surrey Municipal department and having a very limited time period. Several times while he was working, he had to abandon his trenches and rescue burials uncovered by the city work crews. In his thesis (Percy 1974) ties in these burials with his major trenches, and he also incorporated a description of an extensive artifact collection privately held by a Crescent Beach resident. His excavations uncovered the earliest component present at Crescent Beach, dated to more than 4000 years ago. Based on the artifact assemblage, burial types, and features present, Percy defined this early assemblage as Mayne phase (Carlson 1970) in part because at the time, there was little other information available for this early time period within the Gulf of Georgia region. Two more recent cultural phases were also well represented in his data and these were defined as Locarno Beach and Marpole. Using the standard salvage procedures of his time, Percy excavated in arbitrary 10 cm levels which may have led to some mixing of distinct cultural phases and to a blurring of archaeological cultural boundaries. As typical of salvage excavations of that time, little subsistence information was sought or recovered. Trace’s excavations took place in the summers of 1976 and 1977 (Trace 1981). This was a combined salvage and field school situation, where a University of British Columbia field in 1977 contributed to the material reported by Trace. The excavations took place because the Municipality of Surrey wanted to excavate a series of drainage ditches on the west site the Burlington Northern railway right of way (Figure II-3). Trace’s work at Crescent Beach is important because it proved that there were extensive Locarno  9  Chap.2, Feb. 15,2008  Beach deposits present there, and that the pre-Locarno deposits did not appear to extend to the west side of the railroad tracks. The Locarno Beach deposits from Percy’s work were not as large as those from the preLocarno deposits, so the size and extent of the Locarno deposits was uncertain. Trace worked as much as possible with natural layers and interpreted the basal cultural layers as being interlaced with natural beach deposits (Trace 1981:16). As was not uncommon at the time, he did not attempt a faunal analysis for this project, but instead, focussed on the artifact assemblage. The area in which he worked appeared to have been disturbed by previous land modification, making his analytical task more difficult. Ham’s work, carried out in the summer of 1977, dealt with the youngest deposits present at Crescent Beach, which are dated to the Marpole and Late phases (Ham 1982). From the three excavations it becomes clear that the oldest material are adjacent to the bluffs which run to the east of Bayview Street, and that this is the only place where pre-Locarno material exists. Close to the west side of the railroad tracks, Locarno Beach is the deepest cultural stratum, but it does not exist much beyond that. Further away from the Bluffs, Marpole is the basal stratum, and later material is widely spread. This pattern agrees with the idea of the occupation being near the coast at the edge of the bluff, before the spit existed, and moving north and west as the Crescent Beach spit developed out from the bluff over the last 4500 years or so. Ham’s techniques for and experience in excavating a shell midden and his analysis of the faunal materials and shellfish remains are important to our study because we could adapt his excavation and analytical strategies where the older are deposits present, which are the focus of our work. While Ham’s excavation strategy was useful to our work, we required information concerning an older section of the site than that excavated by him. Therefore, while we have borrowed from his methodology, we could not use the information he obtained to answer the questions posed for this work.  10  Chap.2, Feb. 15,2008   Chapter III EXCAVATIONS IN 1989 AND 1990 AT CRESCENT BEACH H.Pratt and R.G. Matson  We knew from the past research completed at Crescent Beach that there would be adequate preservation of faunal remains from the Locarno Beach and contingent phases. Since no adequate faunal analysis existed for any mainland or Gulf Island Locarno component (Matson and Coupland 1995; Table 61) the faunal remains we recovered at Crescent Beach would help fill in gaps in our knowledge concerning the subsistence base present during a key period in Northwest Coast prehistory, as well as provide information on our specific research questions. The previous excavations had not only supplied us with a general knowledge of Crescent Beach’s cultural chronology but also with information concerning the areas where the different phases were present. We decided the best place for our excavations would be in the vicinity of Percy’s original trenches. This is the area that Locarno Beach and adjacent phases were present. We believed that excavating in close proximity to Percy would facilitate the comparison of our data with his, including correlating the stratigraphy (See Figure II-3 for a map of our excavations vis-a-vis Percy’s). The ability to closely link our excavations with Percy’s was particularly important in that we did not anticipate recovering a large artifact collection and hoped to be able to correlate our stratigraphy with his and thus use his existing collections for the majority of the planned artifact comparisons. Our 1989 excavations ran for four months, from May through August 1989, with the first two months of excavation conducted by the 1989 University of British Columbia’s Archaeology Field School directed by Matson, and two months excavation conducted by a paid crew of nine university students. There was also a public information program running concurrently throughout the four months supported by B.C. Heritage Trust (Holm 1989). This first season of excavation concentrated on two “Trenches” (Figure II -3 and III-1). The area available for excavation was on the railroad right-of-way between the road bed of Bayview Street and the railroad tracks. Furthermore, we were restricted by Burlington Northern how close to the tracks we could excavate to the west and, on the east, by the large sewer pipe that the reason for Percy’s excavation. Therefore, we were narrowly constrained where we could excavate, and the narrow corridor of available intact deposits lay between the trench excavated for the sewer and the limit imposed by the Burlington Northern. Because of the presence of a manhole cover for the sewer we had faith that we knew where the sewer lay, and armed with engineering drawings of the sewer trench, we laid out our excavation units. We planned a wide area excavation of the midden, following Ham. Ham (1982) had problems in following layers across the full four metre width of his excavation. Therefore, we decided on a narrower area of 2 by 6 metres. The idea was that one side of our excavation would be in the sewer trench, which we would dig out so that we would have a preview of the stratigraphy. With these considerations we laid out two trenches of 2X6 metres, one referred to at the “North” Trench (units A,B,C) and the other as the “South” Trench (units D,E,F) (Figures III-1, 2, -3). The same general excavation procedures were followed in both trenches. All excavation was by natural layers, with thick layers crosscut by 10 cm arbitrary levels. The first and every tenth bucket was kept as a matrix sample, while every fifth bucket was washed through one-eighth inch (3 mm) screen and kept as a “shell” sample. All other material was water screened through  1  Chapter III, December 19, 2008  2 Chapter III, December 19, 2008  Figure III-1. Contour map of 1989 and 1990 excavation locations  Burlington Northern  1989 N  100 80 60  Scale 1/250 4.446 Geodetic Metric  0 -10  Railroad  40 60 20  -20  10 -10 -20  Manhole Cover grooved on north side  Stake at end of 75 m baseline  50 m S  L M I K A B C  0 0  5  -20  10 m  5652 Bayview  100  80  -10  0  D  E  F J  0  10  20  G NW  Baseline -10 0  0  -20  Telegraph Pole Stub  25 m S  -40  60  -10  -30  Baseline  40  20  5644 Bayview  Site Datum  Bayview Street  10 20  12 m N  25 m N  10  Stake at end of 75 m baseline  Apparent edge of trench, first visible at 70 cm  J sw nw  Unit Fnw excavated to 260 cm, intact deposits begin approxmately 190 cm  G nw F  Disturbed material west of sewer trench excavated from 45 to 85 cm  sw  Apparent disturbed sewer trench, excavated to 110 cm N magnetic  E sw  se Units D, Esw and Ese excavated to 20 cm  D  Pole Stub 0  1 Site Datum used  2m  Plan View 1989, North Trench Excavations  Figure III-2. Plan View North Trench Excavations Edge of sewer trench at 20 cm  Edge of sewer trench at 80 cm  ne nw  ne  H M 1990 extensions  I  C  se sw ne nw  L  se ne  B  K se sw  Pole Stub  Excavated to 20 cm  se N magnetic  A  Excavated to 80 cm below surface. Disturbed sewer trench 0  1  2m  Plan View, South Trench Excavations  Figure III-3. Plan View South Trench Excavations 3  Chapter III, December 19, 2008  one-eighth inch screen and sorted for lithics, artifacts, and faunal remains. Detailed layer/level notes were kept, contour maps were drawn with each change in stratigraphy and every ten centimetres in the thicker layers. Intact cultural deposits were excavated by quarter units (denoted as sw, se, nw, and ne), so that each 1 x 1m subunit was excavated separately and a complete set of notes and forms kept for each quarter unit. Photographs were taken in both color and black and white. As we were working in an urban area, we had to face the twin problems of preventing vandalism and the safety problem of open pits in an area where people were used to parking their cars. As per our permit with the municipality of Surrey, the units were framed with heavy timbers, and a system of locking heavy pieces of plywood was developed. This resulted in a structure that one could walk over easily, and that would take a considerable effort to defeat, and provided a source of humor for visiting archaeologists, when we “unlocked” the units. This safety feature was more important in the second season, when greater depths were reached. Disturbance was universal in the intial units. In the South Trench on June 13, the northwest 1/4 of H was laid out (Figure III-3) in order to give us a greater east/west cross-section across the sewer trench. This unit was abandoned on July 11 at 80cm below datum, still in disturbed deposits. Within the initial North Trench units, midden disturbance was extreme throughout. The field school did not uncover intact deposits through May and June. At this time, on examining the North Trench units and sewer trench engineering plans, it was decided that sewer trench was much wider than the plans showed. Instead of continuing excavating the entire 2X6 metre trench, we concentrated on the 1X1 metre unit Fnw and proceeded to excavate it by 20 cm arbitrary levels as we determined that this ought to be well outside what was planned for the sewer trench. We continued until almost two metres of overburden and disturbed soil matrix was removed (Figure III-2). At approximately 190 cm we encountered our first intact deposits present in the North Trench. Figure III-5 shows a final plan view of the North Trench at the end of the 1989 field season and Figure III-4, after profiling in 1990. We attempted to excavate the undisturbed strata by natural layers, but this bay mussel dominated deposit was not as well layered as the later deposits in the South Trench. Further inhibiting our ability to distinguish natural layers was the fact that we were digging in a one by one meter unit(Fnw), a classic ‘telephone booth’, with poor lighting. To complicate the excavation even further, within the 70 cm of intact deposit present, two small clay lined depressions as well as an intact burial of a child were encountered (Figure III-8). The burial was left pedestalled, and the excavation of this test pit removed approximately 0.50 cubic metres of undisturbed deposit. Sterile deposits of coarse angular sand were reached at 250 to 270 cm below the surface in the southwest corner of Fnw as shown in Figure III-8. In the South Trench, the original units of A,B,C, turned out to be, not straddling the edge of the sewer trench, but to be within the sewer trench which was much wider here as well as in the North Trench than indicated on the engineering plans (Figure III-3). The fact of disturbance was more obvious than in the North Trench, and a 1x1 metre unit was laid out to the east of unit C (Hnw on Figure III-3). Two more units, I and K, were laid out to the west on July 11, 1989 (Figure III-3) and the edge of the sewer trench was located within them. Unlike the North Trench, intact deposits were located between the sewer trench area and the limits imposed by Burlington Northern relatively close to the surface (Figure III-7). Once I and K were laid out, excavation in the South trench proceeded at a better rate, because the stratigraphic situation became clear very rapidly. Either intact midden deposits were found just below the surface along the entire face of I and K or disturbed deposits indicating the fill of the sewer trench. Once this edge of the sewer trench was located, we excavated within the sewer trench deposits until a substantial exposure of the interface between the intact and sewer trench deposits were encountered, revealed, profiled and photographed. This excavation procedure allowed us to work from within the sewer trench and ‘peel’ 4  Chapter III, December 19, 2008  Cross Section of Feature 9 Feature 9 Fill, BC-H1 and BC-HB  180 190  Shoring  BC-F BC-H1  BC-I  Shell Lense  Orange Ashy Lense  BC-H1  Shoring  BC-H1 Mytilus Midden  Roots  BC-H1  0  190 Ochre Sand Lense Wall Collapse Area  Root  BC-HB Unexcavated  Firecracked Rock  BC-I  180  Clay Lense  BC-HB  Rock  170  BC-F  Orange Ashy Lense  Unexcavated  E  BC-E  BC-I  BC-I  BC-HB  F(sw)  D  BC-F  BC-F  200 centimetres  E(nw)  C  BC-E  BC-E  170  E(sw)  B  10  20  30  40  50  60  70  80  BC-I(s)  90  BC-I1(i)  100 cm  BC-I(s)  200 centimetres  D(nw)  A  N  Figure III-4. Stratigraphic profile of west wall of the North Trench, below 160 cm. back the midden’s layers from our exposed section of intact midden which was 4 metres north/south by approximately 80 cm east/west. This midden material (units Inw, Isw, Knw and Ksw) was excavated by natural layers, cross cut by 10 cm arbitrary levels. Natural layers encountered ranged from two cm to about fifteen cm in thickness. Excavations in intact deposits in the South Trench reached 80 cm below the surface by the end of August. About 3.2 cubic metres of intact midden were excavated. The surface most intact layer was denoted C-L0, and the deepest layer reached in 1989 was layer C-R. The beginning of the 1990 Crescent Beach field season commenced the first week of July, with a paid crew of eight under the direction of Matson assisted by Grant Beattie. Running concurrently with the paid crew was the University of British Columbia’s Field School under the direction of Richard Pearson. The overall direction of the excavation was coordinated by Matson. The paid crew’s first responsibility was the reopening of the South Trench units along with a 4X1 metre extension running directly beside the original units and designated as Units Lse, Lne, Mse, and Mne (Figure III-3). These two expanded units were directly west of the original trench, adjacent to the railway tracks. The old trench was easily re-established because plastic sheeting had been placed over unexcavated deposits before backfilling in 1989. The crew excavated within the sewer trench deposits down to about the one metre mark, further exposing the interface between the intact and disturbed deposits. Once the interface was exposed to the one metre level, the exposed stratigraphy was profiled and the results compared with the stratigraphic profile produced at the end of the field season in 1989. Work commenced on the South Trench with little problem. There was an obvious advantage in being able to work from the exposed stratigraphy, although it was surprising in some units how quickly a layer disappeared as one moved away from the interface into the unknown deposits. We excavated using natural layers, starting with those already delineated in the 1989 field season. The number of layers encountered and excavated in 1990 began with C-L0 in the new L and M units and ended with C-Y. The largest new layer encountered was C-R which was almost 25 cm thick in some areas (Figure III-6). The 1990 excavation procedures followed those already established in 1989. A total of about 15.6 cubic metres of intact midden was excavated in the South Trench during the second year. All units in the South Trench were excavated down to between 110 and 150 cm below the surface including the units comprising sections of the sewer trench. Figure III-6 is a stratigraphic profile of the west wall of units Lse, Lne, Mse, and Mne, along with the north walls of units Inw and Mne, at the end 5  Chapter III, December 19, 2008  ne  nw  220 cm  260 cm  F 220 cm  240 cm  se ne  sw nw  211 cm  210 cm  E 214 cm  220 cm sw nw  N magnetic  se ne  250 cm  220 cm  D 240 cm  220 cm  se  sw  0  1  2m  “260 cm” Maximum Depth BSD of Unit Excavation  Plan View 1990, North Trench Excavations Figure III-5. Plan View North Trench Excavations 1990 of the 1990 field season (see also Figure III-7). Although there were a number of interesting features excavated from the South Trench, they were all identified as hearths (see Chapter VIII for full details). Two of the most completely represented were features 10 and 13. Feature 10 was uncovered in units Inw and Isw, between 80 and 90 cm below the surface in layer C-S, and was a concentration of burned shell of a very light color surrounded by large cobbles. Feature 13 was encountered in the last few days of excavation and is another large hearth full of fire cracked rock. The sewer trench was relatively regular in the region of the South Trench, running almost directly magnetic north, through units I and K (Figure III-3). Instead of the circa 1.5 wide trench with vertical walls shown in the engineering drawings, though, it turned out to be at least 3 metres wide at the top with sloping walls (Figure III-6, 7). The North Trench was reopened by the paid crew who started at the site a few days before the field school. A backhoe operator removed approximately 190 cm of overburden within the boundaries of the 1989 North trench. We knew from the excavation of Unit Fnw in 1989 that the intact deposits were ‘capped off’ by a thick sterile layer of clay (Figure III-4, Layer BC-F). The backhoe operator excavated to the top half of this clay layer (BC-F) over an area of 2 x 6 metres (Figure III-5). Under the supervision of Grant Beattie, a wooden supports and braces were placed into the two metre deep trench in order to provide adequate shoring support for the trench. The Field School was responsible for working in the North Trench through the month of July and half way through August. The first task was the reopening of unit Fnw which had been excavated to more than 260 cm in parts and still contained the pedestalled juvenile burial, all of which was located directly 6  Chapter III, December 19, 2008  30  L SE  10  L NE A  0 10  B  20  CL-0 to CN-2 undifferentiated  30  CM-1+2  70  * CP *CR  CS  80 90  CR-2 CT  *CS  120  CL-0  CL-1  CL-1  CP-2 CN-5  CP-2  CQ-2  CV-2  CT/U CW  *CT  CN-5  CP-3  CL-1 may include CM-1 and CN-N  CV-2 CW  CT/U  C-V  CV  Root Disturbance  Rocks  CV or CW  Unexcavated  Rodent Disturbance  90  CV ? CW  0  20  40  60  100 110 120  CX-1  Feature 13  140  70 80  CT/U  CW  CW  Unexcavated  Shelly Layers  CR  CS  Sand CS variant  CT/U  60  CQ-1  CS  30 40  CN-4  CR  20  50  CN-5 ?  CR CS  Sewer Trench  CV-3 (1989)  CW  130 150 cm  CN-3A  10  B  CQ-1 CS  CT  CL-1  CP-3 CQ-2  CN-5  CQ-1  CR CT  B CL-1  CN-5  0  AG  CL-1  CN-5 CQ-1  10  A  B  CL-0  CP-1  20  I NE A  A  B  B  CM-1+2  CV-2  100 110  CP-1 CQ-1  CN-4  60  CL-0  M NE  M NE  A B  CN-1 to 4  40 50  M SE  B  A  30  NORTH WALL  WEST WALL  20  CY  CX-2 130  140 80  100 cm  150 cm  Firecracked Rocks  Figure III-6. Stratigraphic profile of west wall of the South Trench, 1990. underneath a sheet of plastic laid down at the end of the 1989 field season. Once the burial was removed, Fnw could be profiled and information concerning the stratigraphy could be used to excavate the rest of the units. Figure III-7 is a stratigraphic profile of Fnw, north and west walls, at the end of the 1990 field season. Excavations during 1990 in the North trench concentrated on Fnw, Fsw, Enw, Esw, and Dnw (Figure III-3). There was extensive disturbance in the southern section of the trench in Dsw, and Dse. Dne held the interface between the sewer trench and the intact deposits. Unlike the interface in the South Trench, the north sewer trench interface proved to have a ragged and uneven edge that was a source of some difficulty, but ultimately, we succeeded in locating the edge. It became apparent that the North Trench area had been the location of a large cave-in during the excavation of the sewer trench which explained the wide area of the disturbed area and the lack of intermixture of historic material within the disturbed zone. The edge of  Figure III-7. South Trench, at end of excavation, facing North.  7  Chapter III, December 19, 2008  Unit F - nw west wall  160  north wall  160  BC-E 170  BC-F  180 190  170  BC-F  180  BC-I  190  BC-I  210  200  Shoring  BC-I I(i)  210  BC-I I(i)  220  220  230  Burial Removed  BC-I I(i)  240  230  centimetres  centimetres  200  240  250  250  260  260  Unexcavated  270  270  clay  ash  black soil with shell flecks  matrix with 20% shell  fire-cracked rock  dark matrix with shell  black matrix with shell  fish bone interface  silty sand  coarse yellow sand  outline of burial pit  0  10  20  30  40  50  60  70  80  90 100 cm  Figure III-8. Stratigraphic profile of Unit Fnw, North and West Walls. Fsw  Ene  Enw 205  Artifact  Sewer Trench  BC-1  5 20  21 0  21 5  BG-H 0 22  Ash Fish Vertebrae 20  222  0  Esw  Ese Anvil  B  BC-1 205  Orange Ash 10 Yr 6/8  BG-H  Plywood Anvil  21  5  D  210  Sewer Trench  Dnw Posthole Mold Worked Bird Bone 210  Fish Bone Concentration == ==== == = ==== 5 20  Root Scar  N  0  10  20  30  40  50 cm  Artifact Rock Firecracked Rock  BG-H Ash 200  Posthole molds BG-H, house floor  BC-1  Sewer Trench  Figure III-9. Plan view of Feature 9, showing contour intervals of the floor of Feature 9. 8  Chapter III, December 19, 2008  the sewer trench varied significantly according to depth, and seemed to expand far to the west within Unit D. For this reason, Dsw was not excavated extensively, and Units Dne and Dse were found to be almost entirely within the disturbed area at 200cm below datum, complete with a relatively vertical piece of plywood which apparently was used to shore the original sewer trench (Figure III-9)! The midden deposits were excavated by natural layers and the same procedures were followed as at the south end of the site with all intact material water screened through 3 mm mesh, and the same proportion of buckets and shell samples saved. About 2.5 cubic metres of intact midden were excavated from the North Trench in 1990. After the field school ended in mid-August, excavation in the North Trench continued with other crew members. The designation of layers in the North Trench in 1990 was much easier than in 1989 as there were definite differences exhibited between the natural layers starting with layer BC-H and ending with BC-K. There was some uniformity within these layers in that crushed mussel shell was the dominant shellfish in all of them. Although sterile was reached in unit Fnw, up to 50 cm of intact midden was left in North Trench Units Dnw, Esw, Enw, Ese, Ene, Fse and Fne at the end of the excavation. Figure III-5 is a plan view map of the North Trench showing maximum depths excavated in all units and the intact/disturbed material interface. The most interesting feature from the Crescent Beach 1990 field season presented itself in the North trench and has been designated Feature 9 (Figures III-4 and -9). It is a dense, thick mussel shell layer in a semi-circle shape up to 35 cm thick. The complete outline of the feature was not revealed during excavations. On the outer edges of this feature the inside shelly deposits were differentiated from those layers outside it by the presence of both large cobbles and fire cracked rock which was abundant within Feature 9 (Figure III-5). This semi-circle of fire cracked rock (approximately 3.5 to 4.5 metres in diameter) was too large to be a simple hearth, and the orangy yellow ashy deposits present were localized and did not extend across the feature. The cultural layer present on the outside of the feature did not have the intense shelly nature of the inside cultural layer. During the last few days of the field school two of four possible postmolds were discovered, mapped, and excavated. These two postmolds were less than 10 cm in diameter and one was at least 5 cm deep while the other was at least 4 cm deep. One of the postmolds contained dark soil while the other postmold had a lighter and sandier soil matrix. We believe that Feature 9 is a house floor/living area and it does resemble living floors found and excavated at both the middle component from the Glenrose Cannery site and the early component at the St. Mungo Cannery site (Matson 1976; Ham et al. 1986) but is more similar to small housepits discovered subsequently by Morgan(1999) at Sequim, Washington and elsewhere as described in Chapter