Searching for the Stone Age in the Harbour of Ghent How to Combine Test Trenching and Stone Age Archaeology

Searching for the Stone Age in the Harbour of Ghent How to Combine Test Trenching and Stone Age Archaeology

NotaeSearching Praehistoricae for the Stone 27-2007 Age in : the69-74 harbour of Ghent 69 Searching for the Stone Age in the harbour of Ghent How to combine test trenching and Stone Age archaeology Caroline RYSSAERT, Yves PERDAEN, Wouter DE MAEYER, Pieter LALOO, Wim DE CLERCQ & Philippe CROMBÉ Summary This contribution deals with the difficulties in assessing Stone Age sites within the methodology of current project archaeology in the coversand area of Flanders. A combination of test trenching and auguring is proposed to deal with this problem. Two case studies, Desteldonk - Moervaart-Zuid and Evergem-Kluizendok, both positioned in the harbour of Ghent, are discussed in this paper. Keywords: Stone Age archaeology, methodology, test trenches, auguring, Desteldonk, Evergem, Ghent (B) 1. Introduction ments associated with clay patches, indicative for struc- tured hearths were discovered (Crombé et al., 2004). In the coversand area of Flanders a growing And in these instances the features were protected by a number of the archaeological projects are currently thick peat and clay layer. At the Middle Neolithic site of conducted in a standardized way. The first stage consists Doel-Deurganckdok, only a diffuse scatter consisting of flint of (dis-)continuous test trenching. In the second stage it is and sherds was recorded. No features were found, although decided wither larger excavation areas are to be opened the preservation conditions were similar to the other up, based on the features found in these trenches (e.g. sections. For the Final Neolithic the information is slightly Cherreté & De Clercq, 2007). This methodology has better. Alongside some funerary contexts belonging to the proven its efficacy in detecting sites characterized by Bell beaker culture (e.g. at Sint-Denijs-Westrem - Flanders middle- to low density in soil-features, although compara- Expo, Kruishoutem, Temse, etc…), some rare isolated tive research has demonstrated the dangers for some features have been recorded as for example an elongated periods such as the Early Middle Ages (Hey & Lacey, pit containing a limited number of flint and pottery frag- 2001). However, this method of archaeological investi- ments at Evergem-Kluizendok. Unique was the discovery gations is not well adopted to the detection of Stone Age of a trapezoidal, two-aisled house assigned to the Deûle- sites. The Palaeolithic and Mesolithic record in the cover Escaut group at Waardamme (Demeyere et al., 2004). sand area is largely known by its lithic scatters as little or This limited number of features does not imply that no features are preserved. A small number of possible prehistoric people only seldom constructed houses in the storage pits containing numerous carbonised hazelnut coversand area. Probably the majority of these prehistoric shells, dating from the (Early) Mesolithic, are known from features have been destroyed or blurred due to agricul- Verrebroek - Dok 1, Verrebroek - Aven Ackers and Turnh- ture and/or soil formation processes. With the exception out-Ravelskamp (Crombé et al., 2005; Perdaen et al., 2005; of Doel-Deuganckdok all of the above mentioned examples Van Roeyen, 1990). Another type of feature occurring were found in the C-horizon, on top of heavily truncated occasionally on Mesolithic sites is the so called hearth-pit sand ridges with a partially preserved podzol soil. But (Groenendijk, 1987). Hearth-pits are small circular to also in better preserved contexts, such as at the peat and elliptical features with a homogeneous dark grey to black clay covered sites of Doel, soil processes may have fill coloured by the large amounts of ash and charcoal blurred features; as a matter of fact numerous hearth-pits fragments. Usually they occur in clusters of many tens or only became visible underneath a bioturbated B-horizon. even hundreds of hearth-pits. A the sites of Verrebroek - When these soil formation processes took place remains Dok 1 and Doel-Deurganckdok altogether more han a a question. What we do know is that in many features, hundred hearth-pits have been excavated (Crombé et al., dating from the Bronze Age up till the Roman period, 2005). But even for the Neolithic evidence of structural traces of podzolisation are visible. Therefore it may be features is still very limited. For example at the Final concluded that almost all traces older than the Bronze Age Mesolithic/Early Neolithic sites of Doel-Deurganckdok are erased unless they were dug deep into the C-horizon. only a limited number of accumulated burnt bone frag- But even in the latter cases their visibility remains limited 70 C. Ryssaert, Y. Perdaen, W. De Maeyer, P. Laloo, W. De Clercq & Ph. Crombé and they may pass the archaeologists eye unnoticed. In Desteldonk - Moervaart-Zuid and Evergem- Luckily prehistoric people also left a lot of rubbish behind. Kluizendok palaeotopographical information could be A more adjusted method for the detection of retrieved from the stratigraphical sections within the test these flint scatters could be auguring surveys. This tech- trenches. Instead of the information from the soil map and nique is based on a systematic boring of the surface within the 20 m auguring grid the test trenches were used to a fixed grid, taking samples of the underlying sand matrix detect potential areas for well preserved Stone Age sites. (in this case the podzol) which are consequently sieved So the auguring survey was oriented towards the detection and examined for the presence of minor archaeological of lithic scatters. remains such as chips, charcoal, bone, hazelnut fragments, In addition an attempt was done to find palaeo- etc. (Crombé & Meganck, 1996). When using this method soils on a lower level. To record earlier Stone Age sites it is crucial to sieve the sediment on a fine mesh (maximum at Desteldonk - Moervaart-Zuid and Evergem-Kluizendok 3 mm, ideally 1 mm) and to use a small grid in order to some deep trenches were dug. Deep trenching can only detect the small flint scatters (e.g. Bats 2000-2001, Bats be done in areas where no features have been detected 2007, Crombé & Meganck, 1996, Groenewoudt, 1994). which could be destroyed. It is also important to take An alternative but more time-consuming and destructive into account what kind of developments will be done on method is the use of systematic test pits. Depending on the site (e.g. the construction of a road, buildings, water preservation conditions of the sites and landscape features cistern, etc.). As archaeological surveys are quite often arguments can be put forward for both methods (Bats, planned just in advance of the start of the building 2001; Depraetere et al., 2006). activities, this is necessary in order not to jeopardize the Currently auguring or test pits are only excep- stability in a later stage. tionally applied in project archaeology. A limited knowledge of the Stone Age record within the responsible administration, and so-called economical restrictions are 3. Results the main reason for this. As a result Stone Age sites are seldom discovered. 3.1. Desteldonk - Moervaart-Zuid At Desteldonk - Moervaart-Zuid (East Flanders) 2. Methodology the Havenbedrijf Gent GAB is extending their industry zone. Therefore an archaeological survey was put up to In the two case studies presented in this paper, we detect if sites were present and excavations were necessary. choose to conduct an auguring survey in addition of the Two of the present authors (Wouter De Maeyer & Caroline test trenches. The methodology proposed here is not the Ryssaert) conducted this project (Ryssaert et al., 2007). ideal way to deal with Stone Age sites. It is merely an Philippe Crombé and Wim De Clercq were responsible for attempt of some archaeologists, concerned with Stone the scientific coordination. Age archaeology, who had to deal with the restrictions of The research area is situated on the southwest test trenching. Keeping these remarks in mind, this bank of the Moervaart depression, a late glacial mire attempt has to be seen as a compromise rather than a well which extended over a length of c. 13 km. Although the funded method. Moreover, it is oriented on the detection depression has been known for its numerous Final of relatively recent Stone Age sites (Mesolithic and Neo- Palaeolithic and Mesolithic sites, the research area is lithic), as the detection of deeper lying Palaeolithic sites is situated just outside the main concentration of Stone Age only integrated to a certain limit. sites (Van Vlaenderen et al., 2006; Kerrinkx, 1989). The Traditionally an augering survey proceeds through industrial site of Desteldonk (19 ha) is positioned between three stages. It starts with a study of the soilmap, in order the large sand ridge of Desteldonk and the Moervaart to seek potential areas where Stone Age sites could be River. Besides a few smaller sand ridges, the area is known preserved. For the purpose of a palaeotopographical and as a wet area and is assumed to have been unsuitable for palaeoenvironmental reconstruction borings are affected early occupation. within a 20 m interval grid. Secondly for the strictly The survey started with test trenching. Trenches archaeological purpose a smaller grid is used. Due to the were implanted parallel with the parcel borders and in particularly small surface of dwelling units the interval relation to the local topography every 13 m. Based on the between the boring-points is set to 5 m using a staggered soil map two sand ridges were known, and if possible the triangular grid (Bats, 2007; Crombé & Meganck, 1996; trenches were oriented crosswise over their short sides. Groenewoudt, 1994: 170; Van Gils & De Bie, 2006). The Stratigraphical information was recorded based last stage is off course an evaluation of the sites detected on characteristics seen on the surface. It was also gained (preservation, chronology, spatial lay out).

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