Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex NGR: 532938 104787 (TQ 32938 04787) Scheduled Ancient Monument: 1010929 ASE Project No: P106 ASE Report No. 2014165 By John Cook BSc (Hons) AIFA May 2014 The Whitehawk Community Archaeology Project Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 Abstract Archaeology South East along with Brighton and Hove Archaeological Society undertook a detailed fluxgate gradiometer survey on Whitehawk Camp, Brighton, East Sussex. The survey took place between Monday 28th April and Friday 2nd May 2014. Despite the magnetic ‘noise’ encountered the magnetic survey at Whitehawk Camp has successfully indicated possible archaeological features. The most significant features noted in the survey were possible ditches and linear areas of magnetic debris that corresponded to the causewayed enclosure. The magnetic debris and disturbance relating to the previous use of much of the site as both allotments and a dumping ground has served to potentially obscure any archaeology. However, the more modern magnetic material has also highlighted the lines of the causewayed enclosure. Two linear areas of magnetic debris in the north of the race course and a linear positive anomaly in the south west of the survey may relate to further circuits of the enclosure. However, these anomalies may also relate to features associated with track maintenance and the previous use of the site as allotments. Statement of Indemnity Geophysical survey is the collection of data that relate to subtle variations in the form and nature of soil and which relies on there being a measurable difference between buried archaeological features and the natural geology. Geophysical techniques do not specifically target archaeological features and anomalies noted in the interpretation do not necessarily relate to buried archaeological features. As a result, magnetic and earth resistance detail survey may not always detect sub-surface archaeological features. This is particularly true when considering earlier periods of human activity, for example those periods that are not characterised by sedentary social activity. © Archaeology South-East UCL i Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 CONTENTS 1.0 INTRODUCTION 2.0 SURVEY METHODOLOGY 3.0 GEOPHYSICAL SURVEY RESULTS 4.0 CONCLUSIONS Bibliography Acknowledgements Appendix 1: Raw survey data (CD) Appendix 2: Section 42 License HER Summary sheet OASIS Form Figures Figure 1: Figure 2: Figure 3: Figure 4: Figure 5: Figure 6: Figure 7: Figure 8: Figure 9: Site location Plan showing areas of magnetometer survey Raw data southern viewport Raw data northern viewport Processed data southern viewport Processed data northern viewport Interpretation southern viewport Interpretation northern viewport Plan showing geophysics interpretation over previous work © Archaeology South-East UCL ii Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 1.0 INTRODUCTION 1.1 Site background 1.1.1 Archaeology South-East, with the assistance of members of the Brighton and Hove Archaeological Society (BHAS), conducted a Magnetometer survey on a site totalling approximately 8 hectares on land at Whitehawk Camp, East Sussex hitherto referred to as ‘the site’ (NGR.TQ 32938 04787; Fig.1). The work was undertaken as part of the wider 'Whitehawk Community Archaeology Project' funded by an 'Our Heritage' grant from the Heritage Lottery Fund (HLF). 1.1.2 Permission for the work was given by Paul Roberts, Inspector of Ancient Monuments, English Heritage under a Section 42 License to use a metal detector and/or geophysical survey, as defined by the Ancient Monuments and Archaeological Areas Act 1979. A copy of the licence is attached to this document in Appendix 2. 1.1.3 Permission to undertake the work was also given by the landowner Brighton and Hove City Council via Robert Walker, Head of Operations, City Parks. 1.2 Geology and topography 1.2.1 According to the British Geological Survey (2014) the site lies predominately over bedrock geology of Newhaven Chalk Formation. No superficial deposits are recorded. 1.3 Aims of Geophysical Investigation 1.3.1 The purpose of the geophysical survey was to detect any buried archaeological anomalies that might provide a measurable magnetic response. The specific aims of the project were to investigate whether the Neolithic causewayed enclosure of Whitehawk Camp extends beyond the known extent and to assess the site for further work to be carried out as a part of the HLF funded scheme. 1.4 Scope of report 1.4.1 The scope of this report is to report on the findings of the survey. The project was conducted by John Cook and John Hurst with assistance during fieldwork from BHAS members Jon Baczkowski, John Funnell, Joan MacGregor, John Skelton, Eddie Start, Peter Tolhurst and volunteers. The Maria Gardiner and the fieldwork volunteers also took part in an office based training course on processing geophysical survey data following the completion of fieldwork. The project was managed by Jon Sygrave. © Archaeology South-East UCL 1 Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 2.0 SURVEY METHODOLOGY 2.1 Geophysical survey 2.1.1 A fluxgate gradiometer (magnetometry) survey was undertaken in the areas depicted in Figure 2 (NGR 532938 104787). 2.1.2 The field work was undertaken between Monday 28th April and Friday 2nd May 2014 when the weather was warm and dry. 2.2 Applied geophysical instrumentation 2.2.1 The Fluxgate Gradiometer employed was the Bartington Instrumentation Grad 601-2. The Grad 601-2 has an internal memory and a data logger that store the survey data. This data is downloaded into a PC and is then processed in a suitable software package. 2.2.2 30m x 30m grids were set out using a GPS (see below). Each grid was surveyed with 1m traverses; samples were taken every 0.25m. 2.2.3 Data was collected along north-south traverses in a zigzag pattern beginning in the south-west corner of each grid. 2.3 Instrumentation used for setting out the survey grid 2.3.1 The survey grid for the site was geo-referenced using a Leica Viva Smartrover. The GPS receiver collects satellite data to determine its position and uses the mobile phone networks to receive corrections, transmitting them to the RTK Rover via Bluetooth to provide a sub centimetre Ordnance Survey position and height. Each surveyed grid point has an Ordnance Survey position; therefore the geophysical survey can be directly referenced to the Ordnance Survey National Grid. 2.4 Data processing 2.4.1 All of the geophysical data processing was carried out using TerraSurveyor published by DW Consulting. Minimally processed data was produced using the following schedule of processing. Due to the very high positive readings of some of the magnetic disturbance the values were replaced with a dummy value so as to avoid detrimentally affecting the dataset when further processed. The first process carried out upon the data was to apply a DESPIKE to the data set which removes the random ‘iron spikes’ that occur within fluxgate gradiometer survey data. A ZERO MEAN TRAVERSE was then applied to survey data. This removes stripe effects within grids and ensures that the survey grid edges match. Figures 5 and 6 display the processed survey data. 2.5 Data presentation 2.5.1 Data is presented using images exported from TerraSurveyor into Autocad software and inserted into the geo-referenced site grid. Data is presented (Figures 3-6) as raw data and processed data greyscale plots. © Archaeology South-East UCL 2 Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 3.0 GEOPHYSICAL SURVEY RESULTS (Figures 7-9) 3.1 Description of site 3.1.1 The survey area consisted of approximately eight hectares currently used as public amenity land and a race course. 3.2 Survey limitations 3.2.1 There were a number of physical obstructions encountered on site. Including metal fences, footpaths and significant amounts of fly tipped waste. Obstructions are noted in the results. Areas where physical obstructions form a barrier to survey, or a health and safety issue, have been omitted. 3.2.2 In addition to the physical limitations of the survey, the effectiveness of magnetometer surveys depends on a contrast between the absolute magnetic susceptibility of the topsoil to the underlying subsoil (Clark 1996). Features may also be difficult to detect where there has been significant primary silting. 3.3 Introduction to results 3.3.1 The results should be read in conjunction with the figures at the end of this report. The types of features likely to be identified are discussed below. 3.3.2 Positive Magnetic Anomalies Positive anomalies generally represent cut features that have been infilled with magnetically enhanced material. 3.3.3 Negative Magnetic anomalies Negative anomalies generally represent buried features such as banks or compacted ground that have a lower magnetic signature in comparison to the background geology. 3.3.4 Magnetic Disturbance Magnetic disturbance is generally associated with interference caused by modern ferrous features such as fences and service pipes or cables. 3.3.5 Magnetic Debris Low amplitude magnetic debris consists of a number of dipolar responses spread over an area and is indicative of ground disturbance. 3.3.6 Dipolar Anomalies Dipolar anomalies are positive anomalies with an associated negative response. These anomalies are usually associated with discreet ferrous objects or may represent buried kilns or ovens. 3.3.7 Bipolar Anomalies Bipolar anomalies consist of alternating responses of positive and negative magnetic signatures. Interpretation will depend on the strength © Archaeology South-East UCL 3 Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 of these responses; modern pipelines and cables typically produce strong bipolar responses. 3.3.8 Thermoremanence Thermoremanence is most commonly encountered through the magnetizing of clay through the firing process although stones and soils can also acquire thermoremanence. 3.4 Interpretation of fluxgate gradiometer results (Figures 7 and 8) 3.4.1 The survey area assigned for geophysical survey was situated on the crest of a southward running spur of down land ranging from gentle slopes to steep undulating ground with the road of Manor Hill running through the site. 3.4.2 Evidence for possible archaeological features in the form of discrete moderate positive anomalies representing possible cut features are noted in a small number of places. However, due to the ‘noise’ created by modern ferrous material the possibility of discrete features being obscured is not discounted. In addition to these, linear moderate positive anomalies (A1) indicating possible ditches are noted. Several of these appear to align with the upstanding remains of the causewayed enclosure. Additionally, a linear anomaly is observed running across the southern section of the race course (A2) which may represent land division prior to the current race course. 3.4.3 The most significant anomalies noted within the survey data are of areas of magnetic debris. It is likely that most of these anomalies relate to modern material in the near surface caused by ground disturbance or dumping of waste material. However, some linear areas of magnetic debris (A3) were observed to correspond with the causewayed enclosure. It is likely that these anomalies represent where the monument ditches have filled with more modern material and does the most to highlight the form of the monument within the data. Other linear areas of magnetic debris were noted crossing the racecourse in the northern extent of the survey (A6). 3.4.4 A possible thermoremanent anomaly (A4) is observed in the south of the race course. This anomaly may be indicative of kilns, furnaces, ovens or other heating activity. However, the anomaly noted here correspond to a section of the causewayed enclosure previously excavated and therefore may relate to the process of backfilling. 3.4.5 Bipolar anomalies with associated magnetic disturbance (A5) are observed both across the race course and in the south east of the monument. These anomalies correspond to below ground services such as a pipes and cables. 3.4.6 A scattering of dipolar anomalies across the area may represent archaeological features such as kilns or ovens, but more likely they indicate discrete ferrous objects. These anomalies are not individually marked due to number. © Archaeology South-East UCL 4 Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 4.0 CONCLUSION 4.1 Discussion 4.1.1 Despite the magnetic ‘noise’ encountered, the magnetic survey at Whitehawk Camp has successfully indicated possible archaeological features. The most significant features noted in the survey were possible ditches and linear areas of magnetic debris that corresponded to the causewayed enclosure. The magnetic debris and disturbance relating to the previous use of much of the site as both allotments and a dumping ground has served to potentially obscure any archaeology. However, the more modern magnetic material has also highlighted the lines of the causewayed enclosure. Two linear areas of magnetic debris (A6) in the north of the race course and a linear positive anomaly in the south west of the survey may relate to further circuits of the enclosure. However, these anomalies may also relate to features associated with track maintenance and the use of the site as allotments. Magnetometry does not specifically target archaeological features and anomalies noted in the interpretation do not necessarily relate to buried archaeological features. The technique may not always detect sub-surface archaeological features. This is particularly true when considering earlier periods of human activity. Therefore, areas where archaeology may not have been interpreted may also need to be ground truthed. Acknowledgements Archaeology South-East would like to thank the Heritage Lottery Fund for funding the work, Brighton Racecourse for access and use of facilities, Brighton and Hove City Council for agreeing to the survey and all the volunteers from Brighton and Hove Archaeological Society who helped. © Archaeology South-East UCL 5 Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 Bibliography BGS 2014 British Geological Survey, Geology of Britain Viewer, accessed 12.05.2014. http://mapapps.bgs.ac.uk/geologyofbritain/home.html Clark, A. 1996. Seeing Beneath the Soil. (2nd edition). London: Routledge. © Archaeology South-East UCL 6 Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 SMR Summary Form Site Code Identification Name and Address County, District &/or Borough OS Grid Refs. Geology Arch. South-East Project Number Type of Fieldwork Type of Site Dates of Fieldwork Sponsor/Client Project Manager Project Supervisor Period Summary - Whitehawk Camp, Brighton, East Sussex Brighton, East Sussex 532938 104787 Newhaven Chalk Formation P106 Eval. Excav. Green Field Eval. Shallow Urban Excav. HLF Jon Sygrave John Cook Palaeo. Meso. AS MED Watching Brief Deep Urban WB. Standing Structure Other Neo. PM BA Other Modern Survey Other 5th – 9th May 2014 IA RB 100 Word Summary. Archaeology South East along with Brighton and Hove Archaeological Society undertook a detailed fluxgate gradiometer survey on Whitehawk Camp, Brighton, East Sussex. The survey took place between Monday 28th April and Friday 2nd May 2014. Despite the magnetic ‘noise’ encountered the magnetic survey at Whitehawk Camp has successfully indicated possible archaeological features. The most significant features noted in the survey were possible ditches and linear areas of magnetic debris that corresponded to the causewayed enclosure. The magnetic debris and disturbance relating to the previous use of much of the site as both allotments and a dumping ground has served to potentially obscure any archaeology. © Archaeology South-East UCL 7 Archaeology South-East Detailed Magnetometer Survey at Whitehawk Camp, Brighton, East Sussex ASE Report No:2014165 Appendix 1 Included on C.D 1. 2. Raw Magnetometry Data Positive and negative trace plots © Archaeology South-East UCL 8 N 106000 105000 The Site 104000 Contains Ordnance Survey data Crown copyright and database right 2014 © Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC 534000 533000 0.5km 532000 0 103000 Whitehawk Camp Site location Fig. 1 N 533170, 104930 Ma no rH ill R oa d 533170, 104640 532820, 104440 533070, 104440 Reproduced by permission of Ordnance Survey on behalf of HMSO. Ordnance Survey Licence no. AL 503 10 A Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC Whitehawk Camp Fig. 2 Plan showing areas of magnetometer survey N 10nT 0nT -3SD mean 0 3SD 50 m -10nT Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC Whitehawk Camp Fig.3 Geophysics raw data southern viewport N 10nT 0nT -3SD mean 0 3SD 50 m -10nT Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC Whitehawk Camp Fig.4 Geophysics raw data northern viewport N 7nT 0nT -3SD mean 0 3SD 50 m -7nT Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC Whitehawk Camp Fig.5 Geophysics processed data (south) N 7nT 0nT -3SD mean 0 3SD 50 m -7nT Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC Whitehawk Camp Fig.6 Geophysics processed data northern viewport N A3 A1 A5 A5 A3 A3 A2 A5 A5 A4 A5 A1 A5 A5 Moderate positive anomaly (Possible archaeology) Weak positive anomaly (Possible archaeology) Moderate negative anomaly Weak negative anomaly Magnetic disturbance Magnetic debris Dipolar/Bipolar anomaly (Modern) Thermoremanent anomaly Linear anomaly land drain/former field boundary Linear positive anomaly possible agricultural origin Area positive anomaly possible agricultural origin A1 0 Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC 50 m Whitehawk Camp Fig.7 Geophysics interpretation southern viewport N A6 A5 A1 A3 A1 A5 A5 A3 A3 A2 A5 A5 Moderate positive anomaly (Possible archaeology) Weak positive anomaly (Possible archaeology) Moderate negative anomaly Weak negative anomaly Magnetic disturbance Magnetic debris Dipolar/Bipolar anomaly (Modern) Thermoremanent anomaly Linear anomaly land drain/former field boundary Linear positive anomaly possible agricultural origin Area positive anomaly possible agricultural origin A4 A1 A5 0 50 m A5 Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC A5 Whitehawk Camp Fig.8 Geophysics interpretation northern viewport N 533170, 104930 Ma no rH ill R oa d 533170, 104640 532820, 104440 533070, 104440 Archaeology South-East Project Ref: P106 Report Ref: 2014165 May 2014 Drawn by: JC Whitehawk Camp Fig. 9 Plan showing geophysics interpretation over previous work Sussex Office Units 1 & 2 2 Chapel Place Portslade East Sussex BN41 1DR tel: +44(0)1273 426830 email: fau@ucl.ac.uk web: www.archaeologyse.co.uk Essex Office The Old Magistrates Court 79 South Street Braintree Essex CM7 3QD tel: +44(0)1376 331470 email: fau@ucl.ac.uk web: www.archaeologyse.co.uk London Office Centre for Applied Archaeology UCL Institute of Archaeology 31-34 Gordon Square London WC1H 0PY tel: +44(0)20 7679 4778 email: fau@ucl.ac.uk web: www.ucl.ac.uk/caa