Tag Archives: ERT

THaWS 2016. A Late Start and Sediments Beyond the Temple of Ay and Horemheb

So another season of survey and augering is under way at Thebes. The Theban Harbours and Waterscapes Survey has, for the past 5 years, been using geoarchaeological and geophysical survey to study the changing floodplain of the river Nile, and the dynamics between the ancient harbours and waterways and the Theban temple complexes on the West Bank and Luxor and Karnak temples. In 2015 the survey work focused on the areas around Kom El Hetan and the Ramesseum, with Electrical Resistivity Tomography profiles and auger locations running from the edge of the floodplain to the modern course of the Nile. In addition an area survey was conducted over the mounds at Malqata, associated with the harbour of Birket Habu. This year the season is focussing its attention on the floodplain between the colossal seated statues of Amenhotep III and his huge ceremonial lake (Birket Habu), immediately to the east of the funerary temple of Ay and Horemheb.

 

Sunrise over the Nile floodplain as viewed from the West Bank

Sunrise over the Nile floodplain as viewed from the West Bank

 

After a slight delay at the start of the project for permits, the work commenced on 19th January. Reconnaissance of the area to the east of the temple, looking for a route across the floodplain for both ERT and auger locations, was conducted last autumn and walked over by the team as we waited for our paperwork to be completed.

The aim of the transect of boreholes (hand augering and a percussion coring) and geophysical survey (Electrical Resistivity Tomography (ERT)) is to understand the geoarchaeological history of the floodplain in this area of Thebes. We are using our RTK GPS to establish the location of the ERT profiles and to survey in borehole locations during the course of the work.

Carolin Johansson (Medelhavsmuseet, Stockholm) setting up the GPS base station

Carolin Johansson (Medelhavsmuseet, Stockholm) setting up the GPS base station

 

Carolin conducting GPS survey along an ERT traverse

Carolin conducting GPS survey along an ERT traverse

 

As the ERT survey was set up and continued to collect data across the floodplain from west to east, the team also attempted some GPR. However, issues with the equipment meant that no survey could be completed, and this will have to wait until later in the season. The augering got off to a flying start, with boreholes starting immediately east of the temple of Ay and Horemheb and supported by the ERT profile data. The coring and hand augering both revealed the variation in the sediments from the desert edge, running east across the floodplain, with different depths of silts and sands.

 

Ben Pennington (University of Southampton) removing sediment from the auger head assisted by Mohammed

Ben Pennington (University of Southampton) removing sediment from the auger head assisted by Mohammed

 

Dominic Barker (University of Southampton) gets to grips with a corer sample

Dominic Barker (University of Southampton) gets to grips with a corer sample

 

Jan Peeters (Utrecht University) recording sediments from Auger site 71 in the West Bank floodplain with the Theban hills in the background and assisted by Moustapha (auger) and Hassan (sitting) and onlooked by Zazou, who is working on the ERT profile behind them

Jan Peeters (Utrecht University) recording sediments from Auger site 71 in the West Bank floodplain with the Theban hills in the background and assisted by Moustapha (auger) and Hassan (sitting) and onlooked by Zazou, who is working on the ERT profile behind them

 

Willem Toonen (Aberystwyth University) working at auger site 67 with Youssef and Ahmed in front of the funerary temple of Ay and Horemheb with Medinet Habu immediately south (in the background)

Willem Toonen (Aberystwyth University) working at auger site 67 with Youssef and Ahmed in front of the funerary temple of Ay and Horemheb with Medinet Habu immediately south (in the background)

 

The work with the augers was matched by the pace of the ERT, with resistivity data being collected along a traverse completed in four separate profiles, measuring over 2.7km in length. This traverse is located to complement the borehole data and the ERT data collected in the traverse to the east of the Ramesseum in 2014 and 2015, allowing comparison of the varying resistivity values from both locations.

 

Zazou, Ahmed, Reis Alaa and Sumara take a well-earned rest while the ERT collects data

Zazou, Ahmed, Reis Alaa and Sumara take a well-earned rest while the ERT collects data

 

As with many field projects, in some cases the work in the field marks only a part of the overall effort. Once the geophysical survey data is collected, and the auger samples are bagged or put into plastic tubes, the hard work of data processing and study of the augered samples begins. After a week of work, the whole team was called on to soak, sieve and pick through the sediments, weighing and measuring the different inclusions in the sediment to glean as much information about the nature and chronology of the floodplain sediments as possible. This data will be compared with the geophysics to help ground-truth the data and provide crucial information of the potential date of different deposits.

The preliminary data is already pointing to some interesting results on the deposition of sediments deposits, and their relationship with the West Bank monuments. There is still lots of processing and studying to be done!

 

Bird’s eye view of clasts from sieved samples drying and then being sorted from the borehole sediments

Bird’s eye view of clasts from sieved samples drying and then being sorted from the borehole sediments

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The Portuslimen Project. Geophysical Survey and Fieldwalking at Ephesus

One of the more constraining factors of geophysical survey in an archaeological context is the potential difficulty in dating or phasing anomalies in the data. Although hard science forms the main component of survey work, there is a large subjective element involved in the interpretation of geophysical survey data, which ultimately can decide the nature, function and phase of features. Our interpretation sometimes belies the complexity of the archaeological remains in question (issues relating to survey resolution and the nature of deposits can affect this) and this is particularly true of the different phases of construction and occupation at a site. Complementary information on the phases of deposits represented in geophysical survey data can be provided through surface collection and recording over the survey area, and this integrated approach to archaeological survey is particularly pertinent to the recent Portuslimen survey conducted at Ephesus.

In August and September of 2015 a small team of archaeologists from the University of Southampton travelled to Ephesus in Turkey, to take part in the season of fieldwork run by the Österreichisches Archäologisches Institut (ÖAI). The ÖAI has conducted archaeological research at Ephesus for 120 years (http://www.oeai.at/index.php/grabungsgeschichte.html ), and for the last 16 years has conducted geophysical survey across the site, with work directed by Dr Sirri Seren of the Central Institute for Meteorology and Geodynamics (https://www.zamg.ac.at/cms/en/news). The Portuslimen team were invited to look at some very specific areas of the ancient site and landscape, namely the areas of the inner and outer Roman harbours, and the surrounding landscape of the river. The aim of the survey was to add to the areas already surveyed by the ÖAI, and to address the development and possible phasing of the harbour complexes of ancient Ephesus. The team comprised the author, together with Dominic Barker, Ben Urmston, Jack Pink and Jack Frowde.

Panoramic view of the area of the outer harbour and river as seen from the promontory

Panoramic view of the area of the outer harbour and river as seen from the promontory

 

Magnetometry being undertaken at the inner harbour

Magnetometry being undertaken at the inner harbour

To address these aims the team utilised fluxgate gradiometers, with gridding out and topographic survey conducted using an RTK GPS. Magnetometry was used in a field to the east of the inner harbour of Ephesus, and in fields around the outer harbour and river channel, also on the promontory overlooking the outer harbour.

In addition Electrical Resistivity Tomography (ERT) profiles were conducted at sites along the northern edge of the river channel, across the area of land between the outer harbour and river, and in the area of the floodplain to the north of the inner harbour. These were designed to assess the nature of the deeper sediments associated with the geoarchaeology of the landscape, for comparison with the borehole data collected by the University of Koln.

Although the geophysical survey techniques were deemed appropriate for the conditions of the site, the broad geographical range of the different survey areas,and the potential variations in phasing for the different results, presented the team with a problem; how to recognise the different periods of occupation in these areas, together with an idea of the character and function of many of the structures. To address these issues, fieldwalking was undertaken over each of the survey areas., utilising the grid set out for the geophysics, and using each of the survey markers as the central point for an area of surface material to be collected and recorded within a a 3m radius.

 

Set out of the survey grid using an RTK GPS

Set out of the survey grid using an RTK GPS

 

ERT survey to the north of the river channel

ERT survey to the north of the river channel

 

Surface collection to the north of the river channel, using the RTK GPS and note-taking

Surface collection to the north of the river channel, using the RTK GPS and note-taking

 

The method of sampling allowed collection of all pottery, with a record of presence and absence of CBM (? meaning )and building material. The collection of surface ceramics provides the diagnostic sherds necessary for establishing the type and chronology of the vessels, while its total collection over a small but standard sample area make it possible to calculate the count and weight of sherds and, thus, the potential ceramic density density in each area.

The results of the survey not only provided some excellent information about structures and port infrastructure in the different areas, but also provided some useful spot-dating of the potential phases of occupation of the areas. On the promontory overlooking the outer harbour a number of pit and gully features were found in the geophysical survey results, matching other surface evidence for Archaic settlement pre-dating the Roman harbour. The results of survey to the north and west of the outer harbour indicated large structures associated with the port, dating to the Roman and Late Antique periods. Finally the survey results to the north of the modern river channel detected structures and a possible canal that, when compared to the surface collection, seem to represent Late Roman and Byzantine phases of the port of Ephesus.

 

Location of surface collection points across the 2015 survey area

Location of surface collection points across the 2015 survey area

 

Roman amphora bases located to the west of the outer harbour

Roman amphora bases located to the west of the outer harbour

 

The results of the season are only preliminary, and further work needs to be undertaken on the data and at the site to fully understand the complexities of the changing harbours of Ephesus. However, a pattern is emerging which seems to indicate a gradual shift in the development of port infrastructure, with activity moving from the inner and outer harbours between the early Roman and Late Antique periods, to a later complex to the north of the modern river between the Late Antique and Byzantine periods. The evidence for pre-Roman occupation in the area is also of interest.

There are obvious caveats about the methodology that we have applied to the site, such as the depth of potential deposits and the nature of material exposed at the surface, which will ultimately affect the dating of material to particular periods of occupation. However, the combined strategy of surface collection and geophysical survey does provide us with a more nuanced data-set than with geophysics on their own, and has already started to raise interesting questions relating to the development and use of this fascinating port complex.

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The Portuslimen Project. Geophysical survey at Tarragona, and the constraints of modern urban areas

Over the past few months of field survey, work has swung around to a series of projects lined to Roman ports in the Mediterranean. In June and July I headed back for a season of excavations at Portus, and in August and September geophysical survey at the site of Ephesus in Turkey (more on this in a future post). In October and November work has commenced on a geophysical and topographic survey of the Roman port area of the town of Tarragona in Catalonia, Spain. The work, together with that of Ephesus, forms part of the Roman Meditteranean Ports (RoMP) project, or Portuslimen (http://portuslimen.eu/). A component of this project involves the survey of a number of port sites, to understand the form and extent of these sites, and help analyse the ways in which they may have functioned through time. The work at Tarragona is being conducted in collaboration with colleagues from l’Institut Català d’Arqueologia Clàssica (ICAC).

 

The modern port of Tarragona, with its harbour, docks and factories

The issue with Tarragona is that the development of the town and port spans from the pre-Roman period, to the establishment of the Roman town in the third century BC, to Late Roman and Visigothic settlement in the 6th, 7th and 8th centuries, and later Islamic influence. Over this time the town and its port expanded and contracted, and archaeological deposits were buried under fluvial deposits from the Francolí river to the west of the port. Later post-medieval expansion of the town, particularly in the 19th and 20th centuries saw much of the Roman and later port built over, and a new harbour constructed over the remains of the ancient port. The aim of our survey is to attempt to locate significant structural remins of the Roman port and harbour through intrusive methods. The good news is that a number of areas in the city have been excavated in the past 40 years, which helps in the location of the survey to gain as much as possible from the efforts. The bad news is that, due to the modern town plan, many of the survey areas are constrained by modern buildings and infrastructure. Thus our work has to use some specific techniques to conduct survey in the areas that are available. This includes topographic survey and location of survey grids using RTK GPS and total station survey, and use of GPR and ERT along streets and in plazas to map buried remains.

Set up of the GPS and GPR by the University of Southampton team in the Placa dels Carros

Set up of the GPS and GPR by the University of Southampton team in the Placa dels Carros

 

The GPS base station collecting static data for the survey

The GPS base station collecting static data for the survey

 

Fortunately for the University of Southampton team, the open plazas of the town provided sufficient space for static data to be collected by the GPS base station, and for a series of preliminary stations to be established using the GPS. Where the streets became narrow a total station was used to establish further stations in a traverse around the port area of the town.

Geophysical survey s far has focused on 500MHz GPR, propagating 3-4m below the modern street level to find the buried archaeology. In some of the streets in the northern part of the port area, particularly along the roads close to the Roman baths and theatre a number of walls and other features are visible. As the survey progresses southwards, however, modern infrasructure such as manhole covers, and the nature of the made-up ground close  to the modern harbour, make the results more difficult to interpret. The restrictions in terms of spatial coverage have also provided a challenge in terms of data interpretation.

Total station survey in one of the streets of Tarragona

Total station survey in one of the streets of Tarragona

 

500MHz GPR survey in one of the plazas

500MHz GPR survey in one of the plazas

 

To better understand the geoarchaeology of the site we have been applying Electrical Resistivity Tomography (ERT) to record both archaeology and deeper deposits in the town. The main constraint with this is that the paved areas of the town preclude the use of survey probes (these cannot be dug through cement and Tarmac). Thus we have had to adapt using a system of electrode copper conductors and a conductive gel. Most surfaces will allow an electrical current to be passed through them, but asphalt and Tarmac act as insulators, meaning that for the ERT to work long stretches of cement pavement need to be surveyed.

A conductor formed from crocodile clips, wire and pipe end copper usually used for plumbing.

A conductor formed from crocodile clips, wire and pipe end copper usually used for plumbing.

The ERT profile being conducted adjacent to the Roman theatre

The ERT profile being conducted adjacent to the Roman theatre

 

In spite of our initial misgivings, the conductors and gel, with the ERT equipment, have proved to work very well indeed. The profile alongside the Roman theatre has revealed a number of areas of walls and rubble aligned adjacent to the excavated theatre remains. The team hope to conduct a long profile of ERT in the southern part of the modern port which, together with the boreholes of Ferreol Salomon, will investigate the nature of the harbour deposits.

The survey work is being conducted until 15th November, and there are many features of the topography of the ancient harbour that remain to be discovered, including the line of the Roman seafront and mole.

The bay to the east of the port

The bay to the east of the port

 

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Between the Desert and the Nile. Theban Harbours and Waterscapes

The West Bank of Thebes

The West Bank of Thebes

Back in 2011 the Theban Harbours and Waterscapes Survey (THaWS) started with a field season of geophysics. This Egypt Exploration Society project (www.ees.ac.uk), directed by Dr Angus Graham,  was established with the aim of using different techniques to study the settlements and temples on the east and west banks of the Nile, and how they relate to the changing floodplain and river. Unfortunately the season had to be aborted after the 25th January revolution, and the survey was postponed to the 2012 season, when the fieldwork progressed at a cracking pace.

After five years of the project a large quantity of survey data, together with sedimentary data from auger samples, has been collected and is pushing forward some tentative interpretations about the archaeology and geomorphology of the area. Fieldwork in areas as diverse as Malqata, Birket Habu and the floodplain in front of Kom El Hetan and the Ramesseum has provided food for thought on the depth of ancient ground levels and the organisation of the waterways on the West Bank, with interesting results from some of the East Bank work, including Karnak.

For the 2015 season the fieldwork has shifted up a notch with a larger and more diverse team. The plan was to run different geophysical survey techniques, while also continuing the auger sample strategy and processing of samples from the 2014 and 2015 seasons. Work has very much focused on Electrical Resistivity Tomography (ERT) surveys on the West Bank, particularly in the area to the east of the Ramesseum heading up to the current course of the Nile, with Ginger Emery working on the instrument. This has been complemented by an intensive season of auger work conducted by Ben Pennington and Willem Toonen, to investigate changes in the sediments represented in the ERT.

ERT survey under way on the West Bank

ERT survey under way on the West Bank

Auger work along ERT profile 32, West Bank

Auger work along ERT profile 32, West Bank

The survey has allowed a solid dataset to be collected running from c.600m to the east of the Ramesseum all the way the the modern banks of the Nile, with the resistivity and auger data integrating to allow some more nuanced interpretations of the development of the floodplain and the presence of possible man-made canals to be ascertained. The work in this area relates closely to the function of temples further to the south between the Birket Habu and the Ramesseum.

ERT profile running at the foot of the Colossi of Memnon, Kom El Hetan

ERT profile running at the foot of the Colossi of Memnon, Kom El Hetan

This week we have focused the work in the area of Kom El Hetan. Previous seasons provided information on the axis of theTemple of Amenhotep and the possible presence of channels associated with the temple. The aim this week has been to expand on this information with more intensive ERT and Ground Penetrating Radar (GPR) survey in the area.

ERT survey at Kom El Hetan

ERT survey at Kom El Hetan

Hopefully by the end of the week we will have a series of close (5m) profiles of ERT data to model, and GPR data at 0.5m intervals across the front of the Colossi, in the first court, and in the third court for comparison, with a second plan to conduct more GPR profiles in the fields to the south to detect the possible enclosure of the temple. It promises to be an exciting week.

There have been trials and tribulations in the fieldwork, including negotiations with landowners, and issues with the burning of sugar cane chaff during the first two weeks. There have also been compensations, not least in the form of tea and cake, the latter being provided by the wife of Sumara, one of our workmen.

Burning sugar cane chaff promises to engulf the ERT equipment

Burning sugar cane chaff promises to engulf the ERT equipment

Husam cuts the cake provided by Sumara's wife. One of the perks of fieldwork in Egypt!

Husam cuts the cake provided by Sumara’s wife. One of the perks of fieldwork in Egypt!

The fieldwork will be carrying on at Thebes until 1st April. However, results from the previous seasons of work are presented in the last three editions of the Journal of Egyptian Archaeology, and in other papers listed below. Happy reading!

 

Graham, A. and Strutt, K. 2012, The Theban Harbours and Waterscapes Survey. Recent Fieldwork to Investigate the Canals and Harbours on the West and East Banks at Ancient Thebes (Luxor), Egypt. The Newsletter of the International Society for Archaeological Prospection 31, April 2012, 6-7.

Graham,A., Strutt, K., Hunter, M., Jones, S., Masson, A., Millett, M., Pennington, B. 2012, Reconstructing Landscapes and Waterscapes in Thebes, Egypt. In Journal for Ancient Studies eTopoi, 3, 135-142.

Graham, A., Strutt, K.D., Hunter, M. , Jones, S., Masson, A., Millet, M., and Pennington, B.T. 2012, Theban Harbours and Waterscapes Survey, 2012. Journal of Egyptian Archaeology 98, 27-42.

Graham, A. and Strutt, K. 2013, Ancient Theban Temple and Palace Landscapes. In Egyptian Archaeology 43, Autumn 2013, 5-7.

Graham, A, Strutt, K., Emery, V.L., Jones, S. and Barker, D. 2014, Theban Harbours and Waterscapes Survey, 2013. The Journal of Egyptian Archaeology 99, 35-52.

Graham, A. and Strutt, K. (forthcoming), Ancient Theban Temple and Palace Landscapes. Egyptian Archaeology. Journal of Egyptian Archaeology 100.

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Blog Catch-up #1: Archaeology and Survey in the Nile Delta at Naukratis

Due to commitments in the field over the last month or so it has proved difficult to keep up to date with the blog. Now seemed like a good time to produce a few posts to highlight some recent fieldwork and site visits, starting with a recent survey at Naukratis. In May 2014 I conducted geophysical survey at this archaeological site in the Nile Delta. The Naukratis fieldwork project is directed by Ross Thomas of the British Museum, and seeks to assess the surviving archaeology of this important ancient site using a range of complementary methods including topographic and geophysical survey, in addition to borehole survey and excavation, as part of a larger project directed by Alexandra Villing of the Greek and Roman department of the British Museum called ‘Naukratis: Greeks in Egypt’.

Magnetometer survey being conducted to the east of Kom Ge'if

Magnetometer survey being conducted to the east of Kom Ge’if

 

The season in May (the third season of fieldwork) added to the existing dataset from the first two seasons in 2013, mapping the extent of the ancient settlement and its association with the Canopic Branch of the River Nile.

The port of Naukratis was the earliest Greek port in Egypt, established in the late 7th century BC as a base for Greek (and Cypriot) traders and the port of the royal Pharaonic city of Sais. It was an important hub for trade and cross-cultural exchange long before the foundation of Alexandria and continued to be significant through the subsequent Ptolemaic, Roman and Byzantine periods. Previous fieldwork was conducted by Flinders Petrie amongst others, and concentrated on excavation of the central areas of the ancient town. Further research was required to fully understand this very important archaeological site. For this season, the magnetometer survey of the site was continued in the fields surrounding the modern village.

Two ERT profiles were also undertaken using an Allied Associates Tigre ERT. The first of the profiles ran from a point some 400m to the west of the site, over the kom or mound, to a point 400m to the east of the site, incorporating the line of the Canopic Branch of the Nile and Naukratis. This provided a section 15m deep running west-east across the southern part of the site. The main aim was to better understand the geological relationship between the river and the settlement, and to tie the profile in with the series of borehole surveys conducted along the same traverse.

 

Mohamed Roshti assisting with the ERT survey on the kom

Mohamed Roshti assisting with the ERT survey on the kom

The survey work at Naukratis has produced significant new data on the layout of the ancient town, its local environment and hinterland, including the location of the Greek sanctuary complex, the Hellenion, and the Temenos or temple enclosure at the site. The magnetometer results located a large number of mud brick and stone structures in the fields around Kom Ge’if, particularly in the north and east of the site. In addition to the plan of the ancient town, the magnetometer results also give us a much better idea of the extent of the ancient site in relation to the location and development of the Canopic branch of the Nile, which ran to the west of the ancient settlement. The magnetometry clearly shows the change from settlement to canal infilling, with structures positioned along the edge of the canal. This data is reinforced by the results of the ERT survey. The depth of deposits underlying and surrounding Kom Ge’if is suggested by the topography, with a sharp contrast between the kom and the surrounding fields. The remains of the ancient site are present, if buried, but life in the modern village of Kom Ge’if carries on. The village, with its new mosque, stands out from the surrounding floodplain, a mixture of bean fields, and brown ploughed and saturated fields prepared for planting melon. A number of venerable sheikhs’ tombs stand out on the fringes of the village. The local shepherd crosses from field to field, allowing his sheep and goats to graze on the stubble remaining from the wheat harvest, and manuring the fields in the process, then herds the flock back through the winding streets of Kom Ge’if.

 

Detail of survey results from Naukratis

Detail of survey results from Naukratis

Many of the areas of the ancient settlement still require surveying using magnetometry, and a combined strategy of ERT survey with drilling of boreholes will provide useful comparative data for particular parts of the site and its hinterland.

Shepherd leading flock to feed on cut fields

Shepherd leading flock to feed on cut fields

Donkey transport for the ERT

Donkey transport for the ERT

 

More information on the fieldwork at Naukratis can be found on the project website at: http://www.britishmuseum.org/research/research_projects/all_current_projects/naukratis_the_greeks_in_egypt.aspx

Also, you can discover more about the artefacts recovered from Naukratis by visiting the Online Research Catalogue at:

http://www.britishmuseum.org/research/online_research_catalogues/ng/naukratis_greeks_in_egypt.aspx

 

Sunset over Kom Ge'if

Sunset over Kom Ge’if

This post is a reworking of an article recently published in the International Society for Archaeological Prospection (ISAP) Newsletter for May 2014.

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Electrical Resistivity Tomography on the Isola Sacra

Further to my last post, the week before last was spent with a team from the British School at Rome carrying out a single Electrical Resistivity Tomography (ERT) profile across part of the Isola Sacra, designed to complement the magnetometer survey of the area, and recent coring undertaken by Ferreol Salomon.

IMAG0924

The Necropolis di Porto, showing the Via Flavia, between Portus and Ostia Antica. The ERT survey was carried out in an effort to cover the area of the necropolis, ancient road and dune cordon along the Roman coastline, together with the features including a large canal to the east of the necropolis

The profile ran from the westernmost point of the Necropolis di Porto in a north-east direction along one of the principal trackways of the Isola Sacra, along the edge of the fields established by the bonificazione of the area. Levels of readings were taken down to a depth of 7m to match the sediments recorded in Ferreol’s cores. The short field season highlights a useful way of targetting features found in the broader blanket survey of the landscape to aid our understanding of the depth and nature of features located in area datasets. Alice James and Matt Berry from the British School at Rome assisted in the survey on the ground, and are now hard at work processing this data and ERT data from some other projects conducted in the Autumn.

IMAG0906

ERT survey probes running alongside the fencing of the necropolis looking west.

IMAG0918

The profile along the trackway to the east of the necropolis. 180m were covered in total.

A preliminary look at the survey data shows that the tombs of the necropolis are indicated as high resistivity anomalies, although the road surface is not clear – perhaps indicating the robbing out of paving – and a high resistivity surface of material is visible running across the landscape to the east.

IMAG0907

Data collection using the Tigre and laptop. Some battery life issues curtailed the work on the first day, although the heads-up imaging of the data as it is collected is useful in the field.

The data further to the east, in the area of the canal, is more difficult to assess on the basis of a cursory glance. The high resistivity readings near the surface have a double break in them, correlating approximately with the canal width. However, the sandy infilling sediment, and the sandier subsoil in the area, coupled with waterlogging across the survey area, has made visualisation of the canal profile difficult. Further processing and clipping of the data may give a clearer indication of the canal profile, and its relationship to the nectropolis and Via Flavia to the west.

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Geophysics at Karnak – Intensive GPR survey and the beginning of the end of the survey

The latest work on the THaWS project has been marked by the intensity of survey profiles and survey areas covered, and  the fact that the team have been working almost exclusively in and around Karnak temple. The transition of the GPS survey from the West to the East Bank went smoothly, as reported in the last post. We established a base station on the roof of Chicago House on the West Bank, with the very kind permission of the staff. Some wonderful views were visible across the Nile to the banana plantation and desert edge on the West Bank, andthe set-out made survey convenient for the work at Karnak.

Sarah setting up the base station

Sarah setting up the base station

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