Friday, 23 August 2024

 This post is a contribution by Dr Edward Pollard who was with me on a recent trip to Tanzania as part of a British Council sponsored research grant with the University of Dar es Salaam

Prehistoric animal tracks, Swahili ruins and Climate change in Tanzania


Tanzania has several World Heritage Sites including Ngorongoro Conservation Area, and the rock art at Kondoa, both in the Rift Valley, and the Swahili sites of Zanzibar Stone Town, and Ruins of Kilwa Kisiwani on the Indian Ocean coast. I returned last week from two weeks of fieldwork and training to implement measures to mitigate climate change impacts on heritage sites, one in the north east of Tanzania, the other on the coast. This concentrated on the world-famous Laetoli early hominin footprint trackway, and a recently identified 19th-century slave trade warehouse complex at Winde, on the mainland side of the Zanzibar Channel.

Ngorongoro has the famous volcanic caldera filled with wildlife but also encompasses archaeological and palaeontological sites of Laetoli and Olduvai showing how our ancestors and relatives lived across millions of years. Staying the first week at the Endulen Catholic Mission, about a 27km drive from Laetoli. Breakfast varied between oranges, roast potato, pancakes, soup, chapati (flatbread), mandazi (doughnut), and banana. This was supplemented with some honey bought from local Maasai who have hives hanging from the baobab trees. As part of the conservation area giraffes and zebra were grazing especially near the watering holes every day driving to work. While walking, a warden with a gun had to accompany us, as there are prides of lions presiding over the conservation area. Evidence of elephants recently passing through could be seen by broken trees, dung and stripped bark. Laetoli is about 1,700 m above sea level so was up to 30°C during the day but cold at night needing a warm top. It was the dry season so there were a few mosquitoes, but I still climbed into sleeping bag at night for extra warmth after tucking the edges of the mosquito net under the mattress so nothing bigger than 2mm could get in.

Meeting the first day at the Wardens House for introductions and download of a phone app to digitally capture heritage. The first day involved the visit to the site of the famous early hominin track. The first set of footprints, lying on a cemented ash layer produced by a volcanic eruption and dated at 3.66 million years ago, were recorded by Mary Leakey in 1978. About 40-years later, Fidelis Masao and Elgidius Ichumbaki recorded the second set of footprint a few meters from the earlier recorded site. It is assumed that these were made by Australopithecus afarensis, the same species as the skeleton known as ‘Lucy’, found in 1974 in the Afar region of Ethiopia. The footprints were conclusive evidence that our ancestors were walking upright before brain-size increased.

 


The original track and later footprint discoveries were covered in the 1980s by plastic and basalt boulders to protect them from erosion by people, animals and the rainy season. A new Government sponsored building with a high roof covering the tracks was under construction during my visit with plans to uncover the tracks again to see if they have been preserved. Many tourists leave disappointed because they could not see the footprints, but the animal track layer can be traced intermittently for about 2.5km up the valley, which become exposed and eroded during the rainy season. It was an aim of our visit to map these out making them more widely known that there are more sites to see and explore so visitors can have a more fulfilling experience.



Following the different layers of rock, it was possible to find this animal track layer from over three million years ago in several locations along the valley. Some footprints have such a wide diameter they must be an elephant relative such as a mastodon, but also similar giraffe and buffalo could be recognised. Dust had to be brushed off to fully expose for photogrammetry. One set of marks has been described as footprints of a predator dragging its kill across the mud. Surrounding softer layers have bone beds of ancestors of the modern megafauna including rhino bone, zebra tooth, warthog tusk and rhino bone. Concrete blocks with letters and numbers carved into their surface mark where hominin bones have previously been found.

 


The site is on the slopes of a seasonal river valley where artefacts from a range of different periods can be found including Middle Stone Age (Middle Palaeolithic in European terms) from 300,000 to 50,000 years ago to Late Stone Age beginning 50,000 years ago and pottery perhaps from around 1000 years ago was found at one location. Today the pastoralist Maasai, who arrived around the 18th century, have settlements in the area and often pass by with their goats and cows curious at the visitors.

Lunch at the site consisted of ugali (maize meal), rice, hot chili sauce, and stews made from beef, goat or even the small sprat-like freshwater fish known as dagaa in Swahili. On the first day, still trying to acclimatise myself, I staggered back to room suffering from heat exhaustion. A bucket of hot water for a shower was delivered but it was too late, I had already had my cold one.

Over the week, GPS was used to record positions of bone, worked flakes of quartz, basalt, chert, and quartzite. Electromagnetic Methods of geophysics were tested to find evidence of earlier river channels and springs that could be contemporary with the sites. High-resolution drone imagery mapped the artefacts that were recorded by GPS so future monitoring may be able to identify them as they are exposed over wide areas. After collection, artefacts were 3D scanned back in the Warden’s House.



It was apparent how vulnerable these tracks are being exposed during rainy seasons by channels cutting the beds, waterfalls eroding upriver, and the crumbling of the edges and wearing as people walk across these exposures as they form convenient paths in the dry season. The importance of recording them as they appear and before they are wiped away was evident.


About 45km from Laetoli is Olduvai Gorge. There have been decolonisation initiatives as Olduvai should now be known as Oldupai, the Maasai word for Mother-in-Law’s Tongue or Snake Plant that is common in the gorge. The warehouses at the research laboratories at the Leakey camp have extensive bone collections from previous and continuing expeditions in this area.

The coast

Over the next two days we drove east and south passing the extinct volcanoes Mount Meru and Kilimanjaro, and through the Eastern Arc Mountains. Arriving in the port of Bagamoyo, famous for boat building and being the terminus of the caravan trade in the 19th century. Winde is about 20km north of Bagamoyo. This is the southern area of the Wami Delta, a 20km wide area of coast covered by mangrove swamp, beach ridges, islands and tidal channels that are difficult to navigate without a boat. Surveying the beach ridges, that have grown seaward over the centuries, reveal dense concentrations of pottery, mostly undecorated local earthenware, and stone gravestones dating from the 16th to the 19th centuries. This suggests that there were important industries here in pottery, salt and mangrove poles, and perhaps even slaves and ivory.



The area has not had much investigation until recent studies by Professor Ichumbaki of the University of Dar es Salaam. Parts of a complex of ruins precariously remain on a sand bar between the sea and tidal channels of the delta. It’s remote and difficult to reach location today may suggest smuggling activities to Zanzibar during Colonial rule but we mustn’t underestimate how linked places were by the sea in the past compared to road travel today. Therefore, the ruins today could mark an important port for exporting goods from the mainland to Zanzibar, which lies 35km directly east.

We had to take the two-hour motorboat to Winde as the land route was impassable due to the rainy season extending into June this year, part of the unpredictability in recent years attributed to climate change. Therefore, there were many seasonal lakes that would bog down the vehicles approaching the site. Using the boat, landing was difficult as the delta is exposed to the SW monsoon, which is prevalent at this time of year but there is evidence from the eroding artefacts on the landward side of the site that and the remains of channels that boats may have harboured with the delta estuary. 

Evidence that these ruins were more extensive was that more parts can be found 70m lower down on the foreshore suggesting the beach ridge once extended at least this distance. We also walked past peat deposits on the beach, further evidence that the delta is continuing to erode in the present climate. Glass beads and bottles, European porcelain and gun flints were found eroding on the landward side of the sand bar. Tracks of a hippo disappearing into the mangroves from the ruins made us pause before exploring further though these animals are more likely to be sheltering from the sun in the river channels at this time of day.

 


The evidence of charcoal making can be seen while surveying and the bags of charcoal are stacked close to the channels before being smuggled by boat to Zanzibar. An illegal activity unless the charcoal maker has a permit. Several large fires were seen when surveying as this often lights surrounding vegetation. This deforestation exposes the sediments to extra erosion by rainfall, sea and the tidal channels. We recorded some artefacts at the back of the ruin and looked at the test pit laid open from last year to see if the sand in it was from a tsunami or cyclone.


Much of the site had quickly grown over with grass and shrub since clearing last year so would need clearing again before droning. However, the use of a multispectral drone revealed changes in vegetation that could be anthropogenic features. Coring in the mangroves for evidence of storms over topping the barrier beach was suggested as a method to determine past cyclones and tsunamis that could have affected the site. Unsuccessfully trying to persuade a boat owner to let me paddle a canoe upriver to reach the islands in the delta and examine the stratigraphy in the river cut sections, Richard suggested to bring fold-out canoes next year.

Packed lunch back on the beach consisted of potato, roast meat, chapati and roast banana though ants had found our food and had to be brushed off. For the second day of this, I learnt that washing the ants off in the sea first was more successful than brushing and shaking. The rough journey on the way back resulted in numerous wave soakings and early stages of hypothermia that required the warm hoodie again despite it being about 20°C in the evening. Back in Bagamoyo, the mosquitoes were great in number and not afraid to bite so I grabbed dinner from the table on the terrace and ran inside as the rooms had been sprayed. More coconut is used in the food with fish when the sea is not too rough for fishing. As the team started to leave, data was exchanged, goat was barbequed with pilau and kachumbari (onion and tomato salad).

 The final few days were spent surveying easier to reach sites upriver in the Ruvu and Wami rivers continuing surveys from previous years. Being able to keep lunch of left-over goat and banana in a vehicle saved it from the ants. It is interesting how artefacts become older landward with Chinese porcelain and Late Stone Age flakes and hammerstones suggesting differences in sea level and sedimentation. Cultivation ridges were good to look at as the disturbed soil often brought pottery to the surface. This often led to introductions to and welcomes by the farmers, who I think were hoping I was an investor to bring some development to the village. At one point we came to a quarry where a group of Maasai woman doing the washing in the stream who said they had also have come down from Ngorongoro though I suspect their journey with animals grazing took a lot longer than ours.

To break up the journey on the way to the airport in Dar es Salaam, we stopped at the Kunduchi Ruins that have sacred baobabs and graves, some of which still having the porcelain intact in the pillar tombs. The standing buildings are around 18th century though the pottery indicated occupation here from the late first millennium.



The team, funded by the British Council’s Cultural Protection Fund, involved cooperation between the University of Saint Andrews, University of Dar es Salaam, National Museum of Tanzania, Ministry of Natural Resources and Tourism, Ngorongoro Conservation Area Authority (NCAA), Discovery Programme, and the University of Wales Trinity Saint David.

Dr Edward Pollard

Coastal and Maritime Research Archaeologist

The Discovery Programme: Centre for Archaeology and Innovation Ireland

Unit 2, Merchants House, 27-30 Merchants Quay, Dublin 8, Ireland, D08 K3KD

E-mail: edward@discoveryprogramme.ie

18/07/2024


Thursday, 4 April 2024

 

The Dead Sea, Jordan

I wonder just how many times has the Treasury building at Petra in Jordan featured in Hollywood movies.  Certainly the sight of if appearing as glimpses of rock hewn burnt sandstone from the dark shades of the cooling canyon walls is evocative of a lost past and secrets hidden in the desert.  To get the chance to survey in Jordan was therefore not something I was going to say no to.  Back when I was surveying in Sudan for the director of ACOR (American Center of Research in Jordan), Pearce Paul Creasman asked if I could suggest geophysical methods that might help out with a project he had going at the Dead Sea and what might help to survey sites at Petra.  From his descriptions of both sites and the targets, buried wall features in both, then a combination of electromagnetic, magnetic and GPR were likely candidates.

The first trip was scheduled to investigate the Dead Sea site and to make a recognisance at Petra. The site at Callirrhoe on the Dead Sea has a history of occupation from at least early Roman through Byzantine to periodic Bedouin use in more recent times. 

During Roman occupation it was used as a harbour serving a small village that nestles in the steep hillside to the east.  The village is supplied by a series of fresh water springs outflowing from palaeo-shorelines that extend up the hillside in a series of steps for at least 300m higher than the village.  The port site is now located at -400m elevation, that is approximately 50m above the present level of the Dead Sea.  Previous investigations suggest that the Dead Sea could almost have completely dried out during the last interglacial and with palaeo-shorelines extending some hundreds of meters above present levels then this makes our sea level records up in Scotland look positively pedestrian!

Geophysics

The geophysical investigation objectives included mapping the site for buried wall structures, defining the boundaries of the site and in particular the habour front and mapping spring sites associated with the site.  Previous investigations had uncovered parts of the inshore buildings at the site and shown that these were covered by different types of sediment accumulation.  In the field I was once again joined by my brother, Prof Martin Bates who was to investigate the sedimentation history of the site with respect to the periods of occupation and use and sealevel heights.  The investigation was conducted in conjunction with the Jordanian Department of Antiquities and run as a training program for their staff in geophysics and geo-archaeology.

Ground Conductivity from CMD Explorer, (1mS/m - 2000mS/m)

The main geophysical investigation tool was the CMD explorer.  The results from this are shown below draped on the topographic landscape.  We mapped from the site down the steep slope to the shore of the Dead Sea.  Ground conductivity showed a large variation in values with a rapid increase in conductivity close to the shoreline.  Across the site conductivity varied between 6-20mS/m with consistency in patterns between all three coil separations/penetration depths.  The magnetic susceptibility showed similar trends to the conductivity with variations in value indicating linear anomalies interpreted as the buried and extant wall structures. The geo-archaeological investigations showed a complex history of flooding and water retreat across the site that matched to historical records of sealevel change during the early Roman era.   


Sealevel projected to -400m at approximate height during early Roman occupation

A projection of the ancient sealevel is shown below with a close correlation to the outline of the harbour front as mapped by the geophysics.

The visit to Petra showed the difficulty that it would be in running geophysics in the narrow canyon and expecting any kind of satellite-based positioning. The arid conditions also suggested that the use of GPR might be possible with penetration to significant depths with 250-500MHtz antenna.  A proposal was made to visit the site and run test surveys early in 2024.  We did return and I will write on this later.

Tuesday, 6 June 2023

Cardigan Bay Mesolithic Landscapes Re-visited


Combining work with fun is a common theme on many of these pages and so my latest travels are once again in that vein.  A few years ago we undertook a small seismic sub-bottom survey in Cardigan Bay to see what the potential was for mapping buried and submerged land surfaces.   In a similar situation to Doggerland, the west coast of the UK also hides secrets of past landscapes that our early ancestors used.  Mapping these however has been at a slower pace than in the North Sea mainly due to the lack of hydrocarbon exploration data and more recently the slower uptake of offshore wind.  Research undertaken by Aberystwyth University (Rob Wittington et al) and the BGS does give us some clues to the situation through sub-bottom records and some deep boreholes.

Our data from 2018 With the Irish Marine Institute and the Celtic Explorer identified a complex landscape from which I was able to speculate on a series of possible geographical models for the time periods from early Mesolithic to today (in press, Europe’s Lost Frontiers: Vol II).

Coastal geographies and positions of major river and associated archaeological sites. A: Early Mesolithic, 10,000 cal yrs BP. Sites 0: Aberdaron; 1: Pencilan Head; 2: Y Bryn;  3: Afon Wen; 4: Aberystwyth; 5: New Quay; 6: Newport; 7: Pencaer.  

These models were based on the limited seismic data that we had acquired, the old seismic data and some limited boreholes. Using the boreholes I created a function to adjust the present day bathymetry with the seismic mapped river/estuaries and a different function for the land that fell between them.  Sarah Boyd provided palaeo-sealevels from PhD research and tidal regimes were derived from the work of James Scourse.  Armed with these we now needed to test against new seismic and ground truth data.

Teaming together with Dei Huws from Bangor Uni we used a sub-bottom profiler to acquire new data during a particularly calm period in late May.  We used the 13m ketch Ivilia for the survey and she proved a stable platform for 24hr ops.


 


New survey lines were acquired north of Aberdovey down to NewQuay.  The fidelity of the sub-bottom data was far higher than the earlier information from the Celtic Explorer but the major horizons match nicely. The major palaeo-channels that parallel the coast offshore were confirmed and showed more complexity than we had originally been able to see.  As always, the more you look, the more complex the history becomes. Tying these to the onshore story is going to be quite a challenge.

Bully (Prof Martin Bates) has been working the onshore side of this paleo-reconstruction game on the West coast of Wales for many years with a particular focus on the forest site at Borth. Here many finds, including some impressive antlers record very different environments back through hundreds to thousands of years.

The new data will allow us now to better target key locations with the palaeo-geography and to acquire higher density seismic and ground truth data. Out there somewhere will be sites with key evidence of what the people were doing.  Just got to keep looking for them.

Sunrise over Cardigan Bay - a sight that I have rarely seen

Wednesday, 12 April 2023

Hunting Pyramids in Sudan

 Hunting Pyramids in Sudan

Over the past few years I have worked with a number of TV companies on shows that have highlighted the use of geophysics for archaeological investigation.  One of the most fun teams that has presented me with some of the greatest challenges to the use of both land and marine geophysics is led by Josh Gates at ExpeditionUnknown.  In his long-running series that airs on the Discovery Channel he has allowed me to run various geophysics in Dwarka (India), Namibia, and at various sites around the UK.

Early this year Josh asked if I would join him for a project in Sudan trying to find a lost pyramid.  Now you would think that it would be pretty hard to lose a pyramid, but it turns out that this might not be the case.  Pyramids are sometimes only partially completed or sometimes never really get beyond the foundations. They are often robbed of material to build other structures, let alone that they weather over time in the harsh desert environments where they are typically found.

The Nubian pyramids in Sudan were built by rulers of the Kushite kingdom from 1000BCE to 300AD.  While they have similar forms to those of Egypt the Sudan ones tend to be steeper sided and are constructed mainly out of the local coarse sandstone bedrock. The focus of this research project was the site of Nuri where it is thought that once over 80 pyramids may have stood marking the tombs of the royals from around 670BCE to 310BCE. The oldest, that of Taharqa (690-664BCE), a pharaoh of the 25th Dynasty of Egypt and King of the Kingdom of Kush stands 50m tall and appears to contain a pyramid within a pyramid as seen from the stones eroding from the summit.  



One of the most interesting projects running at the site currently is led by Dr Pearce Paul Creasman who has an intrepid team of divers who are excavating the tomb of Nastasen.  Diving you may well ask?! Yes, because the nearby waters of the Nile and recent dam projects have caused the ground water level to increase to the point of flooding the tombs.  While I resisted the temptation of joining them (Josh did not) in zero visibility water that contains bits of old pharaoh my task was to find evidence for both the pyramid within a pyramid for Taharqa and also to search for a pyramid of a known king which could not be accounted for. 

For the task at hand in such dry conditions then ground penetrating radar was the tool of choice but since those who know me will also know I never trust just one technique, and especially if that is GPR. So, I also took along the trusty CMD Explorer electromagnetic ground conductivity meter as well.

The GPR was a Mala system with a 250MHz antenna.  Normally this should have been adequate in a dry, sandy environment to penetrate to at least a few meters.  I surveyed lines with a spacing of no more than 1m between lines and for most of the site a spacing of 0.5m between lines to form dense grids. An example of the results for a grid in front of the most northerly pyramid is shown below.  


Here you can see the sides of the tunnel stairway to the burial tomb close to the surface where it begins to descend.  While the edge is visible  the data shows the relatively limited penetration of the radar. This was curious and all I can think is that the wind-derived sand from the local coarse bedrock has winnowed the grains to leave a large proportion of the heavy metal minerals thus inhibiting the radar signal.

The results of the EM across the site showed much more promise.  The tomb entrances stand out clearly in the conductivity and magnetic susceptibility signatures against the backdrop area.  Interesting results were also obtained over a large flat and open area between the upstanding pyramids. The data here was consistent with there being a tomb entrance and foundations for a pyramid but clearly one does not exist – it is postulated that the missing pyramid was never built beyond the tomb and foundations. I hope that the dig team on site under the direction of Dr Pearce Paul Creasman will open up some test trenches to prove this in the near future.  

A cross section walked over the top of Taharqua’s pyramid also revealed the encased structure within the pyramid and now all that needs to happen is to extend this survey over the whole structure.

The survey, and especially the diving will be fully featured by Josh later this summer so watch out for the next program as part of Expeditions Unknown and pay careful attention to my new survey vehicle with its 1dp (donkey power) engine!



Wednesday, 5 April 2023

Croatia 2023

 The drowned landscapes off Croatia

I visited Croatia a number of years ago after diving on some of the submerged Roman sites in Greece and seeing the Temple of Serapis in Naples (https://upload.wikimedia.org/wikipedia/commons/9/9e/Charles_Lyell_-_Pillars_of_Pozzuoli.jpg) . The temple is geologically infamous as the front piece to Charles Lyell’s seminal work The Principals of Geology where he notes the mark of marine boring organisms at some height up the columns thus indicating that they were once submerged.  He correctly interprets this as representing tectonic movements that have caused both a submergence and subsequent re-emergence of the temple since its construction in the late first to early second century AD. Contemplating the potential for drowned landscape reconstructions around the Mediterranean and Adriatic seas I briefly looked for papers describing sea level changes.  These were almost entirely absent from the academic literature.  Fast-forward to 2023 and I am here on the invite of Dr Simon Fitch (Bradford University) as part of his Future Leaders project. The idea is to map paleo-landscape surfaces in the many rias (drowned river valleys) along the Adriatic eastern shore. 

Split, Croatia
The project in Croatia is partnered with Dr Vedran Barbarić at the Faculty of Humanities and Social Sciences, University of Split and the first trial survey was undertaken on board the Pram, expertly skippered by the enthusiastic and knowledgeable captain Jerko Macura . For the acquisition we had chosen to use an Innomar Quattro parametric sonar (https://www.innomar.com/products/multi-transducer/quattro-sbp).  This hull-mounted sonar is configurable as either a line of four transducers emitting separate signals for high-resolution 3D type survey or as a block of four transducers working together for greater power and thus sea floor penetration.  The unit was side-mounted together with a Novatel IMU GNSS unit to provide heave corrections.  

Innomar Quatro with Novatel dual antenna motion reference unit

Over the course of 5 days we surveyed a number of small bays, outlets to the main large bays, channel crossings and both large and small deltas.

The weather cooperated for the most part until the Bora winds (a sever katabatic northerly wind from the shore) stopped play on our last day. The survey exceeded our expectations with penetration to greater than 15m sub-bottom in water depths up to 70m deep.  The seismic reflectors and character demonstrated sequences that could be interpreted as eroded bedrock, basin sediment infill, channel cuts, deltaic progression with periods of both regression and transgression. 

Channel entrance to the old harbour of Split

The potential for mapping multiple palaeo-landscapes and associated environments is huge. We now need a program to accomplish this that has ground truth from coring and careful modelling.  The project has only just begun so here is looking forward to returning and working with a great team.


Friday, 23 September 2022

Electric storms and digital stones: technology reveals the hidden secrets of stone circles on the Isle of Lewis

 Calanis - Beneath the Peat 2019-2020



Over the past few years we have been going to the Calanais site in Lewis, Scotland to try to map parts of the Neolithic landscape that are hidden today.  Rolling back the clock to over 5000yrs ago means that we have to consider significant changes in the landscape that include agricultural practice and natural changes such as the prolific growth of peat across the islands.  Further, there are have been changes associated with coastal position following the rise in sea level to present day heights. The Calanais Virtual Reconstruction Project is a joint venture led by the University of St Andrews with the Calanais Visitor Centre and the University of Bradford. The project team has been surveying the satellite sites near the Tursachan, the main prehistoric stone circle at Calanais. The surveys have revealed evidence for lost stone circles, buried beneath the peat and we have also used this data to create digital reconstructions that will allow visitors to virtually “walk” around the stones.

One rarely visited site surveyed known as Site XI or Airigh na Beinne Bige, consists of a single stone on an exposed hillside overlooking the whole valley and a couple of kilometres directly north of the Tursachan.  At the site we conducted a range of geophysics including electromagnetic ground conductivity mapping, electrical resistivity tomography, surface resistivity, magnetic gradiometry, and also used handheld magnetic susceptibility sensors to measure both the upstanding stone and to take measurements on the local rock exposures. The magnetic gradiometry revealed that the single stone was originally part of a circle of standing stones but that many of these are now buried by the thick peat deposits.


Magnetometry data at Site XI. Red columns indicate features interpreted as the position of lost stones. At the centre of the rough circle of smaller anomalies is a massive, star shaped feature which has resulted from a historic lightning strike

The gradiometry also revealed a very unexpected result – that of a star-shaped magnetic pattern right at the heart of the stone circle. This massive, star-shaped magnetic anomaly in the centre of the circle we believe to be the result of a single, large lighting strike or many smaller strikes on the same spot.

Such clear evidence for lightning strikes is extremely rare in the UK and the association with this stone circle is unlikely to be coincidental. Whether the lightning at Site XI focused on a tree or rock which is no longer there, or the monument itself attracted strikes, is uncertain. However, this remarkable evidence suggests that the forces of nature could have been intimately linked with everyday life and beliefs of the early farming communities on the island.

The project is now studying more archaeological sites in the area around the Tursachan, the main stone circle at Calanais. There are at least a dozen stone circles in the area, but at many sites the stones have fallen and become buried beneath the blanket peat that covers much of the landscape over the millennia. 

A view of the 3D model created by the computer science team at the University of St Andrews under Dr Alan Miller can be seen at https://vimeo.com/273858929.

At site X, also known as Na Dromannan the fallen stones sit on a hill overlooking the main valley.  Here careful scanning of the stones allowed a full 3D model of the site to be built. The virtual recreation allows the passage of the sun and moon around this circle to be tracked for the first time in four millennia. Now, anyone can virtually visit this remote site and get a real sense of what it was like just after it had been constructed. 

You can read a full account of the geophysics is given here:

Geophysical investigation of the Neolithic Calanais landscape Bates, C. R., Bates, M., Gaffney, C., Gaffney, V. & Raub, T. D., 11 Dec 2019, In: Remote Sensing. 11, 24, 2975.

https://www.mdpi.com/2072-4292/11/24/2975

Thursday, 22 September 2022

Durrington Pits – monumental structures in the Stonehenge landscape 2020

The pandemic provided some unusual opportunities and for me this was especially marked in the Stonehenge landscape by the absence of hordes of visitors.  This allowed a reuniting of brothers in survey, Vince and Chris Gaffney from Bradford University together with my brother, Martin from University of Trinity St Davids. We were joined in our field campaign by Eamonn Baldwin from Birmingham and my colleague Tim Kinnaird from St Andrews. The focus of our attention was a series of curious features seen on the magnetic gradiometer survey data. The features were evident as over 20 separate 10-20m diameter circles arranged in a concentric pattern around the Durrington Walls.  Fieldwork and analysis revealed evidence suggesting that they were massive shafts, measuring more than 5 metres deep. The circle formed by the shafts encloses an area greater than 3 square kilometres around the Durrington Walls henge, itself one of Britain’s largest henge monuments, and the famous, smaller prehistoric circle at Woodhenge.

Figure 1. Shaft locations surrounding Durrington Walls.

 Geophysical investigations included electromagnetic ground conductivity surveys, magnetic gradiometer, ground penetrating radar and electrical resistivity tomography.  The results of ground penetrating radar as a series of time slices are show in in figure 2.

 


Figure 2 Anomaly 8A – 250MHz antenna: Ground penetrating radar time slices at 10cm depth intervals, decreasing L–R from ground surface (top left) down to approximately 3.3m depth (bottom right).

Coring of the shafts provided radiocarbon and Optically Stimulated Luminescence dates suggesting these features are Neolithic and were excavated more than 4500 years ago, around the time that Durrington Walls was constructed.  The shafts may have served as a boundary to a sacred area or precinct associated with the henge. The Neolithic period, which is associated with the first farmers in Britain, is characterised by the development of ornate, and occasionally very large, rituals structures and enclosures, including the great stone circle at Stonehenge. However, no comparative prehistoric structure in the UK encloses such a large area as the circle of shafts at Durrington, and the structure is currently unique. 

 


Figure 3. Coring the sites with a mini-percussion corer

Aside from the scale of the structure, the circuit of shafts has other surprising characteristics. The boundary appears to have been deliberately laid out to include an earlier prehistoric monument within the boundary - the Larkhill Causewayed Enclosure. This site was built more than 1500 years before the henge at Durrington. This distance between the henge and earlier enclosure, more than 800 metres, seems to guide the placement of shafts around Durrington.  The evidence for how these pits were laid out is extremely important as it implies that the early inhabitants of Britain used a tally or counting system to track pacing across long distances (Figure 4).  Evidence for such careful planning, at such a scale, is unexpected at such an early period and emphasises how important the positioning of these pits was.


Figure 4. Least cost pathway analysis showing the use of pacing to mark out location of the pits.  They are further distance away down slope than parallel to slope

Archaeologists believe the effort invested in the great circle inscribed by the pits reflects an important  cosmological link between these two ritual sites, and that the large shafts were dug to record what must have been an important, sacred boundary.  The presence of these massive pits, and perhaps an internal post line, guided people towards the religious sites within the circle or even warned those who were not permitted to cross the boundary marked by the shafts.

Research on the pits at Durrington was undertaken by a consortium of archaeologists led by the University of Bradford as part of the Stonehenge Hidden landscape Project, and with the Ludwig Boltzmann Institute for Archaeological Prospection and Virtual Archaeology, the universities of Birmingham, St Andrews, Warwick, Trinity Saint David (university of Wales), and the Scottish Universities Environmental Research Centre (University of Glasgow).


Animation illustrating the landscape setting of the Durrington pit group, major monuments and the average distance from Durrington Walls to identified features as a line.

© Crown copyright and database rights 2013 (OS Profile DTM Scale 1:10000); EDINA Digimap Ordnance Survey Service (100025252) http://digimap.edina.ac.uk

To read more on this project:

Gaffney, V. et al. 2020 A Massive, Late Neolithic Pit Structure associated with Durrington Walls Henge, Internet Archaeology 55

https://intarch.ac.uk/journal/issue55/4/index.html


Notes

The universities undertaking field research supporting this press release included the University of Bradford with the Ludwig Boltzmann Institute for Archaeological Prospection and Virtual Archaeology the universities of Birmingham, St Andrews, Trinity Saint David (University of Wales), Warwick,, and the Scottish Universities Environmental Research Centre.  The work was undertaken a part of the Stonehenge Hidden Landscapes Project and brought together experts in non-invasive geophysical prospection and remote sensing, and specialists in British prehistory and landscape archaeology in order to carry out research in one of the most important archaeological landscapes  in Europe. The outstanding geophysical survey and visualization capabilities of the team has been made possible only because of the unique expertise and combined resources of the wider project partnership. an international collaboration of the Ludwig Boltzmann Gesellschaft (Austria), Amt der NiederösterreichischenLandesregierung (Austria),the University of Vienna (Austria), the Vienna University of Technology (Austria), ZAMG– the Central Institute for Meteorology and Geodynamics (Austria), Airborne Technologies (Austria), 7reasons (Austria), ÖAW– Austrian Academy of Sciences (Austria), ÖAI – Austrian Archaeological Institute (Austria), RGZM Mainz – Römisch‐GermanischesZentralmuseum Mainz (Germany), the University of Birmingham in collaboration with the University of Bradford (GB), Arkeologerna of StatensHistoriskaMuseer (Sweden), NIKU – Norwegian Institute for Cultural Heritage (Norway), and Vestfold fylkeskommune – Kulturarv (Norway).