It’s the start of week 2 of the excavation and in Area I excavation of the palaeosol is well underway: a series of samples have been taken for laboratory analysis, and the excavation team are now carefully troweling through this former landsurface. A number of exciting finds have already been made!
Meanwhile in Area III, steady progress is being made: 10 cm spits of sediment are being dug, bagged and moved to the sieving area for processing.
Preparations are also underway for future planned work. Rain threatens and the forecast is not good for the next 24 hours!
Peter Hoare explains some unusual features of the Breckland landscape that are best seen from the air.
Across substantial regions of the modern world, winters are sufficiently cold to freeze the ground to a depth of several metres, but complete thawing takes place during the following summer. In periglacial regions, with their significantly harsher conditions (mean annual air temperature <−2ºC), long-term freezing may create so-called permafrost that is hundreds of metres deep; ca 60% of Russia, 50% of Canada, 23% of China and 90% of Alaska are underlain by permafrost. Here, summer temperatures are only sufficient to melt the top few metres, forming an active layer. Alternate freezing and thawing of the active layer rearranges the component sediments, and may also disturb the bedrock surface if it is sufficiently shallow. Under these conditions, patterned ground is formed.
Throughout much of the East Anglian region known as Breckland (which includes Barnham East Farm), Upper Cretaceous Chalk bedrock lies within 2.5 m of the ground surface; its upper part is frost shattered (brecciated) and this material is often overlain by windblown (aeolian) coversand and other thin sediments. Large areas of Breckland display inactive or ‘fossil’ patterned ground, consisting of stripes and cellular (often polygonal) forms, indicating that active layer processes took place in the past. Polygons are commonly ca 10 m in diameter; they grade into stripes, which are spaced ca 7.5 m apart, on slope angles of between ca 1° and 6°.
Shallow-lying patterned ground is evident at the surface because vegetation responds to variations in subsoil characteristics (particle size, pH, depth, moisture content, etc.) created by periglacial processes. Crop- or scorch-marks such as those seen in the photograph were especially clear during the long spell of hot and dry weather in the summer of 2018. Every other Breckland stripe is underlain by coversand with a pH of <4.5 (acidic) and heather thrives; Chalk bedrock lies close to the surface beneath the intervening stripes, the soil pH is >8 (alkaline) and grass flourishes.
In the most recent study of the Breckland patterns (Boreham & Rolfe 2016–17), the authors concluded that Devensian (MIS 2) frost cracks developed into what they termed ‘tiger’ stripes; solifluction played its part in drawing material downslope. Although the exact mechanisms underlying patterned-ground formation in Breckland are not fully understood, their presence may be used to say something about former climatic conditions.
Further reading
Boreham, S. & Rolfe, C.J. 2016-17. Imaging periglacial stripes using ground penetrating radar at the ‘GRIM’ training site, Grime’s Graves, Breckland, Norfolk. Bulletin of the Geological Society of Norfolk 66, 31–43.
Archaeological excavations are about the minutiae of a site or a trench, and it is sometimes difficult to think about the wider context of the work immediately at hand.
A tradition of the Barnham excavations is to take a day out to visit other sites in the local area and to use the opportunity to consider Barnham in its regional landscape, environmental and archaeological setting and introduce the students to some of the research questions that the work at Barnham is working to address.
Today’s field trip visited Maidscross Hill, Lakenheath, Warren Hill, Mildenhall, Beeches Pit, West Stow and Barnham Heath to explore the Breckland’s Palaeolithic record. The trip generated some interesting questions and discussion.
After a week, the excavation is settling into its routine. People are getting to know each other, the areas are looking more like archaeological trenches and the pattern of daily life is established. From time to time someone, usually a visitor to the site, ‘volunteers’ to give a short talk to the group that is relevant to the work on the site. Today we had a talk from Peter Hoare about the history of brickmaking in Barnham and the pit which was dug for clay to make bricks from the 18th to the early 20th century. After lunch work resumed on site and by the end of the day, and the first week, the site is looking tidy and the artefacts are beginning to appear. The evening’s entertainment began with a game of rounders and continued with a barbecue enjoyed by all as the mid-summer sun dipped below the horizon.
Tuesday was our first full day on site and a buzz of excitement filled the air, with eager faces and an intrigue to learn. We started by fully uncovering Area III, the largest and deepest trench on the site, and prepared for this season’s excavation by cleaning what has been buried for over a year, battling creepy crawlies and the warm weather.
Once this was completed, I and a team led by Claire and Anne-Lyse began work on Area I. This area had been excavated previously in the 1990s and again last year, but the hillside had partially collapsed revealing more of the Palaeolithic deposits. We secured the unstable edge and removed the backfill from previous excavations, neatened out the sections and began trowelling off the topsoil, eager to find the palaeosol and any potential finds. This was surprisingly strenuous and time-consuming, but we supported each other through chatter, banter and occasional jokes about rocks.
We continued on Wednesday, after sponging out the rainfall from the stormy night, but we were getting desperate to reach the palaeosol as our wrists were strained and concentration was wavering. Our morale was boosted by the occasional flint flake and burnt flint find. After working through what felt like 50 shades of clay – brown, reddish brown, black, and so on – we finally hit it and a mixture of elation and relief was mutually felt; I have never been so happy to see another layer of sediment! However, this excitement was cut short as the heavens opened and we had to pack up quickly before the site got too slippery. We covered the site to protect our work and headed home early for a well-deserved shower and a sit down.
Nick Ashton, Simon Parfitt and Simon Lewis discuss the research highlights of the archaeological excavations at Barnham.
Archaeological excavations in an abandoned brickearth pit at East Farm, Barnham have uncovered one of the richest Lower Palaeolithic archaeological sites in western Europe, dating to about 400,000 years ago. Finds include butchered large-mammal bones, flint tools and evidence for fire.
The 1989-94 excavations established the significance of the site, with its in situ artefact assemblages and its substantial quantities of vertebrate remains, include fishes, amphibians and small and large mammals. The second round of excavations that started in 2013 have refined our understanding of these lithic assemblages and also provided an opportunity to explore the evidence for technological transitions and how early humans developed strategies for survival. Recent investigations at the site have identified an earlier core and flake industry that was replaced by a later handaxe industry (Clactonian and Acheulian respectively). This technological transition may reflect arrival of different human populations into Britain from different regions within Europe, bringing with them different technologies.
Area III, pictured in a photogrammetric reconstruction of the excavation (above), shows ‘islands’ of undisturbed sediments cut by late 19th and early 20th century brickearth pits. These sediments contain stone tools and a rich assemblage of vertebrate remains. Area III has provided important evidence for the environment in which early humans lived; pollen grains contained within the sediments enable the vegetation at the time to be reconstructed and the landscape can be populated with both large and small animals based on the fossil remains found in the sediments.
Among the many examples from these deposits are a macaque tooth and elements of pond terrapin carapace (shell) indicating warm conditions and diverse habitats that included both woodland and aquatic environments.
In a different part of the site, the excavations in Area VI, revealed a new dimension to the Barnham story; along with the many flint artefacts that make up the lithic assemblage, there is also a surprising quantity of burnt flint. This material, with its distinctive cracked and crazed surface and often red colouration, was found within the black clay, a layer that we know to have once been a land surface as it shows signs of soil development.
As the excavations have progressed, our research has focused on this evidence for burning and the critical question of whether the burnt flint, which includes some artefactual as well as natural pieces, provides evidence for hearths or does it record ancient forest fires?
To address this question we have excavated and carefully recorded the spatial distribution of hundreds of fragments of burnt flint in order to plot the variation in density across the excavated area. We are also using laboratory analyses, particularly Fourier-transform Infrared Spectroscopy (FTIR) to identify heating signals in the sediments. Another avenue of enquiry is the use of experimental fires, set and maintained under carefully controlled conditions, to investigate the changes that take place within and beneath a hearth.
If the evidence points to human use of fire, this would provide further indications of the development of new technology that goes beyond the stone tool evidence and it may also begin to tell us something about societies and culture in the different human groups that entered Britain during this interglacial some 400,000 years ago.
With a focus on the archaeological and environmental evidence, the Barnham Palaeolithic Project is able to address important questions concerning Palaeolithic societies 400,000 years ago at spatial scales ranging from domestic sites with evidence of fire through group territories to relationships between groups across Europe.
Written by Sarah, a volunteer at the 2019 Barnham excavation.
Tea breaks are integral to field work at Barnham. In the mornings, team members shrug off yesterday’s aching muscle memory, cleaning up debris that has accumulated in the trenches overnight and picking up where we left off the day before. Morning tea break offers a circle of cushioned chairs beneath a sweeping sky of swirling grey and white clouds. Beside us, a rolling field of grass spreads out towards a horizon of tall trees. The grass veils tractors and equipment that remind us we are gracious guests trying to make sense of an ancient landscape on modern farmland.
As we are divided into different areas to work, first tea is the first opportunity to check in on everyone’s progress and exchange stories. Here we discuss small moments of interest, where things have not quite gone as planned, or someone has found something interesting. By afternoon, the team has broken into the prime vigour of progress for the day, and everyone has worked up a proper appetite. Lunch (with tea) is a welcome halfway mark to the day’s work. By afternoon, aches, pains, setbacks, and tedium begin to take their toll – broken by moments of surprise and laughter (or a bit of sarcasm). Afternoon tea is a final pause before the last push to meet goals, piece together the day’s big-picture puzzles about the site, and wrap up work.
The tea breaks lift morale and facilitates social health on site. Tea duty is therefore an important responsibility that rotates through each team member. Today was my day to make tea for the team. Being Mormon myself (a member of the Church of Jesus Christ of Latter Day Saints), I don’t drink tea. Nevertheless, I was happy and excited to help. I was amused (and so were the kind staff members and fellow students checking on me) as, at first, I kept repeating my questions about the difference between the hot water “teapots” and the steeping kettles. Not to mention I spilled quite a bit of hot water and tea while preparing for morning break, trying to figure out how to pour out of typical teapot spots into kettles and mugs. It was immensely satisfying to serve my wonderful team members and help host these essential gatherings that punctuate our work day. And, according to my new friends, I made a mean cup of tea!
It’s the first day of the excavation, a day for getting to know each other and the site, sorting out the equipment, tool shed and office and beginning to prepare the excavation areas for the work ahead. This year’s team sees a nice mix of old and new faces; students studying at Leiden University, UCL, and Durham, Brighton, Liverpool and Reading universities will be working alongside staff and volunteers from the British Museum, Natural History Museum and Queen Mary University of London.
Following a site induction, most of the team got to work recovering Area III from the ravages of winter, bailing out water, removing leaf litter and lifting the plastic sheeting that has protected the area since last year’s excavation. This job has been done well, so tomorrow we should be able to begin excavating. Meanwhile, our digger driver Dave and his brother Colin are extending Area I by removing the backfill to reveal in-situ sediments to the east of the old excavation area. This may take a couple of days, but once it is complete a team will begin to excavate the ancient soil horizon along the southern margin of the site that we hope will preserve evidence of human activity.
On the eve of the 2019 season, Simon Lewis reflects on three decades of fieldwork in the Breckland.
In 1989 a team of six people, led by Nick Ashton, ventured into the old pit at East Farm, Barnham. Armed with spades, mattocks and trowels, and guided by information from earlier investigations by TT Paterson and John Wymer, the aim was to explore the potential for fresh excavations at this important, but perhaps somewhat overlooked Palaeolithic site. In the 1980s the British Lower Palaeolithic was dominated by Boxgrove; excavations were in full swing and the wealth of new data emanating from the excavation’s HQ in farm buildings near the site was transforming our understanding of early human behaviour and the environments in which they lived as well as setting new standards in excavation, recording and sampling procedures. In contrast to the scale and organisation at Boxgrove, excavations at Barnham adopted, from the outset, an approach that suited a small Breckland brickearth pit abandoned since the early years of the 20th century, now completely taken over by oak trees, hawthorn and bramble thickets and with little to disturb the tranquillity of the location.
John Wymer’s work in 1979, had revealed the potential of the site; he excavated a small area and recovered a refitting group of 13 flakes and a core. The team set about the task of re-exposing the sediments and the archaeological levels, previously described by Wymer. The 1989 results demonstrated that there was indeed scope for larger-scale excavations at the site and so, with the enthusiastic support of the Heading family at East Farm and the Euston Estate, began a six-year programme of fieldwork at East Farm. The results of these investigations have been published in a comprehensive volume, as well as papers in academic journals.
After the 1989-94 excavations ended the now-established research team turned their attention to another Breckland site; the former pit at Elveden, some 7 km west of East Farm. Excavations at Elveden ran from 1995-99 and together these two sites provided important new geological, environmental and archaeological evidence for understanding the Palaeolithic of the region.
Nineteen years after concluding the first round of excavations at East Farm, a decision was taken to return to the site. There were three main reasons for doing this, the first was to re-evaluate the key archaeological question of the relationship between Acheulian and Clactonian assemblages in the light of wider developments in understanding of this problem in the intervening years. The second was the opportunity to add to the already rich environmental information from East Farm, in particular to increase the vertebrate assemblage and to explore the linkages between the archaeological and environmental evidence. The third was to provide an opportunity for archaeology students to gain experience of excavation on a Lower Palaeolithic site. Following on from the work at Happisburgh with the Faculty of Archaeology at Leiden University, Barnham provided an ideal setting for this.
So 2013 saw a return to East Farm, with a small team of Dutch students, to embark on a new programme of research again led by Nick Ashton. The first season was primarily about finding our feet again and identifying areas for excavation. Over the subsequent five seasons, archaeological work has focused on the southeast corner of the pit, Area IV(4), where evidence of handaxe manufacturing had been found in 1994, which has now been expanded into the adjacent Area VI. The environmental work focused on the centre of the pit, Area III, which has been considerably enlarged from the earlier work. Material excavated from Area III has been processed on-site; several tonnes of sediment being excavated, dried, disaggregated and sieved during the course of each season.
This second Barnham campaign has already provided an array of new information. Among the key developments since 2013 are the reassessment of the stratigraphic relationship of the handaxe and non-handaxe assemblages, the addition of several new species to the faunal list, the discovery of an intriguing burning signal though recovery of large quantities of burnt flint and location of an organic deposit, with a pollen profile showing the development of interglacial woodland vegetation. We have also welcomed students from several UK universities alongside new and returning Leiden students.
As the 2019 season gets underway, with new and exciting objectives for this year’s excavation, it is good to look back over thirty years of excavation and related research in and around the Breckland area. As always, the support of the British Museum, as well as other funding bodies through the Ancient Human Occupation of Britain (AHOB) and Pathways to Ancient Britain (PAB) projects and the Breckland Palaeolithic Project, has played a vital role in the excavations at Barnham and other Palaeolithic sites. Three decades of collaborative research in the Breckland, with fieldwork at East Farm playing a prominent part, demonstrate that a great site and a dedicated team of people, united by a shared interest in the lost world of our distant ancestors, are the foundations on which this endeavour has been built.
Today saw the start of the 2019 field season with delivery of machinery, tools and equipment and other essentials to the site. The site hut, office and tool store will soon be ready for the start of the dig next week. Clearance of areas for this year’s work got underway, though conditions on site are rather muddy after several days of heavy rain.
This year we hope to continue the extensive excavation, sampling and sieving of the sediments in Area III, reassess Area V and also have another look at a small part of Area I to explore further the evidence of burning that has been found in Area VI. We look forward to getting things underway next week.