“I’d always thought that trees helped with carbon but I did not know how much carbon peat bogs hold, and how important they are.” Splat participant.
Galloway’s landscape is typically one of trees bordering grazing land and wetlands. People think about how trees sequestrate carbon quickly, but we also need to bear in mind how peatlands store carbon in the long term. They need to be protected to keep their carbon store in the ground.
Image: Sphagnum Splat Placard
Peat is created by bog mosses which make layers of carbon-rich material from air and rainwater. Peatlands comprise Scotland’s largest carbon store. Most peatbogs are in poor condition and need to be restored, not just for climate but also for wildlife, food production, and water quality.
Environmental managers now emphasise how important peatbogs are for ecosystem services and policy has changed. Formerly, people thought of peatbogs as unproductive land which should be brought into cultivation.
With forestry, the right tree species needs to be planted in the right place. Previous conifer planting on deep peatbogs is now regarded as unproductive and to have caused unanticipated problems like acidification. ‘Forest to Bog’ projects in Galloway Forest Park are one means by which peatbogs are being restored.
‘A bog functions when the water table is high. A high water table means that the bog is not releasing carbon into the atmosphere. The point of restoration is to stabilise the water table.’ Emily Taylor, Crichton Carbon Centre.
Earlier conifer plantations mistakenly planted on deep peat are felled, and the peatland can be nurtured back into life. The images below show the first flush of colonising plants.
Sphagnum species offer a natural path to climate action. Once mosses and sedges have started to grow, the bog as a whole can start to recover. The peat underneath will then be protected by a living layer of special bog plants. Sometimes these need to be introduced back into the area. Amazingly, Sphagnum can grow from the tiniest wee fragment on the surface. The different species each have their own preferred conditions, and will grow in the microclimate which is right for them. It’s hard to know exactly how the peatbog will shape itself given the changing levels of the water table, but having a range of native Sphagnum species is important.
Image: Sphagnum Splat Placard inspired by Jos Smith’s poem Upstream Thinking
Over thousands of years since the last Ice Age, these bog mosses played a central role in creating the raised bogs that are typical of Galloway’s landscape. It’s easy to become a moss enthusiast when you learn how Sphagnum mosses grow and what they do. Collectively they reach upwards to the light, and underneath their older strands become part of a deep, dark suspension. Sphagnum moss absorbs water and, with time, a raised bog grows in the landscape. A peatbog in good condition quakes when you walk on it because it is a liquid depth of several metres.
Dr Emily Taylor of the Crichton Carbon Centre is a specialist in sustainable land management. She is a peatland restoration expert and leads a training programme for Peatland Action, a Scottish government initiative.
The sites are often in remote places where large machinery is at work. How can people see and learn about such exciting and significant restoration work?
The Crichton Carbon Centre took the initiative to invited local people to come and help. People took in the message that peatlands need to be in good condition and made placards to communicate this.
Image: Placard created by Sphagnum Splat Participant
With permission of Forestry and Land Scotland, on 14th October a group gathered at Clatteringshaws Visitor Centre to help with the South Dee Moss Restoration, in a most symbolic, enjoyable and educational way.
Emily Taylor explained the concept behind the Sphagnum Splat.
“What the restoration site really needs is more Sphagnum, so we are going to try this innovative method. We’ve got some Sphagnum, and we’ll collect some more on the way. We are going to Splat the bog with Sphagnum! We’ll make balls with peat and Sphagnum, and hurl them across the bog.
It sounds wacky – and it has been the most bizarre access permission the Forestry has had, they said. But there is a scientific basis for it, and they are excited about this development too.
This is about celebrating the amazing work going on in Galloway, restoring bogs for carbon benefit as well as water quality and habitat.”
Emily Taylor, Splat Co-ordinator.
This concept appealed to people of all ages.
We set off at a brisk walk, with placards and all the kit needed for a Splat from the appointed place in the Forest Park.
We learned to identify and gather Sphagnum species on the way.
When we got to the edge of the South Dee Moss, Emily Taylor gathered us on a small hillock at the edge of the bog.
This area had been clear-felled of conifers and the low areas that had been deep bog had been flattened again. In terms of landscape restoration, the view to the Southern Upland Way could eventually open out.
Now the former drains are blocked, the water can rise again to create a bog. Historic aerial photos, taken before the trees were planted, show a landscape of deep peatbogs strung along the Black Water of Dee valley.
‘Right Tree – Right Place! That’s the thing!’
Some areas were always just too boggy to be planted and these are at the heart of the process of recovery. The aim is to help the peat to stay in the bog rather than wash into the watercourse.
Image: Placard by Splat Participants
We executed the plan to Splatter the bog so that bog mosses could grow in this vicinity – as well as the sedges which had already started to grow.
The joyful experience of the Sphagnum Splat has been captured in a short video by Jayne Murdoch of the Crichton Carbon Centre. It is available here on facebook and the quotes below give further responses.
‘We’ve never been to a bog before! We had no idea how important they were until we had contact with someone at the Crichton Carbon Centre. After hearing about the environment on the news lately it’s great to be able to come along and help make a difference.’
The event was celebrated with new lines for a well known tune, that became a Bog Anthem and was premiered with great gusto, and unique style.
What’s it like taking music instruments to a bog? Who persuaded you? [Another musician] phoned up and said: ‘Do you fancy playing Land of Hope and Glory in a peat bog?’ It seemed such a way out idea that we said yes!
This placard echoes the words of a poem inspired by restoration work elsewhere: “something as small as a wish can root and breathe the peat alive again.”
Banner: Sphagnum Splat Placard inspired by Jos Smith’s poem Upstream Thinking
Although Emily Taylor recognised the need for an army of Splatters to scale up the restoration effort, she was pleased with progress:
‘This was the first Sphagnum Splat in Galloway, if not in the world! It worked well – it was successful and grown-ups were having just as much fun as the kids! A site like this is difficult to walk across, and you can get Sphagnum over quite a good area. It is good to do a restoration technique with people not just machines. Anyone can come out and have a bit of fun, and we can talk about the joys of peatbogs.’
Emily Taylor, Sphagnum Splat co-ordinator.
Acknowledgements and thanks to all Participants of Sphagnum Splat, an event led by Crichton Carbon Centre. This event was a marker for the completion of the Peat Culture project supported by the Galloway Glens Landscape Project. Thank you to Jos Smith for permission to refer to unpublished work created in celebration of peat restoration projects in south west England. Any unintended errors are entirely my responsibility.
This show took its lead from different technical activities of peatland survey and restoration. As an artist who wants to support this work, I’m interested in the cultural values of peatland and different ways of understanding them. This has meant looking close-up at bogs, as well as my own preconceptions. Scotland has a good share of peatlands. Their significance is now widely recognised, largely because healthy wetlands are one of the natural solutions for climate mitigation. Politicians are beginning to accept that we are in a climate and ecological crisis, thanks to the detemination of some scientists to communicate what is happening and the activism of groups such as the school strikers in breaking through societal denial. Environmental protection is a cultural as well as political concern; many artists, like myself, are working out what to contribute.
I am drawn to wetlands because I grew up near salt marshes, but peatbogs have a different character. In the uplands I am still always somehow waiting for the saltwater tide to come in. Spending time in peatlands has been a curious process – not necessarily comfortable, with moments of enchantment as well as uncertainty.
Peatbogs are landforms created principally by bog mosses; studying them turns attention to time and connectivity. As air and rainwater pull sphagnum mosses’ crown-shaped heads upwards, the moss stems are collectively pushed down. Over millennia their brief life in the light creates a deep, dark, suspension in water. A quaking peatbog is a sensory memory, archiving varied patterns of life after Ice Age meltwaters left a foundation of boulder-clay.
The following sections describe three groups of work in the exhibition.
Mending the Blanket
This booklet is about erosion and how people are restoring peatlands in remote places.
The booklet began as a series of prints made from peat from a restoration site in Southern Scotland. You can read more about the process here .
This series of prints, drawings and models was inspired by the extraction and return of a peat core at Kirkconnell Flow, a raised bog on the Nith Estuary near Dumfries. In 2016 the core was taken out of the ground during an arts-environment workshop (further information here). A scientific peat core is used as an environmental archive for research; I was able to use this demonstration core for artwork. After the core had been shown in different events, I made prints from each section. In June 2019 I returned each section of the peat core to Kirkconnell Flow with the permission of Scottish Natural Heritage, who manage the reserve.
Kirkconnell Flow is six metres deep. Peat accumulates by about one millimetre a year, so each 50 cm section represents about 500 years of growth. When we took the peat core, we put the sections in gutter pipe (on the floor in the photo).
Having got six metres down, it was exciting to find a clear line where the peat ended and a sedimentary layer of boulder clay began. This clay was laid down at the beginning of the Holocene era (perhaps 9000 years ago) and created an impermeable base on which bog mosses grew over the millennia.
Here you can download more information about the Kirkconnell peat core with references to other writings (the booklet in the photo above).
These were made from each section of the Kirkconnell Flow peat core (one section is missing because we were just learning how to use the peat corer).
Here are the prints being made on the Columbian Press in Edinburgh College of Art.
I returned the peat core last June to a small pool on Kirkconnell Flow. Putting the peat in water reduces the oxidation that occurs when it is exposed to air.
I found I wanted to keep the boulder clay. After a bit of dreaming, I used it to model some Holocene figures, using a simple coil technique.
The first form was a dug-out canoe. This referenced a prehistoric artefact in Dumfries Museum that had been preserved in a nearby raised bog.
Being taught to row in the Holocene
I made a concertina bookwork while forming an oar for the canoe. Rolling out the coils evoked childhood memories of learning to model things out of clay, and being taught to row in muddy salty southern estuaries.
Quadrat Drawings: making connections through field drawing
For me, field drawing is always work in progress. It’s about taking time to hone observation, and reflect on where I’m coming from and going to.
With the start of the growing season I began to make square drawings in imitation of a botanical field survey tool called a ‘quadrat’ (see the photo below). I had seen a quadrat being used to count plant species in a Galloway Glens Landscape Partnership workshop. I wanted to learn to see the living layer of peatland as offering different kinds of habitat for sentient and expressive beings.
I began in March at Knowetop Lochs in Galloway, during very wet weather. I was drawing crouched up on the ground. I knew theoretically the plant layer provides space for many varied activities but at first I only saw things – different wet shapes. I trained myself to make more connections and gradually began to use action words to label the drawings. For example, a rubbing of bare peat signalled ‘oxidising’.
As spring progressed, I became absorbed by plant growth. After the leaves came out, I became intrigued by interactions between different species of plants and insects.
The bog makes itself in tiny lively moments, such as when cotton grass seeds catch in willow branches. It was an experience of glimpsing many small carbon sequestrations, a kind of ‘shimmer’.
As I made discoveries about how to look better, I made guidelines for myself which I kept disobeying. I reflected on what was influencing me and began to make more insightful choices of how to interpret what I was seeing.
I saw how scientific plant illustration inspires careful attention to form but can lead to objectification. Other ways of looking, like Paul Klee’s dynamic plant drawings, help see process but can move the images towards abstraction. A painter called David Measures documented momentary glimpses of butterflies – and only drew when he could see the insect. His remarkable attentiveness gave new information about butterfly behaviour. His approach made more and more sense to me as a way of focussing on what is happening in the present moment. As I sensed the huge variety of interactions on a peatbog, I began to get a feel of how, in combination, this liveliness can become a substantial landform – given time.
Death was also present, for example when I looked at a deer skeleton mired in Dunhog Moss by Selkirk.
Pixels are replacing the traditional square survey unit as drone and satellite data makes surveys old-fashioned. Yet my commitment to close-up drawing grew as I saw more of the interconnectedness and minutiae of life on the bog. A distant view misses all this liveliness.
This learning process had emotional edges. By starting to treasure interactions that have evolved over the Holocene, I also realised what is being lost. I found myself wanting to spend time reconstructing patterns from what I had seen, taking time to draw courage from the intricacy of lives lived.
This project is background research for Kate Foster’s project called Peat Cultures, an element of Crichton Carbon Centre’s peatland restoration programme in South West Scotland supported by the Galloway Glens Landscape Partnership. It is part of a body of work submitted for a Masters by Research in Interdisciplinary Creative Practice.
Peatlands are a defining feature of Galloway, and on Tuesday 25th June, a group of creative practitioners gathered with staff from the Crichton Carbon Centre and Galloway Glens Landscape Partnership to spend time on a peatbog. This was a forerunner of a forthcoming restoration programme, Peatland Connections, that will focus on the important role that peatland plays in Galloway Glens landscapes. Peat Cultures is a strand within this programme drawing out different cultural aspects. This workshop was an opportunity for participants to learn more about the thinking behind the project as a whole, and an invitation to work creatively with its themes and develop different ways of getting to know these landscapes.
Dr Emily Taylor of the Crichton Carbon Centre and myself (Kate Foster) welcomed participants in the magnificent and accommodating Corsock Village Hall.
Introduction by Emily Taylor: background to peatland restoration and the site at Knowetop Lochs
Galloway Glens Landscape Partnership covers the Ken-Dee catchment, whose headwaters include a huge area of peatland mostly used for commercial forestry. Forestry and Land Scotland (formally Forest Enterprise) and the Crichton Carbon Centre are planning peatland restoration within a large-scale forestry programme. Carbon sequestration is just one of the benefits – others include water quality, biodiversity, landscape. It’s about culture too: what do local people want to see happening? It’s important to make connections between people in the area and how the local countryside is managed – to help make landscape decisions at local scale. Working with artists opens up different ways of communicating. Peatland restoration in general has to learn how to communicate why public money is being put into restoration.
Knowetop Lochs is a little bit of deep peat. This is not a pristine site but pockets of lovely bog habitat still thrive; there is probably no pristine bog left in Scotland. We will see cotton grass, forestry, heather, and now in June it is not too overgrown. This is typical landscape in Galloway, a peaty pocket within a matrix of other habitat and land use. Around here it is mainly farm and forest.
Perhaps we think when we are going into countryside, we are in wilderness but really we are somewhere that is intensively managed. Aerial photographs show peatland and its condition and there is commercial forestry on deep peat (more than 0.5 m deep) in this area. It has been drained and ploughed, probably herbicide to clear the heather, and fertilizer. Elsewhere peatland is drained for grazing.
Copies of the Peatland Condition Assessment Guide are available, free. These explain practically what we are talking about. We have four categories (near-natural, modified, drained systems, and actively eroding places) which link to carbon figures, so we can communicate how much carbon is being lost in an area, and the carbon benefits of undertaking restoration. We are condensing science to something that is practical and easy to understand.
At the outset of Galloway Glens Landscape Partnership we had a workshop at Beggers Moss, which is a little bit of peat that was too deep to plant, in a sea of conifer plantations. It has been left to do its own thing – it is an oasis. This got us thinking about other areas too.
What are peatlands?
Peatlands are unique! Peat is made up of organic matter that has not fully decayed, so vegetation builds up. This slowly decays and is acidic and starts to compact. Lowland raised bogs are big mounds of peat which filled in glacial lakes after the last Ice Age. Ice melted and became wetlands that infilled with reeds and eventually became ombrotrophic (“rain-fed”) peatland. So these are nutrient poor systems, just depending on rainfall. Fens are wetlands with more nutrients. This will become clear when we do a peat probe. Peat forms at about a rate of 1 metre per thousand years, so you might be standing on 8000 years of history.
Peatland Connections has a peat corer. The workshop plan included bringing up a core between us.
Kate Foster: some lines of enquiry for peat cultures
Peatland restoration – like all land reclamation – involves re-narrating ideas about our past and future, as well as doing the work on the ground. There are many possible lines of enquiry into peatland, and there is a big change of emphasis in how people are relating to these landscapes.
New themes move into the foreground, especially that of ‘carbon’. It is no longer a discourse about wastes and wilderness; the image of peatland is being re-written. All of us here are now involved in making new stories about peatland. Also, there is a wide range of new publications.
Six MSPs addressed the first People’s Climate Assembly outside Holyrood Parliament (on the 20th June, prompted by Extinction Rebellion). Peatland restoration has become an important part of government targets, as Claudia Beamish (Scottish Labour Environment Climate Change and Land Reform Spokesperson) mentioned.
When I first came to Scotland I saw peat hags and thought this was normal. From the publications by Emily and her colleagues, I learnt “Bare Peat” is actually an alarm signal.
I discovered that ‘squagy’ peat – old and compressed peat near the bog’s bottom – makes a good printing medium. The above image is inspired by a fieldworker probing peat depth. It is one of a series, Mending the Blanket. This was made in appreciation of the work of the proejct staff. Doing this work in isolated places requires tenacity.
Once the living layer bog is restored, we can turn the image the other way up!
Making peat prints showed how friable this is as a material. It washes away in a moment, and blows into dust even in the still air of Edinburgh College of Art.
In 2016, at a Borderlands Network meeting, Dr Lauren Parry led the extraction of a peat core on Kirkconnell Flow, near Dumfries. We thought of it as ‘getting down to the Ice Age” when we reached the boulder clay. This core went down to 6 metres – you see some ‘ghost prints’ of each section above. A botanist said she got goose-pimples when she saw the boulder clay emerge from the depth, thinking of how it had been made by glaciers grinding stone into ‘flour’ and depositing this as the temperature fluctuated. Separately, I’ll document the return of this core, with the permission of Scottish Natural Heritage (the site managers).
The quote above conveys the nub of my experimental drawing enquiry: a peatbog has a vulnerable living layer that creates an environmental archive beneath itself. How can I better connect to this as a vital living space for many other species?
These are some ideas that have come up – above is a “viewfinder” with some suggestions. For example, how can I position myself differently? We use a frame all the time: choosing a time, a space, and editing things consciously and unconsciously. We have limits to our knowledge and we only have human perceptions, a sensorium bequeathed by evolution.
However, Emily pointed out that drones and remote sensing via satellite are increasingly used to survey the 2 million hectares of Scottish peatland. The traditional half a metre quadrat used by botanical survey on the ground has become aerial, researchers looking down at ten kilometres square.
Another influence is Approaching Choreography by Claire Pençak, who developed a Proposal for Engagement: an Action Score for Place-Making. She proposed sixty ways of thinking about how we and other species are using a diversity of spaces out of doors.
On peatbogs I have experienced a sense of puzzlement, even disintegration (especially of paper!). Including myself in the picture helps me consider what influences me, for example I’ve found the practice of scientific plant illustration is sometimes unhelpful as it tends to portray plants as single stationary objects. I am interested in interactions, seeing connections over time and place.
Small movements catch your eye on the bog. These cotton grass seeds have fallen on an annual from last year. I see this as a moment of ‘shimmer’, a tiny sequestration of carbon. Cotton grass is an important constituent of peat: seeing this seasonal pattern is a way of relating to the time implied by the bog’s depth.
Arriving at the deep bog in Knowetop Lochs Reserve
At Knowetop Lochs, Emily pointed out aspects of the site. When it was afforested, the peat was ploughed to make ridges for planted trees to grow on. Cross-drains lower the watertable, and a compacted track changes how the water moves through the peat.
The large amount of heather shows this bog is still rather dry. However the presence of sphagnum moss (with its amazing water-holding capacity) and cotton grass was a good sign.
Having a high water table underpins all the other processes in a peatbog. Sphagnum creates an acidic bog with slow decay rates. Bogs sequester carbon slowly compared to trees. The climate equation depends on what happens to that tree: if it is harvested for biomass – even timber for a house – then the carbon is not stored for long. Based on current cover, peatbogs contain more carbon than forestry, but the depth of all the peat is not known. The current estimate is that there is 25 times more carbon in peat than in forests, UK wide.
Peatlands secure a long term carbon store, but erosion means carbon is lost into the atmosphere very quickly. Methane (a powerful greenhouse gas) is naturally emitted by peatbog but sphagnum’s methanotropic bacteria ‘eat’ methane. If a peatbog is in balance, methane is not a big issue.
This area would lave been a lake – a mineral bund infilled by water which over time became ombrotrophic, becoming an acidic bog supporting sphagnum. Within this time there were periods when it was dominated by sedge, heather, and woodland. Machines on a bog expose tree roots, especially willow, birch, alder. Over 8000 years, climate has changed.
Emily discussed several points we were curious about.
What about the peat extraction sites you see in Dumfries and Galloway? Peat is still being used as a growing medium and, elsewhere, for power on an industrial scale. There is ongoing commercial extraction with potentially an increasing global market especially as soils deteriorate in China (though no new licences can currently be given in UK).
Will global warming – and the extreme weathers we will get – impact the state of the bog? Yes, very dry springs are an issue. A bog should be more resilient if you raise the watertable, and less likely to dry out than if it was drained. In Germany now there are sites that are so dry in summer that they are pumping water back into peatlands in summer – perhaps not sustainable in the long term.
What about heather burning? Grouse chicks need to eat invertebrates that live amongst sphagnum. Heather burning creates a mix of heights so grouse chicks can both eat and hide. Environmentally? Generally intensity of management for just one species does not really give ecological benefit. Burning has been going on for a long time, it is a quick management tool but intense burning can mean heather is replaced by molinia – the dry hummocks of grass common in Galloway. This is a result of over-grazing and over-burning. All our systems are no longer natural: you might need fire in some areas. Possibly the Flow Country is as natural as it gets, but there has been fire there too.
If this area is 8000 years old, then how would it have been for Neolithic people, 5000 years ago? A lot more standing water. What would they have made of it? Bogs would have been important. Think of Bog Bodies, Bog Butter! It was special, and useful. Sphagnum was used until recently as wound dressings. Diaries about collecting sphagnum have been found recently in Galloway, and people had family memories of picking sphagnum extending to Perthshire.
Probing the depth
How deep is the peat here? An orange peat probe is flexible fibreglass which you push down until you hit bed rock. You can tell how good the condition is by how smoothly the probe goes in and out. Poor condition forestry peat feels much more ‘crinkly’. We reached 4.5 metres and then 6 metres.
Image Elizabeth Tindal
Images above courtesy of Elizabeth Tindal
What is the deepest peat? The deepest found by Peatland Action in Scotland is around 11 metres. When you do a survey, it is a point every 100 metres.
We found sundews, looked at lichens and learnt that wood ants love sphagnum to nest in. We picnicked where there were least flies.
Taking a core
A Russian corer needs to be turned clockwise to cut against resistance and close its flap. It brought up a column of peat, changing in texture as it went down and changing colour as it oxidised in air. At six metres deep, this core visualised a time line of history – 6000 to 8000 years old.
Sphagnum grows from the top (its capitulum) and decays at the bottom. It slowly turns into peat as it goes down. Even for quite a dry site, the peat still was very wet.
The slice of peat in Emily’s hands, above, represents perhaps 100 years growth. It was near the surface and so less compressed.
Do you ever hit anything? Yes, tree roots, and standing stones in the west. In Ireland the peat extraction site workers often come across archaeological sites. There they are systematically stripping off the whole surface.
A vehicle in the bog? There was reminiscence about a large vehicle going over into the bog on the road Newton Stewart to New Galloway. The cab filled up with water and the driver got out – but the rescue team had to bring a huge crane and build a platform. It was a tourist attraction!
What about peat pipes at Silver Flowe? Silver Flowe is a blanket bog in good condition, perhaps 6 metres deep. There are slower rates of deposition on blanket bog that lowland raised bogs so there the rate might be possibly 5000 years for two metres. It has sink holes and an underpeat water course. Peat pipes are natural openings within the peat that are also increased by forestry. The sink-holes are hard to see, but you can pick them out because they are grassy around their edges.
How long does sphagnum live? A classic experiment with sphagnum took discs from a peat core and grew fragments on a windowsill, which grew. Pollen from other plants is a key thing that can be revealed by a scientific study of a peat core.
A Dorodango (shiny mudball in the Japanese tradition) began to take form in the hands of the Freelance Ranger. The technique of turning it migrates small pieces to surface and then it is left to dry out slowly.
Other conversations were about a sense of going backward in time; a love of peat from the smell of a home fire, how peaty water stains bath porcelain, the possibility of extracting ochre. We returned, some with some peat for inspiration.
Discussion in Corsock Hall
Peatland Connections plans more workshops, and this first one was especially intended for creative practitioners. We talked about developing an interest in peat through different kinds of art practice, and what our context of an ecological emergency means.
Emily outlined that the eventual Peatland Connections exhibition plan is about bringing together art, science, and music to find different ways to reach people.
Coffee and cake (and the absence of flies) helped discussion develop. Here are some headlines, grouping themes in the conversation.
Kate, being asked more about using peat to make prints: I wanted to understand the peatbog through making prints. It would be possible to over-focus on the aesthetics of a medium but you need to make connections. With Emily’s voice in my ear saying ‘Bare Peat is an alarm signal’, I turned to illustration to document a Peatland Action project in a remote part of Southern Uplands, which was reprofiling peat hags on blanket bog. This became a series of print/drawings, Mending the Blanket.
How do you overcome the challenges of this particular landscape in engaging wider audiences?
“I’ll be taking away with me the memory of the flies.”
A formal element could help, where people put on a kind of costume. Some people might not feel they need it, but it still could become a performative element. Knowing you have the right gear helps. You can go at different times of year, and use rhymes as well as clothing. It’s about finding things that can make you feel better.
A fieldworker might just see insects as part of the landscape, an indicator of the healthy bog, and look straight through the flies.
“I’ve got so used to focusing on the work itself that I have become used to not noticing the wind or the flies. But this can be unpleasant! Grim! Can be floundering around, with exhaustion perhaps – can be challenging.”
“But then we laugh and laugh!” Peat bogs are challenging, and this can also be celebrated.
If you grew up on bogs, can read them, but other people need time to learn to see where the dry and wet bits are – and also to recognise drains.
Perhaps we can do more to take things to people?
In rural areas, inclusivity means people coming from far via difficult public transport.
Word of mouth is powerful. So let’s tell people about peat!
It’s good to tune into culture of area – music jumps out in Galloway.
The area at the top of the catchment has seen movement of people historically. Hardly anyone goes there now – we have lost stories. We want to create new stories, things in future people remember, perhaps as sessions, or as a climate march.
People ask internationally: what does it mean that a climate emergency has been declared?
Dumfries and Galloway Council considers itself to be carbon neutral – but this is through offsetting. Carbon sequestration through forestry is how the accounting is done. In rural areas people are often dependent on cars and have oil fired heating. We are exporting emissions elsewhere. There is always a temptation politically to take the short-term route – for example, forestry. There is a need also to push action on transport, fertiliser use, and so on. £11m has jsut recently been allocated for Peatland Action, but peatland restoration is not just about carbon. Local drivers point to more direct benefits for communities and landowners.
What did artists feel about being in the bog this afternoon?
– Looking at it from further way, things will coalesce at home.
– I felt happy out there – peaceful, happy, engaged.- I will continue to tend the dorodango ball and make sure it does not crack. Might make a clay layer as a shell. This gives a story to tell, a reminder of the day.
– You may be the unfortunate one, to be a fly magnet.
– What really matters to me is being on the site, going and returning, reflection and conversation. Two hours on a sunny day feel might different than on a wet winter’s day when I fought through feeling alien by focussing on particularities.
– A moor can be an exposed place, it helps to look at small things such as sundew, cotton grass, a dragonfly.
– Sundews are my special study, but you can’t specify that you want to see this! You have to let your mind wander around. This gave me way of looking for them, learning that they are in lines, that people can walk on them. So will revisit sundew in different places, maybe creating performance, but not in a staged way.
– I liked it, I want to go back on my own wearing the right things, on a day when not so warm. I would walk up and down, thinking about duration, take video, photographs, work with this. You need to be introduced to a place before you can just go.
I don’t understand why you say a peatbog does not look good! Where does this idea come from? In Greece the landscape is dry, but you still like it, and get used to these colours. You become used to looking at lines, rather than at greenery and flowers.
It is about where you grew up, too. Childhood years can inform what you have a passion, whether it’s brownfield sites or whether you want to spend holiday time camping on peatbog, or the seashore.
– I would like to work with some boulder clay. The undulation is significant, and hummocks – you can zoom in, find things inside.
-How can you present the depth of core sample? It took thousands of years to create so these ideas take time to percolate.
What about finding beauty in these places, how can you do it?
As one example, Kerry Morrison mentioned the Wetland life project being about communicating the value and beauty of mosquitoes. Artists are drawn to the challenging, and making sense of them. I’ve learnt about mosquitoes from scientists – they sing, males dance, to attract a mate – and won’t mate until they sing in harmony. And do murmurations. I think how can I work with that? and it can be truly beautiful.
There is a tactile response too – we all sat on the hummocks. It would be nice to see how long they take to bounce up. We left an impression!
This is a developing conversation: comments and contributions are welcome.
Emily Taylor led the thanks to everyone present for pushing boundaries of thinking on peatbogs. Our thanks also to Galloway Glens, Corsock Village Hall for accommodation, the Scottish Wildlife Trust for permission to hold the event at Knowetop Lochs reserve, and Pantea Armanfar for documenting the workshop.
Thank you to Morag Paterson for the photograph of a sundew below.
Further images by Kate Foster / Pantea Armanfar unless otherwise stated.