How do underground peat fires keep burning after wildfires are out?
Peat fires keep burning underground because they are smouldering, a slow low-temperature burn that survives after the flames are out.
Covers: The science of smouldering combustion in peat and other organic soils, why these fires persist underground through winter or drought, how they are detected and extinguished, and their climate and health impacts. Does not cover surface wildfire behaviour or firefighting tactics for above-ground flames.
Also answers: Why do peat fires keep burning underground? · How do underground fires burn after wildfires are out? · What are zombie fires and how do they work? · How long can a peat fire smoulder underground?
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The short answer
Evidence-backed AI-prepared starting mapPeat fires persist underground because the fire is not a flame but smouldering combustion inside the soil: it burns slowly at low temperature with little oxygen, so it survives after the surface flames die out and can keep going for weeks. Laboratory work on 1-m deep peat columns found smouldering temperatures falling from about 550°C near the surface to about 350°C at 40 cm depth and holding near 300°C in deeper layers, with the fire burning in deep layers for weeks and losing only a small fraction of mass because oxygen supply is limited and temperatures are low. A separate deep-layer experiment found underground smouldering could sustain itself for more than a week with no additional oxygen supply, and identified a critical depth of 55 cm below which it cannot self-sustain. Smouldering is also described as the dominant process in the residual burning left after flames have died out.123
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Be the first to voteIn brief
Underground peat fires keep burning because they are smouldering, not flaming: low-temperature, oxygen-starved combustion that continues after surface flames are out.3
Evidence-backedAn underground peat fire can resurface and ignite flames in surface litter, with the chance falling as peat moisture and litter density rise.4
Evidence-backed
At a glance
The picture in numbers
Live · updated just now
- Near surface550 °C
- 40 cm depth350 °C
- Deeper layers300 °C
55 cm
1 week
- Upward spread300 °C
- Downward spread600 °C
The evidence behind it
7 sources- Reviews of many studies1
- Other studies and data5
- Background1
When it was published
Newest from 2026
| Source | Kind | Year |
|---|---|---|
| Deep peat fire persistently smouldering for weeks: a laboratory demonstration | Other studies and data | 2022 |
| Persistent Underground Smouldering Fire in Deep Peat Layer | Other studies and data | 2022 |
| Smouldering wildfires in peatlands, forests and the arctic: Challenges and perspectives. | Other studies and data | 2021 |
| Upward-and-downward spread of smoldering peat fire | Other studies and data | 2018 |
| Resurfacing of underground peat fire: smouldering transition to flaming wildfire on litter surface | Other studies and data | 2024 |
| Review of combustion issues in underground fires | Reviews of many studies | 2013 |
| How drones are hunting fires hidden beneath the Cairngorms | Background | 2026 |
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What it means for you
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If you want to know whether a peat fire is still burning after the flames are gone
look for surface carbon monoxide, which the deep-peat experiments used to detect underground fire and monitor its intensity, rather than relying on visible smoke or flame.1
Evidence-backedIf you are assessing how long a peat fire might persist
expect weeks rather than days in deep layers, based on laboratory columns that burned for weeks at around 300°C and a deep-layer experiment that sustained smouldering for more than a week without added oxygen.12
Evidence-backedIf the peat is wet or the fire is shallow
expect slower in-depth spread and shorter burning, and note that a laboratory critical depth of 55 cm was found below which smouldering cannot self-sustain.12
Evidence-backedIf you are managing an area where an underground peat fire has been detected
treat resurfacing as a real risk: laboratory and field experiments showed a smouldering peat fire propagating upwards and igniting flames in surface litter, which can create new spot fires and accelerate progression.4
Evidence-backedIf you are weighing the wider consequences of a peatland fire
account for extensive air pollution, very large carbon emissions and a possible acceleration of climate change, alongside the difficulty of detection and suppression.3
Evidence-backedIf you are in or near an area with known underground peat burning
treat it as a lasting safety threat: such fires can persist for a very long time and are extremely difficult to extinguish.5
Evidence-backedThe full story · 3 chapters
01
Why the fire keeps going underground
AI summary:Smouldering, not flaming, is what continues underground; depth and moisture set its limits, and a critical depth of 55 cm stops it self-sustaining.
Evidence-backed: A wildfire is not one process. Flaming and smouldering combustion are fundamentally different in chemical and physical terms, and one can transition into the other; smouldering dominates the residual burning after flames have died out. That is why extinguishing the visible fire does not end the event: the part that continues is a different kind of combustion, and it is the kind that produces the largest fires on Earth in peatlands.3
Evidence-backed: In peat, the fire moves in two stages. An initial upward spread towards the free surface runs against the airflow (opposed smouldering) at a peak temperature of about 300°C and leaves behind a char structure that does not collapse. A second, downward spread then begins, this time with the airflow (forward smouldering), reaching a peak temperature of about 600°C and causing the surface to regress. The upward stage is faster than the downward one, and both slow down as peat density or depth increases. Modelling points to oxygen diffusion as the control on the whole upward-to-downward sequence, with peat oxidation sustaining the first stage and char oxidation sustaining the second.6
Evidence-backed: Depth and moisture set the limits. In 1-m deep peat columns, smouldering temperature dropped from roughly 550°C near the surface to about 350°C at 40 cm and then held at about 300°C deeper down; the fire burned in deep layers for weeks, and combustion was incomplete with only small mass loss because oxygen supply was limited and the smouldering temperature low. High moisture content slowed in-depth propagation and shortened burning duration. A separate experiment on layers up to 60 cm deep found underground smouldering could sustain itself for more than a week with no additional oxygen supply, and derived a critical depth of 55 cm: below that, the competition between oxygen supply and heat loss means smouldering cannot propagate on its own.12
Evidence-backed: The low temperature and slow spread that let the fire hide are the same properties that make it hard to fight. Underground fires are difficult to detect, especially in their early stages, and for the same reasons it is hard to estimate how far a detected fire has spread; they are also extremely difficult to extinguish and can last a very long time, with serious safety, environmental and economic consequences.5
02
The fire can come back to the surface
AI summary:Lab and field tests show an underground peat fire can resurface and ignite flames in surface litter, with wetter peat and denser litter making that less likely.
Evidence-backed: An underground peat fire is not necessarily contained below ground. In laboratory tests, a smouldering peat fire ignited at the bottom of a 10-cm peat sample propagated upwards and resurfaced, igniting a flaming wildfire in a 5-cm litter layer of banyan leaves (density 27–53 kg/m³) placed on top. The likelihood of the litter catching flame fell as peat moisture content (tested from 10% to 100%) and litter layer density increased, and the researchers identified a threshold for surface flaming based on the temperature and the rate of temperature rise at the peat–litter interface. Large field experiments reproduced and validated the laboratory observations. The authors note this ignition pathway has received little attention but may cause new spot fires, accelerate fire progression and worsen hazards.4
Evidence-backed: A reported case fits the pattern: after the large Cairngorms wildfire in July, the dramatic flames had disappeared, but hot spots can continue to burn beneath the earth.7
03
Detecting it, and why it matters
AI summary:Carbon monoxide near the surface can reveal an underground fire, which matters because these fires are hard to detect and emit very large amounts of carbon.
Evidence-backed: One practical detection route comes out of the deep-peat experiments: measuring carbon monoxide concentration near the surface can reveal an underground fire and be used to monitor its intensity. That matters because smouldering fires are otherwise difficult to detect and their extent hard to judge, particularly early on.15
Evidence-backed: The stakes are large. Smouldering wildfires are emerging as a global concern because they cause extensive air pollution, emit very large amounts of carbon, are difficult to detect and suppress, and could accelerate climate change; peatlands are important terrestrial carbon pools and are becoming more vulnerable to smouldering fires as a result of climate change and human activities. Smouldering is also an important part of Arctic wildfires, which are increasing in frequency.32
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In laboratory peat columns the fire burned in deep layers for weeks at roughly °C, with incomplete combustion and small mass loss; another deep-layer experiment sustained smouldering for more than a week with no added oxygen.
Depth and moisture bound the fire: a critical depth of cm was found below which smouldering cannot self-sustain, and higher moisture slows in-depth spread and shortens burning.
Underground peat fires keep burning because they are smouldering, not flaming: low-temperature, oxygen-starved combustion that continues after surface flames are out.
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- 1Deep peat fire persistently smouldering for weeks: a laboratory demonstrationInternational Journal of Wildland Fire (Qin et al.)Published Dec 7, 2022Checked Oct 11, 2026
“Peatlands are becoming more vulnerable to smouldering fires, driven by climate change and human activities. This work explores the persistent burning, propagation, and emission of the deep peat fire. Laboratory experiments are conducted with a 1-m deep peat column, and smouldering fires are initiated at different depths. Key results We found localised burning and multi-directional smouldering fire spread in deep peat layers. The smouldering temperature first decreases with depths up to −40 cm (from around 550 to 350°C) and then remains at about 300°C in the deeper layers. High moisture content can slow down in-depth fire propagation and reduce the burning duration. Peat fire can burn in deep layers for weeks, and its combustion is incomplete with small mass loss, because of a limited oxygen supply and low smouldering temperature. Measuring the carbon monoxide concentration near the surface can detect underground fire and monitor its intensity. Implications This work helps reveal the underlying mechanism of the in-depth smouldering wildfires in peatland and supports future larger-scale peat fire experiments in the field.”
- 2Persistent Underground Smouldering Fire in Deep Peat LayerImprensa da Universidade de Coimbra eBooks (Qin et al.)Published Jan 1, 2022Checked Oct 11, 2026
“Peatlands are important terrestrial carbon pools. Due to climate change and human activities, peatlands are more prone to large-scale fires than ever before, especially deep underground fires. However, most current smouldering researches focus on small-scale smouldering behaviour in relatively shallow layers, which poses a research gap. This work explores in-depth (up to 60 cm) smouldering behaviour, such as persistence, propagation and emission. Experimental results demonstrate that underground smouldering fires can sustain in deep soil layers for more than a week without any additional oxygen supply. Because of the competition of oxygen supply and heat losses, a critical depth of 55 cm for smouldering propagation was obtained, below which smouldering cannot self-sustained propagate. This work will help better connect lab-scale experiments with real underground smouldering peat fires and understand smouldering dynamics in deep soil layers.”
- 3Smouldering wildfires in peatlands, forests and the arctic: Challenges and perspectives.Current opinion in environmental science & health (Rein & Huang)Published Dec 1, 2021Checked Oct 11, 2026
“Wildfires can be divided into two types, flaming or smouldering, depending on the dominant combustion processes. Both types are present in most wildfires, and despite being fundamentally different in chemical and physical terms, one transitions to the other. Traditionally, science has focused on flames, while smouldering is often misinterpreted. But smouldering wildfires are emerging as a global concern because they cause extensive air pollution, emit very large amounts of carbon, are difficult to detect and suppress, and could accelerate climate change. Central to the topic are smouldering peat fires that lead to the largest fires on Earth. Smouldering also dominates the residual burning after flames have died out and firebrand ignition. Finally, smouldering is an important part of Arctic wildfires, which are increasing in frequency. Here, we present a scientific overview of smouldering wildfires, the associated environmental and health issues, including climate change, and the challenges in prevention and mitigation.”
- 4Resurfacing of underground peat fire: smouldering transition to flaming wildfire on litter surfaceInternational Journal of Wildland Fire (Zhang et al.)Published Feb 4, 2024Checked Oct 11, 2026
“Smouldering wildfires in peatlands are one of the largest and longest-lasting fire phenomena on Earth, but it is unclear whether such underground peat fires can resurface to the ground and ignite a flame on the litter layer. This work conducted a laboratory experiment by putting a 5-cm thick litter layer (banyan tree leaves with a density of 27–53 kg/m3) onto a 10-cm thick peat sample (moisture content of 10–100%). Key results and conclusions Tests confirmed that a smouldering peat fire, ignited at the bottom, can propagate upwards and resurface to ignite a flaming wildfire on the surface litter layer. The propensity of litter to be flaming ignited decreased with increasing peat moisture content and litter layer density. We found the threshold of such surface flaming as a function of temperature and temperature increase rate at the interface between peat and litter. Finally, large field experiments successfully reproduced and validated the laboratory observations. Implications This work reveals an important wildfire ignition phenomenon that has received little attention but may cause new spot fires, accelerate fire progression and exacerbate its hazards.”
- 5Review of combustion issues in underground firesResearch paper (Saulov et al.)Published Jan 1, 2013Checked Oct 11, 2026
“Due to specific characteristics of smouldering, such as low temperatures and small propagation velocities, underground fires are difficult to detect, especially in their initial stages. For the same reasons, estimation of the extent of the detected fire is problematic. Underground fires are also extremely difficult to extinct. Such fires can last for a very long period of time, posing a serious safety threat and having substantial adverse environmental and economic consequences. In this paper, we review current understanding of several major combustion issues in underground fires, which originated from the specifics of smouldering processes, including fire detection and measurements as well as some approaches to control and extinct the fire. We also review environmental and socioeconomic impact of underground fires. Limited number of publications on the issues associated with smouldering, in general, and underground fires, in particular, is available. As a result, our understanding of the phenomena involved is incomplete. Further research in the area is required.”
- 6Upward-and-downward spread of smoldering peat fireProceedings of the Combustion Institute (Huang & Rein)Published Jun 21, 2018Checked Oct 11, 2026
“Once ignited, the 1st-stage upward fire spread is initiated towards the free surface (opposed smoldering) with a peak temperature of 300 °C, leaving behind a char structure that does not collapse. Then, a 2nd-stage downward spread (forward smoldering) is activated with a peak temperature of 600 °C and regression of free surface. The upward spread is faster than the downward spread. The rates of both upward and downward spread decrease as the peat density or depth is increased. These experimental observations are successfully captured by a 1D computational model of heat and mass transfer with 5-step kinetics. Modelling results further suggest that (1) the oxygen diffusion controls the entire upward-to-downward spread of peat fire, (2) the oxidation of peat sustains the 1st-stage upward spread, and (3) the oxidation of char sustains the 2nd-stage downward spread. This is the first study investigating the upward spread of peat fire, which helps understand the persistence of peat fire and guide the fire prevention and suppression strategies.”
- 7How drones are hunting fires hidden beneath the CairngormsBBC NewsPublished Oct 10, 2026Checked Oct 11, 2026
“Dramatic flames from the huge Cairngorms wildfire in July have disappeared - but hot spots can continue to burn beneath the earth.”
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Open questions
How long do real peatland fires actually smoulder in the field, and how much does that vary with peat type, drainage and weather? The available persistence figures come from laboratory columns.
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Does the 55 cm critical depth for self-sustaining smouldering hold in natural peatlands, where layers, moisture and structure differ from prepared samples?
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How early and how reliably can carbon monoxide or other surface measurements locate an underground fire, and how well can they map its extent?
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Which suppression approaches actually work on deep smouldering peat, and how is success measured?
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How often do underground peat fires resurface into flaming wildfires in real events, and what conditions make that most likely?
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