Somerset Levels (wetlands, water, wide skies)
One of England’s most important wetland habitats is the Somerset Levels, shaped by rivers and peat to provide lowlands that are haven for local wildlife, thanks to reed beds and shallow lakes.
Bitterns, marsh harriers and thousands of winter starlings call this place home. Along with cranes (England’s tallest birds) who have returned after 400 years. And it’s one of the few places in England where raft spiders live (they sit near bogs and ‘float’ while catching prey.
Learn more on how to restore England’s Wetlands.
If out walking, always follow the Countryside Code to keep all creatures safe. If at the coast, read about how to keep dogs safe by the seaside.
The first thing you notice is the space. Flat fields, big skies, and long straight ditches that seem to run on for ever. Roads sit a little higher, houses cluster on slight rises, and the horizon feels unusually open.
People care about the Somerset Levels for a few simple reasons. It’s rich farmland, it’s a stronghold for birds and wetland life, and it holds a lot of local history in its soil. It also sits at the centre of a hard truth: when land is this low, water always has the final say.
Still, the Levels aren’t permanently under water. They’re a managed place, shaped by drains, banks, gates, and constant routine. Most days, it looks calm, even ordinary. That’s part of the point.
Where are the Somerset Levels, and what makes them different from the Moors?
The Somerset Levels sit in the low-lying centre and north of Somerset, between higher ground like the Mendip Hills and the Quantock Hills, stretching towards the Bristol Channel. Think of a shallow basin with hills around the edges, where rivers slow down and spread out.
Locally, “Levels” and “Moors” don’t mean quite what people expect. The Levels often refers to the broader flat plain, much of it drained and farmed. The Moors are the lower, wetter parts that flood more easily, and tend to hold water for longer in winter. In practice, people use both terms loosely, but the feel on the ground does change. You can sense it in how close the water sits to the field surface.
Several rivers shape the area. The River Parrett and the River Tone meet near Bridgwater. The River Brue crosses the central Levels. The River Axe drains areas closer to the Mendips. Because the land is so flat, these rivers don’t rush. They creep along, and that’s why the drainage network matters.
Those straight ditches you see are rhynes (pronounced “reens”). They’re working channels, not just pretty lines on a map. They collect water from fields, hold it, and guide it towards larger drains and rivers. Without them, much more of the land would stay wet for longer.
How the land was shaped, peat, rivers, and a long history of drainage
After the last Ice Age, sea levels rose and low ground filled with water. Over time, plants grew, died back, and built layers. In the wettest places, that slow build-up formed peat. Meanwhile, rivers brought in silts and clays, laying them down in thin sheets during floods.
People then started to manage the water, because wet ground limits crops, roads, and settlement. Monastic communities and later landowners dug channels, straightened drains, and built banks. As tools improved, pumping and organised drainage became more common. The goal stayed the same: keep fields workable for more of the year.
The result is a landscape that can feel almost levelled by hand. On a clear day, you can see for miles, like looking across a huge village green, only it’s stitched with water.
A map in your head, towns, viewpoints, and what you might notice first
It helps to anchor the area with a few familiar names. Glastonbury sits on higher ground at the edge of the wetland. Bridgwater lies to the west, closer to the Parrett. Burnham-on-Sea is on the coast. Wells is nearby, set against the Mendips.
When you arrive, the first clues are small but steady. Straight ditches run beside lanes. Raised roads cross fields like causeways. Pumps sit quietly by sluices. In winter, birds lift off in waves, then settle again, as if the whole field has breathed.
Living with water, how the Levels are managed, and why floods still happen
Water management on the Levels is mostly about pace and timing. Because the ground has such a low gradient, water doesn’t clear quickly on its own. So the system gives it routes, holds it back in places, and moves it on when conditions allow.
Many areas follow a seasonal pattern. Winter often brings higher water tables and wetter fields, and in some places controlled flooding helps wildlife. Summer is usually drier, with water levels managed to suit crops and grazing. This isn’t a wild swamp. It’s more like a carefully watched bath where someone keeps adjusting the taps.
Even with all that work, floods still happen. Heavy rain can fall on already saturated ground, so water has nowhere to soak in. Rivers can only carry so much, and when they meet high tides near the coast, outflow slows again. Add the low slope of the land, plus silt build-up in channels, and you get long-lasting flooding rather than sudden torrents.
The 2013 to 2014 winter floods sit in many people’s memories. They weren’t the first, and they won’t be the last. They did, however, make the trade-offs clearer, between farms, homes, roads, and the wetland habitats that also need water.
The everyday tools, rhynes, sluices, pumps, and why maintenance matters
Rhynes collect field water and guide it towards larger drains. Sluices (water gates) control when water moves from one channel to another, which matters when tides or river levels rise. Pumps lift water over banks or into higher channels, especially when gravity alone can’t do the job.
Banks and raised embankments keep rivers in their course during higher flows, although they also need careful checking. On top of that, some areas use washlands, where water can spread in a planned way during wet spells.
Maintenance is the unglamorous part that makes everything else work. Ditches silt up and grow in. Banks slump. Gates stick. Because water moves slowly here, small blockages matter more. Clearing and inspections aren’t a one-off fix, they’re a regular cycle.
Flood risk in plain English, what increases it, and what helps reduce it
Flooding usually comes from several pressures arriving together. The main drivers tend to be:
- Intense rainfall: more water than the ground and drains can take.
- High tides and storm surges: slower river outflow near the coast.
- Silt and channel capacity: less room in rivers and drains over time.
- Low gradient: water lacks the natural push to clear quickly.
- Land use and soil condition: compacted ground sheds water sooner.
Responses also come as a mix, and each has limits:
- Targeted dredging where suitable: can help in some stretches, but it isn’t a universal answer.
- Upstream storage: holding water higher in the catchment reduces pressure downstream.
- Habitat and floodplain areas: giving water room can protect homes, while supporting wildlife.
- Property-level measures: airbrick covers, door barriers, and raised sockets reduce damage.
Small choices that protect the Levels, paths, dogs, drones, and litter
A few habits make visits easier for everyone:
- Stick to signed paths where possible, fields are often working land.
- Keep dogs close (and on a lead when asked), especially near birds in winter.
- Skip drones in sensitive areas, sudden noise can flush flocks.
- Take litter home, even small scraps travel fast in water.
Somerset is a large county in southwest England, home to England’s smallest city, beautiful villages and a stunning sandy coastline.
The Strawberry Line Path is a converted 10-mile railway track near Wells. It stretches from Yatton to Cheddar, with shorter sections like the 2 miles from Wells to Dulcote through ancient woodland, with spectacular views of the cathedral. All routes are wheelchair-friendly (save a steep lane at Axbridge)
