A medieval Yorkshire town sent two men to Parliament, collected tolls from over a hundred ships a year, and today lies completely underwater off Spurn Point.
In 1295, a port on the Yorkshire coast sent two representatives to Edward I’s Model Parliament, the assembly that historians treat as the template for the modern House of Commons. That port isn’t on any current map. Ravenser Odd stood on a sandbank at the mouth of the Humber, and by the end of the 14th century, the sea had taken every trace of it.
For a few decades, Ravenser Odd outpaced Kingston upon Hull, the city that would go on to dominate the same stretch of coast. Both received royal borough charters from Edward I on the same day, 1 April 1299. Hull is still there. Ravenser Odd is somewhere under the Humber, and nobody has definitively found it.
The Story
Ravenser Odd began in the mid-13th century, built on a shifting sandbank at the mouth of the Humber estuary, close to what’s now Spurn Point. The name comes from the Old Norse Hrafn’s Eyr, Raven’s Ear, a reference to the spit of land the town grew on. Within a few decades it had become a genuine working port: wharves, warehouses, its own court, a prison, and a market busy enough to collect dues from more than a hundred merchant ships a year.
The 1299 charter formalised what had already become obvious. The National Archives holds the charter roll recording Ravenser Odd’s new rights alongside Hull’s, the two towns listed one after the other in the same official record. For a period, Ravenser Odd’s trade outweighed its now-famous neighbour’s. It had the political weight to match: in 1295, it returned two members to the Model Parliament, the assembly Edward I convened to include representatives from towns as well as nobility and clergy.
The same sandbank geology that made the port possible made its end inevitable. An inquisition in 1346 recorded that flood damage had already driven out two-thirds of the townsfolk. Storms through the winter of 1356-57 flooded what remained, and the Grote Mandrenke, the great drowning, a catastrophic North Sea storm surge in January 1362 that reshaped coastlines across England and the Low Countries, finished the job. The Meaux Abbey Chronicle recorded what was left by the end of the century: a graveyard with corpses exposed by the sea, and a chapel stripped by looters who no longer had a town to answer to.
What You See When You Visit
There’s nothing to see, and that’s the point. Ravenser Odd sits somewhere beneath the Humber off Spurn Point, and no confirmed archaeological trace of it has ever been recovered above water. Researchers have looked. A search effort investigated the seabed near Spurn in 2022, hoping to locate the foundations of the seawall and harbour. Interest in relocating the site remains among local historians, but nothing has been definitively confirmed as Ravenser Odd’s remains.
What you can see is Spurn itself, the narrow curving spit of sand and shingle that the same coastal processes which destroyed Ravenser Odd continue to build and reshape. Standing at the Spurn Discovery Centre and looking out towards the river mouth, you’re looking at the same forces, working on the same stretch of coast, seven centuries on. On a clear day with the tide dropping, the light on the water and the low calls of wading birds working the mudflats are the closest thing left to what a 13th-century sailor approaching the port would have seen and heard.
Why It Matters
Most lost-village stories in Britain involve slow abandonment: a plague, a change in farming, a landlord’s decision. Ravenser Odd is different. It was a functioning, prosperous, politically represented town, wealthier than its neighbour for a stretch of its life, and the sea simply took it, over roughly a century of documented flooding, storms and finally one catastrophic surge. Nobody chose to leave. There was, eventually, nowhere left to leave from.
The Holderness coast, running north from Spurn, remains one of the fastest-eroding coastlines in Europe, losing an average of two metres a year and up to ten metres a year in the worst-affected stretches. Over 30 settlements have been lost to the sea along this coast in the last 2,000 years, a slower, ongoing version of what happened to Ravenser Odd in a single generation. The same mechanism claimed villages further south along the Lincolnshire coast, covered in our piece on Lincolnshire’s lost villages.
When to Go
Spurn National Nature Reserve is worth visiting in any season, though spring and autumn bring the strongest birdwatching, with Spurn’s position on the coast making it one of the best migration-watching points in Britain. Winter storms show the erosion process in its rawest form, waves working directly against the point. Summer offers the calmest conditions for walking the reserve’s paths in comfort.
Getting There
Spurn Discovery Centre sits at Spurn Road, Kilnsea, Hull HU12 0UH, signposted from Easington. By car from Hull, take the A1033 towards Patrington, then the B1445 towards Easington and Kilnsea, turning right at the Easington T-junction and following the minor road through to the Discovery Centre. A weekend bus service run by East Yorkshire Buses connects Hull Interchange to the Discovery Centre via Patrington and Easington on Saturdays and Sundays; check the current route number and timetable directly on the East Yorkshire Buses website before travelling, as service numbers on this route have changed between seasons.
Where to Eat and Drink Nearby
Crown and Anchor, Kilnsea. A three-room pub on Easington Road with a dining room looking out over the Humber estuary, serving locally sourced food and about as close to Spurn as a proper meal gets.
Where to Stay
Spurn Bird Observatory, Kilnsea. Hostel-style accommodation a few doors from the Crown and Anchor, built for birdwatchers and walkers who want to be on the reserve at first light rather than driving in.
Westmere Farm, Kilnsea. Self-catering accommodation in the village at the head of the Spurn peninsula, a practical base for a longer stay on this stretch of coast.
Worth Knowing
- Ravenser Odd and Hull received their royal borough charters from Edward I on the same day, 1 April 1299, recorded one after the other in the same National Archives charter roll.
- The town’s name comes from the Old Norse Hrafn’s Eyr, Raven’s Ear, describing the sandbank spit it stood on, the ancestor of the modern Spurn Point.
- The Holderness coast north of Spurn is still eroding at up to 10 metres a year in places, meaning the process that destroyed Ravenser Odd hasn’t stopped; it’s just moved a few miles up the coast.
Practical Tips
- Wear proper walking shoes. Spurn’s paths cross shingle, sand and boardwalk, and conditions change with the tide and weather.
- Check tide times before visiting, since parts of the reserve and the approach road can flood at high tide.
- Bring binoculars if you’re visiting during migration season, spring or autumn, when Spurn draws serious birdwatchers from across the country.
- Use the AllTrails app to check the current condition of paths in the reserve before setting out, as coastal erosion can alter routes with little warning.
- Entry to the reserve and Discovery Centre is free, though Yorkshire Wildlife Trust members get free parking.
Reader Q&A
Can you visit the actual site of Ravenser Odd?
No. The site lies underwater off Spurn Point, and no confirmed archaeological remains have been recovered, though research into locating it continues.
Was Ravenser Odd really bigger than Hull?
Yes, for a period in the 13th century. Ravenser Odd was the more important port of the two, collecting dues from over a hundred merchant ships a year before its decline.
What destroyed Ravenser Odd?
Sustained coastal flooding through the mid-14th century, worsened by storms in the winter of 1356-57, and finished by the Grote Mandrenke storm surge of January 1362.
Is the Holderness coast still eroding today?
Yes. It remains one of the fastest-eroding coastlines in Europe, losing an average of two metres a year, with some stretches losing up to ten metres a year.
Ravenser Odd left no ruins, no walls, nothing you can put your hand on. What’s left is the Humber itself, still moving the same sand it moved seven hundred years ago, and a stretch of coast at Spurn that’s still deciding what happens next.
