The Cheddar Yeo is a small river in Somerset, England.[1] Beneath the limestone of the Mendip Hills it forms the largest underground river system in Britain.[2] After emerging into Cheddar Gorge it flows through the village of Cheddar, where it has been used in the past to power mills. From the Middle Ages until the 19th century the river had ports for seagoing vessels but is no longer navigable. Some of the water, which is of good quality, is diverted into Cheddar Reservoir to provide drinking water for Bristol.
The Yeo rises from a spring near Charterhouse and then disappears under the Limestone of the Mendip Hills before reappearing in Gough’s Cave before emerging into Cheddar Gorge. Within Gough’s Cave the river forms the largest underground river system in Britain.[2][3] From a point relatively close to the areas of the cave open to the public, the cave-divers’ descent into Sump 1a begins through a tight passage known as Dire Straits. The bottom of that passage opens into the river passage, which is several meters across. This has been explored for 335 m (1,099 ft) downstream, whilst upstream a dive of 150 m (490 ft) brings the diver out in a 20 m (66 ft) long chamber named Lloyd Hall (which can now also be reached by an alternative, dry, route).[4][5] Another dive of 140 m (460 ft) through Sump 1b, finishing with an ascent through a rising passage, leads to another chamber, 60 metres (197 ft) long and 25 metres (82 ft) wide at its widest point, and full of large boulders, called Bishop’s Palace. This chamber is the largest chamber currently found in the Cheddar caves. Further on, three sump pools (named the Duck Ponds) lead to Sump 2 which is about 27 metres (89 ft) deep at its lowest point and 150 metres (492 ft) long.[4][5] Air is again reached at Sheppard’s Crook, which is followed by Sump 3. This sump is 55 metres (180 ft) deep and at its bottommost point is about 30 metres (98 ft) below sea level. Following Sump 3, a wide ascending passage continues for 370 metres (1,214 ft) before reaching an impassable blockage, still below the water’s surface.[4][5]
After emerging from the cave the river flows through Cheddar past the site of a Saxon palace,[6][7] in the grounds of The Kings of Wessex School, together with a 14th-century chapel dedicated to St. Columbanus.[8] Roman remains have also been uncovered at the site.[7][9]
It then flows south under a disused railway bridge which used to carry the Cheddar Valley line and west through Rackley before joining the River Axe.
The catchment area is 54 square kilometres (21 sq mi).[3]
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