The Camel valley in winter. Taken from between Pendavey bridge and Polbrock looking upstream.
Sketch map of the River Camel and its tributaries
|Native name||Dowr Kammel|
|⁃ location||Bodmin Moor|
|⁃ elevation||218 m (715 ft)|
|Padstow, North Cornwall coast|
|Length||48 km (30 mi)|
|Basin size||413 km2 (159 sq mi)|
|⁃ left||River Ruthern|
|⁃ right||De Lank River, River Allen|
The River Camel (Cornish: Dowr Kammel, meaning crooked river) is a river in Cornwall, England, United Kingdom. It rises on the edge of Bodmin Moor and with its tributaries its catchment area covers much of North Cornwall. The river flows into the eastern Celtic Sea between Stepper Point and Pentire Point having covered about 30 miles. The river is tidal upstream to Egloshayle and is popular for sailing, birdwatching and fishing. The name Camel comes from the Cornish language for 'the crooked one', a reference to its winding course. Historically the river was divided into three named stretches. Heyl (Cornish: Heyl, meaning estuary) was the name for the estuary up to Egloshayle, the River Allen (Cornish: Dowr Alen, meaning shining river) was the stretch between Egloshayle and Trecarne, whilst the Camel was reserved for the stretch of river between its source and Trecarne.
- 1 Geology and hydrology
- 2 Estuary
- 3 Recreation
- 4 Wildlife and conservation
- 5 History and infrastructure
- 6 Water pollution incident
- 7 Tributaries and their names
- 8 References
- 9 External links
Geology and hydrology
The River Camel rises on Hendraburnick Down (UK Grid Reference SX135875) on the edge of Bodmin Moor, an area which forms part of the granite spine of Cornwall. The river's course is through upper and middle Devonian rocks, predominantly the Upper Delabole Slates, Trevose Slates and Polzeath Slates that stretch to the coast, although Pentire Head is composed mainly of pillow lavas. The only active quarry in the River Camel catchment area is at Delabole and there has been mining for lead and silver on Pentire Head, a copper mine at Credis above Little Petherick, and building stone extraction at various locations. Further inland the Camel and its tributaries border the St Austell mining lodes near Lanivet, and mines in this area produced tin, lead, silver, and copper. Iron ore in the form of haematite and associated manganese oxides were also mined in the area. Although not considered a great producer, Mulberry Mine near Ruthernbridge produced in the region of 1300 tons of tin between 1859 and 1916. Records show that copper ore was shipped from Padstow to Neath for smelting, and it can be assumed that other ores were similarly treated.
The source of the Camel is at 218 metres (715 ft) above sea level and it has an average incline of 7m/km. The upper reaches of the Camel and its tributaries are mainly moorland giving way to woodland and farmland, predominantly livestock. This means that 64.8% of the catchment is grassland, with a further 14.8% arable land and 12.9% woodland. Of the remaining 7.4%, 4.5% is through urban or built-up areas, 2.7% is mountain, heath and bog and the remainder is inland waters.
The Camel's catchment area covers 413 km2 on the western side of Bodmin Moor, and is mainly Devonian slates and granite, with some shales and sandstones. Water volumes are affected by the reservoir at Crowdy Marsh, by abstraction of water for public supply, and by effluent from the sewage system around Bodmin. Data collected by the National Water Archive shows that water flow in the River Camel for 2006 was considerably below average. This correlates with reduced rainfall, particularly between the months of June and September. Data from 2013 and 2014 also shows below average annual flow but with points of higher than average flow during Winter.
The next five and a half miles beside the broadening Camel to Padstow is the most beautiful train journey I know— John Betjeman, Betjeman's Cornwall
The Camel Estuary (Cornish: Heyl Kammel) stretches from Wadebridge downstream to the open sea at Padstow Bay. The quays at Wadebridge are now developed with apartments and retail space on the west bank. North of the quays, the river passes under a concrete bridge carrying the A39 bypass and past the disused Vitriol Quay. Downstream of Burniere Point the valley widens on the right with acres of salt marsh where the River Amble flows in. Here the Cornwall Birdwatching and Preservation Society has hides on both sides of the river; those on the Camel Trail are open to the public. The main river follows the western side of the valley, while on the eastern side a barrage prevents the rising tide from entering the River Amble.
Downstream from the Amble an adit can be found on the foreshore below Dinham Hill, part of Wheal Sisters copper mine. The adit is only accessible from the foreshore at low tide, and is situated near to the location of a tide mill that is recorded as being in the region of Dinham creek, although no sign of this now remains. Cant Cove lies on the east bank below Cant Hill where the rotting ribs of two ship project from the mud, these being discernable on Google Maps in 2019, and almost opposite Cant Hill on the west bank is Camel Quarry with the piles of waste rock clearly visible above the river and the remains of a quay visible at low water. From here the mud gives way to sand and Gentle Jane, named after a legendary lady who treated the ills of all comers.
From Porthilly Cove on the east bank, the estuary widens and swings to the north. On the west bank, the Camel Trail crosses the triple-span “Iron Bridge” over Little Petherick Creek then passes below Dennis Hill and its obelisk.
The mouth of the Camel lies between Stepper Point on the west and Pentire Point on the east, and each headland shelters sandy beaches. On the west side of the estuary, Tregirls beach is protected by Stepper Point. At the northern end of Tregirls beach is Harbour Cove and between here and Hawker's Cove evidence has been found of occupation during the Bronze Age, Iron Age and Roman periods, and use of Harbour Cove for trading vessels.
In 1827, Padstow Harbour Association chose Hawker's Cove as the location for the Padstow lifeboat. Operations were taken over by the RNLI in 1856. A new lifeboat station and slipway were built in 1931 and a second lifeboat stationed at Hawker's Cove. The station closed in 1962 because silting rendered the channel too shallow. The building is now converted to residential use.
Beyond Hawkers Cove, the Doom Bar extends across the estuary. The sandbank has been the graveyard of many ships. A legend as to how the Doom Bar came about describes how a local fisherman is reputed to have shot a mermaid with an arrow, with the result that she cursed Padstow by putting the sandbar between the harbour and the sea.
On the east side of the estuary, the village of Rock is centre for sailing, dinghy racing and marine leisure. From Rock, dunes and intertidal sands extend north as far as Brea Hill. Beyond Brea Hill is Daymer Bay with a beach north of which is the settlement of Trebetherick. A stretch of rocky foreshore swings east to the bay and beach at Polzeath, a location for surfing. North of Polzeath, Pentire Point marks the northeast extremity of the estuary.
The Camel Estuary has been designated an Area of Outstanding Natural Beauty (AONB), covering the area between Padstow/Rock and Wadebridge. The estuary comprises part of the Cornwall Area of Outstanding Natural Beauty.
Beaches and bathing
On the western bank Hawker's Cove, Tregirls beach and St Georges Cove lie between Stepper Point and Padstow, while on the eastern bank moving upstream from Pentire Point is Polzeath beach, Daymer Bay and Rock. Water quality is monitored at Polzeath and Daymer Bay with water classification for the years 2012 to 2015 for both locations being "Excellent". Water quality was previously monitored at Rock, results from 2007 for all three locations on the eastern bank of the river being either "good" or "excellent".
The Camel Trail
The Camel Trail, used by walkers and cyclists, follows the trackbed of the Bodmin and Wadebridge Railway from Wenfordbridge, past the outskirts of Bodmin at Dunmere, and through Wadebridge to Padstow.
Long distance footpaths
The Saints' Way footpath links Padstow with Fowey. It follows first the River Camel, and then Little Petherick Creek from Padstow to Little Petherick, before striking inland and crossing the county to the River Fowey. This route is a very ancient one used by travellers from Ireland and Wales making for Brittany and wishing to avoid the dangerous seas around Lands End.
GUIDE TO THE RIVER CAMEL
(Tuckingmill to Penrose)
A reasonable wind-down after the above section. There are lots of grade 2 rapids to enjoy. The river opens out and you pass through some gardens and at the end, right in front of the chalets of a fishing resort. Obviously, a small quiet group is advisable.
The following section is not very pleasant. 
Water skiing takes place on the estuary based in Rock, with four set courses located between Dennis cove and Pinkson creek.
Wildlife and conservation
There are five Sites of Special Scientific Interest (SSSIs) along the length of the Camel. Four small SSSIs at Harbour Cove, Rock Dunes, Trebetherick Point and Pentire Peninsula are on the estuary, while the River Camel Valley and Tributaries SSSI covers much of the Camel Valley between Egloshayle and Blisland, and extends in several further sections of varying size up to its source. This SSSI covers much of the River Allen, a tributary which flows into the river immediately upstream of Egloshayle, and some smaller unnamed tributaries. In addition there is an SSSI at Amble Marshes on the River Amble which flows into the Camel Estuary between Wadebridge and Rock.
The River Camel has been designated by the Joint Nature Conservation Committee as a Special Area of Conservation of European importance for the otter and the bullhead. However, information on the area is confused: The DEFRA Joint Nature Conservation Committee website shows the area stretching from Pinkson Creek on the Camel estuary up to Polbrock bridge, but incorporating Pinkson Creek, the River Allen to just upstream of Sladesbridge, and the Polmorla Brook almost to the edge of the Wadebridge built-up area, and incorporating all of the intertidal zone. In contrast, both the Marine Conservation Institute and ProtectedPlanet show the area from Wadebridge bridge upstream, including the Ruthern, Allen, De Lank and Stannon, all being shown as covered to their respective sources., the only part of this area considered tidal is between Wadebridge bridge and St Marys church Egloshayle.
There are two nature reserves on Camel and its tributaries. The Walmsley sanctuary of the Cornwall Birdwatching and Preservation Society is on the Amble marshes on the River Amble above Trewornan Bridge. Hawke's Wood reserve, owned by the Cornwall Wildlife Trust, is on the south side of the Camel Valley between Wadebridge and Dunmere. Here is an abandoned quarry in a mature woodland of predominantly sessile oak.
With the large areas of salt marsh on the estuary, the river provides an excellent location for birds. Large flocks of waders can be seen in winter, preyed on by peregrine falcons, and a migrant osprey often pauses a few days to fish in spring and autumn. Mute swans nest at several locations, particularly near to the bridge in Wadebridge. Shelduck, shoveller and mallard are found on the river and teal further upstream.
An American belted kingfisher was seen in the 1980s for only the second time in England and the Estuary has been noted for early colonisation by Egret species. In the 1980s and 1990s Little egrets were to be seen on mudflats at low tide, and more recently large numbers of Cattle Egrets have been found on the River Amble and near Burniere, and have now become sufficiently common not to require corroborated evidence when reporting sightings
There are three birdwatching hides. Tregunna Hide (Grid reference SW 969 738), owned by Cornwall County Council, is located by the Camel Trail and is open to the public. Burniere Hide (Grid Reference SW 982 740) is owned by the Cornwall Birdwatching and Preservation Society (CBWPS) is open to members. In addition the CBWPS own the Walmsley Sanctuary which covers over 20 hectares (49 acres) on the River Amble, with two further hides for use by its members. The Walmsley sanctuary is nationally important for wintering waders and wildfowl. These hides are located on the estuary below Wadebridge while upstream of Wadebridge there is a hide overlooking Treraven Meadow located 500m from Guineaport towards Bodmin
In 2016 a Dalmatian Pelican was recorded on the River Camel at various locations between Rock and Dinham
The estuary is a sea bass conservation area. This was originally designated as being upstream from a line drawn between Stepper Point and Trebetherick Point but this was extended to include all waters upstream of a line between Stepper Point and Pentire Point in 1999. Surfers at Polzeath have recounted seeing Bass swimming around their surfboards in summer.
Flounders can be found in the brackish waters as far upstream as Cant Hill, and Daymer Bay is noted as a location for fishing from the rocks.
Salmon and sea trout are found in the River Camel and have been fished since the 12th Century. The Camel had a reputation for good runs of both species up to the early 2000s, particularly in the area around Bodmin  but there has been a rapid decline in the late 2010s, leading to the Environment Agency placing restrictions on Salmon fishing in 2017.
By the Atlantic Ocean the flora is distinctly maritime, characterised by Thrift and Sea campion on exposed clifftops and spring squill and heather in the turf. Stunted blackthorn and gorse tolerate more exposed sites, while the quarry on Stepper Point is home to many species of marsh plants. Above Egloshayle there are beds of yellow flag Iris while the wooded slopes of the valley are filled with bluebells in spring.
The Camel and its tributatries are home to Otters. These were hunted up to the early 20th century but are now one of the species cited in the River Camel and Tributaries SSSI.
History and infrastructure
Transportation and Industry
Cornwall is an undulating county with high cliffs, rough moors and deep valleys, so rivers have been used for transport throughout history. Being one of the few safe havens on the north coast of Cornwall, the Camel Estuary has been used since Roman times, and most likely earlier. The river has been navigable beyond Wadebridge with the highest quays being at Guineaport and Egloshayle, and ships being recorded beyond that at least as far as Pendavy a mile further upstream,. The river as far as Wadebridge was considered navigable for vessels up to 150 tons in 1830.
With boats as one of the main methods of transporting goods until the advent of the railways there were several quays along the river, often at the limit of navigation of the many tributaries and creeks on the estuary. Thus there were quays at Little Petherick on Little Petherick Creek and at Pinxton Creek although the latter became inaccessible when the creek was cut off from the main river by construction of the railway to Padstow. The River Amble was also navigable up to Chapel Amble on high spring tides, with seaweed, sand and coal being taken up to the village and grain brought out again, although the Amble is now protected by a tidal barrage which prevents salt water going upstream past Burniere Point. Nearer to Wadebridge there was a quay at Trevilling on the North bank of the river built in the 19th century for a Vitriol works and thus known as the 'Vitriol Quay', the location downstream from the town near the current A39 Wadebridge Bypass bridge being appropriate for the product.
Despite the many opportunities for transport along the estruary, historically the main traffic on the River above Padstow was to the Quays at Wadebridge where there is evidence of a dock dating back as far as Elizabethan times. Construction of the Bodmin and Wadebridge Railway in 1834 was based on taking sand brought up to Wadebridge by barges that were poled under the bridge, the sand then being transhipped to the railway for onward transport, the railway replacing the previous use of pack animals that took the sand from landings at Sladesbridge and a quay at Marsh cottages near Egloshayle church.
In common with much of Cornwall lime was a common commodity for transportation in the 18th and 19th centuries and the Camel was no exception with lime kilns being recorded at Egloshayle with a quay adjacent, another at Bishop's Quay below Gonvena Hill, and one on the town side of the river adjacent to the Pomorla brook
There are several ancient defensive sites along the Camel Valley. Penhargard Castle is an Iron Age defended settlement near Helland situated high on the eastern side of the Camel valley, and not far away on the other side of the river is an older hillfort. Rather later in date there is the remains of a Roman fort near Nanstallon overlooking the Camel valley. Once thought to have been the only Roman Fort in Cornwall, the fort was only occupied between 60 and 80AD.
The river and its tributaries are crossed by more Listed bridges than any other river in Cornwall. Most notable is at Wadebridge, the lowest bridge on the river, which was built in the 15th century to replace an earlier ford which was considered so dangerous to use at certain times that a chapel was built on either bank; one ot pray for a safe crossing and the other to give thanks. Thomas Loveybond, Vicar of Egloshayle, was the mover of construction while John de Harlan was the actual builder. The bridge was made a county bridge in the reign of James I, and has been widened at theee times over the years, being granted Grade II listed status in 1969.
Moving upstream from Wadebridge, the other listed bridges are Helland Bridge, Wenfordbridge, Coombe Mill Bridge, Gam Bridge, and Slaughterbridge, this latter so named as it is the location of an historic battle, possibly that of King Arthur's last battle.
One of the largest structures on the Estuary is the "Iron Bridge", a three span girder bridge of 400 ft (120 m) originally built to carry the North Cornwall Railway between Wadebridge and Padstow over Petherick Creek. Good use was made of the river during construction as the metalwork was brought to Wadebridge by boat and then floated on barges down to where the bridge was being built. Sitting on Dennis Hill overlooking the bridge is an Obelisk erected to celebrate the Golden Jubilee of Queen Victoria'. Erected in 1889 the granite obelisk is Grade II listed.
Water pollution incident
In July 1988, the water supply to Camelford and the surrounding area was contaminated when 20 tons of aluminium sulphate was poured into the wrong tank at Lowermoor Water Treatment Works on Bodmin Moor. An inquiry into the incident (the worst of its kind in British history) started in 2002, and a report was issued in January 2005 but questions remain as to the long-term effects on the health of residents. Michael Meacher, who visited Camelford as environment minister, called the incident and its aftermath, "A most unbelievable scandal."
Tributaries and their names
The main tributaries of the River Camel are the Allen, the Ruthern, the De Lank and the Stannon. Other tributaries include Little Petherick Creek which joins the main estuary through the Iron Bridge on the Camel Trail, the River Amble which joins the Camel though a tidal barrage near Burniere Point, and the Polmorla Brook (historically Treguddick Brook) which joins the Camel immediately above the bridge at Wadebridge.
In terms of its name there is evidence that what is now known as the River Camel has had several names in the past. The name Camel is derived from Middle Cornish "Cam-El", "Crooked one", and seems originally to have referred only to the upper parts. The lower part of the river was referred to as the River Allen, a common Celtic river name of unknown derivation, however in the 19th Century the name Allen was transferred to the River Layne which flows into the Camel just above Egloshayle. The Camel estuary appears to have been called the River Hayle from Middle Cornish "Hayle", estuary and while this may have been as much a description as a proper name, the continued use of the name Hayle Bay for the bay containing Polzeath beach supports this. In turn it has been suggested that the River Layne may have previously been called the River Dewi given the number of places along its course which contain the element.
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Credis lies within the parish. It was once the location of a small copper mine. The mine employed forty men and the shaft at Credis was thirty fathoms (55m) deep.
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Table 3 and Table 4
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Minchinton and Perkins record that Dinham salt water mills were advertised for sale in 1851 (2). The 1st Edition 1:2500 OS c1880 map records a disused tidal bone mill at the site (1). A tidal pond is recorded on the 1963 OS map but this is not apparent on the current 1:10000 edition (3, 4). The CCC 1999-2001 vertical aerial photograph shows no survival of the mill
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County Bird News: As of 1st Jan, the two expanding egret species in the UK, Cattle and Great White have been taken off the ‘County Description Species’ List. Care over id may still need to be taken, & recorder/committee may request further information for any particular sighting.
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All tidal waters enclosed by a line drawn 116 deg true from stepper point to Trebetherick Point
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A quay on the south bank of the River Camel, adjacent to the old line of the London and South Western Railway (now the Camel Trail). The quay survives substantially intact, although partly obscured by modern infill to the east. It is constructed of slate stone masonry in alternate vertical and horizontal bedding, with granite capstones (JRS, 2002)
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A sand wharf on the Camel at Egloshayle
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Some of the wharves and quays where goods such as lime and grain were loaded are still clearly visible on the west side of the creek
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most of Cornwall’s tiny ports had a lime kiln in the vicinity
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The Tithe Award for Egloshayle records a lime kiln at the location, owned by Susannah Hawken and worked by Richard Hawken (b1). No remains are now extant (b2)
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The Tithe Award for Egloshayle records a lime kiln at the location, owned by Nevell Norway (b1). No remains survive (b2)
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Sand quays on the Egloshayle side of Wadebridge are recorded on the Tithe map of 1840. The quay has now been overbuilt by modern housing (h1).
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Situated on Bishop's Quay, this kiln existed at least as early as 1834, as it appeared then in a 'for sale' notice. Run in its latter days by Messrs Martyn (b1). Marked on the 2nd Edition 1:2500 OS map (b2)
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A limekiln at Wadebridge is shown at this location on the Tithe Map of 1840, when its owner was Sir William Molesworth and its occupier was Thomas Trebilcock (b1). It is shown on both the 1st and 2nd Edition 1:2500 OS maps (b2, b3), but is believed to have been derelict well before 1910 (b4).
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- "BRIDGE AT WENFORDBRIDGE". Historic England. Retrieved 2018-03-18.
- "ROADBRIDGE 70 METRES TO NORTH EAST OF COOMBE MILLHOUSE". Historic England. Retrieved 2018-03-18.
- "GAM BRIDGE". Historic England. Retrieved 2018-03-18.
- "SLAUGHTERBRIDGE 500 METRES TO SOUTH EAST OF WORTHY MANOR". Historic England. Retrieved 2018-03-18.
- Gregory, Edward (2016). "King Arthur in Cornwall". www.king-arthur.co.uk. Edward Gregory. Retrieved 28 April 2019.
The area has yielded up information that Slaughterbridge, on the River Camel, was undoubtedly, the site of a ferocious battle in ancient times; though, whether this was the Battle of Camlann in 542 is open to speculation
- "Slaughter Bridge, Cornwall". legendofkingarthur.co.uk. Retrieved 28 April 2019.
Slaughter Bridge still remains a candidate for the Camlann battle site
- "The Legend of Arthur". www.bbc.co.uk/cornwall. BBC. 25 July 2008. Retrieved 28 April 2019.
Visitors can walk through the fields where King Arthur and Mordred were believed to have met for their last battle.
- "Little Petherick Creek bridge". www.forgottonrelics.co.uk. Four by Three. 2017. Retrieved 5 May 2019.
- "OBELISK". Historic England. Retrieved 2018-03-18.
- The Independent, 16 April 2006, Poisoned: The Camelford scandal Archived 2008-05-20 at the Wayback Machine
- Weatherhill, Craig (1995). Cornish Place Names and Language. Sigma Leisure. ISBN 1-85058-462-1.
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