The Ouse Washes Websitean independent research and information projectWelches Dam |
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IntroductionWelches Dam is an area in Cambridgeshire, England, alongside the Old Bedford, Counter Drain and Delph rivers. Once a civil parish, it is now part of the parish of Manea.It takes its name from a dam that was built here in 1651 when a channel called the Forty Foot or Vermuyden's Drain was cut to drain water from Ramsey into the Old Bedford River. There hasn't been an actual dam for perhaps 250 years (lots of suposition but little evidence), but there are two pumping stations (yes!) a few houses (four, I think), a disused lock, several bridges and a large nature reserve run by the RSPB and Wildlife Trusts. Photo: EE, March 2006 The west bank of the Counter Drain looking South. From left to right: in the distance is the lock entrance with a bridge over it; next is the old Lock-keepers Cottage; then ?; nearest is a house named Princess Victoria, once a pub. back to contents |
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DamIn the 1650s the Old Bedford River was cut in two by a dam just south of where the Forty Foot River, aka Vermuyden's Drain, joins it. Samuel Wells, Register of the BLC, wrote in 1830 that the dam was made to turn the water of the Forty Foot (cut in 1651) towards Salters Lode.Prof. Darby also says in his later work that Welches Dam seems to have been named after Edmund Welch, an official of BLC, and it is mentioned in the BLC Minutes and Accounts for the 1650s [yet the BLC was not incorporated until 1663!] back to contents |
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Inner gates, one open, one closed |
LockPhoto: EE, Apr 2011The original lock was built in 1651 when Vermuyden dug the Forty Foot Drain, aka Vermuyden's Drain, (top of photo, now overgrown with reeds) from Ramsey to here to drain waters from the Middle Level into the Old Bedford River (bottom of photo) thence to sea via the Old Bedford Sluice at Salters Lode and the Great Ouse River. Known as the Forty Foot Lock, it was rebuilt in 1991 by the National Rivers Authority (NRA). Since 1997 is has been owned by the NRA's successors, the Environment Agency (EA) which now calls it Welches Dam Lock. In 1996 an NRA report stated that high seepage losses of water in the Forty Foot River made it impractical to keep the channel open for navigation at all times. Entry into the Forty Foot from the OBR would be arranged in agreement with the Inland Waterways Association (IWA) on about 20 week-ends a year, assuming sufficient water available [from the OBR ?] to fill it. It was still navigable, with difficulty, in 2001 - see Tuesday Night Club cruise page for full report on a trip from the 16 Ft Drain to the Old Bedford with lots of photos. However a few years later the lock was sealed off with steel piles, and so it remains today. back to contents |
They've missed out "No Boating" The words "Welches Dam" have been taped over the original "Forty Foot" |
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BridgesThis section is still to be written.back to contents |
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Pumping StationThis section is still to be written.back to contents |
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Google satelite image. Wooden pumphouse in centre. Inlet from the Old Bedford. Pumphouse top right. |
Transfer StationThis is situated south (upstream) of the Pumping Station. Seen below looking south, on the left is the Old Bedford River (which becomes the Delph River) and the barrier bank; in the centre is the wooden pumphouse; on the right is the Counter Drain (which becomes the Old Bedford River).All photos: EE, Apr 2011 It was used (may be still is?) to transfer water from the Old Bedford River into the Middle Level system for irrigation during drought. Three 300mm inlet valves under the centre gate at Erith Sluice could be opened if the level in the Bedford Ouse was above 2.13m AOD and here water could be taken out via four six-inch pipes. Flow meters at Erith and here enabled the volumes of water coming in & going out to be balanced. (Source: NRA OW WLMP, March 1996.) Earith Sluice was refurbished in 2010 and according to Ryan Ely the EA Project Manager "the redundant water transfer system below the centre sluice gate has been removed". back to contents |
The transfer station pumphouse |
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RSPBback to contents |
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Prof. HC Darby, in his 1956 book The Draining of the Fens (2nd Ed) said on page
74 that
he had been unable to find any early reference to the bend in the Old Bedford River at Welches Dam. He said CN Cole's map of the Bedford Level (1789) shows it as a straight line with, apparently, a bank across the river at Welches Dam. RG Baker's map of Cambridgeshire (1821) shows a bend in two parallel rivers.On p187 Darby says that S Wells referred in 1821 to "The Delph or Thiry Feet [drain]". Darby says the history of that it is obscure, but it was subsequent to the Bedford Rivers. Writing in 1983 Prof Darby says in The Changing Fenland, that Vermuyden didn't mention Welches Dam in either his Discourse of 1642 nor his statement in 1653, and Dugdale did not mention it in his 1662 Diaries. On p 82 Prof Darby shows a map with a caption dating it as "1706?" which he says is Jonas Moore's map, showing the Old Bedford cut in two with a second river [which we know as the Delph] joined on to the southern part of the OBR, then running parallel to the northern section. Although not clear on the map, it could be assumed that the water from the Forty Foot drain flowed into the northern section of the OLB, thence to Salters Lode. Moore had been a surveyor on the drainage works from 1650-1657 and published his map in 1658. The dam is shown as "Welsh's" Dam. He died in 1679 and later editions of the map may have been added to by others. In 1830 Samuel Wells, Register of the BLC, said the dam was made to turn the water of the Forty Foot Drain (cut in 1651) towards Salters Lode when it entered the OBR at what has subsequently been known as Welches Dam. At some later stage between then and the 1750s (no one seems to know for sure) a new river, the Thirty Foot or Delph, was cut from Welches Dam running north to the east of the Old Bedford. It was joined on to the cut off southern section of the OBR just south of the dam, the running alongside and to the east of the Old Bedford for several miles before veering across the Washes to Welmore Lake Sluice from where it joins the New Bedford River. |
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Index and linksback to contents |
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