Salters Lode Lock, Well Creek
Introduction
Salters Lode is a hamlet situated on the west bank of the tidal River Great Ouse at
a point where the non-tidal rivers Well Creek and the Counter Drain/Old Bedford
River (CD/OBR) join it via
navigation locks.
Well Creek is a canalised 8 mile waterway running from Marmont Priory near Upwell to
Salters Lode, linking the old course of the River Nene to the Great River Ouse. The
waterway was once an important commercial navigation but that ceased in the 1950s and the waterway soon declined into a weed ridden, rubbish strewn stagnant ditch prompting
Mr [Frank/Fred?] Hartley, Chairman of the drainage authority (MLC), to tell his board “The Well Creek is an eyesore and has become a burden to the MLDB. Its relationship to sea level means it does not drain one acre of our land therefore I would suggest we fill it in”
(source: William Smith, Upwell).
Thanks to the efforts of the Well Creek Trust, the waterway was brought back to life
and navigation restored in 1975, and it is now used by many pleasure craft.
The photo below shows the end of the Creek. the mooring point, Salters Lode Lock
(leading into the River Great Ouse), the road
bridge over it, and the lock-keepers cottage just to the right.
Photo: Peter Cox, 28/08/2007, Olympus SP550UZ
This is all part of the Middle Level system, administered by the Middle Level
Commissioners (MLC) and not actually part of the Ouse Washes. But there is a
connection, as you will see later ......
According to the Well Creek Trust
back to contents
Google satellite view
River Great Ouse on right.
Well Creek bottom left to topright.
Old Bedford River below, looking black
|
Salters Lode Lock
Photo: Peter Cox, 28/08/2007, Olympus SP550UZ
According to Samuel Wells, Register of the Bedford Level Corporation, a sluice was originally built here in 1630, and re-built in 1828, both times by BLC.
(Samuel
Wells, 1830 Vol 1 page 724). Summers say a new sluice was built here in 1826
(The Great Level, p.177).
(The differences in dates may indicate start and finish of construction.)
The Well Creek Trust handbook says that a simple sluice was built here in 1556,
and the Well Stream [then] ceased to be tidal. The handbook also says that the
sluice was "modernised and electrified" in the 1950s, and new gates were fitted
in 1981 (p12).
The northern (tidal) end has a steel vertical ("guillotine") gate. This was
installed in November 2008, replacing an earlier vertical gate. At the southern
end there are two sets of wooden vee gates; the
outermost pointing into Well Creek are about 12-13 feet high and hydraulically
controlled; the inner ones point inwards and are 5 feet higher and maually
operated. This double arrangement allows use of the lock regardless of whether
the tidal river level is higher or lower than in the Creek. Denver had a similar
layout with two sets of Vee doors both ends (see diagram on Denver Sluice page)
and I think that must have been the same here prior to 1981. The pivot and
recess for the inner inward facing vee gates at the tidal end are still evident,
but the lock walls beyond were rebuilt for the vertical gate.
Navigation through the earliest sluice was probably only possible for short
periods when the level in the tidal river Ouse was the same as that in Well
Creek.
When it became a navigable lock regardless of tides, I do not yet know, nor when the Middle Level
Commissioners took control from BLC.
Index and links
|