River Roach
The River Roach is a river that flows entirely through the English county of Essex. It is one of four main streams that originate in the Rayleigh Hills to the west, and flow east. They then flow towards the centre of the Rochford Basin, a circular feature which may have been caused by an asteroid impact in the Late Oligocene or Early Miocene periods. To the east of Rochford, the river becomes tidal, and is governed by the Crouch Harbour Authority. It joins the River Crouch between Wallasea Island and Foulness Island. To the west of Rochford, there is some doubt as to which of the four streams is officially the Roach.
At Stambridge, there was a tidal mill from at least the 1500s, although few details are known until it was rebuilt in 1809. A pound was filled by the incoming tide, and was released to drive a water wheel as the tide fell. On spring tides, this gave around 7 hours of operation, which gradually decreased as the tides reduced, and at neap tides, the operation of the mill was entirely dependent on the flow from the upper river. Rankins, the millers, objected to plans by the Great Eastern Railway to build a dam and reservoirs in Rochford, as it would damage their operation, but a single reservoir was authorised in 1904.
The river channels are designated as "heavily modified" from their natural state by the Environment Agency, who measure the water quality. This is moderate for most of the tributaries, and the chemical status has improved since 2013. Charles Darwin's HMS Beagle was moored on the river from 1850 as a Coast Guard watch ship. It was sold for breaking, but an archaeological survey concluded in 2008 that much of it still remains buried beneath the mud near Paglesham. The Paglesham Reach is also significant for its native oysters.
Geology
The River Roach flows across the Rochford Basin, a nearly circular topographical basin, with Rochford near its centre. To the south is the River Thames, and to the north, the River Crouch, but the basin is surrounded on three sides by the low hills of Canewdon, Ashingdon, Hockley, Eastwood, Westcliff-on-Sea, Prittlewell and Southend-on-Sea. These continue in a westerly and south-westerly direction to become the Rayleigh Hills, in Rayleigh and Thundersley. The basin is approximately in diameter, and its base consists of London Clay covered by a layer of sands, gravels, and river brick-earths, dating from the Upper Pleistocene period. The hills also consist of London Clay in their lower levels, but are covered by Claygate Beds, between thick, and where they are highest, by Bagshot Beds.Four main streams drain from the Rayleigh Hills, and flow in a generally easterly direction until they reach the Rochford Basin. The southernmost is the Prittle Brook. Next comes the Eastwood Brook, and then the Noblesgreen Ditch. The fourth stream originates in Hockley Woods, and is joined by a fifth in Hawkwell, on the edge of the Rochford Basin. Once they enter the basin, they all flow towards its centre, and join up near Rochford. The way in which they are all roughly parallel until they reach the basin, and then change direction, together with the presence of a small chalk inlier near Stambridge Mill, when the chalk layer throughout the area is between below sea level, has led Stratford to suggest that the Rochford Basin may be the result of an impact by an asteroid in the Late Oligocene or Early Miocene periods.
Names
Rochford takes its name from Rochefort, Old English for "Ford of the Hunting Dogs". The River Roach was originally called the "Walfleet" or "Walflete". It is believed that it was renamed the Roach in what is known as a back formation. This is where it is assumed that Rochford means ford over the River Roach, so they could have renamed the river to fit the theory. Until the 1900s, Oysters from the River Roach and sometimes from the River Crouch were called Walfleet Oysters.Which one of the four main streams draining the Rayleigh Hills and entering the Rochford Basin is the Roach is ambiguous. Modern Ordnance Survey maps, and all historical editions since they were first published, do not name any of the streams to the west of Rochford. Essex County Council, who publish a 16-page walking guide to the Roach Valley Way, a route around the district, label the third stream as the River Roach. The Environment Agency, who are responsible for measuring the water quality of English rivers, label the third stream as the Noblesgreen Ditch, and the fourth stream, from Hockley and Hawkwell, as the Roach. However, the Strategic Flood Risk Assessment prepared for Rochford District Council includes a map of the tributaries of the Roach, on which the third stream is called Noblesgreen Ditch, and parts of the fourth stream are called the Hawkwell Brook and River Roach. This usage has been followed here.
Routes
Noblesgreen Ditch
Noblesgreen Ditch rises in the hill near The Gattens and Nelson Road, which are either side of Hockley Road, Rayleigh. The stream is joined by several others, and then runs south, under Bull Lane, beside then under The Chase where it turns to run east behind Milton Close and Bramfield Road East. It then passes north of the Grove Playing Fields, and past Rayleigh Sewage Works where its flow is augmented by the discharge from the reed-bed purification system. With an outflow of 179 litres/second or 15534 m3/day, the sewage works is the largest flow into the ditch. It runs south of Rewreth Hall Wood, north of Grove Woods, and past New England Wood. From there, it flows through the Cherry Orchard Jubilee Country Park, past The Scrubs where a weir supplies a feeder channel to the 1.2 ha Cherry Orchard Lake. The stream flows under Cherry Orchard Way, past Southend Airport and on through Rochford Hundred Golf Course, where it is joined by Eastwood Brook, to reach Rochford. It passes under the Shenfield to Southend Line, and then over a weir, which ensures that water fills Rochford Reservoir, built by the Great Eastern Railway in 1904. Then it is joined by the Roach, and the overflow from the reservoir empties into it soon afterwards.Eastwood Brook
The Eastwood Brook is a 7.519 km watercourse comprising one of the tributaries of the River Roach. It has a catchment area of 1133.71 ha. It arises adjacent to the Weir roundabout, at an elevation of 200 ft above ordnance datum. It flows in an easterly direction to the north of Wyburns school, then south-east to Rayleigh Downs Road. It then runs south of, and parallel to, Rayleigh Road before flowing under Rayleigh Road, Whitehouse Lane, Western Approaches, Cherry Orchard Way and Aviation Way. It then flows in a north-easterly direction along the western boundary of Southend Airport to join the Noblesgreen Ditch at Rochford Golf Course. The Eastwood Brook has an Environment Agency monitoring station at Cherry Orchard Way.Hawkwell Brook
The Hawkwell Brook rises on the edge of Hockley Woods, to the north of the former HM Prison Bullwood Hall. It flows eastwards, through the woods and to the south of Great Bull Wood, and runs across the northern end of Belchamps Scout Centre. It is culverted under Elmwood Avenue, and re-emerges to pass under the B1013 Main Road and Thorpe Close in Hawkwell. From this point it is designated as a main river, and is therefore the responsibility of the Environment Agency. It flows to the south of the Clements Hall Sports Complex, to be joined by the Hockley Brook, which rises near Southbourne Grove, Hockley, flows under the Shenfield to Southend Railway and then alongside it, to the junction on the north side of Rectory Road. Now officially the Roach, it turns to the south east, passing under Rectory Road, and continuing to Rochford, running broadly parallel to Ironwell Lane. It then crosses beneath the railway and Hall Road, running beside Bradley Way to reach its junction with Noblesgreen Ditch by Rochford Reservoir.At Salt Bridge it passes under South Street beside the Horse and Groom public house. The River Roach then continues east, running through flood plain marshes before discharging into the northern arm of the River Roach at Stambridge Mills, downstream from the town. Just after this point, Sutton Wharf with jetties, slipways, a boatyard and moorings, is on the south bank. This is where its main tributary, the Prittle Brook from Leigh-on-Sea and Southend-on-Sea joins as its southern arm.
The tidal river
From Stambridge Mills eastwards, the River Roach is tidal and becomes a wide river. It passes Great Stambridge Hall, Mucking Hall, Barton Hall and Roper's Farm. Barlinghall Creek joins Potton Creek and is called "The Violet" before it joins the Roach on the right bank. From here the Roach is about wide. It passes Paglesham, significant for its native oysters and the location of Charles Darwin's HMS Beagle which lies under the mud west of Paglesham's boatyard and slipway. After being retired from the Royal Navy in 1845, the vessel was used by the Coast Guard as a watch ship. It was moved to the centre of the river near Paglesham in 1850, eventually becoming Watch Ship No. 7. Its condition deteriorated, and it was moved to the shore in 1863, to be sold for breaking up in 1870. A six-year archaeological investigation ending in 2008 concluded that much of the vessel still lies beneath of mud near to the Paglesham hard.Further east, it meets Paglesham Pool on the north bank, a creek which separates Wallasea Island from the mainland, although it is no longer an island, as a causeway has been built across the creek to carry the road onto Wallasea. At Potton Point on Devil's Reach, the Middleway creek, which separates the islands of Potton and Foulness, joins from the south and defines the western edge of Foulness Island. The Middleway creek splits to pass either side of Rushley Island, and becomes Havengore Creek once the two channels rejoin. Shallow-draughted boats can use Havengore Creek to access the river, but the route needs careful preparation, as there is a lifting bridge carrying the road to Foulness Island, which is only opened for a limited period either side of high tide. In addition, Havengore Creek opens out onto Maplin Sands, and boaters must check that the Shoebury Artillery Range is not in operation before crossing the sands. The Roach passes eastwards between Foulness Island and Wallasea Island and then it turns northwards between them, where it widens to almost until it joins the River Crouch at Wallasea Ness on the Ness Hole. The combined rivers then flow eastwards past Holliwell Point and discharge into the North Sea at Foulness Point.