The River Aire is a major river in Yorkshire, England, 92 miles (148 km) in length. Part of the river below Leeds is canalised, and is known as the Aire and Calder Navigation.
The River Don is a river in South Yorkshire and the East Riding of Yorkshire, England. It rises in the Pennines, west of Dunford Bridge, and flows for 69 miles (111 km) eastwards, through the Don Valley, via Penistone, Sheffield, Rotherham, Mexborough, Conisbrough, Doncaster and Stainforth. It originally joined the Trent, but was re-engineered by Cornelius Vermuyden as the Dutch River in the 1620s, and now joins the River Ouse at Goole. Don Valley is a UK parliamentary constituency near the Doncaster stretch of the river.
The River Sheaf in Sheffield, South Yorkshire, England, flows northwards, past Dore, through Abbeydale and north of Heeley. It then passes into a culvert, through which it flows under the centre of Sheffield before joining the River Don. This lower section of the River Sheaf, together with the Don between the Blonk Street and Lady's Bridges, formed two sides of the boundary of Sheffield Castle.
The Porter Brook is a river which flows through the City of Sheffield, England, descending over 1,000 feet (300 m) from its source on Burbage Moor to the west of the city to its mouth where it joins the River Sheaf in a culvert beneath Sheffield railway station. Like the other rivers in Sheffield, its steep gradient made it ideal for powering water mills and works associated with the metalworking and cutlery industries, and around 20 dams were constructed over the centuries to facilitate this. At its lower end, it is extensively culverted, but parts of it are gradually being restored to open channels, as part of a daylighting scheme for the city.
The River Rother, a waterway in the northern midlands of England, gives its name to the town of Rotherham and to the Rother Valley parliamentary constituency. It rises in Pilsley in Derbyshire and flows in a generally northwards direction through the centre of Chesterfield, where it feeds the Chesterfield Canal, and on through the Rother Valley Country Park and several districts of Sheffield before joining the River Don at Rotherham in Yorkshire. Historically, it powered mills, mainly corn or flour mills, but most had ceased to operate by the early 20th century, and few of the mill buildings survive.
The River Loxley is a river in the City of Sheffield, South Yorkshire, England. Its source is a series of streams which rise some 10 miles (16 km) to the north-west of Sheffield on Bradfield Moors, flowing through Bradfield Dale to converge at Low Bradfield. It flows easterly through Damflask Reservoir and is joined by Storrs Brook at Storrs, near Stannington, and the River Rivelin at Malin Bridge, before flowing into the River Don at Owlerton, in Hillsborough. The Loxley valley provided the initial course of the Great Sheffield Flood, which happened after the Dale Dyke Dam collapsed shortly before its completion in March 1864.
The River Kent is a short river in the county of Cumbria in England. It originates in hills surrounding Kentmere, and flows for around 20 miles (32 km) into the north of Morecambe Bay. The upper reaches and the western bank of the estuary are located within the boundaries of the Lake District National Park. The river flows in a generally north to south direction, passing through Kentmere, Staveley, Burneside, Kendal and Sedgwick. Near Sedgwick, the river passes through a rock gorge which produces a number of low waterfalls. This section is popular with kayakers as it offers high quality whitewater for several days after rain. The village of Arnside is situated on the east bank of the Kent estuary, just above Morecambe Bay, and a tidal bore known as the Arnside Bore forms in the estuary at this point on high spring tides.
The Little Don River also known as the Porter, is a tributary of the River Don in South Yorkshire, England. Arising on the Langsett Moors in the northern Peak District, the Little Don River feeds the Langsett and Underbank Reservoirs. It runs through the town of Stocksbridge before joining the River Don.
The Blackburn Brook is a stream in Sheffield, South Yorkshire, England which flows through the Blackburn Valley along the M1 and Ecclesfield Road and joins the River Don near the Meadowhall shopping centre. Downstream from the A61 road at Chapeltown the Blackburn Brook is defined as a main river by the Environment Agency, which requires new building development to be at least 26 feet (8 m) from the bank side as a flood defence measure and to allow access to the watercourse for maintenance.
Peasey Beck is a 19.6-kilometre-long (12.2 mi) beck flowing through Cumbria, England. It rises on Lambrigg Fell where it is known as the Sparishaw Beck, flows through Killington Reservoir and converges with Stainton Beck to form the River Bela at Milnthorpe. Prior to 1913, it was known as the River Beela throughout its length.
Stainton Beck is a watercourse in Cumbria, England. Its upper reaches are known as St. Sunday's Beck.
Skipton Wood is a 36-acre (15 ha) wood following the valley of Eller Beck to the north of Skipton behind Skipton Castle in North Yorkshire, England. The wood is owned by Skipton Castle but has been leased to the Woodland Trust.
Kentmere Reservoir is a water storage facility situated in the Kentmere valley in the county of Cumbria, England. It is located 10.5 kilometres (6.5 mi) north-northeast of the town of Windermere. The reservoir is fed by the streams which form the headwaters of the River Kent which rise 1.5 kilometres (0.93 mi) to the north in Hall Cove on the southern slopes of a mountainous ridge called High Street, which is named after the nearby Roman road. It is also fed by Lingmell Gill, which drains the large corrie on the western side of Harter Fell beneath the Nan Bield Pass.
The River Drone is a river which flows south from its source on the Sheffield, South Yorkshire, border. It flows through Dronfield, Unstone and Unstone Green in Derbyshire before merging at Sheepbridge to the north of Chesterfield with the Barlow Brook. Below the junction, it is often referred to as the River Whitting. It then flows south-east till it merges with the River Rother at Brimington Road North (B6050) at Chesterfield. It is one of the three main tributaries of the Rother.
Bedale Beck is a river that flows through the eastern end of Wensleydale and passes through Crakehall, Bedale and Leeming before entering the River Swale at a point between Morton-on-Swale and Gatenby. Between source and mouth its length is 25.7 miles (41 km).
Skipton Golf Club is a golf club located within the English county of North Yorkshire. Founded within 1893, the club was originally located a short distance away in the village of Gargrave before moving to its present site just outside the market town of Skipton in 1896.
Pickering Beck is a river that runs for over 18 miles (29 km) from its source in the North York Moors National Park through the town of Pickering and on to its confluence with Costa Beck at Kirby Misperton. It is a meandering river that is fed by numerous named and unnamed becks and streams which flow over sandstone and limestone beds and an alluvia of sand, clay silt and gravel. The beck is known for flooding and in recent times has been a beneficiary of funding and experimental flood protection schemes.
Walverden Water is a minor river in Lancashire, England. It is approximately 2.6 miles (4.2 km) long and has a catchment area of 5.04 square miles (1,304.23 ha).
Wyke Beck is a stream that runs from Roundhay Park to the River Aire in east Leeds, West Yorkshire, England. Described as an Urban Beck, the stream flows through housing estates and then an industrial landscape in its lower reaches. Wyke Beck has been prone to flooding so often, that remediation of its course and flood storage schemes have been initiated by Leeds City Council.
Holgate Beck is a small watercourse that flows north-eastwards through Holgate across the west side of the City of York, England. Primarily flowing through Holgate, from which it derives its name, the beck drains a large part of Askham Bog and Hob Moor, then running underneath the various lines near York railway station. It empties into the River Ouse at Water End, being one of five main tributaries for the River Ouse in York, and consequently added to the flooding in the river and immediate environs. To counter this, some flood diversionary schemes have been implemented near to Askham Bog and Hob Moor.
