River Trent in the context of "Pennines"

Newark-on-Trent (/ˌnjuːərk -/) or Newark is a market town and civil parish in the Newark and Sherwood district in Nottinghamshire, England. It is on the River Trent, and was historically a major inland port. The A1 road bypasses the town on the line of the ancient Great North Road. The town's origins are likely to be Roman, as it lies on a major Roman road, the Fosse Way. It grew up around Newark Castle, St Mary Magdalene church and later developed as a centre for the wool and cloth trades.

In the English Civil War, it was besieged by Parliamentary forces and relieved by Royalist forces under Prince Rupert. Newark has a marketplace lined with many historical buildings and one of its most notable landmarks is St Mary Magdalene church with its towering spire at 232 feet (71 metres) high and the highest structure in the town. The church is the tallest church building in Nottinghamshire and can be seen when entering Newark or bypassing it. The population of the town was recorded at 30,345 at the 2021 census.

The archbishop of York is a senior bishop in the Church of England, second only to the archbishop of Canterbury. The archbishop is the diocesan bishop of the Diocese of York and the metropolitan bishop of the province of York, which covers the northern regions of England (north of the Trent) as well as the Isle of Man.

The archbishop's throne (cathedra) is in York Minster in central York, and the official residence is Bishopthorpe Palace in the village of Bishopthorpe outside York. The current archbishop is Stephen Cottrell, since the confirmation of his election on 9 July 2020.

The River Tame is a river in the West Midlands of England, and one of the principal tributaries of the River Trent. The Tame is about 95 km (59 mi) long from the source at Oldbury to its confluence with the Trent near Alrewas, but the main river length of the entire catchment, i.e. the Tame and its main tributaries, is about 285 km (177 mi).

It forms part of the Severn-Trent flyway, a route used by migratory birds to cross Great Britain.

The River Cole is a 25-mile-long (40-kilometre) river in the English Midlands. It rises on the lower slopes of Forhill, one of the south-western ramparts of the Birmingham Plateau, at Red Hill and flows south before flowing largely north-east across the plateau to enter the River Blythe below Coleshill, near Ladywalk, shortly before the Blythe meets the Tame. This then joins the Trent, whose waters reach the North Sea via the Humber Estuary. Its source is very near the main watershed of Midland England: tributaries are few and very short except in the lower reaches, so the Cole is only a small stream. The stretch between Shard End and Tyseley formed part of the historic border between Warwickshire and Worcestershire.

The River Blythe flows through the English Midlands from central Warwickshire, through the Borough of Solihull and on to Coleshill in north Warwickshire. It runs along the Meriden Gap in the Midlands Plateau, is fed by the River Cole and is a tributary of the River Tame beside the West Midland Bird Club's Ladywalk reserve. This then joins the River Trent, whose waters reach the North Sea via the Humber Estuary.

The river rises at various sources near Earlswood Lakes, but the principal tributary is listed as Spring Brook (52°21′03″N 1°50′37″W / 52.350915°N 1.843601°W / 52.350915; -1.843601; grid reference SP107725). From here it winds north east, skirting Cheswick Green, towards Solihull. Here it passes through a local wildlife park, Malvern and Brueton Park and Nature Reserve, where it briefly splits/outpours for approximately 250 metres to form Brueton Park Lake. From here it meanders east, past several old country houses—Old Berry Hall, Ravenshaw Hall and Eastcote Hall—before turning sharply south towards Barston, which is encircled within a large meander of the river. At Temple Balsall the Cuttle Brook feeds the river, which now arcs north, and again close by Barston. Past Hampton in Arden the river is fed by Shadow Brook, at Diddington Hall. Travelling further north it passes to the east of Coleshill, and is fed by the River Cole, only a few hundred yards before it itself feeds into the River Tame (52°31′20″N 1°41′18″W / 52.522317°N 1.688242°W / 52.522317; -1.688242; grid reference SP212916), at Ladywalk Nature Reserve.

Burton upon Trent, also known as Burton-on-Trent or simply Burton, is a market town in the borough of East Staffordshire in the county of Staffordshire, England, close to the border with Derbyshire. At the 2021 census, it had a population of 76,270. The demonym for residents of the town is Burtonian. Burton is located on the River Trent 11 miles (18 km) south-west of Derby and 20 miles (32 km) south of the Peak District National Park.

Burton is known for its brewing. The town grew up around Burton Abbey. Burton Bridge was also the site of two battles, in 1322, when Edward II defeated the rebel Earl of Lancaster and in 1643 when royalists captured the town during the First English Civil War. William Lord Paget and his descendants were responsible for extending the manor house within the abbey grounds and facilitating the extension of the River Trent Navigation to Burton. Burton grew into a busy market town by the early modern period.

Mercia (/ˈmɜːrsiə, -ʃə/) was one of the principal kingdoms founded at the end of Sub-Roman Britain; the area was settled by Anglo-Saxons in an era called the Heptarchy. It was centred on the River Trent and its tributaries, in a region now known as the Midlands of England.

The royal court moved around the kingdom without a fixed capital city. Early in its existence Repton seems to have been the location of an important royal estate. According to the Anglo-Saxon Chronicle, it was from Repton in 873–874 that the Great Heathen Army deposed the King of Mercia. Slightly earlier, King Offa seems to have favoured Tamworth. It was there where he was crowned, and where he resided during multiple Christmases.

The Humber /ˈhʌmbər/ is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers Ouse and Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Also known as the River Humber, it is tidal its entire length.

Below Trent Falls, the Humber passes the junction with the Market Weighton Canal on the north shore, the confluence of the River Ancholme on the south shore; between North Ferriby and South Ferriby and under the Humber Bridge; between Barton-upon-Humber on the south bank and Kingston upon Hull on the north bank (where the River Hull joins), then meets the North Sea between Cleethorpes on the Lincolnshire side and the long and thin headland of Spurn Head to the north.

The Derwent is a river in Derbyshire, England. It is 50 miles (80 km) long and is a tributary of the River Trent, which it joins south of Derby. The river's course is largely in the Peak District and its foothills.

Much of the river's route, with the exception of the city of Derby, is rural. However, the river has also seen many human uses, and between Matlock and Derby was one of the cradles of the Industrial Revolution. It is the site of the Derwent Valley Mills, the first industrial-scale cotton mills. Today it provides a water supply to several surrounding cities, and its steep-sided valley is an important communications corridor through the uplands of the Peak District.