Rothbury is a market town and civil parish in Northumberland, England, on the River Coquet. It is 14 miles (22.5 km) northwest of Morpeth and 26 miles (42 km) of Newcastle upon Tyne. At the 2011 Census, it had a population of 2,107.
Morpeth is a historic market town in Northumberland, North East England, lying on the River Wansbeck. Nearby towns include Ashington and Bedlington. In the 2011 census, the population of Morpeth was given as 14,017, up from 13,833 in the 2001 census. The earliest evidence of settlement is believed to be from the Neolithic period, and some Roman artifacts have also been found. The first written mention of the town is from 1080, when the de Merlay family was granted the barony of Morpeth. The meaning of the town's name is uncertain, but it may refer to its position on the road to Scotland and a murder which occurred on that road. The de Merlay family built two castles in the town in the late 11th century and the 13th century. The town was granted its coat of arms in 1552. By the mid-1700s it had become one of the main markets in England, having been granted a market charter in 1200, but the opening of the railways in the 1800s led the market to decline. The town's history is celebrated in the annual Northumbrian Gathering.
Alnwick was a local government district of Northumberland, England. Its council was based in the town of Alnwick and the district had a population of 31,029 according to the 2001 census.
The River Coquet runs through the county of Northumberland, England, discharging into the North Sea on the east coast at Amble. It rises in the Cheviot Hills on the border between England and Scotland, and follows a winding course across the landscape ("Coquetdale"). The upper reaches are bordered by the Otterburn Ranges military training ground, and are crossed by a number of bridges built in the 20th century. It passes a number of small villages and hamlets, and feeds one of the lakes created by extraction of gravel that form the Caistron Nature Reserve, before reaching the town of Rothbury, where it is crossed by a grade II listed bridge. Below the town is Thrum Mill, the restoration of which was featured on Channel 4 television.
Cartington is a village and former civil parish, now in the parish of Thropton, in Northumberland, England. It is about 11 miles (18 km) south west of Alnwick, and about 2 miles (3 km) north west of Rothbury. In 2019 it had an adult population of 95, after having returned a population of 97 in 2001.
Clifton is a hamlet in Northumberland, in England. The population is between 20 and 30. It is situated a short distance to the south of Morpeth, on the A1. It forms a trio with Hepscott and Glororum, a series of farms founded by the Brown brothers at the end of the 19th century. However, Clifton as a habitation stretches back earlier. In the 12th century lands were held at Clifton, under Roger de Merlay, by William of Clifton. There was a coaching inn here dating from the 17th century.
The Simonside Hills are a hill range in Northumberland, England near the town of Rothbury. Most of the hills are around 300–400 metres (980–1,310 ft) high and are popular spots for hikers in the area. The highest point is Tosson Hill at 440 metres (1,444 ft).
The A1068 is a road in northern England that runs from Seaton Burn in North Tyneside to Alnwick in Northumberland. The section between Ellington and Alnmouth is signposted as part of the Northumberland Coastal Route.
The Coquet Stop Line, which ran from Amble in Northumberland up the valley of the River Coquet, formed part of the defences constructed to meet the threat of a Nazi invasion during the Second World War. It was intended to slow the advance of the German army from the north to give time for a field army to assemble on the Tyne Stop Line around 30 miles to the south.
Barrowburn is a hamlet in Upper Coquetdale in the county of Northumberland, England. It comprises a working farm with associated buildings and two holiday lets. One of the holiday lets is the Old School House, which closed as a school in the 1970s. The settlement is situated by the River Coquet, at its confluence with Barrow Burn (stream), after which the settlement is named. There is a road bridge over the Coquet and a ford over the burn here.
Hepple is a small village and parish in rural Northumberland, 4 miles (6.4 km) west of Rothbury, which provides most of its local services. It is on the edge of the Northumberland National Park, and lies on the bank of the river Coquet, at a location which was on the Coquet Stop Line, of which a pillbox remains. It is on the road between Rothbury and Otterburn. The village contains a church, village hall and post office.
Stannington railway station was a railway station which served the village of Stannington in Northumberland, England. It was located on the East Coast Main Line. It was opened in 1847 as Netherton, and closed in 1958. The community around the location of the station is today known as Stannington Station.
David Dippie Dixon was an English local historian and writer on his native Northumberland.
The Northumberland Sandstone Hills are a major natural region in the English county of Northumberland. The hills form distinctive skylines with generally level tops, northwest facing scarps and craggy outcrops offering views to the Cheviots further west.
The geology of Northumberland in northeast England includes a mix of sedimentary, intrusive and extrusive igneous rocks from the Palaeozoic and Cenozoic eras. Devonian age volcanic rocks and a granite pluton form the Cheviot massif. The geology of the rest of the county is characterised largely by a thick sequence of sedimentary rocks of Carboniferous age. These are intruded by both Permian and Palaeogene dykes and sills and the whole is overlain by unconsolidated sediments from the last ice age and the post-glacial period. The Whin Sill makes a significant impact on Northumberland's character and the former working of the Northumberland Coalfield significantly influenced the development of the county's economy. The county's geology contributes to a series of significant landscape features around which the Northumberland National Park was designated.
Harwood Forest is a 3,527 hectares conifer plantation located to the south of Rothbury in North Northumberland, England, and managed by Forestry England.
The geology of Northumberland National Park in northeast England includes a mix of sedimentary, intrusive and extrusive igneous rocks from the Palaeozoic and Cenozoic eras. Devonian age volcanic rocks and a granite pluton form the Cheviot massif. The geology of the rest of the national park is characterised largely by a thick sequence of sedimentary rocks of Carboniferous age. These are intruded by Permian dykes and sills, of which the Whin Sill makes a significant impact in the south of the park. Further dykes were intruded during the Palaeogene period. The whole is overlain by unconsolidated sediments from the last ice age and the post-glacial period.
