Rothbury is a town and civil parish in Northumberland, England, on the River Coquet, 13.5 miles (21.7 km) northwest of Morpeth and 26 miles (42 km) of Newcastle upon Tyne. At the 2001 Census, it had a population of 2,107. It is sometimes referred to as the ‘capital of Coquetdale’
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. 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.
Warkworth is a village in Northumberland, England. It is probably best known for its well-preserved medieval castle, church and hermitage. The population of Warkworth was 1,493 in 2001, increasing to 1,574 at the 2011 Census. The village is situated in a loop of the River Coquet, about 1 mile (1.6 km) from the Northumberland coast and lies on the main A1068 road. It is 30 miles (48 km) north of Newcastle, and about 40 miles (64 km) south of the Scottish border. An ancient bridge of two arches crosses the river at Warkworth, with a fortified gateway on the road mounting to the castle, the site of which is surrounded on three sides by the river.
Haltwhistle is a market town and civil parish in Northumberland, England, 10 miles (16 km) east of Brampton. It had a population of 3,811 at the 2011 Census.
Guyzance, historically Guizance, is a small village or hamlet in Northumberland, England. It is located on the River Coquet, roughly 6 miles south of Alnwick and around 3 miles west of Amble. Guyzance is one of only two places in Great Britain with a -zance ending; the other is Penzance in Cornwall. The similar names are co-incidence however.
The Simonside Hills are a hill range in Northumberland, England near the town of Rothbury. Most of the hills are around 300 metres (984 ft) to 400 metres (1,312 ft) high and are popular spots for hikers in the area. The highest point is Tosson Hill at 440 metres (1,444 ft).
Gosforth is a suburb of the city of Newcastle upon Tyne, Tyne and Wear, North East England. It is situated to the north of Central Newcastle. Gosforth constituted a separate urban district from 1895 until 1974. In 2001, it had a population of 23,620.
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 World War II. 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.
Swarland is a small modern village in the county of Northumberland, England, situated about 7 miles (11 km) south of the market town of Alnwick and 25 miles (40 km) north of the city of Newcastle upon Tyne. Swarland's 'village rival' is Felton. Swarland is the highest settlement between London and Edinburgh.
Elsdon is a village and civil parish in the English county of Northumberland about 10 miles (16 km) to the southwest of Rothbury. The name is derived from the Old English meaning Elli's valley.
Harbottle Castle is a ruined medieval castle situated at the west end of the village of Harbottle, Northumberland, England, 9 miles (14 km) west-north-west of Rothbury overlooking the River Coquet. It is a Scheduled Ancient Monument and a Grade I listed building.
Longframlington is a small village in Northumberland, England, located on the A697, 11 miles (18 km) north-west of Morpeth and 5 miles (8 km) south-east of Rothbury. Longframlington is a former pit village and on the site of the pit now stands Fram Park, a log cabin holiday park. The village was previously the site of the Longframlington Music Festival.
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.
David Dippie Dixon was an English local historian and writer on his native Northumberland.
The Northumberland Sandstone Hills are a major natural region that lies entirely within the English county of Northumberland. Their sandstone hills form distinctive skylines with generally level tops, northwest facing scarps and craggy outcrops offering exceptional 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.
Rothbury Racecourse was a horse racing venue in Northumberland, England which closed in 1965. It was situated just outside the village of Rothbury, on a plain by the River Coquet.
Harwood Forest is a 3,527 hectares conifer plantation located to the south of Rothbury in North Northumberland, England, and managed by the Forestry Commission.
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.
