A glen is a valley, typically one that is long and bounded by gently sloped concave sides, unlike a ravine, which is deep and bounded by steep slopes. The word is Goidelic in origin: gleann in Irish and Scottish Gaelic, glion in Manx. The designation "glen" also occurs often in place names. Glens are appreciated by tourists for their tranquility and scenery.
The Pennines, also known as the Pennine Chain or Pennine Hills, are a range of uplands mainly located in Northern England. Commonly described as the "backbone of England" because of its length and position, the range runs from Derbyshire and Staffordshire in the North Midlands to Northumberland in North East England, near the Anglo-Scottish border. The range starts near the valley of the River Trent to the south and extends northwards across the Peak District, South Pennines, Yorkshire Dales, and North Pennines, ending at the Tyne Gap. Beyond the gap are the Border Moors and Cheviot Hills, which are included in some definitions of the range.
Wooler is a town in Northumberland, England. It lies on the edge of the Northumberland National Park, near the Cheviot Hills. It is a popular base for walkers and is referred to as the "Gateway to the Cheviots". As well as many shops and pubs, the town has a youth hostel, many hotels, and campsites. It lies on the St. Cuthbert's Way long-distance footpath between Melrose Abbey and Lindisfarne.
The River Aln runs through the county of Northumberland in England. It rises in Alnham in the Cheviot Hills and discharges into the North Sea at Alnmouth on the east coast of England.
The River Esk, sometimes called the Cumbrian Esk, is a river in Cumbria, England. It flows for approximately 25 km from its source in the Scafells range of mountains to its estuary at Ravenglass. The valley it flows through is known as Eskdale. It is one of two Rivers Esk in Cumbria, and not to be confused with the Border Esk which flows into Cumbria from Scotland.
The Cheviot is an extinct volcano and the highest summit in the Cheviot Hills and in the county of Northumberland. Located in the extreme north of England, it is a 1+1⁄4-mile (2-kilometre) walk from the Scottish border and, with a height of 2,674 feet above sea-level, is located on the northernmost few miles of the Pennine Way, before the descent into Kirk Yetholm.
The River Till is a river of north-eastern Northumberland. It is a tributary of the River Tweed, of which it is the only major tributary to flow wholly in England. Upstream of the locality of Bewick Bridge, 8.5 km to the southeast of Wooler the river is known as the River Breamish. It rises on Comb Fell in the Cheviot Hills.
Otterburn is a small village in Northumberland, England, 31 miles (50 km) northwest of Newcastle upon Tyne on the banks of the River Rede, near the confluence of the Otter Burn, from which the village derives its name. It lies within the Cheviot Hills about 16 miles (26 km) from the Scottish border. The parish of Otterburn is at the heart of Redesdale, a Northumbrian upland valley.
Ingram is a small village and civil parish in Northumberland, England. It is located in the Cheviots on the River Breamish, and on the edge of Northumberland National Park; it houses a National Park visitor centre.
Eglingham is a village in Northumberland, England, situated about 7 miles (11 km) north-west of Alnwick and 10 miles (16 km) from Wooler. It lies in the sheltered valley of the Eglingham Burn, a tributary of the River Aln, about 100 metres (330 ft) above sea level, in a rural conservation area set amongst rolling countryside, within 5 miles (8 km) of the Cheviot Hills. The village is surrounded by mainly arable farmland, moorland and woodland, including an arboretum and some commercial forestry.
Mindrum is a village in Northumberland, England, in the district of Berwick-upon-Tweed. Now little more than a postal address, it forms the centre of a number of farms.
The Douglas Water is a river in South Lanarkshire of south-central Scotland. It is a tributary of the River Clyde.
The River Gelt is a river in Cumbria, England and a tributary of the River Irthing.
Hedgehope Hill is a mountain in the Cheviot Hills of north Northumberland in northeast England, and categorised as a Hewitt. It is the second-highest mountain in the area after The Cheviot itself.
The Battle of Piperdean was an engagement in the Scottish Borders, fought on 10 September 1435 between the Kingdom of Scotland and the Kingdom of England.
The Cheviot Hills, or sometimes The Cheviots, are a range of uplands straddling the Anglo-Scottish border between Northumberland and the Scottish Borders. The English section is within the Northumberland National Park. The range includes The Cheviot, plus Hedgehope Hill to the east, Windy Gyle to the west, and Cushat Law and Bloodybush Edge to the south.
The Usway Burn is an upland river on the southern flanks of the Cheviot Hills, in the Northumberland National Park, England.
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.
Linhope is a small village in the civil parish of Ingram, in Northumberland, England. It is located in the Cheviots on the River Breamish, and within Northumberland National Park.
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.
