The Brittoniclanguages form one of the two branches of the Insular Celtic language family; the other is Goidelic. It comprises the extant languages Breton, Cornish, and Welsh. The name Brythonic was derived by Welsh Celticist John Rhys from the Welsh word Brython, meaning Ancient Britons as opposed to an Anglo-Saxon or Gael.
Loch is the Irish, Scottish Gaelic and Scots word for a lake or sea inlet. It is cognate with the Manx lough, Cornish logh, and one of the Welsh words for lake, llwch.
The toponymy of England derives from a variety of linguistic origins. Many English toponyms have been corrupted and broken down over the years, due to language changes which have caused the original meanings to be lost. In some cases, words used in these place-names are derived from languages that are extinct, and of which there are no known definitions. Place-names may also be compounds composed of elements derived from two or more languages from different periods. The majority of the toponyms predate the radical changes in the English language triggered by the Norman Conquest, and some Celtic names even predate the arrival of the Anglo-Saxons in the first millennium AD.
Derwentwater, or Derwent Water, is a lake in the Lake District in North West England, immediately south of Keswick. It is the third largest lake by area, after Windermere and Ullswater. It has a length of 4.6 kilometres (2.9 mi), a maximum width of 1.91 kilometres (1.19 mi), and an area of 5.4 square kilometres (2.1 sq mi). Its primary inflow and outflow is the River Derwent, which also flows through Bassenthwaite Lake before reaching the Irish Sea at Workington. There are several islands within the lake, one of which is inhabited. It is in the unitary authority of Cumberland and the ceremonial county of Cumbria.
Cumbric was a variety of the Common Brittonic language spoken during the Early Middle Ages in the Hen Ogledd or "Old North" in what is now the counties of Westmorland, Cumberland, northern Lancashire in Northern England and the southern Scottish Lowlands, alongside the Kingdom of Elmet in modern day Yorkshire. It was closely related to Old Welsh and the other Brittonic languages. Place name evidence suggests Cumbric may also have been spoken as far south as Pendle and the Yorkshire Dales. The prevailing view is that it became extinct in the 12th century, after the incorporation of the semi-independent Kingdom of Strathclyde into the Kingdom of Scotland.
Coniston Water is a lake in the Lake District in North West England. It is the third largest by volume, after Windermere and Ullswater, and the fifth-largest by area. The lake has a length of 8.7 kilometres, a maximum width of 730 metres (800 yd), and a maximum depth of 56.1 m. Its outflow is the River Crake, which drains into Morcambe Bay via the estuary of the River Leven. The lake is in the unitary authority of Westmorland and Furness, and the ceremonial county of Cumbria.
Wast Water or Wastwater is a lake located in Wasdale, a valley in the western part of the Lake District National Park, England. The lake is almost 3 miles (4.8 km) long and more than one-third mile (500 m) wide. It is a glacial lake, formed in a glacially 'over-deepened' valley. It is the deepest lake in England at 258 feet (79 m). The surface of the lake is about 200 feet (60 m) above sea level, while its bottom is over 50 feet (15 m) below sea level. It is owned by the National Trust.
Ullswater is a glacial lake in the Lake District in North West England. It is the second largest lake in the region by both area and volume, after Windermere. The lake is about 7 miles (11 km) long, 0.75 miles (1 km) wide, and has a maximum depth of 63 metres (207 ft). Its outflow is River Eamont, which meets the River Eden at Brougham Castle before flowing into the Solway Firth. The lake is in the administrative county of Westmorland and Furness and the ceremonial county of Cumbria.
Buttermere is a lake in the Lake District in North West England. It has a length of approximately 2 kilometres (1.2 mi) and a maximum width of 0.54 kilometres (0.34 mi), an area of 0.9 square kilometres (0.35 sq mi), a maximum depth of 28.6 metres (94 ft), and a surface elevation of 100.3 metres (329 ft) above sea level. Its primary outflow is Buttermere Dubs, a short stream which connects the lake to Crummock Water. From Crummock Water the River Cocker flows to Cockermouth, where it joins the River Derwent and finally enters the Irish Sea at Workington. The lake is in the unitary authority of Cumberland, and the ceremonial county of Cumbria.
In much of the "Old World" the names of many places cannot easily be interpreted or understood; they do not convey any apparent meaning in the modern language of the area. This is due to a general set of processes through which place names evolve over time, until their obvious meaning is lost. In contrast, in the "New World", many place names' origins are known.
Blennerhasset and Torpenhow is a civil parish in Cumbria, England. According to the 2001 census it had a population of 437, reducing to 423 at the 2011 Census. It includes the villages of Blennerhasset grid reference NY178415 and Torpenhow at NY202397 and the smaller settlement of Kirkland Guards at NY187401. It is located just outside the Lake District National Park. Baggrow railway station was immediately north of Blennerhasset.
Elter Water is a small lake in the Lake District in North West England, half a mile southeast of the village of the same name. It has a length of 0.62 miles (1.00 km), maximum width of approximately 0.24 miles (0.39 km), a maximum depth of 7 metres (7.7 yd), and an area of 0.16 square kilometres (0.062 sq mi). Its outflow is the River Brathay, which flows south to join Windermere near Ambleside. Windermere is itself drained by the River Leven, which flows into Morecambe Bay. The lake is in the unitary authority of Westmorland and Furness and the ceremonial county of Cumbria.
Gleaston is a village with a population of around 400 in the Furness area of South Cumbria, situated between the towns of Barrow-in-Furness, Dalton-in-Furness and Ulverston. Historically in Lancashire, the history of the village can be traced as far back as the mesolithic period and it was the centre of the manor of Muchland in the Middle Ages. Today it is largely a commuter village for the nearby towns, but its past is still visible in the remains of Gleaston Castle and Gleaston Water Mill, which is open as a tourist attraction.
Cumbrian dialect or Cumberland dialect is a local dialect of Northern England in decline, spoken in Cumberland, Westmorland and Lancashire North of the Sands. Sounding similar and not to be confused with the area's extinct Celtic language, Cumbric. Some parts of Cumbria have a more North-East English sound to them. Whilst clearly spoken with a Northern English accent, the Cumbrian dialect shares much vocabulary with Scots. A Cumbrian Dictionary of Dialect, Tradition and Folklore by William Rollinson exists, as well as a more contemporary and lighthearted Cumbrian Dictionary and Phrase Book.
Muchland is a medieval manor in Low Furness in the county of Cumbria in northern England. The manor was the seat of the Lords of Aldingham, and included at its peak the villages of Bardsea, Urswick, Scales, Stainton, Sunbrick, Baycliff, Gleaston, Aldingham, Dendron, Leece and Newbiggin. The area also features the historic remains of Gleaston Castle, Aldingham Castle, Gleaston Water Mill, the Druids' Temple at Birkrigg, plus many prehistoric remains around Urswick and Scales.
Ulpha is a small village and civil parish in the Duddon Valley in the Lake District National Park in Cumbria, England. Historically in Cumberland, it forms part of the Cumberland unitary authority area. At Ulpha a road leaves the Duddon Valley to cross Birker Fell to the valley of Eskdale. In the 2001 census the parish had a population of 159, reducing at the 2011 Census to 128.
Rydal Water is a small body of water in the central part of the English Lake District, in the county of Cumbria. It is located near the hamlet of Rydal, between Grasmere and Ambleside in the Rothay Valley.
Glenridding Dodd is a small fell in the English Lake District, at the end of a ridge descending from the Helvellyn range in the Eastern Fells. It stands above the village of Glenridding and on the western shore of Ullswater. Although small and not of great elevation, its top is a fine viewpoint for Ullswater and for the fells clustered round the valleys above Patterdale.
Howtown is a hamlet in Cumbria, England, situated at a small harbour on the east shore of Ullswater in the Lake District. It lies within the civil parish of Martindale.
