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Kentmere
Kentmere is a valley, village and civil parish in the Lake District National Park, a few miles from Kendal in the South Lakeland district of Cumbria, England. Historically in Westmorland, at the 2011 census Kentmere had a population of 159. Geography The narrow valley spans about in length and begins with a bowl of hills known as the Kentmere Round; a horseshoe of high fells which surrounds Kentmere Reservoir. The River Kent, which gives Kendal its name, begins from Hall Cove, a corrie at the head of the valley, before flowing through the reservoir. Access to this part of the valley is available via the Roman High Street, over Nan Bield Pass, from Troutbeck over Garburn Pass ( Bridleway only. No motor vehicles), or along an old bridleway up from the village. The valley is sandwiched between Troutbeck on the west side and Longsleddale on the east. It can be reached by road only by travelling through the village of Staveley, which sits at its mouth where the river meets the ...
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River Kent
The River Kent is a short river in the county of Cumbria in England. It originates in hills surrounding Kentmere, and flows for around 20 miles (32 km) into the north of Morecambe Bay. The upper reaches and the western bank of the estuary are located within the boundaries of the Lake District National Park. The river flows in a generally north to south direction, passing through Kentmere, Staveley, Burneside, Kendal and Sedgwick. Near Sedgwick, the river passes through a rock gorge which produces a number of low waterfalls. This section is popular with kayakers as it offers high quality whitewater for several days after rain. The village of Arnside is situated on the east bank of the Kent estuary, just above Morecambe Bay, and a tidal bore known as the Arnside Bore forms in the estuary at this point on high spring tides. The river has been used as a source of power since at least the 13th century. In 1848, the construction of Kentmere Reservoir was completed, which was ...
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Kentmere Reservoir
Kentmere Reservoir is a water storage facility situated in the Kentmere valley in the county of Cumbria, England. It is located north-northeast of the town of Windermere. The reservoir is fed by the streams which form the headwaters of the River Kent which rise to the north in Hall Cove on the southern slopes of a mountainous ridge called High Street, which is named after the nearby Roman road. It is also fed by Lingmell Gill, which drains the large corrie on the western side of Harter Fell beneath the Nan Bield Pass. After Kentmere Tarn was drained to provide agricultural land in the 1840s, water supply to the mills further downstream became erratic, and the mill owners met to plan a reservoir to regulate the flow. They employed the water engineer John Frederick Bateman to advise, and the Act of Parliament obtained in 1845 authorised five reservoirs. Despite Bateman's preference for the reservoir at Skeggles Water, the millers opted to build that at Kentmere Head, which was c ...
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Staveley, Cumbria
Staveley () is a village in the South Lakeland district, in Cumbria, England. Historic counties of England, Historically part of Westmorland, it is situated northwest of Kendal where the River Kent is joined by its tributary the River Gowan, Cumbria, Gowan. It is also known as Staveley-in-Westmorland and Staveley-in-Kendal to distinguish it from Staveley-in-Cartmel (a small village near Newby Bridge which is now in Cumbria but was previously in Lancashire). There are three civil parishes – Nether Staveley, Over Staveley and Hugill (part). Their total population at the 2011 Census was 1,593 but this includes those living in the hamlet of Ings, Cumbria, Ings in Hugill parish. Governance Historic counties of England, Historically within the county of Westmorland, it became part of the new non-metropolitan county of Cumbria in 1974. Staveley is divided between three civil parishes; * The village south of the rivers Gowan and Kent is in Nether Staveley, * Most of the village nor ...
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Longsleddale
Longsleddale () is a valley and civil parish in the South Lakeland district of the English county of Cumbria. It includes the hamlet of Sadgill. The parish has a population of 73. As the population taken at the 2011 Census was less than 100, details are maintained in the civil parish of Whitwell and Selside. The valley is bounded to the west by Kentmere Pike and Shipman Knotts, one arm of the ''Kentmere Horseshoe'', and to the east by Sleddale Fell and its summits of Grey Crag and Tarn Crag; one of several Cumbrian hills named Great Howe is on the east of the valley above Sadgill. The River Sprint starts on the slopes of Harter Fell and Branstree, and flows south through the valley before joining the River Kent to the north of the town of Kendal. Half-way between Garnett Bridge and Sadgill, Ubarrow Hall is a mediaeval pele tower, reduced in height, adjoining a 17th-century farmhouse. Haweswater aqueduct The aqueduct carrying water from Haweswater Reservoir to Heaton Park Rese ...
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Garburn Pass
Hill passes of the Lake District were originally used by people in one valley travelling to another nearby without having to go many miles around a steep ridge of intervening hills. Historically, in the Lake District of northwest England, travel on foot or by pony was difficult because of the region's steep-sided valleys so tracks across the ridges were created taking the easiest route over passes – often, but not always, via a col. Since Roman times long-distance travel had tended to be along ridges. From the 19th century these passes and ridge routes were brought back into use when recreational hill walking become popular. Forty hill passes within the Lake District National Park are listed here, using criteria for selecting the major routes. Background The Lake District National Park was created in 1951 covering an area of over and, although its population is only 42,000, over 10 million visitors arrive each year, mostly attracted by the lakes and fells. Geology Abou ...
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Nan Bield Pass
Hill passes of the Lake District were originally used by people in one valley travelling to another nearby without having to go many miles around a steep ridge of intervening hills. Historically, in the Lake District of northwest England, travel on foot or by pony was difficult because of the region's steep-sided valleys so tracks across the ridges were created taking the easiest route over passes – often, but not always, via a col. Since Roman times long-distance travel had tended to be along ridges. From the 19th century these passes and ridge routes were brought back into use when recreational hill walking become popular. Forty hill passes within the Lake District National Park are listed here, using criteria for selecting the major routes. Background The Lake District National Park was created in 1951 covering an area of over and, although its population is only 42,000, over 10 million visitors arrive each year, mostly attracted by the lakes and fells. Geology Abou ...
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Westmorland
Westmorland (, formerly also spelt ''Westmoreland'';R. Wilkinson The British Isles, Sheet The British IslesVision of Britain/ref> is a historic county in North West England spanning the southern Lake District and the northern Dales. It had an administrative function from the 12th century until 1974. Between 1974 and 2023 Westmorland lay within the administrative county of Cumbria. In April 2023, Cumbria County Council will be abolished and replaced with two unitary authorities, one of which, Westmorland and Furness, will cover all of Westmorland (as well as other areas), thereby restoring the Westmorland name to a top-tier administrative entity. The people of Westmorland are known as Westmerians. Early history Background At the beginning of the 10th century a large part of modern day Cumbria was part of the Kingdom of Strathclyde, and was known as '' "Scottish Cumberland" ''. The Rere Cross was ordered by Edmund I (r.939-946) to serve as a boundary marker between England an ...
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High Street (Lake District)
High Street is a fell in the English Lake District. At 828 metres (2,718 ft), its summit is the highest point in the far eastern part of the national park. The fell is named after the Roman road which ran over the summit. History Roman road A Roman road, a scheduled monument, crosses the fell between Roman forts at Brougham ('' Brocavum'') near Penrith and Ambleside ('' Galava''). Although the route takes the road higher than any other Roman road in England, the High Street range has quite gentle slopes and a flat summit plateau, characteristics that may have persuaded Roman surveyors to build the road over the fell tops rather than through the valleys which were densely forested and marshy making them susceptible to ambush. There has been speculation that the Romans made use of a prehistoric trackway. The nature of the Roman road remains problematic, as much of it is sunken in a hollow, rather than being built on top of an embankment or ''agger'' in the usual ...
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High Knott
High Knott, marked on some Ordnance Survey maps as Williamson's Monument, is a hill in the eastern part of the English Lake District, near Staveley, Cumbria. The monument on its summit was built by the Reverend T. Williamson in 1803, in memory of his father Thomas Williamson, who had climbed the fell every day before breakfast. The fell is the subject of a chapter of Wainwright's book ''The Outlying Fells of Lakeland''. It reaches and Wainwright's route starts near the 17th-century Ulthwaite Bridge on the River Kent, climbing High Knott and then making a clockwise circuit to the early British village site at Hugill and ''"over the pleasant heights on the west side of mid-Kentmere Kentmere is a valley, village and civil parish in the Lake District National Park, a few miles from Kendal in the South Lakeland district of Cumbria, England. Historically in Westmorland, at the 2011 census Kentmere had a population of 1 ..."''. Access to the summit is (at May 2016) forbidde ...
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Cumbria
Cumbria ( ) is a ceremonial and non-metropolitan county in North West England, bordering Scotland. The county and Cumbria County Council, its local government, came into existence in 1974 after the passage of the Local Government Act 1972. Cumbria's county town is Carlisle, in the north of the county. Other major settlements include Barrow-in-Furness, Kendal, Whitehaven and Workington. The administrative county of Cumbria consists of six districts ( Allerdale, Barrow-in-Furness, Carlisle, Copeland, Eden and South Lakeland) and, in 2019, had a population of 500,012. Cumbria is one of the most sparsely populated counties in England, with 73.4 people per km2 (190/sq mi). On 1 April 2023, the administrative county of Cumbria will be abolished and replaced with two new unitary authorities: Westmorland and Furness (Barrow-in-Furness, Eden, South Lakeland) and Cumberland ( Allerdale, Carlisle, Copeland). Cumbria is the third largest ceremonial county in England by area. It i ...
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Westmorland And Lonsdale (UK Parliament Constituency)
Westmorland (, formerly also spelt ''Westmoreland'';R. Wilkinson The British Isles, Sheet The British IslesVision of Britain/ref> is a historic county in North West England spanning the southern Lake District and the northern Dales. It had an administrative function from the 12th century until 1974. Between 1974 and 2023 Westmorland lay within the administrative county of Cumbria. In April 2023, Cumbria County Council will be abolished and replaced with two unitary authorities, one of which, Westmorland and Furness, will cover all of Westmorland (as well as other areas), thereby restoring the Westmorland name to a top-tier administrative entity. The people of Westmorland are known as Westmerians. Early history Background At the beginning of the 10th century a large part of modern day Cumbria was part of the Kingdom of Strathclyde, and was known as '' "Scottish Cumberland" ''. The Rere Cross was ordered by Edmund I (r.939-946) to serve as a boundary marker between England ...
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Lingmell
Lingmell is a fell in the English Lake District, standing above the village of Wasdale Head. It is an outlier on the north-west flank of Scafell Pike, England’s highest mountain. Topography Although standing in the shadow of its taller parent, Lingmell is very much a separate entity. In the manner of many fells it displays two contrasting aspects. The southern and western slopes– although steep– are smooth and rounded, while the northern and eastern faces fall as crags directly from the summit. The northern crag drops for a thousand feet toward the valley floor, with a further thousand feet of scree below. The connection to Scafell Pike is via Lingmell Col, a grassy depression at 734 metres (2,410 ft.) Flowing west from the col is Lingmell Gill, descending through Hollow Stones to Brackenclose at the head of Wast Water. To the east of Lingmell Col runs Piers Gill, a stream descending from high on the Scafells. This flows right around the northern perimeter of Ling ...
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