Kentmere | |
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Looking north up Kentmere from High Knott | |
Location within Cumbria | |
Population | 159 (2011) |
OS grid reference | NY4504 |
Civil parish |
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Unitary authority | |
Shire county | |
Region | |
Country | England |
Sovereign state | United Kingdom |
Post town | KENDAL |
Postcode district | LA8 |
Dialling code | 01539 |
Police | Cumbria |
Fire | Cumbria |
Ambulance | North West |
UK Parliament | |
Kentmere is a valley, village and civil parish in the Lake District National Park, a few miles from Kendal in the Westmorland and Furness district of Cumbria, England. Historically in Westmorland, at the 2011 census Kentmere had a population of 159. [1] The current lord of the manor is American philanthropist Terry A. Perkins.
The narrow valley spans about 3 miles (4.8 km) 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), [2] 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 Gowan Beck coming in from Ings. A walk described by Wainwright in his Far Eastern Fells series as the Kentmere Round involves an all-inclusive round trip of 12 miles (19 km). In the past there were drove roads up over the horseshoe in the north to the village of Mardale which is now under the water of the Haweswater Reservoir. In the past it was a tradition of the valley's inhabitants to travel from Kentmere to Mardale village church as part of the Easter Sunday celebrations.
The River Kent begins above the reservoir in the heights of Bleathwaite Crag. It collects beneath Kentmere Common in the reservoir which was built in 1848 to control the flow of water to the lower pastures. Lingmell Gill also feeds into the reservoir. Beside the reservoir sits a disused quarry and a cottage formerly used for maintenance of the river. The river opens out into a transitory lake called Kentmere Tarn just south of the confluence with Hall Gill. The lake has at times in the past completely disappeared into marshland and in 1840 it was purposely drained to provide reclaimed farm land, but in the past 100 years the "mere" has reappeared again. It is currently 1 mile in length. An archaeological excavation there uncovered an 'extended' log boat dated to c. 1300 AD (D.M. Wilson, A Medieval Boat from Kentmere, Westmorland, in Medieval Archaeology (1966) 10. 81–88). Other tributaries within the valley include Ullstone Gill, Nunnery Beck, Nuttera Beck, Park Beck and Hall Beck. A waterfall known as Force Jump is situated just north of the village, and there are two bridges at the Staveley end of the valley. The first is called Barley Bridge and includes a dramatic weir. The second straddles the Kent further up the valley and is known as Scrogg's Bridge.
A little further down the valley is the village of Kentmere, which includes Kentmere Hall and the church of St Cuthbert's. The parish of Kentmere is divided into four quarters:
Over Staveley and Hugill are also situated within the Kent valley, along with the small settlements of Elfhowe and Browfoot.
Near Kentmere Hall stands the "Brock Stone" or Badger Rock, a large free-standing rhyolite boulder. It is one of many challenges popular with climbers in the area. It is said that: "Kentmere valley has the greatest number of recorded [climbing] problems in the Lake District (over 125)" [3]
The main rocks and minerals to be found in the valley are green slate and granite. There has been some record of opal being found too [4] though it has never been mined. Much of the local stone has been used since pre-history as the raw material for field boundaries using a local technique known as dry stone walling. Just below the reservoir is a Geological Conservation Review site known as Jumb Quarry. [5] The site is significant due to its volcanic rock which displays "bird's-eye tuffs", which contain lapilli (fragments of lava that erupted from a volcanic centre and probably fell into standing bodies of water). The lapilli are believed to have been spherical originally, but were squashed into elliptical shapes as a result of intense pressure during the formation of the Caledonian Mountains.
The valley has evidence of habitation going back to roughly 4000 BC, when the valley and surrounding hillsides were almost entirely covered with forest. A major archaeological research project conducted in the valley by a local archaeology group between 1983 and 1999 surveyed and recorded hundreds of archaeological features, as well as excavating two sites – a (radiocarbon dated) pre-Viking and Viking Age upland settlement at Bryant's Gill, south of Rainsborrow Crag (on private land, not publicly accessible), and part of a medieval platform site and farmstead near Kentmere Hall [6] The results of this survey and excavation project are to be made publicly available via a new Lake District and Cumbrian archaeology website in 2012.
The valley's rich archaeological heritage also includes the remains of at least five large prehistoric compound or curvilinear sites incorporating the remains of round houses, stockyards and more. One of these sites is on a public footpath at Tongue House in the northern part of the valley.
Kentmere Hall is famous for its tower house; a fortification built for status in the 13th – early 14th centuries – ostensibly to guard against raiding parties from Scotland. Similar towers occur elsewhere in Cumbria and other northern English and southern Scottish counties. Kentmere Hall's tower has 5-foot-thick (1.5 m) walls, tunnel-vaulted ceilings, a crenellated roof with turrets and a spiral staircase; all built out of local stone. The farmstead to the east of it shows signs of many building phases and changes, in common with many other significant Lake District valley bottom medieval and post-medieval buildings such as Dalegarth Hall in Eskdale.
The manor, having been handed down to the eldest son, the rest of the valley was divided between the younger sons of the Gilpins for generations. What remains of the original estate is now a farm in possession of a private owner. Other important parts of the manor include Green Quarter on the eastern slopes of the valley where there is a bed and breakfast house, called Maggs Howe, that once was home to a branch of the Gilpin family.
St Cuthbert's Church, Kentmere was built to the east of Kentmere Hall. As is often the case with medieval churches, there is an ancient yew tree situated nearby which has been estimated to date back to the time of William I; indicating that worship had been taking place there at an early stage in the village's history. Written records of the chapel do not begin until 1692 making earlier history difficult to establish. A graveyard for the church was dedicated in 1701, and the Lord of the Manor paid the curate "a rate of 2s. levied for every 13s. 4d. paid to the lord of the manor". In 1757 this was supplemented with money paid out of Queen Anne's Bounty roughly £400–800. The chapel was remodelled in the 19th century and again in the 1950s. The roof was of 16th century date, but in 2016 was replaced.
The valley used to be known for its bobbin mills and for Waterfoot factory which dredged the bottom of the Kentmere Tarn in the 1950s searching for diatomite. A water mill was established by the first Lord of the Manor in 1272. The records state that he had "Liberty granted to erect a mill on the banks of the River Kent at Ulthwaite, upstream of Croft Head" they also stated that the mill was used to cut the sleepers for the Kendal and Windermere Railway in 1860. The mill was restored in the 1970s and is now a pottery studio producing handmade ceramics. Also, at the Staveley end of the valley, is a photographic paper manufactory known as Kentmere Ltd. A fishery is situated beside the reservoir and every year trout and salmon are released into the River Kent for the benefit of anglers because the river's native population has been diminished.
The area has had a history of mining. This appears to have been predominantly for the green slate available in the valley.
Official records of mining in the area go back at least as far as 1898. Before that it is likely, due to the particularly craggy nature of the valley, that the local dry stone walls and stone for housing were taken from the slopes around the valley, even as far back as the Bronze Age. There are two main open cast mines in the valley. The first is Jumb Quarry, situated within a few hundred yards of the early settlement at Tongue House, suggesting that the two may have been coexisting in some form or other. However the general proliferation of rock in this part of Kentmere means the early inhabitants may easily have taken their building material from almost anywhere in the valley, so it is by no means certain.
The second is situated at Steelrigg near Staveley. Both produced green slate.
There were also at least six underground mines in the valley. At the height of production in 1914 Steelrigg employed five men below ground and nine above. The quarry fell out of use in 1923 and 1925 and employed only four men with no active mining listed between 1921 and 1926. Mining was resumed in 1927 and continued until at least 1938. [7]
Jumb quarry was in continuous use throughout the same period, employing 10 men below ground and five above at its height in 1934. [8]
The two quarries changed hands on a number of occasions, with three companies listed in the pre-war period; James Stevenson & Co., Kendal, Tilberthwaite Green Slate Co Ltd., Kendal and Buttermere Green Slate Quarries Ltd., Station Buildings, Keswick. Throughout this time the agent for the quarries was local man J.J. Thomas.
By 1945 a company recorded as being the Kentmere Green Slate Co. Ltd. having its offices in the St. George's Buildings, Blackhall, Kendal owned both sites.
For a valley of its size, Kentmere has produced more than its fair share of famous families. Most notably the Gilpin family who were the main landowners in the village. Secondly the family of Airy who are first officially recorded in the 14th century, although in 1692 a history of the Barony of Kendal recorded that the church of St. Cuthbert, which is known to be of Norman date or earlier, was "reported to have been built by one Airay of this dale" [9] but this may refer to the re-roofing in the mid-16th century. The Aireys still have descendants of the same name in the valley today, although many of them were driven out during the Civil War, when they removed to Lincolnshire. Their notable descendants include George Biddell Airy the astronomer and Henry Airay, who was born in the valley and became Provost of Queen's College, Oxford in 1599. He bequeathed 40 shillings (£2) a year to ensure a monthly sermon was held at St. Cuthbert's. Postman Pat the cartoon character lived in Greendale which is claimed by his creator to be based on Kentmere and the neighbouring valley of Longsleddale.
The valley is famous for the Gilpin family who were given the valley and much surrounding land after an act of bravery by a member of the court of King John. According to legend, around the time of the signing of the Magna Carta Richard de Gilpin, known as "Richard the Rider" accompanied the Baron of Kendal to Runnymede as his secretary because the Baron himself was unable to read or write. After their return, Richard achieved renown for killing the Wild Boar of Westmorland a ferocious animal that had been terrorising the local villages. As a reward for his bravery, the Baron gave him the land in and around Kentmere, about 4,000 acres (16 km²), described as "a breezy tract of pasture land" by the French Chronicler Froissart. From this time onward, the Gilpin's crest included a sable boar on a gold background. Many areas near and surrounding Kentmere still sport the name of Gilpin given to them by descendants of this family.
Richard's achievement and his ancestry were immortalised by minstrels of the period in a song known as "the Minstrels of Winandermere" after Windermere which is less than 10 miles (15 km) from the valley.
The estate of Kentmere was increased during the reign of Henry III by a grant of the Manor of Ulwithwaite to Richard, the grandson of the boar-slayer.
The family later became famous for their alliance with the neighbouring de Bruce family who went on to become ancestors of the Kings of Scotland.
Bernard Gilpin also known as the "Apostle of the North" was a youngest son of the Gilpins of Kentmere Hall during the 16th century, and grew up there. In his adulthood he stayed there on occasion, preaching at the church. Concerning Bernard Gilpin; Thomas Cox states:
Bernard's eldest brother was George Gilpin who was commissioned by Queen Elizabeth I to form an alliance between the Dutch States and the English against the Spanish Armada. He was minister to The Hague during her reign. He carried with him an autographed letter written by the Queen stating:
The second brother, William Gilpin, took residence in the mill in 1578 after marrying Elizabeth Washington of Hall Head (the great-great aunt of George Washington).
Kentmere Hall remained in the hands of the Gilpins for 12 generations. It was lost during the English Civil War when Cromwell's troops destroyed the hall leaving only the fortified tower standing. The head of the household at that time left the land in trust to a friend and fled the country. When returning the gentleman's heir was unable to lay hold of the official deeds to the estate and so possession was lost. In 1660 ownership of the hall passed to the Philipson family.
The following lyrics were found by Reverend Charles Farish, whose mother was Elizabeth Gilpin (née Washington). He claimed they dated to the 13th century. However, the style is somewhat affected for the 13th century and everything but the first verse must be regarded with a suspicious eye.
(note; Charles Farish was a friend of William Wordsworth. In his book Poetical Works vol. 1 a footnote to Guilt and Sorrow; or, Incidents upon Salisbury Plain states that some of its lines were taken "From a short MS. poem read to me when an under-graduate, by my schoolfellow and friend Charles Farish, long since deceased. The verses were by a brother of his, a man of promising genius, who died young."—W. W. 1842 in a statement by the editor of the volume the footnote goes on to say that: "Charles Farish was the author of The Minstrels of Winandermere" as a result there is some debate as to authorship of the song commemorating Richard Gilpin's achievements).
Or, a boar statant sable, langued and tusked gules. Crest: A dexter arm embowed I armour proper, the naked hand grasping a pine branch fesswise vert.
Motto: Dictis Factisque Simplex (Latin; "Honest in Word and Deed").
Kendal, once Kirkby in Kendal or Kirkby Kendal, is a market town and civil parish in the Westmorland and Furness district of Cumbria, England. It lies within the River Kent's dale, from which its name is derived, just outside the boundary of the Lake District National Park.
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.
Longsleddale is a valley and civil parish in the South Lakeland district of Cumbria, England. 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.
Staveley is a village in the Westmorland and Furness Unitary Authority, in Cumbria, England. Historically part of Westmorland, it is situated 4 miles (6 km) northwest of Kendal where the River Kent is joined by its tributary the Gowan. It is also known as Staveley-in-Westmorland and Staveley-in-Kendal to distinguish it from Staveley-in-Cartmel. 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 in Hugill parish.
The Barony of Kendal is a subdivision of the English historic county of Westmorland. It evolved from one of two ancient baronies that make up the county, the other being the Barony of Westmorland. In 1974, the entire county became part of the modern county of Cumbria and ceased to have an administrative function. At the same time, Kendal borough along with some other rural and urban districts in Westmorland was merged with the neighbouring parts of Lancashire, Furness and Cartmel, and also the Sedbergh Rural District of the West Riding of Yorkshire into the new South Lakeland district of the new county.
The Wild Boar of Westmorland is a legend concerning Richard de Gilpin and the villagers and pilgrims visiting the ruins of the Holy Cross at Plumgarths, and the Chapel of the Blessed Virgin on St. Mary's Isle on Windermere.
Waberthwaite is a small, former rural civil parish on the south bank of the estuary of the River Esk, in Copeland, Cumbria, England. Since 1934 it has been part of the combined parish of Waberthwaite and Corney, which covers 10 square miles and has a population of 246. It is located opposite Muncaster Castle and the village of Ravenglass which lie on the north bank of the Esk. It is well known for its Cumberland sausages, and lists among its other assets a granite quarry that is a Site of Special Scientific Interest (SSSI); the Esk estuary, which forms part of the Drigg Coast Special Area of Conservation (SAC) - a designation for areas of European importance; the 800-year-old St. John's Church, and the remains of two Anglian/Norse crosses of an earlier period. Archeological finds within 3 kilometres of Waberthwaite indicate that the area has been continuously inhabited since Mesolithic times.
Shipman Knotts is a fell in the English Lake District in Cumbria, England. It reaches a height of 587 metres (1,926 ft) and is situated in one of the quieter areas of the national park, 2 kilometres north-east of Kentmere village. Although not one of the best-known Lake District fells, it earned a separate chapter in Alfred Wainwright’s Pictorial Guide to the Lakeland Fells due to “Its characteristic roughness. .. rocky outcrops are everywhere on its steep slopes”.
Kentmere Reservoir is a water storage facility situated in the Kentmere valley in the county of Cumbria, England. It is located 10.5 kilometres (6.5 mi) north-northeast of the town of Windermere. The reservoir is fed by the streams which form the headwaters of the River Kent which rise 1.5 kilometres (0.93 mi) 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.
Staveley Mill Yard is a former bobbin (spool) mill, which is now used for a variety of different local industries, shops and other commercial ventures. It is situated in the centre of the village of Staveley, Cumbria, just off the main street.
Cliburn is a village and civil parish in the Eden district of Cumbria, England. The civil parish includes the hamlet of Town Head. In 2001 the population was 204, increasing to 274 at the 2011 Census.
Hugill is a civil parish in Cumbria, England. Hugill includes the village of Ings and the hamlets of Grassgarth, and Reston plus a large part of the village of Staveley and the west bank of the River Kent north of Barley Bridge. It was formerly a part of the Barony of Kendal. In the 2001 census the parish had a population of 416, increasing at the 2011 census to 446. Approximately 60% of the population live in Staveley or the Kent valley.
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 901 feet (275 m) 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".
Hugill Fell is a hill in the English Lake District, near Staveley, Cumbria, on the western side of the Kentmere valley.
Staveley-in-Cartmel is a small village and civil parish in South Lakeland district, Cumbria, England. It lies east of Newby Bridge, near the south end of Windermere, 9 miles (14 km) northeast of Ulverston. It is sometimes known as Staveley-in-Furness. Both names distinguish it from another Staveley in Cumbria. In the 2001 census the parish had a population of 428, decreasing at the 2011 census to 405.
Kentrigg is a northern suburb of Kendal, Cumbria, England. By road, Kentrigg is located 1.2 miles (1.9 km) north of the centre of Kendal and 1.4 miles (2.3 km) southeast of Burneside. It contains the Carus Green Golf Club, which separates it from Burneside just to the northwest. Across the River Kent to the east is the Shap Road Industrial Estate, north of the district of Mintsfeet and the Mintsfeet Industrial Estate which marks the southeastern side of Kentrigg.
St Cuthbert's Church, Kentmere is a Grade II listed parish church in the Church of England in Kentmere, Cumbria. Its benefice is united with that of St Martin's Church, Bowness-on-Windermere; St Anne's Church, Ings; St James' Church, Staveley; Jesus Church, Troutbeck and St Mary's Church, Windermere.
St James' Church, Staveley is a Grade II listed parish church in the Church of England in Staveley, Cumbria. Its benefice is united with that of St Martin's Church, Bowness-on-Windermere; St Anne's Church, Ings; St Cuthbert's Church, Kentmere; Jesus Church, Troutbeck and St Mary's Church, Windermere.