Ingleton, Yorkshire: Difference between revisions

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==Geography==
==Geography==
The civil parish of Ingleton is extensive, stretching from [[Blea Moor]] near [[Wold Fell]] SD&nbsp;793847 in the north to [[Newby Moor]] SD&nbsp;704698 in the south. The north of the parish follows the former county boundary with Lancashire to [[Whernside]] SD&nbsp;739816. From here is follows the ridge south-west to West Fell and down to [[Thornton Force]] on the [[River Twiss]], and thence along the river, and the [[River Greta (Lune)|River Greta]] to Fourlands Hill SD&nbsp;698713. The east of the parish follows the watershed of the [[River Ure]], a headwater of the [[River Humber]], and the [[River Ribble]] to Grove Head where it is only 200m from the [[Pennine Way]], it drops to the B6255 road and the River Ribble at the milepost at SD&nbsp;793816 The boundary follows the Ribble through [[Ribblehead]], then takes the ridge through Park Fell and Simon Fell to [[Ingleborough]]. It passes due south over Ingleborough Common to Newbury Moss, descending to Cold Cotes on the old road at SD&nbsp;722712.  Ingleborough is 2,373 feet high.<ref name=mapit>[https://maps.google.co.uk/maps?q=http://mapit.mysociety.org/area/63370.kml Mapit overlay]</ref>
The civil parish of Ingleton is extensive, stretching from [[Blea Moor]] near [[Wold Fell]] ({{map|SD793847}}) in the north to [[Newby Moor]] ({{map|SD704698}}) in the south. From the north-west, the parish boundary runs from [[Whernside]], following the ridge south-west to West Fell and down to [[Thornton Force]] on the [[River Twiss]], and thence along the river, and the [[River Greta (Lune)|River Greta]] to Fourlands Hill {{map|SD698713}}. The east of the parish follows the watershed of the [[River Ure]], a headwater of the [[River Humber]], and the [[River Ribble]] to Grove Head where it is only 200 yds from the [[Pennine Way]], it drops to the B6255 road and the River Ribble at the milepost at {{map|SD793816}} The boundary follows the Ribble through [[Ribblehead]], then takes the ridge through Park Fell and Simon Fell to [[Ingleborough]]. It passes due south over Ingleborough Common to Newbury Moss, descending to Cold Cotes on the old road at {{map|SD722712}}.  Ingleborough is 2,373 feet high.<ref name=mapit>[https://maps.google.co.uk/maps?q=http://mapit.mysociety.org/area/63370.kml Mapit overlay]</ref>


The village sits at the foot of Ingleborough, separated from [[Thornton-in-Lonsdale]] by the Rivers Greta and Twiss, some of the facilities that form the settlement being thus outside the civil parish. The peaks of Ingleborough and Whernside lies within the parish; separated by the deeply eroded valley of the [[River Doe]]. Both these peaks are formed by millstone grit on limestone footings. To the north of the river are the Twistleton Crags with the important limestone pavement of Scales Moor. Here are two SSSIs: Whernside and Scales Moor Common which is managed as stinted common pasture land.{{efn|Stinted common land is a system where the commoners are restricted to the sheep they can keep in the common; this prevents overgrazing}} To the south of the river is one SSSI: Ingleton on the stinted Ingleton Common, in the number of  an equivalent limestone pavement. This area of challenging potholes and caves.<ref>{{cite journal|url=http://commons.ncl.ac.uk/wp-content/uploads/files/IngletonQualitativeRevised.pdf|title=-Modern Environmental Governance: Qualitative Research Data Case Study : Ingleton North Yorkshire }}</ref> The show cave [[White Scar Caves]] SD&nbsp;712745 has its entrance. Ingleton Common adjoins Clapham Common and they are collectively referred to as Ingleborough Common.
The village sits at the foot of Ingleborough, separated from [[Thornton-in-Lonsdale]] by the Rivers Greta and Twiss, some of the facilities that form the settlement being thus outside the civil parish. The peaks of Ingleborough and Whernside lies within the parish; separated by the deeply eroded valley of the [[River Doe]]. Both these peaks are formed by millstone grit on limestone footings. To the north of the river are the Twistleton Crags with the important limestone pavement of Scales Moor. Here are two SSSIs: Whernside and Scales Moor Common which is managed as stinted common pasture land.{{efn|Stinted common land is a system where the commoners are restricted to the sheep they can keep in the common; this prevents overgrazing}} To the south of the river is one SSSI: Ingleton on the stinted Ingleton Common, in the number of  an equivalent limestone pavement. This area of challenging potholes and caves.<ref>{{cite journal|url=http://commons.ncl.ac.uk/wp-content/uploads/files/IngletonQualitativeRevised.pdf|title=-Modern Environmental Governance: Qualitative Research Data Case Study : Ingleton North Yorkshire }}</ref> The show cave [[White Scar Caves]] SD&nbsp;712745 has its entrance. Ingleton Common adjoins Clapham Common and they are collectively referred to as Ingleborough Common.
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A varied geology is found within the boundaries of the parish, ranging from rocks laid down in the Iapetus Ocean in Ordovician times, through the Carboniferous limestones of the Askrigg Block on Whernside and Ingleborough and coal measures within the Craven Basin, to the Quaternary drumlin field in Ribblehead. It is a classic field study area for students of geology.<ref>{{cite web|title=Ingleton Virtual Field Excursion|url=http://www.ljmu.ac.uk/NSP/ingleton/|publisher=Liverpool John Moores University|accessdate=21 March 2014}}</ref>
A varied geology is found within the boundaries of the parish, ranging from rocks laid down in the Iapetus Ocean in Ordovician times, through the Carboniferous limestones of the Askrigg Block on Whernside and Ingleborough and coal measures within the Craven Basin, to the Quaternary drumlin field in Ribblehead. It is a classic field study area for students of geology.<ref>{{cite web|title=Ingleton Virtual Field Excursion|url=http://www.ljmu.ac.uk/NSP/ingleton/|publisher=Liverpool John Moores University|accessdate=21 March 2014}}</ref>


Much of the parish is dominated by Carboniferous deposits deposited on the submarine platform of the Askrigg Block, which was a relatively high area forming a shelf sea buoyed up by Devonian Wensleydale Granite.{{sfn|Waltham|2007||page=18}} It is separated from the Craven Basin to the south and west by the Craven Fault system.{{sfn|Waltham|2007||pages=54–57}} The lower Carboniferous deposits are dominated by the 660-ft-thick Great Scar limestones laid down during the Viséan stage. A mature karst landscape has formed where it outcrops, with bare limestone pavements, subterranean streams, and major solutional cave systems such as White Scar Caves and Meregill Hole.{{sfn|Waltham et alia|1997|pages=46–55}} Scales Moor on the Whernside flanks of Chapel-le-Dale has one of the largest exposures of pavement in the Dales, measuring some {{convert|4|km|mi}} long {{convert|800|m|yd}} wide.{{sfn|Waltham et alia|1997|pages=43–46}} On Whernside and Ingleborough above the flat plateau formed by the top of the Great Scar limestone, are the Brigantian and Namurian aged Yoredale cyclothem sequences of sandstone, limestone, and shales which were deposited on the edge of a huge delta.{{sfn|Waltham|2007||pages=30–31}} The upper ramparts of these hills are capped by thick beds of Grassington Grit, a course poorly-sorted sandstone laid down in shallower water as the delta prograded south.{{sfn|Waltham|2007||pages=40–45}}
Much of the parish is dominated by Carboniferous deposits deposited on the submarine platform of the Askrigg Block, which was a relatively high area forming a shelf sea buoyed up by Devonian Wensleydale Granite.{{sfn|Waltham|2007||page=18}} It is separated from the Craven Basin to the south and west by the Craven Fault system.{{sfn|Waltham|2007||pages=54–57}} The lower Carboniferous deposits are dominated by the 660-ft-thick Great Scar limestones laid down during the Viséan stage. A mature karst landscape has formed where it outcrops, with bare limestone pavements, subterranean streams, and major solutional cave systems such as White Scar Caves and Meregill Hole.{{sfn|Waltham et alia|1997|pages=46–55}} Scales Moor on the Whernside flanks of Chapel-le-Dale has one of the largest exposures of pavement in the Dales, measuring some 2½ miles long and ½ mile wide.{{sfn|Waltham et alia|1997|pages=43–46}} On Whernside and Ingleborough above the flat plateau formed by the top of the Great Scar limestone, are the Brigantian and Namurian aged Yoredale cyclothem sequences of sandstone, limestone, and shales which were deposited on the edge of a huge delta.{{sfn|Waltham|2007||pages=30–31}} The upper ramparts of these hills are capped by thick beds of Grassington Grit, a course poorly-sorted sandstone laid down in shallower water as the delta prograded south.{{sfn|Waltham|2007||pages=40–45}}


The Carboniferous rocks were deposited unconformably onto basement rocks which are exposed as inliers in Chapel-le-Dale and lower Kingsdale (Swilla Glen). They are Ordovician in age, deposited as turbidites about 480 million years ago in the Iapetus Ocean, and heavily folded and lightly metamorphosed in late Ordovician times. They are currently quarried for roadstone, and were once quarried for slate in the Ingleton Glens.{{sfn|Waltham|2007||pages=14–18}}
The Carboniferous rocks were deposited unconformably onto basement rocks which are exposed as inliers in Chapel-le-Dale and lower Kingsdale (Swilla Glen). They are Ordovician in age, deposited as turbidites about 480 million years ago in the Iapetus Ocean, and heavily folded and lightly metamorphosed in late Ordovician times. They are currently quarried for roadstone, and were once quarried for slate in the Ingleton Glens.{{sfn|Waltham|2007||pages=14–18}}
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==Transport==
==Transport==
Ingleton had two railway stations at opposite ends of Ingleton Viaduct. Ingleton (Midland) station opened for ten months only in 1849, then reopened in 1861 until 1954. Ingleton (L&NW) station opened along with the Ingleton Branch Line in 1861, but such was the rivalry between competing railway companies that initially passengers were forced to walk between the stations across the [[River Greta (Lune)|Greta]] valley floor, despite the viaduct between them. The L&NW station closed in 1917.<ref>{{Butt-Stations|page=126}}</ref><ref>Western, Robert (1990), ''The Ingleton Branch'', Oakwood Press, Oxford, {{ISBN|0-85361-394-X}}, p.29</ref> The nearest railway station is now {{stnlnk|Bentham}}, {{convert|3.5|mi|km|0}} by road to the south of Ingleton.
Ingleton had two railway stations at opposite ends of Ingleton Viaduct. Ingleton (Midland) station opened for ten months only in 1849, then reopened in 1861 until 1954. Ingleton (L&NW) station opened along with the Ingleton Branch Line in 1861, but such was the rivalry between competing railway companies that initially passengers were forced to walk between the stations across the [[River Greta (Lune)|Greta]] valley floor, despite the viaduct between them. The L&NW station closed in 1917.<ref>{{Butt-Stations|page=126}}</ref><ref>Western, Robert (1990), ''The Ingleton Branch'', Oakwood Press, Oxford, {{ISBN|0-85361-394-X}}, p.29</ref> The nearest railway station is now at Bentham, 3½ miles by road to the south of Ingleton.


The village is on the A65 road between Skipton and Kendal and at the head of the A687 that branches westwards towards [[Burton in Lonsdale]] and Lancaster. The B6255 takes the south bank of the River Doe heading north-east to Chapel-le-Dale, [[Ribblehead]] and [[Hawes]].
The village is on the A65 road between Skipton and Kendal and at the head of the A687 that branches westwards towards [[Burton in Lonsdale]] and Lancaster. The B6255 takes the south bank of the River Doe heading north-east to Chapel-le-Dale, [[Ribblehead]] and [[Hawes]].

Latest revision as of 10:23, 26 April 2018

Ingleton
Yorkshire
West Riding

Ingleton and the viaduct across Swilla Glen
Location
Grid reference: SD691729
Location: 54°9’4"N, 2°28’20"W
Data
Population: 2,186  (2011)
Post town: Carnforth
Postcode: LA6
Dialling code: 015242
Local Government
Council: Craven
Parliamentary
constituency: 		Skipton and Ripon

Ingleton is a village and civil parish in the West Riding of Yorkshire. The village is 20 miles from Kendal and 17 miles from Lancaster on the western side of the Pennines. It is 10 miles from Settle. The River Doe and the River Twiss meet to form the source of the River Greta, a tributary of the River Lune. The village is on the A65 road and at the head of the A687. The B6255 takes the south bank of the River Doe to Ribblehead and Hawes. All that remains of the railway in the village is the landmark Ingleton Viaduct.[1] Arthur Conan Doyle was a regular visitor to the area and was married locally, as his mother lived at Masongill from 1882 to 1917. There is growing evidence to support a claim that the inspiration for the name Sherlock Holmes came from here.[2]

Whernside, six miles north-north-east of the village, one of the Yorkshire Three Peaks, is the highest point in the parish at 2,415 feet.

There are major quarries within the parish. Ingleton Quarry is active; Meal Bank Quarry no longer is, but extracted Carboniferous limestone and possesses an early Hoffman kiln. There was a textile mill, and the coalfield supported twelve or more small collieries, but Ingleton is mostly known for its tourism, being partially in the Yorkshire Dales National Park, offering waterfalls in a SSSI, limestone caves and Karst landscape walking opportunities.

History

Ingleton and the surrounding area was settled in the Iron Age by the Brigantes who built a hill fort on top of Ingleborough with walls nearly a mile in circumference. The Romans defeated the Brigantes in battle and built a fort alongside the hill fort. The valley was crossed by Roman roads as Ingleton was a strategic river crossing. By the 12th century the Normans had built a church in the village.[3]

Manor

Willian Lowther (1574–1641) of Ingleton Hall was Lord of the Manor, Justice of the Peace for the West Riding and had seven children. His son Richard (1602–1645) inherited the manor and two sons joined the church. His daughter Frances (1612–1665) married John Walker who leased the Ingleton Colleries, and Elizabeth (1615-?) married Anthony Bouch in 1633[4] and mortgaged Ingleton Manor.[5]

Richard Lowther and his son Gerrard were on the losing Royalist side at the Civil War siege of Pontefract Castle in 1645, and later at Newark. The war ended and his father dead, Gerrard was fined by the new government for his delinquency, and entered into a series of agreements to pay the debt and court appearances to maintain the estate. The Lord of Manor title had passed to Anthony Bouch by 1665, and the coal rights passed to the Walker family after a settlement in the chancery court in 1678.[5]

Industry

Template:Details

The Ingleton Coalfield was worked for 400 years. It is about 6 miles long by 4 mile wide and extends into the neighbouring parishes of Burton in Lonsdale and Thornton-in-Lonsdale. The coalfield terminates at the South Craven fault. The coal measures are shallow and represent the lowest layers in the Pennine coal measures sequence. The earliest coal mining occurred along the River Greta where Four Foot and Six Foot seams outcrop. Most deep mining was at New Ingleton Pit sunk in 1913. Its sinking led to the discovery of the Ten Foot seam (house and steam coal) at 127 yards, and the Nine Foot seam (steam and house coal) at 134 yards. Beneath them are the Four Foot seam (house, gas and coking coal) at 233 yards, the Three Foot seam (house and gas coal) at 236 yards and the Six Foot seam (steam and house coal) at 260 yards. Commercially viable deposits of fireclay lay under the Three Foot seam and pottery clay beneath the Six Foot seam used to make Ingleton Bricks.[6][7] The Walkers achieved their legal victory through a son-in-Law William Knipe. Thomas Moore(?-1733) was the second husband of Marianne Walker and between 1702 and 1711 bought out other share holders in the collieries while building a successful medical practice in Wakefield. He left the collieries to be managed by an agent. His daughter Susannah married William Serjeantson- and his family ran the collieries from 1736 to 1828. Coal was delivered by horse and cart.[8] Ingleton and Bentham Moors were enclosed in 1767. Plans were drawn up in 1780 to connect Ingleton to the Leeds and Liverpool Canal via Clapham, Settle and Foulridge, Colne but it never progressed.[9] Boys and girls as young as four worked the collieries in the 1780, first as 'messengers' and from six, underground, as 'trailers', pulling coal tubs.[10] The last mine was closed in 1940.[11]

Ingleton Mill was built in 1791 by four partners who also had built a mill in Clapham in 1786. The partners, George Armitstead, a cotton spinner, Ephraim Ellis, William Petty and Thomas Wigglesworth bought the barn beside the old corn mill and built the mill. They obtained iron for its construction from Kirkstall Forge. They ran a joiner's shop, smithy and cotton mill. It was sold in 1807 and used to spin flax by John Coates, before reverting to cotton spinning in 1837.[12] (National Building Register:63815: [13]).

Geography

The civil parish of Ingleton is extensive, stretching from Blea Moor near Wold Fell (SD793847) in the north to Newby Moor (SD704698) in the south. From the north-west, the parish boundary runs from Whernside, following the ridge south-west to West Fell and down to Thornton Force on the River Twiss, and thence along the river, and the River Greta to Fourlands Hill SD698713. The east of the parish follows the watershed of the River Ure, a headwater of the River Humber, and the River Ribble to Grove Head where it is only 200 yds from the Pennine Way, it drops to the B6255 road and the River Ribble at the milepost at SD793816 The boundary follows the Ribble through Ribblehead, then takes the ridge through Park Fell and Simon Fell to Ingleborough. It passes due south over Ingleborough Common to Newbury Moss, descending to Cold Cotes on the old road at SD722712. Ingleborough is 2,373 feet high.[14]

The village sits at the foot of Ingleborough, separated from Thornton-in-Lonsdale by the Rivers Greta and Twiss, some of the facilities that form the settlement being thus outside the civil parish. The peaks of Ingleborough and Whernside lies within the parish; separated by the deeply eroded valley of the River Doe. Both these peaks are formed by millstone grit on limestone footings. To the north of the river are the Twistleton Crags with the important limestone pavement of Scales Moor. Here are two SSSIs: Whernside and Scales Moor Common which is managed as stinted common pasture land.[lower-alpha 1] To the south of the river is one SSSI: Ingleton on the stinted Ingleton Common, in the number of an equivalent limestone pavement. This area of challenging potholes and caves.[15] The show cave White Scar Caves SD 712745 has its entrance. Ingleton Common adjoins Clapham Common and they are collectively referred to as Ingleborough Common.

Historically, mining and agriculture were the predominant industries in the area. Coal was extracted from the Ingleton Coalfield from the early 1600s, to the turn of the 20th century, eventually closing in 1936. The New Village estate was built for mine workers.[16]

Geology

The Craven faults
The strata along the River Twiss, below Quaternary terminal moraine at Raven Ray[17]

A varied geology is found within the boundaries of the parish, ranging from rocks laid down in the Iapetus Ocean in Ordovician times, through the Carboniferous limestones of the Askrigg Block on Whernside and Ingleborough and coal measures within the Craven Basin, to the Quaternary drumlin field in Ribblehead. It is a classic field study area for students of geology.[18]

Much of the parish is dominated by Carboniferous deposits deposited on the submarine platform of the Askrigg Block, which was a relatively high area forming a shelf sea buoyed up by Devonian Wensleydale Granite.[19] It is separated from the Craven Basin to the south and west by the Craven Fault system.[19] The lower Carboniferous deposits are dominated by the 660-ft-thick Great Scar limestones laid down during the Viséan stage. A mature karst landscape has formed where it outcrops, with bare limestone pavements, subterranean streams, and major solutional cave systems such as White Scar Caves and Meregill Hole.[20] Scales Moor on the Whernside flanks of Chapel-le-Dale has one of the largest exposures of pavement in the Dales, measuring some 2½ miles long and ½ mile wide.[20] On Whernside and Ingleborough above the flat plateau formed by the top of the Great Scar limestone, are the Brigantian and Namurian aged Yoredale cyclothem sequences of sandstone, limestone, and shales which were deposited on the edge of a huge delta.[19] The upper ramparts of these hills are capped by thick beds of Grassington Grit, a course poorly-sorted sandstone laid down in shallower water as the delta prograded south.[19]

The Carboniferous rocks were deposited unconformably onto basement rocks which are exposed as inliers in Chapel-le-Dale and lower Kingsdale (Swilla Glen). They are Ordovician in age, deposited as turbidites about 480 million years ago in the Iapetus Ocean, and heavily folded and lightly metamorphosed in late Ordovician times. They are currently quarried for roadstone, and were once quarried for slate in the Ingleton Glens.[19]

Just to the north of Ingleton village the Craven Faults running north-west to south-east mark the southern margin of the Askrigg Block. The North Craven Fault has a downthrow of about 660 ft, and a few hundred yards away the South Craven Fault has a downthrow of about 4,000 ft.[19] The fault plane of the North Craven Fault is exposed in Swilla Glen.[19] To the south of the Craven Faults is the Craven Basin where the Westphalian stage Pennine Coal Measures are exposed, once exploited by the Ingleton coalfield.[19]

The landscape in the north-east of the parish, beyond the Ribblehead Viaduct, is dominated by Devensian glacial deposits, and includes some of the Ribblehead Drumlin Field.[19]

Economy

Tourism, mostly from hiking and caving, accounts for most of the economic activity of the village, especially in spring and summer. There are craft businesses, such as pottery.[21]

Of two quarries in the parish, Ingleton Quarry, owned by Hanson Aggregates,[22] is active and extracts Ordivician greywacke for roadstone[19] but Meal Bank Quarry that extracted Carboniferous limestone and possessed an early Hoffman kiln is no longer active.[23]

In 1933 an open-air swimming pool was constructed by volunteers, with materials supplied by the New Ingleton Colliery.[24] The European (Objective 5b) Community Fund, the National Lottery and private donations have been used to improve and modernise the pool.[25]

Landmarks

Thornton Force, on the Ingleton Waterfalls Trail

This area of Craven is best known for its natural landmarks, since the parish includes the summits of two of the Yorkshire Three Peaks, Ingleborough and Whernside. Two miles north-east of the village on the road to Chapel-le-Dale are the show caves at White Scar Caves.[26] An access tunnel has been cut to allow visitors to visit.

The Ingleton Waterfalls Trail is a five-mile circular walk from the village, opened in 1885.[27]

Ingleton Viaduct is a Grade-II-listed structure in the village.[28] Six miles to the north east on Batty Moss is the Ribblehead Viaduct, a Grade-II*-listed structure on the Settle and Carlisle Line, and on the land underneath and around it, the scheduled remains of the construction camp and navvy settlements.[29]

Religion

The parish church is dedicated to St Mary There is also a Methodist chapel and an Evangelical Church.[30] The parish church, designed by Cornelius Sherlock dates principally from 1886 and is dedicated to St Mary the Virgin. It is built on the site of an earlier church. It stands on a bank of boulders and sediment from the last ice age which make for unstable foundations. The Norman font is dated at around 1150, and the 15th-century tower is built in the perpendicular style. The nave was replaced on new compacted foundations in 1743 but demolished in 1886 to make way for the present one, which is built in blue limestone from Skirwith Quarry. The foundations were consolidated with concrete in 1930 and again in 1946. The church was dedicated to St Leonard but in the 18th century the dedication was changed.[31] Other treasures include a Vinegar Bible and a reredos with a carving of the Last Supper.

Transport

Ingleton had two railway stations at opposite ends of Ingleton Viaduct. Ingleton (Midland) station opened for ten months only in 1849, then reopened in 1861 until 1954. Ingleton (L&NW) station opened along with the Ingleton Branch Line in 1861, but such was the rivalry between competing railway companies that initially passengers were forced to walk between the stations across the Greta valley floor, despite the viaduct between them. The L&NW station closed in 1917.[32][33] The nearest railway station is now at Bentham, 3½ miles by road to the south of Ingleton.

The village is on the A65 road between Skipton and Kendal and at the head of the A687 that branches westwards towards Burton in Lonsdale and Lancaster. The B6255 takes the south bank of the River Doe heading north-east to Chapel-le-Dale, Ribblehead and Hawes.

Education

There is now one school in the village, Ingleton Primary School.[34] It is a partner in 'The Three Peaks Family of Schools', a grouping of secondary schools, primary schools and middle schools.[35] serving North Craven. Ingleton Primary School is a small school, that teaches pupils in mixed classes, two classes serve the Key stage 1 pupils, years 3 and 4 are together and years 5 and 6.[34]

This was once a first school until the re-organisation on 31 August 2012. The pupils transferred to the adjacent Ingleton Middle School after year 5, at the age of ten. They remained here until 13 when the transferred to the upper school in Settle. The Middle School buildings are now used as a Community Information Centre which is run as a not-for-profit organisation.[36] The playing fields have been sold.[37] Settle Middle school buildings were transferred to Settle College to provide the extra capacity needed for two extra year groups.[38]

Students from Ingleton transfer at the age of eleven to the receiving secondary schools, Settle College[39] and Queen Elizabeth School, Kirkby Lonsdale.[40] After secondary education pupils can either stay on to sixth form or transfer to a local college like Kendal College, Lancaster and Morecambe College.

Facilities

Ingleton has a community open air swimming pool which is closed in the winter.

Notable people

Reverend Thomas Dod Sherlock was vicar of St Mary the Virgin, Ingleton from 1874 to 1879, while his Uncle Edgar was Rector of Bentham. His father, Randall Hopley Sherlock, a Liverpool newspaper proprietor, was killed by lightning at [ngleton (Midland) railway station on 9 August 1875 while visiting his son. A stained glass window is dedicated to his memory in the church tower.

The area below the north end of Ingleton viaduct is known as Holme Head.

Mary Doyle, the mother of Sir Arthur Conan Doyle, lived from 1882 to 1917 in Masongill, a hamlet near Thornton-in-Lonsdale. In 1885 Arthur, a regular visitor to the area, was married to his first wife Louise in St Oswald's Church, Thornton-in-Lonsdale.[41][42] When visiting his mother, Arthur would have arrived at Ingleton (Midland) railway station, where Randall Sherlock died, and continued his onward journey by cart to Masongill passing through Holme Head.

In 1886 when Conan Doyle wrote A Study in Scarlet, the first Sherlock Holmes story, he was originally going to call his hero Sherrinford Holmes. That same year, St Mary the Virgin, Ingleton, was rebuilt to the design of Cornelius Sherlock, the celebrated Liverpool architect responsible for the Picton Reading Room and the Walker Art Gallery, both now listed buildings in Liverpool. Pupils of Storrs Hall School, Ingleton, raised the funds to purchase a brass lectern for the new church. Pupils of this private school for young ladies at that time included Conan Doyle's two youngest sisters.

References

Footnotes

  1. ↑ Stinted common land is a system where the commoners are restricted to the sheep they can keep in the common; this prevents overgrazing

Notes

  1. ↑ OS map 98, Wensleydale and Upper Wharfdale.
  2. ↑ Tunningley, Alan (11 July 2015). "Dales link to Sherlock Holmes’ creation". The Westmorland Gazette. http://www.thewestmorlandgazette.co.uk/news/13408067.Dales_link_to_Sherlock_Holmes____creation/. Retrieved 6 December 2015. 
  3. ↑ "St Mary the Virgin Ingleton". http://www.achurchnearyou.com/ingleton-st-mary-the-virgin/. Retrieved 6 December 2015. 
  4. ↑ England, Marriages, 1538–1973. Salt Lake City, Utah: FamilySearch, 2013.
  5. ↑ 5.0 5.1 Bentley, Bond & Gill 2005, p. 19.
  6. ↑ Ellis (1993). "The Ingleton Coalfield—A Slumbering Dwarf?". http://www.northcravenheritage.org.uk/nchtjournal/Journals/1993/J93A14.html#tmpBB9-13. Retrieved 14 March 2014. 
  7. ↑ Bentley, Bond & Gill 2005, p. 45.
  8. ↑ Bentley, Bond & Gill 2005, p. 25.
  9. ↑ Bentley, Bond & Gill 2005, p. 29.
  10. ↑ Bentley, Bond & Gill 2005, p. 27.
  11. ↑ Bentley, John; Bond, Bernard; Gill, Mike (2005). Ingleton Coalfield. Northern Mine Research Society. pp. 95–121. ISBN 9780901450586. 
  12. ↑ Ingle 1997, p. 204.
  13. ↑ "NBR63815". Yorkshire Industrial Heritage. http://yorkshire.u08.eu/?b=63815. 
  14. ↑ Mapit overlay
  15. ↑ -Modern Environmental Governance: Qualitative Research Data Case Study : Ingleton North Yorkshire. http://commons.ncl.ac.uk/wp-content/uploads/files/IngletonQualitativeRevised.pdf. 
  16. ↑ Bentley, Bond & Gill 2005, p. 115.
  17. ↑ CPGS 2003, p. 8.
  18. ↑ "Ingleton Virtual Field Excursion". Liverpool John Moores University. http://www.ljmu.ac.uk/NSP/ingleton/. Retrieved 21 March 2014. 
  19. ↑ 19.00 19.01 19.02 19.03 19.04 19.05 19.06 19.07 19.08 19.09 Waltham 2007.
  20. ↑ 20.0 20.1 Waltham et alia 1997.
  21. ↑ "Economy". http://www.visitingleton.co.uk/. Retrieved 7 April 2012. 
  22. ↑ Kidd, Adrian. "The 'Your Dales Rocks Project' – A Draft Local Geodiversity Action Plan (2006–2011) for the Yorkshire Dales and the Craven Lowlands". North Yorkshire Geodiversity Partnership. http://www.nygp.org.uk/dox/Draft_%20LGAP_Your_Dales_Rocks_Project_final.pdf. Retrieved 5 March 2014. 
  23. ↑ CPGS 2003, p. 14.
  24. ↑ Bentley, Bond & Gill 2005, p. 118.
  25. ↑ "Ingleton Swimming Pool". http://www.ingletonpool.co.uk/. 
  26. ↑ White Scar Cave- Caving notes
  27. ↑ Ingleton Waterfalls Trail. "History of the Trail". http://www.ingletonwaterfallswalk.co.uk/history.htm. Retrieved 9 July 2007. 
  28. ↑ National Heritage List 1335083: Ingleton Viaduct
  29. ↑ National Heritage List 1015726: Ribblehead railway construction camp and prehistoric field system (Grade II*, scheduled listing)
  30. ↑ "Churches". http://www.ingleton.co.uk/inginfo.asp. Retrieved 7 April 2012. 
  31. ↑ St Marys church, Ingleton: about the church Template:Webarchive
  32. ↑ Butt, R. V. J. (1995). The Directory of Railway Stations: details every public and private passenger station, halt, platform and stopping place, past and present (1st ed.). Sparkford: Patrick Stephens Ltd. p. 126. ISBN 978-1-85260-508-7. OCLC 60251199. 
  33. ↑ Western, Robert (1990), The Ingleton Branch, Oakwood Press, Oxford, ISBN 0-85361-394-X, p.29
  34. ↑ 34.0 34.1 "Ingleton Primary School". http://www.ingleton-pri.n-yorks.sch.uk/. Retrieved 12 March 2014. 
  35. ↑ "The Three Peaks Family of Schools". Archived from the original on 17 October 2013. https://web.archive.org/web/20131017124938/http://www.settlecollege.org.uk/homedir/three-peaks.html. 
  36. ↑ "NYCC Executive Papers". 18 December 2012. Archived from the original on 13 March 2014. https://web.archive.org/web/20140313001545/https://www3.northyorks.gov.uk/n3cabinet_exec/reports_/20121218_/07redeploymento/07redeploymento.pdf. 
  37. ↑ "School Playing Fields in North Yorkshire Sold Off". 17 August 2012. http://www.minsterfm.com/news/local/745069/school-playing-fields-in-north-yorkshire-sold-off/. Retrieved 6 December 2015. 
  38. ↑ Proctor, Katie (22 February 2011). "Ingleton and Settle middle schools closure confirmed". http://www.thewestmorlandgazette.co.uk/news/yorkshire_dales/8868621.Ingleton_and_Settle_middle_schools_closure_confirmed/. 
  39. ↑ "Settle College". http://www.settlecollege.org.uk/. Retrieved 19 October 2013. 
  40. ↑ "Queen Elizabeth School". Archived from the original on 20 October 2013. https://web.archive.org/web/20131020051555/http://www.queenelizabeth.cumbria.sch.uk/2010/index.php. Retrieved 19 October 2013. 
  41. ↑ St Mary's Church, Ingleton Template:Webarchive
  42. ↑ http://www.ingleton.co.uk/inghist.asp

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