Difference between revisions of "River Doe"

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(Created page with "{{county|York}} River Doe near Ingleton, flowing over Beezley Falls The '''River Doe''' is a river in t...")
 
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{{county|York}}
 
{{county|York}}
 
[[File:River Doe Ingleton - geograph.org.uk - 1131607.jpg|thumb|250px|River Doe near Ingleton, flowing over Beezley Falls]]
 
[[File:River Doe Ingleton - geograph.org.uk - 1131607.jpg|thumb|250px|River Doe near Ingleton, flowing over Beezley Falls]]
The '''River Doe''' is a river in the [[West Riding of Yorkshire|West Riding]] of [[Yorkshire]]. The river's source is near God's Bridge close to the settlement of [[Chapel-le-Dale]] and flows through Twisleton in a south-westerly direction to [[Ingleton, Yorkshire|Ingleton]], where it meets the [[River Twiss]] to form the [[River Greta (Lune)|River Greta]]. The river forms part of the [[River Lune]] system that flows into the [[Irish Sea]].
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The '''River Doe''' is a river in the [[West Riding of Yorkshire|West Riding]] of [[Yorkshire]], within the [[Yorkshire Dales]].  It is four and a half miles long, though the part bearing the name ‘Doe’ is just three and a half miles; the remaining miles being its main headwater, the Chapel Beck.
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The river's source as the Chapel Beck is in a pool named the Jingle Pot just outside [[Chapel-le-Dale]].  From here the Beck flows south-west until it disappears underground at God's Bridge south-west of Chapel-le-Dale:  the stream emerging from beneath the 'Bridge' is the River Doe. From here the Doe flows through Twisleton in a straight line in a south-westerly direction to [[Ingleton, Yorkshire|Ingleton]], where it meets the [[River Twiss]], and the two rivers form the [[River Greta (Lune)|River Greta]], a tributary of the [[River Lune]].
  
 
==Course==
 
==Course==
The source of the river is found at a place named God's Bridge where Chapel Beck disappears underground and the Doe begins. The river flows south-west, fed by a number of small unnamed springs on the valley sides. The first named tributary is Light Water Spring which feeds north-west into the river near a disused quarry. Near Twisleton Dale House, the river can be crossed by some stepping stones at a fording point as well as some 700 yds later near the disused granite quarry. Further down stream near Twisleton Hall there are another set of stepping stones at a fording point just above Beezley Falls. After flowing under a footbridge, there are another set of falls, Snow Falls, just below the quarry which is operated by Hanson.<ref>{{cite web|url=http://www.heidelbergcement.com/NR/rdonlyres/75E5C76B-09C9-4937-A575-520D5DA1FC7A/0/Hanson_Quarry_Products_ISO_9001_QSRMC.pdf|title=Active quarrying|publisher=Hanson Heidleberg Cement Group|accessdate=15 January 2014}}</ref> The river continues past several disused quarries and a footbridge until it reaches the town of Ingleton where it forms a confluence with the [[River Twiss]].
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The nominal source of the River Doe is a place named God's Bridge, which is not a bridge but a natural formation where Chapel Beck disappears underground and the Doe emerges. From here the river flows south-west, fed by a number of small unnamed springs on sides of the dale. The first named tributary is Light Water Spring which feeds north-west into the river near a disused quarry.
  
==Falls==
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Near Twisleton Dale House, the river can be crossed by some stepping stones at a fording point as well as some 700 yds later near the disused granite quarry. Further down stream near Twisleton Hall there are another set of stepping stones at a fording point just above Beezley Falls. After flowing under a footbridge, there are another set of falls, Snow Falls, just below the quarry which is operated by Hanson.<ref>{{cite web|url=http://www.heidelbergcement.com/NR/rdonlyres/75E5C76B-09C9-4937-A575-520D5DA1FC7A/0/Hanson_Quarry_Products_ISO_9001_QSRMC.pdf|title=Active quarrying|publisher=Hanson Heidleberg Cement Group|accessdate=15 January 2014}}</ref>
Beezley Falls are reached approximately two miles from the source at God's Bridge. These falls consist of a series of cascades, including the ''triple spout'', running through Baxengyhll Gorge. Rival Falls has a plunge pool known as the ''Black Hole''. The steepest drops are between nine feet and 12 feet approximately. Snow Falls are situated in the lower gorge about ½ mile downstream and has similar drops.<ref>{{cite web|url=http://www.ukriversguidebook.co.uk/rivers/england/north-west/river-doe|title=UK River Guide - Doe|accessdate=15 January 2014}}</ref>
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The river continues past several disused quarries and a footbridge until it reaches the town of Ingleton where it forms a confluence with the [[River Twiss]].
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==Waterfalls==
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*'''Beezley Falls''' are reached approximately two miles from the source at God's Bridge. These falls consist of a series of cascades, including the 'triple spout', running through Baxengyhll Gorge.
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*'''Rival Falls''' have a plunge pool known as the ''Black Hole''. The steepest drops are between 9 feet and 12 feet approximately.
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*'''Snow Falls''' are in the lower gorge about half a mile downstream and have similar drops.<ref>{{cite web|url=http://www.ukriversguidebook.co.uk/rivers/england/north-west/river-doe|title=UK River Guide - Doe|accessdate=15 January 2014}}</ref>
  
 
==Geology==
 
==Geology==
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|width=120 |height=100 |lines=4
 
|width=120 |height=100 |lines=4
 
|align=center
 
|align=center
|File:Stepping stones, River Doe - geograph.org.uk - 66150.jpg|Stepping stones, River Doe between Dale House and Twistleton Dale House  
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|File:Stepping stones, River Doe - geograph.org.uk - 66150.jpg|Stepping stones between Dale House and Twistleton Dale House
|File:Stream confluence at head of River Doe. - geograph.org.uk - 880475.jpg|Stream confluence at head of River Doe.
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|File:Stream confluence at head of River Doe. - geograph.org.uk - 880475.jpg|Stream confluence at head of River Doe
 
|File:Baxengill Gorge, River Doe, near Ingleton - geograph.org.uk - 830376.jpg|Baxengill Gorge, River Doe, near Ingleton
 
|File:Baxengill Gorge, River Doe, near Ingleton - geograph.org.uk - 830376.jpg|Baxengill Gorge, River Doe, near Ingleton
 
|File:Wide flood-bed of River Doe - geograph.org.uk - 880940.jpg|Wide flood-bed of River Doe
 
|File:Wide flood-bed of River Doe - geograph.org.uk - 880940.jpg|Wide flood-bed of River Doe
 
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==References==
 
{{Commons category|River Doe, North Yorkshire|position=right}}
 
{{reflist|2}}
 
  
==Outside links==
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==Location==
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*Location map: {{wmap|54.153333|-2.470833}}
 
*Map of the source: {{wmap|54.182778|-2.411111|zoom=14|name=Source of the Doe}}
 
*Map of the source: {{wmap|54.182778|-2.411111|zoom=14|name=Source of the Doe}}
 
*Map of the confluence with the Twiss: {{wmap|54.153333|-2.470833|zoom=14|name=Confluence of the Doe and Twiss}}
 
*Map of the confluence with the Twiss: {{wmap|54.153333|-2.470833|zoom=14|name=Confluence of the Doe and Twiss}}
  
[[Category:Rivers of Yorkshire|Doe, River]]
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{{commons|River Doe, North Yorkshire}}
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==References==
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{{reflist|2}}
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[[Category:Rivers of Yorkshire|Doe River]]

Revision as of 12:25, 28 May 2019

River Doe near Ingleton, flowing over Beezley Falls

The River Doe is a river in the West Riding of Yorkshire, within the Yorkshire Dales. It is four and a half miles long, though the part bearing the name ‘Doe’ is just three and a half miles; the remaining miles being its main headwater, the Chapel Beck.

The river's source as the Chapel Beck is in a pool named the Jingle Pot just outside Chapel-le-Dale. From here the Beck flows south-west until it disappears underground at God's Bridge south-west of Chapel-le-Dale: the stream emerging from beneath the 'Bridge' is the River Doe. From here the Doe flows through Twisleton in a straight line in a south-westerly direction to Ingleton, where it meets the River Twiss, and the two rivers form the River Greta, a tributary of the River Lune.

Course

The nominal source of the River Doe is a place named God's Bridge, which is not a bridge but a natural formation where Chapel Beck disappears underground and the Doe emerges. From here the river flows south-west, fed by a number of small unnamed springs on sides of the dale. The first named tributary is Light Water Spring which feeds north-west into the river near a disused quarry.

Near Twisleton Dale House, the river can be crossed by some stepping stones at a fording point as well as some 700 yds later near the disused granite quarry. Further down stream near Twisleton Hall there are another set of stepping stones at a fording point just above Beezley Falls. After flowing under a footbridge, there are another set of falls, Snow Falls, just below the quarry which is operated by Hanson.[1]

The river continues past several disused quarries and a footbridge until it reaches the town of Ingleton where it forms a confluence with the River Twiss.

Waterfalls

  • Beezley Falls are reached approximately two miles from the source at God's Bridge. These falls consist of a series of cascades, including the 'triple spout', running through Baxengyhll Gorge.
  • Rival Falls have a plunge pool known as the Black Hole. The steepest drops are between 9 feet and 12 feet approximately.
  • Snow Falls are in the lower gorge about half a mile downstream and have similar drops.[2]

Geology

The main rock of the river valley is turbidite sandstone with some siltstone which are prevalent in the waterfalls and plunge pools. These lay on a bed of Precambrian sedimentary rock which show evidence of its oceanic origins in the ripple and folding marks on exposed surfaces.[3]

Habitat

The river is home to Brown trout.[4] From Beezley falls to Snow falls, the sides of the gorge are lined with a variety of trees and shrubs.[5]

Gallery

Views of the River Doe
Stepping stones between Dale House and Twistleton Dale House  
Stream confluence at head of River Doe  
Baxengill Gorge, River Doe, near Ingleton  
Wide flood-bed of River Doe  

Location

Commons-logo.svg
("Wikimedia Commons" has material
about River Doe)

References