Difference between revisions of "River Garnock"
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{{River | {{River | ||
| name = River Garnock | | name = River Garnock | ||
| + | | gaelic = Gairneag / Abhainn Ghairneig | ||
| country = Scotland | | country = Scotland | ||
| county = North Ayrshire | | county = North Ayrshire | ||
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| − | The '''River Garnock''' | + | The '''River Garnock''', the smallest of Ayrshire's six principal rivers, has its source on the southerly side of the Hill of Stake in the heart of the Clyde Muirshiel Regional Park. About a mile and a half south of this starting point the untested stream tumbles over the Spout of Garnock, the highest waterfall in Ayrshire, once thought to be the river's origin. The river then continues, for a total length of {{convert|20|mi|km}} or so, through the towns of [[Kilbirnie]], [[Glengarnock]], [[Dalry]] and [[Kilwinning]] to its confluence with the [[River Irvine]] at [[Irvine Harbour]]. |
| − | The main tributaries are the | + | The main tributaries are the Rye Water and Caaf Water which join north and south of Dalry respectively and the Lugton Water which joins just south of Kilwinning. |
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[[File:111007 River Garnock from Burnt Hill.jpg|thumb|200px|<center>The river upstream from Glen Garnock.]] | [[File:111007 River Garnock from Burnt Hill.jpg|thumb|200px|<center>The river upstream from Glen Garnock.]] | ||
[[File:111007 Glengarnock Castle above glen and river.jpg|thumb|200px|<center>The ravine of Glen Garnock, and Glengarnock Castle.]] | [[File:111007 Glengarnock Castle above glen and river.jpg|thumb|200px|<center>The ravine of Glen Garnock, and Glengarnock Castle.]] | ||
| − | " | + | "Glen Garnock" pertains specifically to the short, sometimes precipitous, section of ravine overlooked by the ruins of [[Glengarnock Castle]] north of Kilbirnie, whereas "The [[Garnock Valley]]" refers to a wider geographic area of [[North Ayrshire]] abutting [[Renfrewshire]], which encompassees the former parishes of [[Beith]], [[Dalry]], and [[Kilbirnie]]. |
== Estuary == | == Estuary == | ||
[[Image:Irvineharbourseaward.JPG|left|thumb|<center>The Garnock Estuary with Irvine Harbour.]] | [[Image:Irvineharbourseaward.JPG|left|thumb|<center>The Garnock Estuary with Irvine Harbour.]] | ||
| − | Within Ayrshire by far the largest [[estuary]] has developed, behind the Ardeer Peninsula, at the confluence of the Irvine and Garnock Rivers. This is one of the best examples of a bar-built estuary in the UK and is the only major estuary between the | + | Within Ayrshire by far the largest [[estuary]] has developed, behind the Ardeer Peninsula, at the confluence of the Irvine and Garnock Rivers. This is one of the best examples of a bar-built estuary in the UK and is the only major estuary between the Solway Firth and Inner River Clyde. The majority of the estuary has been designated a SSSI, in recognition of its national importance for three bird species Common Eider, red-breasted merganser and Goldeneye duck). It is also a nationally important feeding ground for thousands of migrating birds during the spring and autumn. Otters and water voles live on the estuary as well as numerous breeding birds, including water rail, grasshopper warbler and sand martin. The Garnock/Irvine estuary is also a Wildlife Site. |
| − | Bogside Flats SSSI covers 253.8ha that include inter-tidal mudflats, salt-marsh and adjacent pasture land. | + | Bogside Flats SSSI covers 253.8ha that include inter-tidal mudflats, salt-marsh and adjacent pasture land. |
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*[[Spout of Garnock]] is the highest waterfall in Ayrshire. | *[[Spout of Garnock]] is the highest waterfall in Ayrshire. | ||
*[[Glengarnock Castle]] is a ruined keep standing on a remote rocky promontory overlooking the river, located about {{convert|2|mi|km}} north of Kilbirnie. | *[[Glengarnock Castle]] is a ruined keep standing on a remote rocky promontory overlooking the river, located about {{convert|2|mi|km}} north of Kilbirnie. | ||
| − | *Nether Mill | + | *Nether Mill (or Nethermyln), in Kilbirnie, is a ruined watermill that leaves as its legacy the name of the local football team, [[Kilbirnie Ladeside]], who originally played in a field beside the mill lade running from a weir on the river to the mill at the end of Knoxville Road. |
| − | *[[Dalgarven Mill]] still draws water from the Garnock to turn the restored undershot | + | *[[Dalgarven Mill]] still draws water from the Garnock to turn the restored undershot waterwheel. The mill complex, located off the A737 road north of Kilwinning, is now a tourist attraction with the mill building being home to the Museum of Ayrshire Country Life and Costume. |
| − | * Kilwinning Viaduct, on the former [[Lanarkshire and Ayrshire Railway]], is now used by the | + | * Kilwinning Viaduct, on the former [[Lanarkshire and Ayrshire Railway]], is now used by the Sustrans Garnock Valley Cycleway to get across the river. |
*[[Eglinton Country Park]] was developed around the ancient Eglinton Estate, home for 600 years to the Earls of Eglinton and Winton. | *[[Eglinton Country Park]] was developed around the ancient Eglinton Estate, home for 600 years to the Earls of Eglinton and Winton. | ||
| − | *In the River Garnock some distance below Kilwinning Bridge in the Dirrans area, in the vicinity of the old saw mill and close to where the lade to the mill started, | + | *In the River Garnock some distance below Kilwinning Bridge in the Dirrans area, in the vicinity of the old saw mill and close to where the lade to the mill started, was Saint Ninian's Isle, named after the saint who is otherwise mainly commemorated at Whithorn. It is now part of the river banking. |
*Down river near the confluence with the Lugton Water were the 'Mess(rs?) Johns Steps'; stepping stones across the river as shown on the first edition of the 6 inch OS map. | *Down river near the confluence with the Lugton Water were the 'Mess(rs?) Johns Steps'; stepping stones across the river as shown on the first edition of the 6 inch OS map. | ||
*Between Ninian's Isle and the steps, just before the bend of the river, is an area named Cullim's Hole. | *Between Ninian's Isle and the steps, just before the bend of the river, is an area named Cullim's Hole. | ||
| − | *Smith records in 1895 that an island called Ringen's Isle existed in the Garnock. This may have been named after Saint Ringen or Winning. | + | *Smith records in 1895 that an island called Ringen's Isle existed in the Garnock. This may have been named after Saint Ringen or Winning. |
| − | *[[Atlantic salmon|Salmon]] generally arrive in the Garnock at the end of July, with the most productive part of the river being the stretch between Kilbirnie and Dalry. | + | *[[Atlantic salmon|Salmon]] generally arrive in the Garnock at the end of July, with the most productive part of the river being the stretch between Kilbirnie and Dalry. |
| − | *Garnock Floods is a wildlife reserve of the Scottish Wildlife Trust in Kilwinning; sandwiched between the railway line, Sandy Road and the river. | + | *Garnock Floods is a wildlife reserve of the Scottish Wildlife Trust in Kilwinning; sandwiched between the railway line, Sandy Road and the river. |
| − | *[[Nobel Enterprises|Ardeer Factory]], once the world's largest commercial explosives factory, is situated on a natural peninsula with the Firth of Clyde on its west side, the River Garnock to the east, and the mouth of the River Irvine to the south. | + | *[[Nobel Enterprises|Ardeer Factory]], once the world's largest commercial explosives factory, is situated on a natural peninsula with the Firth of Clyde on its west side, the River Garnock to the east, and the mouth of the River Irvine to the south. |
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=== Pundeavon Burn === | === Pundeavon Burn === | ||
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The Pundeavon Burn drains from Pundeavon Reservoir and enters the Garnock just upstream of Kilbirnie Cross. | The Pundeavon Burn drains from Pundeavon Reservoir and enters the Garnock just upstream of Kilbirnie Cross. | ||
=== Paduff Burn === | === Paduff Burn === | ||
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The Paduff Burn is a small stream, known locally as Jock's Burn, which comes into play on the golf course at Kilbirnie Place Golf Club. | The Paduff Burn is a small stream, known locally as Jock's Burn, which comes into play on the golf course at Kilbirnie Place Golf Club. | ||
| − | [[Image:Speir's Powgreen burn upper.JPG|right|thumb|Powgree Burn<br> near | + | [[Image:Speir's Powgreen burn upper.JPG|right|thumb|Powgree Burn<br> near Speir's school from Broadstone Bridge.]] |
=== Powgree Burn === | === Powgree Burn === | ||
| − | + | The Powgree Burn rises on Cuff hill in the Gateside area, runs east of the old Speir's school, through Meikle Auchengree and Longbar then shortly after runs under [[Glengarnock railway station]]. | |
| − | The Powgree Burn rises on Cuff hill | ||
=== Pitcon Burn === | === Pitcon Burn === | ||
| − | + | The Pitcon Burn cuts deep into the hillside causing the tree lined gully known as Swinlees Glen, a Nature Conservation Site, and enters the Garnock near its namesake Pitcon House. | |
| − | The Pitcon Burn cuts deep into the hillside causing the tree lined gully known as Swinlees Glen, | ||
=== Rye Water === | === Rye Water === | ||
[[Image:Rye Water Ford, Dalry.JPG|right|thumb|<center>The Rye Water and ford in Dalry.]] | [[Image:Rye Water Ford, Dalry.JPG|right|thumb|<center>The Rye Water and ford in Dalry.]] | ||
| − | + | The Rye Water drains from the area of Muirhead Reservoir and Camphill Reservoir and runs through the old village of Drakemyre to join the Garnock north of Dalry near Brownhill Junction on the main [[Glasgow, Paisley, Kilmarnock and Ayr Railway|railway line]]. A ford across the river at Drakemyre is associated with the song "Comin' Thro' the Rye". | |
| − | The Rye Water drains from the area of Muirhead Reservoir and Camphill Reservoir and runs through the old village of | ||
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=== Putyan Burn === | === Putyan Burn === | ||
[[Image:Broadlie House Dam.JPG|right|thumb|<center>The weir or dam on the Putyan Burn.]] | [[Image:Broadlie House Dam.JPG|right|thumb|<center>The weir or dam on the Putyan Burn.]] | ||
| − | The Putyan Burn forms from a number of small burns, etc., such as the Baidland Burn from Baidland Hill and springs at Baidland Mill. It reaches its confluence with the Garnock at Putyan Cottage and the Lynn Holm, near the road junnction for Ardrossan at the Kilwinning end of the town. It passes Broadlie House where a small weir or dam still exists as part of an abandoned 1892 hydroelectric scheme which provided the house with its own electricity. | + | The Putyan Burn forms from a number of small burns, etc., such as the Baidland Burn from Baidland Hill and springs at Baidland Mill. It reaches its confluence with the Garnock at Putyan Cottage and the Lynn Holm, near the road junnction for Ardrossan at the Kilwinning end of the town. It passes Broadlie House where a small weir or dam still exists as part of an abandoned 1892 hydroelectric scheme which provided the house with its own electricity. The burn has its confluence with the Garnock near the Lovers' Bridge in Dalry. |
[[Image:Lynn Spout, Caaf Water.JPG|thumb|right|Lynn Glen]] | [[Image:Lynn Spout, Caaf Water.JPG|thumb|right|Lynn Glen]] | ||
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=== Caaf Water === | === Caaf Water === | ||
{{Main|Caaf Water}} | {{Main|Caaf Water}} | ||
| − | + | The Caaf Water drains from Caaf Reservoir and soon passes the Michelin star rated Braidwoods Restaurant, before entering the Lynn Glen with its picturesque waterfall and finally enters the Garnock south of Dalry. | |
| − | The Caaf Water drains from Caaf Reservoir | ||
=== Bombo Burn === | === Bombo Burn === | ||
| − | + | The Bombo Burn is a small stream, only about {{convert|5|mi|km}} in length, that runs across the north side of Bankhead Moss, a Special Area of Conservation and joins the Garnock soon after passing through the Blair Estate: | |
| − | The Bombo Burn is a small stream, only about {{convert|5|mi|km}} in length, that runs across the north side of Bankhead Moss, a Special Area of Conservation | + | <blockquote> The delightfully landscaped grounds and gardens of the Estate contain a wonderful mixture of species trees and shrubs from all over the world. The Bombo Burn meanders gently for a mile through the gardens creating many natural beauty spots. The ancient yew tree recorded in the ''Domesday Book'' leans over the banks of the Bombo Burn presiding on the changes over the centuries.</blockquote> |
| − | <blockquote> The delightfully landscaped grounds and gardens of the Estate contain a wonderful mixture of species trees and shrubs from all over the world. The Bombo Burn meanders gently for a mile through the gardens creating many natural beauty spots. The ancient yew tree recorded in the '' | ||
{{clr}} | {{clr}} | ||
=== Dusk Water === | === Dusk Water === | ||
| − | + | [[Image:Dusk Water at Hessilhead Farm Town.JPG|right|thumb|<center>The Dusk Water at Hessilhead Town Farm running down towards the old saw mill.]] | |
| − | [[Image:Dusk Water at Hessilhead Farm Town.JPG|right|thumb|<center>The Dusk Water at | + | The Dusk Water is a stream that has its beginnings on Cuff Hill, near [[Beith]], and runs through [[Barrmill]] to eventually join the Garnock upstream of Dalgarven Mill. |
| − | The Dusk Water is a stream that has its beginnings on Cuff Hill, near [[Beith]], and runs through [[Barrmill]] to eventually join the Garnock upstream of | ||
| − | Interesting places along its course, as well as several old watermills, are | + | Interesting places along its course, as well as several old watermills, are Barony and Castle of Giffen, a large and handsome mansion-house, and Cleeves Cove, a system of caves in the Dusk Glen. |
[[Image:Coldstreammillk.jpg|thumb|left|Coldstream Mill]] | [[Image:Coldstreammillk.jpg|thumb|left|Coldstream Mill]] | ||
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==== Mills ==== | ==== Mills ==== | ||
| − | *[[Hessilhead|Coldstream Mill]] is located on the south side of Cuff Hill. The grain mill can still operate today, albeit only for demonstration purposes, | + | *[[Hessilhead|Coldstream Mill]] is located on the south side of Cuff Hill. The grain mill can still operate today, albeit only for demonstration purposes, with water supplied from the scenic mill dam. |
| − | *[[ | + | *[[Giffen Mill]] (or Barr Mill) is a ruined grain mill in the village of [[Barrmill]]. |
| − | *Blair Mill was a traditional corn mill for the large Blair estate in Dalry. It was probably built in the late 18th century and ceased to be used as a mill in the 1950s. | + | *Blair Mill was a traditional corn mill for the large Blair estate in Dalry. It was probably built in the late 18th century and ceased to be used as a mill in the 1950s. |
*Waterside Mill, lying downstream of the Dusk Glen, is now a residence. | *Waterside Mill, lying downstream of the Dusk Glen, is now a residence. | ||
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[[Image:Lugton Water and Garnock Confluence.JPG|right|thumb|<center>The confluence of the Lugton Water and the River Garnock.]] | [[Image:Lugton Water and Garnock Confluence.JPG|right|thumb|<center>The confluence of the Lugton Water and the River Garnock.]] | ||
{{Main|Lugton Water}} | {{Main|Lugton Water}} | ||
| − | + | The Lugton Water, the largest tributary of the Garnock, runs 14 miles from Loch Libo (395 feet above sea-level) in [[Uplawmoor]], through [[Lugton]] and the parishes of Neilston, Beith, Dunlop, Stewarton and Kilwinning. The Lugton joins the Garnock below the tidal limit, shortly after passing through [[Eglinton Country Park]], developed around the ancient estate of the Earl of Eglinton. | |
| − | The Lugton Water, the largest tributary of the Garnock, runs | ||
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== River Irvine == | == River Irvine == | ||
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{{main|River Irvine}} | {{main|River Irvine}} | ||
| − | The two main rivers of North Ayrshire, the Irvine and the Garnock, come together in the | + | The two main rivers of North Ayrshire, the Irvine and the Garnock, come together in the River Garnock at Irvine Harbour where they jointly enter the [[Firth of Clyde]]. |
Major tributaries of the Irvine are the Glen Water, Cessnock Water, Kilmarnock Water (combined Fenwick and Craufurdland Waters), Carmel Water and Annick Water.. | Major tributaries of the Irvine are the Glen Water, Cessnock Water, Kilmarnock Water (combined Fenwick and Craufurdland Waters), Carmel Water and Annick Water.. | ||
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On June 20, 1833 the surface of the Garnock was seen to be ruffled and it was discovered that a section of the river bed had collapsed into mineworkings beneath. The river was now flowing into miles of mineworkings of the Snodgrass, Bartonholm and Longford collieries. Attempts were made to block the breach with clay, whin, straw, etc. to no avail. The miners had been safely brought to the surface and were able to witness the sight of the river standing dry for nearly a mile downstream, with fish jumping about in all directions. The tide brought in sufficient water to complete the flooding of the workings and the river level returned to normal. The weight of the floodwater was so great that the compressed air broke through the ground in many places and many acres of ground were observed to bubble up like a pan of boiling water. In some places rents and cavities appeared measuring four or five feet in diameter, and from these came a roaring sound described as being like steam escaping from a safety valve. For about five hours great volumes of water and sand were thrown up into the air like fountains and the mining villages of Bartonholm, Snodgrass, Longford and Nethermains were flooded. | On June 20, 1833 the surface of the Garnock was seen to be ruffled and it was discovered that a section of the river bed had collapsed into mineworkings beneath. The river was now flowing into miles of mineworkings of the Snodgrass, Bartonholm and Longford collieries. Attempts were made to block the breach with clay, whin, straw, etc. to no avail. The miners had been safely brought to the surface and were able to witness the sight of the river standing dry for nearly a mile downstream, with fish jumping about in all directions. The tide brought in sufficient water to complete the flooding of the workings and the river level returned to normal. The weight of the floodwater was so great that the compressed air broke through the ground in many places and many acres of ground were observed to bubble up like a pan of boiling water. In some places rents and cavities appeared measuring four or five feet in diameter, and from these came a roaring sound described as being like steam escaping from a safety valve. For about five hours great volumes of water and sand were thrown up into the air like fountains and the mining villages of Bartonholm, Snodgrass, Longford and Nethermains were flooded. | ||
| − | Archibald William, the enterprising 13th [[Earl of Eglinton]] purchased all the lands concerned in 1852 and through the simple expedient of cutting a short canal at Bogend, across the loop of the river involved, he bypassed the breach and once the river course had been drained and sealed off he was able to have the flooded mineworkings pumped out. The breach lay on the sea side of the loop close to Bogend on the Snodgrass Holm side. | + | Archibald William, the enterprising 13th [[Earl of Eglinton]] purchased all the lands concerned in 1852 and through the simple expedient of cutting a short canal at Bogend, across the loop of the river involved, he bypassed the breach and once the river course had been drained and sealed off he was able to have the flooded mineworkings pumped out. The breach lay on the sea side of the loop close to Bogend on the Snodgrass Holm side. The Earl leased the mines to Bairds of Gartsherrie and the "Eglinton Iron Works" were born. |
== The curse of Saint Winning == | == The curse of Saint Winning == | ||
[[File:Bridgend weir on the Garnock.JPG|thumb|200px|The old Bridgend Mill weir, once the possession of Kilwinning Abbey]] | [[File:Bridgend weir on the Garnock.JPG|thumb|200px|The old Bridgend Mill weir, once the possession of Kilwinning Abbey]] | ||
| − | A legend tells of [[Kilwinning Abbey|Saint Winning]] sending his monks to fish in the Garnock, however no matter how hard they tried or how long they persevered they could catch nothing. The saint in response placed a curse on the river, preventing it from ever having fish in its waters; the river responded by changing course and thereby avoiding the curse. It is clear that the river has substantially changed its course in recorded history, previously having entered the sea at Stevenston. Ardeer therefore being an island at that time. Blaeu's map printed in 1654 shows this. | + | A legend tells of [[Kilwinning Abbey|Saint Winning]] sending his monks to fish in the Garnock, however no matter how hard they tried or how long they persevered they could catch nothing. The saint in response placed a curse on the river, preventing it from ever having fish in its waters; the river responded by changing course and thereby avoiding the curse. It is clear that the river has substantially changed its course in recorded history, previously having entered the sea at Stevenston. Ardeer therefore being an island at that time. Blaeu's map printed in 1654 shows this. |
It was also noted during the construction of a canal serving early coal pits at Ardeer that the small lochans used to ease construction lay on the old course of the River Garnock. | It was also noted during the construction of a canal serving early coal pits at Ardeer that the small lochans used to ease construction lay on the old course of the River Garnock. | ||
==The Earls of Eglinton== | ==The Earls of Eglinton== | ||
| − | It is recorded in official documents of the 1770 ''"Trial of Mungo Campbell for the Murder of Alexander, Earl of Eglinton"'' that [[Alexander Montgomerie, 10th Earl of Eglinton|Alexander Montgomery, 10th Earl of Eglinton]] was very protective of his fishing rights on the River Garmock to the extent that he banned fishing on the river altogether. | + | It is recorded in official documents of the 1770 ''"Trial of Mungo Campbell for the Murder of Alexander, Earl of Eglinton"'' that [[Alexander Montgomerie, 10th Earl of Eglinton|Alexander Montgomery, 10th Earl of Eglinton]] was very protective of his fishing rights on the River Garmock to the extent that he banned fishing on the river altogether. Murder of Alexander Montgomerie even sold his fishing rod; however the murder of the earl in 1769 was as a direct result of Mungo being accused of poaching at Ardrossan's North Bay and Lord Eglinton's attempt to confiscate his gun. |
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Revision as of 09:43, 25 October 2015
| River Garnock Gairneag / Abhainn Ghairneig | |||
| Spout_of_Garnock.jpg | |||
| Country | |||
| Scotland | |||
| Local Authority | |||
| North Ayrshire | |||
| Length | |||
| 39 miles (62.8 km) | |||
| Source | |||
| Hill of Stake | |||
| Source Elevation | |||
| 522 metres (1712.6 ft) | |||
| Mouth | |||
| Irvine, Firth of Clyde | |||
The River Garnock, the smallest of Ayrshire's six principal rivers, has its source on the southerly side of the Hill of Stake in the heart of the Clyde Muirshiel Regional Park. About a mile and a half south of this starting point the untested stream tumbles over the Spout of Garnock, the highest waterfall in Ayrshire, once thought to be the river's origin. The river then continues, for a total length of 20 miles (32 km) or so, through the towns of Kilbirnie, Glengarnock, Dalry and Kilwinning to its confluence with the River Irvine at Irvine Harbour.
The main tributaries are the Rye Water and Caaf Water which join north and south of Dalry respectively and the Lugton Water which joins just south of Kilwinning. Template:TOC left
Contents
Garnock Valley
File:111007 River Garnock from Burnt Hill.jpg The river upstream from Glen Garnock.
File:111007 Glengarnock Castle above glen and river.jpg The ravine of Glen Garnock, and Glengarnock Castle.
"Glen Garnock" pertains specifically to the short, sometimes precipitous, section of ravine overlooked by the ruins of Glengarnock Castle north of Kilbirnie, whereas "The Garnock Valley" refers to a wider geographic area of North Ayrshire abutting Renfrewshire, which encompassees the former parishes of Beith, Dalry, and Kilbirnie.
Estuary
File:Irvineharbourseaward.JPG The Garnock Estuary with Irvine Harbour.
Within Ayrshire by far the largest estuary has developed, behind the Ardeer Peninsula, at the confluence of the Irvine and Garnock Rivers. This is one of the best examples of a bar-built estuary in the UK and is the only major estuary between the Solway Firth and Inner River Clyde. The majority of the estuary has been designated a SSSI, in recognition of its national importance for three bird species Common Eider, red-breasted merganser and Goldeneye duck). It is also a nationally important feeding ground for thousands of migrating birds during the spring and autumn. Otters and water voles live on the estuary as well as numerous breeding birds, including water rail, grasshopper warbler and sand martin. The Garnock/Irvine estuary is also a Wildlife Site.
Bogside Flats SSSI covers 253.8ha that include inter-tidal mudflats, salt-marsh and adjacent pasture land.
Places of interest
File:Dalagarvenbridge.JPG
Dalgarven Bridge
leading to the Mill
leading to the Mill
File:Kilwinning viaduct.jpg
Kilwinning Viaduct
File:Rivergarnockici.JPG
Ardeer Factory
the disused jetty
the disused jetty
File:Garnock Island at Kilwinning.JPG The islet in the Garnock at Kilwinning, just upstream of the bridge and shown as part of the old Bleaching Green on the 1896 OS map.
- Clyde Muirshiel Regional Park is the source of the headwaters of the Garnock.
- Spout of Garnock is the highest waterfall in Ayrshire.
- Glengarnock Castle is a ruined keep standing on a remote rocky promontory overlooking the river, located about 2 miles (3.2 km) north of Kilbirnie.
- Nether Mill (or Nethermyln), in Kilbirnie, is a ruined watermill that leaves as its legacy the name of the local football team, Kilbirnie Ladeside, who originally played in a field beside the mill lade running from a weir on the river to the mill at the end of Knoxville Road.
- Dalgarven Mill still draws water from the Garnock to turn the restored undershot waterwheel. The mill complex, located off the A737 road north of Kilwinning, is now a tourist attraction with the mill building being home to the Museum of Ayrshire Country Life and Costume.
- Kilwinning Viaduct, on the former Lanarkshire and Ayrshire Railway, is now used by the Sustrans Garnock Valley Cycleway to get across the river.
- Eglinton Country Park was developed around the ancient Eglinton Estate, home for 600 years to the Earls of Eglinton and Winton.
- In the River Garnock some distance below Kilwinning Bridge in the Dirrans area, in the vicinity of the old saw mill and close to where the lade to the mill started, was Saint Ninian's Isle, named after the saint who is otherwise mainly commemorated at Whithorn. It is now part of the river banking.
- Down river near the confluence with the Lugton Water were the 'Mess(rs?) Johns Steps'; stepping stones across the river as shown on the first edition of the 6 inch OS map.
- Between Ninian's Isle and the steps, just before the bend of the river, is an area named Cullim's Hole.
- Smith records in 1895 that an island called Ringen's Isle existed in the Garnock. This may have been named after Saint Ringen or Winning.
- Salmon generally arrive in the Garnock at the end of July, with the most productive part of the river being the stretch between Kilbirnie and Dalry.
- Garnock Floods is a wildlife reserve of the Scottish Wildlife Trust in Kilwinning; sandwiched between the railway line, Sandy Road and the river.
- Ardeer Factory, once the world's largest commercial explosives factory, is situated on a natural peninsula with the Firth of Clyde on its west side, the River Garnock to the east, and the mouth of the River Irvine to the south.
Tributaries
Pundeavon Burn
The Pundeavon Burn drains from Pundeavon Reservoir and enters the Garnock just upstream of Kilbirnie Cross.
Paduff Burn
The Paduff Burn is a small stream, known locally as Jock's Burn, which comes into play on the golf course at Kilbirnie Place Golf Club.
File:Speir's Powgreen burn upper.JPG
Powgree Burn
near Speir's school from Broadstone Bridge.
near Speir's school from Broadstone Bridge.
Powgree Burn
The Powgree Burn rises on Cuff hill in the Gateside area, runs east of the old Speir's school, through Meikle Auchengree and Longbar then shortly after runs under Glengarnock railway station.
Pitcon Burn
The Pitcon Burn cuts deep into the hillside causing the tree lined gully known as Swinlees Glen, a Nature Conservation Site, and enters the Garnock near its namesake Pitcon House.
Rye Water
File:Rye Water Ford, Dalry.JPG The Rye Water and ford in Dalry.
The Rye Water drains from the area of Muirhead Reservoir and Camphill Reservoir and runs through the old village of Drakemyre to join the Garnock north of Dalry near Brownhill Junction on the main railway line. A ford across the river at Drakemyre is associated with the song "Comin' Thro' the Rye".
Putyan Burn
File:Broadlie House Dam.JPG The weir or dam on the Putyan Burn.
The Putyan Burn forms from a number of small burns, etc., such as the Baidland Burn from Baidland Hill and springs at Baidland Mill. It reaches its confluence with the Garnock at Putyan Cottage and the Lynn Holm, near the road junnction for Ardrossan at the Kilwinning end of the town. It passes Broadlie House where a small weir or dam still exists as part of an abandoned 1892 hydroelectric scheme which provided the house with its own electricity. The burn has its confluence with the Garnock near the Lovers' Bridge in Dalry.
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Lynn Glen
Caaf Water
The Caaf Water drains from Caaf Reservoir and soon passes the Michelin star rated Braidwoods Restaurant, before entering the Lynn Glen with its picturesque waterfall and finally enters the Garnock south of Dalry.
Bombo Burn
The Bombo Burn is a small stream, only about 5 miles (8.0 km) in length, that runs across the north side of Bankhead Moss, a Special Area of Conservation and joins the Garnock soon after passing through the Blair Estate:
The delightfully landscaped grounds and gardens of the Estate contain a wonderful mixture of species trees and shrubs from all over the world. The Bombo Burn meanders gently for a mile through the gardens creating many natural beauty spots. The ancient yew tree recorded in the Domesday Book leans over the banks of the Bombo Burn presiding on the changes over the centuries.
Dusk Water
File:Dusk Water at Hessilhead Farm Town.JPG The Dusk Water at Hessilhead Town Farm running down towards the old saw mill.
The Dusk Water is a stream that has its beginnings on Cuff Hill, near Beith, and runs through Barrmill to eventually join the Garnock upstream of Dalgarven Mill.
Interesting places along its course, as well as several old watermills, are Barony and Castle of Giffen, a large and handsome mansion-house, and Cleeves Cove, a system of caves in the Dusk Glen.
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Coldstream Mill
Mills
- Coldstream Mill is located on the south side of Cuff Hill. The grain mill can still operate today, albeit only for demonstration purposes, with water supplied from the scenic mill dam.
- Giffen Mill (or Barr Mill) is a ruined grain mill in the village of Barrmill.
- Blair Mill was a traditional corn mill for the large Blair estate in Dalry. It was probably built in the late 18th century and ceased to be used as a mill in the 1950s.
- Waterside Mill, lying downstream of the Dusk Glen, is now a residence.
Lugton Water
File:Lugton Water and Garnock Confluence.JPG The confluence of the Lugton Water and the River Garnock.
The Lugton Water, the largest tributary of the Garnock, runs 14 miles from Loch Libo (395 feet above sea-level) in Uplawmoor, through Lugton and the parishes of Neilston, Beith, Dunlop, Stewarton and Kilwinning. The Lugton joins the Garnock below the tidal limit, shortly after passing through Eglinton Country Park, developed around the ancient estate of the Earl of Eglinton.
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Together at Irvine Harbour and out to the Firth of Clyde
River Irvine
The two main rivers of North Ayrshire, the Irvine and the Garnock, come together in the River Garnock at Irvine Harbour where they jointly enter the Firth of Clyde.
Major tributaries of the Irvine are the Glen Water, Cessnock Water, Kilmarnock Water (combined Fenwick and Craufurdland Waters), Carmel Water and Annick Water..
The Garnock and the Irvine
These rivers flow into the estuary, the Garnock being swelled by the Annick Water that has its confluence at the Dirrans in Kilwinning. The silt from these rivers has created the Bogside mudflats and the course of these rivers has been greatly altered over the centuries through natural, man made and even spiritual influences.
A mining disaster
On June 20, 1833 the surface of the Garnock was seen to be ruffled and it was discovered that a section of the river bed had collapsed into mineworkings beneath. The river was now flowing into miles of mineworkings of the Snodgrass, Bartonholm and Longford collieries. Attempts were made to block the breach with clay, whin, straw, etc. to no avail. The miners had been safely brought to the surface and were able to witness the sight of the river standing dry for nearly a mile downstream, with fish jumping about in all directions. The tide brought in sufficient water to complete the flooding of the workings and the river level returned to normal. The weight of the floodwater was so great that the compressed air broke through the ground in many places and many acres of ground were observed to bubble up like a pan of boiling water. In some places rents and cavities appeared measuring four or five feet in diameter, and from these came a roaring sound described as being like steam escaping from a safety valve. For about five hours great volumes of water and sand were thrown up into the air like fountains and the mining villages of Bartonholm, Snodgrass, Longford and Nethermains were flooded.
Archibald William, the enterprising 13th Earl of Eglinton purchased all the lands concerned in 1852 and through the simple expedient of cutting a short canal at Bogend, across the loop of the river involved, he bypassed the breach and once the river course had been drained and sealed off he was able to have the flooded mineworkings pumped out. The breach lay on the sea side of the loop close to Bogend on the Snodgrass Holm side. The Earl leased the mines to Bairds of Gartsherrie and the "Eglinton Iron Works" were born.
The curse of Saint Winning
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The old Bridgend Mill weir, once the possession of Kilwinning Abbey
A legend tells of Saint Winning sending his monks to fish in the Garnock, however no matter how hard they tried or how long they persevered they could catch nothing. The saint in response placed a curse on the river, preventing it from ever having fish in its waters; the river responded by changing course and thereby avoiding the curse. It is clear that the river has substantially changed its course in recorded history, previously having entered the sea at Stevenston. Ardeer therefore being an island at that time. Blaeu's map printed in 1654 shows this.
It was also noted during the construction of a canal serving early coal pits at Ardeer that the small lochans used to ease construction lay on the old course of the River Garnock.
The Earls of Eglinton
It is recorded in official documents of the 1770 "Trial of Mungo Campbell for the Murder of Alexander, Earl of Eglinton" that Alexander Montgomery, 10th Earl of Eglinton was very protective of his fishing rights on the River Garmock to the extent that he banned fishing on the river altogether. Murder of Alexander Montgomerie even sold his fishing rod; however the murder of the earl in 1769 was as a direct result of Mungo being accused of poaching at Ardrossan's North Bay and Lord Eglinton's attempt to confiscate his gun.
