River Irvine facts for kids
Quick facts for kidsIrvine
The Irvine near Drybridge
|Main source||near Loudoun Hill, Drumclog, Lanarkshire, Scotland
810 ft (250 m)
|River mouth||Firth of Clyde|
|Length||42 km (26 mi)|
|Basin size||380 km2 (150 sq mi)|
The River Irvine (Scottish Gaelic: Irbhinn) is a river that flows through southwest Scotland. Its watershed is on the Lanarkshire border of Ayrshire at an altitude of 810 feet (250 m) above sea-level, near Loudoun Hill, Drumclog, and 7 miles (11 kilometres) SW by W of Strathaven. It flows 29 1⁄2 mi (47.5 km) westward, dividing the old district of Cunninghame from that of Kyle, until it reaches the sea via Irvine Harbour in the form of the Firth of Clyde, and flows into Irvine Bay by the town of Irvine. It has many tributaries, some of which form parish, district and other boundaries.
- The course of the Irvine and its tributaries
- The river at work
- The river at play
- Holy waters and mineral springs
- Minor tributaries
- Waterfalls and weirs
- Crossing the river
- Taming the river
- The river system and its wildlife
- Micro history
Irvine was first recorded in 1258 as Yrewyn, and several etymologies have been proposed. According to Groome, Irvine is derived from the Gaelic iar-an meaning 'westward-flowing' river. A Brittonic origin is also possible. The root *arb-īno, meaning "wild turnip" has been suggested (c.f. Welsh erfin), though the earliest record and the possibly identical River Irfon in Wales do not encourage this. The Middle Welsh adjective erbyn meaning "hostility, fighting against" might also be considered here. An ancient river-name formation of very obscure origin is also quite probable.
The course of the Irvine and its tributaries
The River Irvine rises in two head-waters, the one in a moss at Meadow-head, on the eastern boundary of the parish of Loudoun or of Ayrshire, and the other a mile eastward in the parish of Avondale in Lanarkshire, near the battle-field of Drumclog.
About 2¾ miles (4.4 km) from the point it enters Ayrshire, Glen Water joins it from the north. Strictly speaking Glen Water is the parent stream, because it is longer and carries more water; for the Glen Water rises at Crosshill in Renfrewshire, a mile (1.6 km) north of the East Ayrshire boundary, and runs 6 miles (9.7 km) southward, joined by five rills (small streams) in its progress, to the point of confluence with the Irvine. Swollen by the Glen Water, the Irvine immediately passes the town of Darvel on the right, then 1¾ mile (2.8 km) onward, the town of Newmilns and 2¼ miles (3.6 km) farther on, the town of Galston, on the left. The Hagg burn joins before the town, having run past the old ruined castle of Arclowden: Old Loudoun Castle or "The Old Place", near the present Loudoun castle. The Burnanne joins at Galston.
A mile and a quarter (2 km) below Galston it receives from the north the Polbaith burn; ¾ of a mile (1.2 km) lower down, the Cessnock water joins it from the south; and 3 miles (4.8 km) later it passes Kilmarnock and Riccarton on opposite sides, and receives on its right bank the tributary of the Kilmarnock (or Marnock) Water. Four miles (6.4 km) or more along its bed, Carmel Water joins it on the right bank; and 2½ miles (4 km) farther on, it receives the Annick Water, again on the right bank. The river now runs 1½ mile (2.4 km) in a north-west direction, passing through the town of Irvine; it then suddenly bends round until it follows a southerly direction; and opposite the town of Irvine, when running southward, it suddenly expands into a basin ¾ of a mile (1.2 km) wide. It receives the Garnock river at its north-west extremity, and communicates by a narrow mouth or strait with the Firth (previously Frith) of Clyde. The course of the Irvine is recorded as having shifted in an old Eglinton Estates document, a map recording the previous course with a note that the water left the old riverbed in 1758. This altered the confluence of the River Irvine with the Annick Water.
The Irvine is tidal as far as the nature reserve at Shewalton, half-a-mile (800 m) or so upstream from the confluence with the Annick Water.
The main contributing rivers and rivulets in descending order of their confluences are therefore the Glen Water, Polbaith Burn, Cessnock Water, Kilmarnock Water, Carmel Water, Annick Water, and the Garnock.
Views of the River Irvine in 2007
Many watercourses have changed direction over the years for various reasons. The Kilmarnock Water used to run slightly to the west as it passes through the Howard Park in Kilmarnock, previously 'Barbadoes Green'; the old 'fossilised' river bank is still discernible. It is said that this was done deliberately by a Lord Boyd, the local laird, so that he could claim more land. The river formed the boundary and by moving it permanently he gained more land.
St. Winnan of Kilwinning is said to have made the River Garnock change its course and follow another "adverse to nature". The river's mistake was to fail to deliver up any fish to one of the saint's angler friends!
The Garnock, Annick and Irvine did not even have the same confluence within recorded history, for Timothy Pont's (1604–08) and Herman Moll's (1745) maps show the Garnock emptying into the sea, about two miles (3 km) from the mouth of the Irvine. The Annick did not flow into the Garnock at this time and the Ardeer peninsula was an island. Subsequent to Pont's time, the sea came right up to the town, with vessels loading and unloading at the Seagate, which is now half-a-mile from the sea.
The Earl of Eglinton changed the course of the Lugton Water where it ran through what is now Eglinton Country Park.
Adamson records that a link once existed between the Carmel Water and the Fenwick Water so as to provide more water for the needs of cutlers and tinkers in Kilmaurs. The king allowed the diversion of water that would flow through the 'leg of a boot'.
The parishes that border the river's south bank are Galston, Riccarton, and Dundonald; and on its north side are Loudoun, Kilmarnock, Kilmaurs, Dreghorn and Perceton, and Irvine.
The presence of country estates effected the river and its tributaries, often through landscaping and engineering works such as weirs, embankments and minor alterations of its course. The feudal or Victorian estates of Loudoun castle (ruin), Cessnock house, Lanfine house, Holms house (ruin), Kilmarnock house (demolished), Peel house, Caprington, Fairlie house, Craig house (restored 2006), Newfield, Auchans (demolished), and Shewalton (demolished) were all connected with the River Irvine and on the banks of its tributaries are Craufurdland (Craufurdland Water) and Dean castle (Fenwick Water), the two joining to form the Kilmarnock Water; Rowallan, Tour house, Kilmaurs Place, Carmel Bank and Busbie castle (demolished) on the Carmel; Lainshaw (restored 2006), Chapelton (demolished), Annick Lodge, and Bourtreehill (demolished) on the Annick Water; Aiket, Bonshaw (demolished) and Kennox House on the Glazert, and Lambroughton on the Garrier. In the area around Stewarton the valley of the Annick Water was known as 'Strathannick'. Dunlop house and Corsehill castle (ruin) are on the Clerkland Burn and Robertland House is on the Swinzie Burn, both of which flow into the Annick Water.
A large procumbent boulder known on the OS map as the 'Carlin's Stone' lies next to the Carlin Burn near Craigends Farm below Cameron's Moss in East Ayrshire. A Carl is a commoner, a husband or in a derogatory sense, a churl or male of low birth. More commonly the name Carlin was used as a derogatory term for a woman meaning an 'old hag'. It is also said to be a corruption of the Gaelic word "Cailleach", meaning a witch or the 'old Hag', the Goddess of Winter. This would therefore be the Witch's or Hag's Stone, one of several in Scotland with this name. It has been much visited at one time, with the clear remains of a footbridge running to it across the Hareshawmuir Water.
The Grannie Stane (or Granny Stane) is described as "one of Irvine's prehistoric puzzles", this boulder is either left behind from the Ice Age or is the last remaining stone of a stone circle – others were removed, by blasting, after the Irvine weir was constructed in 1895, but popular protests saved this remaining stone. The Grannie Stane is visible when the water is low. It is unlikely to have gained its name from various similar sounding Roman and Celtic deities.
The river at work
Many of the weirs, dams and fords on the rivers were built on or developed at natural stone dikes, which already raised the water level at that point.
|Carmel, the oldest form of which is Caremuall, is thought to be derived, according to McNaught, from the Gaelic 'Car' meaning a 'fort', and 'Meall'. meaning a hill. Therefore, 'The fort on the hill'.|
In Kilmarnock in 1880 the Glencairn Mill stood near Riccarton, just before the two bridges, with a long lade running up to join the river near the Glenfield Iron Works; Richardland Brewery sat on the river bank and no doubt used its waters. A slaughter house sat where the Kilmarnock Water joins the Irvine, with an engine works just upstream from it. A Foundry, a forge and an engine works sat beside the Kilmarnock Water at Townholm.
A large number of mills existed along the length of the Annick Water, with only Cunninghamhead Mill still standing today (2006). The Corsehill Mills (corn and wool) were at Stewarton, powered by water from the Corsehill Burn, which arose from the Clerkland Burn. Lambroch Mill was located near Laigh Castleton Farm. Scroaggy or Fairliecrevoch Mill was a waulk mill for preparing cloth and existed until the 1960s, with its lade cutting across the large loop in the river near Ramstane. Downstream from Cunninghamhead was a sawmill and a corn mill existed in Perceton near the old church. Scroag or scrog is a crab apple or gnarled tree stumps in old Scots and this 'nickname' well describes the area where the mill stood.
At Galston the Burnanne joins the Irvine. This tributary was famous for its rich jasper pebbles; semi-precious stones, which were collected, cut and polished for use in jewellery.
The gravel bed of rivers was an important source of income for millers and others who owned the rights of extraction. The gravel was sold for various farm and horticultural purposes, such as infilling drainage ditches, the surfacing of field entrances and driveways, road surfaces, horticulture, etc.
In 1656 a report to Oliver Cromwell describes the port of Irvine at being "clogged up and almost choked with sand." In 1760 Irvine was the third most important port in Scotland, behind Port-Glasgow and Leith second.
The river at play
The River Irvine and its tributaries have many leisure uses, such as sailing, swimming, fishing, riparian walks, etc. Irvine harbour is now officially closed as a commercial port and now houses a number of privately owned pleasure craft. It is also now home to part of the Scottish Maritime Museum with numerous vessels on display, including the 'Spartan', one of the last surviving Clyde puffers.
Fishing is a very popular pursuit and many angling clubs maintain the river and its banks, monitor fish stocks, report on pollution and carry out conservation measures. Pont in 1604 – 08 writes that salmon are plentiful in the River Irvine. The river contains, amongst others, brown trout, sea trout, salmon, eels, minnows, and sticklebacks.
Rivers have always been used for swimming and one such favourite swimming pool, called the 'Toad Hole' is found near Ramstane on the Annick Water above Cunninghamhead. Many others exist, such as the 'Auld dam' and the 'Munt' on the Corsehill (Clerkland) burn at Stewarton, running into the Annick, which had 'Andra Sweelzies' and the Ladies 'Dookin' Hole.
Tributaries of the Irvine – 2007
The Annick Water from Bourtreehill.
The Chapel Burn near its confluence with the Annick Water.
The Cowlinn Burn from Clonbeith joining the Lugton Water at Montgreenan Castle.
The Glazert Rivulet and the Annick Water at Water Meetings with Rashillhouse Farm on the Horizon.
The River Garnock downstream from Dalgarven Mill.
Holy waters and mineral springs
The Burnanne or Burnawn joins the Irvine at Galston. It is named after St Anne, said to be the mother of the Virgin Mary. The St Anne's holy well is marked on the OS and lies above Bank wood, flowing into the Burn Anne. Maria's well lies on the Byrebank burn, in the Loudoun castle policies, which runs down near Loudoun Academy to join the Irvine.
A mineral spring is recorded as being near Stewarton, North Ayrshire, called the Bloak Well. Robinson gives the Scot's word 'blout' as meaning the 'eruption of fluid'.
Bloak Well was first discovered in 1800, 1810, or in around 1826, by the fact that pigeons from neighbouring parishes flocked here to drink. Mr. Cunningham of Lainshaw built a handsome house over the well in 1833 and appointed a keeper to take care of it as the mineral water was of some value. The mineral well waters empty into the Glazert, which joins the Annick Water at Watermeetings near Cunninghamhead.
The Chapel Burn rises near the Anderson Plantation in the fields below Lainshaw Mains and it is marked as a chalybeate or mineral spring on the 1911 6" OS map. Bore holes nearby suggest that the water was put to a more formal use at one time, supplying cattle troughs or possibly even for a stand pipe as mineral water was popular for its supposed curative properties. According to the opinion of the day, it could cure 'the colic, the melancholy, and the vapours; it made the lean fat, the fat lean; it killed flat worms in the belly, loosened the clammy humours of the body, and dried the over-moist brain. The main spring here has been covered over and the water piped out to the burn, which runs down to join the Annick Water at Chapeltoun Bridge.
In the woodland policies of Chapeltoun House is the Monk's Well (OS 1974), fountain or spring as indicated on the OS maps going back as far as 1858. Its present appearance is probably as a Victorian or Edwardian 'whimsy' or 'folly' with a large, thick sandstone 'tombstone appearance' with a slightly damaged cross carved in relief upon it and a spout through which the spring water once passed into a cast iron 'bowl'. It seems unlikely from the workmanship that this stone and cross have anything to do with the old chapel, but one possibility is that it came from over the entrance door to Laigh Chapelton as the custom was for a Templar property to have the 'cross' symbol of the order displayed in such a fashion. On the other hand, it could have been made for the Chapelton (old) House to associate the building with the Christian history of the site. The stone is unusually thick and has been clearly reworked to pass a spout through it. The OS record that in the 1970s a Mr. H. Gollan of Chapeltown stated that the 'Monk's Well', was believed to have been associated with the chapel. In July 1956 the OS state that the 'Monk's Well' is a spring emerging through a stone pipe, situated in a stone-faced cutting in the hill slope, the spring water running into the Annick Water.
The Monk's or Mack's or Maaks Well at Kilmaurs, pronounced 'Manks Well' runs into the Carmel beneath Kilmaurs Place. It is said that many years ago the local laird tried to prevent the local people from using the well. It dried up until the lord changed his mind, but has run continuously ever since. A few deaths have occurred here by drowning or by physical trauma
Next to the Kilmaurs-Glencairn church in Kilmaurs is a patch of woodland that was once an orchard. The Tour streamlet joins the Carmel nearby and before the confluence can be found an old well, arched over, known as the Lady's Well, with never-failing, excellent and refeshingly cool water. A small wooden bridge used to run across to the Lady's Well from the church glebe side.
Saint Inans well lies close to the river Irvine on a path running parallel to the Old Irvine Parish churchyard. It bears the date 839 AD (see photograph).
A monastic settlement and chapel of Saint Mary at the Thurgartstone near Dunlop's Chapel Crags, is a Christian centre established to eradicate the pagan significance of the site. Monastic cells, a chapel and a graveyard are all now lost to view, originally constructed by the monks of Kilwinning Abbey; only the name 'St. Marys' given to the nearby 'modern' dwellings, built on the site of the chapel record past significance. The Holy Well still exists, the nearby houses pumping water up from its source. The water from the well used to run under the road and emerge in a trough surrounded by a metal fence and then on into the Black Water, which joins the Glazert nearby. Only a concrete manhole indicates this trough now (2006). In 1856 the water for baptism in Dunlop Kirk was still drawn from this Holy Well.
St Winnans Well runs into the Garnock at Kilwinning and tradition ascribes healing properties to its holy waters. Dentibert well is on Mid Muir hill on the upper reaches of the Craufurdland water. A Lady's Well is also present near Auchmannoch farm on the upper reaches of the Craufurdland water.
A large number of burns and sykes run into the various Waters that eventually reach the Irvine. Many of these burns are either unnamed or the names are unrecorded. They are of interest in their own right as sources of local history through their etymology or as sites of historical events. The following list is not exhaustive and will be added to if printed evidence of otherwise 'lost' names is uncovered.
Auchmannoch burn flows into the Cessnock water. Auchruglin burn flows into the Irvine at Greenholm in Newmilns. Auldhouse burn joins the Rough Skye burn and flows into the Pogiven burn, which itself flows into the Glen water, which joins the Irvine at Darvel. Balgray Burn flows into the Carmel Water. Bareshaw burn flows into the Glen water. Barneight burn joins the Cessnock water near Lawers bridge. Birk burn flows into Craigendunton Reservoir, its water flowing out as part of the Dunton water. Black Gill waters flow into the Pockinan burn, which joins the Hareshawmuir water. Black water flows into the Glazert water at Dunlop. Blacks burn joins the Cessnock water at Lawers bridge. Bog burn rises below Whitelee Hill and flows into the Hareshawmuir water. Bowhill burn joins the Hag Burn and flows into the Irvine at Galston. Brackenburn flows into the Garrier burn, then into the Carmel and finally into the Irvine at Springside. Brides burn flows into the Annick Water in Stewarton near Brides Bridge. Brocklees burn flows into the Glen water via the Mucks water. Bucht burn rises at Todhills Moss and flows into the Whiteleehill burn and then on into the Hareshawmuir water. Bught burn rises near Lochgoin farm and flows into the Drumtee water, which itself flows into the Fenwick water. Burflatt burn flows into the Isles burn and joins the Irvine at Newmilns. Burnanne (Burnawn) flows directly into the Irvine at Galston.
Calf Fauld burn flows into the Dunton water at Dunton Cove, this water flows from Craigendunton Reservoir and joins the head water of the Craufurdland Water near Waterside. Capringstone Burn flows passed Overton and into the Annick Water near Dreghorn. Carlin burn flows near the Carlin stane and into the Hareshawmuir water. Clerkland burn rises near the Totherick and flows into the Corsehill burn, which joins the Annick water at Stewarton. Collorybog burn rises from the bog of that name and flows into the Fenwick water via the Drumtee water. Corsehill burn joins the Annick water at Stewarton. Cowlinn burn flows into the Lugton water at old Montgreenan castle. Cross Burn joins the Lugton Water near Caldwell House. Chapel burn rises near Lainshaw House from a chalybeate spring and runs into the Annick water at Chapeltoun bridge. Cuts burn flows into the Annick water near Games Hill in Stewarton. Davy's burn flows into the Hareshawmuir water. Downie's burn joins the Irvine at Townhead in Newmilns, having flowed through the Parkerston glen. Drumduff burn flows from the base of Drumduff Hill into the Loudoun water, which flows into the Glen water and into the Irvine at Darvel. Drumtee water flows into the Fenwick water. Dunton water flows from Craigendunton Reservoir and joins the head water of the Craufurdland Water near Waterside. Draught burn joins the Lugton water near Eglinton Country Park. Duniflat Burn joins the Lugton Water near Lugton. East burn joins the Annick water in Darlington, Stewarton. Fenwick water joins with the Craufurdland water and forms the Kilmarnock water, which runs into the Irvine at Riccarton. Gardrum Mill burn joins the Carmel water near Fenwick. Garrier burn flows into the Irvine near Springside. Garroch burn joins the Cessnock water. Gill burn rises below Queenseat Hill and its waters flow into the Greenfield burn, then into the Soame burn, next into the Kingswell burn and into the Fenwick water. Gills burn flows into the Black water near Dunlop. Glazert (Glassard in 1779) water flows into the Annick water at Watermeetings near Cunninghamhead. Glen Burn at Darvel, flowing into the Irvine directly. Glen Burn rises near Over Auchentiber by Blacklaw Hill. Gower water joins the Irvine at Priestland outside Darvel. Gowkshaw burn has a confluence with the Rough Hill burn and runs into the Hareshawmuir water. Greenfield burn flows into the Soame burn near Soame bridge on the B764 and flows into the Kingswell burn and then flows into the Fenwick water. Grassyard burn flows into the Craufurdland water near Craufurdland bridge.
Hag burn joins the Irvine directly near Galston. Hags burn or gill rises at Crinshill Moss and flows into the Whiteleehill burn. Hall burn joins the Lugton water near Caven Mill. Hareshawmuir water joins the Craufurdland water near Waterside. Harperland burn flows into the Irvine directly near Laigh Milton mill. Hazel syke runs from below Quarry Hill, near the Wham Brae, into the Glen Water, which enters the Irvine at Darvel. Haymouth burn flows into the Burn Anne near Cessnock castle. Heads burn flows into the Huggin Craig burn, which joins the Irvine at Newmilns. Heather syke rises from below the Crook of the Clench at Crook Hill and flows into the West burn, which joins the Pogiven burn and flows into the Glen water. Hillhouse Burn runs down from the farm of that name, collects water from the old Newfarm Loch, and joins the new Mill Burn before joining the River Irvine in Kilmarnock. Horn burn is joined by the Kings Moss burn and then flows into the Irvine near Allanton at Loudoun Hill. Howe burn rises at Howeburn moss, then joins the Drumtee water and this flows into the Fenwick water. Huggin Craig burn joins the Irvine at Newmilns. Isles burn is joined by the Burflatt burn and flows into the Irvine at Newmilns. Jangle burn joins the Glen water and flows into the Irvine at Darvel. Killochy burn flows into the Cessnock water. Kilmarnock water runs into the Irvine at Riccarton. Kingsland Burn rises near Kingsford, flowing into the Clerkland Burn, which joins the Annick water via the Corsehill burn. Kingswell burn rises at Kingswell on the B764 and flows into the Fenwick water, which joins the Irvine via the Kilmarnock water. Kings Moss burn flows into the Horn burn and then joins the Irvine at Allanton near Loudoun Hill. Limper burn joins the Auchmannoch burn. Little Sorn burn joins the Cessnock water at Little Sorn. Loch burn rises at the Flow moss below Larchet Hill and flows into the Whiteleehill burn, on into the Hareshawmuir water and joins the Craufurdland water. Loch burn flows into the Mucks water, which reaches the Glen water and then the Irvine at Darvel. Lochrig (Lochridge) burn flows into the Brackenburn near Kilmaurs. Loudoun water rises from below Corse Hill and flows into the Glen water and into the Irvine at Darvel.
Maidenmire burn flows into Craigendunton Reservoir, its water flowing out as part of the Dunton water. Mareburn flows into the Auchmannoch burn, which enters the Cessnock water. Matthew burn joins the Irvine near Ranoldcoup bridge in Darvel. Mid burn joins the Soutors burn, which then joins the Drumtee water and this flows into the Fenwick water. Montgomery's burn rises below Crook Hill on Crinshill Moss and runs into the Gowkshaw burn, which has a confluence with the Rough Hill burn and runs into the Hareshawmuir water. Mucks water flows into the Glen water. Myres burn flows into the Birk burn, which itself flows into Craigendunton Reservoir, its water flowing out as part of the Dunton water. Neilson's burn flows into the Whitley burn and then on into the Carlin burn. Newlands burn joins the Irvine from Lanfine. New Mill Burn collects water from the Hillhouse Burn before emptying into the River Irvine. Otter burn rises at the Flow moss and flows into the Whiteleehill burn, on into the Hareshawmuir water and joins the Craufurdland water. Pochweer burn joins the Dunton water, which flows from Craigendunton Reservoir and joins the head water of the Craufurdland Water near Waterside. Pockinan burn joins the Hareshawmuir water at Hareshaw Mill near Waterside. Pogiven burn flows into the Glen water, which joins the Irvine at Darvel. Polbaith burn flows into the Irvine at Loudoun Kirk. Pomack burn rises at Whitelee Hill and flows into the Brocklees burn and on into the Glen water. Potesby burn rises below Rough Hill at Potesby Rig and flows into the Loch burn, which joins the Glen water and flows into the Irvine at Darvel. Quaw burn flows into the Bowhill burn, which joins the Hagg Burn and flows into the Irvine at Galston. Rab's burn flows into the Glen water. Rough Hill burn rises below the hill of that name and flows into the Gowkshaw burn and then runs into the Hareshawmuir water. Rough Syke burn flows into the Pogiven burn, which itself flows into the Glen water which joins the Irvine at Darvel. Shaw burn flows into the Carmel Water. Shelgo burn joins the Fenwick water near Fenwick. Simon's burn flows into the Irvine at Riccarton. Sinclair's burn runs from below the Crook of the Lench at Crook Hill and joins the Gawkshaw burn, which flows into the Hareshawmuir water. Slough burn from the Flow Moss and runs into the confluence of the Hareshawmuir water and the Whiteleehill burn.
Small burn flows into the Black Water near Dunlop Hill and then into them Glazert Water. Snab burn rises below Rough Hill, flows into the Glen water and then into the Irvine at Darvel. Soame burn rises below Drumboy Hill, flows into the Kingswell burn and then flows into the Fenwick water. Soutors burn rises from Craigenfaulds moss near Lochgoin farm, then joins the Mid and Bught burns and passes into the Drumtee water and this flows into the Fenwick water. Stagmire burn rises at Pley Moss and flows into the Pogiven burn, which itself flows into the Glen water, which joins the Irvine at Darvel. Stanley burn rises at Cameron's moss; it joins the Black Gill which then flows into the Pockinan burn, which joins the Hareshawmuir water. Stock burn flows into Craigendunton Reservoir, its water flowing out as part of the Dunton water.Stockshaw burn runs into the Cessnock water. Stra burn flows into the Limper, which flows into the Auchmannoch burn. Swinzie burn flows into the Annick water at Robertland outside Stewarton.
Templeton burn joins the Irvine directly at Crookedholm. Thrashy Knowe burn rises below the knowe of that name and then runs into the Polbaith burn. Threap syke rises below Muir Hill and flows into the Glen water and then into the Irvine at Darvel. Todrigs burn begins as the Slough burn and passes through the 'Slough of Despond' near Dankeith House before once feeding an old curling pond at Todrigs and then passing on through the Caprington estate before reaching its confluence with the Irvine near Gatehead. Tongue burn joins the Irvine directly near Priestland outside Darvel. Tour burn rises near Tour House in Kilmaurs and runs passed Lady's well and into the Carmel water. Volga burn runs through Moscow and into the Irvine near Hurlford. Wallace Gill burn flows into the Glen water. Whiteleehill burn flows into the Hareshawmuir water and joins the Craufurdland water. Whitley burn flows into the Carlin burn and then on into the Hareshawmuir water. Woodhall burn flows into the Carmel Water near Knockentiber.
Waterfalls and weirs
A fair number are present, often on the higher reaches of the rivers. Some are named, such as Lizzie's Linn at Caven Mill, Montgreenan, on the Lugton Water. The Cessnock Water has a number on its course through the woods at the Carnell estate near Fiveways outside Kilmarnock. A series of low waterfalls occur at Cunnighamhead on the Annick Water, these being, like many others, dykes that are more resistant to erosion than the surrounding rocks. Other notable waterfalls are on the Polbaith burn, Fenwick Water (near Rigghill), Glen water (Darvel) and Burn Anne.
Weirs were often built to divert and provide a head of water for the many mills. A more unusual use of a weir was that at Lainshaw House where two weirs, together with a realignment of the Annick Water, provided a large area of water for waterfowl, shooting and ornament.
It is recorded that a deep pool in the River Irvine at Irvine was called the 'Witches Plumb' and that it may have been used to duck supposed witches to see if the Devil would save them. This pool lay near the site of the old Gallows Knowe where the old Irvine Royal Academy building was constructed.
Crossing the river
It is recorded that stilts were sometimes used to cross the river, for example Thomas Raeburn of Holmhead near Hurlford worked as a gardener at Shawhill House and regularly crossed the River Irvine using stilts. At nearby Barleith, Mayday festivities sometimes included stilt races across and back, resulting in much amusement as many competitors fell into the water.
Ferries and carrying
Rivers form physical boundaries and are only crossed with either trouble or expense. At the port of Irvine itself ferry boats took passengers across to Ardeer, further upstream fords and /or stepping stones were present in many places. These were often treacherous and could turn from tranquil to lethal in a matter of minutes, often with no warning as the rainfall could well have fallen far upstream or at the moors that form the watershed.
At one time people were carried across rivers, usually at fords, but not necessarily. A fee would normally be charged or it might be part of the 'job description' of a servant. One Ayrshire story tells of a rich farmer who employed a servant girl to carry him across the river on his way to church each Sunday. As time went by he became very fond of the servant and eventually they married. She willingly carried him across on the way to their wedding, but she refused on the way back and never carried him again.
The Kilmarnock Standard newspaper recorded in 2011 that a leisure boat service had been set up in the 1930s, running from a short concrete jetty, however it was not a success and did not continue for long.
Many sets of stepping stones are recorded on OS maps, such as at Shawhill Farm near Hurlford, crossing over to Templetonburn and Skerrinngton Mains nearby. Stepping stones are marked on the 1897 OS map as being located just downstream from the present Chapeltoun bridge over the Annick Water and further upstream near Townhead of Lambroughton. The then owner of Chapeltoun Mains had the Chapeltoun stepping stone sremoved in the 20th century. Stepping stones are shown near Waterside Farm on the Irvine at Galston. Stepping stones and a ford existed at Kaimshill House near Crookedholme in the 1870s; called 'Struthers Steps' they crossed the river Irvine below Struther's Farm, home to James Paterson. The Kilmarnock Glenfield Ramblers in 1931 remark on the stepping stones at Struthers having long since disappeared and that stepping stones at Haining on the Cessnock Water still survived.
|The name Annick, previously Annock, Annoch (1791) or Annack Water, possibly derives from the Gaelic abhuin, meaning water and oc or aig meaning little or small.|
An interesting possible origin of the name of the Puddle ford at Irvine is 'holy steps' ('pas de Dieu'), referring to the stepping stones the Carmelite Priory monks made their way across on their way to Church. Some of the stepping stones may have come from the stone circle, later removed, of which the Grannie stone is the last survivor. Use of the Puddleford by horses was prohibited in 1836 to safeguard access to the Puddly Well, one of the public wells all of which were repaired at about that time.
The toll road authorities found fords something of a nuisance as passage was free unlike the bridge where a toll was levied. To prevent this they often obtained authority to deepen the fords in the river to force the use of bridges on the toll roads; very few fords therefore remain in Ayrshire. Even the Dean Ford has ceased to exist on the Kilmarnock Water after resolution of difficulties to do with the legal transfer of the property to the council by Lord Howard de Walden and the legal definition of the boundaries of the lands gifted. Further up the Fenwick Water the Bringan Ford still survives. Many of the fords eventually developed wooden footbridges alongside, such as at the Bringan Ford and as at Knockentiber in 1860 on the old Kilmarnock Road ford. The fine 'suspension bridge' footbridge at the Dean Ford was famous for collapsing with the weight of sightseers on its opening day. It was replaced with a stronger structure but has been removed due to the ford being bridged over circa 2016.
A 'Romford', 'Rameford', 'Room' or 'Rome Ford' was situated where the modern road bridge crosses the Irvine at Gatehead. In Scots 'Rommle' is to rumble or stir violently, a more likely explanation than some memory of the Roman occupation of Scotland. Another suggestion is that 'Room' or 'Rome' meant a small farm. Adamson states that this bridge was built in around 1870, replacing an older bridge.
The Hurling Ford existed at Shewalton where it crossed the river to the Warrix Holm (see video).
Pedestrian and road bridges
Bridges were built where they could be afforded or where they were most needed. Many of the older bridges were built by local lairds, such as Chapeltoun Bridge over the Annick Water, which was built in the 1850s to replace a ford downstream at Bankend, opposite West Lambroughton.
Archibald Adamson on his Rambles Round Kilmarnock in 1875 records that the Irvine is the Parish boundary between Kilmarnock and Riccarton and that the ancient bridge running into Riccarton bears the date 1726. Aiton states that the stones used to build this bridge were conveyed in the first wheeled carts used in Ayrshire, sledges having been employed on the poor quality roads that existed prior to this time. The new brisge was built here about 1845.
The pedestrian 'Auld Brig' across the Carmel water in Kilmaurs was built to replace stepping stones in 1824. It has been the scene of two deaths.
Both Beattie and the Kilmarnock Glenfield Ramblers refer to Murdock's or Murdoch's iron bridge over the Carmel Water near Kilmaurs-Glencairn church as being the oldest iron bridge in Scotland. It was erected following a 1d subscription from each of the house-houlders of Ayrshire. The council demolished it in around the year 2000 and replaced it with a wooden bridge.
The bridge over the Craufurdland Water at Craufurdland was built by Mr. Craufurdland, using the balusters from the original part of the battlements of Cessnock Castle, which had originally been given to Captain Whyte of The Cottage.
A bridge at Haining in 1931 went over the Cessnock. It was made from two wires stretched, one above the other, across the water. The one-man-at-a-time bridge was traversed by the passager holding the top wire and placing their feet on the lower wire.
Railways appeared very early in this part of Scotland and one of the first built was the stone viaduct over the Irvine at Laigh Milton, part of the Kilmarnock and Troon Railway. It has four arches, and although not used since 1846, it was restored in 1996. The railway carried steam locomotives 9 years before the Stockton and Darlington Railway and is believed to be the first passenger steam railway in the world. The viaduct itself, built in 1811, is the oldest surviving railway viaduct in Scotland. and one of the oldest in the world:
Many of the railways that crossed the river were mineral lines, which often had an intensive but short life, such as the 1923 OS mineral lines that ran to collieries near Earlston, Nether Craig and Cockhill farm (Fairlie (Pit No.3)). The 1860 OS names the 'Fairlie Branch' and indicates its operation by the Glasgow and South Western Railway company. The bridges built for these lines are still clearly visible.
Taming the river
Flood prevention schemes have canalised the Kilmarnock (previously the Marnock) Water where it runs down through Kilmarnock towards the Irvine, with significantly raised banks and automatically closing gates. The Irvine has likewise been tamed with a large flood prevention scheme at east Holmes Wetlands near Galston. Here the river is directed into its old floodplains when the water rises above a certain height, thereby protecting Kilamarnock. A scheme on the River Cessnock is underway (2007). Many sections of the other rivers have been canalised and / or have bunds on either bank to prevent the watercourses flooding into their flood plains.
The river system and its wildlife
Many of the water meadows are rich in pignut (Conopodium majus), a relative of parsley, which formed a breaktime snack for children in former times. The plant is dug up to harvest a small potato-like structure that, eaten raw, has a slightly nutty taste. It is available commercially for salads, etc. Hemlock water dropwort grows well in the wetter areas and is best left alone as the name hemlock suggests. The large leaves of the butterbur (Petasites hybridus) are found in several areas; its name harkens back to the days before clingfilm or cheap paper when the leaves were used to wrap butter destined for the market. Water ragwort (or Saracen's ragwort) (a species of Senecio) is an introduced plant that grows along the Garnock in tall stands. Although it is common on the Garnock and at present quite rare elsewhere. Himalayan balsam or policemen's helmets is another introduction, but a common one. Giant hogweed is beginning to make its presence felt. It is another plant that should never be handled, as the sap can cause severe blistering and scarring of the skin.
The Stewarton Flower or pink purslane (Claytonia sibirica) is common in wetter areas. It has white or pink flowers at this site, but closer to Stewarton it is almost always white. It seems that it was first introduced as a white variety in the Stewarton area in Victorian times and the common pink variety, introduced later, spread to other areas. Dalgarven, it seems, is on the edge of the white flower zone of dominance.
Coppicing of the riverside alder trees is still carried out, often unintentionally by the anglers. Alders grow well in wet soils and are specially adapted for the low nutrient conditions through having large root nodules containing nitrogen-fixing bacteria that enrich the soil in the same way as clover plants and other legumes.
The trees in the vicinity of the rivers were not planted by farmers for 'visual effect', they were crops and the wood was used for building and fencing; The millers needed beech or hornbeam wood for mill machinery, in particular the cogs on the drive wheels from the waterwheel.
It is not generally appreciated how much the Ayrshire landscape has changed its character over the last few hundred years, for even in the 1760–70 Statistical Account it is stated that "there was no such thing to be seen as trees or hedges in the parish; all was naked and open."
Birds, fish and other animals
The river and its banks, support, amongst others, Kingfishers, tawny and barn owls, herons, moorhean, coot, mallard, ravens, rooks, treecreepers, buzzards, peewits or lapwings, roe deer, mink, moles, shrews, grey squirrels, hares, hedgehogs, foxes, badgers, pipistrelle bats and otters. Migrating Canada and Graylag Geese frequent the nearby fields on their way up from the Solway Firth / Caerlaverock area or coming down from Spitzbergen in the winter.
|The name 'Glazert' may come from the Celtic, glas in Gaelic meaning grey or green and dur meaning water.|
The river's water quality is generally quite good nowadays, proven by the presence of freshwater limpets and shrimps, together with leeches, caddis fly larvae and water snail species. Pont in 1604 – 08 writes that salmon are plentiful in the River Irvine. The river system contains, amongst others, brown trout, sea trout, salmon, eels, minnows, lampreys, and sticklebacks. The brown colour of the Irvine at places like Darvel and Newmilns is not a result of pollution, but simply organic material washed out of the peat banks at the watershed. Freshwater mussels, a species persecuted for its pearls, are found in places on the Glazert and the Garnock.
Pont in 1604–08 records that so thickly was the district about Stewarton and along the banks of the Irvine populated for a space of three or four miles "that well travelled men in divers parts of Europe (affirm) that they have seen walled cities not so well or near planted with houses so near each other as they are here, wherethrough it is so populous that, at the ringing of a bell in the night for a few hours, there have seen convene 3000 able men, well-horsed and armed."
Shewalton Sand Pits is a Scottish Wildlife Trust nature reserve on the River Irvine near Irvine.
Immense labour has been expended over the years in retaining building walls on either side of many of the rivers and burns. At Chapeltoun on the Annick Water even the Chapel Burn bed is 'cobbled'. This drystone walling was important in reducing the erosion of the river banks.
The Brackenburn near Kilmaurs has been misnamed as the Garrier by the Ordnance Survey since the 1860s. When burns or rivers join it is usually the largest that decides the name of the river downstream, unless the name changes completely, such as the Kilmarnock Water forming from the Fenwick and Craufurdland Waters. Occasionally a water course is reduced in volume due to changes upstream, a case in point being the Garrier, which used to drain Buiston Loch near Kilmaurs. This was drained as part of agricultural improvements and now the Garrier is only seasonal, even though it keeps the name Garrier, even when joined by the Brackenburn and the Lochrig burns that flow all year.
It was not easy being a miller, for instance some people held the belief that it was wrong to use water artificially; that to turn water from its course was to act against God's plan.
Ancient mills, it was believed, had been piously placed by their forefathers where they could be worked according to God's order, without artificially embanking the water or turning it from its natural course, which would be sinful.
New field drainage work on farms in the 18th and 19th centuries had dramatic effects on water courses, most often recorded through complaints by millers that they could no longer get enough water to turn their mills waterwheels.
The weir at Dalgarven on the River Garnock is made of boulders which are carefully placed and locked together to create a natural millpond to supply a good head of water to the wheel through the lade. The weir is built on a natural dyke across the Garnock at this point, its existence being carefully exploited by the monks of Kilwinning Abbey who chose the site for Dalgarven Mill.
In February 2009 the Lochrig or Lochridge Burn was severely polluted with diesel oil spilled from a train derailed at the railway bridge near Peacockbank farm, Stewarton. Mitigation measures were put in place, however pollution eventually reached the River Irvine.
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