Knockewart or Loch Jargon | |
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Location | Knockewart, North Ayrshire, Scotland |
Coordinates | Coordinates: 55°41′25.5″N4°48′5.4″W / 55.690417°N 4.801500°W |
Lake type | Drained freshwater loch |
Primary inflows | Rainfall and runoff |
Primary outflows | Rowanside Burn |
Basin countries | Scotland |
Max. length | 500 m (1,600 ft) |
Max. width | 140 m (460 ft) |
Surface elevation | 188 m (617 ft) |
Islands | None |
Settlements | Ardrossan |
Knockewart Loch or Loch Jargon was situated in a hollow lying area beneath Knockewart Hill in the Parish of Ardrossan, North Ayrshire, Scotland. The old loch has become largely drained and overgrown since the late 19th century. [1]
The loch is recorded as Loch Jargon on the earlier maps after the prominent fort situated nearby. [2] Once Knockewart Farm was established the maps use this name for it.
The Ordnance Survey Map of 1897 shows the loch as having been drained through a breaching of the natural dam bank and a significant deepening of the outflow for a distance of a hundred metres or so.
In 1858 Fullarton [3] records that it was once a haunt of pike, however, the accumulation of vegetable matter in the bed of their domain made it unlikely that pike could survive and that it was now an excellent site for the breeding of wild ducks. By 1876 Dobie records that the loch has nearly dried up and is little more than a swamp. [4] In 1887 the Natural History Society of Glasgow had an excursion to West Kilbride and observed in their transactions that 'the party reached Knockewart Loch, a small sheet of water which is now almost wholly covered with a growth of surface vegetation. [5]
The loch's drainage may have begun in the 18th century when Alexander Montgomerie, 10th Earl of Eglinton, was pursuing a number of agricultural improvements on his extensive estates and other landowners followed his example. Intensive drainage work may have taken place as part of the improvements undertaken to provide employment for Irish estate workers during the Irish potato famines of the mid-19th century. Many drainage schemes also date to the end of World War I when many soldiers returned en masse to civilian life. [6]
Busbie Muir Reservoir was constructed in the glen beneath the loch, opening in 1903. The loch's outfall water still drain into it before continuing as the Rowanside Burn, joining the Stanley Burn, flowing over the aqueduct at the Parkhouse Cutting and running into the sea at Ardrossan South Beach. The reservoir is now used by the Ardrossan Eglinton Angling Club. [7]
A cairn and possible vitrified fort are located at North Hill in the Knockewart Hill (NS 2387 4806). An enclosure (NS 2356 4812) is located near rising ground that has the appearance of having once been cleared of stone and cultivated. No field plots or clearance heaps are identifiable. A well-preserved fort is present at Knock Jargon, upon a rock outcrop with steep sides. Surrounding the summit are the remains of two ramparts and ditches constructed upon the slopes, best preserved on the south side where each is broken by an entrance. [2] Campbell records that Knockjargon is built upon a Neolithic hilltop burial cairn. Cup-and-ring marked stones are to be found at nearby Blackshaw Hill. [8] Smith records the name 'Knock-Georgan'. [9] A fort with a double ditch cut from rock is located near Coalhill. [10]
Knook-Ewart (sic) belonged after the Battle of Largs, to the Crawfurds of Auchnames ; subsequently it came into the possession of the Mures of Caldwell. In 1713 John Simson of Kirkton-hall, parish of Kilbride, purchased the property; he was the father of Dr Robert Simson, professor of mathematics in the University of Glasgow. The professor never married, and the estate was purchased from his representative, in 1787, by James Montgomerie, Esq., a magistrates of Irvine, a descendant of Adam Montgomerie of Broadstane near Beith. On his death, it was inherited by his eldest daughter, Mary, who married Captain John Brooks, of the 20th regiment, who became proprietor in right of his wife. [11]
Blaeu's map of 1654, dating from Timothy Pont's survey of circa 1604, clearly shows the loch and erroneously indicates that its outflow entered the sea near Montfode. A dwelling named 'Iargan' is recorded and a 'Knokawart'. [12] Herman Moll's map of 1745 marks, but does not name the loch. [13] Roy's map of 1747 shows and names 'Loch Jargen', situated without an inflow burn. [14] Armstrong's map of 1775 does not show the loch, but Knock Jargon fort is clearly marked. William Aiton's map of 1811 shows a loch at Jargon, however, the outflow runs in entirely the wrong direction. [15] Thomson's map of 1832 marks and records Loch Jargon. [16]
The 1854-9 Ordnance Survey map show the loch as open water with small areas of woodland above and below. [17] In 2011 the drainage here remains inadequate and the area is dominated by marsh plants. [18]
Knockjargon is a distinctive and ancient name as indicated by evidence from old maps. The word 'Jargoun' in Scots, dating from as early as 1340–70, refers to the twittering or chattering of birds. [19] Knock is from the Gaelic, An Cnoc, refers to a small hill, and as such often fortified.
The old loch is a designated wildlife site, surveyed by the Scottish Wildlife Trust in 1982, with the following observations - "The loch, which is now completely vegetated being covered in a sphagnum carpet, is extremely interesting. It supports a number of plant communities and a diversity of plant species including cotton grass, bottle sedge and various mosses, especially Polytrichum commune. The margins are dominated by sharp-flowered rush and the wetland area grades out to dry land where soft rush and grasses dominate." [20]
The site is well suited to birds of prey, snipe and curlew. Willow warbler, tawny owl, chaffinch have been recorded and roe deer are present, together with common lizard and frog. Botanically the site is dominated by sphagnum mosses and heathers with the carnivorous sundew commonly encountered. The roe deer have prevented regeneration of the areas of woodland. [20]
The fishing rights on the Rowanside and Stanley Burns were held by the Earls of Eglinton and at one time reservoirs were also present at Whitlees, Parkhouse and Millglen. [21]
Coalhill is named from the coal that was once mined on its eastern edge. [10]
Kilwinning Abbey is a ruined abbey located in the centre of the town of Kilwinning, North Ayrshire.
Eglinton Castle was a large Gothic castellated mansion in Kilwinning, North Ayrshire, Scotland.
Little Cumbrae Castle sits on Allimturrail or Castle Island, a small tidal island, situated off the east coast of Little Cumbrae, in the Firth of Clyde. It is designated as a scheduled monument.
Skelmorlie Castle stands on the eastern shore of the Firth of Clyde, Scotland, at the north-western corner of the county of Ayrshire. The structure dates from 1502, and was formerly the seat and stronghold of the Montgomery Clan. The modern village of Skelmorlie lies to the north of the castle.
Polnoon Castle was a 14th-century fortification located on a motte beside the Polnoon Water in Millhall, in the Parish of Eaglesham, East Renfrewshire, Scotland.
Loch Brand or Loch of Boghall was a loch situated in a depression between the Grange Estate, Crummock, Hill of Beith Castle site and Boghall in the Parish of Beith, North Ayrshire, Scotland. The loch was fed by the Grange Burn and surface runoff, such as from the old rig and furrows indicated by Roy's Maps of the mid 17th century. The loch was drained by the Boghall Burn that runs passed the 'Court Hill' and into Powgree Burn at Gateside.
Lambroughton Loch or Wheatrig Loch was situated in a low-lying area between the farms and dwellings of Hillhead, Lambroughton, Wheatrig, Titwood and Lochridge mainly in the Parish of Dreghorn, North Ayrshire. The loch was mainly fed by the Lochridge Burn, the Garrier Burn and surface runoff, such as from the old rig and furrows indicated by Roy's maps of the mid-18th century. The loch outflow was via the Lochridge Burn that runs into the Garrier Burn, passes the site of the old Lochend habitation and into the Bracken Burn near Little Alton. The rivulet or watercourse is known as the Garrier Burn beyond this point.
Buiston Loch, also known as Buston, Biston, and Mid Buiston was situated in the mid-Ayrshire clayland at an altitude of 90 m OD. The loch was natural, sitting in a hollow created by glaciation. The loch waters drained via the Garrier Burn that joins the Bracken and Lochridge Burns before joining the River Irvine.
Halket Loch' also known as Halkhead or Halketh, was situated in the mid-Ayrshire clayland near Lugton. It is visible as a surface depression in pastureland, sometimes partially flooded, situated in a low-lying area close to farms and dwellings of East, North and Middle Halket and Craighead in the Parish of Dunlop, East Ayrshire, Scotland. The loch was natural, sitting in a hollow created by glaciation. The loch waters drained via the Glazert Water that joins the Annick Water.
Littlestane Loch, was situated in the mid-Ayrshire clayland near Stanecastle, Irvine, North Ayrshire, Scotland. It is nowadays (2011) only visible as an area of permanent water in the Scottish Wildlife Trust Sourlie Nature Reserve. The loch was natural, sitting in a hollow created by glaciation. The loch waters outflow was via the Red Burn that flows into the River Garnock. The site of Littlestane Loch site is partly built over and much of the site is now public open space lying within the Parish of Girdle Toll.
Fail Loch or Faile Loch was situated in a low-lying area near the old monastery of Fail in the Parish of Tarbolton, South Ayrshire, Scotland. The old Lochlea Loch lies nearby and its waters still feed into Fail Loch via the Mill Burn.
Hessilhead Loch or Hazelhead Loch was situated in a low-lying area near the old Castle of Hessilhead in the Parish of Beith, North Ayrshire, Scotland. The old loch, used in the defence of the castle, was probably infilled when the castle ruins were landscaped in the 19th century.
The Blae Loch is a small freshwater loch situated in a hollow in a low-lying area beneath Blaelochhead Hill in the Parish of Beith, North Ayrshire, Scotland.
The Galrigs Loch was a substantial freshwater loch situated in low lying area between Newfield and Dundonald in South Ayrshire, Scotland. It was drained in the early 18th century.
Clevens Loch was a substantial freshwater loch situated in a low-lying area below Clevance Farm and Langholm Farm in Dundonald parish, South Ayrshire, Scotland.
The Loch of Stair was a typical Ayrshire post-glacial 'Kettle Hole', situated in a low-lying area below the farm of Loch Hill, in the Parish of Stair, East Ayrshire, Scotland. This freshwater loch was drained in the 19th century, leaving a wetland area which still periodically floods.
The Rt Hon. Alexander Montgomerie, 10th Earl of Eglinton, was a wealthy Scottish peer and landowner. Lord Eglinton was mortally wounded on the beach near his stables at Parkhouse on his own estate of Ardrossan in Ayrshire by an excise officer named Mungo Campbell on 24 October 1769, following a dispute about poaching and the latter's right to bear arms on the Earl's grounds.
The Reed Loch was also known as Loch Green. As a curling pond it was probably known as the Fullarton House Pond, located as it was on the edge of the Fullarton House and Crosbie Castle estate curtilage, It was originally a shallow and overgrown freshwater loch, hence the name Reed Loch and its marshy appearance on Johnson's 1828 map. It was cleaned out and used as a curling pond in the latter part of the 19th century before falling out of use and being drained in the late 20th century.
The Lands of Doura, Dawra, Dawray, DowreyDowray, Dourey or Douray formed a small estate, at one time part of the Barony of Corsehill and Doura, situated near the Eglinton Estate in the Parish of Kilwinning, North Ayrshire, Scotland.
The Murder of Hugh Montgomerie, 4th Earl of Eglinton at the Annick Ford in Stewarton, East Ayrshire, Scotland, took place in 1586 as a consequence of a long running feud between the Montgomeries, Earls of Eglinton and the Cunninghames, Earls of Glencairn, families who were competing for power and influence locally and nationally. The significant repercussions of this act were felt throughout the county of Ayrshire and beyond. The spelling 'Montgomerie' is used throughout for both the family and Montgomery for the clan and clan and district names 'Cunninghame' in the same fashion.
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