Irvine is a town on the coast of the Firth of Clyde in North Ayrshire, Scotland. The 2011 Census recorded the town's population at 33,698 inhabitants, making it the largest settlement in North Ayrshire, and 22nd largest settlement in Scotland.
Stanecastle was a medieval barony and estate in North Ayrshire, Scotland, first mentioned in 1363 and now part of the Irvine New Town project. Its nearest neighbours are Bourtreehill and Girdle Toll.
The River Irvine 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 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 Capitulation of Irvine was an early armed conflict of the Wars of Scottish Independence which took place on 7 June 1297. Due to dissension among the Scottish leadership, it resulted in a stand-off.
The Castle of Clonbeith is in the old feudal Baillerie of Cunninghame, near Auchentiber, on a sideroad off the B778, in what is now North Ayrshire, Scotland.
The Drukken, Drucken Steps or Drunken Steps were stepping stones across the Red Burn in Irvine, North Ayrshire, Scotland and are associated with Scotland's national poet, Robert Burns. Drukken is used on the commemorative cairn plaque, but Druken or Drucken may also be used.
Seagate Castle is a castle and fortified town house in North Ayrshire, in the town of Irvine, close to the River Irvine, Scotland. The castle was formerly a stronghold, a town house, and later a dower house of the Montgomery Clan. The castle overlooks the oldest street in Irvine, which was once the main route between the town and the old harbour at Seagatefoot, which by 1606, was useless and abandoned due to silting. The remains of the castle are protected as a scheduled ancient monument.
Kilbirnie Loch is a freshwater Loch situated in the floodplain between Kilbirnie, Glengarnock and Beith, North Ayrshire, Scotland. It runs south-west to north-east for almost 2 km (1.2 mi), is about 0.5 km (0.31 mi) wide for the most part and has an area of roughly 3 km2. It has a general depth of around 5.2 metres to a maximum of around 11 metres. The loch is fed mainly by the Maich Water, which rises in the Kilbirnie Hills near Misty Law, and is drained by the Dubbs Water that runs past the Barr Loch into Castle Semple Loch, followed by the Black Cart, the White Cart at Renfrew and finally the River Clyde. The boundary between East Renfrewshire and North Ayrshire, in the vicinity of the loch, runs down the course of the Maich Water along the northern loch shore to then run up beside the Dubbs Water.
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.
Lochlea or Lochlie was situated in a low-lying area between the farms and dwellings of Lochlea and Lochside in the Parish of Tarbolton, South Ayrshire, Scotland. The loch was natural, sitting in a hollow created by glaciation. The loch waters ultimately drained via Fail Loch, the Mill Burn, and the Water of Fail. It is well-documented due to the presence of a crannog that was excavated and documented circa 1878, and its association with the poet Robert Burns, who lived here for several years whilst his father was the tenant. Lochlea lies 2+1⁄2 miles northeast of Tarbolton, and just over three miles northwest of Mauchline.
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.
Helenton Loch was situated in a low lying area between the farms and dwellings of Helentongate, Mains, and Burnbank in the Parish of Symington, South Ayrshire, Scotland. The loch was natural, sitting in a hollow, a kettle hole, created by glaciation. The loch waters ultimately drained via the Pow Burn. Helenton Hill is a prominent landmark to the west of the old loch site. The nearby lands of Rosemount were in 1549 known as 'Goldring' and were the property of the Schaws of Sornbeg.
The Loch of Trabboch or Dalrympleston Loch (NS440211) was situated in a low-lying area below the old Castle of Trabboch, once held by the Boyd family in the Parish of Stair, East Ayrshire, Scotland.
Whitehill Loch, previously known as Hillhouse Loch was a freshwater loch in the East Ayrshire Council Area, now drained, near Galston, in the Parish of Riccarton, lying in a glacial Kettle Hole.
Bruntwood Loch was a freshwater loch, now drained, lying in a glacial kettle hole in Galston, East Ayrshire, Scotland.
The harbours serving Irvine at Seagatefoot and Fullarton in North Ayrshire have had a long and complex history. Irvine's harbour was one of the most important ports in Scotland in the 16th century. Across from the main harbour at Fullarton on the River Irvine there was also terminal for the ICI-Nobel Explosives plant on the River Garnock. Much of the harbour went into decline in the 19th century when Glasgow, Greenock and Port Glasgow achieved higher prominence as sea ports. There was still some commercial sea traffic linked to local needs, though the harbour went into further terminal decline in the 20th century. The weir on the River Irvine forms the formal upper limit of the harbour.
The Tanzie Well, also known as Saint Anne's Well, the Washing House Well or the Spoot is located beside the River Irvine in the Golf-fields or Golffields at the end of the footbridge across the River Irvine in Irvine, North Ayrshire, Scotland. It has been suggested that 'Tanzie' may be a corruption of St Inan's Well. The old Irvine Pouther House of 1801 is located nearby.
The lands of Broomlands or Broumlands formed a small country estate about a mile to the east of Irvine, North Ayrshire, Scotland situated on the east bank of the Annick Water in the Parishes of Dreghorn and Irvine.
Newton Loch was situated in a low-lying area near Newton-on-Ayr, South Ayrshire, just south of the old South and West Sanquhar Farms. It is now (2016) only visible as remnant heath land and surface darkening in pastureland, situated mainly in the Parish of Ayr and partly in St Quivox, South Ayrshire, Scotland.
