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.
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.
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.
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.
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 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.
Lochspouts Loch or Lochspouts was situated in a hollow, surrounded by hilly ground on three sides and bounded by a narrow trap dyke to the north. The land was once held by the Ferguson family of Kilkerran and lies in the Parish of Kirkoswald, South Ayrshire, Scotland. The loch became a reservoir in the 19th century.
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.
Loch Fergus is a freshwater post-glacial "Kettle Hole" sometimes recorded as Fergus Loch. It is quite visible and is situated in a low-lying area close to the B742 road between the farms and dwellings of Trees, Lochfergus and Bowmanston in the Parish of Ayr, South Ayrshire, Scotland. The loch lies to the north of Martnaham Loch, four miles east-southeast of Ayr. It drains to the southwest into the Snipe Loch.
Martnaham Loch is a freshwater loch lying across the border between East and South Ayrshire Council Areas, two kilometres from Coylton, in the parishes of Coylton and Dalrymple, three miles from Ayr. The loch lies along an axis from northeast to southwest. The remains of a castle lie on a possibly artificial islet within the loch. The Campbells of Loudoun once held the lands, followed by the Kennedys of Cassillis.
Lindston Loch was a small freshwater loch situated within a glacial 'kettle hole.' The loch lies in the South Ayrshire Council Area, Parish of Dalrymple, Scotland.
Kerse Loch, also recorded as Carse Loch (1841) is a small freshwater loch in the East Ayrshire Council Area, lying in a glacial Kettle Hole, Parish of Dalrymple, Scotland.
Plaid Loch was a freshwater loch in East Ayrshire, now a remnant due to drainage, near Sinclairston and 2 miles (3 km) south-east of Drongan, 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.
