Dunbartonshire in the context of "Loch Lomond"

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👉 Dunbartonshire in the context of Loch Lomond

Loch Lomond (/ˈlɒx ˈlmənd/; Scottish Gaelic: Loch Laomainn) is a freshwater Scottish loch which crosses the Highland Boundary Fault (HBF), often considered the boundary between the lowlands of Central Scotland and the Highlands. Traditionally forming part of the boundary between the counties of Stirlingshire and Dunbartonshire, Loch Lomond is split between the council areas of Stirling, Argyll and Bute and West Dunbartonshire. Its southern shores are about 23 kilometres (14 mi) northwest of the centre of Glasgow, Scotland's largest city. The Loch forms part of the Loch Lomond and The Trossachs National Park which was established in 2002. From a limnological perspective, Loch Lomond is classified as a dimictic lake, meaning it typically undergoes two mixing periods each year. This occurs in the spring and autumn when the water column becomes uniformly mixed due to temperature-driven density changes

Loch Lomond is 36.4 kilometres (22.6 mi) long and between one and eight kilometres (12–5 miles) wide, with a surface area of 71 km (27.5 sq mi). It is the largest lake in Great Britain by surface area; in the United Kingdom, it is surpassed only by Lough Neagh and Lough Erne in Northern Ireland. In the British Isles as a whole there are several larger loughs in the Republic of Ireland. The loch has a maximum depth of about 190 metres (620 ft) in the deeper northern portion, although the southern part of the loch rarely exceeds 30 metres (98 ft) in depth. The total volume of Loch Lomond is 2.6 km (0.62 cu mi), making it the second largest lake in Great Britain, after Loch Ness, by water volume.Due to its considerable depth and latitudinal location, Loch Lomond exhibits thermal stratification during the summer months, with a distinct epilimnion, metalimnion, and hypolimnion forming in deeper areas. These stratification patterns have important implications for nutrient cycling and aquatic ecology within the loch. During periods of stratification, a decrease in hypolimnetic oxygen can occur in the deeper northern basin, which can affect the species distribution patterns.

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Dunbartonshire in the context of Helensburgh

Helensburgh (/ˈhɛlənzbərə/ HEL-ənz-bər-ə; Scottish Gaelic: Baile Eilidh) is a town on the north side of the Firth of Clyde in Scotland, situated at the mouth of the Gareloch. Historically in Dunbartonshire, it became part of Argyll and Bute following local government reorganisation in 1996.

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Dunbartonshire in the context of North Lanarkshire

North Lanarkshire (Scots: North Lanrikshire; Scottish Gaelic: Siorrachd Lannraig a Tuath) is one of the 32 council areas of Scotland. It borders the north-east of the Glasgow City council area and contains many of Glasgow's suburbs, commuter towns, and villages. It also borders East Dunbartonshire, Falkirk, Stirling, South Lanarkshire, and West Lothian. The council area covers parts of the historic counties of Dunbartonshire, Lanarkshire, and Stirlingshire. The council is based in Motherwell.

The area was formed in 1996, covering the districts of Cumbernauld and Kilsyth, Motherwell, and Monklands, plus the Chryston and Auchinloch areas from Strathkelvin district, all of which had been in the Strathclyde region between 1975 and 1996. As a new single-tier authority, North Lanarkshire became responsible for all functions previously performed by both the regional council and the district councils, which were abolished.

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Dunbartonshire in the context of Clydebank

Clydebank (Scottish Gaelic: Bruach Chluaidh) is a town in West Dunbartonshire, Scotland. Situated on the north bank of the River Clyde, it borders the village of Old Kilpatrick (with Bowling and Milton beyond) to the west, and the Yoker and Drumchapel areas of the adjacent City of Glasgow immediately to the east. Depending on the definition of the town's boundaries, the suburban areas of Duntocher, Faifley and Hardgate either surround Clydebank to the north, or are its northern outskirts, with the Kilpatrick Hills beyond.

Historically part of Dunbartonshire and founded as a police burgh on 18 November 1886, Clydebank is part of the registration County of Dumbarton, the Dunbartonshire Crown Lieutenancy area, and the wider urban area of Greater Glasgow.

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Dunbartonshire in the context of Dumbarton

Dumbarton (/dʌmˈbɑːrtən/; Scots: Dumbairton, Dumbartoun or Dumbertan; Scottish Gaelic: Dùn Breatann [t̪um ˈpɾʲɛht̪ən̪ˠ] or Dùn Breatainn [t̪um ˈpɾʲɛht̪ɪɲ], meaning 'fort of the Britons') is a town in West Dunbartonshire, Scotland, on the north bank of the River Clyde where the River Leven flows into the Clyde estuary. In 2006, it had an estimated population of 19,990.

Dumbarton was the capital of the ancient Kingdom of Strathclyde, and later the county town of Dunbartonshire.Dumbarton Castle, on top of Dumbarton Rock, dominates the area. Dumbarton was a royal burgh between 1222 and 1975.

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Dunbartonshire in the context of Perthshire

Perthshire or the County of Perth, is a historic county and registration county in central Scotland.

Geographically Perthshire extends from Strathmore in the east, to the Pass of Drumochter in the north, Rannoch Moor and Ben Lui in the west, and Aberfoyle in the south; it borders the counties of Inverness-shire and Aberdeenshire to the north, Angus to the east, Fife, Kinross-shire, Clackmannanshire, Stirlingshire and Dunbartonshire to the south and Argyllshire to the west.

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Dunbartonshire in the context of Stirlingshire

Stirlingshire or the County of Stirling (Scottish Gaelic: Siorrachd Sruighlea [ˈʃirˠəxk ˈs̪t̪ɾuʝlə]) is a historic county and registration county of Scotland. Its county town is Stirling.

It borders Perthshire to the north, Clackmannanshire to the east, West Lothian to the south-east, Lanarkshire to the south, and Dunbartonshire to the south and south-west (this latter boundary is split in two owing to Dunbartonshire's Cumbernauld exclave).

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