Loch Lomond is a freshwater Scottish loch which crosses the Highland Boundary Fault, 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.
The Stirling council area is one of the 32 council areas of Scotland, and has a population of about 94,330. It was created under the Local Government etc (Scotland) Act 1994 with the boundaries of the Stirling district of the former Central local government region, and it covers most of Stirlingshire and the south-western portion of Perthshire. Both counties were abolished for local government purposes under the Local Government (Scotland) Act 1973.
Luss is a village in Argyll and Bute, Scotland, on the west bank of Loch Lomond. The village is within the Loch Lomond and The Trossachs National Park.
Loch Long is a body of water in Argyll and Bute, Scotland. The Sea Loch extends from the Firth of Clyde at its southwestern end. It measures approximately 20 miles (32 km) in length, with a width of between 1 and 2 miles. The loch also has an arm, Loch Goil, on its western side.
Loch Lomond and The Trossachs National Park is a national park in Scotland centred on Loch Lomond and the hills and glens of the Trossachs, along with several other ranges of hills. It was the first of the two national parks established by the Scottish Parliament in 2002, the second being the Cairngorms National Park. The park extends to cover much of the western part of the southern highlands, lying to the north of the Glasgow conurbation, and contains many mountains and lochs. It is the fourth-largest national park in the British Isles, with a total area of 1,865 km2 (720 sq mi) and a boundary of some 350 km (220 mi) in length. It features 21 Munros and 20 Corbetts.
Ben Lomond, 974 metres (3,196 ft), is a mountain in the Scottish Highlands. Situated on the eastern shore of Loch Lomond, it is the most southerly of the Munros. Ben Lomond lies within the Ben Lomond National Memorial Park and the Loch Lomond and The Trossachs National Park, property of the National Trust for Scotland.
The Trossachs generally refers to an area of wooded glens, braes, and lochs lying to the east of Ben Lomond in the Stirling council area of Scotland. The name is taken from that of a small woodland glen that lies at the centre of the area, but is now generally applied to the wider region.
Crianlarich is a village in Stirling council area and in the registration county of Perthshire, Scotland, around 6 miles (10 km) north-east of the head of Loch Lomond. The village bills itself as "the gateway to the Highlands".
Killin (; is a village in Perthshire, in the central highlands of Scotland. Situated at the western head of Loch Tay, the village is administered by the Stirling council area. Killin is a historic conservation village and sits within the Loch Lomond and The Trossachs National Park. It is the central settlement of the historic region of Breadalbane.
The River Dochart is in Perthshire, Scotland.
Kinloch Rannoch is a village in Perth and Kinross, Scotland, at the eastern end of Loch Rannoch, 18 miles (29 km) west of Pitlochry, on the banks of the River Tummel. The village is a tourist and outdoor pursuits centre. It has a small population and is fairly remote.
National Cycle Route 7 is a route of the National Cycle Network, running from Sunderland to Inverness.
Breadalbane – from Scottish Gaelic Bràghad Albainn, "the upper part of Alba" – is a region of the southern/central Scottish Highlands, traditionally comprising the watershed of Loch Tay. The Breadalbane Hydro-Electric Scheme lies within the region.
Strathyre is a district and settlement in the Stirling local government district of Scotland. It forms the south-eastern part of the parish of Balquhidder and was, prior to the 1973 reorganisation of local government, part of Perthshire. It is within the bounds of the Loch Lomond and the Trossachs National Park. In Gaelic, the district is Srath Eadhair and the village is An t-Iomaire Riabhach or an t-Iomaire Fada.
The Bracklinn Falls are a series of waterfalls north-east of Callander, Scotland on the course of the Keltie Water, where the river crosses the Highland Boundary Fault.
Falls of Falloch is a waterfall and local beauty spot on the river Falloch off the A82. It is 7 km (4 mi) south-west of the village of Crianlarich in the county of Stirling in Scotland. It is also on the West Highland Way.
The Falls of Leny are a series of waterfalls in the Trossachs of Scotland on the course of the Garbh Uisge, otherwise known as the River Leny, where the river crosses the Highland Boundary Fault. The falls are located near the Pass of Leny, just north-west of Callander.
The Inverarnan Canal was a short length of canal terminating at Garbal, close to the hamlet of Inverarnan, Scotland. This waterway once linked the old coaching inn, now the Drovers Inn, at Inverarnan, on the Allt Arnan Burn to the River Falloch and passengers could continue southward to Loch Lomond and finally to Balloch. From Inverarnan stagecoaches ran to various destinations in the north of Scotland.
Loch Iubhair pronounced yoo-ar meaning yew loch, is a freshwater loch, located in Glen Dochart, and 4 miles east of the village of Crianlarich. Loch Dochart is located immediately to the south east, and the outflow of Loch Dochart, as the River Dochart flows into Loch Iubhair.
The geology of Loch Lomond and The Trossachs National Park in the southwestern part of the Scottish Highlands consists largely of Neoproterozoic and Palaeozoic bedrock faulted and folded and subjected to low grade metamorphism during the Caledonian orogeny. These older rocks, assigned to the Dalradian Supergroup, lie to the northwest of the northeast – southwest aligned Highland Boundary Fault which defines the southern edge of the Highlands. A part of this mountainous park extends south of this major geological divide into an area characterised by younger Devonian rocks which are assigned to the Old Red Sandstone.
