Perthshire, officially the County of Perth, is a historic county and registration county in central Scotland. Geographically it 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. It was a local government county from 1890 to 1930.
Kinross is a burgh in Perth and Kinross, Scotland, around 13 miles south of Perth and around 20 miles northwest of Edinburgh. It is the traditional county town of the historic county of Kinross-shire.
The County of Kinross or Kinross-shire is a historic county and registration county in eastern Scotland, administered as part of Perth and Kinross since 1930. Surrounding its largest settlement and county town of Kinross, the county borders Perthshire to the north and Fife to the east, south and west.
Milnathort is a small town in the parish of Orwell in the county of Kinross-shire, Scotland and since 1996, the local council area of Perth and Kinross. The smaller neighbour of nearby Kinross, Milnathort has a population of around 2,000 people. It is situated amidst countryside at the foot of the Ochil Hills, and near the north shore of Loch Leven. From 1977 it became more easily accessible due to the development of the M90 motorway. The name comes from the Gaelic maol coirthe meaning "bare hill of the standing stones".
Clunie is a small settlement in Perthshire, Scotland, four miles west of Blairgowrie. It lies on the western shore of the Loch of Clunie.
Amulree is a small hamlet in Perth and Kinross, Scotland. It lies in hilly country on the A822 road, 1 km (0.62 mi) east of Loch Freuchie in Strathbraan, 8 km (5.0 mi) west of Dunkeld and 10 km (6.2 mi) north of Crieff. It lies close to the geographical centre of Scotland.
Saline is a village and parish in Fife, Scotland, situated 5 miles (8.0 km) to the north-west of Dunfermline. It lies in an elevated position on the western slopes of the Cleish Hills.
The Lomond Hills, also known outside the locality as the Paps of Fife, are a range of hills in central Scotland. They lie in western central Fife and Perth and Kinross, Scotland. At 522 metres (1,713 ft) West Lomond is the highest point in the county of Fife.
Torryburn is a village and parish in Fife, Scotland, lying on the north shore of the Firth of Forth. It is one of a number of old port communities on this coast and at one point served as port for Dunfermline. It lies in the Bay of Torry in south western Fife.
Portmoak is a parish in Kinross-shire, Scotland. It consists of a group of settlements running north to south: Glenlomond, Wester Balgedie, Easter Balgedie, Kinnesswood, Kilmagadwood and Scotlandwell.
Rubers Law is a prominent, conical hill in the Scottish Borders area of south-east Scotland. It stands on the south bank of the River Teviot, between the towns of Hawick and Jedburgh, and south of the village of Denholm. The hill is on the border between the historic parishes of Cavers and Hobkirk, and until 1975 it stood within the historic county of Roxburghshire.
Scotlandwell is a village in Portmoak, Kinross-shire, Scotland. It is within the Perth and Kinross council area. It lies to the east of Loch Leven, at the junction of the A977 and B920 roads, approximately 4 miles west of Glenrothes and 4 miles east of Kinross.
Moonzie is a small parish in Fife, Scotland, about 3 miles north-west of Cupar. It is bounded on the west by Creich, on the north by Kilmany, on the south-east by Cupar and on the south-west by Monimail.
Abdie is a parish in north-west Fife, Scotland, lying on the south shore of the Firth of Tay on the eastern outskirts of Newburgh, extending about 3 miles eastwards to the boundary of Dunbog parish, with which it is now united ecclesiastically and for the Community Council. It is also bounded by Collessie on the south and has a small border with the parish of Moonzie in the south-east.
Cameron is a parish in east Fife, Scotland, 3½ miles south-west of St Andrews.
Mary Lundie Duncan was a Scottish poet and hymnwriter from Kelso, Scotland.
Sgor Gaibhre is a mountain in the Grampian Mountains of Scotland. It lies on the border of Highland and Perth and Kinross, near Loch Ossian.
The geology of national parks in Britain strongly influences the landscape character of each of the fifteen such areas which have been designated. There are ten national parks in England, three in Wales and two in Scotland. Ten of these were established in England and Wales in the 1950s under the provisions of the National Parks and Access to the Countryside Act 1949. With one exception, all of these first ten, together with the two Scottish parks were centred on upland or coastal areas formed from Palaeozoic rocks. The exception is the North York Moors National Park which is formed from sedimentary rocks of Jurassic age.
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.
The geology of Northumberland National Park in northeast England includes a mix of sedimentary, intrusive and extrusive igneous rocks from the Palaeozoic and Cenozoic eras. Devonian age volcanic rocks and a granite pluton form the Cheviot massif. The geology of the rest of the national park is characterised largely by a thick sequence of sedimentary rocks of Carboniferous age. These are intruded by Permian dykes and sills, of which the Whin Sill makes a significant impact in the south of the park. Further dykes were intruded during the Palaeogene period. The whole is overlain by unconsolidated sediments from the last ice age and the post-glacial period.
