Carsphairn And Scaur Hills
The Carsphairn and Scaur Hills are the western and eastern hills respectively of a hill range in the Southern Uplands of Scotland. Ordnance Survey maps don't have a general name for the hill area as a whole. Also, Ordnance Survey use "Scar" rather than the local spelling of "Scaur" - the word is pronounced as "Scar" however. In their Landranger Series of maps, it requires four separate sheets to cover the area. Location The range lies between two other ranges, the Galloway Hills to the west and the Lowther Hills to the east. The overall shape of this hill area is oval with the longer curved sides to top and bottom. From the north western point of the oval at Dalmellington to the south eastern one at Thornhill is around 39 kilometres (as the crow flies), though Dalmellington lies some 10 kilometres further north than Thornhill. So the axis of the oval runs from north west to south east. Taking a section across the west end of the oval, from New Cumnock in the north to Carsphair ...
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Southern Uplands
The Southern Uplands ( gd, Na Monaidhean a Deas) are the southernmost and least populous of mainland Scotland's three major geographic areas (the other two being the Central Lowlands and the Grampian Mountains and the Highlands, as illustrated in the accompanying map). The term is used both to describe the geographical region and to collectively denote the various ranges of hills and mountains within this region. An overwhelmingly rural and agricultural region, the Southern Uplands are partly forested and contain many areas of open moorland - the hill names in the area are congruent with these characteristics. Geology The Southern Uplands consist mainly of Silurian sedimentary deposits deposited in the Iapetus Ocean 420 million years ago. These rocks were pushed up from the sea bed into an accretionary wedge during the Caledonian orogeny, roughly 400 million years ago ( Ma), when the continents and terranes of Laurentia, Baltica and Avalonia collided. The Caledonian or ...
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