|
Finzean Estate
Finzean (; gd, Fìnnean) is a rural community, electoral polling district, community council area and former ecclesiastical parish, which forms the southern part of the Parish of Birse, Aberdeenshire, Scotland. Finzean was the subject of many well-known landscape paintings by the artist Joseph Farquharson, whose family have owned Finzean Estate (which occupies the eastern half of Finzean) since the 17th century. Finzean extends to approximately 8000 hectares in area and had a population of approximately 270 in 2002. Toponymy Finzean is pronounced /ˈfɪŋən/. This is due to the original Scots spelling, Finȝean, containing the letter yogh, which was later erroneously confused with the tailed z. Geographical extent Finzean occupies the upper catchment of the Water of Feugh within the area of the Lower Deeside, the main tributary of the River Dee. The southern boundary of Finzean is the old county boundary between Aberdeenshire and Kincardineshire which follows the Water o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aberdeenshire
Aberdeenshire ( sco, Aiberdeenshire; gd, Siorrachd Obar Dheathain) is one of the 32 Subdivisions of Scotland#council areas of Scotland, council areas of Scotland. It takes its name from the County of Aberdeen which has substantially different boundaries. The Aberdeenshire Council area includes all of the area of the Counties of Scotland, historic counties of Aberdeenshire and Kincardineshire (except the area making up the City of Aberdeen), as well as part of Banffshire. The county boundaries are officially used for a few purposes, namely land registration and Lieutenancy areas of Scotland, lieutenancy. Aberdeenshire Council is headquartered at Woodhill House, in Aberdeen, making it the only Scottish council whose headquarters are located outside its jurisdiction. Aberdeen itself forms a different council area (Aberdeen City). Aberdeenshire borders onto Angus, Scotland, Angus and Perth and Kinross to the south, Highland (council area), Highland and Moray to the west and Aber ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Dee, Aberdeenshire
The River Dee ( gd, Uisge Dhè) is a river in Aberdeenshire, Scotland. It rises in the Cairngorms and flows through southern Aberdeenshire to reach the North Sea at Aberdeen. The area it passes through is known as Deeside, or Royal Deeside in the region between Braemar and Banchory because Queen Victoria came for a visit there in 1848 and greatly enjoyed herself. She and her husband, Prince Albert, built Balmoral Castle there which replaced an older castle. Deeside is a popular area for tourists, due to the combination of scenic beauty and historic and royal associations. It is part of the Cairngorms National Park, and the Deeside and Lochnagar National Scenic Area. The Dee is popular with anglers and is one of the most famous salmon fishing rivers in the world. The New Statistical Account of Scotland attributed the name Dee as having been used as early as the second century AD in the work of the Alexandrian geographer Claudius Ptolemy, as ''Δηοῦα'' (=Deva), meaning ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calluna
''Calluna vulgaris'', common heather, ling, or simply heather, is the sole species in the genus ''Calluna'' in the flowering plant family Ericaceae. It is a low-growing evergreen shrub growing to tall, or rarely to and taller, and is found widely in Europe and Asia Minor on acidic soils in open sunny situations and in moderate shade. It is the dominant plant in most heathland and moorland in Europe, and in some bog vegetation and acidic pine and oak woodland. It is tolerant of grazing and regenerates following occasional burning, and is often managed in nature reserves and grouse moors by sheep or cattle grazing, and also by light burning. ''Calluna'' was separated from the closely related genus ''Erica'' by Richard Anthony Salisbury, who devised the generic name ''Calluna'' probably from the Ancient Greek (), "beautify, sweep clean", in reference to its traditional use in besoms. The specific epithet ''vulgaris'' is Latin for 'common'. ''Calluna'' is differentiated from ''Er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clachnaben
Clachnaben (archaically "Cloch-na'bain"; Scottish Gaelic: "Clach na Beinne") is a 589-metre hill in Glen Dye, Aberdeenshire, Scotland. It is a distinctive hill visible from many points on Lower Deeside and is topped with a large granite tor. ''Clachnaben'' is the war cry of Clan Strachan. The hill gives its name to one of the houses at Aboyne Academy. Geography A popular walk starts at the car park on the Cairn O' Mounth (Banchory–Fettercairn) road, 10 kilometres south of Banchory. Popularity has caused some erosion on the old steep path which climbs this hill directly; however, efforts have been made to stabilise the erosion. A new improved path takes an easier and less direct route from Millar's Bog to the summit. There are views to Mount Battock, Lochnagar and Bennachie. The granite tor provides some rock climbing Rock climbing is a sport in which participants climb up, across, or down natural rock formations. The goal is to reach the summit of a formation or the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Finzean From South
Finzean (; gd, Fìnnean) is a rural community, electoral polling district, community council area and former ecclesiastical parish, which forms the southern part of the Parish of Birse, Aberdeenshire, Scotland. Finzean was the subject of many well-known landscape paintings by the artist Joseph Farquharson, whose family have owned Finzean Estate (which occupies the eastern half of Finzean) since the 17th century. Finzean extends to approximately 8000 hectares in area and had a population of approximately 270 in 2002. Toponymy Finzean is pronounced /ˈfɪŋən/. This is due to the original Scots spelling, Finȝean, containing the letter yogh, which was later erroneously confused with the tailed z. Geographical extent Finzean occupies the upper catchment of the Water of Feugh within the area of the Lower Deeside, the main tributary of the River Dee. The southern boundary of Finzean is the old county boundary between Aberdeenshire and Kincardineshire which follows the Water o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Finzean Estate
Finzean (; gd, Fìnnean) is a rural community, electoral polling district, community council area and former ecclesiastical parish, which forms the southern part of the Parish of Birse, Aberdeenshire, Scotland. Finzean was the subject of many well-known landscape paintings by the artist Joseph Farquharson, whose family have owned Finzean Estate (which occupies the eastern half of Finzean) since the 17th century. Finzean extends to approximately 8000 hectares in area and had a population of approximately 270 in 2002. Toponymy Finzean is pronounced /ˈfɪŋən/. This is due to the original Scots spelling, Finȝean, containing the letter yogh, which was later erroneously confused with the tailed z. Geographical extent Finzean occupies the upper catchment of the Water of Feugh within the area of the Lower Deeside, the main tributary of the River Dee. The southern boundary of Finzean is the old county boundary between Aberdeenshire and Kincardineshire which follows the Water o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forest Of Birse
The Forest of Birse is a remote upland area in the upper catchment of the Water of Feugh, which forms the south-western portion of the Parish of Birse, Aberdeenshire, Scotland. It also forms the western part of the community of Finzean, but has a separate, complex history of landownership relating to its status as a commonty, which has involved a large number of disputes since the 16th century. In more recent decades, the forest has been a popular destination for people from Aberdeen taking picnics, as it is the closest area of Highland scenery to the city. Description The eastern boundary of the Forest of Birse is marked by the Finlets and Laird's burns; two minor tributaries of the Feugh (itself a tributary of the River Dee) which join the river about 1 kilometre upstream from Woodend. Otherwise the boundary generally follows the watershed of the Feugh, which runs along the tops of the following hills (clockwise from the south): Baudnacauner, Cock Hill, Hill of Cammie, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River North Esk, Angus
The North Esk ( gd, Easg Thuath) is a river in Angus and Aberdeenshire, Scotland. It is formed by the meeting of the Water of Mark (from Glen Mark) and the Water of Lee (from Loch Lee), and enters the North Sea four miles north of Montrose. It forms the boundary between Angus and Aberdeenshire at certain stages in its course. It was also noted in the 19th century as a good point for fishing. Tributaries Downstream of the meeting of the headwaters referred to above, the River North Esk is joined by various other tributaries. The Water of Effock enters on its right side and then the Water of Tarf enters on its left bank at Tarfside. The West Water is a considerable right bank tributary which enters near Stracathro in Strathmore. Its upper reaches are known as the Water of Saughs. The Luther Water is the last significant tributary of the North Esk; it enters on the left bank near North Water Bridge. The Luther Water drains the Howe of the Mearns. Glen Esk Villages Tarfside ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Tanar
Glen Tanar ( gd, Gleann Tanar) is a glen in Aberdeenshire, eastern Scotland, through which the Water of Tanar flows. Near the mouth of the glen, at Tower o' Ess, the Water of Tanar flows into the River Dee. This flows through Deeside into the North Sea at Aberdeen. Glen Tanar contains the third largest area of Caledonian Forest in Scotland, and is of national and European importance.Glen Tanar SSSI Site Management Statement. p. 1. It is around 18 miles East from the King's private residence at Balmoral Castle. 42 km2 of the glen is designated by NatureScot as a national nature reserve (NNR). Most of the area remains under private ownership as part of the Glen Tanar Estate. However 182 ha is owned by NatureScot, being designated as the "Strict Reserve Zone" of the NNR.Glen Tanar SSSI Site Management Statement. p. 4. Glen Tanar lies within the Cairngorms National Park, and is also designated as a Site of Special Scientific Interest (SSSI), a Special Protection A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
