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Kempstone Hill
Kempstone Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. The peak elevation of this mountain is 132 metres above mean sea level. This hill has been posited by Gabriel Jacques Surenne, Archibald Watt and C.Michael Hogan as the location for the noted Battle of Mons Graupius between the Romans and the indigenous Caledonians. The major Roman Camp of Raedykes is situated about three kilometres to the west. From Kempstone Hill there are fine views to the North Sea facing east and slightly to the north of Muchalls Castle. There is a UK trigpoint installation on Kempstone Hill. Geology and hydrology Kempstone Hill is situated approximately 2.3 kilometers to the north of Stonehaven; surface runoff and drainage from the northern and eastern slopes of Kempstone Hill flow north to the Burn of Muchalls. Surface runoff from the south and west flanks flow to the Burn of Monboys, a very slightly alkaline stream These low pH levels ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kempstone Hill Wind Farm (ii)
Kempstone is a village and civil parish situated in the English county of Norfolk. Kempston is located north-west of Dereham and west of Norwich. History Kempstone's name is of Anglo-Saxon origin and derives from the Old English for ''Cymi's'' farmstead. In the Domesday Book, Kempstone is listed as a settlement of 9 households in the hundred of Laundich. In 1086, the village was part of the East Anglian estates of William de Warenne. Geography Due to its small size, separate population statistics are not available for Kempstone as it is amalgamated with Great Dunham. St. Paul's Church The ruins of St. Paul's Church, which formerly served the parish, are within the parish. The church collapsed in the 1950s. Governance Kempstone is part of the electoral ward of Launditch for local elections and is part of the district of Breckland. The village's national constituency is South West Norfolk South West Norfolk is a Constituencies of the Parliament of the United ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burn Of Muchalls
The Burn of Muchalls is an easterly flowing stream in Aberdeenshire, Scotland that discharges to the North Sea. Its point of discharge is on a rocky beach set with scenic sea stacks. Flowing principally over agricultural lands, the Burn of Muchalls traverses through the hamlet of the Bridge of Muchalls, flows beneath the A90 road and thence to the rugged shoreline of the North Sea slightly to the south of Doonie Point. Just above the discharge to the North Sea is a scenic pool, used in the drowning scene of Ophelia in the Franco Zeffirelli film ''Hamlet''. A northern fork of the Burn of Muchalls flows over lands of Muchalls Castle prior to the confluence with the mainstem Burn of Muchalls within the Bridge of Muchalls. History In the Middle Ages the only coastal land route, the over the Mounth, the Causey Mounth, crossed the Burn of Muchalls at the Bridge of Muchalls. Near the mouth of the Burn of Muchalls is an old mill that earlier functioned to harness the power of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Renewable Energy Resources
Renewable energy (also called green energy) is energy made from renewable resource, renewable natural resources that are replenished on a human lifetime, human timescale. The most widely used renewable energy types are solar energy, wind power, and hydropower. Bioenergy and geothermal power are also significant in some countries. Some also consider Nuclear power proposed as renewable energy, nuclear power a renewable power source, although this is controversial, as nuclear energy requires mining uranium, a nonrenewable resource. Renewable energy installations can be large or small and are suited for both urban and rural areas. Renewable energy is often deployed together with further electrification. This has several benefits: electricity can heat pump, move heat and Electric vehicle, vehicles efficiently and is clean at the point of consumption. Variable renewable energy sources are those that have a fluctuating nature, such as wind power and solar power. In contrast, ''contro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Standing Stone
A menhir (; from Brittonic languages: ''maen'' or ''men'', "stone" and ''hir'' or ''hîr'', "long"), standing stone, orthostat, or lith is a large upright rock (geology), stone, emplaced in the ground by humans, typically dating from the European middle Bronze Age. They can be found individually as monoliths, or as part of a group of similar stones. Menhirs' size can vary considerably, but they often taper toward the top. Menhirs are found across Europe, Africa, and Asia, with a concentration in Western Europe, notably in Ireland, Great Britain, and Brittany. Theories concerning their purpose remain speculative, with hypotheses ranging from Ancient Celtic religion, druidic rituals to territorial markers or elements of an ideological system. Some menhirs feature Engraving, engravings, including anthropomorphic figures and symbols, and are often associated with ancient religious ceremonies and Chamber tomb, burial chambers. Etymology The word ''menhir'' was adopted from F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neolithic
The Neolithic or New Stone Age (from Ancient Greek, Greek 'new' and 'stone') is an archaeological period, the final division of the Stone Age in Mesopotamia, Asia, Europe and Africa (c. 10,000 BCE to c. 2,000 BCE). It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the History of agriculture, introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of sedentism, settlement. The term 'Neolithic' was coined by John Lubbock, 1st Baron Avebury, Sir John Lubbock in 1865 as a refinement of the three-age system. The Neolithic began about 12,000 years ago, when farming appeared in the Epipalaeolithic Near East and Mesopotamia, and later in other parts of the world. It lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BCE), marked by the development ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aberdeenshire Council
Aberdeenshire Council is the local authority for Aberdeenshire, one of the 32 council areas of Scotland. The council has been under no overall control since its creation in 1996. It is based at Woodhill House, which is outside its own territory in the neighbouring Aberdeen City council area. History The Aberdeenshire council area was created in 1996 under the Local Government etc. (Scotland) Act 1994, which abolished the regions and districts which had been created in 1975, replacing them with single-tier council areas. Aberdeenshire covered the area of the abolished Banff and Buchan, Gordon and Kincardine and Deeside districts, all of which had been part of the Grampian region. It is named after the historic county of Aberdeenshire, but covers a larger area, also including most of the historic county of Kincardineshire and eastern parts of the historic county of Banffshire. Governance The council is the fifth largest Scottish council by number of councillors, having ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woodland
A woodland () is, in the broad sense, land covered with woody plants (trees and shrubs), or in a narrow sense, synonymous with wood (or in the U.S., the '' plurale tantum'' woods), a low-density forest forming open habitats with plenty of sunlight and limited shade (see differences between British, American and Australian English explained below). Some savannas may also be woodlands, such as ''savanna woodland'', where trees and shrubs form a light canopy. Woodlands may support an understory of shrubs and herbaceous plants including grasses. Woodland may form a transition to shrubland under drier conditions or during early stages of primary or secondary succession. Higher-density areas of trees with a largely closed canopy that provides extensive and nearly continuous shade are often referred to as forests. Extensive efforts by conservationist groups have been made to preserve woodlands from urbanization and agriculture. For example, the woodlands of Northwest Indiana ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riparian
A riparian zone or riparian area is the interface between land and a river or stream. In some regions, the terms riparian woodland, riparian forest, riparian buffer zone, riparian corridor, and riparian strip are used to characterize a riparian zone. The word ''riparian'' is derived from Latin '' ripa'', meaning " river bank". Riparian is also the proper nomenclature for one of the terrestrial biomes of the Earth. Plant habitats and communities along the river margins and banks are called riparian vegetation, characterized by hydrophilic plants. Riparian zones are important in ecology, environmental resource management, and civil engineering because of their role in soil conservation, their habitat biodiversity, and the influence they have on terrestrial and semiaquatic fauna as well as aquatic ecosystems, including grasslands, woodlands, wetlands, and even non-vegetative areas. Riparian zones may be natural or engineered for soil stabilization or restoration. These zon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limpet Burn
Limpet Burn is a watercourse in Aberdeenshire, Scotland whose discharge is deemed part of the North Sea coastal drainage. Prominent geographic features in the vicinity of Limpet Burn are Megray Hill and Kempstone Hill. Notable buildings in proximity to Limpet Burn are Ury House, Muchalls Castle and Chapel of St. Mary and St. Nathalan. Part of the watershed of Limpet Burn has been suggested by some as the site of the first recorded battle in the history of Scotland, the Battle of Mons Graupius. See also * Cowie Water References Rivers of Aberdeenshire {{Scotland-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Curlethney Hill
Curlethney Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. (Grid Reference NO 918 839) The peak elevation of this mountain is 246 metres above mean sea level. This landform lies slightly southwest of the village of Netherley. The northwest boundary of the moorland atop Curlethney Hill is formed by the southwestern flanks of Craggie Cat, a nearby peak. Geology and hydrology This mountain is covered virtually entirely with moorland. Curlethney Hill is situated approximately 0.9 kilometers to the east of Meikle Carewe Hill; surface runoff and drainage from the northern and eastern slopes of Curlethney Hill flows north to Crynoch Burn, at reaches above the Red Moss. Waters within the Red Moss are decidedly acidic, with measured summer pH values in the range of 5.67. These low pH levels may be caused in part by the peat drainage from the moorland on Meikle Carewe Hill and Curlethney Hill. The southwest flanks of Curlethn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meikle Carewe Hill
Meikle Carewe Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. (Grid Reference NO 921 828) The peak elevation of this mountain is 266 metres above mean sea level. Meikle Carewe is a prominent landform visible from a number of coastal hills such as Kempstone Hill and Megray Hill; it also forms a major backdrop to the community of Netherley, Aberdeenshire, Netherley. Geology and hydrology This mountain is covered virtually entirely with moorland. Its northwestern slopes drain to the Cairnie Burn, whilst the northern and eastern slopes drain to Crynoch Burn. The western slopes yield surface runoff that drains into Cowton Burn. Curlethney Hill is situated approximately 0.9 kilometers to the east of Meikle Carewe Hill Surface runoff and drainage from Curlethney Hill also drain north to Crynoch Burn, at reaches above the Red Moss, Aberdeenshire, Red Moss. Waters within the Red Moss are decidedly acidic, with measured summer pH values in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
