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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 (compa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kempstone Hill Wind Farm (ii)
Kempstone is a village situated in the Breckland District of Norfolk and covers an area of 331 hectares (1.3 square miles) with an estimated population of 18 as of UK census 2001 At the 2011 Census the population remained less 100 and is included in the civil parish of Great Dunham. The village lies south of Litcham and by road east from Dereham Dereham (), also known as East Dereham, is a town and civil parishes in England, civil parish in the Breckland District of the England, English county of Norfolk. It is situated on the A47 road, about 15 miles (25 km) west of the city .... The villages name means 'Cymi's farm/settlement'. It is served by All Saints church, Litcham (with Kempston) in the Benefice of Litcham. It was once served by the now derelict St.Pauls References http://kepn.nottingham.ac.uk/map/place/Norfolk/Kempstone External links {{authority control Villages in Norfolk Breckland District Civil parishes in Norfolk ... [...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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Renewable Energy Resources
Renewable energy is energy that is collected from renewable resources that are naturally replenished on a human timescale. It includes sources such as sunlight, wind, the movement of water, and geothermal heat. Although most renewable energy sources are sustainable, some are not. For example, some biomass sources are considered unsustainable at current rates of exploitation. Renewable energy often provides energy for electricity generation to a grid, air and water heating/cooling, and stand-alone power systems. Renewable energy technology projects are typically large-scale, but they are also suited to rural and remote areas and developing countries, where energy is often crucial in human development. Renewable energy is often deployed together with further electrification, which has several benefits: electricity can move heat or objects efficiently, and is clean at the point of consumption. In addition, electrification with renewable energy is more efficient and therefore lead ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scots Language
Scots ( endonym: ''Scots''; gd, Albais, ) is an Anglic language variety in the West Germanic language family, spoken in Scotland and parts of Ulster in the north of Ireland (where the local dialect is known as Ulster Scots). Most commonly spoken in the Scottish Lowlands, Northern Isles and northern Ulster, it is sometimes called Lowland Scots or Broad Scots to distinguish it from Scottish Gaelic, the Goidelic Celtic language that was historically restricted to most of the Scottish Highlands, the Hebrides and Galloway after the 16th century. Modern Scots is a sister language of Modern English, as the two diverged independently from the same source: Early Middle English (1150–1300). Scots is recognised as an indigenous language of Scotland, a regional or minority language of Europe, as well as a vulnerable language by UNESCO. In the 2011 United Kingdom census, 2011 Scottish Census, over 1.5 million people in Scotland reported being able to speak Scots. As there are ... [...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 human-made upright rock (geology), stone, 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. They are widely distributed across Europe, Africa and Asia, but are most numerous in Western Europe; particularly in Ireland, Great Britain, and Brittany, where there are about 50,000 examples, and northwestern France, where there are some 1,200 further examples. Standing stones are usually difficult to date. They were constructed during many different periods across pre-history as part of the larger megalithic cultures in Europe and near areas. Some menhirs stand next to buildings that have an early or current religious significance. One example is the South Zeal Menhir in Devon, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. 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 introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aberdeenshire Council
Aberdeenshire ( sco, Aiberdeenshire; gd, Siorrachd Obar Dheathain) is one of the 32 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 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. 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 and Perth and Kinross to the south, Highland and Moray to the west and Aberdeen City to the east. Traditionally, it has been economically dependent upon the primary sector (agriculture, fishing, and forestry) and relat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woodland
A woodland () is, in the broad sense, land covered with trees, 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). 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 have been preserved as part of the Indiana Dunes. Definitions United Kingdom ''Woodland'' is used in British woodland management to mean tre ... [...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. 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 fauna and aquatic ecosystems, including grasslands, woodlands, wetlands, or even non-vegetative areas. 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". Characteristics Riparian zones may be natural or engineered for soil stabilization or restoration. These zones are important natural b ... [...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 The Cowie Water ( gd, Uisge Chollaidh) is a river of Scotland. Geography The river rises in the Grampian Mountains in Kincardineshire, and discharges to the North Sea in the northern part of Stonehaven,United Kingdom Ordnance Survey Map Landra ... 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 Curlethney Hill ... [...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. 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. Waters within the Red Moss are decidedly acidic, with measured summer pH values in the range of 5.68. These low pH levels may be caus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
