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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] |
Scotland
Scotland is a Countries of the United Kingdom, country that is part of the United Kingdom. It contains nearly one-third of the United Kingdom's land area, consisting of the northern part of the island of Great Britain and more than 790 adjacent Islands of Scotland, islands, principally in the archipelagos of the Hebrides and the Northern Isles. To the south-east, Scotland has its Anglo-Scottish border, only land border, which is long and shared with England; the country is surrounded by the Atlantic Ocean to the north and west, the North Sea to the north-east and east, and the Irish Sea to the south. The population in 2022 was 5,439,842. Edinburgh is the capital and Glasgow is the most populous of the cities of Scotland. The Kingdom of Scotland emerged as an independent sovereign state in the 9th century. In 1603, James VI succeeded to the thrones of Kingdom of England, England and Kingdom of Ireland, Ireland, forming a personal union of the Union of the Crowns, three kingdo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mainstem (hydrology)
In hydrology, a main stem or mainstem (also known as a trunk) is "the primary downstream segment of a river, as contrasted to its tributaries". The mainstem extends all the way from one specific headwater to the outlet of the river, although there are multiple ways to determine which headwater (or first-order tributary) is the source of the main stem. Water enters the main stem from the river's drainage basin, the land area through which the mainstem and its tributaries flow.. A drainage basin may also be referred to as a ''watershed'' or ''catchment''. Hydrological classification systems assign numbers to tributaries and mainstems within a drainage basin. In the Strahler number, a modification of a system devised by Robert E. Horton in 1945, channels with no tributaries are called "first-order" streams. When two first-order streams meet, they are said to form a second-order stream; when two second-order streams meet, they form a third-order stream, and so on. In the Horton sy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Netherley, Scotland
Netherley, Scotland is a village in Aberdeenshire, situated approximately five miles northwest of Stonehaven.United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004 Netherley is located in the Mounth area of the Grampian Highlands. At the eastern edge of Netherley is a significant wetland bog known as Red Moss. To the southwest of Netherley lie Meikle Carewe Hill and Curlethney Hill. At the south edge of Netherley is the peak of Craggie Cat. Natural features The Red Moss is a national Site of Special Scientific Interest within the United Kingdom, due to its diverse species content and its undisturbed habitat; the outlet of Red Moss is Crynoch Burn. To the west of Netherley lies another watercourse, Cairnie Burn, which is a tributary of the Crynoch Burn. Education Netherley School is an historic primary school A primary school (in Ireland, India, the United Kingdom, Australia, New Zealand, Trinidad and Tobago, Jamaica, So ... [...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] |
Hill Of Muchalls
The Hill of Muchalls is a coastal mountainous landform situated approximately 1.4 kilometres west of the Bridge of Muchalls in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. The peak elevation of this mountain is 120 metres above mean sea level. From Megray Hill there are expansive views to the North Sea facing east. The summit affords scenic vies of the historic harbour of Stonehaven. Geology and hydrology The surface runoff and flank drainages of the Hill of Muchalls flow to the Burn of Muchalls, situated nearby to the north. Nearby similar landforms include Kempstone Hill, Garrison Hill, Craggie Cat and Curlethney Hill. History Neolithic traces of civilisation appear on the nearby Kempstone Hill in the form of standing stones. This hill is near to the posited location for the noted Battle of Mons Graupius between the Romans and the indigenous Caledonians. Hogan, C. Michael, ''History of Muchalls Castle'', (2005) The major Roman Camp of Rae ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff or rock face is an area of Rock (geology), rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and Dolomite (rock), dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bothy
A bothy is a basic shelter, usually left unlocked and available for anyone to use free of charge. It was also a term for basic accommodation, usually for gardeners or other workers on an estate. Bothies are found in remote mountainous areas of Scotland, Northern England, Ulster and Wales. They are particularly common in the Scottish Highlands, but related buildings can be found around the world (for example, in the Nordic countries there are wilderness huts). A bothy was also a semi-legal drinking den on the Isle of Lewis. These, such as ''Bothan Eòrapaidh'', were used until recent years as gathering points for local men and were often situated in an old hut or caravan. Definition In Scots law, bothies are defined as: "a building of no more than two storeys which— * (a) does not have any form of— ** (i) mains electricity, ** (ii) piped fuel supply, and ** (iii) piped mains water supply, * (b) is 100 metres or more from the nearest public road (within the meaning of section ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Causey Mounth
The Causey Mounth is an ancient drovers' road over the coastal fringe of the Grampian Mountains in Aberdeenshire, Scotland. This route was developed around the 12th century Anno Domini, AD as the main highway between Stonehaven and Aberdeen, and it continued to function as the principal route connecting these two cities until the mid-20th century, when construction of the modern A90 road occurred in this area. There are extant paved and usable sections of this road over part of the alignment; however, many parts of the ancient route are no more than Trail, footpaths, and in some cases the road has vanished into agricultural fields. Constructed in the Middle Ages, the Causey Mounth was created as an elevated rock causeway to span many of the boggy areas such as the Portlethen Moss. A considerable portion of the alignment of the Causey Mounth is illustrated on the UK Ordnance Survey map, although a large fraction of the route cannot be navigated by a conventional passenger vehicle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mounth
The Mounth ( ) is the broad upland in northeast Scotland between the Highland Boundary and the River Dee, at the eastern end of the Grampians. Name and etymology The name ''Mounth'' is ultimately of Pictish origin. The name is derived from ''*monɪð'', meaning "mountain" (cf. Welsh ''mynydd''). It is invariably referred to as "the Mounth" and pronounced "munth". Details The ranges to the north-west are known as the Monadh Liath and the Monadh Ruadh (called the Cairngorms in English), meaning the ''Grey Mounth'' and the ''Red Mounth''. Some sources regard the Mounth as extending as far west as Drumochter Pass ( A9), but it is now generally agreed to start at the Cairnwell Pass ( A93 – highest main road pass in Britain, Glen Shee ski centre). Here, a high undulating plateau invaded by deep glacial troughs (Glen Isla, Glen Callater, Glen Muick, Glen Clova) culminates in Glas Maol () on the main watershed, with the outlying granite Lochnagar () and its surroundi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coast
A coast (coastline, shoreline, seashore) is the land next to the sea or the line that forms the boundary between the land and the ocean or a lake. Coasts are influenced by the topography of the surrounding landscape and by aquatic erosion, such as that caused by wind wave, waves. The geology, geological composition of rock (geology), rock and soil dictates the type of shore that is created. Earth has about of coastline. Coasts are important zones in natural ecosystems, often home to a wide range of biodiversity. On land, they harbor ecosystems, such as freshwater marsh, freshwater or estuary, estuarine wetlands, that are important for birds and other terrestrial animals. In wave-protected areas, coasts harbor salt marshes, mangroves, and seagrass meadow, seagrasses, all of which can provide nursery habitat for finfish, shellfish, and other aquatic animals. Rocky shores are usually found along exposed coasts and provide habitat for a wide range of sessility (motility), sessile ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Ages
In the history of Europe, the Middle Ages or medieval period lasted approximately from the 5th to the late 15th centuries, similarly to the post-classical period of global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern period. The medieval period is itself subdivided into the Early, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralised authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the 7th century, North Africa and the Middle East—once part of the Byzantine Empire� ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muchalls Castle
Muchalls Castle stands overlooking the North Sea in the countryside of Kincardine and Mearns, Aberdeenshire, Scotland. The lower course is a well-preserved Romanesque, double-groined 13th-century tower house structure, built by the Frasers of Muchalls. Upon this structure, the 17th-century castle was begun by Alexander Burnett of Leys and completed by his son, Sir Thomas Burnett, 1st Baronet, in 1627. The Burnetts of Leys built the remaining four-storey present-day castle. One of the most interesting castles in North-East Scotland, according to noted architectural historian Nigel Tranter, it is designed in the classic L style with a further extension wing at the west end. Muchalls Castle entered national history in 1638 when a seminal Covenanter gathering took place there, precedent the English Civil War. The plasterwork ceilings of the principal drawing rooms are generally regarded as among the three finest examples of plasterwork ceilings in Scotland. These adornments ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
