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Megray Hill
Megray Hill is a low-lying coastal mountainous landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. The peak elevation of this mountain is 120 metres above mean sea level. This hill has been posited as a likely 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 Megray Hill there are expansive views to the North Sea facing east. The summit affords scenic views of the historic harbour of Stonehaven. Geology and hydrology Megray Hill is situated approximately 1.1 kilometers to the north of Stonehaven; surface runoff and drainage from the northern and eastern slopes of Megray Hill flow north to the Burn of Muchalls. Surface runoff from the south flank flows is within the Cowie Water catchment area, the Cowie Water being a very slightly alkaline stream These low pH levels (compared to other area streams) may be ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landform
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004 south of the ruined Cowie Castle. Tributaries of the Cowie Water include the Burn of Monboys, which drains the area to the north, in which the archaeological site Raedykes Roman Camp is situated; and Cowton Burn. Notable features in this vicinity include Dunnottar Castle, Fetteresso Castle and Muchalls Castle. Other nearby coastal waterways discharging to the North Sea include Burn of Muchalls to the north and Carron Water to the south. Hydrology and water quality Summer flow rates are typically in the range of at the river's mouth. July values for pH have been measured at 8.2 or slightly alkaline July water temperatures are about 11.9 degrees Celsius and electrical conductivi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aberdeen
Aberdeen (; sco, Aiberdeen ; gd, Obar Dheathain ; la, Aberdonia) is a city in North East Scotland, and is the third most populous city in the country. Aberdeen is one of Scotland's 32 local government council areas (as Aberdeen City), and has a population estimate of for the city of Aberdeen, and for the local council area making it the United Kingdom's 39th most populous built-up area. The city is northeast of Edinburgh and north of London, and is the northernmost major city in the United Kingdom. Aberdeen has a long, sandy coastline and features an oceanic climate, with cool summers and mild, rainy winters. During the mid-18th to mid-20th centuries, Aberdeen's buildings incorporated locally quarried grey granite, which may sparkle like silver because of its high mica content. Since the discovery of North Sea oil in 1969, Aberdeen has been known as the offshore oil capital of Europe. Based upon the discovery of prehistoric villages around the mouths of the rivers ... [...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 as the main highway between Stonehaven and Aberdeen around the 12th century AD and it continued to function as the principal route connecting these two cities until the mid 20th century, when modern highway construction of the 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 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 (particul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drovers' Road
A drovers' road, drove ''roador droveway is a route for droving livestock on foot from one place to another, such as to market or between summer and winter pasture (see transhumance). Many drovers' roads were ancient routes of unknown age; others are known to date back to medieval or more recent times. Description Drovers' roads are often wider than other roads, able to accommodate large herds or flocks. Packhorse ways were quite narrow as the horses moved in single file, whereas drove roads were at least and up to wide.Addison (1980), Pp. 70-78. In the United Kingdom, where many original drovers' roads have been converted into single carriageway metalled roads, unusually wide verges often give an indication of the road's origin. In Wales, the start of many droveways, drovers' roads are often recognisable by being deeply set into the countryside, with high earth walls or hedges. The most characteristic feature of these roads is the occasional sharp turn in the road, which p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Middle Ages
The High Middle Ages, or High Medieval Period, was the periodization, period of European history that lasted from AD 1000 to 1300. The High Middle Ages were preceded by the Early Middle Ages and were followed by the Late Middle Ages, which ended around AD 1500 (by historiography, historiographical convention). Key historical trends of the High Middle Ages include the medieval demography, rapidly increasing population of Europe, which brought about great social and political change from the preceding era, and the Renaissance of the 12th century, including the first developments of rural exodus and urbanization. By 1250, the robust population increase had greatly benefited the European economy, which reached levels that would not be seen again in some areas until the 19th century. That trend faltered during the Late Middle Ages because of a Crisis of the Late Middle Ages, series of calamities, most notably the Black Death, but also numerous wars as well as economic stagnation. Fro ... [...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] |
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] |
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] |
Burn Of Monboys
Burn of Monboys is a stream that rises in the Mounth, or eastern range of the Grampian Mountains, northwest of Stonehaven and south of Netherley, Aberdeenshire, Scotland. Monboys Burn is a tributary to the Cowie Water. Hydrology The headwaters of the Burn of Monboys rise on the southern and western slopes of the Meikle Carewe Hill where the stream flows downslope at a first westerly and thence southerly as it makes its way to discharge to the Cowie Water. The southwestern flanks of Craggie Cat, a hill in the northeast part of the Burn of Monboys drainage basin, drain to the Burn of Monboys. The stream has a greenish brown appearance and generally has lush vegetation growing all the way to its margins throughout most of its course of the middle and downstream reaches. The turbidity typically measures approximately 10 JTU and the July flow rate is roughly five cubic feet per second in the headwaters reach. pH levels have been measured at 7.27, very slightly alkaline, but undo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...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] |
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