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Saddleworth Moor
Saddleworth Moor is a moorland in North West England. Reaching more than above sea level, it is in the Dark Peak area of the Peak District National Park. It is crossed by the A635 road and the Pennine Way passes to its eastern side. Geography The moor takes its name from the parish of Saddleworth to the west, historically in the West Riding of Yorkshire, although it is on the western side of the Pennines and so has been part of Greater Manchester since 1974. The moor, an elevated plateau with gritstone escarpments or edges and, around its margins, deeply incised v-shaped valleys or cloughs with fast-flowing streams, straddles the metropolitan boroughs of Oldham in Greater Manchester and Kirklees in West Yorkshire. Moorland east of the county boundary with West Yorkshire is known as Wessenden Moor and Wessenden Head Moor. The moor is crossed by the A635 between the Greater Manchester and West Yorkshire Urban Areas. The A635 is known locally as the Isle of Skye road, taking the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dovestone Reservoir
Dovestone Reservoir lies at the convergence of the valleys of the Greenfield and Chew Brooks above the village of Greenfield, on Saddleworth Moor in Greater Manchester, England. The reservoir is on the western edge of the Peak District National Park. It supplies drinking water to the surrounding area and is a tourist attraction, providing several walks amongst picturesque landscapes. History John Platt of Oldham built a Neo-Gothic mansion at Ashway Gap on the south side of the valley in 1850. It was used as a shooting lodge but after his brother James's death in a shooting accident on the moor above it, the house was left empty. The house was later acquired by the Ashton-under-Lyne, Stalybridge and Dukinfield Waterworks Joint Committee. Boundary stones demarcating the extent of the estate are located at intervals along the footpaths along the south side of the reservoir. During World War I the waterworks board offered the house for use as a hospital. It was demolished in 1981 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metropolitan Borough Of Oldham
The Metropolitan Borough of Oldham is a metropolitan borough of Greater Manchester in North West England. It is named after its largest town, Oldham, The borough had a population of 237,628 making it the seventh-largest district by population in Greater Manchester. The borough spans . Geography Part of Oldham is rural and semi-rural, with a quarter of the borough lying within the Peak District National Park. The Metropolitan Borough of Rochdale lies to the north-west, the Metropolitan Borough of Kirklees (of West Yorkshire) to the east, and the Metropolitan Borough of Tameside to the south. The City of Manchester lies directly to the south west and the Derbyshire Borough of High Peak lies directly to the south east, but Derbyshire is only bordered by high moorland near Black Hill and is not accessible by road. History Following both the Local Government Act 1888 and Local Government Act 1894, local government in England had been administered via a national framework of r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blanket Bog
Blanket bog or blanket mire, also known as featherbed bog, is an area of peatland, forming where there is a climate of high rainfall and a low level of evapotranspiration, allowing peat to develop not only in wet hollows but over large expanses of undulating ground. The blanketing of the ground with a variable depth of peat gives the habitat type its name. Blanket bogs are found extensively throughout the northern hemisphere - well-studied examples are found in Ireland and Scotland, but vast areas of North American tundra also qualify as blanket bogs. In Europe, the southernmost edge of range of this habitat has been recently mapped in the Cantabrian Mountains, northern Spain, but the current distribution of blanket bogs globally remains unknown. In the southern hemisphere they are less well-developed due to the relatively low latitudes of the main land areas, though similar environments are reported in Patagonia, the Falkland Islands and New Zealand. The blanket bogs known as 'f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Freedom To Roam
The freedom to roam, or "everyman's right", is the general public's right to access certain public or privately owned land, lakes, and rivers for recreation and exercise. The right is sometimes called the right of public access to the wilderness or the "right to roam". In Scotland, Finland, Iceland, Norway, Sweden, Estonia, Latvia, Lithuania, Belarus, Austria, Czech Republic and Switzerland, the freedom to roam takes the form of general public rights which are sometimes codified in law. The access is ancient in parts of Northern Europe and has been regarded as sufficiently basic that it was not formalised in law until modern times. However, the right usually does not include any substantial economic exploitation, such as hunting or logging, or disruptive activities, such as making fires and driving offroad vehicles. In countries without such general rights, there may be a network of rights of way, or some nature reserves with footpaths. Europe Nordic countries Ancient traces p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peat
Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of , which is the average depth of the boreal orthernpeatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. ''Sphagnum'' moss, also called peat moss, is one of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry Stone Wall
Dry stone, sometimes called drystack or, in Scotland, drystane, is a building method by which structures are constructed from stones without any mortar to bind them together. Dry stone structures are stable because of their construction method, which is characterized by the presence of a load-bearing façade of carefully selected interlocking stones. Dry stone construction is best known in the context of stone walls, traditionally used for the boundaries of fields and churchyards, or as retaining walls for terracing, but dry stone sculptures, buildings, bridges, and other structures also exist. The term tends not to be used for the many historic styles which used precisely-shaped stone, but did not use mortar, for example the Greek temple and Inca architecture. The art of dry stone walling was inscribed in 2018 on the UNESCO representative list of the intangible cultural heritage of humanity, for dry stone walls in countries such as France, Greece, Italy, Slovenia, Cro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gritstone
Gritstone or grit is a hard, coarse-grained, siliceous sandstone. This term is especially applied to such sandstones that are quarried for building material. British gritstone was used for millstones to mill flour, to grind wood into pulp for paper and for grindstones to sharpen blades. "Grit" is often applied to sandstones composed of angular sand grains. It may commonly contain small pebbles. " Millstone Grit" is an informal term for a succession of gritstones which are to be found in the Pennines (including the Peak District) of northern England. These sediments were laid down in the late (upper) Paleozoic era, in the Carboniferous period, in deltaic conditions. The Millstone Grit Group is a formal stratigraphic term for this sequence of rocks. The gritstone edges of the Peak District are an important climbing area and the rock is much relished by English climbers, among whom it has almost cult status and is often referred to as "God's own rock". The rough surface provide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holme Moss
Holme Moss ( a.s.l.) is high moorland on the border between the Holme Valley district of Kirklees in West Yorkshire and the High Peak district of Derbyshire in England. Historically on the boundary between the West Riding of Yorkshire and Cheshire, it is just inside the boundary of the Peak District National Park. The A6024 road between Holmfirth and Longdendale crosses the moor near its highest point close to Holme Moss transmitting station's prominent mast. Watershed Water seeping from the surrounding moorland into Rake Dike is the source of the River Holme. Rake Dike rising from Kay Edge on the moor flows through the village of Holme into Brownhill Reservoir, about a mile below the moor, and passes down through the Holme Valley to Huddersfield, where it flows into the River Colne. The upper part of the moor continues into Black Hill which is crossed by the Pennine Way north–south footpath. Transmitting station Holme Moss transmitting station is the highest in Engl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Hill (Peak District)
Black Hill, in the Peak District, is the highest hill in West Yorkshire, England. Its summit has a maximum elevation of above sea level. It is surpassed in height by only two other major summits in the Peak District (Kinder Scout and Bleaklow). Black Hill is a typical Pennine moorland mountain, with a very flat and extensive plateau (but steeper sides). The top is peaty, poorly drained, and thus very boggy after rain. The area surrounding the summit itself had virtually no vegetation and was very dark, giving the hill an appropriate name. However, recent restoration work has eliminated much of the exposed peat. Black Hill is crossed by the Pennine Way whose now-paved surface allows walkers to reach the top dry-shod even in the wettest of weather. Black Hill was the highest point (county top) of the historic county of Cheshire, lying at the tip of what was once known as the Cheshire Panhandle, a long projection of the county which lay to the north of the reservoir filled valle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wessenden Valley
The Wessenden Valley is a moorland valley in the Dark Peak, immediately south of Marsden in West Yorkshire, England. The name Wessenden derives from Old English and means the 'valley with rock suitable for whetstones'. The valley was formed by retreating glaciers at the end of the last ice age and continues to be cut by the Wessenden Brook a tributary of the River Colne with a catchment of . The valley is in the Marsden Moor Estate and occupied by four reservoirs, namely Wessenden Head, Wessenden, Blakeley and Butterley, the largest. The Kirklees Way and Pennine Way The Pennine Way is a National Trail in England, with a small section in Scotland. The trail stretches for from Edale, in the northern Derbyshire Peak District, north through the Yorkshire Dales and Northumberland National Park and ends at Kir ... long-distance footpaths follow the valley. The upper part of the valley near Wessenden Head is managed by the National Trust as part of the Marsden Moor Estate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Public House
A pub (short for public house) is a kind of drinking establishment which is licensed to serve alcoholic drinks for consumption on the premises. The term ''public house'' first appeared in the United Kingdom in late 17th century, and was used to differentiate private houses from those which were, quite literally, open to the public as "alehouses", "taverns" and "inns". By Georgian times, the term had become common parlance, although taverns, as a distinct establishment, had largely ceased to exist by the beginning of the 19th century. Today, there is no strict definition, but CAMRA states a pub has four characteristics:GLA Economics, Closing time: London's public houses, 2017 # is open to the public without membership or residency # serves draught beer or cider without requiring food be consumed # has at least one indoor area not laid out for meals # allows drinks to be bought at a bar (i.e., not only table service) The history of pubs can be traced to Roman taverns in B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Yorkshire Urban Area
The West Yorkshire Built-up Area, previously known as the West Yorkshire Urban Area is a term used by the Office for National Statistics (ONS) to refer to a conurbation in West Yorkshire, England, based on the cities of Leeds, Bradford and Wakefield, and the large towns of Huddersfield and Halifax. It is the 4th largest urban area in the United Kingdom. However, it excludes other towns and villages such as Featherstone, Normanton, Castleford, Pontefract, Hemsworth, Todmorden, Hebden Bridge, Knottingley and Wetherby Wetherby () is a market town and civil parish in the City of Leeds district, West Yorkshire, England, close to West Yorkshire county's border with North Yorkshire, and lies approximately from Leeds City Centre, from York and from Harrogat ... which, though part of the county of West Yorkshire are considered independently. There are substantial areas of agricultural land within the designated area – more than in any other official urban area in England – m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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