|
Roaches Grit
{{no footnotes, date=July 2010 Roaches Grit is a coarse sandstone which outcrops widely throughout the western part of the Peak District of northern England and gives rise to several significant landscape features in the area. Its counterpart in the eastern part of the National Park is the Ashover Grit. The combined Roaches Grit and Ashover Grit are amongst the most widespread sandstone units within the Millstone Grit Group of the Peak District. Along with other similar sandstones, such as the immediately overlying Chatsworth Grit, it is assigned to the Marsdenian sub-stage of the Namurian stage within the Carboniferous period. The two units which, prior to the doming and erosion of the central Peak District were once one, are interpreted as delta-top sandstones. The deposited material was brought down from a northerly source by braided rivers. Landscape features Amongst the features for which the Roaches Grit is responsible are Axe Edge, The Roaches, Hen Cloud, Ramshaw Rock ... [...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] |
The Roaches
The Roaches (from the French ''les roches'' - the rocks) is a prominent rocky ridge above Leek and Tittesworth Reservoir in the Staffordshire Peak District of England. The ridge with its rock formations rises steeply to . Along with Ramshaw Rocks and Hen Cloud they form a gritstone escarpment, which is popular with hikers, rock climbers and freerunners. It is often very busy especially at weekends. The Roaches Estate which includes Hen Cloud was purchased by the Peak District National Park Authority in the 1980s to safeguard the area from adverse development. From May 201Staffordshire Wildlife Trusttook on the management of the Roaches Estate. In clear conditions, it is possible to see much of Cheshire and views stretching as far as Snowdon in Wales and Winter Hill in Lancashire. The Roaches are the most prominent part of a curving ridge which extends for several miles from Hen Cloud in the south to Back Forest and Hangingstone in the northwest. At the top there is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baslow
Baslow is a village in Derbyshire, England, in the Peak District, situated between Sheffield and Bakewell, just over north of Chatsworth House. It is sited by the River Derwent, which is spanned by a 17th-century bridge, alongside which is a contemporary toll house. Baslow village is composed of several distinct areas: Bubnell, Bridge End, Over End and Nether End. The village's civil parish is called Baslow and Bubnell, which in the 2011 census had a population of 1,178. History St Anne's Church has a Saxon coffin lid in the porch entrance, but the oldest part of the current building, the north aisle, dates from about 1200. The tower was constructed in the 13th century but the rest of the church is newer and was the subject of an extensive restoration in the 19th century. A sundial lies in the church grounds, atop the shaft, base and steps of a cross. This may have acted as a market cross in the 17th century. A second cross lies in the graveyard, moved from Bubnell by Doct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edensor
Edensor (pronounced ) is a village and civil parish in Derbyshire, England. The population of the civil parish at the 2011 census was 145. Much of the village is privately owned, by the Dukes of Devonshire, the Cavendish family. Most of the deceased of the family are buried in the churchyard of St Peter's Church. History A village near this location was included in the Domesday Book of 1086. At that time, it was owned by Henry de Ferrers and included ten villagers plus seven "smallholders". One report describes the area in the early 1700s as: "it straggled across towards the river Derwent in front of Chatsworth, skirting the hill opposite the village known as 'The Crobbs'." In 1762 the 4th Duke of Devonshire of Chatsworth House arranged for the demolition of several buildings because they intruded on his view of the parkland that had been created by Capability Brown. In the 1800s, a new road was being built and the Duke arranged to have the rest of the village removed. A new vi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Robin Hood's Stride
Robin Hood's Stride (also known as Mock Beggar's Mansion) is a rock formation on the Limestone Way in Derbyshire close to the village of Elton. The nearest town is Bakewell, to the north. The popular tourist spot can be accessed via the Limestone Way just off the B5056 between Haddon Hall and Winster, or from the unclassified road from Alport to Elton using either the Limestone Way, a concessionary footpath or Access Land. Both options have limited parking at the side of the road. It consists of gritstone boulders deeply seamed by water flows. Limited short climbing is possible; nearby Cratcliffe Tor provides more serious routes. The two "pinnacles" are Weasel pinnacle (eastern end; Diff) and Inaccessible pinnacle (west; V Diff). An ancient road, possibly prehistoric or Roman, the Derbyshire Portway (also known as Old Manchester Lane and The Chariot Way) passed close to the outcrop. Nearby is Nine Stones Close, a four-stone circle, and, at Cratcliffe Tor, a rock shelter kn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harthill Moor
Harthill Moor is a small upland area in the Derbyshire Peak District of central and northern England, lying between Matlock and Bakewell near the villages of Birchover and Elton. The moor is within the southern portion of Harthill civil parish. Its highest point is above sea level. The River Bradford flows along the northern edge of the moor past Youlgreave and into the River Lathkill at Alport. Harthill Moor is a rich prehistoric landscape with several protected Scheduled Ancient Monuments. The rock of Harthill Moor and nearby Stanton Moor is known as Ashover Grit, an outlier of Millstone Grit. This is a coarse-grained sandstone which weathers to produce coarse sub-soils, rich in sand, and the soils themselves are typically podzols. The Ashover Grit sandstone layer lies on top of shale, which in turn lie upon Carboniferous limestone. Robin Hood's Stride (also called Mock Beggar Hall) is a prominent natural rock formation with distinctive pinnacle towers. Prehistoric ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stanton Moor
Stanton Moor is a small upland area in the Derbyshire Peak District of central northern England, lying between Matlock and Bakewell near the villages of Birchover and Stanton-in-Peak. It is known for its megaliths – particularly the Nine Ladies stone circle – and for its natural, wind-eroded sandstone pillars. The Peak District Boundary Walk runs across the moor. Geology Stanton Moor consists of an outlier of Millstone Grit, known as Ashover Grit. This is a coarse-grained sandstone which weathers to produce coarse sub-soils, rich in sand, and the soils themselves are typically podzols. The Ashover Grit sandstone layer lies on top of shale, which in turn lie upon Carboniferous limestone. The whole of the moor is of geological interest as a syncline. Several large, wind-eroded pillars of sandstone are found around the edge of Stanton Moor, and form significant features of its topography. From north, clockwise, these outcrops are the Duke of York Stone (in which the legend ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shutlingsloe
Shutlingsloe is a hill near the village of Wildboarclough, in the east of the county of Cheshire. It stands to the south of Macclesfield Forest, on the edge of the Peak District and within the Peak District National Park.Cheshire County Council: Landscape Character Type 20: Moorland Plateau (2007) (accessed 19 April 2010) A steep-sided hill with a distinctive profile, sometimes described as the ' of Cheshire', it is the third highest peak in the historic county ( [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lud's Church
Lud's Church (sometimes written as Ludchurch) is a deep chasm penetrating the Millstone Grit bedrock created by a massive landslip on the hillside above Gradbach, Staffordshire, England. It is located in a wood known as Back Forest, in the Dark Peak, towards the southwest fringe of the Peak District National Park about west of the A53 between Leek and Buxton. Over long and deep, all but the upper third of the slope has slipped forward towards the River Dane. It is mossy and overgrown, wet and cool even on the hottest of days. Geological origins Lud's Church is formed within the thick bed of coarse Carboniferous sandstone known as the Roaches Grit which here dips northeastwards into the Goyt Syncline. The rocks of this area are traversed by numerous roughly northwest-to-southeast-oriented faults and fracture planes. In addition, weak layers of mudstone exist within the sequence. It is along such lines of weakness that a large mass of the Roaches Grit bounding the northeast sid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Back Forest
The human back, also called the dorsum, is the large posterior area of the human body, rising from the top of the buttocks to the back of the neck. It is the surface of the body opposite from the chest and the abdomen. The vertebral column runs the length of the back and creates a central area of recession. The breadth of the back is created by the shoulders at the top and the pelvis at the bottom. Back pain is a common medical condition, generally benign in origin. Structure The central feature of the human back is the vertebral column, specifically the length from the top of the thoracic vertebrae to the bottom of the lumbar vertebrae, which houses the spinal cord in its spinal canal, and which generally has some curvature that gives shape to the back. The ribcage extends from the spine at the top of the back (with the top of the ribcage corresponding to the T1 vertebra), more than halfway down the length of the back, leaving an area with less protection between the bottom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
