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River Rye, Yorkshire
The River Rye in the English county of North Yorkshire rises just south of the Cleveland Hills, east of Osmotherley, and flows through Hawnby, Rievaulx, Helmsley, Nunnington, West and East Ness, Butterwick, Brawby, and Ryton, before joining the River Derwent at near Malton. The river valley (dale) gave its name to the Ryedale shire district, which extends southwest into the Vale of Pickering along the River Derwent. Course The river rises at Rye Head near Snilesworth Lodge on Snilesworth Moor in the Cleveland Hills and collects the River Seph which flows along Bilsdale. It passes Rievaulx Abbey and enters the Vale of Pickering at Helmsley. In its eastward course from Helmsley, the Rye receives the River Dove from Farndale which has previously added the Hodge Beck from Bransdale. Hodge Beck is partly swallowed by the limestone aquifer in Kirkdale and issues again further down the valley. Kirkbymoorside is on the River Dove which, like Hodge Beck has a partly sub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cleveland Hills
The Cleveland Hills are a range of hills on the north-west edge of the North York Moors in North Yorkshire, England, overlooking Cleveland, England, Cleveland and Teesside. They lie entirely within the boundaries of the North York Moors National Park. Part of the long Cleveland Way National Trail runs along the hills, and they are also crossed by a section of Alfred WainwWainwright's Coast to Coast Walk. The hills, which rise abruptly from the flat Tees Valley to the north, include distinctive landmarks such as the cone-shaped peak of Roseberry Topping, near the village of Great Ayton – childhood home of Captain James Cook. Geology The hills are formed by multiple stacked layers of Jurassic age sedimentary rocks. The scarp rises above the low ground to the north and west formed by the mudstones of the Redcar Mudstone Formation, though largely buried beneath glacial till from the Last Glacial Period, last ice age. The same formation also provides the lowermost slopes of the sc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Church Bridge At Hawnby After The Rebuild - Geograph
Church may refer to: Religion * Church (building), a building for Christian religious activities * Church (congregation), a local congregation of a Christian denomination * Church service, a formalized period of Christian communal worship * Christian denomination, a Christian organization with distinct doctrine and practice * Christian Church, either the collective body of all Christian believers, or early Christianity Places United Kingdom * Church (Liverpool ward), a Liverpool City Council ward * Church (Reading ward), a Reading Borough Council ward * Church (Sefton ward), a Metropolitan Borough of Sefton ward * Church, Lancashire, England United States * Church, Iowa, an unincorporated community * Church Lake, a lake in Minnesota Arts, entertainment, and media * '' Church magazine'', a pastoral theology magazine published by the National Pastoral Life Center Fictional entities * Church (''Red vs. Blue''), a fictional character in the video web series ''Red vs. Blue'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North York Moors
The North York Moors is an upland area in north-eastern Yorkshire, England. It contains one of the largest expanses of heather moorland in the United Kingdom. The area was designated as a National Park in 1952, through the National Parks and Access to the Countryside Act 1949. Covering an area of , the National Park has a population of 23,380. It is administered by the North York Moors National Park Authority, whose head office is based in Helmsley. Location and transport To the east the area is clearly defined by the impressive cliffs of the North Sea coast. The northern and western boundaries are defined by the steep scarp slopes of the Cleveland Hills edging the Tees lowlands and the Hambleton Hills above the Vale of Mowbray. To the south lies the broken line of the Tabular Hills and the Vale of Pickering. Four roads cross the North York Moors from north to south. In the east the A171 joins Whitby and Scarborough. Further inland, the A169 runs between Pickering and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pickering Beck
Pickering Beck is a river that runs for over from its source in the North York Moors National Park through the town of Pickering and on to its confluence with Costa Beck at Kirby Misperton. It is a meandering river that is fed by numerous named and unnamed becks and streams which flow over sandstone and limestone beds and an alluvia of sand, clay silt and gravel. The beck is known for flooding and in recent times has been a beneficiary of funding and experimental flood protection schemes. History The valley that Pickering Beck inhabits was carved by glacial melt water before the late Devensian period of history. It was initially thought to be a drainage channel for a glacial lake, either by two ice sheets abutting and the waters reaching the same height as the surrounding ice sheets (about above sea level), or as a simple drainage channel for the meltwater when the temperatures rose. Either way, the deep meandering channel has been estimated to have been carved by water flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newton Dale
Newton Dale is a narrow dale within the North York Moors National Park in North Yorkshire, England. It was created by meltwater from a glacier carving the narrow valley. Water still flows through the dale and is known as Pickering Beck. The dale starts between Goathland Moor and Lockton High Moor where water runs southwards towards Pickering. In its upper reaches, the dale is very twisting and deep with the floor of the dale being above sea level. The dale is spelt either Newtondale or Newton Dale. Ordnance Survey maps and the North York Moors Railway refer to it as ''Newton Dale''. History The dale was carved out by a massive amount of water charging through it in the last ice age. At the start of the twentieth century, Percy Kendall suggested that several massive glacial lakes at what is now the watershed between Eller Beck, the River Derwent and Pickering Beck effectively dammed the water and it was released at a torrent to carve the dale. It has been estimated that a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rosedale, North Yorkshire
Rosedale is a valley located almost in the centre of the North York Moors national park in North Yorkshire, England. The nearest town is Kirkbymoorside, some to the south. Rosedale is surrounded by moorland. To the north-west sits Blakey Ridge at over above sea level. At Dale Head is the source of the River Seven,which flows down the valley to join the River Rye at Little Habton near Malton. At its southern end Rosedale is squeezed between Spaunton Moor and Hartoft Rigg, where the river flows out through Forestry Commission woodland before passing the village of Cropton to reach the plains of the Vale of Pickering. Few inhabitants of Rosedale work in farming. The majority of houses are bought as second homes and as such the permanent local population has been significantly reduced. In the late 19th century the valley quickly became a major centre for iron-ore extraction, which gave rise to the modern village of Rosedale Abbey, built around the site of a former Cist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kirkdale, North Yorkshire
Kirkdale is a valley in North Yorkshire, England, which along with Sleightholmedale makes up the larger Bransdale and carries the Hodge Beck from its moorland source near Cockayne to the River Dove and onto the River Rye in the Vale of Pickering. Corallian Limestone which outcrops on the hills surrounding the Vale of Pickering runs across the region, and this appears as an aquifer in Kirkdale swallowing most of the water from Hodge Beck, which reappears further downstream. During summer months the river bed often runs dry as most of the water takes a subterranean passage. Kirkdale is noted for a bone cave, an ancient animal den, into which scavengers such as hyenas dragged the remains of many other animals. Numerous bones can still be found in the cave today. History Although there is no village in the dale, Kirkdale was the centre of a large ancient parish. The Saxon parish church of St Gregory's Minster stands by the river. It was built in 1055 on the site of an e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bransdale
Bransdale is a valley running south through North Yorkshire, England, and part of the North York Moors National Park. Sandwiched between Bilsdale to the west and Farndale to the east, it is formed from the dales of Bransdale itself at the top of the valley, Sleightholmedale and Kirkdale. It carries a river called Hodge Beck en route from Cockayne to the River Dove from Farndale of Kirkbymoorside, which runs on into the Vale of Pickering and the River Rye. Bransdale is also a civil parish in the Ryedale district of North Yorkshire, England. History Bransdale was historically divided between two ancient parishes. Bransdale Westside was a township in the parish of Kirkdale. Bransdale Eastside was part of the township of Farndale High Quarter (also known as Farndale Westside) in the parish of Kirkbymoorside Kirkbymoorside () is a market town and civil parish in the Ryedale district in North Yorkshire, England. It is north of York, It is also midway between Pic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hodge Beck
Hodge Beck is a stream that flows through the North York Moors national park in North Yorkshire, England. It is a tributary of the River Dove which it joins near Welburn south of Kirkbymoorside. The beck is long and has a total catchment area of . Course The beck rises on the flanks of Round Hill in the Cleveland Hills of the North York Moors and flows south through Bransdale to reach Cockayne where it is joined by Bloworth Slack. It continues south to meet Ouse Gill, another tributary before it flows through Sleightholme Dale and Kirkdale where it is forded by a minor road. The beck often runs dry at this point as it disappears into the local limestone bedrock in the summer months. Near the Kirkdale ford, is Kirkdale Cave, where the fossilised remains of Pleistocene megafauna were found. On leaving Kirkdale, it is bridged by the A170, and the original A road crossing at Tilehouse Bridge, near Welburn, where it passes Welburn Hall. It continues past Slingsby Aviation ai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Farndale
Farndale is a valley and community in Ryedale district, North Yorkshire, England, which is known for the daffodils which flower each spring along a stretch of the River Dove. The valley is in the North York Moors National Park, some north of Kirkbymoorside, the nearest town. Pickering is some to the south-east and Helmsley to the south-west. The combined population of the civil parishes of Farndale East and Farndale West was 207 in 2011, and was estimated to have dropped to 180 by 2015. Farndale is an isolated, scattered agricultural community with traditional Yorkshire dry stone walls. The valley is popular with walkers due to its famous wild daffodils, which can be seen around Easter time all along the banks of the River Dove. To protect the daffodils the majority of Farndale north of Lowna was created a Local Nature Reserve in 1955. Farndale is home to two hamlets; Church Houses at the top of the valley and Low Mill further down. Low Mill is a tourist honey ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Dove, North Yorkshire
The River Dove is a river in North Yorkshire, England. It rises on the North York Moors and flows south to join the River Rye, itself a tributary of the River Derwent. The upper valley of the river is known as Farndale. The name is of Brittonic Celtic origin, meaning "dark river". Its principal tributary is the Hodge Beck. Course The river flows through Farndale south-east past several small settlements to Church Houses. Here it turns south and continues meandering past Low Mill to Lowna. At Gillamoor it heads south-east again past Hutton-le-Hole before returning southwards past Ravenswick and to the east of Kirkbymoorside. It continues past Keldholme and Kirkby Mills to Great Edstone. From there it flows south south-east to where it joins the River Rye in the Vale of Pickering near the village of Salton. The Environment Agency have a gauging station at Kirkby Mills where the average low river level is and the high river level with a record high level of . The recor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vale Of Pickering
The Vale of Pickering is a low-lying flat area of land in North Yorkshire, England. It is drained by the River Derwent. The landscape is rural with scattered villages and small market towns. It has been inhabited continuously from the Mesolithic period. The present economy is largely agricultural with light industry and tourism playing an increasing role. Location and transport The Vale of Pickering is a low-lying plain, orientated in an east–west direction. It is well defined by the Yorkshire Wolds escarpment to the south, the Corallian limestone foothills of the North York Moors to the north, the North Sea coast to the east and the Howardian Hills to the west. The east–west-orientated main roads ( A64 and A170) in the vale follow the shoreline of the glacial lake, which formed in the vale after the last ice age. The main A169 road crosses the vale in a north–south direction, joining the market towns of Malton and Pickering. At the eastern edge of the vale the A165 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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