1.
Swaledale
–
Swaledale is one of the northernmost dales in the Yorkshire Dales National Park in northern England. It is the dale of the River Swale on the east side of the Pennines in North Yorkshire. Swaledale runs broadly from west to east, from the moors on the Cumbria–Yorkshire boundary at the watershed of Northern England to the market town of Richmond. Nine Standards Rigg, the prominent ridge with nine ancient tall cairns, to the south and east of the ridge a number of smaller dales join to form the narrow valley of upper Swaledale at the small village of Keld. From there, the valley runs south then turns east at Thwaite to broaden progressively as it passes Muker, Gunnerside, Low Row, Healaugh. The Pennine valley ends at Richmond, where an important medieval castle still watches the important ford from the top of a cliff. Below Richmond, the valley sides flatten out and the Swale flows across lowland farmland to meet the Ure just east of Boroughbridge at a point known as Swale Nab, the Ure becomes the Ouse, and eventually the Humber. From the north, Arkengarthdale and its river the Arkle Beck join Swaledale at Reeth, to the south, Wensleydale, home of the famous Wensleydale cheese, runs parallel with Swaledale. The two dales are separated by a ridge including Great Shunner Fell, and joined by the road over Buttertubs Pass, the upper parts of the dale are particularly striking because of its large old limestone field barns and its profusion of wild flowers. The latter are thanks to the return to the practice of leaving the cutting of grass for hay or silage until wild plants have had a chance to seed. Occasionally visible from the valley bottom road are the slowly fading fellside scars of the 18th and 19th century lead mining industry, ruined stone mine buildings remain, taking on the same colours as the landscape into which they are crumbling. Swaledale is home to small but beautiful waterfalls, such as Richmond Falls, Kisdon Force. Sheep-farming has always been central to life in Swaledale, which has lent its name to a breed of round-horned sheep. Traditional Swaledale products are woollens and Swaledale cheese, which was made from ewe’s milk. These days it is made from cow’s milk, during the 19th century, a major industry in the area was lead mining. Today, tourism has become important, and Swaledale attracts thousands of visitors a year and it is very popular with walkers, particularly because the Coast to Coast Walk passes along it. In May and June every year, Swaledale hosts the two-week-long Swaledale Festival, which combines a celebration of small-scale music, Swaledale Festival Swaledale Museum Swaledale and Arkengarthdale Archaeology Group
2.
Carboniferous Limestone
–
These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones, within Great Britain the suite of rocks known traditionally as the Carboniferous Limestone Series was deposited as marine sediments in three distinct ‘provinces’ separated by contemporary landmasses. One of these landmasses was the Wales-London-Brabant Massif, an east-west aligned belt of land stretching through central Wales and these rocks continue eastwards at depth beneath Oxfordshire. It is characterised by the presence of numerous ‘blocks’ and ‘basins’ each with its own particular depositional style, to the north of the Southern Uplands are the limestones of the Scottish Midland Valley stretching from Ayrshire and Arran in the west to Fife, Lothian and Berwickshire in the east. Though of Carboniferous age, the limestones of this Scottish province are not assigned to the Carboniferous Limestone Supergroup, the Carboniferous Limestone is widespread throughout Ireland. The Carboniferous Limestone is a significant landscape-forming rock unit in each of the provinces of Great Britain within which it is found. It forms prominent headlands such as those of Stackpole Head and Lydstep Point and it is here referred to as the ‘north crop’ as distinct from a sub-parallel outcrop, the ‘south crop’ which defines the southern rim of the South Wales Coalfield. The outcrop continues through Ystradfellte to Pontneddfechan, Penderyn and Pontsticill and it then runs near the southern margin of the national park via Trefil and the Llangattock escarpment to Blorenge where it turns southwards. A very narrow ‘east crop’ and ‘south crop’ run by Cwmbran and it turns west again to meet Swansea Bay at Porthcawl. West of the bay, the forms the renowned southern coast of Gower between Mumbles Head and Worms Head. There are further occurrences in the Vale of Glamorgan, both inland and on the coast, an important outlier is that of the Forest of Dean basin which forms the cliffs of the Wye Valley, straddling the England/Wales border and extends southwestwards through Chepstow to Undy. The larger part of the Mendip Hills are formed from Carboniferous Limestone, showing notable geomorphological features, including Cheddar Gorge, Burrington Combe, the Avon Gorge west of Bristol and the coastal cliffs at Clevedon and Weston-super-Mare are cut in this rock. The limestone islands of Flat Holm and Steep Holm are prominent in views across the mouth of the Severn Estuary, there are limited outcrops on the Isle of Man and more extensive ones in Anglesey notably along the Menai Strait, around Benllech and towards Puffin Island. The Carboniferous Limestone belt extends eastwards to from the Great Orme at Llandudno, the neighbouring Little Orme, there are a few outcrops in Shropshire such as Titterstone Clee Hill and at Little Wenlock. The White Peak is named for the limestone which characterises the heart of the Peak District and through deep gorges have been cut by rivers such as the Wye, Dove. The limestone is concealed beneath younger rocks to the east and west, to the north the limestone is exposed once again in east Lancashire and in the Yorkshire Dales. An outcrop extends from Kirkby Stephen along the side of the Vale of Eden. North again, it is a major landscape forming feature in the North Pennines, there are scattered outcrops along the north coast of the Solway Firth
3.
Panorama
–
A panorama is any wide-angle view or representation of a physical space, whether in painting, drawing, photography, film, seismic images or a three-dimensional model. The word was coined in the 18th century by the English painter Robert Barker to describe his panoramic paintings of Edinburgh. The motion-picture term panning is derived from panorama, a panoramic view is also purposed for multi-media, cross-scale applications to an outline overview along and across repositories. This so-called cognitive panorama is a view over, and a combination of. The device of the panorama existed in painting, particularly in murals, as early as 20 A. D. in those found in Pompeii, cartographic experiments during the Enlightenment era preceded European panorama painting and contributed to a formative impulse toward panoramic vision and depiction. In the mid-19th century, panoramic paintings and models became a popular way to represent landscapes, topographic views. Audiences of Europe in this period were thrilled by the aspect of illusion, immersed in a winding 360 degree panorama, the panorama was a 360-degree visual medium patented under the title Apparatus for Exhibiting Pictures by the artist Robert Barker in 1787. The earliest that the word appeared in print was on June 11,1791 in the British newspaper The Morning Chronicle. The inaugural exhibition, a View of Edinburgh, was first shown in that city in 1788, by 1793, Barker had built The Panorama rotunda at the center of Londons entertainment district in Leicester Square, where it remained until closed in 1863. Large scale installations enhance the illusion for an audience of being surrounded with a real landscape, the Bourbaki Panorama in Lucerne, Switzerland was created by Edouard Castres in 1881. The painting measures about 10 metres in height with a circumference of 112 meters, in the United States of America is the Atlanta Cyclorama, depicting the Civil War Battle of Atlanta. It was first displayed in 1887, and is 42 feet high by 358 feet circumference, also on a gigantic scale, and still extant, is the Racławice Panorama located in Wrocław, Poland, which measures 15 x 120 metres. In addition to historical examples, there have been panoramas painted and installed in modern times, prominent among these is the Velaslavasay Panorama in Los Angeles. Panoramic photography soon came to painting as the most common method for creating wide views. Not long after the introduction of the Daguerreotype in 1839, photographers began assembling multiple images of a view into a wide image. Pinhole cameras of a variety of constructions can be used to make panoramic images and this generates an egg-shaped image with more than 180° view. They could run autonomously with silent synchronization pulses to control projector advance and fades, precisely overlapping slides placed in slide mounts with soft-edge density masks would merge seamlessly on the screen to create the panorama. Cutting and dissolving between sequential images generated animation effects in the panorama format, digital photography of the late twentieth century greatly simplified this assembly process, which is now known as image stitching
4.
Malham
–
Malham is a village and civil parish in the Craven district of North Yorkshire, England. Before 20th century boundary changes, the village was part of the Settle Rural District, in the Domesday Book, the name is given as Malgun, meaning settlement by the gravelly places. In 2001 the parish had a population of approximately 150, Malham parish increased in size geographically and so at the 2011 Census had a population of 238. Malham lies at the end of the valley of the River Aire, known above Airton as Malhamdale. The surrounding countryside is known for its limestone pavements and other examples of limestone scenery. Tourist attractions include Malham Tarn, Malham Cove, Gordale Scar, Janets Foss, the village hosts an annual agricultural and horticultural show on the Saturday before the August Bank Holiday. Known as the Malham Show, it has competitions for everything from Lego models to fell running, another major annual event is the Malham Safari, when the villagers and particularly the local school build sculptures around the village. This event attracts tourists and stalls are put up on the green. Malham is a popular walkers destination, the footpaths in the area are maintained by the Yorkshire Dales National Park Authority. In the village there is a National Park Information Centre and a car park. The Pennine Way long distance path passes through the village, nearby natural landmarks include Malham Cove, Malham Tarn, Gordale Scar and Janets Foss. The Malham Show Fell Race course runs over the nearby 301-metre Cawden, in May 2006, it was reported that a covert listening device was discovered hidden in the local parish hall, leaving the villagers baffled. The electronic transmitter was found in a wall socket during a safety inspection at Malham village hall, Part of Harry Potter and the Deathly Hallows Part 1 was filmed around the Malham Cove limestone pavement. In the 1950s the village gave its name to a Ham class minesweeper, Malham has a joint parish council, Kirkby Malhamdale Parish Council, with the parishes of Malham Moor, Kirkby Malham and Hanlith. Malham has an Oceanic climate, but is generally colder and wetter than most settlements in Britain and it has a relatively low altitude of around 200 metres, but is partly surrounded by fells. This exposed position means the range is limited, due to little pooling of cold air. Extremes of temperature range from 28.2 °C during August 1990, Malham Tarn Field Studies Centre Village and area web site Malham and district information/history pages
5.
Ingleborough
–
Ingleborough is the second-highest mountain in the Yorkshire Dales, at 723 metres. It is one of the Yorkshire Three Peaks, the two being Whernside, at 736 metres, and Pen-y-ghent, at 694 metres. Ingleborough is frequently climbed as part of the Yorkshire Three Peaks Challenge, if done anti-clockwise Ingleborough is the last mountain climbed, and ascent is from Chapel-le-Dale. The second part of the name Ingleborough is derived from the Old English word burh, meaning a place, in this case. On the top of Ingleborough the remains of an old walled enclosure have been discovered inside which foundations of Iron Age huts have been found. Ingleborough is situated in the corner of the Yorkshire Dales, being at the highest point of a large triangle of land with corners at Ingleton, Ribblehead. The hill is connected to its nearest higher neighbour, Whernside, Ingleborough throws out a ridge to the north-east which develops into a summit, Simon Fell, and another summit further down, Park Fell. On the slopes of the former are the famed Norber Boulders, continuing south-east the high land is broken by a divide which carries the minor road from Austwick to Helwith Bridge. On the other side of the divide rises the low summit of Smearsett Scar along with its subsidiaries, Pot Scar and Giggleswick Scar, on the western side of Ingleborough is a large limestone plateau appropriately known as White Scars, below which White Scar Caves run for 4 miles. The entrance series of these has developed as a show cave. The plateau is bounded by Raven Scar, the longest unbroken cliff in the district, on the southern side is a similar plateau, this one containing potholes such as Fluted Hole and Pillar Hole. The plateau to the north of Norber, a known as The Allotment, is particularly rich in potholes, one of these, Long Kin East, can be followed by all. Also located here is Juniper Gulf, which descends 420 feet underground through an arduous rift, the Smearsett Scar region is not devoid of interesting features either, here can be found the Celtic Wall, the Ebbing and Flowing Well and a glacial hollow known as the Happy Valley. There are several popular hillwalking routes to its summit, the most frequently-used starting point is probably the village of Ingleton, which lies about 4 miles to the southwest. An ascent from here is about 7 1⁄2 miles there and back, the route follows a walled lane, Fell Lane, before emerging onto a flat area, Crina Bottom, scattered with potholes including the considerable Quaking Pot. A steep climb through the limestone cliffs leads to the summit, the hill may also be climbed from Horton in Ribblesdale 6 miles to the east, following a route crossing extensive areas of limestone pavement in the region of Sulber Nick. This is the route of descent of the Three Peaks Walk and has been improved by the National Trust after going in just thirty years from no path at all to a serious example of footpath erosion. Another route on this flank is from the farmstead of Crummack
6.
Pennines
–
The Pennines /ˈpɛnaɪnz/, also known as the Pennine Chain or Pennine Hills, are a range of mountains and hills in Northern England separating North West England from Yorkshire and North East England. The Pennines are an important water catchment area with numerous reservoirs in the streams of the river valleys. The region is considered to be one of the most scenic areas of the United Kingdom. The North Pennines and Nidderdale are designated Areas of Outstanding Natural Beauty, as are Bowland, parts of the Pennines are incorporated into the Peak District National Park, the Yorkshire Dales National Park and the Northumberland National Park. Britains oldest long-distance footpath, the Pennine Way, runs along most of the Pennine Chain and is 268 miles long, various etymologies have been proposed treating Pennine as though it were a native Brittonic/Modern Welsh name related to pen-. He found that the derivation from Bertram was widely believed and considered uncomfortable, in fact, he found repeated comparisons going back at least as early as Camden, many of whose placenames and ideas Bertram incorporated into his work. Bertram was responsible with popularizing the name against other such as Daniel Defoes English Andes. His own form of the name was the Pennine Alps, which today is used for a section of the continental Alps. Those mountains derive their name from the Latin Alpes Pœninæ, the St Bernard Pass whose name has been derived from the Carthaginians, a local god. This was also the used in the invasions of Italy by the Gallic Boii. Various towns and geographical features within the Pennines retain Celtic names, including Penrith, the fell Pen-y-ghent, the River Eden, more commonly, local names result from later Anglo-Saxon and Norse settlements. In Yorkshire and Cumbria, many words of Norse origin, not commonly used in standard English, are part of speech, for example, gill/ghyll, beck, fell. This is located within parts of Cumbria, southern parts of Northumberland. This is within parts of Yorkshire and eastern parts of Derbyshire with foothills also continuing into western parts of Nottinghamshire. This is within the Stoke-on-Trent conurbation of northern Staffordshire and the parts of Derbyshire above the city of Derby. Apart from the uplands in the Lake District fringes, other Cumbrian Fells, the Pennines have been carved from a series of geological structures whose overall form is a broad anticline whose axis extends in a north–south direction. The North Pennines are coincident with the Alston Block, whilst the Yorkshire Dales are coincident with the Askrigg Block, in the south the Peak District is essentially a flat-topped dome. Each of these consists of Carboniferous limestone overlain with Millstone Grit
7.
Northern England
–
Northern England or the North of England, also known as the North Country or simply the North, is the northern part of England, when considered as a single cultural area. The area roughly spans from the River Trent and River Dee to the Scottish border in the north, Northern England roughly comprises three statistical regions, the North East, North West and Yorkshire and the Humber. These have a population of around 14.9 million as of the 2011 Census. The region has been controlled by groups from the Brigantes. After the Norman conquest in 1066, the Harrying of the North brought destruction, a Council of the North was in place during the Late Middle Ages until the Commonwealth after the Civil War. The area experienced Anglo–Scottish border fighting until the unification of Britain under the Stuarts, in the late 19th and early 20th centuries, the economy of the North was dominated by heavy industry such as weaving, shipbuilding, steelmaking and mining. The deindustrialisation that followed in the half of the 20th century hit Northern England hard. For government and statistical purposes, Northern England is defined as the covered by the three statistical regions of North East England, North West England and Yorkshire and the Humber. This definition will be used in article, except when otherwise stated. Using historic county boundaries, the North is generally taken to comprise Cumberland, Northumberland, Westmorland, County Durham, Lancashire and Yorkshire, the Isle of Man is occasionally included in definitions of the North, although it is politically and culturally distinct from England. Additionally, some areas of Derbyshire and Nottinghamshire have been associated with the North. The geographer Danny Dorling includes most of the West Midlands and part of the East Midlands in his definition of the North, conversely, more restrictive definitions also exist, typically based on the extent of the historical Northumbria, which exclude Cheshire and Lincolnshire. Personal definitions of the North vary greatly and are sometimes passionately debated, when asked to draw a dividing line between North and South, Southerners tend to draw this line further south than Northerners do. Various towns have been described as or promoted themselves as the gateway to the North, including Crewe, Stoke-on-Trent, through the North of England run the Pennines, an upland chain often referred to as the backbone of England. This stretches from the Cheviot Hills on the border with Scotland to the Peak District, the geography of the North has been heavily shaped by the ice sheets of the Pleistocene era, which often reached as far south as the Midlands. On the other side of the Pennines, a glacial lake forms the Humberhead Levels, a large area of fenland which drains into the Humber. This has left the North a region of contrasts, the Lake District includes Englands highest peak, Scafell Pike, which rises to 978 m, its largest lake, Windermere, and its deepest lake, Wastwater. However, dense areas have emerged along the coasts and rivers
8.
Historic counties of England
–
The historic counties of England were established for administration by the Normans, in most cases based on earlier kingdoms and shires established by the Anglo-Saxons and others. They ceased to be used for administration with the creation of the counties in 1889. They are alternatively known as ancient counties or traditional counties, where they are not included among the modern counties of England they are also known as former counties. Counties were used initially for the administration of justice, collection of taxes and organisation of the military and they continue to form the basis of modern local government in many parts of the country away from the main urban areas, although sometimes with considerably altered boundaries. The name of a county often gives a clue to how it was formed, either as a division took its name from a centre of administration. The majority of English counties are in the first category, with the name formed by combining the central town with the suffix -shire, for example Yorkshire. Former kingdoms, which became earldoms in the united England did not feature this formulation, so for Kent, Counties ending in the suffix -sex are also in this category and are former Saxon kingdoms. Many of these names are formed from compass directions, the third category includes counties such as Cornwall and Devon where the name corresponds to the tribes who inhabited the area. County Durham is anomalous in terms of naming and origin, not falling into any of the three categories, instead it was a diocese that was turned into the County Palatine of Durham, ruled by the Bishop of Durham. The expected form would otherwise be Durhamshire, but it was rarely used, there are customary abbreviations for many of the counties. In most cases these consist of simple truncation, usually with an s at the end signifying shire, some abbreviations are not obvious, such as Salop for Shropshire, Oxon for Oxfordshire, Hants for Hampshire and Northants for Northamptonshire. Counties were often prefixed with County of in official contexts, such as County of Kent and those counties named after central towns lost the -shire suffix, for example Yorkshire would be known as County of York. This usage was sometimes followed even where there was no town by that name, the -shire suffix was also appended for some counties, such as Devonshire, Dorsetshire and Somersetshire, despite their origin. There is still a Duke of Devonshire, Great Britain was first divided into administrative areas by the Romans, most likely following major geographical features such as rivers. Before their arrival there were distinct tribal areas, but they were in a constant state of flux as territory was gained, the areas that would later form the English counties started to take shape soon afterwards, with the Kingdom of Kent founded by settlers around 445. Once the Kingdom of England was united as a whole in 927 it became necessary to subdivide it for convenience and to this end. The whole kingdom was divided into shires by the time of the Norman conquest, robert of Gloucester accounts for thirty-five shires and William of Malmesbury thirty-two, Henry of Huntingdon, thirty-seven. In most cases the counties or shires in medieval times were administered by a sheriff on behalf of the monarch, after the Norman conquest the sheriff was replaced and the shires became counties, or areas under the control of a count, in the French manner
9.
Limestone
–
Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral, forams and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate, about 10% of sedimentary rocks are limestones. The solubility of limestone in water and weak acid solutions leads to karst landscapes, most cave systems are through limestone bedrock. The first geologist to distinguish limestone from dolomite was Belsazar Hacquet in 1778, like most other sedimentary rocks, most limestone is composed of grains. Most grains in limestone are skeletal fragments of organisms such as coral or foraminifera. Other carbonate grains comprising limestones are ooids, peloids, intraclasts and these organisms secrete shells made of aragonite or calcite, and leave these shells behind when they die. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragment, some limestones do not consist of grains at all, and are formed completely by the chemical precipitation of calcite or aragonite, i. e. travertine. Secondary calcite may be deposited by supersaturated meteoric waters and this produces speleothems, such as stalagmites and stalactites. Another form taken by calcite is oolitic limestone, which can be recognized by its granular appearance, the primary source of the calcite in limestone is most commonly marine organisms. Some of these organisms can construct mounds of rock known as reefs, below about 3,000 meters, water pressure and temperature conditions cause the dissolution of calcite to increase nonlinearly, so limestone typically does not form in deeper waters. Limestones may also form in lacustrine and evaporite depositional environments, calcite can be dissolved or precipitated by groundwater, depending on several factors, including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits a characteristic called retrograde solubility, in which it becomes less soluble in water as the temperature increases. Impurities will cause limestones to exhibit different colors, especially with weathered surfaces, Limestone may be crystalline, clastic, granular, or massive, depending on the method of formation. Crystals of calcite, quartz, dolomite or barite may line small cavities in the rock, when conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together, or it can fill fractures. Travertine is a banded, compact variety of limestone formed along streams, particularly there are waterfalls. Calcium carbonate is deposited where evaporation of the leaves a solution supersaturated with the chemical constituents of calcite. Tufa, a porous or cellular variety of travertine, is found near waterfalls, coquina is a poorly consolidated limestone composed of pieces of coral or shells. During regional metamorphism that occurs during the building process, limestone recrystallizes into marble
10.
River Ure
–
The River Ure is a river in North Yorkshire, England, approximately 74 miles long from its source to the point where it changes name to the River Ouse. It is the river of Wensleydale, which is the only one of the major Dales now named after a village rather than its river. The old name for the valley was Yoredale after the river runs through it. The Ure is one of many rivers and waterways that drain the Dales into the River Ouse, tributaries of the Ure include the River Swale and the River Skell. The earliest recorded name of the river is Earp in about 1025, probably an error for Ear Ƿ, by 1140 it is recorded as Jor, hence Jervaulx Abbey, and a little later as Yore. In Tudor times the antiquarians John Leland and William Camden used the form of the name. The name probably means the strong or swift river and this is on the assumption that the Brittonic name of the river was Isurā, because the Roman name for Aldborough was Isurium, intervocalic s is known to have been lost in Brittonic at an early date. This explanation connects the name with an Indo-European root is- meaning strong and the names of the Isar in Germany. The source of the river is Ure Head on Abbotside Common where it flows west south-west to the valley floor, where it reaches the A684 it turns east along Wensleydale as far as Wensley. From here it flows south-east to Jervaulx Abbey and shortly after south to Mickley, here it returns east and then south to Ripon. A little way after Ripon it flows east again to Boroughbridge, to the east of Boroughbridge, the Ure is joined by the River Swale. About 6 miles downstream of confluence, at Cuddy Shaw Reach near Linton-on-Ouse. Low and High Water Levels are an average figure, upper Wensleydale is high, open and remote U shaped valley overlying Yoredale Beds. The gradient is gentle to the end of the valley. Drumlins lay either side of the river, which is shallow, the river is fed from many gills cutting through woodland and predominantly sheep farmsteads. The Settle to Carlisle railway runs along the side of the valley here. Mid Wensleydale is made of Great Scar limestone under Yoredale beds that make up the sides which are marked with stepped limestone scars. The valley floor is made from glacial drift tails and moraine, the river here is broad and gently flowing in meanders in a stony channel
