82-412: Saltburn The Cleveland Way is a National Trail in the historic area of Cleveland in North Yorkshire , Northern England . It runs 110 miles (177 km) between Helmsley and the Brigg at Filey , skirting the North York Moors National Park. Development of the Cleveland Way began in the 1930s when the Teesside Ramblers' Association pressed for the creation of a long-distance path in
164-649: A circular long distance bridle route created around the North York Moors which can be accessed at a number of locations. The steep escarpments that define the edges of the National Park on three sides are used by several gliding clubs. In late 2020, the National Park was named as an International Dark Sky Reserve. This honour confirms that the area has "low levels of light pollution with good conditions for astronomy". The National Park has two visitor centres which have tourist information and exhibitions, as well as
246-543: A collection of circular stone hut foundations on Percy Rigg. Other evidence of Iron Age occupation is scarce, having been obliterated by subsequent agricultural activity. By 71 AD, the Roman army had reached Yorkshire, where they established a fort at Malton. Wade's Causeway may have been one of the several Roman roads which radiated from this point. It led north-eastwards over the Vale of Pickering and across Wheeldale Moor towards
328-635: A low watershed, is drained by the River Leven , which flows west to join the River Tees . On their south side, the moorland is incised by a series of dales which drain into tributaries of the River Derwent . The westernmost dale is Rye Dale , to the west of which rise the Hambleton Hills . Bilsdale is a side dale of Rye Dale. East of Bilsdale Bransdale , Farndale , Rosedale and Newton Dale cut into
410-521: A new Danish kingdom based at York. The Danes settled in the area and later themselves became Christian. They introduced their language, elements of which still remain in the local dialect, and renamed a number of settlements. King William I of England and his Norman barons took control of the nation in 1066. Central to the imposition of Norman rule was the building of castles. There are well-preserved castle ruins at Helmsley, Pickering and Scarborough and others existed at Ayton, Danby, Mulgrave and Whorlton. In
492-504: A number of gods, notably Woden . However, Christianity came to Yorkshire when King Edwin of Northumbria was baptised in 627 AD at York. Christian monasteries were established at Lastingham in 654 and Whitby in 657. A nunnery was built at Hackness in 680. In the 9th century, Viking raiders began to attack the Yorkshire coast, and in 867 these Danes destroyed the religious houses at Whitby, Lastingham and Hackness and after battle set up
574-520: A widespread scattering of flint tools and the barbed flint flakes used in arrows and spears. By 5000 BC, as global sea levels rose and the North Sea came into existence, Britain was cut off from mainland Europe. During the New Stone Age, which lasted from around 4500 to 2000 BC, the population increased and agriculture was adopted. These early farmers were the first to destroy the forest cover of
656-598: Is abundant rain and poor drainage. Cotton grass is a distinctive plant which grows in the boggy areas. In the cold acid waters of peat bogs there is little decomposition of organic material with the result that the dead sphagnum moss gradually accumulates to form peat. This raises the levels of the bogs and they dry out. Heather then invades the area. Large areas of the moorland are now covered in heather, bilberries and grasses growing on thick layers of peat. The acid soils and peat bogs are unsuitable for earthworms so species which usually feed on earthworms such as moles and
738-697: 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 554 sq mi (1,430 km ), the National Park has a population of 23,380. It is administered by the North York Moors National Park Authority, which
820-489: Is at the end of the Tees Valley Line from Middlesbrough and Darlington . Beyond Saltburn a mineral goods line continues across Saltburn Viaduct and the edge of Hunt Cliff to the potash mine at nearby Boulby . There are now only three buses an hour to Redcar and Middlesbrough and two an hour to Loftus and Whitby. There was an infrequent direct bus service to Guisborough and Stokesley, Monday to Friday only, but this
902-709: Is based in Helmsley . 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
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#1732851522316984-450: Is burned in strips by gamekeepers and farmers to encourage new heather growth to feed the grouse. Grouse shooting is part of the moorland economy. About 20 per cent of the national park is covered in bracken . Few things can grow under its dense cover and it does not support many insects and is unpalatable to most animals. The bracken is extremely invasive. Sheep are a ubiquitous part of the moorland landscape. Their grazing helps to maintain
1066-437: Is influenced by predominantly westerly winds with depressions and their associated fronts , bringing with them unsettled and windy weather, particularly in winter. Between depressions, there are often small mobile anticyclones that bring periods of fine weather. In winter, anticyclones bring cold dry weather. In summer, the anticyclones tend to bring dry settled conditions, which can lead to drought. For its latitude, this area
1148-579: Is milder in winter and cooler in summer due to the influence of the Gulf Stream in the North Atlantic Ocean . Air temperature varies on a daily and seasonal basis. The temperature is usually lower at night and January is the coldest time of the year. The two dominant influences on the climate of the North York Moors are the shelter against the worst of the moist westerly winds provided by the Pennines and
1230-512: Is the original settlement, located in the Saltburn Gill . Records are scarce on its origins, but it was a centre for smugglers , and publican John Andrew is referred to as 'king of smugglers'. In 1856, the hamlet consisted of the Ship Inn and a row of houses, occupied by farmers and fishermen. In the mid-18th century, authors Laurence Sterne and John Hall-Stevenson enjoyed racing chariots on
1312-719: Is variable from year to year, but the area gets much more snow on average than other parts of the country. Heavy falls are associated with northeasterly winds off the North Sea. Roads over the high moorland areas are notoriously prone to drifting snow due to the exposed nature of the terrain. Average recordings are: The geology of the North York Moors is dominated by rocks of the Jurassic period. They were mostly laid down in subtropical seas 205 to 142 million years ago. Fluctuations in sea level produced different rock types varying from shales to sandstones and limestones derived from coral. These marine and delta deposited rocks are well exposed on
1394-617: The Bom Jesus funicular in Braga , Portugal. After the opening of Saltburn Pier in February 1869, it was concluded that the steep cliff walk was deterring people from walking from the town to the pier. After the company was taken over by Middlesbrough Estates in 1883, they discovered that the wooden Cliff Hoist had a number of rotten supports. The Saltburn tramway, as it is also known, was developed by Sir Richard Tangye's company, whose chief engineer
1476-674: The Countryside and Rights of Way Act 2000 . Popular named walks include the Cleveland Way , which circles the North York Moors, including a coastal section; and the Lyke Wake Walk , which leads directly across the heart of the National Park. The route of the White Rose Way , a long distance walk from Leeds to Scarborough also passes through. The area also offers opportunities for cycling , mountain biking , and horse-riding , including
1558-673: The Dales Way ) to Helmsley. The White Rose Walk from Kilburn White Horse to Roseberry Topping crosses the Cleveland Way. The whole coastal section of the Cleveland Way forms part of the North Sea Trail . The route of the White Rose Way follows the same coastal section. The Esk Valley Walk from Castleton ends at Whitby . The Coast to Coast Walk starts or ends at Robin Hood's Bay , and
1640-515: The Devensian , ended about 11,000 years ago. The higher parts of the North York Moors were not covered by the ice sheets but glaciers flowed southwards on either side of the higher land mass. As the climate became warmer at the end of the ice age, the snowfields on the North York Moors began to melt. The meltwater was unable to escape northwards, westwards or eastwards because it was blocked by ice. Huge torrents of water were forced southwards. Water from
1722-566: The Lyke Wake Walk crosses the moors from Osmotherley to Ravenscar . The Tabular Hills Walk , a regional route developed by the North York Moors National Park Authority, links the two southerly ends of the Cleveland Way, enabling walkers to walk the complete perimeter of the North York Moors National Park . The Yorkshire Wolds Way goes from Filey to Hessle , near Hull , where it connects with
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#17328515223161804-682: The Trans Pennine Trail which forms part of the European walking route E8 . The Hardmoors Race Series features ultramarathons , marathons and shorter races based on the Cleveland Way route. Included in the ultramarathon series are a 110 mi (180 km) race circumnavigating the entire length of the Cleveland Way, and a 55 mi (89 km) and 60 mi (97 km) race which race between Helmsley and Guisborough, and Guisborough and Filey respectively in differing directions. There are also longer routes which link up to other trails including
1886-424: The common shrew are absent on the moorland. The pygmy shrew survives by eating the insects and spiders that live in the heather. Lapwing , curlew and redshank breed on the moorland and there are sandpipers along the streams. Wheatear and golden plovers inhabit grassier patches on the moorland and ring ouzels live in stony areas. Red grouse , which feed on young heather shoots, are abundant. The heather
1968-453: The historic boundaries of the North Riding of Yorkshire . The development of Saltburn was driven by the discovery of ironstone in the Cleveland Hills and building of railways to transport the minerals. In 1961, the parish had a population of 5,708. The town itself had a population of 5,958 in 2011. Saltburn was formerly in the parish of Brotton , however, after 1894 Saltburn by
2050-431: The trailheads of Helmsley ( grid reference SE6125183849 ) and Filey ( grid reference TA1155480742 ) in a horseshoe configuration. The trail is waymarked along its length using the standard National Trail acorn symbol. The trail falls into two roughly equal sections. The inland section leads west from Helmsley, then north, then east around the west of the North York Moors National Park . It then leaves
2132-470: The wood vetch and orchids are also to be found. Adders are widespread throughout the national park. On the moors they eat common lizards and around the hedgerows and woodland edges they feed on mice and voles. The limestone grasslands support a wide variety of wild flowers, and many rarer butterflies can be seen. Pearl-bordered fritillary , Duke of Burgundy fritillary , marbled white , dingy skipper and grayling are just some of species that inhabit
2214-435: The 11th and 12th centuries monasteries were established on the moors at Whitby Abbey , Rievaulx Abbey , Byland Abbey and Mount Grace Priory . Gifts of land and money were bestowed on these establishments and the monastic orders became notable landowners, eventually owning about a third of the land in the area. The abbeys managed their land as sheep farms and became very rich on the profits. They continued to take in land from
2296-409: The 19th century railways were built from Pickering to Whitby (1836), Middlesbrough to Whitby (1868) and Scarborough to Whitby (1884). Locally sourced iron ore has been processed on the North York Moors from medieval times. In the 19th century it became a boom industry. Dozens of ironstone mines and several short-lived blast furnaces were constructed. Between 1856 and 1926 high-grade magnetic ironstone
2378-499: The Esk Valley, and East Yorkshire route 128 connects Scarborough and Helmsley. On weekends during the summer, these are complemented by Moorsbus services, which run from local urban centres into more remote parts of the national park which are difficult to access without private transport. Some of the routes across the North York Moors are noted for their beauty – the 840 was declared Britain's most scenic bus route by Bus Users UK while
2460-480: The Esk valley area flowed southwards gouging out the deep Newtondale valley as it went. Water from the North York Moors formed a vast lake in the area of the Vale of Pickering. Eventually this lake filled its basin and then overflowed at the lowest point which was at Kirkham. Here it cut the steep sided Kirkham gorge. When the ice finally retreated it left deep deposits of boulder clay (or till ) behind. The boulder clay blocked
2542-750: The Lottery. The Saltburn Cricket Club play in the NYSD league . The North Riding Duck Race is held each year on 1 August to celebrate Yorkshire Day . The winner receives the Colin Holt Cup, named in honour of the late Colin Holt , for many years the Chairman of the Yorkshire Ridings Society . A prize is given also for the duck with the most original name. The coastline is known for national surfing events held during
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2624-584: The Moors and finally destroyed much of the original forest. The climate was relatively warmer and drier at this time so it was possible to live on the high moors throughout the year. When a piece of land was exhausted of nutrients, these people moved on, leaving behind land that was incapable of supporting anything but a heathland vegetation. There are about 3,000 Bronze Age burial mounds on the moors. The Iron Age dates from about 600 BC. There are remains of two promontory hill forts at Boltby Scar and Roulston Scar and
2706-772: The National Park near Guisborough to meet the coast at Saltburn . It re-enters the National Park just north of Staithes ; the coastal section follows the coast from Saltburn to Whitby , then leaves the National Park for the final time at Cloughton Wyke to reach Scarborough and Filey. The moorland sections of the trail provide a habitat for species including red grouse , curlews and emperor moth caterpillars . The coastal sections may provide sightings of seabirds such as great cormorants , shags , Atlantic puffins , common guillemots and herring gulls . The Cleveland Way connects with various other long-distance footpaths . These are listed in order from Helmsley to Filey . The Ebor Way goes from Ilkley (where it connects with
2788-461: The North Sea coast. There are Roman camps at Cawthorn and Lease Rigg near Grosmont and signal stations along the coast at Filey, Scarborough, Ravenscar, Goldsborough and Hunt Cliff . The Romans left Britain in 410 AD. After the departure of the Romans, Germanic tribes arrived and settled in the area. These Angles, Saxons and Jutes gave many of the place names to villages on the moors. They worshipped
2870-678: 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 Whitby. More centrally, a minor road departs from the A170 at Keldholme and passes through Castleton before joining the A171 which connects Whitby and Guisborough . The most westerly route is the B1257 connecting Helmsley to Stokesley . The A170 from Thirsk to Scarborough marks
2952-565: The S&;DR, and agreed to develop Henry's vision by forming the Saltburn Improvement Company (SIC). Land was purchased from the Earl of Zetland , and the company commissioned surveyor George Dickinson to lay out what became an interpretation of a gridiron street layout , although this was interrupted by the railway which ran through the site. With as many houses as possible having sea views,
3034-529: The S&DR, with the name Pease set into the brick. The jewel in Henry Pease's crown is said to have been The Zetland Hotel with a private platform, one of the world's earliest railway hotels. The parcel of land known as Clifton Villas was sold by the SIC in 1865 to William Morley from London who built the property, 'The Cottage' (now Teddy's Nook) on a site originally intended for three villas. The SIC stipulated in
3116-574: The Sea became a separate civil parish , being formed from the part of Marske parish in Saltburn by the Sea Urban District. Saltburn by the Sea Urban District was also formed in 1894. On 1 April 1932, the urban district was abolished to form Saltburn and Marske By the Sea Urban District. The original civil parish was also abolished on 1 April 1974 to form "Saltburn and Marske by the Sea". Old Saltburn
3198-570: The Stepping Stones and the Saltburn Viaduct. Saltburn's only secondary school is Huntcliff School which was rebuilt during 2007–8, re-opening on 8 September 2008. The redundant 50-year-old school buildings were then demolished to allow the town's Junior and Infant schools to relocate to the same site in 2009 because the Junior and Infant schools used to be located in a different building, not in
3280-517: The Vale of Pickering flowing westwards, turns southwards at Malton and flows through the eastern part of the Vale of York before emptying into the River Ouse at Barmby on the Marsh . As part of the United Kingdom, the North York Moors area generally has warm summers and relatively mild winters. Weather conditions vary from day to day as well as from season to season. The latitude of the area means that it
3362-578: The Valley Gardens gives access to the Italian Gardens and leads on to the railway viaduct . On the shore of Old Saltburn stands the Ship Inn, which dates to the 17th century. In the town there are plenty of Victorian buildings . There is also a thriving local theatre, The 53 Society , and a public library. The Saltburn Cliff Lift is one of the world's oldest water-powered funiculars —the oldest being
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3444-572: The X93 was the tenth most scenic. The cyclists in the 2018 and 2019 Tour de Yorkshire passed through a section of the North York Moors. The North York Moors consist of a moorland plateau, dissected by a number of deep dales or valleys containing cultivated land or woodland. The largest dale is Eskdale , the valley of the River Esk which flows from west to east and empties into the North Sea at Whitby . The Cleveland Hills rise north of Eskdale. At
3526-677: The Yorkshire Wolds Way. Official circular walks along the Cleveland Way include: [REDACTED] Media related to Cleveland Way at Wikimedia Commons Saltburn-by-the-Sea Saltburn-by-the-Sea , commonly referred to as Saltburn , is a seaside town in the civil parish of Saltburn, Marske and New Marske , in the Redcar and Cleveland district, in North Yorkshire , England, 12 miles (19 km) south-east of Hartlepool and 5 miles (8 km) south-east of Redcar . It lies within
3608-445: The Yorkshire coast from Staithes to Filey. Subsequently, about 30 million years ago, the land was uplifted and tilted towards the south by earth movements. The upper layers of rock were eroded away and the older rocks were exposed in places. Because of the tilt the oldest rocks became exposed in the north. These are the bands of shales and ironstones on the northern scarp of the North York Moors and Cleveland Hills. The middle layers form
3690-434: The air and salt or clear water. Rock pools contain sea anemones , blennies , crabs and molluscs . Sandy shores harbour a variety of plants and animals which are buried in the sand. Birds such as curlews and oyster catchers are to be seen prodding the sand to find these creatures for food. A few cormorants and fulmars breed along the coast where stonechats and rock pipits can also be spotted. Herring gulls are
3772-472: The area, leaving little point in extending the S&DR tracks further. In 1858, while walking along the coast path towards Old Saltburn to visit his brother Joseph in Marske-by-the-Sea , Henry Pease saw "a prophetic vision of a town arising on the cliff and the quiet, unfrequented and sheltered glen turned into a lovely garden". The Pease family owned Middlesbrough Estate and had control of
3854-548: The autumn and winter months, attracting competitors from England, Scotland and Wales. Annual events include the Saltburn Custom Classic Car Show—a lower prom display of mostly American cars—and the Saltburn Festival of Folk Music, Dance and Song. Anticlockwise Marske-by-the-Sea Saltburn-by-the-Sea Clockwise Skinningrove North York Moors National Park The North York Moors
3936-479: The campus area. In the early 1900s the building where the Earthbeat Centre is now located was a girls grammar school, and later a primary school until 2009. "After many months of intensive renovation the former Saltburn School has now opened its doors to the public as the Earthbeat Centre." The site is now the home of the Earthbeat Centre, with a fifty-year lease that began in 2015. Saltburn railway station
4018-505: The cold climate of the ice age ameliorated and temperatures rose above growing point of 5.5 °C (41.9 °F). Plant life was gradually re-established and animals and humans also returned. Around 8,000 BC, Britain was still part of the European landmass, and communities of Middle Stone Age people migrated to England and began to inhabit the North York Moors. Relics of this early hunting, gathering and fishing community have been found as
4100-506: The commonest breeding birds and are an interesting sight nesting in the chimneys of coastal towns. There are records of 12,000 archaeological sites and features in the North York Moors National Park of which 700 are scheduled monuments . Radio carbon dating of pollen grains preserved in the moorland peat provides a record of the actual species of plants that existed at various periods in the past. About 10,000 years ago,
4182-643: The deed of covenant that "any trees planted along Britannia Terrace (now Marine Parade) were not to exceed 1' 6" above the footpath" (46 cm) to preserve sea views for Britannia Terrace residents and visitors. The Redcar to Saltburn Railway opened in 1861 as an extension of the Middlesbrough to Redcar Railway of 1846. The line was extended to Whitby as part of the Whitby Redcar and Middlesbrough Union Railway . The coastline at Saltburn lies practically east–west, and along much of it runs Marine Parade. To
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#17328515223164264-535: The east of the town is the imposing Hunt Cliff , topped by Warsett Hill at 166 metres (545 ft). Skelton Beck runs through the wooded Valley Gardens in Saltburn, then alongside Saltburn Miniature Railway before being joined by Saltburn Gill going under the A174 road bridge and entering the North Sea across the sandy beach. The A174 road number is now used for the Skelton/Brotton Bypass. A forest walk in
4346-462: The eastern end of the Vale of Pickering causing a permanent deviation in the course of the River Derwent. Alluvium from the glacial meltwater covers many areas to the north of the moors and in the Esk valley. The North York Moors National Park encompasses three main types of landscape, whose differences are clearly visible, and the coastal belt. There are predominantly green areas of pasture land,
4428-464: The foundation of the seaside resort and the sturdy sandstone house was first named The Cottage . Lillie Langtry — The Jersey Lily , stayed at the house at sometime between 1877 and 1880. She was often visited by Edward Prince of Wales (later Edward VII of the United Kingdom ) who had a suite of rooms at the Zetland Hotel . The cottage, consequently, became known as Teddy's Nook. The Cottage
4510-415: The high ground. These woodland areas are the home of pied flycatchers, sparrow hawks and wood warblers . Roe and fallow deer can also be found here. The woodlands and south facing grasslands on the limestone belt provide a good habitat for many butterflies. The fertile alkaline soils support an abundance of wild flowers. Bluebells and primroses grow in the hedgerows in spring and rarer plants such as
4592-449: The industry grew in the middle of the 19th century in response to a fashion for the jewellery produced from it. In the 1880s cheap imports produced a decline in the industry which was focused on Whitby. The remains of alum quarries are to be found to the north of the area and along the coast. Alum was important to the textile industry because it was used as a mordant or fixative for dyes that were used to colour cloth. The industry thrived in
4674-426: The livestock farms. The main arable crops are barley, wheat, oilseed rape, potatoes, and sugar beets. There is also some intensive production of pigs and poultry. Many visitors to the North York Moors are engaged in outdoor pursuits, particularly walking ; the National Park has a network of public rights of way almost 1,400 miles (2,300 km) in length, and most of the areas of open moorland are open access under
4756-480: The moorland. In the south east, the landscape is marked by the narrow valleys of the upper reaches of the Derwent and its upper tributaries. About 23 per cent of the North York Moors is under woodland cover (mostly located to the south-west and south-east), equivalent to more than 300 square kilometres of trees. It is home to the largest concentration of ancient and veteran trees in northern England. The Derwent crosses
4838-455: The moors. Their settlements were concentrated in the fertile parts of the limestone belt and these areas have been continuously farmed ever since. The Neolithic farmers grew crops, kept animals, made pottery and were highly skilled at making stone implements. They buried their dead in long low burial mounds. Around 2000 BC, the early Bronze Age Beaker People inhabited the Moors. During a 1,400 year period, these people inhabited all areas of
4920-779: The national park. The cliffs and sandy bays of the northern end of the Yorkshire Coast offer an assortment of seashore habitats. An area where the Cleveland Hills meets the sea has been designated as a Heritage Coast . The cliff at Boulby, at 690 feet (210 m), the highest point on the east coast of England is formed by Jurassic shales, clays and ironstones. There are also fine exposures of Jurassic rocks with their characteristic fossils around Robin Hoods Bay and Ravenscar. Rocky shores offer an abundance of seaweeds in zones of different types which are more and less tolerant of exposure to
5002-612: The north-east of Yorkshire linking the Hambleton Drove Road, the Cleveland escarpment and footpaths on the Yorkshire coast. Subsequently, in 1953, a formal proposal to create the route was submitted to the North Riding of Yorkshire Council by the National Parks Commission. The trail was officially opened in 1969. It was the second official National Trail to be opened. The trail can be walked in either direction linking
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#17328515223165084-416: The only pleasure pier on the whole of the North East and Yorkshire coast. The Saltburn Miniature Railway is a 15 in ( 381 mm ) gauge railway that runs south from Cat Nab Station close to the beach, for about ½ mile inland to Forest Halt , where there is a woodland walk and the Italian Gardens. As the town had been founded by Quakers , the SIC had a ban on public houses . Alcohol
5166-493: The open wild landscape that is needed for many other plants and animals to thrive. Limestone weathers quickly to produce nutrient rich alkaline soils on well drained rocks. Gouging by glacial meltwaters has left spectacular valleys along whose floors run streams. The limestone streams with their nutrient rich waters support an abundance of aquatic invertebrates such as insect larvae and crustaceans . These in turn support such fish as trout and grayling . Insects which emerge from
5248-455: The park each year, has been formed and maintained by generations of farmers. The 1996 Agricultural Census recorded a total workforce of 2,913 employed on 1,342 working farms. Sheep and cattle provide the prime source of farm income. The dale farms have rights to graze sheep on the open moor. The rights to moorland grazing are often essential to the economic viability of a farm. In recent years agriculture in Britain has suffered economic setbacks and
5330-406: The proximity of the North Sea . Late, chilly springs and warm summers are a feature of the area, but there are often spells of fine autumn weather. Onshore winds in spring and early summer bring mists or low stratus clouds (known locally as sea frets) to the coasts and moorland. Within the area, variations in climate are brought about by local differences in altitude, aspect and shelter. Snowfall
5412-406: The purple and brown heather moorland, and woodland. The three kinds of scenery are the result of differences in the underlying geology and each supports different wildlife communities. Sandstones erode slowly and form poor acid soils which are deficient in nutrients. They are less permeable to water, impeding drainage and encouraging the formation of bogs. Sphagnum moss bogs are common where there
5494-442: The region from the early 17th century until 1871. Its decline came when chemical dyes were discovered. The scars of industrial activity on the moors make it an interesting area in which to pursue industrial archaeology. The area's economy is mainly founded on tourism and agriculture . For over a thousand years the basis of the economy in the North York Moors was agriculture. The rural scene, which attracts millions of visitors to
5576-443: The sands at Saltburn. The Pease family of Darlington developed Middlesbrough as an industrial centre and, after discovery of iron stone, the Stockton & Darlington Railway and the West Hartlepool Harbour and Railway Company developed routes into East Cleveland. By 1861, the S&DR reached Saltburn with the intention of continuing to Brotton , Skinningrove and Loftus ; but the WHH&RCo had already developed tracks in
5658-405: The sandstones of the high moorland and the youngest layers of limestone form the Tabular Hills. In the dales, where the rivers have cut through the younger rocks, there are also exposures of older shales, ironstone and sandstone. Rosedale is an example of this. During the Quaternary period , the last 2 million years, the area has experienced a sequence of glaciations . The most recent glaciation,
5740-420: The settlements took the form of isolated farms and hamlets rather than villages. Very few had an open field system of agriculture so Enclosure Acts were rarer than in other parts of England. The 17th century saw a major acceleration in the reclaiming of marginal waste land and in the eighteenth century forward looking landlords attempted to improve their lands using drainage schemes and fertilisation measures. In
5822-423: The so-called "Jewel streets" along the seafront—Coral, Garnet, Ruby, Emerald, Pearl, Diamond and Amber Streets, said to be a legacy of Henry's vision, were additional to the grid pattern. After securing the best positions for development by the SIC, money was raised for construction by selling plots to private developers and investors. Most buildings are constructed using 'Pease' brick, transported from Darlington by
5904-676: The southern boundary of the North York Moors area. The Esk Valley Line is an east-west branch line rail link from Whitby to Middlesbrough in the north, and the North Yorkshire Moors steam railway runs from Pickering to Grosmont with a link to Whitby. Other public transport within the North York Moors includes a number of bus services. Yorkshire Coastliner route 840 runs from Whitby to Pickering (and continues to York and Leeds), Arriva North East routes X93 and X94 run from Scarborough to Middlesbrough via Whitby and Guisborough, Arriva North East route 95 runs from Whitby to Lealholm along
5986-419: The viability of hill farming has become questionable. A number of environmental schemes to improve farm incomes have been devised but the industry continues to decline. Agricultural use of the moors is shared with grouse shooting as a means of gaining financial return from the vast expanse of heather. There is richer farmland across the southern limestone belt, where there are arable and mixed farms as well as
6068-435: The waste and what remained of the forest and in the process gave the moors the distinctive landscape that still remains. Between 1536 and 1541, Henry VIII of England dissolved the monasteries, and confiscated and sold off their property. This was bought by individual people, some rich, but also some who had been tenants of the monasteries, and became privately owned land. In many areas of the moors and their associated dales
6150-404: The water in summer are also a rich source of food for birds. Grey wagtails , swallows and spotted flycatchers are commonly seen. Dippers and kingfishers are also typical. The otter , after a period of decline, is starting to recolonise the rivers and streams. Farndale is famous for its wild daffodils in spring. Sheltered woodlands dominated by sessile oaks can be found to the south of
6232-503: The western end of Eskdale, the valley divides into three smaller dales, Westerdale (the upper valley of the River Esk), Baysdale and Commondale . A series of side dales drain into Eskdale from the moorland on its southern side, from west to east Danby Dale, Little Fryup Dale , Great Fryup Dale , Glaisdale and the Goathland valley. Kildale , west of Commondale and separated only by
6314-413: Was George Croydon Marks . The cliff tramway opened a year later and provided transport between the pier and the town. The railway is water-balanced and since 1924 the water pump has been electrically operated. The first major maintenance was carried out in 1998, when the main winding wheel was replaced and a new braking system was installed. Saltburn's attractions include a Grade II* renovated pier ,
6396-520: Was The Victoria, opened on 8 December 1982. Today the following public houses exist in Saltburn: Alexandra Vaults (known locally as Back Alex), The Victoria, The Marine, The Ship Inn, Vista Mar and The Hop and Vine (formerly Windsor's). Teddy's Nook is a house built in 1862 by Henry Pease , a director of the Stockton and Darlington Railway , for his own occupation. Pease was responsible for
6478-480: Was mined in Rosedale. A railway was built around the top of the dale to serve the mines, and kilns were built to process the ore. In two decades the population of the valley rose from 558 to nearly 3000. Poor-quality coal was mined in many places on the moors from the 18th century to the early 20th century. The North York Moors is the only source for British jet . It has been mined in the area from prehistoric times but
6560-537: Was only one of four similar houses to be called Clifton Villas . The cottage was the family home of Audrey Collins, MBE, who served as Mayor of Saltburn and chair of the South Tees Health Authority. Middlesbrough's James Cook University Hospital has named a teaching unit in her name. Locally known as Fairy Glen, the Saltburn Valley Woods run through Saltburn Beck. Places in these woods include
6642-465: Was served in the hotels and the bars attached to them, and in private members' clubs, which included; Ruby Street Social Club (formerly The British Legion; now demolished), Lune Street Social Club (Top Club), Milton Street Social Club (Bottom Club), The Red Lodge, The Conservative Club, Saltburn Golf Club, Saltburn Cricket, Tennis and Bowls Club and The Queens (known locally as The Swingdoors). Saltburn's first public house (independent of an existing hotel)
6724-577: Was withdrawn in January 2023.New Services(1 and 2) were introduced in 2023. These run every seven minutes but are little used as the routes seem to suit very few people. Sports played in Saltburn include cricket, bowls and tennis also played at the Club in Marske Mill Lane. The club has existed for over 100 years and is nearly as old as the town itself. New facilities were provided in 2002 with financial help from
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