Things to do in York and North Yorkshire

Gaping Gill represents one of Britain's most spectacular natural phenomena, where Fell Beck plunges 105 metres (344 feet) through a shaft into a vast underground chamber within the limestone heart of Ingleborough. This is not a traditional waterfall in the conventional sense, but rather a vertical shaft entrance to one of England's most impressive cave systems, where the stream simply disappears into the earth in a dramatic free-falling drop. The main chamber into which the water falls is large enough to contain the entire volume of York Minster, measuring approximately 145 metres long, 25 metres wide, and reaching heights of up to 35 metres. The entrance shaft itself is roughly 10 metres by 5 metres at the surface, opening into the darkness below where the water crashes onto the floor of the main chamber with tremendous force, creating a continuous roar and a perpetual mist within the cavern. Fell Beck rises on the moorland slopes above Ingleborough, gathering water from the peaty uplands and limestone pavements that characterise this part of the Yorkshire Dales. The stream flows across the characteristic stepped limestone terrain before reaching Gaping Gill, where the soluble nature of the Carboniferous limestone has allowed water to erode and dissolve the rock over countless millennia, creating the vast subterranean void. After disappearing at Gaping Gill, the water follows an underground course through the cave system before re-emerging at Ingleborough Cave and Beck Head, eventually joining other watercourses in the valley below. The catchment area experiences high rainfall typical of the Pennine uplands, and during wet weather the volume of water entering the shaft can be truly impressive, though it can reduce to a modest flow during dry summer periods. The first recorded descent of Gaping Gill was made by Édouard-Alfred Martel, the pioneering French speleologist, in 1895. Martel was lowered on a rope ladder by a team of Yorkshire potholers, becoming the first person to reach the floor of the main chamber and document its extraordinary dimensions. This expedition marked a significant moment in the history of British caving and helped establish the sport of speleology in the United Kingdom. Since then, Gaping Gill has attracted cavers, explorers, and scientists from around the world, with extensive exploration revealing over 20 kilometres of interconnected passages extending in various directions from the main chamber. The cave system has been the site of numerous expeditions and has yielded important geological and hydrological data about the region's karst landscape. Local folklore and legend have long surrounded this dramatic feature in the landscape. Before its exploration, the shaft was regarded with considerable superstition by local people, and various tales spoke of the mysterious abyss and its unfathomable depths. The name "Gaping Gill" itself evokes the mouth-like appearance of the shaft opening in the fellside, and the constant sound of falling water echoing from the depths would have added to its mysterious and somewhat forbidding character. The area around Ingleborough has a rich tradition of folklore relating to caves, streams, and underground waters, reflecting the profound impact that the limestone landscape has had on the imagination of those who have lived and worked in these hills over the centuries. The landscape surrounding Gaping Gill is quintessentially that of the Yorkshire Dales, with extensive limestone pavements, open moorland, and characteristic upland vegetation. Ingleborough itself, at 723 metres, is one of the famous Three Peaks and dominates the skyline, its distinctive flat-topped summit a landmark visible from great distances. The geology is predominantly Carboniferous limestone, which creates the classic karst scenery of this area with its swallow holes, sink holes, limestone pavements with their clints and grykes, and underground drainage systems. The exposed limestone supports specialised flora adapted to the alkaline conditions and thin soils, while the moorland areas feature grasses, sedges, and heather. Birdlife includes typical upland species such as curlews, lapwings, and skylarks, while the becks and surrounding grasslands support various invertebrates and small mammals. Twice a year, typically during the Spring and August bank holiday weekends, local caving clubs set up a winch system that allows members of the public to descend into the main chamber of Gaping Gill. These events, organised by the Bradford Pothole Club and Craven Pothole Club on alternate holidays, provide a rare opportunity for non-cavers to experience the spectacular underground chamber, with visitors being lowered in a specially designed bosun's chair through the shaft to the chamber floor below. Outside of these organised winch meets, the cave entrance itself can be viewed from the surface, though extreme caution must be exercised as the shaft opening is dangerous and unfenced, with a sheer drop into the darkness below. Access to Gaping Gill typically begins from Clapham village, where parking is available in the National Park car park. From Clapham, a popular walking route follows the estate path through the grounds of Ingleborough Estate, passing the small lake and continuing up the valley past Ingleborough Cave (a show cave where part of the underground system can be visited). The path continues to climb onto the open fell, eventually reaching Gaping Gill after approximately 5 kilometres of walking. The route gains considerable height and crosses sometimes boggy terrain, so appropriate footwear and clothing are essential. An alternative approach can be made from other directions, including from Horton-in-Ribblesdale or Ingleton, though these routes are generally longer. The area is part of the Yorkshire Dales National Park, and the usual countryside codes apply regarding livestock, gates, and respecting the landscape. The cave system beneath Gaping Gill has been the subject of extensive exploration and surveying, revealing a complex three-dimensional maze of passages at various levels. Some passages are fossil systems formed when the water table was at a higher level, while others carry active streams. The system connects with other cave systems in the area, forming part of a vast underground drainage network beneath Ingleborough. Several other entrances to the system exist, including Disappointment Pot, Stream Passage Pot, and Flood Entrance Pot, though these require full caving equipment and expertise to access. The cave has also been important for scientific research, including studies of underground hydrology, cave formation processes, limestone dissolution rates, and even cosmic ray research conducted in the stable, deep underground environment. The stream passage leading from the base of the main chamber has been explored and contains several impressive features, including formations, cascades, and pools. The water temperature remains constantly cold throughout the year, as is typical of cave systems, and the environment supports specialised cave-adapted invertebrates. The main chamber itself contains some breakdown material from roof collapses, though the chamber has remained remarkably stable over the documented period of human exploration. During the public winch meets, the chamber is illuminated, revealing the true scale of this underground cathedral and allowing visitors to appreciate the power of water to dissolve and transport rock over geological time scales.

Mill Scar Lash is a waterfall on the River Wharfe located south of the village of Conistone in the Yorkshire Dales, North Yorkshire, England. The waterfall is positioned at OS grid reference SD979664, corresponding to coordinates 54.093947, -2.032837, placing it within the limestone country that characterizes this section of Wharfedale. The feature represents one of several points where the River Wharfe tumbles over the distinctive Carboniferous limestone geology that dominates the Yorkshire Dales landscape, creating a sequence of ledges and steps as the river continues its journey southward through this scenic valley. The River Wharfe itself is one of Yorkshire's principal watercourses, rising high on the flanks of Cam Fell in the Pennines at an elevation of approximately 500 metres above sea level. From its source, the river flows generally southward and eastward through Upper Wharfedale, passing through Langstrothdale before entering the broader valley section near Kettlewell and continuing past Grassington, Burnsall, and eventually through Ilkley and Otley before joining the River Ouse. The catchment encompasses a significant portion of the Yorkshire Dales, draining an area of mixed moorland, limestone pavements, and agricultural land. By the time the Wharfe reaches the vicinity of Conistone, it has already gathered substantial flow from numerous tributary becks and streams that descend from the surrounding fells. The geological setting of Mill Scar Lash reflects the complex limestone stratigraphy of the region, with the waterfall likely formed where the river crosses resistant beds within the Great Scar Limestone or related Carboniferous formations. These limestones were deposited approximately 330 million years ago in warm, shallow tropical seas and now form the characteristic stepped topography of the area. The action of the river over millennia has exploited joints and bedding planes in the rock, creating the scar—a local term for a limestone cliff or steep rocky face—over which the water cascades. The flow characteristics vary considerably with season and recent rainfall, ranging from a modest trickle during dry summer periods to a powerful surge during winter spates or after prolonged rain in the upper catchment. Conistone itself is a small village situated on the eastern side of the River Wharfe, with a history extending back to medieval times and beyond. The name derives from Old English or Old Norse elements, and the settlement appears in Domesday Book records. The landscape around the waterfall has been shaped by centuries of human activity, including farming, quarrying, and the management of water resources. The "mill" component of Mill Scar Lash may indicate former industrial use of the river's power at or near this location, as watermills were once common features along Yorkshire rivers, serving agricultural communities for grinding corn and other purposes. However, specific historical documentation regarding a mill at this precise location would require consultation of local archives and historical surveys. The surrounding landscape is characteristic of the mid-Wharfedale region, with limestone walls dividing fields used primarily for sheep grazing and some cattle farming. The valley sides rise steeply in places, with patches of woodland—predominantly ash, hazel, and oak—occupying the less accessible slopes and gill ravines. The area supports typical limestone grassland flora where conditions permit, including species such as bird's-foot trefoil, rock-rose, and various fescue grasses. The limestone pavement features that occur nearby provide habitat for specialized plant communities, including hart's-tongue fern and herb robert sheltering in the grikes between the clints. Birdlife includes species common to upland farm country such as curlew, lapwing, and meadow pipit, while dippers and grey wagtails frequent the river itself, feeding on invertebrates in the fast-flowing waters. Access to Mill Scar Lash requires some knowledge of local paths and rights of way, as it is not as heavily promoted as some of the more famous waterfalls in the Yorkshire Dales such as Janet's Foss or Aysgarth Falls. Visitors to Conistone can park in the village, where limited roadside parking is available with consideration for local residents and farm access. The Dales Way, a long-distance footpath that follows much of the length of the River Wharfe from its source to the Humber estuary, passes through this area and provides one potential approach to the waterfall, though precise route-finding may require detailed Ordnance Survey maps of the area. The walking is generally moderate but can be muddy and slippery, particularly after rain, and appropriate footwear is essential given the limestone terrain. The nearest significant facilities are found in Grassington, approximately two miles to the south, which serves as one of the main tourist centers in Wharfedale with shops, cafes, pubs, and visitor information. Kettlewell, a few miles to the north, offers similar amenities on a smaller scale. Both villages provide excellent bases for exploring the central section of Wharfedale and its various natural and historical attractions. The area is within the Yorkshire Dales National Park, established in 1954 to protect and promote the unique landscape, wildlife, and cultural heritage of the region, and visitors are encouraged to follow the Countryside Code, respecting farmland, livestock, and the natural environment.

Thornton-le-Dale near Pickering in the North Yorkshire Moors is consistently voted the most beautiful village in Yorkshire, a settlement of stone cottages along a beck fringed with daffodils in spring and lined with willows in summer. A thatched whitewashed cottage by the beck is one of the most photographed buildings in the north of England, appearing on calendars and in photographic collections of English village scenes with remarkable frequency. The village has the genuine character of a working agricultural settlement rather than a preserved tourist artefact, its residents managing working farms and ordinary village life alongside the considerable visitor interest its reputation generates. The beck flowing through the centre creates the visual element that defines the scene and provides the perpetual gentle sound of flowing water that animates any visit. The stocks on the village green and the medieval market cross provide historical focal points, and the surrounding architecture of limestone and pantile roofs reflects the characteristic building tradition of the North Yorkshire Moors. The North Yorkshire Moors Railway station at Pickering nearby and Dalby Forest to the north provide excellent complementary heritage and outdoor experiences.

Middle Force is the central section of the celebrated Aysgarth Falls, a spectacular triple cascade on the River Ure in Wensleydale, North Yorkshire. This particular drop represents the middle tier of three distinct falls that collectively form one of the most visited natural attractions in the Yorkshire Dales National Park. Middle Force is characterized by a broad, stepped series of limestone shelves over which the Ure tumbles in a powerful display, particularly impressive after periods of sustained rainfall when the river is in spate. The waterfall drops approximately 10 to 13 feet across its width, though the exact height varies depending on water levels and the specific measurement point along the irregular limestone terraces. The rock formations here consist of Yoredale Series limestone and sandstone laid down during the Carboniferous period, creating the distinctive stepped profile that defines all three of the Aysgarth Falls. The River Ure rises on the slopes of Abbotside Common in the high Pennines and flows eastward through the length of Wensleydale, one of the major dales of the Yorkshire Dales. By the time it reaches Aysgarth, the river has gathered waters from numerous tributaries draining the surrounding fells and has developed into a substantial watercourse with a considerable catchment area. The river continues beyond the falls through Wensleydale and eventually joins the River Swale near Boroughbridge to form the River Ouse, which flows to the Humber estuary. The geology of the area means that the river has carved its course through alternating bands of hard limestone and softer shale, creating the natural stepped formations that produce the three-tiered waterfall system at Aysgarth. Middle Force sits between the Upper Falls upstream and the Lower Falls downstream, with all three sections lying within approximately half a mile of river. The Middle Force is often considered by visitors to offer the most dramatic and photogenic views, particularly from the viewing areas on the south bank where the full width and power of the cascade can be appreciated. The limestone ledges create a complex pattern of water flow, with the river splitting into multiple channels during lower flows but becoming a single thundering torrent during flood conditions. The force of the water over thousands of years has carved smooth curves and potholes into the limestone bedrock, and the constant erosion continues to shape the falls today. The Aysgarth Falls have attracted visitors for centuries, and Middle Force in particular gained fame through various artistic and literary associations. The celebrated artist J.M.W. Turner sketched the falls during his tours of Yorkshire in the late 18th century, and his romanticized depictions helped establish Aysgarth as an essential stop on the picturesque tours popular among wealthy travelers of the period. The poet William Wordsworth also visited and mentioned the falls in his writings. More recently, the falls achieved cinematic fame when Middle Force and the surrounding areas featured in the 1991 film "Robin Hood: Prince of Thieves" starring Kevin Costner, with the dramatic fight scene filmed at the waterfall bringing international attention to the location. The landscape surrounding Middle Force is characteristic of the Yorkshire Dales, with ancient broadleaved woodland clinging to the steep valley sides. The Freeholders' Wood on the south bank is particularly notable, being an area of ancient semi-natural woodland containing oak, ash, wych elm, and hazel. This woodland environment supports a rich diversity of wildlife including numerous bird species such as dippers, grey wagtails, and common sandpipers that frequent the river margins. The damp conditions around the falls support lush growths of ferns and mosses on the rock faces, while the surrounding meadows in early summer display traditional hay meadow flowers. The river itself supports populations of brown trout and other fish species, though the falls themselves present a barrier to upstream migration. Access to Middle Force is relatively straightforward, with the falls lying within a short walk from the village of Aysgarth. The main car park operated by the Yorkshire Dales National Park Authority is located near the A684 road close to the parish church and provides the most convenient starting point for visitors. From here, well-maintained footpaths lead down through woodland to viewing points for all three sections of the falls. The path to Middle Force takes visitors through the Freeholders' Wood, descending gradually toward the river with several viewpoints offering different perspectives of the cascade. The paths can be steep in places and may be slippery when wet, so appropriate footwear is recommended. The site is accessible year-round, though the falls are naturally most impressive during winter and spring when water levels are highest. The village of Aysgarth itself offers various facilities for visitors including public toilets near the car park, a National Park Centre (which has historically operated seasonally), and refreshment options. The historic St Andrew's Church in Aysgarth is worth visiting for those interested in heritage, containing a notable rood screen brought from Jervaulx Abbey after the Dissolution of the Monasteries. Several footpaths in the area allow for extended walks combining visits to all three falls, and the location serves as a starting point for longer hikes into the surrounding Wensleydale landscape. There is a small admission charge for the main car park, which helps support the maintenance of paths and facilities. The industrial heritage of the Aysgarth area adds another dimension to the falls' history, as the water power of the Ure was harnessed for various mills over the centuries. Near the Lower Falls, the remains of a former cotton mill can still be seen, later converted to a woolen mill and eventually becoming a museum. While the Middle Force itself was not directly exploited for industrial purposes in the same way, the entire falls system represented a significant concentration of natural power that shaped the economic development of this part of Wensleydale. The preservation of the falls and surrounding woodland for public enjoyment represents a triumph of conservation over industrial exploitation, ensuring that Middle Force continues to cascade as it has for millennia, delighting visitors with its natural beauty and raw power.

Malham Cove in the Yorkshire Dales is one of the most dramatic natural features in England, a curved limestone cliff 80 metres high and approximately 300 metres wide that was formed as a waterfall at the end of the last Ice Age when meltwater cascading over the limestone edge of the Craven fault created the massive curved face visible today. The stream that once fell over the lip of the cove now disappears underground at the top of the cliff and re-emerges at the base through the cave system within the limestone, and the dry cliff face and the limestone pavement at its summit create a landscape of stark and powerful beauty that is entirely unlike the pastoral character of the surrounding Dales. The limestone pavement at the top of the cove is one of the finest examples in Britain, its surface of large flat slabs called clints, separated by deep fissures called grykes, extending for some distance back from the cliff edge. The grykes provide a sheltered and humid microclimate in which ferns, rare limestoneloving plants and wood-land species grow in conditions quite different from the exposed pavement surface, creating a botanical diversity compressed into a small area. The pavement is a protected landscape feature and walking on it is permitted only on designated routes. The approach to Malham Cove from the village of Malham follows the dry valley of Malham Beck through classic Yorkshire Dales limestone scenery, and the cliff face itself provides a high-quality rock climbing venue whose routes include some of the finest limestone climbs in the north of England. The natural amphitheatre formed by the curved cliff concentrates sound and creates a particular acoustic quality noticeable even in moderate wind conditions. The broader Malham landscape, including Malham Tarn above and Gordale Scar nearby, provides one of the most concentrated collections of outstanding limestone features available within a single short walking circuit in Britain.

Helmsley is the finest market town in the North Yorkshire Moors National Park, a stone town of considerable charm surrounding a market square that provides the principal visitor centre for the southern section of the moors. The combination of the ruined medieval castle, the walled garden, the excellent independent shops and restaurants and the access it provides to the walking of the Cleveland Way and the Tabular Hills makes Helmsley the most complete and most welcoming base for exploring the western North Yorkshire Moors. Helmsley Castle, managing by English Heritage, is a castle of considerable historical depth whose ruined towers and keep provide excellent views over the town and the surrounding countryside, and the unusual combination of the medieval fortification with the substantial domestic range that was added in the sixteenth century by the Manners family reflects the transition of this castle from a purely military function to a comfortable aristocratic residence. The earthwork defences that surround the castle are among the most complete and best-preserved of any English castle. The Helmsley Walled Garden, restored from dereliction since 1994 by a charitable trust, provides one of the finest examples of a Victorian walled garden restoration in Yorkshire, its productive beds, glasshouses and ornamental sections creating an excellent horticultural visit complementary to the castle. The Ryedale Folk Museum at nearby Hutton-le-Hole and the ruins of Rievaulx Abbey seven miles to the northwest provide excellent complementary heritage destinations for a base at Helmsley.

The North Yorkshire Moors Railway is one of the finest heritage railways in Britain, a line of outstanding scenic character that runs for 18 miles from Pickering through the heart of the North York Moors National Park to Grosmont, where it connects with the main Esk Valley line to Whitby. The combination of exceptional moorland scenery, a well-preserved Victorian railway infrastructure and the atmospheric experience of travelling behind a steam locomotive makes it one of the most popular heritage attractions in the north of England. The railway's origins lie in the Whitby to Pickering Railway opened by George Stephenson in 1836, one of the earliest railways in the world, which originally used horse traction for much of its length before being converted to steam. The line was incorporated into the North Eastern Railway and eventually into British Railways, but declining passenger numbers and freight revenue led to its closure under the Beeching cuts in 1965. The North Yorkshire Moors Railway Preservation Society purchased and reopened the line in 1973, and it has been operated by volunteers and professional staff ever since as one of Britain's great examples of railway preservation. The route is spectacular throughout its length. Departing Pickering, a market town with a Norman castle and a good range of visitor facilities, the line climbs steadily through the Newtondale gorge, a dramatic valley carved by glacial meltwater that provides some of the finest scenery on the line. The station at Goathland, used as Hogsmeade station in the Harry Potter films, is one of the most visited on the line and sits within a particularly beautiful section of moorland. Continuing north the line drops to Grosmont through Newtondale before reaching the Esk Valley. The railway operates primarily with steam locomotives from its impressive collection of mainly 1920s to 1960s British steam engines, though diesel locomotives also feature on the timetable. Special event days including evening Pullman dining trains, wartime recreation weekends and Santa specials throughout December attract additional visitors throughout the year. An extension of the heritage railway service beyond Grosmont to Whitby using the Network Rail Esk Valley line has been operated seasonally, providing the opportunity to travel from Pickering all the way to the coast by heritage and Network Rail services without using a car.

Black Foss Waterfall is a modest but attractive cascade located on West Hall Beck in the parish of Addingham, nestled within the scenic Wharfedale valley in West Yorkshire, England. The waterfall tumbles over a series of gritstone ledges, creating a stepped descent rather than a single dramatic plunge. The character of the falls varies considerably with seasonal rainfall and snowmelt from the surrounding moorland, ranging from a gentle trickle during dry summer months to a more vigorous torrent following periods of sustained precipitation. The dark millstone grit rock from which the waterfall takes its name—"foss" being an Old Norse term for waterfall—forms irregular shelves that break the water's descent into multiple tiers, creating pools and eddies that catch the light filtering through the overhanging trees. West Hall Beck rises on the moorland heights above Addingham, drawing its waters from the peaty uplands that characterize much of the South Pennines. The beck flows generally southward through a wooded valley before joining the River Wharfe in the vicinity of Addingham village. The catchment area is relatively small, comprising rough grazing land, heather moorland, and pockets of woodland, which means the beck's flow can respond rapidly to changing weather conditions. The geology of the area is dominated by Carboniferous millstone grit and coal measures, the resistant sandstones forming the characteristic stepped profiles of many waterfalls in the Yorkshire Dales region. These rocks were laid down approximately 320 million years ago in deltaic environments, and their durability has created the natural architecture that shapes Black Foss. The surrounding landscape reflects the transition zone between the farmed valley floor of Wharfedale and the wilder moorland plateau above. Ancient oak and birch woodland clings to the steeper valley sides around the waterfall, creating a shaded, humid environment that supports a diverse community of ferns, mosses, and lichens. The rocky substrate and spray zone immediately around the falls provide ideal conditions for moisture-loving species, while the beck itself supports invertebrate communities that form the base of the local food web. Dippers and grey wagtails are among the bird species that may be observed along the beck, both being characteristic inhabitants of fast-flowing upland streams. The woodland provides habitat for typical British woodland birds, and the surrounding moorland supports populations of ground-nesting species during the breeding season. Addingham itself is an ancient settlement with a history stretching back to at least Anglo-Saxon times, and the surrounding landscape bears the marks of centuries of human activity. The area's industrial heritage is particularly significant, as the combination of water power, local wool production, and accessible coal deposits made Wharfedale an important centre for textile manufacturing during the Industrial Revolution. While Black Foss itself does not appear to have been harnessed for industrial purposes in the way that many larger waterfalls in the region were, the beck and its tributaries powered numerous mills in the valley below. The footpaths that now provide recreational access often follow routes that were once used for transporting goods and driving livestock to and from the moorland commons. Access to Black Foss Waterfall is typically achieved via public footpaths that lead north from Addingham village toward the moorland edge. The village itself offers parking facilities, and several well-established walking routes extend into the surrounding countryside, allowing visitors to combine a visit to the waterfall with a more extensive exploration of Wharfedale's landscape. The paths can be steep and potentially slippery, particularly in wet conditions, so appropriate footwear is advisable. Addingham provides basic amenities including public houses and shops, making it a convenient base for walks in the area. The waterfall sits within a landscape that is freely accessible thanks to traditional rights of way and, in some areas, access land designated under the Countryside and Rights of Way Act. The name "Black Foss" likely derives from the dark appearance of the wet millstone grit over which the water flows, a common naming pattern in the Pennines where "black" features often reference the color of exposed rock or peat-stained water. The topographic setting is characteristic of the Yorkshire Dales' eastern margins, where the distinctive stepped profiles of millstone grit edges create dramatic transitions between the valley systems and the moorland plateaux above. While Black Foss may not rival the height or fame of more celebrated Yorkshire waterfalls such as Hardraw Force or Aysgarth Falls, it possesses an intimate charm that appeals to those seeking quieter corners of the Dales landscape. The waterfall represents one of numerous small cascades that punctuate the becks draining from the Pennine uplands, each contributing to the intricate hydrology and distinctive character of this well-loved region.

Acroy Gill Force is a secluded waterfall tucked away in the remote upper reaches of Cotterdale, a quiet side valley branching off from Wensleydale in the Yorkshire Dales National Park. The waterfall occurs where Acroy Gill, a modest moorland stream, tumbles over a series of rock ledges in the characteristic Yoredale Series geology that defines much of the upper dale landscape. The falls are modest in scale but possess a wild charm typical of the higher Pennine valleys, with the water cascading through a narrow rocky cleft surrounded by rough grazing land and upland vegetation. The exact height and character of the drop can vary considerably with seasonal water levels, as Acroy Gill is fed primarily by rainfall and drainage from the surrounding fells, meaning it can swell to an impressive torrent after heavy rain or dwindle to a modest trickle during dry summer months. Acroy Gill itself rises on the moorland slopes that form the watershed between Cotterdale and the parallel valleys to the north and west. The stream flows generally southeastward, gathering water from a catchment of rough pasture, heather moorland, and boggy ground typical of the Pennine uplands at this elevation. The beck is one of several small tributary streams that feed into the River Baugh, which in turn joins the River Ure further down Wensleydale. The entire watercourse is relatively short, perhaps only two or three kilometres from source to confluence, but it drains an area of wild, largely unimproved upland that retains much of its natural character. The valley through which Acroy Gill flows is steep-sided and exhibits the classic U-shaped profile associated with glacial activity during the last ice age, though subsequent fluvial erosion has modified the valley floor. Cotterdale itself is one of the most isolated and least-visited side valleys of the Yorkshire Dales, lying roughly midway between Hawes and Kirkby Stephen, accessed via narrow moorland roads that branch off from the main Buttertubs Pass route. The dale has long been associated with farming, with scattered stone farmsteads clinging to the valley sides, some dating back several centuries. The landscape around Acroy Gill Force remains largely agricultural, with traditional stone walls dividing rough pastures where sheep graze throughout much of the year. The remoteness of the location has preserved a sense of wildness and solitude that has largely disappeared from the more accessible parts of the National Park. There is little recorded folklore specific to Acroy Gill Force, which reflects the falls' modest size and isolated position away from major packhorse routes or settlements, though the wider Cotterdale area shares in the general traditions of the Dales farming communities. The ecology of the area around the waterfall is characteristic of upland Pennine habitats, with acidic grassland, scattered rushes, and areas of blanket bog on the higher ground. The stream itself, being relatively unpolluted and fast-flowing, supports invertebrate populations typical of clean upland waters, which in turn provide food for dipper and grey wagtail, both species commonly seen along Pennine becks. The surrounding moorland is habitat for meadow pipit, skylark, and curlew, while the stone walls and scattered trees near lower-lying farms provide shelter for smaller passerines. Red grouse may be encountered on the higher moors, and the area lies within the range of various upland raptors including kestrel and buzzard. During the flowering season, the streamside vegetation includes various mosses, liverworts, and ferns that thrive in the damp, shaded conditions near the waterfall. Access to Acroy Gill Force requires a degree of determination and navigational skill, as there are no signposted paths directly to the falls and the location lies well away from established walking routes. Visitors typically approach Cotterdale via the minor road that runs up the valley from the Buttertubs Pass road, itself a dramatic moorland route between Hawes and Thwaite. Parking is extremely limited and must be undertaken with consideration for farm access and the narrow nature of the road; most visitors find suitable pull-offs near farm gates or field entrances, always ensuring they do not obstruct agricultural vehicles. From the nearest practical parking points, reaching the waterfall involves walking across rough pasture land, and visitors should be aware that much of this is private farmland where access may not be formally designated, though the traditional culture of the Dales generally permits respectful passage on foot. Good waterproof boots are essential as the ground can be boggy and the terrain is uneven, with tussocky grass and hidden drainage channels presenting potential hazards. The nearest facilities of any kind are in Hawes, some five to six miles away depending on the exact starting point, where visitors can find accommodation, pubs, shops, and the Dales Countryside Museum. The tiny hamlet of Cotterdale itself consists only of scattered farms with no public amenities. Those exploring this area should be fully self-sufficient with appropriate clothing, footwear, food, and water, and should carry a detailed Ordnance Survey map and compass or GPS device, as mobile phone signal is unreliable at best in this remote location. The best time to visit is during settled weather between late spring and early autumn, as winter conditions can make the high moorland approach routes treacherous, and snow can linger into April in particularly exposed locations. After heavy rain, Acroy Gill comes into its most impressive form, but this also makes the surrounding ground extremely wet and difficult to traverse. The industrial heritage of the wider area includes the lead mining that once flourished in the Yorkshire Dales, though Cotterdale itself was not a major centre of this activity compared to valleys further south. The landscape still bears subtle traces of past industry in the form of old quarries and limekilns, with lime burning having been important for agricultural improvement in the 18th and 19th centuries. The stone walls that characterize the dale represent centuries of agricultural labour, with many dating from the Parliamentary Enclosure period of the late 18th and early 19th centuries when the open moorland was divided into the pattern of fields that persists today. The traditional farming practices that shaped this landscape continue in modified form, with sheep farming remaining the dominant land use and the dale retaining its essential agricultural character despite the pressures facing upland farming communities across Britain.

Mallyan Spout is a striking waterfall located in the wooded valley of West Beck, near the village of Goathland in the North York Moors National Park. The waterfall drops approximately 70 feet (21 meters) in a single impressive plunge over a ledge of hard sandstone, creating one of the tallest waterfalls in the North York Moors. The water cascades down a moss-covered rock face into a deep pool below, with the fall often appearing as a silvery ribbon against the dark rock, particularly dramatic after periods of heavy rainfall when the beck is in spate. The geological formation consists of Middle Jurassic sandstone and shale beds, with the harder sandstone cap rock creating the resistant ledge over which the water tumbles, while softer rocks beneath have been eroded away over millennia to form the deep amphitheater at the base of the fall. West Beck rises on the moorland to the south of Goathland and flows northward through a steep-sided wooded valley before eventually joining Eller Beck and contributing to the River Esk system. The catchment area encompasses heather moorland and improved pasture, with the beck's flow varying considerably between seasons. During dry summer periods, Mallyan Spout can reduce to a modest trickle, but winter rains and snowmelt can transform it into a thundering torrent that fills the narrow gorge with spray and sound. The stream has carved a distinctive V-shaped valley through the landscape, with the waterfall representing a classic example of a rejuvenation feature where the beck encountered resistant rock during its downcutting process. The waterfall has been a noted beauty spot since at least the Victorian era, when the expansion of the railway network brought tourists to the North York Moors in increasing numbers. The name "Mallyan Spout" is thought to derive from a local dialect word, with "spout" being a common Yorkshire term for a waterfall or cascade. While not as steeped in dramatic legend as some Yorkshire waterfalls, the secluded setting and the atmospheric woodland surroundings have long contributed to the fall's romantic appeal. The area around Goathland became particularly popular with artists and writers during the nineteenth century, drawn by the picturesque combination of moorland scenery, ancient stone crosses, and natural features like Mallyan Spout. The surrounding landscape consists of ancient semi-natural woodland dominated by oak, birch, and rowan, with an understory rich in ferns, mosses, and liverworts that thrive in the humid conditions created by the waterfall's spray. The rocky gorge provides habitat for species adapted to cool, damp conditions, including various fern species that colonize the cliff faces. The woodland is home to typical North York Moors fauna including roe deer, red squirrels, and a variety of woodland birds such as woodpeckers, nuthatches, and woodland warblers during summer months. The beck itself supports populations of brown trout and aquatic invertebrates, though like many upland streams in the area, it can be affected by acidification from surrounding moorland drainage. Access to Mallyan Spout is via a well-established footpath that descends from Goathland village through the woodland to the base of the waterfall, a walk of approximately half a mile that takes fifteen to twenty minutes. The path begins near the Mallyan Spout Hotel in the village and follows a series of steps down through the woods, crossing West Beck via a footbridge before reaching the viewing area at the foot of the falls. While the descent is not particularly long, the path can be steep, uneven, and slippery, especially after rain, and proper footwear is recommended. The route is part of the wider network of paths in the area, and Mallyan Spout can be incorporated into longer circular walks exploring the Goathland area. Goathland village itself offers visitor facilities including the Mallyan Spout Hotel, other accommodation options, a tea room, and a village shop. Parking is available in the village, though spaces can be limited during peak tourist season, particularly when the North Yorkshire Moors Railway is running services. The village is accessible by car via minor roads from the A169, and also by the heritage railway, which stops at Goathland station. The station and village achieved additional fame as filming locations for the television series "Heartbeat" (where Goathland doubled as the fictional village of Aidensfield) and the Harry Potter films (with Goathland station serving as Hogsmeade station), which has increased visitor numbers in recent decades. The waterfall and surrounding woodland are located within the North York Moors National Park, and the area is managed to balance conservation objectives with recreational access. The woodland around Mallyan Spout has been designated as ancient woodland, indicating that it has been continuously wooded since at least 1600 AD and likely for much longer. This continuity of woodland cover contributes to the site's ecological value and its atmospheric character. The geological and geomorphological interest of the waterfall and gorge also contributes to the scientific value of the site, illustrating processes of stream erosion and landscape evolution in the North York Moors.

Keld Scar is a notable waterfall located on Gill Beck in the remote and sparsely populated area of Raydale in the Yorkshire Dales, specifically near the hamlet of Stalling Busk. This waterfall represents one of the lesser-known but geologically significant features in the Upper Wensleydale area of North Yorkshire, England. The fall occurs where Gill Beck descends through a limestone gorge, creating a dramatic cascade that varies considerably in character depending on seasonal water levels. During periods of heavy rainfall or snowmelt, the waterfall becomes a powerful torrent, while in drier summer months it may reduce to a more modest flow trickling over the rock face. The surrounding geology consists primarily of Carboniferous limestone, part of the Yoredale Series that characterizes much of the Yorkshire Dales, with the waterfall having been carved over millennia through the erosive action of the beck cutting through these ancient sedimentary rocks. Gill Beck itself is a tributary system that drains the moorland areas to the north of Raydale, flowing southward through the agricultural landscape before eventually joining the River Bain. The catchment area for Gill Beck encompasses rough grazing land and upland pastures, with the stream gathering water from numerous smaller tributaries and springs emerging from the limestone geology. The beck's course takes it through typical Dales scenery of stone-walled fields and traditional hay meadows before it reaches the more dramatic section at Keld Scar where the topography steepens. The River Bain, which Gill Beck feeds into, holds the distinction of being one of the shortest named rivers in England, flowing just a couple of miles from Semerwater to its confluence with the River Ure. The landscape surrounding Keld Scar exemplifies the characteristic scenery of the Yorkshire Dales, with rolling hills, limestone scars, and traditional field patterns created by drystone walls. Stalling Busk itself is a tiny settlement that sits on the hillside above Raydale, with a handful of farms and cottages representing centuries of continuous habitation in this challenging upland environment. The area has been shaped by both natural geological processes and human activity, particularly traditional farming practices that have maintained the distinctive patchwork of enclosed pastures and hay meadows. The hamlet's name derives from Old Norse origins, reflecting the Viking settlement of this region during the early medieval period, with "Busk" likely referring to a bush or small wood, and "Stalling" possibly relating to a site where animals were kept. The ecology around Keld Scar and Gill Beck is typical of upland limestone areas in the Yorkshire Dales, with specialized plant communities adapted to the alkaline soils and exposed conditions. The beck itself supports aquatic invertebrates and may provide habitat for brown trout in its deeper pools, while the surrounding grasslands contain species-rich hay meadows where traditional management has been maintained. Bird species characteristic of the area include curlews, lapwings, and meadow pipits on the open ground, while the wooded sections along the beck may shelter grey wagtails, dippers, and common sandpipers. The limestone outcrops and scar features provide nesting sites for various species and support distinctive limestone-loving flora in their crevices and ledges. Access to Keld Scar requires walking across farmland, and visitors should be mindful of the working agricultural landscape, keeping to recognized paths and ensuring gates are closed behind them. The waterfall can be reached from Stalling Busk by following footpaths that lead down toward Gill Beck, though the exact route requires careful navigation using Ordnance Survey maps, as this is not a heavily waymarked tourist destination. Parking in the immediate vicinity is extremely limited, with the nearest options being considerate roadside parking near Stalling Busk itself, taking care not to obstruct farm access or narrow lanes. The walk to the waterfall involves crossing typical Dales terrain, which can be muddy and slippery, particularly after rain, so appropriate footwear is essential. The nearest substantial settlements with facilities are Bainbridge, approximately two miles to the east, which offers a shop and pub, and the market town of Hawes, about five miles to the west, which provides a fuller range of services including accommodation, cafes, and outdoor equipment shops. Raydale and Stalling Busk occupy a particularly tranquil corner of the Yorkshire Dales, well away from the main tourist routes that concentrate on more famous attractions like Aysgarth Falls or Hardraw Force. This relative obscurity means that Keld Scar receives far fewer visitors than its better-known counterparts, offering a more solitary experience for those willing to make the effort to reach it. The surrounding area is steeped in the history of upland farming, with the landscape bearing witness to centuries of human endeavor in making a living from these challenging hills. Traditional field barns dot the landscape, many now disused but serving as reminders of the pre-mechanized farming system where each field had its own barn for storing hay and overwintering cattle.

Nelly Ayre Foss is a picturesque waterfall located on West Beck in the village of Goathland on the North York Moors in North Yorkshire, England. The waterfall is situated at OS grid reference SE813996, in a wooded section of the beck that flows through this moorland landscape. While not among the tallest waterfalls in the region, Nelly Ayre Foss presents an attractive cascade where the water tumbles over sedimentary rock formations characteristic of the North York Moors, creating a series of stepped falls and pools. The appearance and flow of the waterfall vary considerably with seasonal rainfall, being most impressive after periods of wet weather when West Beck swells with runoff from the surrounding moorland. West Beck is one of several watercourses that drain the upland areas around Goathland, flowing generally northward through the village and its environs. The stream gathers water from the surrounding moorland catchment, an area dominated by heather moorland, rough grassland, and patches of woodland. The beck's course takes it through varied terrain, creating several waterfalls and cascades as it descends from the higher moorland toward lower elevations. The geology of the area consists primarily of Jurassic sedimentary rocks, including sandstones and shales, which have been eroded over millennia to create the valleys and watercourses visible today. The name "Nelly Ayre Foss" reflects the traditional Yorkshire dialect term "foss" or "force" for waterfall, derived from Old Norse, a linguistic legacy of the Viking settlement of this region. The origins of the "Nelly Ayre" component of the name are less certain, though such place names often commemorate local individuals or refer to landscape features that have been lost to time. Goathland itself has a rich history, with evidence of human settlement dating back to prehistoric times, and the area's becks and waterfalls would have been familiar landmarks to generations of local residents, farmers, and travelers crossing the moors. The landscape surrounding Nelly Ayre Foss is typical of the North York Moors, combining moorland, woodland, and improved pasture. The wooded sections along West Beck provide habitat for a variety of bird species, including common woodland birds such as wrens, robins, and various tits, while the beck itself supports aquatic invertebrates and, in suitable conditions, fish. The surrounding moorland is home to ground-nesting birds and supports the characteristic vegetation of upland Britain, including heather, bilberry, and various grasses and sedges. Red grouse are present on the managed heather moorland in the wider area, and visitors may occasionally spot roe deer in the wooded valleys. Goathland village is perhaps best known to modern visitors as a filming location for the television series "Heartbeat," where it doubled for the fictional village of Aidensfield, and for its railway station, which appeared as Hogsmeade Station in the Harry Potter films. This media exposure has brought many visitors to the area, and while Nelly Ayre Foss may be less famous than some of the village's other waterfalls, it forms part of the network of attractive walking routes in and around Goathland. The village itself has maintained much of its traditional character, with scattered farmsteads and stone buildings across the wide village green. Access to Nelly Ayre Foss typically involves walking from Goathland village, where parking is available in designated areas including near the church and at other points around the village. Various circular walking routes from Goathland take in West Beck and its waterfalls, and the area is well-served by public footpaths. The North York Moors National Park maintains information about walking routes in the area, and local maps and guidebooks provide details of circular walks that can include multiple waterfalls and points of interest. The village has basic facilities including a pub, tea rooms, and shops, making it a practical base for exploring the local waterfalls and moorland. The waterfall is part of the broader appeal of Goathland as a destination for those seeking the natural beauty of the North York Moors. While it may not be individually as celebrated as some larger or more accessible waterfalls in the region, it contributes to the cumulative charm of the area's water features. The combination of moorland walking, woodland paths, and the various cascades along the local becks provides visitors with a genuine sense of the North York Moors landscape and its distinctive character shaped by geology, climate, and centuries of human land management.

Scaleber Force is a picturesque waterfall located on Scaleber Beck in the Yorkshire Dales, situated to the east of the historic market town of Settle in North Yorkshire, England. The falls tumble over limestone bedrock characteristic of this karst landscape, dropping in a series of cascades through a wooded ravine. The waterfall is most impressive following periods of heavy rainfall when Scaleber Beck swells with runoff from the surrounding fells, though during drier summer months the flow can diminish considerably to a gentle trickle over the exposed rock face. The limestone geology creates interesting formations where the water has carved and smoothed the pale grey stone over millennia, with solution features and small pools forming in the channel both above and below the main drop. Scaleber Beck rises on the moorland slopes to the northeast of Settle, gathering water from a modest catchment area in the limestone uplands. The stream flows generally southwestward through a landscape dominated by典型limestone pavement, dry valleys, and scattered farmland before reaching Scaleber Force. Beyond the waterfall, the beck continues its journey toward its eventual confluence with larger watercourses in this part of the Craven district. The catchment characteristics mean that water levels can fluctuate significantly, with the permeable limestone allowing rapid drainage during dry periods but also contributing to swift rises during wet weather as water emerges from underground channels and springs. The wooded glen surrounding Scaleber Force provides a sheltered habitat that contrasts with the more open pastoral landscape of the surrounding area. Native broadleaved trees including ash, hazel, and oak cling to the steeper slopes of the ravine, while ferns and mosses thrive in the damp microclimate created by the falling water. This type of gill woodland is valuable for biodiversity in the Yorkshire Dales, providing cover and feeding opportunities for birds such as grey wagtails, dippers, and various woodland species. The beck itself, when flowing well, supports aquatic invertebrates adapted to the calcium-rich waters typical of limestone streams. The waterfall lies within the broader landscape context of the Yorkshire Dales, an area renowned for its distinctive limestone scenery, cave systems, and upland character. The proximity to Settle places Scaleber Force within reach of a town that has long been a gateway to the Dales, historically important as a market centre and later as a stop on the renowned Settle-Carlisle Railway. The surrounding countryside is characterized by dry stone walls dividing fields, scattered farmsteads, and the dramatic scars and pavements that make this area geologically significant. Visitors to the waterfall are walking in a landscape shaped by both natural processes and centuries of pastoral farming. Access to Scaleber Force typically involves a walk from Settle, with the waterfall lying approximately a mile or so to the east of the town centre. Public footpaths cross the countryside in this direction, though visitors should be prepared for typical Dales walking conditions including potentially muddy paths, stiles, and uneven terrain. Parking is generally available in Settle itself, where there are public car parks serving the town, and the walk to the waterfall can form part of a pleasant circular route exploring the landscape east of the settlement. The paths may cross private land where access is permitted via rights of way, so walkers should follow the established routes and respect the countryside code. Settle itself provides facilities for visitors including shops, cafes, pubs, and accommodation, making it a convenient base for exploring this and other local attractions. The town has a long history dating back to medieval times and retains much character in its market square and surrounding streets. For those interested in combining a visit to Scaleber Force with other activities, the area offers numerous walking opportunities, from gentle valley strolls to more challenging fell walks, as well as the chance to explore the notable geological and archaeological features of the Craven district. The limestone country surrounding Scaleber Force has been shaped by both natural erosion and human activity over thousands of years. Evidence of past settlement and industry can be found throughout this landscape, from prehistoric remains to the traces of more recent farming and mineral extraction. While Scaleber Force itself is primarily a natural feature appreciated for its scenic qualities, it exists within this richly layered landscape where nature and culture have long been intertwined. The waterfall represents one of many such features that contribute to the special character of the Yorkshire Dales, an area designated as a National Park in recognition of its outstanding natural beauty and cultural heritage.

Currack Force is a notable waterfall on Stonesdale Beck in the hamlet of Keld, located in the upper reaches of Swaledale in the Yorkshire Dales National Park, England. This waterfall forms part of a remarkable concentration of waterfalls in the Keld area, which has earned the settlement its reputation as one of the most scenic locations in the northern Yorkshire Dales. The name "Force" derives from the Old Norse word "foss," meaning waterfall, reflecting the Viking heritage of this remote dale. Currack Force tumbles over limestone and sandstone strata that characterize the geology of this part of the Pennines, creating a cascade that varies in character depending on seasonal water levels, from a delicate veil during dry summer months to a thundering torrent after heavy rainfall in the fells. Stonesdale Beck rises high on the moorland between Great Shunner Fell and the watershed with Wensleydale, gathering water from an extensive upland catchment characterized by blanket bog, rough grassland, and exposed gritstone. The beck flows eastward through the secluded valley of Stonesdale before reaching Keld, where it contributes to the remarkable series of waterfalls that mark its confluence with the River Swale. The stream's course through the upper valley is relatively gentle, but as it approaches Keld, the underlying geology creates a series of stepped falls and rapids where the water encounters bands of harder rock. Currack Force represents one of these dramatic descents where the beck has carved through the layered Carboniferous rocks over millennia. The immediate surroundings of Currack Force exemplify the characteristic landscape of upper Swaledale, with traditional stone field barns dotting the valley sides and dry stone walls creating an intricate pattern across the hillsides. The riverside vegetation includes ash, rowan, and hazel, with shade-loving ferns and mosses thriving in the spray zone near the waterfall. The upland areas around the beck's catchment support typical moorland birds including curlew, lapwing, and red grouse, while the wooded gullies and riverside habitats provide shelter for smaller woodland species. The beck itself supports invertebrate life adapted to fast-flowing upland streams, and the water quality remains generally good despite historic lead mining activities in the broader Swaledale area. Keld sits at the meeting point of several long-distance footpaths, making the area around Currack Force accessible to walkers exploring this network of trails. The Pennine Way, Coast to Coast Walk, and Herriot Way all pass through or near Keld, bringing visitors who often explore the local waterfalls as part of their journey. The settlement itself is small, consisting of a handful of stone-built houses and farm buildings, with limited facilities including a seasonal café and accommodation options for walkers. The remote character of Keld has been preserved partly through its lack of through roads, and the community maintains strong connections to traditional hill farming practices that have shaped this landscape for centuries. Access to Currack Force typically involves walking from Keld village, though the exact approach depends on which waterfall circuit visitors choose to follow. Several circular walks from Keld take in multiple waterfalls on both Stonesdale Beck and the River Swale, with paths that can be muddy and uneven, particularly after wet weather. Parking in Keld itself is extremely limited, with only a small parking area serving visitors to this popular walking destination, and many walkers approach Keld from nearby Muker or Thwaite where more extensive parking facilities exist. The terrain around the waterfalls requires appropriate footwear and caution, especially when rocks are wet and slippery, and some viewpoints involve steep or exposed sections. The landscape of upper Swaledale bears witness to centuries of human activity, from Norse settlement patterns evident in place names and field systems to the extensive lead mining industry that flourished particularly during the eighteenth and nineteenth centuries. While Stonesdale Beck itself was less directly affected by industrial mining than some adjacent valleys, the broader landscape contains numerous spoil heaps, levels, and ruined infrastructure from this extractive past. The traditional agricultural economy based on sheep farming and haymaking continues to define the cultural landscape, with the traditional field barns serving as distinctive features throughout Swaledale. These historic buildings originally provided winter shelter and fodder storage for livestock, and many are now protected structures that contribute to the dale's special character. The waterfalls around Keld have attracted visitors for generations, though the area has never developed the intensive tourist infrastructure seen at some more accessible Yorkshire Dales destinations. The combination of dramatic scenery, challenging walking routes, and relative remoteness appeals particularly to serious walkers and those seeking a more authentic experience of the northern Pennines. Photography enthusiasts are drawn to the area by the combination of falling water, limestone geology, and the play of light in the wooded ravines, with conditions changing dramatically between seasons and even throughout a single day as weather patterns sweep across the fells.

Robin Hood's Bay is one of the most picturesque and most visited fishing villages on the Yorkshire coast, a steeply tiered settlement of red-roofed cottages packed into a narrow ravine that descends from the cliff top to the beach below in a composition of extraordinary visual charm that makes it one of the most photographed villages in the north of England. The village has no connection with the legendary outlaw whose name it bears, the origin of the name remaining obscure, but its character as a former fishing and smuggling community on a remote section of the North Yorkshire coast gives it a historical atmosphere that complements its natural beauty. The village descends steeply from the main road parking area to the beach below on a single, very narrow road flanked by the close-packed cottages of the fishing community, their doors, windows and small gardens creating a human-scaled streetscape of considerable intimacy. The narrowness of the space between the buildings, the steepness of the descent and the sound of the sea growing louder as you approach the beach create an experience of progressive revelation characteristic of the finest English seaside villages. At the bottom, the rocky shore opens out and the wide expanse of the bay, enclosed by the headlands of North Cheek and the cliffs toward Whitby to the north, provides a rewarding contrast to the enclosed village. The beach and the rock pools exposed at low tide provide excellent fossil hunting, the alum shales of the Yorkshire coast having produced ichthyosaur and other Jurassic marine reptile remains over many years of collecting by both professional and amateur palaeontologists. Robin Hood's Bay is the eastern terminus of the Coast to Coast walk, Alfred Wainwright's 192-mile crossing of England from St Bees in Cumbria, and arriving walkers traditionally complete their journey by dipping their boots in the sea on the beach below the village.