Helvellyn from the air in December. Red Tarn (centre) is flanked by Striding Edge (left)
and Swirral Edge
|Elevation||950 m. (3,118 ft)|
|Prominence||712 m (2,336 ft)|
|Parent peak||Scafell Pike|
|Listing||Furth, Marilyn, Hewitt, Nuttall, Historic County Top, Wainwright, Birkett|
|English translation||Pale yellow moorland|
|Language of name||Cumbric|
|Parent range||Lake District, Eastern Fells|
|Topo map||OS Landrangers 90, Explorer OL5|
Helvellyn (//; possible meaning: pale yellow moorland) is a mountain in the English Lake District, the highest point of the Helvellyn range, a north–south line of mountains to the north of Ambleside, between the lakes of Thirlmere and Ullswater.
Helvellyn is the third-highest point both in England and in the Lake District, and access to Helvellyn is easier than to the two higher peaks of Scafell Pike and Sca Fell. The scenery includes three deep glacial coves and two sharp-topped ridges on the eastern side (Striding Edge and Swirral Edge). Helvellyn was one of the earliest fells to prove popular with walkers and explorers; beginning especially in the later 18th century. Among the early visitors to Helvellyn were the poets Samuel Taylor Coleridge and William Wordsworth, both of whom lived nearby at one period. Many routes up the mountain are possible so that it may be approached from all directions.
However, traversing the mountain is not without dangers; over the last two hundred years there have been a number of fatalities. The artist Charles Gough is more famous for his death on Striding Edge in 1805 than for what he achieved in his life. Among many human feats upon the mountain, one of the strangest was the landing and take-off of a small aeroplane on the summit in 1926. Since early 2018 the summit of Helvellyn including both Striding and Swirral Edges and the wider Glenridding Common are now managed by the John Muir Trust, a wild places conservation charity under a three-year lease with the Lake District Park Authority.
The volcanic rocks of which the mountain is made were formed in the caldera of an ancient volcano, many of them in violently explosive eruptions, about 450 million years ago during the Ordovician period. During the last ice age these rocks were carved by glaciers to create the landforms seen today.
Since the end of the last ice age, small populations of arctic-alpine plants have survived in favourable spots on rock ledges high in the eastern coves. Rare to Britain species of alpine butterfly, the mountain ringlet, also live on and around Helvellyn.
The top of Helvellyn is a broad plateau, trending roughly from north-west to south-east for about a kilometre between Lower Man and the start of Striding Edge. Throughout this distance it remains more than 900 m (3,000 ft) high. To the west the ground drops gently at first but then more steeply down to Thirlmere, while on the eastern side three deep glacial coves, each backed by high cliffs, are separated by two spectacular sharp ridges or arêtes. The middle of these coves contains Red Tarn.
Streams on the west side drain directly into Thirlmere, apart from Helvellyn Gill which flows into a parallel valley to the east of Great How and empties into St John's Beck. However, when Thirlmere reservoir was built, a leat was constructed to capture the water of Helvellyn Gill, so that it is now directed into the reservoir.
A never-failing spring called Brownrigg Well exists 90 m (300 ft) below the summit of Helvellyn, about 500 m (550 yd) due west of the highest point, at the head of Whelpside Gill. In the nineteenth century a leat was constructed to direct the water of this spring into the gill to its north to serve the needs of the Helvellyn Mine further down. This leat has now fallen into disuse. The gill it led to is not named on any map, but some authors have referred to it as Mines Gill.
Whelp Side, between Whelpside Gill and Mines Gill, appears as a distinct shoulder of the mountain when seen from the west, largely grassy though with a few crags and boulders in places, and with coniferous plantations on its lower slopes which were planted to stabilise the land around the reservoir. North of Mines Gill are the Helvellyn Screes, a more craggy stretch of hillside, beneath the north-west ridge, with a loose scree covering in places.
The deep coves on the rocky eastern side of Helvellyn drain into Ullswater. Water from Brown Cove and Red Tarn unite below Catstye Cam to form Glenridding Beck, which flows through Glenridding village to the lake, while Nethermost Cove drains into the same lake via Grisedale Beck and Patterdale village.
Red Tarn, enclosed between Striding Edge and Swirral Edge, is about 25 m (82 ft) deep, but in the mid-nineteenth century a dam was built to increase its capacity and supply the needs of the Greenside Mine near Glenridding. That dam has now gone and the tarn has returned to its natural size. It contains brown trout and schelly, a species of whitefish found in only four bodies of water in the Lake District.
A second reservoir was built around 1860 in Brown Cove, between Swirral Edge and Lower Man, along with one further down the valley in Keppel Cove. These provided water to generate hydroelectric power for the lead mine. The dam in Keppel Cove is still in place, but water now leaks through its base. The remains of the dam in Brown Cove can be seen, but again water leaks freely through it. It is unclear whether there ever was a natural tarn in Brown Cove. Guidebook writers before 1860 refer only to Keppel Cove Tarn to the north of Swirral Edge.
A total of five ridges diverge from the summit ridge of Helvellyn at different points.
The north-west ridge continues from Lower Man over Browncove Crags, becoming almost insignificant when it reaches the shore of Thirlmere, yet still separating the valley of Helvellyn Gill from the reservoir, before finally rising again to the wooded height of Great How at its terminus.
The east ridge is another sharp arête known as Striding Edge. This joins the summit ridge at its southern end, not far from Helvellyn's summit. It passes over the subsidiary top of High Spying How and leads to Birkhouse Moor before descending to its final top, Keldas, beside the south end of Ullswater.
The former county boundary between Cumberland and Westmorland lay along the Helvellyn Ridge; this meant that the summit of Helvellyn was the highest point in Westmorland, making it a Historic County Top.
(height and prominence)
|Helvellyn||950 m (3,120 ft)||712 m (2,336 ft)||Furth, Marilyn, Hewitt, Nuttall, Historic County Top||Wainwright, Birkett|
|Lower Man||925 m (3,035 ft)||18 m (59 ft)||Nuttall||Birkett|
|Browncove Crags||859 m (2,818 ft)||3 m (9.8 ft)|
|Great How||333 m (1,093 ft)||136 m (446 ft)||HuMP||Birkett|
|Catstye Cam||890 m (2,920 ft)||63 m (207 ft)||Hewitt, Nuttall||Wainwright, Birkett|
|High Spying How||863 m (2,831 ft)||28 m (92 ft)||Nuttall|
|Birkhouse Moor||718 m (2,356 ft)||9 m (30 ft)||Nuttall||Wainwright, Birkett|
|Keldas||311 m (1,020 ft)||35 m (115 ft)|
Routes up Helvellyn can begin from the villages of Glenridding or Patterdale to the east, Grasmere to the south, or from a number of places along the A591 road to the west, and can follow any of the mountain's five ridges, or the ridges of its neighbours, as well as some of the gills and shoulders on the west side of the range. Walkers can choose between many routes.
The eastern ridges
Striding Edge begins at Hole-in-the-Wall and then stretches for over 1.5 km (0.9 mi) to the Helvellyn summit plateau. This starting point is accessible from both Glenridding and Patterdale. Hole-in-the-Wall used to be a prominent gap in the stone wall on the top of the ridge where a gate was missing. Today the gap has been filled in and a ladder stile crosses the wall. From here the initial part of the ridge is relatively rounded and has a solid path running along the right-hand side. This changes upon reaching High Spying How, the highest point on the ridge — 863 m (2,831 ft). At this point a narrow path continues close to the top of the ridge, which becomes increasingly narrow, and scramblers will often follow the very top of the arête.
The path on the right-hand side continues until near the end of the ridge where it switches over to the left-hand side. Scramblers who continue on the top of the ridge are forced to descend an awkward short gully down from the final rock tower to rejoin the path. At this point the ridge connects with the main Helvellyn massif. Reaching the summit plateau involves a steep walk or scramble up about 80 m (260 ft) of rough rocky terrain, known as The Abyss by W. A. Poucher, author of a popular series of mountain guide books between 1940 and the late 1960s. From the top of this climb the summit is only 200 m (220 yd) away.
Striding Edge is a notorious accident spot among hikers and scramblers. In winter conditions the climb from Striding Edge up to the summit plateau can involve crossing steep icy ground and a snow cornice, and can be the most dangerous part of the walk. Without an ice axe or crampons this presents a serious obstacle. In January 2008 two walkers died after falling from the ridge in separate incidents. Another walker died after falling from Striding Edge in May 2008. Over the August Bank Holiday weekend in 2017, Patterdale Mountain Rescue attended a fatal fall from Striding Edge on the Saturday and helped rescue a seriously injured walker and his dog on the Sunday.
Swirral Edge offers a shorter but equally exciting scramble along a similar sharp arête. The main path to it comes up from Red Tarn, which is linked by a surprisingly level path to Hole-in-the-Wall, making this ridge equally accessible from Patterdale as from Glenridding. The ridge walk can be extended to include the summit of Catstye Cam.
The climb up or down from the summit plateau onto Swirral Edge is another well known accident spot. In winter it involves climbing down another snow cornice onto steep icy ground. There have been a number of accidents at this spot in recent years, making it as dangerous as Striding Edge.
Nethermost Pike also has an east ridge which gives an alternative route to Helvellyn from Grisedale, which many walkers overlook. It can be combined with a scramble on Eagle Crag, or this part can be bypassed by taking the path to Nethermost Cove before joining the ridge.
Other approaches from the east
From Patterdale a long but safe and easy walk (11.5 km (7.1 mi)) on a good path follows the track up Grisedale to the tarn, and then takes the old pony track up the south ridge of Helvellyn. The second part of this walk takes a safe route well away from crags on the side of the ridge (see The south ridge below.)
From Glenridding a similar long but safe and easy walk (11.5 km (7.1 mi)) follows Greenside Road, past the old lead mine and towards Keppel Cove. This track, another old pony track, then zigzags up the fellside to join the main ridge path at the col between Raise and White Side.
The south ridge
Grisedale Tarn is the starting point for the south ridge of Helvellyn, and may be reached from Grasmere or Patterdale, or from Dunmail Raise by a path alongside Raise Beck. Above the tarn the old pony track zigzags up the fellside, and takes a safe but unexciting route well away from crags on the side of the ridge, and avoiding all the intermediate tops. In suitable weather a more interesting and scenic route is to follow the edge of the crags as closely as possible, over the tops of Dollywagon Pike, High Crag and Nethermost Pike.
The western approaches
Shorter and quicker routes to the top of Helvellyn, though with less attractive scenery, begin from several points along the A591 road along the west side of the mountain. Two of these may be combined to create a circular walk. Incorporating the south ridge in the route can restore much of the scenic interest.
Stannah at Legburthwaite is the starting point for the bridleway to Sticks Pass, from which Helvellyn can be approached along the main ridge track from the north.
From Thirlspot two routes lead up Helvellyn. The old pony route took a very safe and steady route for the benefit of early visitors, who took horses and a guide from the inn. The route traverses the flank of White Side to join the ridge at the col just below Lower Man. The other route, known as the White Stones Route, originally marked by stones painted white, crosses the fellside at a lower level and fords Helvellyn Gill to join the path from Swirls.
Swirls is the start of the most direct route to the top of Helvellyn, "the modern pedestrian highway" which has been paved where necessary. It zigzags up the fellside above Helvellyn Gill, over Browncove Crags and joins the main ridge at Lower Man.
Several possible routes begin at Wythburn church. A bridleway winds up the fellside, over Comb Crags and traverses the slopes of Nethermost Pike to arrive on the ridge at Swallow Scarth, the col just below Helvellyn. Other routes from Wythburn follow Comb Gill or Whelpside Gill, or Middle Tongue between these two gills. The shortest route of all follows the gill past the old lead mine, perhaps better used as a descent. Wainwright warned walkers with weak ankles to avoid it.
Helvellyn may be included in a traverse of the full length of the Helvellyn range in either direction, but with a greater sense of climax when starting from the north. Most of the ridge track is a bridleway and so the route can be completed by mountain bike in a challenging six-hour circular route of 16 miles off-road and 10 miles on-road riding. This may begin (and finish) at Mill Bridge near Grasmere.
Helvellyn is a popular area for winter climbing in the Lake District. The steep headwall above Red Tarn contains several graded routes, clustered around the prow-shaped buttress on the right-hand side of the face, known to climbers as Viking Buttress, and in a couple of gullies which lead to the summit.
Nethermost Cove also has some routes, including a large gully between Striding Edge and the back of the cove.
Browncove Crags on the western side of the mountain has some north-facing routes. These are easier to access from a car park, and they can be linked with the Red Tarn routes.
Fell top assessors
The Lake District National Park Authority employs two "Fell top assessors" during the winter months, usually between December and March. Working alternate weeks, one of these walks up Helvellyn each day during that period to check the weather, snow and walking conditions. Their report and daily photograph appear on Weatherline, the Lake District weather forecast website and phone line service, which also includes a local weather forecast from the Met Office. The fell top assessors also put their assessments and photos on Twitter. This information is important for people who go out hillwalking and climbing in winter, helping them to plan their routes and get an idea of the mountain conditions.
Many people camp on Helvellyn throughout the year, often near Red Tarn which gives good views of Striding Edge, Swirral Edge, and the summit of Helvellyn itself. Although camping in England is illegal without the permission of the landowner, there is a tradition of wild camping in the Lake District. This has often been tolerated so long as people have camped unobtrusively, for no more than one night, and have left no trace of their campsite behind.
The summit of Helvellyn takes the form of a broad plateau, sloping gently to the south-west, but dropping abruptly to the north-east into Red Tarn cove. So smooth and large is this summit that a small aeroplane was able to land on it in 1926 (see History below). The highest point, 950 m (3,120 ft) above sea level, is the top of a small rocky knoll, marked by a loose cairn. In former times this knoll used to be known as Helvellyn High Man (or Higher Man.) Nearby there is a cross-shaped stone shelter; to the north is an Ordnance Survey trig point, slightly lower than the summit at 949 m (3,114 ft).
The view from the top on a clear day extends across the whole of the Lake District to the Solway Firth and hills of south-west Scotland to the north-west, Cheviot and the Pennine Hills to the north-east, Morecambe Bay, Blackpool and the coast of North Wales to the south, and the Irish Sea to the west. Snowdon is hidden by the Coniston Fells, and the Isle of Man is largely hidden behind the Great Gable and Pillar group of fells.
The subsidiary top, Helvellyn Lower Man, is about 700 m (770 yd) to the north-west. Its summit is small compared to the plateau of Helvellyn, but it offers better views to the north-west, as the ground falls steeply away from it on that side.
For centuries shepherds have walked over all parts of Helvellyn in the course of their work. It is only since the late eighteenth century that people have visited the mountain for pleasure or recreation.
One of the earliest accounts of an ascent of Helvellyn for the pleasure of doing so is contained in James Clarke's guidebook of 1787. He quotes the account of an unnamed gentleman from Penrith who wanted to eat his dinner on Midsummer Day while sitting in a snowdrift on top of Helvellyn. The man left home at two in the morning, rode to Glencoyne and left his horse at a house in the valley there. He started to walk up the mountain at between four and five in the morning and after five hours hot and hard work he reached the snow and the summit. The snow was covered with dust so he had to dig for clean snow to eat with his dinner. He returned by a different route, reaching Glencoyne ten hours after leaving it. This story seems to reflect the colder climatic conditions of the eighteenth century, during the so-called "Little Ice Age".
Poets and artists were among the early visitors to Helvellyn at the beginning of the nineteenth century. Samuel Taylor Coleridge did a lot of fellwalking during the years when he lived near Keswick. In August 1800, barely a month after moving there, he went to visit his friends William and Dorothy Wordsworth in Grasmere, taking a route over Helvellyn and arriving at ten in the evening.
A few days later William Wordsworth with his brother John and their friend Mr Simpson made a trip up Helvellyn, setting out after breakfast and returning home at ten that evening. A year later, in October 1801, William and his sister Dorothy rode to Legburthwaite (to the inn at Thirlspot) and then to the top of Helvellyn before returning the same way. Dorothy recorded that it had been a glorious day. They had mists both above and below them, but the sun shone through and their views extended from the Scottish mountains to the sea at Cartmel. Wordsworth's poem, Inmate of a mountain dwelling (1816), celebrating the captivating power of the old mountain, was dedicated "To … on her first ascent to the summit of Helvellyn."
John Keats speaks of Wordsworth "on Helvellyn's summit, wide awake…" in a sonnet that celebrates the poet and other artists. A portrait of Wordsworth, deep in thought among the clouds on the summit of Helvellyn, was painted by Benjamin Robert Haydon in 1842, an example of romanticism in portraiture.
An early casualty of the mountain was the artist Charles Gough, who slipped and fell from Striding Edge in April 1805. Three months later a shepherd heard a dog barking near Red Tarn and went to investigate. He found Gough's skeleton, his hat split in two, and his dog still in attendance. Initial newspaper reports that the dog had survived by eating the remains of her dead master were quickly forgotten. Gough became regarded as a martyr to the romantic ideal, and his dog Foxie was celebrated for her attachment and fidelity to her long-dead master. William Wordsworth and Sir Walter Scott both wrote poems about the scene; Francis Danby and Edwin Landseer both painted it. A memorial stone to Gough was erected on Helvellyn in 1890 and quotes part of Wordsworth's poem "Fidelity".
A small tourist industry began to grow up around the mountain, with inns providing ponies and guides as well as accommodation for the visitors, and guidebooks being published for visitors. Jonathan Otley's guidebook of 1823 described the view from the summit and claimed it gave a more complete view of the Lake District than any other point. William Ford, in his guidebook of 1839 recommended the Horse Head Inn at Wythburn as a good place to stay and where a guide could be hired "at a moderate charge"; he went on to describe the climb up Whelp Side and the view from the top. Harriet Martineau in 1855 described the ascent from Patterdale. Ponies could be taken as far as Red Tarn, where there were stakes to tether them while undertaking the final part on foot via Swirral Edge. "Though trying to unnaccustomed nerves," she said, "there is no real danger"; the other ridge "is always fool-hardy to do", and "every one knows" the story of Charles Gough. She also mentioned three routes from the west: one by Grisedale Tarn, one from the Nag's Head at Wythburn, "the shortest, but by far the steepest," and a third from Legburthwaite (that is, from the inn at Thirlspot.) An advertisement in her book, placed by the King's Head Inn at Legburthwaite, claimed "A guide always in readiness at this inn."
In 1926 a small aeroplane landed on the summit plateau of Helvellyn and took off again. The plane was an Avro 585 Gosport, a two-seater biplane flown by Bert Hinkler, a test pilot who worked for A V Roe, the plane's manufacturers, at Woodford Aerodrome near Manchester.
A ground party had cleared and marked a landing strip. Attempts on 15 December and on 21 December were abandoned.
On 22 December Hinkler, accompanied by John F. Leeming, president of the Lancashire Aero Club, made another attempt. The landing was no problem. On the steep slope and with a strong headwind the plane stopped quickly. Professor E. R. Dodds witnessed the landing. The uphill take-off was more difficult and the plane dived off the edge of the summit with insufficient airspeed, but picked up speed as it dived, narrowly missing Striding Edge, to return to Manchester.
A stone tablet on Helvellyn, 40 yards (37 m) south of the shelter, commemorates this landing.:21
Mountain birds around Helvellyn include the raven (Corvus corax), which has now become common. Peregrine falcons (Falco peregrinus), buzzards (Buteo buteo) and ring ouzels (Turdus torquatus) have all bred in the immediate area. Skylarks (Alauda arvensis) and wheatears (Oenanthe oenanthe) are frequently encountered. At one time eagles (probably Aquila chrysaetos) soared over the mountain and bred on the steep cliffs above Red Tarn, but even in Wordsworth's day they had gone, having been persecuted to extinction.
The three coves to the east of Helvellyn are all important sites for remnant populations of arctic-alpine plants. Species such as downy willow (Salix lapponum), mountain avens (Dryas octopetala), alpine mouse-ear (Cerastium alpinum), alpine meadowgrass (Poa alpina) and others have been able to survive in these coves since the last glaciation through a combination of rocks rich in basic minerals, a harsh micro-climate, and inaccessibility to grazing sheep on cliff ledges. However, these populations are small and are not reproducing well. Natural England has introduced a recovery plan for them.
Red Tarn, a classic corrie tarn, is a high-elevation tarn with low nutrient levels and poor in the number of species it supports. Characteristic vegetation zones include a water-starwort (Callitriche) in shallower areas and the alga Nitella flexilis in deeper water and around the inlet. Other species include a pondweed (Potamogeton) which grows in 2–3 m (6.6–9.8 ft) of water and the rush Juncus bulbosus. Brown trout and schelly, a species of whitefish, are found in the tarn.
Grassland on the Helvellyn range has been heavily overgrazed for many years, yet it supports a diversity of acid grassland species including sheep's fescue (Festuca ovina) on the summit ridge, matgrass (Nardus stricta) on the middle slopes, and fescue-bent swards on the lower slopes. The Nardus grasslands are the haunt of the scarce mountain ringlet butterfly (Erebia epiphron), the only alpine species of butterfly found in Britain. Acidic flushes (areas of water seepage) with their carpets of sphagnum mosses are common. Less common are basic flushes, which support a greater diversity of species.
The summit and the eastern side of the mountain are part of the Helvellyn & Fairfield Site of Special Scientific Interest (SSSI). This covers an area of 2,418.8 hectares (5,977 acres) and was designated in 1975 because of the area's geological and biological features. Natural England, which is responsible for choosing SSSIs, tries to ensure that the management and use of the area is sustainable.
All the rocks of Helvellyn are part of the Borrowdale Volcanic Group, formed on the margin of an ancient continent during a period of intense volcanic activity during the Ordovician period, roughly 450 million years ago.
Helvellyn lies within a geological structure which is interpreted as evidence of a volcanic caldera. This is a semi-circular series of faults which sweep eastwards to encompass Helvellyn, Patterdale, Deepdale and Fairfield, and which abut against a major north–south fault to the west (along the line of the A591 road).
This caldera was formed by an eruption of exceptional magnitude which produced a series of pyroclastic flows, fast moving currents of hot gas and rock, which buried the whole district of roughly 500 km2 (190 sq mi) beneath at least 150 m (490 ft) (in places up to 800 m (2,600 ft) of ignimbrite). This succession of ignimbrites is known as the Lincomb Tarns Tuff Formation, the most widespread volcanic formation in the Lake District. The eruption of such a huge quantity of magma emptied the magma chamber beneath the volcano and led to the collapse of the overlying rocks to form the caldera.
The lowest and oldest rocks on Helvellyn are those of this Lincomb Tarns Tuff Formation, which outcrop along the western side, up to roughly the 550 m (1,800 ft) contour on Whelp Side. The lowest part of the formation here is the densely welded lapilli-tuff of the Thirlmere Member, in which the individual pieces of semi-molten lava were flattened under the weight of deposits above them. Contemporaneous movement on the caldera's boundary fault has produced a thick deposit of breccia above the Helvellyn Screes and on Browncove Crags. The Thirlmere Member is overlain by a deposit of volcaniclastic sandstone, the Raise Beck Member, deposited in water during a break in the volcanism, but succeeded by further thick ignimbrite deposits.
Above these ignimbrites are found sedimentary rocks of the Esk Pike Sandstone Formation. These were deposited in water, probably in a caldera lake, as the volcanic rocks weathered and were eroded. Structures in these rocks suggest the faults were still active and the caldera was still subsiding. Layers of tuff and lapilli-tuff indicate some ongoing volcanism.
Higher still on Helvellyn, as well as in the coves to the east and covering Swirral Edge and Catstye Cam, are rocks of the Helvellyn Tuff Formation. This consists of up to 400 m (1,300 ft) of ignimbrite, representing another series of pyroclastic flows. This Helvellyn Tuff is found only within the boundary faults of the caldera, and mainly in its western half.
The highest surviving rocks on Helvellyn, found on the summit plateaux of Helvellyn itself and of Nethermost Pike, and along the crest of Striding Edge, are the volcaniclastic sandstones of the Deepdale Sandstone Formation. Again, this formation is confined to the limits of the caldera, and represents another return to erosion and sedimentary deposition within a caldera lake, though with layers of pyroclastic rock showing that the volcanism had not entirely finished.
During the Late Devensian glaciation, which occurred 28,000 to 14,700 years Before Present (BP), the whole of northern England was covered by an ice sheet. Helvellyn was one of a small number of nunataks which protruded above the ice.:218:20
A short period of glacial conditions returned between 12,650 and 11,550 years BP, known in Britain as the Loch Lomond Stadial (and elsewhere as the Younger Dryas stadial), when the Gulf Stream current ceased to flow past the British Isles. Small cirque and valley glaciers formed in north and east facing valleys, including Grisedale and the coves on the east side of Helvellyn. The results are seen in moraines of unsorted boulder gravel in the valleys, the spectacular coves with steep headwalls, and the sharp arêtes formed where the rock was eroded on both sides between adjacent glaciers.:233:20
Glacial conditions ended suddenly, 11,550 years BP, when the Gulf Stream current was re-established.:233 Periglacial processes in seasonal freeze-thaw conditions, both present and past, have produced sorted stone stripes and solifluction lobes and sheets on the summit ridge of Helvellyn. These are one reason why the area was included in the Helvellyn & Fairfield SSSI.
Two unsuccessful attempts to find lead ore in economic quantities on Helvellyn have been made.
Helvellyn Mine or Wythburn Mine opened in 1839 by the gill between Whelpside and Helvellyn Screes. It was operated by a succession of different owners, driving five levels through mostly barren rock to explore three mineral veins. It finally closed in 1880 when Manchester Corporation acquired the land for the Thirlmere reservoir. Only a few hundred tons of galena came out of the mine; probably insufficient to cover its costs.
Little can be seen of the levels now for the entrances were destroyed when the mine closed, but several spoil heaps remain, one covering the gill, along with the old miners’ path which zigzags up the hillside, a self-acting incline to lower ore to the dressing floor, and the old winding-drum house. The narrow leat which once diverted water from Brownrigg Well into the gill beside the mine may also be seen, much higher up the fellside.
Helvellyn. The earliest known record of the name dates from 1577, but early records are spelling variations of the modern name (such as Helvillon, Helvelon or Hell Belyn) rather than any help with the etymology. Various attempts to interpret the name have been made in the past. Some, led by the present spelling, possibly wrongly thought the final syllable was the Welsh word llyn, "lake" which has various historic spellings including 'lin' and 'lynn'. Richard Coates in 1988 proposed a Celtic derivation from the deduced Cumbric word hal, "moorland", and velin, the Cumbric equivalent of the Welsh word melyn meaning "yellow." Hel is a Welsh word meaning to gather, drive or hunt, and helfa (historically spelt helva) has been used to describe a portion of mountain from which sheep are collected.
Recent place-name studies have accepted the "yellow moorland" derivation, but have struggled to understand how Helvellyn can be regarded as a yellow mountain. Colour, in the Celtic languages, is perceived differently from the way it is seen and described in modern English. For example, in Scottish Gaelic the spectrum of colours was "pastel rather than primary, gentle rather than bold." Colours were related to a landscape context in which blues, greens, greys and whites in particular were both more diverse and more differentiated than in English. People who relied on the system of transhumance for their livelihood gained the ability to assess the nutritional value of upland grasses from a distance before moving their stock to a summer shieling, and used appropriate colour terms for grasses which would become progressively more green as the spring advanced.:195 Yellow, at least in Gaelic hill names, is not a bright colour. It describes hills which are distinguished by grasses such as Nardus stricta and Deschampsia flexuosa, both of which appear pale and bleached in winter.:197 These grasses are common on the Helvellyn range, in an area where transhumance also used to be practiced. Nardus stricta in particular is an unpalatable and unproductive grass, and the Flora of Cumbria specifically notes a possible connection between areas of late snow cover and Nardus grassland at high elevations in the Helvellyn range. A name describing the mountain as "pale yellow moorland" is therefore meaningful in a Celtic context.
Lower Man. The mountain has two tops, which used to be distinguished as Helvellyn Low Man (or Lower Man) and Helvellyn High Man (or Higher Man). Both are drawn and labelled on a panoramic view of the range found in Jonathan Otley's guidebook of 1823.
Striding Edge. An edge in mountain place-names is a steep escarpment, on either one side or (as here) on both sides.:396 The first reference to Striding Edge was by Walter Scott in 1805 as Striden-edge. A map of 1823 called it Strathon Edge. It is possible that "Striding Edge" has replaced an earlier name, now lost.
Swirral Edge may be either "The precipitous ridge that causes giddiness" or "The precipitous ridge where the wind or snow swirls around." An edge is a steep escarpment, as above.:396 Swirrel, a dialect variation of "swirl" has two possible explanations. It can be used to mean "giddiness, vertigo", but it can also be used of a place in the mountains where wind or snow swirls around.
- "About". John Muir Trust. Retrieved 8 October 2018.
- Ordnance Survey 1:25,000 Explorer map
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|Wikimedia Commons has media related to Helvellyn.|
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