Saunterings is a set of reflections based upon walks around the counties of Cumbria, Lancashire and
North Yorkshire in North-West England
(more details of my ‘North-West England’ are given in the Preamble).
If you'd like to give a comment, correction or update (all are very welcome) or to
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40.   In the Borderlands of Burton-in-Lonsdale and Bentham
39.   Halls Galore by the Middle Ribble
38.   Reflections from Jeffrey's Mount
37.   Whoopers on Thurnham Moss
36.   The Flow and Ebb and Flow of Morecambe
35.   Dufton Rocks
34.   Thieveley Pike and the Singing Ringing Tree
33.   Is Nappa Hall Napping - or Dying?
32.   Russet Rusland Valley
31.   Pink Stones on the Orton Fells
40.  In the Borderlands of Burton-in-Lonsdale and Bentham
The villages of Burton-in-Lonsdale and Bentham are in the Craven District of North Yorkshire but the rivers that flow through them – the Greta and the Wenning respectively – head west to enter Lancashire and join the River Lune. Both rivers arise on the slopes of Whernside and Ingleborough and have an exciting start in life, the Greta tumbling over the famous Ingleton Falls and the Wenning plunging into Gaping Gill. However, once they cross the A65, near Ingleton and Clapham respectively, they settle, under normal conditions, into a gentle maturity.
They run westwards, more or less in parallel, two or three miles apart, to form a rough quadrilateral of relatively anonymous land between the A65 and the River Lune. It is almost all rolling drumlin farmland that falls from about 200m in the east to about 30m in the west. The region has no features that would appear on a tourist’s itinerary. There’s a golf course and a few caravan parks, and that’s about it for holiday-makers. Midway between the A65 and the Lune the rivers pass the villages of Burton-in-Lonsdale and Bentham (High and Low). I set out to saunter between them, sampling stretches of the two rivers, enjoying the quiet countryside, with no expectations of excitement.
And so it proved. The path from Wennington to Burton-in-Lonsdale crossed many grassy fields, all with sheep
apart from one with a disconsolate set of horses (their field had no grass). I crossed the county border into North
Yorkshire near Old Wennington but there was, of course, no sign to tell me that I had done so. Fine views of
Ingleborough opened out ahead.
Burton-in-Lonsdale and Ingleborough from near Clifford Hall
I found my way past Clifford Hall, where they seem determined to have no footpath signs, into Greta Wood, where there are some impressive beech trees. I saw a sign to say that the wood is “dedicated to remember the coal mine donkeys”, which we have now done. I assume that this is a reference to the Ingleton coalfield within the parishes of Bentham, Burton-in-Lonsdale, Ingleton and Thornton-in-Lonsdale. The Ingleton Colliery, which at one time employed 900 people plus I-don’t-how-many donkeys, closed in 1936.
The River Greta and Burton Bridge
On the walk south from Burton-in-Lonsdale my eyes continued to be drawn towards the noble profile of Ingleborough.
The recent snow seemed to have all gone, although I could occasionally glimpse some distant snowy tops in the Lake
District and perhaps to the north (Great Shunner Fell perhaps?). In High Bentham I passed the home of the
Corio Raptor Care and Rehabilitation Centre
– I had to pass it as the ongoing work is not open to the public, although the owners are often to be seen with their raptors at local shows. I managed, after some firm advice from a local, to find the River Wenning after walking through a caravan park, empty of people as far as I noticed. The path along the north bank is a well-used one, with a couple of benches from which to contemplate the sedate Wenning, but the route beyond Low Bentham higher on the south bank requires more careful navigation. At Robert Hall I left North Yorkshire. It is said that the Hall, built in the 16th century for the Cantsfield family, who were recusant Catholics, provided a refuge for fugitives escaping the law by crossing the county border. If so, perhaps our county borders were once as important as state borders seem to be in the US, if you believe many US films. I then passed The Blands, a building with many dubious legends, which I was pleased to see has been restored after a fire in 2009.
Low Bentham and High Bentham, with Whernside and Ingleborough beyond, from near Robert Hall
Did I get away with it? Did you notice the mention of ‘Craven’ in the first sentence? Almost every document about the Yorkshire Dales mentions Craven as a noun and an adjective (Craven Fault, Craven Heifer, Craven Museum, Craven Herald, Craven this, Craven that) without saying what it is. Maybe I should try to. Today, the meaning of ‘Craven’ is fairly simple. Craven is one of seven local government districts within the county of North Yorkshire. It extends from Bolton Abbey in the east to Burton-in-Lonsdale and Bentham in the west, these two villages forming part of one of the nineteen wards of Craven. Craven is, roughly speaking, the southern half of the Yorkshire Dales plus those parts of North Yorkshire south of it, including villages such as Thornton-in-Craven and Sutton-in-Craven, as it surely ought to. In area (454 square miles) Craven is larger than more than half the English counties!
However, it’s not that simple because some parts of old Craven that were transferred to Lancashire in 1974 are now given the honorary title of West Craven. West Craven is part of the Pendle borough of Lancashire and includes villages such as Barnoldswick and Earby. To further complicate matters, the Church of England’s Archdeaconry of Craven is much bigger than the government district of Craven and includes parts of Cumbria, Lancashire and West Yorkshire. But that’s all a doddle compared to the meaning of Craven over the centuries. In the Domesday Book of 1086 many places (some no longer considered to be within any form of Craven) are said to be ‘in Crave’, with the summary giving the heading of Cravescire, but there is no clear definition of ‘Crave’. As Craven continued to be used without a precise definition ever since, historians have great fun trying to work out what it referred to at various times. I’ll leave it at that.
[January 28th 2019; SD6169; Wennington Green bus stop – NE – Old Wennington – E – Clifford Hall – N, E – Burton Bridge – SE, S – River Wenning – W on north bank – Low Bentham – S, W – Robert Hall, The Blands, Wennington bus stop; 9 miles; 92/400]
39.  Halls Galore by the Middle Ribble
Why are there so many Halls by the middle Ribble? I planned to wander about the River Ribble just below the point where it joins the River Hodder (from the Forest of Bowland) and the River Calder (from the Cliviger Gorge above Burnley) and I noticed from the map that there is a profusion of Halls in this region. A Hall is not a building with a defined function, like a church or a hotel. Anybody can call their house a Hall but the name generally implies a degree of distinctiveness and aloofness, which perhaps the original owners wanted to establish. Most Halls elsewhere are in or near villages but here they seem to be somewhat isolated. I thought I’d have a look at some of them.
First I reached New Hall
, a name indicating a lack of foresight. It was built in 1665.
I suppose it was new relative to something. In general, I am not much interested in the history of a
building, which generally involves a tedious catalogue of the eminent families who lived therein and
the changes they made to it. I will give only a superficial impression, which is all anyone can do
without a close inspection, especially of the interior.
is a characterful three-storey building, recently put up for sale. I couldn’t decide if it had new owners, or any residents at all, as it was rather shrouded by trees.
I walked on past the 1776 Ribchester Bridge to Salesbury Hall
, which is not shrouded at
all but is within open parkland and is surrounded by the new Manor Court offices and other buildings.
The Hall itself is presumably on the site of the base for the original Salesbury Manor dating back to
the 12th century. I read that the previous Hall was demolished in 1883 but the present
looks more modern than that to me.
I walked through Marles Wood, which is clearly a well-trodden path that must be muddy after
rainy periods, alongside the meandering River Ribble, a pleasant walk enlivened by a kingfisher, light
blue and flying straight and quiet. After a detour around the on-going work to replace the Dinckley
footbridge damaged in 2015 (£1.5m for a walkers’ bridge: thank you!), I reached Dinckley Hall
– or at
least as near to it as the footpath allowed.
was also recently for sale. The property
apparently dates back to the 13th century but clearly has been much changed. It looks ordinary now with
only the outline of a cruck frame suggesting antiquity and providing architectural interest.
The River Ribble and the new Dinckley footbridge
I (eventually) found my way past the imposing mansions of the new Brockhall Village to return to the River
Ribble, to find Hacking Hall
at the confluence with the River Calder. This is more like it:
is more of a prototypical ancient Hall. It was built in 1607, has three-storeys, five gables facing the
river, with many mullioned windows with three to six lights. The top storey windows appeared to be
boarded up, indicating that perhaps not all is well within the Hall. No doubt the Hall has been
restored since 1607 but this seems not to have affected its essential structure. However, I can’t help wondering why any buyer would take on the challenge of Hacking or any other ancient Hall when the mansions of Brockhall Village are available.
I now faced a rather dull walk south, away from the Ribble. It was enlivened by a large sign
detailing the many hazards (toxocariasis, neosporosis, sarcocystosis – ugh) that dogs and dog-owners
cause. There should be more of them – the signs, that is, not the dogs. I eventually reached where Hollin
is marked on the map. I found a Hollin Hall Farm, of no distinction that I could see. It is no doubt serviceable as a farm but hardly a Hall.
And so, on to Whittle Hall
. This does not appear on the 1848 map, so I deduce that it is a
relatively new building. It seemed so to me, and modest, for a Hall. Perhaps the owners felt so too, as,
undecided whether it is a hall or a house, they call it both: Whittle Hall House. Compensating for the
unexciting Hollin and Whittle Halls, I found myself on the lofty ridge of Billington Moor, an unexpected
bonus, for it provided wide-ranging views, to Blackpool Tower and Pen-y-ghent, some 25 miles away, as
well as of Pendle, a constantly reassuring presence throughout this walk. Closer below, the Ribble valley between Clitheroe and Preston was arrayed. It is still predominantly green but, of course, has many more buildings than in the days of the ancient Halls, plus the A59 and a railway.
Pendle from Billington Moor (and in the distance the hills of the Yorkshire Dales)
I dropped down to find Carr Hall
. This is marked on the 1848 map but I suspect that nothing of that Hall remains. The building now called Carr Hall forms the large offices of MMB (Mott Macdonald Bentley). Next to it a building in the style of old halls has been built or is being built. Somebody has gone to considerable expense to restore this Carr Hall site but it added little to my survey of Halls.
I walked through Wilpshire and Salesbury towards the immodestly-named Lovely Hall
. Here I made
the wrong decision. After so much road-walking I opted to walk across fields rather than continue on the
road. It turned out that I could see only the chimneys and roofs of Lovely Hall above the large barns at
its rear and so I can say nothing about it. However,
has also recently been for sale, so we can at least read the estate agent’s blurb.
Through Copster Green – which does indeed have a green, a long thin one, bumpier than any other I
have seen, between two rows of houses – I came to Copster Hall
, on a rocky knoll.
is a 17th century farmhouse extolled by Historic England for, amongst other things, having “1st floor windows of 6 lights with ovolo-moulded mullions and transoms”. Two of those lights now have incongruous large white frames (I don’t think that is what ovolo-moulded means). Overall, though, Copster Hall seemed little different to hundreds of other farmhouses to me.
However, the nearby Bolton Hall
was more appealing. The original
of 1655, was rather small – by Hall standards – but looks to have been sympathetically extended, leaving the old Hall appearing much as it did, I imagine. The mullioned windows, still with diamond leading, have been distorted into a rather elegant bow. I see that the website referred to above comments on “inappropriate strap pointing”, which is barely identifiable from a distance by an amateur such as me. Since it seems to be well-known that strap pointing is bad for old stonework I wonder why it was used here.
I had three further Halls to the west (Oxendale, Osbaldeston and Showley) in mind if I had sufficient time, energy and enthusiasm at this point. I didn’t. Nevertheless, I claim a world record (ten, according to the map – and I’m not counting Brockhall Village) for the number of Halls visited on one walk. If anyone would like to claim the record from me they are welcome to it.
[January 17th 2019; SD6634; P south of Ribchester Bridge – N – New Hall, Ribchester Bridge – E – Salesbury Hall – NE by river – Dinckley Hall – E – Brockhall Farm, Hacking Hall – SE – Chew Mill, Whalley Old Road – SW – Hollin Hall, Whittle Hall, Little Snodworth – NW – Carr Hall – SW on A666, NW on B6245, N – Ashes Farm – NW – Lovely Hall, Copster Green, Copster Hall – W – Bolton Hall, B6245 – N – P; 12 miles; 89/400]
38.  Reflections from Jeffrey's Mount
A new year is always a time for reflection. My struggles with a book about “how to aesthetically appreciate the
natural environment” (Carlson and Berleant, 2004) have provoked me to reflect on the natural environment of
North-West England. I have battled with many abstruse words and dense paragraphs to try to grasp the object model,
the landscape model, the scientific model, the arousal model, and so on, and with concepts such as aspection, numinousness,
etiology, noesis, and so on, but I am left with one preliminary question: What natural environment?
There is no fully natural environment in North-West England, although it comes closer to it than most places in
England. There is nowhere that I may stand without being able to point to some human intervention with nature. I realise
that humans are part of nature too and that it could be argued that, say, the Midland Hotel in Morecambe is as natural as a
wasp’s nest. However, the book doesn’t argue this. It focusses upon mountains, waterfalls, forests, whales, and the like.
It seems to me that any attempt to discuss the aesthetics of our environment as it is today must include the effects of
humanity upon it, although this factor is largely ignored by Carlson and Berleant (2004). If there is a spot in our
region where I cannot point to, for example, a building, road, field, pylon, moor, weir, or plantation then I am
sure that I need only point to the contrails of the many jets that cross our region. One morning recently, as I was
grappling with these thoughts about nature, I noticed in the dark sky a thin crescent of the moon, bright white from
the not-yet-risen sun. What could be more natural? Then I saw that three jets were in the process of enclosing the
moon in a bright white triangular frame.
I walked into Borrowdale (the one near Tebay, not the one near Derwent Water) through Borrowdale Wood. Is this a
‘natural’ wood? It certainly looks like an old natural woodland to me. However, the authorities concerned about our
woodland hedge their bets – their formal designation of such woodlands is ‘Ancient Semi-Natural Woodland’ in recognition
of the fact that our woodlands have been managed for centuries to provide wood for various purposes.
Borrowdale from Belt Howe
Borrowdale was described in Wainwright (1972) as “the most beautiful valley in Westmorland outside the Lake District”.
Today it is not in Westmorland and is inside the Lake District. But it is still beautiful. Is it natural? There
are aerials on the Whinfell ridge, conifer plantations on Mabbin Crag, farms, roads/tracks to them, bridges, fences,
walls, and, on this occasion, one helicopter, two low-flying jets, many high-flying jets, and a distant but appalling
(for someone focussed on the natural and unnatural, as I was) view of what seemed to be at least four conflagrations on the North Pennine
moors, as heather was being burned for the grouse. At least there are no wind turbines or reservoirs in Borrowdale, as have been threatened in the past.
A distant view of the North Pennines, on fire
I walked past sheep and fell ponies – and we could debate whether they are natural here – along the ridge to Jeffrey’s Mount. From the small cairn at the top I wandered east to gain a full view of the so-called Lune Gorge but not too far to the east as it is a steep slope with a small cliff at the bottom from which to fall onto the A685. As I stood there idly watching the world dashing by below, I day-dreamed about previous activities in the Gorge.
It’s 19 AD
. It is quiet. The hills are covered with trees. The River Lune runs, unseen, in the valley. There’s a path there for those taking advantage of this natural gap in the hills to travel between north and south.
. I can hear hundreds of Roman soldiers in their barracks below in the rectangular green field at
To the south I can see a legion marching along the Fairmile Road, having walked from the fort at Burrow or Ambleside. To the north further soldiers are heading towards Carlisle walking up Crosby Ravensworth Fell, beyond the Tebay Service Station.
. Men are working to build a motte-and-bailey castle
by a bend of the River Lune near Tebay. The site is clearly of strategic importance to the Normans. It is a castle of wood, not stone, as it is for administrative rather than defensive purposes. There’s a track below towards the next motte-and-bailey down the Lune valley, at Sedbergh.
. The trees have gone from the hills, removed by sheep-farmers. Scottish raiders can be seen moving along the valley.
. I can see herds of cattle on the drove road below and hear the accompanying din. Villages on the way, such as Greenholme and Roundthwaite just to the north, are making the most of this passing trade. Herds from Galloway are funnelled through the Lune Gorge to swing west below Grayrigg Common to continue on the Lune watershed towards Kirkby Lonsdale.
. The busy but narrow road from the south swings east past Low Borrowbridge Inn and then north over a bridge over Borrow Beck. A mile north, before Lune’s Bridge crosses the Lune, a side-road leads north through Roundthwaite. The road through Tebay crosses the Lune at Tebay Bridge and continues to Orton. These two roads form the main thoroughfares north from Lancashire.
. Tebay is a major railway junction with an agglomeration of sidings and engine sheds. A branch line turns east to Appleby and the London and North Western Railway to Scotland, completed in 1846, continues up a steep slope to Shap. It is so steep that extra engines are based in Tebay to give the steam trains more oomph. To the south a branch line to Ingleton over the Lowgill Viaduct can be seen.
. The Tebay station and its branch line have closed. The old road (the A685) no longer
crosses the Lune at Lune’s Bridge (now a dead-end) but at a large new bridge south. The A685 has been shifted west,
necessitating the removal of a chunk of Jeffrey’s Mount, to enable the M6 to pass through the Gorge. The M6 engineers
have been given a
Civic Trust Award
for “an outstanding contribution to the appearance of the Westmorland landscape”. The index of Carlson and Berleant (2004) doesn’t mention motorways. The book is concerned with the ‘natural environment’ and the award is concerned with the ‘landscape’ and they are not the same thing, as many erudite treatises no doubt explain. So I turned to a chapter (Halpern, 2004) that began with the sentence “What is it to appreciate a landscape aesthetically?” This does mention motorways – once. It says “many people … feel revulsion at the slicing of a down … by a motorway cutting”. Do they feel revulsion at the slicing of a northern upland? Are our uplands more suited to slicing by motorways? Are our northern sensibilities less susceptible to revulsion? Have our feelings of revulsion been exhausted by the railway and A685 that already slice through the gorge? Perhaps someone should write a book on how to feel aesthetic revulsion at the unnatural environment.
The M6's Borrowbeck Viaduct nestled within the Lune Gorge, from Casterfell Hill
. It is not quiet. There is no respite from the loud rumble of the M6 plus the occasional clatter of express trains. In a few places the Lune may be glimpsed, having been flowing through all this traffic for centuries and now winding its way under many bridges. But look! Trees (hawthorn, blackthorn and alder) have recently been planted on Tebay Fell, as they have been in Borrowdale. For the first time in 2,000 years we seem to have acknowledged that we cannot just exploit the natural environment of the Lune Gorge but that we need to restore it and protect it. Sadly, no, the tree-planting is, as always, utilitarian, being intended to reduce flooding down-river. Well, I was day-dreaming.
[January 9th 2019; SD6691; layby on the road to Roundthwaite, overlooking the M6 – S – Borrow Beck – W, NW by Borrow Beck – Low Borrowdale – E – Belt Howe, Casterfell Hill, Jeffrey’s Mount – N – Roundthwaite – SE – layby; 6 miles; 85/400]
37.  Whoopers on Thurnham Moss
It is hard to believe, after all the rain, cloud and wind of the last few days, that some of our visitors at
this time of year prefer our climate to that which they’ve left behind. Whooper swans do. They come all the
way from Iceland in order to pootle about in our muddy fields. We thought we’d go to see them in action, but
by walking along the quiet, flat lanes that cross Thurnham Moss not in the muddy fields that looked too waterlogged
for us. We began our search from Tithe Barn Hill, Glasson, which at 20m was the highest point of our walk and
which, from this prodigious height, afforded a fine view over the River Lune to the village of Sunderland. We
set off with optimism because a
Lancaster & District Birdwatching Society's website
entry for the day before had said that hundreds of whooper swans were in the region.
Sunderland from Tithe Barn Hill across Glasson Marsh and the River Lune
I don’t know what those interested in birds prefer to be called nowadays. They used to be birdwatchers – or
ornithologists if especially keen – but now I more often read about ‘birders’ going ‘birding’. Perhaps there is a
subtle distinction between ‘birdwatcher’ and ‘birder’. Rosen (2011) writes that “birdwatchers look at birds;
birders look for them”, although he admits that this distinction is “crudely put”. But ‘birder’ and ‘birding’
are odd words, aren’t they? Normally, words ending in -er and -ing are from a corresponding verb, which would
be ‘to bird’ in this case. If there were such a verb then we could also say “She birds enthusiastically” or
“I birded yesterday”. Do birders ever use such expressions? My dictionary (admittedly a little old) has
‘birding’ meaning ‘the hunting, shooting, snaring, or catching of birds’. Of course, our birding birders
don’t do that – although ‘fishing’, perhaps the closest analogy to ‘birding’, similarly means ‘the catching
of fish’. Never mind: I’ll use ‘birding’.
Walking and birding are not entirely compatible. Both activities get us outside to appreciate the natural
environment but birding demands occasional non-walking. Birders have to pause in order to binocular (anyone can
play this noun-to-verb game) the shrubbery before the little brown bird disappears to another shrub. We have no
such difficulty with swans. They are large, prominent and stay put. We found our first swans, about a score of
them, in the first field south of Brows Bridge. Most were our native mute swans (with a black knob on the base of
the bill) and some were visiting whooper swans (with a yellow-based bill). Thus encouraged we pressed on towards
Thursland Hill where large numbers of swans could be seen and heard (and were therefore not all mute swans) in the
fields to the west. It was a little difficult for us to identify the species because the sun behind made them
silhouettes. We came across two birders with their tripods and camera-binoculars and one of them confirmed that
all the swans were indeed whoopers. He seemed somewhat saddened by this. He was hoping to see a Bewick’s swan.
They visit from Siberia (in lesser numbers than whooper swans) and one had apparently been reported in the region.
Judging from the
I doubt that I would be able to tell the two species apart if they stood side-by-side
in front of me but these two birders obviously would.
Elated by all these whoopers, we walked on to the ruins of the 12th century
a breezy walk along the weather-beaten coastal path back to Glasson. We were treated to clear views over
the choppy bay to the Lake District hills and, inland, to the Bowland fells. The footpath along Marsh Lane
(a reasonable name but a little under-stated) was several feet under water because of all the recent rain,
necessitating an escape via the flood protection wall that was keeping all the water inland. On the coastal
walk many species of birds – some of which we could identify and some perhaps not – obliged with aerial displays.
However, I doubt that I will ever become a true birder, that is, someone who is more saddened by the
absence of one bird than pleased by the presence of three hundred similar ones.
The remains of Cockersand Abbey, Plover Scar lighthouse and Heysham Power Station
[December 9th 2018; SD4455; Tithe Barn Hill, Glasson – E – Brows Bridge – S, W, S – Thursland Hill pond – W, SW –
Cockersand Abbey – N – Crook Farm – NE – Tithe Barn Hill; 5 miles; 83/400]
36.  The Flow and Ebb and Flow of Morecambe
Ruth tipped me out of the car at the northern end of Morecambe Prom on her way to a rehearsal with the esteemed
Promenade Concert Orchestra
I had four hours to fill before the concert. It seemed opportune to re-explore Morecambe because
just three days earlier the local paper had revealed plans for a proposed
Eden Project North
If this project materialises – and everyone seems optimistic – then it will transform Morecambe and the
I was also inspired to have another look around Morecambe and Heysham after re-reading a quirky little
book published in 2003. At that time Morecambe was near its nadir as a seaside resort and yet the authors
were remarkably complimentary, whilst drawing a wistful contrast between past glories and the then tawdriness
(I suspect that they preferred the latter). The Midland Hotel had long been derelict and Frontierland,
the last tourist attraction of any note, had closed in about 2000. No doubt, the nature of the book reflects
the nature of its authors,
. The former is a cultural commentator who has written books on pop music and fashion. The latter
(full name Linder Sterling – she said in a
that “one name seemed sufficient”, which perhaps it is if you spell it wrong) is an artist known
for her radical feminist photomontage. She was a key figure in the 1970s punk scene and in 2017
became artist-in-residence of Chatsworth House, suggesting some accommodation with the establishment.
Anyway, quite a couple to find the Morecambe and Heysham of 2003 interesting enough to write a book about.
I set off with the tide in, lapping at the new sea defences which cost £11m and were finished in 2018.
This is part of a programme to revitalise Morecambe’s seafront that had actually begun with government
funding in 1990. As a result, everything of interest to visitors overlooks the sea. Morecambe is lucky
not to have a view over the bay. It has many. Views when the bay is full (as on my walk), when the sandy mud stretches for miles across the bay, when (in the morning) the sun shines across the bay on the hills, when (in the evening) the sun sets over the sea or behind the hills, when it’s calm, when it’s choppy, and when it’s too misty to see anything.
Across Morecambe Bay
Perhaps the only exception to the seafront focus is Happy Mount Park, which I passed next. It is only
fifty yards from the sea but the sea is irrelevant to it. It is a traditional park, with gardens,
playgrounds and café, now fully recovered from the
fiasco of 1994 when, in desperation at the resort’s falling income, the council embarked on a project that cost it millions. For the next mile all the sea-facing establishments seemed in fine order, with scarcely a ‘for sale’ sign or a hint of dereliction, and the Sunday morning walkers, joggers and cyclists were making the most of the November sunshine.
Surveys always suggest that Morecambe has a higher proportion of old visitors than other seaside resorts but you wouldn’t know it walking along this promenade. There was hardly an oldie to be seen. But then November is not the holiday season and no doubt most of the promenaders were local. Nearing central Morecambe, the average age of my co-walkers began to rise. I expect that it is true that the typical holiday visitor is rather old, which causes or is caused by a pervasive sense of nostalgia. As everywhere, the unchanging nature of the sea and the beach brings memories. For me as a boy, the seaside and holidays were synonymous: we always went to the seaside for holidays and we never went to the seaside except for holidays. I suspect that most Morecambe visitors are reliving their childhoods. Nostalgia is reminiscence plus regret: it is remembering how things were, whilst sadly accepting that those things can never return. There is nothing wrong with this – ‘heritage tourism’ is a perfectly respectable part of the business, but it is only part.
Bookshops of the past were never quite like the
Old Pier Bookshop
Thankfully, it was closed – I didn’t have the time to get lost in the labyrinth of old books piled in no
discernible order. There is, of course, no pier adjacent. The two piers were demolished in 1978 and 1992.
I wandered among the back streets for a while, to confirm that they remain like the rust below a touched-up
car bonnet, and re-emerged near the site of the proposed Eden Project North. It is, as it needs to be, the
prime site in Morecambe, adjacent to the graceful, iconic Art Deco Midland Hotel. If I may presume to say
so, the Midland Hotel looked like it might need to be touched up itself if it’s to meet the standards that
will be set by the Eden Project North (if it happens). The Project’s proposed site is unused at the moment,
as it has been really since the open-air swimming pool was demolished in 1975. According to
the Super Swimming Stadium was “one of the grandest of the 1930s modernist seaside lidos” and “was said to be the largest outdoor pool in Europe when it opened in 1936”.
It is hard now to visualise Morecambe in its prime, the period of 1919-1957 or so, when it was
central to ‘the Sunset Coast’. Morecambe had flourished as a seaside resort after 1850 when the railway
enabled Yorkshire workers to flock there for their holidays. Morecambe had more visitors from Yorkshire
than Blackpool did, although many fewer in total. Bingham (1990) considered that Morecambe was at its
peak of popularity when well over 100,000 people came to see the illuminations switched on in 1949.
Morecambe’s wealth enabled it to develop a relative elegance, leading Bracewell and Linder to comment
that “more than any other seaside town, Morecambe has a claim to being the cradle of glamour and romance”
and that “the greatest modern articulation of this glamour” is the
Or rather was, at the time they were writing. It was re-opened in 2008, confirmation of Morecambe’s developing renaissance.
The Midland Hotel
Morecambe was the well-publicised home of the Miss Great Britain contest from 1956 to 1989 but it took it on
at just the time that its fortunes began to plummet. From 1957 cinemas, theatres and much else besides began
to close, as holidaymakers came to prefer package holidays abroad. No seaside resort rose and fell faster
than Morecambe. By 1975 its plight had become a joke (to others), as shown – warning: on no account watch
anything outside the given times, it’s awful – by this
from 40.25 to 41.30. The bit from 40.25 is awful too. I only mention it because it shows that even a weedy funny-man with ridiculous hair and a punchable face felt able to put the boot in on Morecambe when it was down.
Actually, my memory is that Morecambe wasn’t so bad in the 1970s and 1980s. It provided a reasonable family day-out if your expectations were not set too high. There’s always a beach, or mud. Frontierland (or its then equivalent) was still alive, although it gradually withered and passed away. I walked past it next. Whatever is planned for the site seems not to have been activated yet. Similarly, for Morecambe’s West End, which was once a thriving part of the resort with its hotels and B&Bs. By the 1980s it was more for the unemployed than holidaymakers. In 2005 the North West Regional Development Agency began a programme to revive the West End but the Agency ended in 2010 after the financial crisis. Perhaps Bracewell and Linder had the West End in mind when they wrote that “a defining characteristic of Morecambe and Heysham … is an uneasy coexistence between the victims and the beneficiaries of acute consumerism”. In 2003 there were plenty of victims but not many beneficiaries.
The seafront here is more sombre than that seen to the north. There are more ‘for sale’ and ‘to let’ signs but not so many as to indicate that all hope has been lost. The back streets are struggling. I saw on the relatively grand West End Road that there were half-a-dozen ex-hotels for sale within spitting distance of the sea. The West End needs to be integrated with, not ignored by, central Morecambe. Would a shuttle bus (akin to Blackpool’s trams) that trundled between Happy Mount Park and The Battery help? The Battery! It doesn’t sound appealing. Why not rename the area in honour of the recently-demolished Grosvenor Hotel?
I strode on to Heysham, which seemed to enthral Bracewell and Linder. They wrote that “Heysham village is compositionally-perfect: all details balanced, all perspectives aligned to the luminescence of the seaward light” and that “in all weathers, the view from the headland retains its capacity to awe the viewer, mesmerising in its fully realised, ever-changing grandeur”. Well, they are artists, so they should know. I hadn’t fully appreciated Heysham’s perfection on previous visits but I was determined to do so now.
The Rose Garden, the Winged World (a bird zoo) and the go-kart track have long gone, and the
headland has been restored to a maritime heath by the National Trust, and, yes, there is a good view over
the bay from the rock graves. However, try as I might, I cannot see the village as compositionally-perfect, aligned to the seaward light. If anything, the old Main Street, charming as it may be in its way, has its back to the sea. It saddens me that I lack the artistic sensibility of the professionals.
The view from Heysham Head, looking the wrong way, to the port and the power station
The tide was turning and so was I. I sauntered back to The Platform, which was once the railway station at which the hordes to Morecambe arrived.
The concert provided an apt exercise in nostalgia. The orchestra played programmes from Music While You Work
as heard on the wireless from 1940 to 1967. This light music was intended to raise the morale of ‘the workers’.
Nowadays we are too cynical to allow our morale to be lifted so easily. About 99% of the audience remembered the music
from the first time around and most, no doubt, regretted its disappearance from the wireless. Long may it not
disappear from Morecambe.
[November 25th 2018; SD4565; (linear) Scalestones Point – SW – Chapel Hill, Heysham – NE – The Platform, Morecambe (plus digressions); 7 miles; 82/400]
35.  Dufton Rocks
It is obvious that the character of our North-West England hills and dales is largely determined by the underlying rocks. I should therefore try to gain some basic understanding of our geology – but where should I start? According to the Smith (2010) ‘introductory guide’ to Lakeland rocks, “the Lake District is a rather complicated place. The sort of place where to begin to recognise rock types and to begin geology, you would probably say ‘I wouldn’t start from here’.” On the other hand, somewhere like the Howgills seems to me to be so uniform that I suspect that I’d learn only about a single rock type there. I need somewhere that displays different rocks conveniently side-by-side so that a beginner like me can distinguish between them.
Turnbull (2009) describes just such a walk – from Dufton, around Dufton Pike, and along Great Rundale
Beck. In a distance of about three miles several different types of rock are to be seen. Moreover, Dufton,
being in the North Pennines Area of Outstanding Natural Beauty, is within a Global Geopark, which UNESCO
defines as “a unified area with a geological heritage of international significance” – which sounds promising.
There’s even a ‘geodiversity audit
which is a new concept to me, as is a geopark. I have a lot to learn.
We set out hoping to spot the differences between the various rocks. Having approached Dufton from the south, across the white limestone scars of Orton Fell, we immediately detected that Dufton is different. It is red. Well, the green isn’t red but many of the buildings are. Turnbull tells us – and I am, of course, indebted to Turnbull for such details of the rocks and how they came to be where they are that I feel brave enough to mention here – that the red stone is St Bees Sandstone, 250 million years old. Yes, the St Bees of west Cumbria. What’s it doing over here, by the Pennines? I assume that this sandstone once existed all the way between St Bees and here but has, in between, been eroded away or buried.
The stones in the walls by the path from Dufton, which is part of the Pennine Way, turned from red to grey. The rock here is a shale, called Dufton Shale, reasonably enough, and is, I read, about 450 million years old. St Bees Sandstone and Dufton Shale are sedimentary rocks, created from ocean sediment. Obviously a younger sediment should be on top of an older one but here we have walked uphill to find the older rock. As Turnbull explains, we have crossed a fault, one which has caused the older rock on the east to end up higher relative to the rock on the west.
As the track approached Halsteads we saw that some of the stones in the wall alongside were orange, not grey. Small crystals of mica could be seen in the orange rocks. This is getting complicated. These orange rocks are of Dufton Microgranite and are from an intrusion of molten rock about 390 million years ago. An intrusion has to be into existing older rocks (by definition), therefore once we pass the Dufton Microgranite we return to the shale.
Now we climbed Dufton Pike (481m), battling against a strong, cold wind. There were not many exposed
rocks but what there were did look different to the shale below. Turnbull says that these are volcanic rocks,
although we could not honestly say that we found the bubble holes (vesicles to the cognoscenti) that he mentions.
These are rocks of the Borrowdale Volcanic series, the same series that is found in the most dramatic parts of
the Lake District. It is not dramatic on Dufton Pike. It is a smooth, grassy, conical hill. It does, however,
provide an excellent view of Cross Fell and up Great Rundale. In the opposite direction, across the green
Eden valley, we could not, because of the haze, make out Dufton Pike’s sister hills twenty miles away in
the Lake District. The Dufton Pike volcanic rocks are also about 450 million years old but older than the Dufton Shale, indicating that we have crossed another fault.
Great Rundale from Dufton Pike
Dropping off Dufton Pike and continuing up the valley of Great Rundale Beck, we came across rocks that look familiar to any walker of the Yorkshire Dales. These are slates and limestone of the Carboniferous period, 350 million years ago. Having dropped down to a younger rock, we must have crossed another fault, a fault that also separates the adjacent Knock Pike and Murton Pike volcanic rock from the rocks of the North Pennines to the east. With all these faults within such a short distance, it is surprising to me that the nearby sedimentary layers of the cliffs on both sides of Great Rundale have survived more or less level. Should I deduce that the North Pennine Faults occurred before these sediments were there, say, 400 million years ago?
We continued up Great Rundale, surprised that the beck within was virtually dry when it clearly causes significant
erosion when in the mood, and past a prominent limekiln to reach old mine workings with piles of grey stones that
we assumed are of the gritstone that forms the peaty plateau above. Turnbull admits to some difficulty in telling
the limestone and gritstone apart so we didn’t attempt a close study. We also didn’t attempt to continue up and
over to High Cup Nick as Turnbull did – we had seen enough rocks for one day. So we returned down Great Rundale and around the eastern side of Dufton Pike.
We walked past the nicely-named Pus Gill, which is a Site of Special Scientific Interest for its geology.
Here there are rocks of Onnian and Lower Longvillian age, forming the most extensive Pusgillian section in
the north of England. As you can see, my geology is coming on in leaps and bounds. (OK, I admit it:
I pinched that from the
[November 17th 2018; NY6825; Dufton – N – Halsteads – NE, SW – Dufton Pike – NE – Threlkeld Side – SW – Dufton; 6 miles; 81/400]
34.  Thieveley Pike and the Singing Ringing Tree
Thieveley Pike (449m) is the highest point of Deerplay Moor, five miles south-east of Burnley. The
climb to the top of the moor from the ambitiously-named Cliviger Gorge has a modicum of drama but
the top itself is unassuming. It is a smooth, boggy hump with just a trig point and a fence.
Still, the views are extensive: to Pendle beyond Burnley, to the West Pennine moors over Rossendale,
to the Bowland fells, and, on a clear day, to the Dales Three Peaks – not forgetting about sixty windmills.
From Thieveley Pike towards Burnley and Pendle
However, it seems that the region around Thieveley Pike is too dull for some. It has been enlivened by
various sculptures. I headed south past the source of the River Irwell, which flows through Manchester
to join the Mersey, to find the
Irwell Sculpture Trail
or the beginning of it at least because it is said to be England’s largest piece of public art, running for over thirty miles and including some seventy artworks. Unfortunately, I cannot report upon the artworks because I found no sign of or to the Trail where it is marked on the OS map, north of Weir. I understand that the Trail is a work in progress – perhaps it hasn’t yet progressed to the northernmost end of the Trail. Dark clouds were gathering, so I did not prolong my search.
I headed west on the Rossendale Way, aiming for the acclaimed Singing Ringing Tree. But never mind the artworks – I became depressed by the prevailing scruffiness. OK, autumn is an untidy time, with decay in the air and mud on the ground. This, however, does not excuse the rubbish, rusty machinery, rubble, and so on that litters the footpaths and roadsides. It’s as though the standards are set by the old dark stone walls. The walls are all falling down: why bother to tidy up anything else? There are no grants to keep these walls in order, as there are for walls in the Dales and Lakes, because their sombre appearance has no appeal for visitors.
After Sod Hey Farm I thought I might as well walk directly along the road to Crown Point and the
Singing Ringing Tree. The Tree was designed by Mike Tonkin and Anna Liu in 2006 and a year later won a
Royal Institute of British Architects National Award. It is now the centrepiece of the
Wayside Arts Trail
The Tree is one of four
the others being near Blackburn, Haslingden and Wycoller. I tried
not to let the pretentious re-definition of ‘panopticon’ put me off. The word was first used to describe a prison where all inmates may be monitored and has recently been co-opted for modern surveillance techniques and in photography to describe a kind of panoramic image. The Lancashire structures are called panopticons because they provide a comprehensive view. Actually, the view from the Tree is not that comprehensive: you can’t see far to the south.
The Singing Ringing Tree
Contrary to what I said above, the Panopticons were not designed to enliven dull regions: they “were designed to attract visitors into the countryside to enjoy the stunning landscapes.” Can a landscape dominated by a view of Burnley really be stunning? Aren’t visitors attracted to stunning landscapes anyway? Perhaps the designers, knowing that they would be, wanted more visitors to chance upon their artwork. Perhaps it was hoped that fine artworks would encourage people to treat their countryside with more respect than I had seen on my walk here.
In general, do we need sculptures in our countryside? This question rather presumes that we do need sculptures but not necessarily in the countryside. The countryside, it may be thought, speaks for itself. The word ‘countryside’, coming from the Latin contra (or other), implies that the countryside is other than something, the city. What is suitable for one may not be for the other. If sculptures are thought to be intended for the built environment of cities then we might think that they do not belong in the natural countryside.
I am not referring to structures such as cairns which may be more ornamental than their function
demands but to works constructed by an artist to be viewed in a countryside setting that have no function
other than to have an aesthetic impact upon the viewer. For example, Andy Goldsworthy created a series of
artworks based upon old
– there is one in Tilberthwaite, another near Cautley Spout, and so on. These works are intended to
meld into their surroundings so that a viewer may not even be sure whether they are artworks or not.
Most of these creations are ‘land art’, that is, they are created from natural materials. In many cases,
land art is intended to be ephemeral and to disappear into its surroundings in due course. Some artworks
don’t require materials at all. For example, Richard Long created
A Line Made by Walking
in 1967 by
walking up and down a field, a work considered a formative piece by the Tate Gallery in a 2007 exhibition. (Ah, perhaps we shouldn’t consider our worn hillside tracks as disfigurements but as works of art.)
These, however, are different from the explicitly artistic sculptures that are set prominently in
the landscape, such as the Water Cut in Mallerstang, installed in 1998 as one of a series of
and indeed the Singing Ringing Tree. I cannot think of anything similar on the Lake District fells although there are sculptures rather tucked away in Grizedale Forest, between Esthwaite and Coniston Water. I can’t picture a Singing Ringing Tree ever being installed on Helvellyn.
Anyway, I appreciated the Singing Ringing Tree as an imaginative reflection on the nature of its location. The main natural element of this exposed setting is the wind, which the sculpture certainly captures. As the name indicates, it is a structure to be heard as well as seen, although the noise of the wind in the pipes was, to me, interesting rather than attractive. Overall, is the Singing Ringing Tree more artistic than the windblown hawthorn tree that might otherwise have occupied this spot?
[November 12th 2018; SD8727; P SE of Holme Chapel – S, W, S – Thieveley Pike – SE, W – Height End, Clifton – N – Burnley Road – NW – Crown Point – E – Singing Ringing Tree – E – Dyneley Farm – SE, N, SE – Holme Chapel, P; 8 miles; 79/400]
33.  Is Nappa Hall Napping - or Dying?
I have it on good authority (in fact that of Historic England) that
which is near Askrigg in Wensleydale, is “probably the finest and least-spoilt fortified manor house in the north of England.” In that case, it deserved to be the focus for a saunter around the middle of Wensleydale.
The sun that brightened my drive to Wensleydale had disappeared by the time I reached it. Low cloud smothered the hills. All was grey, silent and still. If there were any remnants of autumn colour then they were thoroughly dampened, apart from a few larch which somehow kept their glow. Nothing moved (except a little traffic): it was as if life was preparing for a winter hibernation. I walked over the River Ure, past Bear Park (no, I didn’t see any) and on towards the famous Aysgarth Falls. It wasn’t on my itinerary to visit the falls but I had a quick look at High Force anyway.
I continued north to the village of Carperby, where every building that I saw was a fitting
stone-grey. The village seemed to disappear into the hillside. There were no white-washed walls
although one or two doors had been bravely coloured. Carperby is said to be a village of two
centres, a West End and an East End. I only saw the former – perhaps the latter is gayer, but I
doubt it. The gloom was getting to me – no doubt Carperby sparkles in the summer sun. I passed
only a few buildings but one of them was a Quaker Meeting House (1864) and two were Wesleyan
Chapels (1826, 1890). According to its
Conservation Area Character Appraisal
there are “dramatic views outwards from the village … towards Penhill, Bishopdale and Addlebrough”. I could see absolutely nothing across the valley and not much more of the nearby hills of Carperby Moor.
I followed the Oxclose Road (which is not a road but a bridleway path) west for three miles.
It is a good path for striding out, which is the best thing to do when the only scars to be seen are
not the limestone scars to the north but the scars of old lead mines near the track. The murk was
harder to accept knowing that it was sunny just five miles south. The only cheery sight was of two
hares lively enough to indicate that they do not have the myxomatosis that is said to be spreading
from rabbits to hares. I was momentarily excited by a sheep with impressive horns, which shows how dull
this walk had been.
Eventually I dropped down to Nappa Hall. The first impression is of large, solid grey
edifice in need of repair – understandably so, since it is mainly of the 15th century. It was
built by the Metcalfe family after land was given to James Metcalfe of Worton by Sir Richard
Scrope of nearby Bolton Castle following service at Agincourt in 1415. The hall is probably more
due to James’s son, Thomas, since James would have been getting on a bit by the time of most of
the building, in the 1470s. Thereafter, for three centuries, the Metcalfes set about consolidating
and enhancing their status in the region. They played a leading part in thwarting Scottish invasions
of northern England and took on various administrative roles. For example, Christopher Metcalfe
became High Sheriff of Yorkshire, a position of power he emphasised by having a retinue of 300
Metcalfes on white horses accompanying him to the York assizes in 1556. The Metcalfes energetically
propagated their name, so much so that by the end of the Middle Ages the Metcalfe family was
thought to be the largest in England (Muir, 1991). They seem to have had something of the
nature of a Scottish clan – indeed, the
today refers to the ‘Metcalfe clan’.
Nappa Hall (sorry, the cloud droplets have fuzzied this photo)
Nappa Hall reflected the growing wealth and status of medieval rural gentry. It has a long hall and two towers, of four and two storeys, with crenellated parapets that give an impression of defensibility. Subsequent alterations by the Metcalfe family are, according to a Historic England report, “not indicative of great wealth or having distinguished craftsmen at command”. After the Metcalfes left Nappa Hall in the 1750s it was occupied by tenant farmers. They had little incentive to maintain the whole building, and parts of it, such as the high tower, suffered from neglect. The wealthy owners did have schemes for the Hall, such as converting it into a shooting lodge, and it seems that a stable and coach house were added but the original Hall remains substantially intact.
Members of the Metcalfe family moved back into Nappa Hall in 1889 but sold it in 2008 to the
publican and artist, Mark Thompson. He put forward plans to renovate the Hall, including converting
some of the Hall and outbuildings for holiday lets. However in 2014 it was
that Thompson, although “in the middle of restoring Nappa Hall”, was moving to Greece. I don’t know what the situation is today.
To me, it seemed that Nappa Hall was grey, silent and still, like almost everything else I’d seen. A close inspection is not possible but I could see no sign of habitation or on-going work. There was nobody about and no cars parked. From the road there was nothing to even indicate that Nappa Hall was there – and I saw no indication that the building is of any significance. If Nappa Hall is as moribund as it seems to be and if it’s as important as Historic England says it is then it’s rather sad. But if all those Metcalfes don’t care about it, why should I? I cheered myself up on the walk back, along the old railway line and by the River Ure, by admiring the many fine barns, which are, in general, much more substantial structures than the acclaimed field barns of Swaledale to the north. The sun never made it to Wensleydale.
The River Ure, still under cloud
[November 5th 2018; SD9988; P on A684 – N, E – Bear Park – SE – High Force – N – Carperby – NW – Oxclose Gate – W, NW on
bridleway – Heugh – S – Nappa Scar Farm, Nappa Hall, old railway line – SE along railway line and by river – P on A684; 9 miles; 77/400]
32.  Russet Rusland Valley
(1914-1987), Lakeland poet and author,
was adamant that there is more to the Lake District than high peaks and large lakes, and for two good reasons.
First, he emphasised the contribution that ‘fringe’ regions made to the culture and heritage of the Lake District.
He lived all his life in Millom, in the south-west corner of Cumbria, and he naturally wanted to ensure that Millom and its residents were not overlooked in any account of the Lake District. I am not competent to judge Nicholson’s poetry but I like his comment when referring to a Keswick dining-room’s stained glass windows depicting the Lake Poets (Wordsworth, Coleridge, Southey and so on) that “it seems a pity they could not have left one window blank in case another local poet turned up” (Nicholson, 1969, p28).
Secondly, he was correct. Take, for example, the Rusland Valley, which lies between the southern ends of Windermere and Coniston Water and is thus hardly a fringe region, lying as it does within the Lake District National Park. It has no high peaks surrounding it. It has no large lakes – in fact, it has no lakes at all. The brochures do not encourage any visitor to travel to the Rusland Valley. And yet “it is a dale which has retained much of the look and tone of what southern Lakeland must have been before the tourists discovered it” (Nicholson, 1969).
However, Nicholson was writing fifty years ago. I went to see if the same might be said today.
I went first to Pool Foot, where Rusland Pool joins the River Leven before entering Morecambe Bay.
Rusland Pool is not a pool but it is hardly a river either. It barely moves, completely lacking the
sprightliness of typical Lakeland becks. I walked to Bouth, which is the valley’s largest gathering of
houses, about thirty of them. In the past, people lived scattered about the valley, making a living from
the pastures and the forests, through farming, coppicing, charcoal-burning, and so on. Some of the houses
have names that self-consciously echo that heritage, such as The Cooperage and Creel Cottage. I saw a notice
advertising the work of
a “community-led Landscape Partnership Scheme” that aims to revive traditional woodland skills in the region. Although I saw only two workmen on this walk (collecting logs in Crooks Pastures), there was much evidence of on-going work in the woods and the footpath trails were exemplary. I gained the impression that the locals were proud of their hidden valley. I don’t know what exactly they do to earn a living. There’s a pub, a caravan park, a farm with a café, and of course plenty of sheep and cows, but I noticed nothing else that would bring any income. No doubt many of the few houses are now holiday homes.
I continued north on the road to the
Hay Bridge Nature Reserve
As the road is a cul-de-sac there is very little traffic. I was passed by one car – or rather, I passed it: it was stationary. It was a very pleasant walk, through fields and woods, with views of surrounding woodland resplendent in their late autumn colours. The enclosing hills are low but high enough to screen all views of the high peaks. I passed a pond and then a larger one, but it was still not large enough for a name, although the hide nearby is named Harold’s Hide (I assume those to whom it matters know which Harold that is).
And then on to Hulleter Moss and Rusland Moss, a National Nature Reserve. These complete the impression that we are a world away from conventional Lakeland. There could hardly be a greater contrast than that between Scafell Pike and these mosses. The mosses are lowland raised mires, a habitat rare in Cumbria. The ‘raised’ means that the middle of the mire tends to accumulate more decaying vegetation and hence, over centuries, becomes slightly higher than the fringes. To the untrained eye the mosses are flat. They present an extensive vista of high, light-brown grasses and reeds, whispering gently in the breeze, with birch and pine growing on drier patches. It would be impossible to cross the mires safely without the boardwalks provided. According to an 1850 map online, spring tides reached inland as far as Rusland Moss, and I don’t see any reason why they shouldn’t do so today. The OS today marks the normal tidal limit at Crooks Bridge, some two miles south of Rusland Moss, but I saw no barrier to further in-flow. Whether this affects the special nature of the moss habitat I cannot say.
I walked past Rusland Hall and noticed that a house called The Syke (which was for sale) had a flock of
which I had never heard of. Perhaps you would inherit the Ouessants if you buy The Syke. On to Rusland
Church, perched on a knoll. It is big enough to welcome all within walking distance and their cattle too.
In the graveyard, by a huge, old yew, is the modest grave of Arthur Ransome (1884-1967), who wrote Swallows
. He lived the last years of his life at Hill Top – no, not Beatrix Potter’s Hill Top, but the Hill Top a few miles south in the Rusland Valley. Neither Hill Top is atop a hill.
South from Rusland Church
The map boldly marks ‘Rusland’ hereabouts but does not seem to refer to anything particular. The signpost at Rusland Church points back south to ‘Rusland’, so I took the church to be the northern end of the Rusland Valley. I walked back through the woodland on the eastern side. If you want a woodland walk then you could hardly do better than this. There were a few yews, as you might hope, in Yewbarrow Wood (a Special Area of Conservation) but the star trees were the tall beeches, aglow in the lowering sun, although perhaps just past their best.
I saw no squirrels or deer. Surely, there would have been more wildlife here when Nicholson was a boy.
Commendable efforts are being made to protect the valley’s special habitats, the mosses and the woodland, and
to revive old traditions – but the fact that a ‘Landscape Partnership scheme’ needs to revive them tells us
that the valley is, inevitably, not as it was. However, Nicholson has a point: the Rusland Valley is a worthy
part of the Lake District. It provides contrast, not competition, to the majestic central regions. Actually,
I did see one deer. It was tame, in the garden of Old Hall Farm.
[October 29th 2018; SD3484; Haverthwaite, by Anglers Arms – W – Pool Foot – N – Pool Bridge – NW –
Bouth – N – Burn Knott, Low Hay Bridge – N, across Hulleter Moss, Rusland Moss – N – Rusland Church – S –
Rusland Cross – E – Hall Brow Wood – S – Border Moss Wood – SW – Crooks Bridge, Pool Bridge – E, S, E –
Haverthwaite; 10 miles; 74/400]
31.  Pink Stones on the Orton Fells
The stone circle one mile east of Orton is magical but not because of its location or its structure.
Compared to the Castlerigg stone circle near Keswick, with its large monoliths in a dramatic setting
with a panoramic view, the
is uninspiring, being set in the corner of an ordinary field, with little view, and being composed of relatively small, prone stones. Not prune stones, prone stones. These stones have obviously fallen from the white limestone cliffs of the Orton Fells to the north and in the process of rolling down to form this circle have been metamorphosed into pink granite. That sounds magical to me.
Geologists have another theory. They say that a different trick has been played upon us. When we weren’t looking, during the last Ice Age, the pink stones were slipped here by glaciers from where the Shap Pink Quarry now is, five miles to the west. They call the stones ‘erratics’. Neolithic men and women must have gathered up 32 of them, plus one limestone boulder by mistake, to make this circle. Now, if the geologists’ theory were correct then the erratics wouldn’t just be in this one field – they would be scattered all around the region. So I would look out for them on this walk around the Orton Fells. I wouldn’t pause or divert from my route but I’d just see how many pink granite boulders I’d come across along the way.
I headed east on what is part of the Coast-to-Coast walk and by the time I reached the road at Acres I’d already spotted eleven ‘pinks’, including two in the wall of a barn (so, 43 in total). I saw another seven (50) around the hamlet of Sunbiggin, where I noticed that they have recently set up a Coast-2-Coast Café. I wonder how well it does, in this spot out-of-the-way except for those walkers. I pressed on to Sunbiggin Moor, where although this heathery land has probably never been cultivated I didn’t see any pinks. Perhaps I was distracted by the views of autumn mist lifting from the Howgill valleys and from Wild Boar Fell.
Sunbiggin and the Orton Fells from Sunbiggin Moor
Turning north, I came upon a pink so big that it has a name, Mitchell’s Stone (51). It is embedded in the wall that forms the parish boundary. Next I walked up and over the limestone terraces of Great Kinmond, with fine views opening out of the North Pennines ahead and of the Lake District hills to the west, with the distinctive profile of Blencathra prominent. I saw another pink when I reached the bridleway and a further seven close by the path further north (59). Here the soil had turned a dark red, which I assume is the influence of Penrith Red Sandstone.
I continued to the ancient settlement near Maisongill which the
Historic England website
considers to be “a good example of a Romano-British enclosed hut circle settlement”. To me, it seemed to be a set of strange humps in a field, with a few stones sort-of-aligned. There were two pinks (61) among the stones. This region appeared to be prime farming land, with lush green fields well stocked with contented cattle and sheep. I passed six more pinks (67) in the fields and by the fine track over Asby Winderwath Common up to the Great Asby Scar gate.
Great Asby Scar
Here Natural England has fenced off an area as part of a
Great Asby Scar National Nature Reserve
The absence of grazers naturally leads to a change in the vegetation. The limestone terraces heretofore had been rather bare, with just the occasional shrub surviving the attentions of the sheep. Here, heather and small shrubs-cum-trees are recolonising. It is a rather captivating, secluded area among limestone outcrops that I imagine at other times of the year has a more impressive display of flowers. I had forgotten about the pinks until I stepped on one embedded in the path (68).
I cut across to see the Thunder Stone, another large pink embedded in a wall, spotting another pink on the way there, and on over Beacon Hill to the road, seeing three more pinks on the way (73). The path down to Broadfell passes fields that have a number of large stones within. With my new expertise at identifying pinks, I’d confidently say, from a distance, that these are also pinks. I counted twelve (85), and, since I’d otherwise have to trespass with a tape measure, I declare two of them joint winners of the largest pink prize. They looked about two metres round. The glaciers did well to shift those.
The Thunder Stone with North Pennines beyond
The beck flowing past Broadfell seemed somewhat jaunty and not fully settled into its bed. At a wee bridge at least eight pinks (93) had been used to protect the bank. I saw three pinks in the beck, two beside it (98) and I suspect many protecting it, overgrown with moss. At this point, two buzzards circled noisily above – which made me realise that the Orton Fells had been devoid of bird sound, unless you count a helicopter.
Entering the village of Orton, I noticed three large pinks embedded in garden walls, two
used as garden ornaments, and about twenty positioned along grass verges – all before I’d reached the ice-cream shop. I stopped counting. Clearly, the residents of Orton are fond of their pinks. Yes, the pink granite boulders are well scattered around the Orton Fells. The geologists might be on to something.
[October 15th 2018; NY6208; Orton – E – Street, stone circle, Acres, Sunbiggin Moor – N – Mitchell’s
Stone – N, NW, N on Dales High Way – settlement – NW, SW on Sayle Lane, SW – Great Asby Scar, Thunder Stone –
SW – Beacon Hill, quarry – S – Broadfell, Orton; 11 miles; 72/400]
30.   Dunsop Bridge, Whitewell and Duchy-land
29.   The Quiet End of the Ribble Way
28.   Broughton Moor, or What's Left of It
27.   The Footpaths of Anglezarke Moor
26.   A Booze by Any Other Name
25.   Mysterious Harkerside Moor
24.   Up Ingleborough with the Holiday Crowds
23.   The Kentmere Diatomite
22.   In the Lancashire Yorkshire Dales
21.   The Fortunes of Fleetwood
20.   On the Sunny Side of Pendle
19.   Viewpoints around Keswick (part 2)
18.   Viewpoints around Keswick (part 1)
17.   Sheep-Wrecked Matterdale?
16.   The Wildflowers of Sulber
15.   On the Hobdale Fence
14.   Logging Along the Cam High Road
13.   The Cairns of Grisedale Pike
12.   Uplifted by High Street
11.   The Struggle over Boulsworth Hill
10.   The 'Hillfort' of Addlebrough
9.   "The Prettiest Mere of All" Lakeland
8.   What Price Catrigg Force?
7.   Castling in Cumbria: From Brougham to Lowther
6.   The Count of Flasby Fell
5.   Circumperambulating Stocks Reservoir
4.   In a Flap at Bolton-le-Sands
3.   Zipping around Thirlmere
2.   The Dentdale Diamonds
1.   The Taming of Caton Moor
(and here's some I did earlier)
© John Self, Drakkar Press, 2018
Top photo: The western Howgills from Dillicar;
Bottom photo: Blencathra from Great Mell Fell