Monday 29 December 2014

White Wonders of Penyghent

The Lion Dons her Winter Coat




Penyghent never fails to impress in the snow, and yesterday was no exception.  Like Ingleborough, she is made up of a massive 'cone' of Yoredale rocks - alternating layers of limestones, sandstones and shales forming a rocky sandwich, which were determined by changes in sea levels millions of years ago.  Also, like her more famous neighbour, she sits on a plinth of Great Scar Limestone - only, here on Penyghent this isn't so obvious as the main benches have been covered by a layer of glacial drift (seen behind the trees in the picture).  Not to be outdone by her cousin, little Penny packs a punch, and yesterday's conditons were perfect to see just how much!


There wasn't much snow in the lower reaches of Ribblesdale.  This youthful section of the River Ribble is an important salmon spawning ground.



Any visit to Stainforth Foss, late in the year, will see the determined fish leaping up the fall on their way to the upper reaches.  It is one of the highlights of the Three Peaks!  I took this shot in late November.


Another wonderful sight, as we drive along Ribblesdale, is the majestic tilted limestone outcrop making up Smearsett Scar - or Smearside.  Its environs are literally peppered with ancient settlements, burial chambers - and, of course, the famous 'Celtic Wall.'  The view from the top is astonishing - as, usually, is the wind!  The 'echo' around Smearsett is also amazing.


The snowline on Penyghent often covers just the upper Yoredale Series slopes, leaving a contrasting panorama of blue, green and white.  


The lane up to Brackenbottom draws the eye onwards towards this magnificent peak.  The famous 'nose' of Penyghent is well seen in this image.  Like Ingleborough, the mountain is topped by a thin layer of millstone grit - formed when rivers washed coarse grits and sand into a very shallow, swampy sea.  Hard to imagine any of that being under water, when you look up there - but it was indeed!


Not often do the works of man fit in well with the great features of limestone country, but this is an exception.  Here, the beautiful simplicity of the church at Horton-in-Ribblesdale fits perfectly with the crouched feline presence of Penyghent.  


There are three very famous potholes on the west flank of the mountain, essentially formed where water rushes off the impermeable Yoredale slopes (seen with a dusting of snow) and meets the Great Scar Limestone.  This is the gigantic opening of Hull Pot - not a quarry - but totally natural.  Water only enters in times of flood, over on the left as you view the image.  It has been formed on a fault, and massive wedges of rock have peeled off the sides at intervals to make the hole bigger over long periods of time.  Hull Pot is one of the truly breathtaking sights of the Yorkshire limestone.  The layer of glacial drift, smothering the benches, is well seen in this picture above the wall.


The second, and completely different in character, is the nasty looking slit of Hunt Pot - most people's standard idea of what a pothole should look like.  Here the stream cascades down a fault guided joint into the depths of the earth ... or so it seems.  Notice how meltwater has managed to carve out a huge basin in which the main sink actually sits.  Hunt Pot is potentially lethal - so keep youngsters and dogs well clear.


Last but by no means least is Penyghent Pot itself.  The Hunt Pot water eventually meets the main drain down in the depths of this monster.  No big drop this time, but a slot into a series of energy sapping long crawls in freezing cold water, eventually reaching great depths and with no way out at the bottom. What goes in ... must come out the same way.  Penyghent Pot tests even the hardest cavers.  


And where does all this water emerge?  Well, in normal conditions - and as far as is known, most of water emerges here, at Brants Gill Head.  The clump of trees hides the secret - but the noise of running water can be picked up easily when walking on the path behind the Crown Hotel in Horton.  


This is the approach to the cave of Brants Gill Head, where the water resurges. The hawthorn berries add beauty to the wild and impressive scene.  


The mouth of the cave sees the water emerging on the left side.  The right hand side quickly closes down to a narrow fissure.  In flood conditions it's impossible to get anywhere near.


I love this view from the mouth of Brants Gill Head, looking downstream at the emerging water - which must have one heck of a tale to tell.


The same view in monochrome is equally impressive.


There are many mysteries involving the water beneath Penyghent.  In high flood, for example, Brants Gill Head cannot cope with all the water and the water suddenly begins to surge out of Douk Gill Cave, seen here - and half a mile away to the south.  Douk Gill is a stunning little spot, described by 19th century writers as 'Malham Cove in miniature' and particularly enchanting.  This view is from the lane behind Horton Primary School as the Gill is on private land.  Winter allows us a glimpse as in summer it is smothered by foliage. In extreme weather, not even Douk Gill can cope, and so another exit, Dub Cote Cave, lying further south still, is used by the water.  


I took the path behind the Crown Hotel to see more of Penyghent's hidden wonders - pausing to admire the works of man, which fit in perfectly in Ribblesdale.


Wandering northwards, this barn forms a great picture backed by the dominating presence of the Ingleborough massif, with a coating of snow.


In the distance, Little Ingleborough can be seen leading up to the summit of Ingleborough itself, with the spur of Simon Fell on the right.  Beneath live the limestone benches, not covered by drift, but having been swept clean by the Ribblesdale glacier to leave smooth pavements of limestone.


I always like to photograph my shadow - just to prove a mortal like me actually had a place for a few seconds in this fantastic landscape.  It is a privilege to walk it!


At the head of the dale, Whernside's 2419 feet provide a massive wall, with a thin layer of swirling cloud.


The path soon reaches the sensational sight of Sell Gill Holes.  The water originally sank in the now dry entrance just right of the wall at the top of the picture.  It has since found its present 'wet' route into the massive Main Chamber below.  


The wet entrance at Sell Gill Holes leads down this slippery staircase into a passage, and then down a big pitch into the Main Chamber.  It is a tricky route and best tackled in dry weather.  Also, hidden inside this way, is the daunting 37 metre Goblin Shaft, an alternative way into the depths.


Most cavers sensibly stick to the dry route, the 'v' shaped notch indicating a former water channel.


The initial drop is only about 35 feet this way - before two more drops requiring ladders or abseiling.


Some idea of the situation at the dry entrance to Sell Gill Holes.


The Sell Gill Suspension Bridge.


Don't try these silly things.  I was just wishing I was still fit enough to descend.  Fortunately I decided to live another day so you can enjoy another post.  I stepped back ...



This was the view behind me when I was peering into the pothole - the obviously abandoned waterfall that formed the original entrance to the system.


This roofless barn beyond Sell Gill Holes always invites a camera.  The dusting of snow adds further beauty, as does the lowering sun.


An alternative view, with the clouds scudding gently over Park Fell in the background.


Jackdaw Hole lies just off the track and is surrounded by a fence.  It is rarely visited, though clearly labelled on the OS map.  The 5o foot deep shaft, plugged by a layer of glacial deposit, is like a setting from The Lord of the Rings.  It's well worth a nosey!


A view into Jackdaw Hole from the southern end, showing the walls of Great Scar Limestone.


A view of the northern end of Jackdaw Hole, with the usual array of ferns and ash saplings clinging to the limestone.


This is where you expect to see Gollum.  A view into the depths of Jackdaw Hole from the west side, showing the glacial debris plugging the shaft, which would originally have been much deeper.  It is clearly very ancient.


The ash tree at the west side provides a sensational view in, but it was too icy today for comfort.


I love this view down into the depths beneath the gnarled and twisted old branches of the ash.  Very wild!



Just beyond, and shyly hidden to the right, is the sinister entrance to Penyghent Long Churn.  This unfenced hole drops at least 70 feet into constricted, inky blackness.  It is possible to wiggle on your tummy to watch the water falling straight as a plumb line into the limestone.  The shaft is extremely flood prone and needs perfect weather to have a go!


This is usually where you do your tummy wiggling, but in ice you may wiggle an inch too far - so I didn't!!



As the sun was lowering and the temperatures dropping, I headed back, well satisfied, along the Pennine Way - past this ancient gatepost - which appears to be lost in another time.


The low angle of the setting sun gave the scene a real sense of being 'lost in time'.  


A quick detour to the east just gave me enough time to capture the last glimmers of light on Penyghent - the Lion of Ribblesdale.


Here she lies, magnificent, above the sweeping layer of glaical drift hiding her biggest secrets.


See you again, pal ... I'll be back soon.



Sell Gill, Jackdaw Hole and Penyghent Long Churn are great objectives for a leisurely stroll from Horton, taking the track behind the Crown Hotel.  Walking eastwards over the moor to Hunt and Hull Pots, the return track to Horton can be picked up for an enjoyable circular - full of suprises.  Enjoy your exploring!


Stephen x

Tuesday 23 December 2014


The forthcoming book: 'A Three Peaks Up and Under' to be published by Scratching Shed Publishing in the Spring of 2015, is the result of 30 years exploring and thinking about the limestone landscapes of the Three Peaks.  With 22 chapters, 15 describing adventures 'above' and seven 'below' ground - the book also contains an extensive introduction 'for rock fans only' - describing how the caves, potholes, pavements and other limestone curiosities came to be.  Illustrated by the author and written in a highly humorous style - it is certain to have seasoned Three Peaks walkers dusting off their boots and examining this amazing region with fresh eyes.

Saturday 6 December 2014

Leck Fell - a Glimpse into Hell?

From the Eyes of Death to the Fairies' Workshop



Leck Fell is an isolated limestone plateau - actually in Lancashire, but an essential part of the 'Dales' limestone country.  The limestone is covered by a layer of boulder clay and the moorland can be bleak to the timid observer - even off-putting.  Yet Leck Fell is a fascinating landscape where many ancient and spectacular pothole shafts drop deep into the bowels of the earth to link up with the longest cave system so far discovered in Britain.  One of the shafts was formerly known as 'Hell Hole', and for many centuries folk believed these yawning chasms were actually gateways to the lair of his satanic majesty.


Great Coum lies to the north, beyond Ease Gill, while the lonely heights of Gragareth rise to the east - overlooking Leck Fell House, surely the most remote dwelling in Lancashire, if not the highest.



On this adventure I explored the north west corner of the landscape shown here - where lurk some of the most bizarrely beautiful, yet dauntingly dangerous surface openings in Britain. Leck Fell is private land, and caving strictly requires a permit - but the landowner does not usually object to a lone walker, or a sensibly small group, having a peek at the marvels on show.  If great care is taken throughout, and the obvious footpaths adhered to - this is a rewarding place of endless fascination.  An obvious car parking spot is reached on the left of the lane which reaches the moor from the A65, two fields down from Leck Fell House - while scanning the skyline above the house in clear weather will reveal the ever present Three Men of Gragareth.


As we enter the enclosure to the left we can see how the boulder clay that covers the limestone has slumped to form dolines or shakeholes like this one, due to the activity of water underneath.


Following the wall westwards, a fenced hole is immediately obvious to the right, hiding the entrance to Short Drop Cave.



Following the wall, as we are, from the parking spot, you can see how we meet the doline and divert to the right (north) to Short Drop Cave, with the forthcoming horrors clearly marked!!!


The neat little entrance drops, as the name suggests, into an active streamway and, with sufficient skill, cavers can emerge in Gavel Pot in the next field.  Short Drop Cave is a wonderful underground experience with some superb cascades and formations.


From Short Drop, a glance to the north will reveal a prominent tree, and approaching it becomes obvious this is hidiing something rather special - if sinister.  This is the tremendous chasm of Rumbling Hole, best described by the Balderstons in their classic 'Ingleton, Bygone and Present' (1888):  'We felt spellbound for the moment, and quite unmatched in our cave hunting attire for the felicitous loveliness before us.'  They go on to say that: 'In the tables of memory we set it down, that others might revel in what so delighted us, accustomed as we have been both from youth and observation to such scenes.'  Clearly, Rumbling Hole's 155 feet shaft left a lasting impression.


The curious name originates from the strange sounds that emanate from depths as the water rushes in from Rumbling Beck Cave; the whole ground seeming to vibrate - and the Balderstons continue: 'Tap tap tap comes slowly from the distant depths; this is the home of the gnomes or fairies; they are at work below in their workshop, and a far-off hammering can be heard.  Leave them in peace!  Some day the good fays may work your weal, although the ill-natured have designated as Rumbling Hole, what we prefer to dream of as the Fairies' Workshop.'


Whatever the name - this is a mind-numbing place: inspiring equal amounts of awe and delight.


Couches of heather and ferns slope perilously down to the drop.  The Balderstons speak of: 'mosses, polpody, blechnum and oxalis.'  This is a botanist's paradise.


This wonderfully coloured spectacle is the view that so captivated those 19th century explorers, a tree at the western end forming a convenient 'v' from which to view the depths of Rumbling Hole.  This is believed to be the most ancient of the holes on Leck Fell, probably carved out along a fault by a long vanished water source certainly well before the last glaciation.


Even the limestone sides of the shaft are coated with luxurious vegetation.


Nearby, a depression on the moor sees Rumbling Beck Cave swallowing a small stream.  The stream emerges as a waterfall in the Fairies' Workshop of Rumbling Hole - 8 metres below the surface.  


A sparkling little cascade forms a pool in the limestone beds before making its way into Rumbling Beck Cave.


Peering into Rumbling Beck Cave - a narrow, clean-washed canyon in the limestone.


Looking across the fell as we exit Rumbling Beck Cave.  Here the uplifted greywackes run along the Dent Fault in Barbondale to form Calf Top: a spectacular sight when catching the sun.


After the massive dimensions of Rumbling Hole, we meet this little fella - the cute and aptly named Humble Pot.  All shapes and sizes are available on Leck Fell.


A dry valley ends in this prominent limestone cliff - below which is the entrance to Long Drop Cave. The Balderstons write that, having lit a candle: 'our progress was unceremoniously arrested eight or nine yards from the mouth by a hideous rift' and 'a sudden descent of thirty feet might have rewarded carelessness.'


The entrance to the main passage of Long Drop Cave.  This was probably formed by a meltwater channel during a warmer 'periglacial' spell, though its exact age is uncertain. Many of the caves and holes on Leck Fell are plugged with glacial debris suggesting they outdate the last glaciation and are very ancient features.


Another entrance into Long Drop Cave.  Boulder clay can be seen on the left, having slumped into the hole.


And  yet another way-in to Long Drop Cave - definitely not for the faint hearted!


Returning to the moor, a breeding site for Red Grouse.  Their persistent call of 'go back, back, back' may well be a wise one considering what lies in store for us next.


Another fenced shaft - this time of a very different nature.  This has been largely filled with glacial debris and was no doubt once a much deeper feature.


It bears the name of 'The Eye Holes' and you can see why: a splendid limestone bridge forming the top of the nose between the two gaunt sockets.


The 'Eye Holes' just have to be explored by the true lover of limestone.  You have to clamber beneath that velvety nose, having already come this far!


Here I am under the 'bridge' of the nose: a special place.  When you stand here, you feel rather special, knowing not many have ever passed beneath this bridge.  You are privileged.


Privileged indeed!


Exiting the Eye Holes, glance south west to the wall running down the field that marked the start of our adventure.  This limestone man, outstetched hand on the left and clenched fist on the right, is the only sign of anything remotely like a human.


The glance will reveal another tree - and this time a hole you just don't want to mess with! This is Death's Head Hole, named by Harry Speight in 1892 as the 'Hell Hole' itself, and take great care if you cross the fence.  


You can easily understand why, to the locals of long ago, this was indeed the entrance to Hell.  The massive shaft drops a straight 200 feet into the limestone, but as the Balderstons tell us (1888) : 'not so richly adonred as the Fairies' Workshop, but still radiant in its embellishments.'


This is the mouth of the Death's Head in close-up, the sinister 200 foot (64 metres) shaft a daunting sight - and some 70 feet (23 metres) down it is possible for cavers to climb into East Passage, a very ancient stretch of cave formed entirely underwater but now left dry and choked by glacial debris.


The fern garden of Death's Head Hole is ironically beautiful considering the shocking scene of the immediate surroundings.  Wainwright calls this ' a twin in terror to Rumbling Hole' and decribes the pair of them, somewhat unromantically for him, as ' places fit for a horror film.'


The best time to visit is in the autumn, as during the summer the luxuriant vegetation covers the finest view of the main shaft.  Death's Head Hole is humbling to the onlooker - and the modern world seems to be of another planet in comparison.  This is the world before we came and spoiled it.


If the main shaft is the mouth, here at the eastern end are the eyes and nose, separated by a bridge of rock with massive drops through the sockets that would be your last.  Let's have a closer look if we dare ...


The staring eyes of the Death's Head.  Here I am standing on one bridge, looking at another, and with sheer drops all around. It's not a place to hang around long.  Sinister if not bizarrely so, Death's Head Hole makes even experienced adventurers shudder.  An amazing place.


It's actually a relief to remain alive and think 'well it didn't get me this time' as you emerge once more onto the heathery moor.  But another mean surprise lies in store ....


... and a big one at that, for this is 'Big Meanie'.  'Mean' I suppose in that it looks like a cute little walk-in cave entrance compared to what we've encountered up to now ... but not far inside a huge 49 metre shaft plunges into the bowels of the earth, so don't even think about entering.  Even worse, the first few metres of the drop are tight, and squeeze the caver's delicate parts before he finally hangs in the black void.  Mean indeed is Big Meanie.


Big Meanie is easy to find as it lies in a shakehole alongside an obvious 'chink' in the stone wall.  It was probably carved out by meltwater stream.  If we could pull off all that boulder clay, we would see the gleaming limestone underneath in which Big Meanie has formed.


It's then a case of following the wall back to the starting point - that way, at least you know you're not goiing to fall down any holes.  Can you believe it - I met another human!!!???  His words were, in an American accent, 'I'm a just gowna chick out da big meaneeeee' .... I thought I was dreaming.  There's others as mad as me in the run up to Christmas.


When you've been 'almost under' for a couple of hours you feel like goiing 'up' and surveying it all, and there is no better way than climbing Gragareth.  To do this we follow the lane up behind Leck Fell House ....  is that Sky tv I detect in this 'untouched' landscape???? Argh!!


What a view though, as we climb, across to Barbon Low Fell and beyond to Morecambe Bay and the Lake District.  The field containing all the potholes we've just visited lies, heather-clad, to the left.


The view across to Calf Top, the massive uplifted wedge of Ordovician rocks uplifted along the Dent Fault.


The sun then reappeared and the view was just ... well, stunning.


A scramble up off the path behind the house, and we meet the Three Men of Gragareth.  At over 2000 feet this might look a drab mountain, but trust me the views are UNBELIEVABLE!!!


How do they remain standing in the elements that must hammer at them, unrelentingly?


In Wainwright's words: 'They have an origin beyond the memory of man ....'


  'they stand side by side, mute sentinels overlooking a vast panorama that has never changed and never will.'


Well they can occasionally!!!  Here's the Four Men of Gragareth.  Self portrait this one ... set the ten second time and leg it!


One of my favourite places on this planet.  It was indeed mute.  Wind, sheep, birds, vehicles .... none of them interrupted absolute silence.  There was a living world down there somewhere.  I had to kick myself to believe it.


Gragareth is formed of the same Yoredale series of alternating sandstones, limestones and shales that make up the more shapely Three Peaks.  Amazing to think that these layers were laid down over a vast amount of time by fluctuating sea levels.  All this lot was once under water, and near the equator!


Geology and the Dales have never-ending stories, more spectacular than any we create.


I stayed here a long time, chewing on my thoughts  ...


Until the light began to fade ...


And the last glimmers of November sun warmed the cockles of the Three Men.


Then it was a melancholy wave goodbye to old friends from an Oldfield.


And very soon my glimpses into hell ...


... had become a glimpse into heaven.




Stephen x