A Photographic Tour of the Finest Showcave in Britain
I can never get a decent picture of Clapham falls, such is the contrast between dark vegetation and foaming white water. Artificially created by the Farrers of Ingleborough Hall, who dammed the valley to create the lake above - they were hidden by vegetation for many years, until recently revealed once more. In spate, they are a magnificent sight.
The Farrers were no doubt keen to show their visitors the delights of Ingleborough Cave, and the track through the dale was soon widened for the passing of horse and carriage, with elaborate stopping points along the way, like this well known 'grotto' complete with vaulted ceiling.
Such elaborate construction would cost a fortune today. The Grotto has the appearance of a chapel, with grotesquely carves limestone boulders protruding above the doors and windows.
A view from the opposite direction. There's a real 'cave-like' feel about the interior. Perhaps it acclimatised the more nervous members of the group for what lay ahead ...
Looking back down the elegant, tree-lined Clapdale Drive, laid out by the Farrer family. Wild garlic is very much in evidence. The trees hide the fact that the slope on the left drops into a tremendous ravine, with Clapham Beck (formerly Fell Beck before dropping down Gaping Gill) winding its way down towards the lake.
Clapham Beck winding its way down the dale. It has, at the top of the photograph, just emerged from Clapham Beck Head, just by the fence at the top left of the photograph - having last seen the light of day several days before when dropping into the tremendous shaft of Gaping Gill, less than two miles to the north. Get your head around that one!
The impressive entrance to Ingleborough Cave always gives me a sense of excitement no matter how many times I have visited. It clearly once discharged, many years ago, the waters from Gaping Gill, as can be seen from the shallow dry valley - the former stream bed - now swathed in grass on the right of the photograph.
Once known as Clapdale Great Cave, only 56 yards of the cavern were accessible before the momentous year of 1837. A Stalagmite barrier on the back wall, known as 'The Bay' appeared to be holding back a lake, with little airspace above. On September 16th of that year a massive flood, one of the heaviest ever known, saw the lake rise to the ceiling with water surging through the cave entrance as well as from Clapham Beck Head, the present resurgence point ....
The flood aroused the curiosity of James Farrer, an intrepid member of the family from Ingleborough Hall. Once the waters resided, he and a gamekeeper friend, Josiah Harrison, tried to force a way into the small hole - but without success. They returned then to this yawning entrance, that of Clapdale Great Cave, with several builders, and set to work removing the stalagmite barrier of 'The Bay' - effectively draining the lake beyond forever. Doing that, they became the first human beings ever to tread where thousands have ventured since ... and all this with just tweed suits and candles. Many perishingly cold, deep pools were ponded by stalagmite barriers, and James himself simply swam through them! Having come this far, he wasn't for letting cold water get the better of him. He was soon 'Farrerway' in the depths of Ingleborough ... (get it?)
Even just a few yards in , the beauties start to reveal themselves - many of the pools, hemmed in by stalagmite, being crystal clear.
The Mushroom Bed, sometimes called the Woolsack - is a gorgeous white pillow of stalagmite, with delicate honeycomb structure. Beside it, to the left, are typical flowstone 'organ' like structures, so typical of the Yorkshire caves.
Features like this have built up over thousands of years - where calcite rich water has seeped into crevices causing a plug of stalagmite to build up. The contasting colours are impressive.
The 'Inverted Forest' area of the cave, just inside the entrance, shows peculiar features, some of which appear to have formed beneath the old level of the lake, as can be worked out by comparing with the 'tide mark' on the wall.
This photograph of the passage, close to the Mushroom Bed, shows the difference in colour between the rock revealed in 1837 (bottom) and the darker limestone above - with the obvious former water level easy to follow.
After heavy rain, some spots are more vulnerable than others. Here the slowly dripping water has altered the composition of this beautiful golden 'haystack' of calcite, smoothing out the honeycomb effect with new layers of deposition.
The Eldon Hall reaches its climax at the stunning Beehive formation. In this picture, the former water level can clearly be seen at centre - the tiny protruding fingers of the Beehive being an ideal indicator of stalagmite formation times, as those final centimetres have taken an incredible 176 years to form! The cave's most famous stalactite, the massive 'Sword of Damocles' adds to the glory of the scene on the right - over 2 metres (7 feet) in length.
The Sword of Damocles is, unquestionably, one of the finest stalactites in the country, and is worth the entrance price alone, in my book. If you consider that one of those tiny stalactites in the ceiling would have been forming before the reign of Queen Victoria, then that gives a mere indication of the age of this monster.
This picture gives a better indication of the growth of the Beehive. Note the water level (the highest of the two bands on the right) and compare the amount of growth beneath. Come back in 1000 years or more - and it may well reach the floor (hey - that was a poem!!!)
Eldon Hall is left where a stalagmite barrier is crossed by a little bridge to meet the Elephant's Legs, two specacular calcite columns, where stalagmite and stalactite formation has combined for the overall effect. Note his tail too - a stalactite well placed. Oh, and you can use your imagination with any other appendages!
On the left, the delicately illuminated chamber, never overpowering, manages to do justice to great sights like this exquisite pillow of stalagmite.
The famous 'Pillar of Inglebrough Cave' is then reached - where Professor W. Boyd Dawkins began, in the 19th century, experiments designed to show the rate of growth of cave formations. It is a perfect example of a joined stalactite/stalagmite, and must be of an immense age. Beyond looms a pothole within the cave floor, termed 'The Abyss' and leading into tight, awkward passages.
Beyond, on the left, is the bizarre Showerbath, or Queen Victoria's Bloomers. Described by Albert Mitchell in Yorkshire Caves and Potholes as 'a couple of Yorkshire hams, hanging from the wall.' A strange, plant-like shape has developed on the stalagmite beneath, noticeably symmetrical.
Keep looking upwards, my dears, for the 'Witch's Fingers' - letting the water drop on you at your peril. Her little finger is hideously deformed in size and ready to spike intruders ...
After a back-breaking low passage (well, it is when you are six feet four anyway) you emerge at a T junction with the right branch leading off to the lovely Gothic Arch. On one side is the First Ring of Bells, while the Lady's Cushion can be glimpsed through the archway.
As with so many 'Organ Pipes' in the Dales, these produce delicate musical notes when lightly tapped, though it is wise never to touch such delicacies.
Towards the end of the accessible show cave, this fossilised coral can be seen on the left wall - the large, wide scallops in the limestone indicating that water has usually once moved slowly along this passage - rather than at force.