I bought a copy of this publication yesterday, it’s wonderful, I’d highly recommend it.
I bought my copy from the excellent Book Corner in Saltburn. Its available as a printed book or digital format, the printed version is selling out quickly so you may have to hunt down a copy. Further details can be found here.
Pretty much at the top of my post-lockdown visit list was a trip to visit Jenny Twigg and her Daughter Tibb and the Sypeland Crags in Upper Nidderdale. Following a minor navigational blunder, nothing new for me, I met up with Mr. Chappell and Mr. Vasey and we set off across Fountains Earth Moor.
Travel almost anywhere in the Pennines and their foothills, you’ll see crags and cliffs defining the upper slopes of the Pennine Dales and hilltops. These outcrops are generally composed of either sandstones or limestone. Millstone Grit is a generic term for a number of Pennine sandstones. Both the sandstones and the limestone were deposited over 300 million years ago during the Carboniferous Period.
At first, with some spread of warm shallow seas, limestone formed, the Carboniferous or Mountain Limestone that was to be built into some of the most solid and respectable piles in England, buttresses of its pride and self confidence. The work of silting up these Carboniferous seas was completed by deposits brought from the northern continent of Atlantis, then hot, mountainous and swept by monsoons. A large river with tributaries drawn from territories stretching from the north of Scotland to Norway poured out its coarse sediments across north-eastern England. So were Norwegian pebbles brought to Yorkshire and held in the Millstone Grits that were laid down as the deltas of this northern river.
The Pennine limestones are massive and dense and form great scars where they outcrop along the scarp edges of the hills. Limestone can be weathered chemically, the weakly acidic rains and rivers of the uplands gradually dissolves the limestone to form the deep gorges and caves and the iconic limestone pavements of the Karst landscapes of the Pennine Uplands.
When Millstone Grits outcrop on the scarp edges they tend to form crags and cliffs. These sandstones are resistant to chemical weathering so are eroded by wind and ice. the weather is able to erode the weaker beds within the sandstones and sculpt the rocks into strange shapes. There are many of these sculpted outcrops along the Pennine edges and tops, almost all were formed during the last Ice Age, the most well known being Brimham Rocks which is now owned by the National Trust and has been a popular tourist attraction for many generations.
Sypeland Crags are little known and somewhat off the tourist beat and track, this was evident by the lack of ancient or modern graffitti on the rocks. The rock type here is the Lower Brimham Grit, a course grained sandstone. There are only 3 named rocks on the moor, Jenny Twigg and her Daughter Tibb and a massive boulder called Tib’s tent.
The origin of the Twigg and Tibb names is not known and there are very few literary references to the stones. I first read about them in Guy Ragland Phillips book, Brigantia – A Mysteriography. Phillips quotes a passage from William Grainges 1863 book, Nidderdale.
..is a large group of naked rocks, some of them of enormous bulk, called Sypeland Crags; they are of the course millstone grit, like those of Brimham, the grotesque grandeur of which they imitate, though on a smaller scale. Two of them a short distance from the main group are tall upright pillers and at a distance have the appearance of giantesses in broad bonnets, from which resemblance they have recieved the names of Jenny Twigg and her Daughter Tibb,
The folklore of the area says that Jenny Twigg and Tibb were the keepers of a drovers inn on the side of Dead Man’s Hill. They are said to have robbed and murdered three drovers and buried their decapitated bodies. When the bodies of the men were discovered Jenny and Tibb were found guilty of murder and hanged. Another tale says that they were witches who were turned to stone, a familiar tale at number of megalithic sites. The tale of the witches being turned to stone is very similar to tales in Scandinavian folklore where are number of large rock features are thought to have been giant trolls, of both sexes, who were instantly petrified when the suns rays fell upon them.
Ragland Phillips book doesn’t mention the murders and there appears to be no official records of the trial and execution of the women. He does mention the summit of Dead Man’s Hill, telling us that three headless bodies were found at a point where three tracks diverge into Wharfedale, Coverdale and Nidderdale. He goes on to say that it is also the point where three walls meet at a ‘peculiar’ structure known as Jenny’s Gate. It strikes me that the burial of three headless bodies at the point where three important tracks meet, if true, sounds more ritualistic than anything else.
Jenny Twigg has a hole running through the stone, the hole is large enough to pass your arm through. In some parts of our islands there was a tradition that any oath or vow sworn, including marriage, and shook upon through a holed stone, was ‘sealed in stone’ and never to be broken
There are a number of beautiful weather-sculpted rocks along the edge of the crags.
Some of the rocks have been undercut by the elements, one has been walled-in to form a rock shelter. Others have small pools of peat-stained water at their base and on the top surface of one large rock there are a number of large basins, the most I’ve ever seen.
Pereidolia – The Kiss
Tibbs Tent and light snow
This is a grouse moor, the butts are well kept, there is a maintained shooting house and there is grit left out for the birds, over the course of our day we only saw one grouse on the moor. We left for home watching squalls drifting over the distant Vale of York.
Sypelands – Sibberlands 1609
Nidd – British river name. Root Nei – to be brilliant. Nedd/Neath – Wales, Nita – Germany, Nidar – Scandanavia
Moors. Remains of Elmet – Ted Hughes 1979
A Land – Jacquetta Hawkes 1978
Brigantia, A Mysteriography – Guy Ragland Phillips 1976
Map Image reproduced with the permission of the National Library of Scotland
The Consise Oxford Dictionary of Place Names – Eilert Ekwall. 1974 edition
For many years I’ve have a deep fascination with sites prefixed with the name ‘Old Wife’. With plenty of time on my hands, I decided to have a go at something I’ve been wanting to do for a long time, create a map. The sites that I’ve select are all physical places and are named on maps. The map covers the three main linguistic elements of my researches, Old Wife, Carling/Carlin, Cailleach.
The word Wife means woman, it has only been used to signify a woman’s marital status relatively recently, therefore the Old Wife means, Old Woman. The second main element is Cailleach, a Scots and Irish Gaellic word which is still in use today and means, Old Woman/Hag/Witch. The Final element is the word Carling, which is the the Scots equivalent of Cailleach. For completeness, I have also included a few sites with a Witch element in their names as these are relatively rare, I’m still not sure if they are relevant but have included them anyway for interest.
The word Carling has been a little problematic as the element Carl means a free peasant in Old English and Old Scandinavian e.g. the etymology of the word Carlton would be a settlement of free peasants. Whereas the etymology of Carling Howe, which was originally called Kerlinghou, means the hill of the old woman or hag. I have tried my best to filter-out these name elements and have hopefully only added relevant sites on the map.
Key – Blue = Cailleach, Green = Carling, Red = Old Wife, Orange = Witch
When looking at the distribution map, I cannot think of any other mythological or folkloric figure who is so well represented in our landscape and yet, as my friend Graeme points out, remains so anonymous . I suppose, given a millennia and a half of an interlinked church and state, which in the past has actively suppressed to any whiff of witchcraft or the supernatural, especially when practiced by women, the fact that her name has survived and remains embedded in our landscape is quite remarkable. The distribution of sites may also say something regarding certain commonalities between the cultures of the early inhabitants of the northern and western parts our islands.