Sharing words: recommendations part one

Victoria Franklin – Conservation Graduate Trainee

Without the Conservation Department’s usual mid morning coffee time over the last 18 months we’ve missed out on the usual office chatter of what everyone thought to the latest BBC Countryfile episode, what people have been growing in their gardens or the interesting things we have seen on our site visits. So with my late summer holiday looming I thought I would ask what everyone’s favorite books are, not that my book shelves are in need of anymore!

So here we go with a list that contains some of the Department’s favorite books, each with its own synopsis. This is part one of a two part series, this part containing ten Natural History books and part two containing ten Local History books. Maybe our recommendations will inspire you to pick up a book and learn something new as the darker nights draw in.

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The Peregrine by J A Baker

J. A. Baker’s extraordinary classic of British nature writing was first published in 1967. Greeted with acclaim, it went on to win the Duff Cooper Prize, the pre-eminent literary prize of the time. Luminaries such as Ted Hughes, Barry Lopez and Andrew Motion have cited it as one of the most important books in twentieth-century nature writing.

Despite the association of peregrines with the wild, outer reaches of the British Isles, The Peregrine is set on the flat marshes of the Essex coast, where J. A. Baker spent long winters looking and writing about the visitors from the uplands – peregrines that spend the winter hunting the huge flocks of pigeons and waders that share the desolate landscape with them.

“… honestly the most beautiful prose by this guy who’d never written a book before … wrote this absolute banger then disappeared back into obscurity.” 
Ann Pease, Ryevitalise Administrator

The Harvest of the Hills’ by Angus Winchester

This illustrated environmental history of rural life in Northern England and the Scottish Borders in the late medieval and early modern periods explores the relationship between society and the environment – the ways in which humans responded to and used the environment in which they lived. The author uses the orders and byelaws made by manorial courts to build up a picture of how pastoral society in the Pennine, Lake District and Border hills husbanded the resources of the uplands. It offers an upland, pastoral paradigm of land use, the management of common land, and the transition from medieval to early-modern farming systems to balance the extensive literature on the agrarian history of the lowlands. The geographical scope of the book includes the Lake District, Yorkshire Dales, the Border hills, the North Pennines and the Forest of Bowland.

“One other that has come to mind – is ‘The Harvest of the Hills’ by Angus Winchester. It’s a historical look at farming practise and kind of environmental history, including the use/exploitation of common land in the upland north and borders. It covers the period 1400 – 1700, so quite useful for understanding the landscape as we see it now.”
Miles Johnson, Head of Historic Environment

“As a general cultural/natural heritage crossover, how about …”
Miles Johnson, Head of Historic Environment

The History of the Countryside by Dr Oliver Rackham

Exploring the natural and man-made features of the land – fields, highways, hedgerows, fens, marshes, rivers, heaths, coasts, woods and wood pastures – he shows conclusively and unforgettably how they have developed over the centuries. In doing so, he covers a wealth of related subjects to provide a fascinating account of the sometimes subtle and sometimes radical ways in which people, fauna, flora, climate, soils and other physical conditions have played their part in the shaping of the countryside.

“Miles great shout, I love that book.”
Holly Ramsden, Conservation Officer

Nightwalk: A journey to the heart of nature by Chris Yates

Chris Yates, one of Britain’s most insightful and lyrical writers, raises his gaze from his beloved rivers and ponds and takes us on a mesmerizing tour of the British countryside.

“Last November, the sudden appearance of a hundred wintering ravens in a wood in Cranborne Chase, where I have lived for twenty-five years without seeing more than a few solitary specimens, reminded me that there is always something ready to flame up again in the landscape, just when it seemed the fire had gone out.”

In Nightwalk we accompany Chris Yates on the most magical of journeys into the very heart of the British countryside. His acute observation of the natural world and ability to transcend it exquisitely sets Chris apart from his contemporaries.

Time slows down for a deeper intimacy with nature, and through Chris’s writing we hear every rustle of a leaf, every call of a bird. He widens the power of our imagination, heightening our senses and revealing beauty in the smallest details.

Edgelands by Michael Symmons Roberts

The wilderness is much closer than you think. Passed through, negotiated, unnamed, unacknowledged: the edgelands – those familiar yet ignored spaces which are neither city nor countryside – have become the great wild places on our doorsteps.

In the same way the Romantic writers taught us to look at hills, lakes and rivers, poets Paul Farley and Michael Symmons Roberts write about mobile masts and gravel pits, business parks and landfill sites, taking the reader on a journey to marvel at these richly mysterious, forgotten regions in our midst.

Edgelands forms a critique of what we value as ‘wild’, and allows our allotments, railways, motorways, wasteland and water a presence in the world, and a strange beauty all of their own.

Feral by George Monbiot

In Feral, George Monbiot, one of the world’s most celebrated radical thinkers offers a riveting tale of possibility and travel in the wild

How many of us sometimes feel that we are scratching at the walls of this life, seeking to find our way into a wider space beyond? That our mild, polite existence sometimes seems to crush the breath out of us?

Feral is the lyrical and gripping story of George Monbiot’s efforts to re-engage with nature and discover a new way of living. He shows how, by restoring and rewilding our damaged ecosystems on land and at sea, we can bring wonder back into our lives. Making use of some remarkable scientific discoveries, Feral lays out a new, positive environmentalism, in which nature is allowed to find its own way.

“A journey to the heart of nature by Chris Yates (guy goes out at dusk and walks through the night in the countryside), Edgelands by Michael Symmons Roberts (wildlife and value of ‘wasteland’ and scraps of land on edges of urban areas), Feral by George Monbiot (rewilding, humans needing to up their game etc) and anything by Robert Macfarlane obs  …. We’ve developed a bit of a problem in this house buying them and our front room does resemble the natural history section of Waterstones.”
Ann Pease, Ryevitalise Administrator

A Sting in the tale by Dave Goulson

One man’s quest to save the bumblebee…

Dave Goulson has always been obsessed with wildlife, from his childhood menagerie of exotic pets and dabbling in experimental taxidermy to his groundbreaking research into the mysterious ways of the bumblebee and his mission to protect our rarest bees.

Once commonly found in the marshes of Kent, the short-haired bumblebee is now extinct in the UK, but still exists in the wilds of New Zealand, descended from a few queen bees shipped over in the nineteenth century.

A Sting in the Tale tells the story of Goulson’s passionate drive to reintroduce it to its native land and contains groundbreaking research into these curious creatures, history’s relationship with the bumblebee, the disastrous effects intensive farming has had on our bee populations and the potential dangers if we are to continue down this path.

“I loved [it].”
Holly Ramsden, Conservation Officer

“… also on my list would be …”
Victoria Franklin, Conservation Graduate Trainee 

The Hidden Life of Trees by Peter Wohlleben

This book is a lens to help you take a closer look at what you may have taken for granted. Slow down, breathe deep and look around. What can you hear? What can you see? What do you feel?

Are trees social beings? How do trees live? Do they feel pain or have awareness of their surroundings?

In The Hidden Life of Trees, Peter Wohlleben makes the case that the forest is a social network. He draws on groundbreaking scientific discoveries to describe how trees are like human families: tree parents live together with their children, communicate with them, support them as they grow, share nutrients with those who are sick or struggling, and even warn each other of impending dangers.

Wohlleben also shares his deep love of woods and forests, explaining the amazing processes of life, death and regeneration he has observed in his woodland. A walk in the woods will never be the same again.

Entangled Life by Merlin Sheldrake

Here is a lifeform so strange and wondrous that it forces us to rethink how life works…

Neither plant nor animal, it is found throughout the earth, the air and our bodies. It can be microscopic, yet also accounts for the largest organisms ever recorded, living for millennia and weighing tens of thousands of tonnes. Its ability to digest rock enabled the first life on land, it can survive unprotected in space, and thrives amidst nuclear radiation.

In this captivating adventure, Merlin Sheldrake explores the spectacular and neglected world of fungi: endlessly surprising organisms that sustain nearly all living systems. They can solve problems without a brain, stretching traditional definitions of ‘intelligence’, and can manipulate animal behaviour with devastating precision. In giving us bread, alcohol and life-saving medicines, fungi have shaped human history, and their psychedelic properties, which have influenced societies since antiquity, have recently been shown to alleviate a number of mental illnesses. The ability of fungi to digest plastic, explosives, pesticides and crude oil is being harnessed in break-through technologies, and the discovery that they connect plants in underground networks, the ‘Wood Wide Web’, is transforming the way we understand ecosystems. Yet they live their lives largely out of sight, and over ninety percent of their species remain undocumented.

Entangled Life is a mind-altering journey into this hidden kingdom of life, and shows that fungi are key to understanding the planet on which we live, and the ways we think, feel and behave. The more we learn about fungi, the less makes sense without them.

“OOH! and Entangled Life by Merlin Sheldrake (best name???) – extraordinary book about fungi.”
Ann Pease, Ryevitalise Administrator  

English Pastoral by James Rebanks

As a boy, James Rebanks’s grandfather taught him to work the land the old way. Their family farm in the Lake District hills was part of an ancient agricultural landscape: a patchwork of crops and meadows, of pastures grazed with livestock, and hedgerows teeming with wildlife. And yet, by the time James inherited the farm, it was barely recognisable. The men and women had vanished from the fields; the old stone barns had crumbled; the skies had emptied of birds and their wind-blown song.

English Pastoral is the story of an inheritance: one that affects us all. It tells of how rural landscapes around the world were brought close to collapse, and the age-old rhythms of work, weather, community and wild things were lost. And yet this elegy from the northern fells is also a song of hope: of how, guided by the past, one farmer began to salvage a tiny corner of England that was now his, doing his best to restore the life that had vanished and to leave a legacy for the future.

This is a book about what it means to have love and pride in a place, and how, against all the odds, it may still be possible to build a new pastoral: not a utopia, but somewhere decent for us all.

“I have loved seeing everyone’s reading suggestions. I now have a long wish list! Like Victoria I have recently read the English Pastoral by James Rebanks and thoroughly enjoyed it.”
Rachel Pickering, Woodland Team Leader

Summer exhibitions

“Staithes Art Club [Annual Exhibition]

For many years now the district about Staithes, though, more especially, at first, at Runswick and Hinderwell, has been the summer home of a few able and conscientious artists, who have discovered unconventional subjects for their brush, and by careful study, have greatly improved their powers of perception, their appreciation of the relative values of lights and colours…Like Whitby, the paintable bits about Staithes and Runswick are illimitable …

… there was a gay and fashionable little assemblage present, which viewed with evident interest the representative collection of works on the walls of the upper room of the building which, from its large window, looked upon the the as from the deck of a steamer …

…There can be but one opinion among the fraternity of the brush as to the value of an exhibition of this kind, for comparison and criticism are the very soul of improvement and are valuable guides to a complete success.”

Whitby Gazette – Friday 8 August 1902

The exhibition referred to was the second of a series of short lived annual exhibitions held by the Staithes Art Club between 1901 and 1907. During the 1880s/1890s and 1900s artists, both professional and amateur, both men and women, lived or regularly stayed in or around Staithes, which has lead to the idea of a ‘Staithes Group’ of artists.

Most of the artists counted in the Group originated elsewhere, many from other places in the north of England. The east coast of Yorkshire had been opened up by a new railway line. Artists came and went during the period, some were just starting out, some were already academicians e.g. Royal Scottish Academy, Royal Society of British Artists, Royal Watercolour Society.

Although many of the pictures displayed at the exhibitions were of Staithes and its environs and local people that wasn’t always the case, what was important was the artists themselves. For a period of their life they were associated with a Staithes Group because of where they lived or worked and whether they displayed their work at the Staithes Art Club annual exhibitions. It’s noticeable that it was a loose association not an artist colony or a Staithes ‘School’; indeed Laura Knight, one of the Staithes Group, gave the yearning for close companionship of other painters as one of the reasons she ended up leaving Staithes.

“Staithes Art Club – A Choice Exhibition

There appears to be no particular leader, or style … Their aims are similar, but their methods are very dissimilar. They each try to give the broad truths of nature, ignoring almost entirely anything which would detract from the first impressions.”

Whitby Gazette, Friday 18 August 1905

The High Tide, Runswick Bay, North Yorkshire – Frederick William Jackson – https://artuk.org/

Most of the pictures were rural landscapes, picturesque people (mostly working people) and conventional horses. Most of it was ‘en plain air’ that is painted outside rather than in a studio. The art was naturalistic, romanticised and sometimes impressionistic (but not too much). There was a sense of little suggestion of bohemian lifestyles or contentious art from the Group, it was all rather respectable. The 1903 Annual Exhibition had patrons including Sir Charles M Palmer MP, a North East Shipbuilder who had a country estate at nearby Grinkle Park, Loftus. Another patron was the MP for Whitby – E W Beckett – although he turned out to be rather more of a free spirit.

The writers in the Whitby Gazette who attend the annual exhibitions approve of the pictures that are well modelled and well managed faithful renderings, of good composition which are peaceful, sweet, harmonious, delightful, pleasing, rich in quality, natural in colour, strong yet tender.

“Staithes Art Club

… The visitors to this small exhibition will be at once struck by the diversity of aim and methods of the artists represented. In this respect, the work is very instructive. We may refer to the manner and treatment of both oils and water colours. May of the exhibits are successful efforts to portray the charm of colour and subtlety of things seen in the open air. We have others in which the painter has apparently ignored the latter quality, depending on bold masses of colour and strong contrasts in light and shade. Then we come to work which almost leaves colour alone, but somehow conveys it, with a hint. In each method we find some merit and reason. It is well that art can be so varied, otherwise, once and for all, colour photography would settle the thing. It is the personal interpretation, after all, which matters – the seizing upon the salient points, to the exclusion or suppression of such minor ones as would, if too much emphasised, detract from the work. If we bear those things in mind, in viewing the exhibits, and try and understand the aim of the painter, we shall receive greater pleasure and instruction.”

Whitby Gazette, Friday 17 August 1906

Carting Sand – James William Booth – https://artuk.org/

It’s clear from the reporting in the Gazette that the venues used for the exhibitions were small. At first it was the Fisherman’s’ Institute in Staithes; then Andersons Gallery, Well Close Square, Skinner Street in Whitby; and then The Gallery, Waterloo Place, Flowergate in Whitby. The pictures exhibited were therefore also small, in one of the exhibition reports the writer suggests this means they could be usefully hung in an ordinary house. Most of the professional artists at least would have been attempting to make some kind of living.

It has been suggestion that this restriction in size as well as the small regional market for pictures were reasons for the falling away of the Staithes Group. It’s noticeable that the same time as the Staithes Art Club annual exhibitions are advertised in the Whitby Gazette each year there are more adverts for other art exhibitions. Art Clubs had become a popular concept in all sorts of provincial places.

Figures on the Shore – Arthur A Friedenson – https://artuk.org/

A loose association is easily dissolved. William Gilbert Foster an original member of the Club died in 1907 and the Knights left Staithes in the same year. The last official annual exhibition of the Staithes Art Club was held in 1907. Joseph Richard Bagshawe suddenly died in 1909, he had been another founding member. Leandro Garrido also died in 1909.

However it didn’t mean everyone just left; it’s clear from paintings held at the Pannett Art Gallery in Whitby that Staithes Art Club artists were still painting locally in 1920.  Around the same time the Fylingdales Group of Artists was founded in Robin Hood’s Bay to the south of Whitby. Nowadays the Fylingdales Group still exist and Staithes is still a focus for artists, there is even a Staithes Art School.

Toil – Mark Senior – https://artuk.org/

So why for that brief period were turn of the 20th century artists drawn to Staithes and the north east coast of Yorkshire – Laura Knight shared her reasons in an autobiography thirty years later.

“The roofs were red tiled or thatched, the walls made of brownish-yellow ironstone, and there and there was a white-washed cottage with green shutters. The wooden quay, called the e stretched right across the beach forming a poor protection against a nor’-easter. Two walls of cliff formed barriers on either side; the northern side reached out its rounded arm, along which the Beck ran into the sea from springs on the high moor. The excuse I offer for writing about Staithes at such length is its tremendous influence on work, life and power of endurance. It was there I found myself and what I might do. The life and place were what I had yearned for the freedom, the austerity, the savagery, the wildness. I love it passionately, overwhelmingly. I loved the cold and the northerly storms when no covering would protect you. I loved the strange race of people who lived there, whose stern almost forbidding exterior formed such contrast to the warmth and richness of their natures.”

Oil Paint and Grease Paint, Autobiography of Laura Knights, 1936

When Laura Knight describes why her and her husband left for Cornwall and the Newlyn ‘School’ in 1907 she describes being tired of wet and cold and lonely winters and tragedies (i.e. the drowning of boat men). But she’s still very sorry to go.

Staithes – James William Booth – https://artuk.org/

Below a is a non comprehensive list of artists associated with the Staithes Group and links to an example of their work from around the same time as the Group was active.

John Atkinson

Joseph Richard Bagshawe

James William Booth

Owen Bowen

John Bowman

Andrew Charles Colley

Lionel Crawshaw

Ernest Dade

William Gilbert Foster

Arthur Friedenson

Leandro Garrido

Ralph Hedley

Rowland Henry Hill

Henry Silkstone Hopwood

John William Howey

Hannah Hoyland

Spence Ingall

Frederick William Jackson

Isa Jobling

Robert Jobling

Harold Knight

Laura Knight

Charles Hodge Mackie

Frank Henry Mason

Fred Mayor

Frederick Stuart Richardson

Mark Senior

Albert George Stevens

Joseph Alfred Terry

Into the shadows

Victoria Franklin – Conservation Graduate Trainee

Thanks to archaeologists and historians we know a lot about the people who lived and worked in the historic landscape, but less about the shape and ecology of the landscape. There have been a lot of theories by ecologists such as Frans Vera and George Peterken, who suggest that the landscape was fluid with more wood pasture rather than the closed canopy dense woodlands we’re more familiar with today.

Historic woodlands were a hub of life, providing fodder for livestock and materials for villagers, farmers, tanners, blacksmiths, carpenters, broom whittlers and charcoal makers. Trees were even a source for medicine, for example the bark of Pedunculate Oak Quercus robur was used as an antiseptic and Ash Fraxinus excelsior was steeped into tea and used to aid kidney problems. This eco-cultural hub seems a far cry from how we see woods today, often used as a place of tranquillity, for bird watching or to seek refuge from everyday life.

Over the past year I’ve been researching ‘Shadow Woods’ – areas where there was woodland in the past that is no longer there. These, now shadows of a former landscape, can be identified in a number of ways. As a starting point for the search, the Doomsday Book and historic Tithe and Enclosure maps can give an indication of how the landscape once looked. Researching old place and field names such as ‘Hagg’ meaning an area where trees were felled or ‘Hollin’ historically a word for Holly or browse, also give clues as to the location of previously wooded areas.

With permission from land managers, we followed up on potential sites by surveying for any ancient woodland indicator species, ground flora that has colonised over generations and gives an indication that the area has been continually wooded for a considerable length of time. These species will change from woodland to woodland and throughout the country, but include Bluebells Hyacinthoides non-scripta, Honeysuckle Lonicera periclymenum, Ramsons Allium ursinum, Wood sorrel ‎Oxalis acetosella, Early purple orchids Orchis mascula, Primroses Primula vulgaris and Climbing corydalis Ceratocapnos claviculata. These plants continue to flower long after the surrounding woodland has gone. The residual flora and soils in these spaces are irreplaceable.  

Primroses Primula vulgaris, Wood anemone Anemonoides nemorosa amongst bracken and Hawthorn Crataegus monogyna scrub. Copyright NYMNPA.

Early purple orchids Orchis mascula and Primroses Primula vulgaris, strong evidence that the area is a Shadow Woodland. Copyright NYMNPA

Any remaining veteran and ancient trees were surveyed for signs of being worked, which gives another glimpse into the past history of the wood. Coppiced trees such as willow were cut at the base when they are relatively young and the wood was used to make fences and shelters. Pollarded trees were cut just above the trunk to provide timber and fodder for animals leaving the tree alive to produce more wood in future years. An historically pollarded tree can be identified by having multiple branches.

Historically coppiced Willow. Copyright NYMNPA.

Ancient and Veteran trees are home to a whole host of deadwood beetles, fungi, lichen mosses and plants that cannot live anywhere else. These trees, botanical indicators and the soil of ancient and shadow woods are irreplaceable micro-habitats that have taken generations to create, once lost they will be gone forever.

The Shadow Wood sites surveyed within the North York Moors National Park were all in upland locations, many in remoter areas with little human disturbance since they were worked woodlands. The majority of these sites have been classed as grassland or as scattered parkland with a small amount of ancient or veteran trees. This classification strengthens the idea that the historic landscape was often open wood pasture rather than closed canopy woodlands.  

The hope is that identified sites can be targeted for woodland creation in the North York Moors National Park, therefore continuing and restoring life in these magical habitats, that are not only home to some amazing species and important trees but are a little bit of folklore too.

Shadow woodland in the North York Moors. Copyright NYMNPA.

The Shadow Woods project within the North York Moors National Park has only been possible due to the dedicated work of Professor Ian Rotherham. His book Shadow Woods: a search for lost landscapes and publication Shadow Woods and Ghosts Survey Guide by C. Handley and I. D. Rotherham have provided invaluable research into these almost lost landscapes.

Keeping it old style

Clair Shields – Planning Officer (Policy and Building Conservation)

The traditional black and white ‘finger post’ signposts in the North York Moors have become a cherished part of our landscape. In order to maintain and conserve these cultural features for future generations to enjoy, at the end of last year Building Conservation officers at the National Park Authority asked parishes and residents to let us know about these signs so they could be mapped and recorded on our Geographic Information System (GIS). The idea was to gain a better understanding of where the signposts are and their current condition. Many signposts are obvious, such as at modern road junctions, however others can be more hidden such as where they are located on old roads which are less used today. Local people looking out for signs during daily exercise was a useful survey method during lockdowns.

At the same time we were able to refurbish a few of the signs most in need of restoration using a locally experienced contractor – this will help ensure the longevity of these iconic features. The long term aim is to restore them all.

There is a vast array of different practical purposes to the signs; some make reference to the old North Riding District (pre North Yorkshire County Council), others warn of steep inclines, point towards historic monuments like a roman road or indicate public route ways and distances. Officers are keen to conserve the variety of designs and styles.

The work over winter was looking to continue previous work carried out by the Authority and the North York Moors, Coast and Hills LEADER Programme. This time there were limited funds available through the Anglo American Woodsmith Project Section 106 compensation and mitigation agreement.

Here is an example at Egton Bridge where signage has been recently consolidated.

 

The Future of the North York Moors National Park?

The National Park Authority has begun a process to develop a new Management Plan for the National Park in collaboration with partners and stakeholders. If you have any interest at all in this National Park or National Parks as a whole – you’re a stakeholder. Since our last Plan was drawn up in 2011/12 there are new environmental challenges to confront, new environmental issues to take on and new environmental priorities to progress…

Paul explains below how you can get involved in shaping the future, if you would like to.

Paul Fellows – Head of Strategic Policy

Every few years we take the opportunity to ask ourselves what we want the North York Moors National Park to be like in the future and how we might realise that vision.

In doing this we would really like your ideas – the people who live and work in, care for and visit this special place. Generation after generation has helped create this landscape, from moorland, dale and forest to village, farm and field. Many millions more cherish this place as visitors and supporters. The National Park looks like it does because of you and your families; its future is in all our hands.

Our task is to help create a shared vision that we can all agree on, because that’s the best way to pass the National Park on to future generations in an even better state. What do we want farming, housing, tourism, transport, business, heritage and nature conservation to look like? What sort of place do we want to grow up in or grow old in? What’s the correct balance that works best for everyone?

Over the course of the next year we’ll enshrine this shared vision in a document called a ‘Management Plan’, which will set out exactly the work that needs to be done. We want the plan to be ambitious but deliverable; we want to anticipate the challenges and work together to meet them. We’ll set dates and targets, so that you can see the progress we’re making together.

This then is your chance to help us by having your say about the future of the North York Moors National Park. You’ll have your own ideas of what the National Park could and should be like in twenty years’ time. Every viewpoint is valid. Each opinion matters. The more perspectives that are offered, the stronger the overall plan and vision will be.

Think of this as a conversation about the future. It’s always an important discussion to have, though perhaps – after the experiences of the last year – more vital than ever before. Tell us your thoughts and hopes. Be bold. It’s your National Park and together we can plan effectively for better days ahead.

To start with, we’ve created a quick survey that asks up to five short questions so you can let us know what you think the main issues are.

If you would like a bit more background, or to look at some of the challenges we think we are facing, please take a look at our ‘working together’ page, which goes into more detail and asks more specific questions. We’ve come up with three themes to think about – Leading Nature Recovery, Landscapes for All, and Living and Working Landscapes. There is bound to be a lot of cross over between these themes, for instance in regards the historic environment. Anyway, have a think yourself and let us know your thoughts by email .

You can also keep in touch – if you want to be kept informed of further work on the Management Plan please join our mailing list.

 

Reading the Past: ‘Snapshots’ of Ironstone Life in Rosedale

David Mennear – Land of Iron Administration Assistant

The Land of Iron Landscape Partnership Scheme, funded by the National Lottery Heritage Fund, David Ross Foundation, and the North York Moors National Park Authority among others, will shortly be coming to an end in March 2021.

Rosedale Bank Top calcining kiln after conservation work was completed in 2019, with the new interpretation panel and Cor Ten silhouette.

Over the past four years the project has helped to protect, interpret and conserve the most iconic of the old ironstone mining sites and remains within the North York Moors. We have also helped to nurture the unique natural environment that surrounds them by working closely with land managers and other national partners ensuring habitats and species, such as riverbanks, ancient woodland and the Ring Ouzel, are cared for in the long term.

Yet even as we help to preserve the integrity of the monuments and help to protect the rich bio-diverse landscapes for the benefit of future generations, the voices of the individuals who once worked in the ironstone mining industry – the navvies (temporary workers), railwaymen, miners and families that expanded the populations of small villages like Rosedale during the Industrial Revolution – remain largely silent within the landscape in which they once worked, memorialised only in the receding industrial remains.

It is with this thought in mind that I turned to one important historical record where the individual stands recorded for posterity – the humble newspaper archive.

It is a place where accidents were recorded and individuals were named, where drunken brawls in isolated villages were highlighted and surreal accidents at remote kilns noted. The current newspapers of the time provide an invaluable insight into the social life and activities of the communities that populated the working life of the ironstone industry. It is here that you can understand the often-hidden tensions and terrors that so bedevilled a thriving but dangerous industry which helped to power the country in the 19^th century.

Rosedale East kilns with new fencing as a part of the Land of Iron project.

Below are a few sample extracts taken from local and regional papers during the height of the ironstone mining industry in the North York Moors, with a particular focus on Rosedale and its concentration of the unique railway, ironstone mines and imposing calcining kilns at Bank Top and Rosedale East. This way we can get a ‘snapshot’ of a particular place within a relatively short amount of time.

Please note that the following extracts reflect mores of the time. You may find elements of the extracts upsetting. 

Liverpool Daily Post 10 June 1862
CLASH BETWEEN MINERS AND IRISH LABOURERS
At Rosedale, last week, the English miners combined to drive out the Irish labourers out of the valley, which they did. Some sharp fighting took place. The cause of the party feeling is stated to have been owing to an Irishman contracting for work at an under price.

Whitby Gazette 8 April 1865
ROSEDALE ABBEY
On Saturday morning last as a boy named John Hugill, 12 years of age was preparing a set of ironstone wagons for being drawn up the incline, another wagon unexpectedly ran against them with great force at the moment the boy was bent down between 2 wagons which he was coupling, and they were driven together with great violence causing such severe injuries to the boy that death resulted in a few minutes.

Whitby Gazette 29 August 1868
ROSEDALE WEST MINES
A fatal accident occurred on Monday 24th to a miner named Thomas Taylor of Low Row, 19 years of age.  It appears that he had gone to his usual work in the mines at 2 o’clock and had only been at work about 10 minutes, when a huge portion of ironstone from the roof, weighing five or six tons, fell suddenly, and in its descent, came in contact with the poor fellow mutilating him in a frightful manner.

York Herald 5 December 1868
HORSE BURNT TO DEATH
On Wednesday night, a valuable horse, belonging to the Rosedale and Ferryhill Mining Company, was accidentally burnt to death. A driver, named Foster, was fetching a set of loaded waggons out of the Rosedale East mines on to the top of the new calcine kiln, when, through neglect of having a spring catch on, he was unable to get the horse unyoked from the waggons. The consequence was that the horse was dragged into the kiln, which was full of burning ironstone, and burnt to death.

Leeds Mercury 10 April 1871
THE ROSEDALE IRON MINERS
Gentlemen, I would earnestly call attention to the sad and disgraceful state of drunkenness prevalent among the workmen engaged in the Rosedale iron mines …. For two or three days following each pay-day Rosedale village presents a scene of inebriation which baffles description. The miners may be seen staggering about the village in all directions, and not unfrequently fighting and kicking each other in true Lancashire style.

Malton Gazette 15 July 1871
ROSEDALE MINING FATALITY
On Saturday morning, a young man named Nelson, a native of Thornton Dale near Pickering, was proceeding to his work underground, being a miner, between 7 and 8 o’clock, having under his arm a small barrel, open at the top, containing 4 to 5 lbs of gunpowder, used for blasting purposes. Wishing to light his pipe, he struck a match, part of the match or a spark from it, ignited the powder, which exploded with great violence. His injuries were fearful, that death terminated his suffering in 2 to 3 hours later. He was accompanied by another man who escaped with rather severe shock and singeing of his whiskers and eyebrows.

Rosedale Hollins Mine and incline, with Bank Top calcining kilns visible at top right.

Of course this is just small selection of the more dramatic clippings from the Land of Iron newspaper archive, but it is a fascinating insight none the less. The tough living and working conditions invariably led to accidents and fatalities, and as we can see above it was not uncommon for fights or brawls to break out when workers were paid their often meagre wages (Hayes and Rutter 2009).

The end of the ironstone industry in the 1920s brought further change to Rosedale as bit by bit the railways were removed, the structures of the kilns were left to decline, and the mines themselves closed down and sealed. It is pertinent to remember those real individuals, the men, women, and children (and animals) who lived and worked here, often did so in adverse conditions. The newspaper clippings can only ever report on a fraction of their lives and experiences.

Further Resources

For those who are interested in researching the lifestyle of the ironstone industry workers further, or are interested in pursuing their own research during the current lock down period, I recommend the British Library-ran Newspaper Archive resource.

For further reading on the ironstone industry within North Yorkshire, I recommend Hayes and Rutter much-reissued ‘Rosedale Mines and Railway’ 2009 publication. A newly updated edition of this book is due to be published this year.

For historic photographs, have a look at a previous blog entry to see two ‘colourised’ historic photographs from Sheriff’s Pit mine entry and the Ingleby Incline railway.

What’s Ironstone?

Tom Kearsley – Mineralogist

Iron is arguably the most important metallic element in the history of human technology. In the most comprehensive modern reference volume on properties, processing and use of metals – the Metals Handbook edited by Davis, 1998 – there are more pages devoted to ‘ferrous’ metals (‘irons’, steels and high performance alloys) than to all of the other metals combined.

Together with Magnesium (Mg) and Aluminium (Al), Iron (Fe) is an abundant element throughout the Solar System (Lodders, 2010), including the Earth. It was inherited from dust created by ancient giant stars, then brought together over four and a half billion years ago during the formation of the planet from the collision of asteroids and meteorites in the early Solar System. Much of the Earth’s Fe, along with Nickel (Ni) and Sulfur (S), is now in the core where it is responsible for the magnetic field of the planet. ‘Iron’ is also occasionally found on Earth’s surface as a ‘native’ metal, this may come from meteorite falls (which will not be pure Iron element, but will also contain a little Ni), and even a little can be found in some volcanic lavas. This raw material has been used by people for at least 5000 years, but it is so rare that ‘iron’ was not the most widely used metal until much later. In nature, Mg and Al readily form common minerals with Silicon (Si) and Oxygen (O), but they are not found as metals without human intervention, and they have only become widely manufactured and used in the last century.

Although now a little dated, ‘Metals in the Service of Man’ by A. Street and W. Alexander (10^th edition, 1994) provides a concise and readable introduction to the sources of metals, their processing, properties and uses. An excellent and detailed explanation of how metals (including ‘irons’) came to be produced, from the earliest methods up to modern large-scale industries, can also be found in ‘A History of Metallurgy’ by R. F. Tylecote (1992). The first widespread use began with discovery that Copper (Cu), and later Tin (Sn) could be extracted relatively easily from their ore minerals, giving rise to the ‘Bronze Age’, beginning perhaps 9,000 years ago. It is likely that the discovery of ‘iron’ smelting was accidental, perhaps around 4,700 years ago, and was possibly linked to the use of Iron-rich material in production of copper. By 3,000 years ago, ‘iron’ was important in human societies, being used widely in making weapons.

To produce ferrous metal in quantity, it’s necessary to find a good supply of a suitable starting material – the ore. Fuel is required to break the ore down into elemental Iron, typically by raising it to a very high temperature, away from air. It’s also important to be able to remove a range of impurities from the molten metal. Improvements in smelting technique have long been driven by pressures of the cost of mining and transporting ore and fuel, but also reflect the availability of different types of ore. Since the Second World War a very unusual type of ore, Banded Iron Formation (BIF) has been mined in enormous quantities in Australia, Brazil, the USA and Russia (among other countries). BIF is a very peculiar sedimentary rock, deposited in ancient seas, more than two billion years ago when the atmosphere and oceans had very different behaviour to the modern world. Because it is available in large quantities (many millions of tonnes per annum) and can be processed quite easily to concentrate the content of Iron, it is now most economic to transport this ore worldwide, rather than smelting at source in areas lacking fuel. Before the use of BIF, most production usually relied upon local supplies of ore, as well as coal, coke or charcoal, and additives to help separate metal and slag. In Britain, we have no BIF, and there’s little in Europe as a whole. The history of ferrous metal production in Britain therefore reflects making do with what was available, and many different types of Iron-rich rocks (ironstones) were used as ore.

The most common natural Iron-rich materials found on the modern Earth’s surface are oxide minerals, carbonates, sulfides and fine aluminosilicates. The oxides may be loose mineral grains from weathering of igneous rocks such as basalt lavas, or may form by reaction of volcanic glass and Iron-bearing silicate minerals (such as olivine or pyroxene) with Oxygen and water, especially during tropical weathering. Two minerals are often formed : Goethite (yellow-brown oxyhydroxide, FeO.OH, about 60% Iron by weight) and Hematite (red-purple-grey oxide Fe₂O₃, nearly 70% Iron by weight), both contain Iron in an oxidised form, Fe³⁺, which is not very soluble in water. As anyone who has owned an old car will know, metallic ‘iron’ and steel are also able (and all too willing) to form similar oxidised rust! The insoluble oxyhydroxides and oxides are very widespread as tiny grains in soils, giving brown or red colouration. Accumulation in dense soil layers can produce material suitable for use as ore, but these minerals were also occasionally deposited from warm water flowing through cracks in rock, and may form patches and veins of very high grade ores, such as the red Hematite ‘kidney ore’ of Egremont in Cumbria. BIF contain mainly Hematite, in layers with silica.

However, if the tiny grains are washed away by streams and rivers until they reach still water, they can sink and become gently buried within muddy sediment in a lake, delta-front or quiet-water sea. Here they are effectively cut off from air, and as bacterial decay of organic matter in the mud proceeds, they may again lose Oxygen, releasing soluble Fe²⁺ ions. In freshwater, the ‘reduced’ soluble Iron may react with carbonate created by bacterial oxidation of organic matter (such as rotting leaves), and can be fixed as an insoluble carbonate mineral called Siderite (FeCO₃). This often forms spherical concretions that may become flattened as the muddy layers are gradually squashed by continuing build-up of sediment above. The hardened (lithified) concretions or nodules are grey-green when broken, although may turn brown on weathering. Often found in mudstones between coal seams of Carboniferous age across Britain, these Siderite nodules (called ‘doggers’ by miners) may contain nearly 50% Iron by weight, and were an important source of ore during the Industrial Revolution of the seventeenth and eighteenth centuries.

Iron-rich mud deposited in seawater may behave differently. The oxides and oxyhydroxides again release soluble Iron as Fe²⁺ ions, but bacterial activity near the surface of the accumulating sediment removes Oxygen from the sulfate ions in the seawater, creating sulfide ions. This is how disturbed marine muds often come to smell of ‘rotten eggs’, the characteristic signature of hydrogen sulfide (H₂S). Soluble Fe²⁺ reacts very quickly with sulfide ions, forming a black iron sulfide, and eventually golden Iron Pyrites (FeS₂), with about 45% Iron by weight. This can be used as an Iron ore, but releases acidic sulfur dioxide fumes during processing, and requires both careful handling and large amounts of fuel. However, if deposition of mud is quite rapid, the production of sulfide can stop well before all of the soluble Fe has reacted, and more of the carbonate Siderite will then form, often becoming the main Iron-bearing mineral in shallow marine ironstones.

Iron may also be found in pale green hydrated aluminosilicate minerals (containing Al, Si and water), these are members of the Clay Mineral and Chlorite groups, called Berthierine and Chamosite, typically containing about 25% Iron by weight. How these minerals form is still not well understood, despite many studies of ancient and modern ironstones (Kearsley 1989; Young, 1989; Mücke and Farshad, 2005; Clement et al., 2019). There are probably several different origins. Some may be formed by soluble Fe reacting with the white clay mineral Kaolinite within the mud, or from insoluble Fe oxides reacting with Al and Si hydroxides. Some may form by tiny crystals growing within a slimy gelatinous blob or layer, some may grow as crystals directly from water in the mud. Strangely, these minerals also seem to favour growing in layers around a central core, making a concentric tiny egg, an ‘oolith’ or ‘ooid’. When ooids/ooliths are common within an iron-rich rock, it is described as an oolitic ironstone. It is not uncommon to find ironstones that contain aluminosilicates, Siderite, Hematite and Pyrite all together, including within ooliths/ooids – even with evidence that these minerals have replaced each other during or after deposition of the layer.

Oolitic ironstones are complicated rocks (see figure above). As their content of Iron can vary a great deal, they may or may not prove to be an economic source of Iron, which may also depend upon the other materials that they contain. High contents of Calcium (Ca) may help smelting, but high Phosphorus (P) can contaminate the metal that is produced. The oolitic ironstones mined in Rosedale and around all of the North York Moors typically contain mixtures of Siderite and Berthierine, as well as Kaolinite and the Calcium carbonate mineral Calcite.

The oxide Magnetite (Fe₃O₄) may also be found in some oolitic ironstones, it contains over 70% Iron by weight. As the name suggests, this mineral is strongly magnetic, unlike almost all of the other Iron ore minerals. It is quite common in Mg- and Fe-rich igneous rocks (formed from molten material), and can occur in massive deposits with a very high percentage of Iron. For example, magnetite has long been mined in Sweden, and was much sought after by both Allied and Axis industries during the Second World War. Magnetite is well known to occur in rocks that have been subjected to burial heating (low grade metamorphism), probably growing as coarser crystals from iron carried through porous rock by hot water.

However, it has also been found (and almost completely mined out) in sedimentary ironstone deposits in Rosedale, it was so rich in Iron. Here its origin is still a mystery, and there have been differing interpretations of when and how it formed. There are several 19^th century accounts of the discovery of magnetic ores in Rosedale (Bewick 1861; Wood, 1969; Marley 1871), as well as descriptions of these rocks in the Geological Survey Reports of Hallimond (1925) and Whitehead et al. (1952). From other evidence in the North York Moors, it doesn’t seem likely that these rocks were heated sufficiently to encourage metamorphic magnetite replacement of other minerals, and these are definitely not rocks formed from hot melt. Perhaps the peculiar setting where these sedimentary ironstones accumulated was an important factor in creating Magnetite? The earlier accounts suggested that the richest ore was found within elongate troughs, eroded into the underlying layers. Young (1994) suggested that there were indeed shallow basins where ooliths were deposited, but that the basins had been formed by fault motion at about the same time. Is it possible that stagnant water saturating the sediment within these hollows allowed Magnetite to form, replacing other more-oxidised Iron-rich minerals?

Ironstones deposited during the early part of the Jurassic Period have been extensively mined throughout England and Western Scotland, as described in Whitehead et al. (1952). There is a wider discussion of other ironstones from a broader range of ages, across England and Wales, in Hallimond (1925).

References

Bewick, Joseph 1861. Geological Treatise on the District of Cleveland, in North Yorkshire, Its Ferruginous Deposits, Lias, and Oolites; With Some Observations on Ironstone Mining. London: John Weale

Clement, A. M., Tackett, L. S., Ritterbush, K. A. and Ibarra, Y. 2019 Formation and stratigraphic facies distribution of early Jurassic iron oolite deposits from west central Nevada, USA. Sedimentary Geology 395 C Web. doi:10.1016/j.sedgeo.2019.105537.

Davis, J. R. (Ed.) 1998 Metals Handbook 2^nd Edition. ASM International, Materials Park, OH 44073-0002, USA. i-xiv, 1521 pp. ISBN 0-87170-654-7.

Hallimond, A. F. 1925 Iron Ores: Bedded Ores of England and Wales. Petrography and Chemistry. Special Reports on the Mineral Resources of Great Britain. Volume XXIX. HM Stationery Office, London. p 75, plate IV fig. 14.

Hawley, D. 2019 Rosedale – the magnetic ironstone conundrum. Field Excursion Notes. The genesis of geology in York and beyond. Yorkshire Philosophical Society and Geological Society of London History of Geology Group. 25th Anniversary Meeting Thursday 24th October 2019. Downloaded on 3^rd December 2020 from: https://www.ypsyork.org/wp-content/uploads/2020/02/HOGG-YPS-YORK-Rosedale-Magnetic-Ironstone-Conundrum-Oct-2019-ONLINE.pdf

Kearsley, A.T. 1989 Iron-rich ooids, their mineralogy and microfabric; clues to their origin. In Young, T.P. and Taylor, W.E.G. (Eds) Phanerozoic Ironstones. Geological Society of London Special Publication 46:141-164.

Lodders, K. 2010 Solar system abundances of the elements. In: Principles and Perspectives in Cosmochemistry. Lecture Notes of the Kodai School on ‘Synthesis of Elements in Stars’ held at Kodaikanal Observatory, India, April 29 – May 13, 2008 (Goswami, A. and Eswar Reddy, B. eds.) Astrophysics and Space Science Proceedings, Springer-Verlag Berlin Heidelberg. p. 379-417 ISBN 978-3-642- 10351-3.

Marley, J. 1871 On the Magnetic Ironstone of Rosedale Abbey, Cleveland. Transactions of the North of England Institute of Mining and Mechanical Engineers. 19, 193-199.

Mücke, A. and Farshad, F. 2005 Whole-rock and mineralogical composition of Phanerozoic ooidal ironstones: Comparison and differentiation of types and subtypes. Ore Geology Reviews 26:227–262.

Powell, J. H. 2010 Jurassic sedimentation in the Cleveland Basin: A review. Proceedings of the Yorkshire Geological Society 58:21-72.

Street, A. and Alexander, W. 1994 Metals in the Service of Man. 10^th Edition. Penguin Books Ltd, London, UK. ISBN 10: 0140148892

Tylecote, R. F. 1992 A History of Metallurgy 2^nd Edition. The Institute of Materials. 1 Carleton House Terrace, London. 255 pp. ISBN 0-901462-88-8.

Whitehead, T. H., Anderson, W., Wilson V., Wray, D. A. and Dunham, K. C. 1952 The Liassic Ironstones. Memoirs of the Geological Survey of Great Britain. Department of Scientific and Industrial Research, Her Majesty’s Stationery Office, London. pp 47-50.

Wood, N. 1869. On the Deposit of Magnetic Ironstone in Rosedale. Spons’ Dictionary of Engineering, Part VIII (Borings and Blasting), pp 501 – 512.

Young, T.P., 1989. Phanerozoic ironstones: an introduction and review. In: Young, T.P. and Taylor, W.E.G. (Eds.), Phanerozoic Ironstones. Geological Society of London Special Publication 46: ix-xxv.

Young, T. P. 1994 The Blea Wyke Sandstone Formation (Jurassic, Toarcian) of Rosedale, North Yorkshire, UK. Proceedings of the Yorkshire Geological Society 50:129-142.

The Yew – An Original Christmas Tree

Sam Newton – Woodland Creation Assistant

Yew links to Christmas and Christianity and back beyond into the depths of time. Like other evergreens, branches of yew were brought into people’s houses at Christmas as decoration and also as bitter reminder of the Christian Passion.

Yew trees (Taxus baccata) are now strongly associated with churchyards. They are a connection to the old Norse and Celt beliefs that yew trees protected against bewitchment and death. Pagans celebrated the yew at the mid winter festival of Saturnalia, which later melted into Christmas. Many old churchyard yews may have been planted by church-builders, brought out of the woods and into a civilised setting. Or later on top of graves to ward off evil around the dead and provide branches to be carried on Palm Sunday and at funerals. It became a tradition without a remembrance of its origins.

There are also a number of churchyard yews predating their churches, and even Christianity. Some trees alive today in Britain are truly ancient. The Fortingall Yew in Scotland is possibly between 2,000 and 3,000 years old – a myth tells of Pontius Pilate as the son of a Roman envoy, being born beneath and playing as a child within its branches. While the Ankerwycke Yew witnessed the signing of the Magna Carta in 1215, as an already 1,000-year-old tree overlooking Runnymede meadows in Surrey.

The first few lines of ‘Lines on the Ancient Yew in Darley Church Yard’ (in Derbyshire)
By Samuel Barker

Thou art an interesting tree,
The fact’s beyond dispute,
Thy monster trunk and giant bows
And intersecting roots,
Rearing in solemn grandeur,
Thy patriarchal head,
Reigning in midnight dimness,
O’er the regions of the dead.

The story of the yew tree is one of life, death, and resurrection. It was said by the noted forester and dendrologist Alan Mitchell, that “there is no theoretical end to this tree, no need for it to die”.

Yews reach such old age through an amazing ability to renew themselves and return from apparent decay. New shoots from the base can coalesce with the main trunk, while lowered branches can put down roots, and fallen trees remain alive as long as the smallest amount of root remains attached. Ancient trees can be split into several parts, and no longer look like one tree, but can go on surviving for many hundreds of years more.

Death lingers in these long-lived trees, with all parts of the plant containing highly poisonous taxine alkaloids. Yet at the same time these same highly poisonous chemicals provide modern day science with anti-cancer compounds. The yew tree can regenerate us, as well as itself.

Yorkshire has a strong but somewhat forgotten link to yew trees. The ancient Celtic name for the City of York is Eborakon, which can be translated to ‘the place where the yew trees grow’, or came from the name Eburos, meaning ‘yew man’. In the North York Moors, yew trees are common in churchyards, and can occasionally be encountered in the surrounding areas.

For more information about this natural and cultural marvel have a look at the Ancient Yew Group’s website

Colouring in

David Mennear – Land of Iron Administration Assistant

Have a look at these two digitally ‘coloured in’ historic photographs of our local mining communities in the North York Moors, from 100 years ago.

Our first photograph (above) shows ironstone miners at Sheriff’s Pitt, Rosedale, getting ready for a day of hard labour in 1900. If you look closely you can notice the clothing they wore and the wide shovels they used for helping to move the heavy ironstone and scoop it into the tubs. From the tubs it was taken out of the mine and along to the nearby calcining kilns to remove the impurities to make it lighter to transport via rail on to blast furnaces in the wider region.

The second photograph (above) was taken by J. Brotton on the 24 July 1903 – it’s of an almighty crash at the bottom of the Ingleby Incline railway. The incline is a 0.8 mile long stretch of rail to the moor top, which reaches a stonking 1 in 5 gradient at its steepest points. It was here that wagons were carefully drawn up and down the incline by a rope pulley system to allow the transport of ironstone from the Rosedale mines on to Teesside for processing into pig iron, before being transported and used across the country and the world.

Does the colourisation help make the people look more relatable? Does it make the scenes seem more immediate? Does it bring the communities of the 1900s to life?

Photos colourised by: Photo Restoration Services

Down in Yon Forest

Rachel Pickering – Woodland Team Leader

Deep in Cropton Forest is a very special place called High Leaf Howe. Its actually just a grassy clearing within the forest with a large mound, the ‘howe’, in one corner and a ruined house in another. Our archaeologists are probably more interested in the howe but for me it’s the ruin that is magical. I recall my grandma Ethel talking very fondly of her childhood at ‘Leaf Howe’ which was a small holding of about 20 acres on the edge of Wheeldale Moor where they grazed 20 sheep. They also had 3 cows and my grandma had hens which she sold the eggs from to help her parents pay the rent to Keldy Estate*. Her dad made besoms (brooms used in the steel works to clean the slag off the rolled steel when it was red hot) from the heather and her mother cleaned the school at Stape to make ends meet.

*The Forestry Commission acquired the freehold of the Keldy Estate in 1948 to incorporate into their Rosedale Forest holding, now named Cropton Forest.

Recently I was looking into the census data for Stape and made a remarkable discovery. Not only had my grandma been born at High Leaf Howe but also her father Bertie in 1895 and his father George in 1851. Four generations of my direct descendants lived there.  During the first lockdown I was looking through some old family photos and imagine my delight when I came across a small black and white photo which had the words ‘Leaf Howe’ penned on the back! Even better I could recognise that the girl outside the house was grandma and the shy head poking out of the door was her mother Ada.

I have taken my father and my two children to see the old homestead, and although my son was more interested in climbing a nearby tree at the time I’d like to think my two will see the significance of this special place in the future.