‘Signor tuberculato’, PH Gosse and Charles Kingsley

Cockle drifts at Balcary bay, April 2015

Cockle drifts at Balcary Bay, April 2015

Cockle shells are piled like snow-drifts amongst the trees at the top of the bay; they form banks and ridges along the shore. Balcary Bay, its entrance partly plugged by Heston Island, looks to be a tranquil and sheltered haven, but it would seem that a mass ‘startle’ by predatory starfish or – far more plausibly – pounding waves, have forced the cockles out of their shallow burrows in the muddy sand and sent them rolling and tumbling, to be hurled onto the upper shore. The stench of dying shellfish must have been impressive.

Cerastodesma edule

Cerastodesma edule, Balcary Bay April 2015

These cockles are Cerastodesma (formerly Cardium) edule, the common cockle, which are gathered commercially and most (in)famously at Morecambe Bay. A large commercial cockle fishery also existed until about 10 years ago in Allonby Bay, on the opposite side of the Firth from Balcary, and we find their empty shells there too, along the tideline. Rarely, there might be a shell of the spiny cockle, its larger relative, which has obvious protrusions on its shell; hence its earlier name of Cardium (now Acanthocardia) tuberculatum.

Amongst the predators of cockles and mussels are starfish, which prise apart the bivalve’s two shells. Mussels, being fixed to the substratum, are unable to escape but a cockle, at the first scent of ‘starfish’ in the water, can attempt to leap away – as Philip Henry Gosse, the Victorian naturalist, writer and lecturer, who devised the marine aquarium and initiated ‘shore-classes’, so delightfully describes.

Starfish invading the mussel beds at Ellison's Scar, Allonby Bay (photo: Dr Jane Lancaster)

Starfish invading the mussel beds at Ellison’s Scar, Allonby Bay (photo: Dr Jane Lancaster)

For several years, Gosse was a close friend of the Rev Charles Kingsley, who shared his enthusiasm for marine life. Kingsley wrote to Gosse, “I am half a sailor, having been bred on the sea-shore, with our own trawl and dredge, with which as a boy I used to work day after day in North Devon for poor dear old opium-eating Dr. Turton, when he lived at Bideford.” Thus it was that Kingsley sent parcels of marine animals to Gosse in London, and the two of them kept up a rich correspondence (the letters are held at the Brotherton Library at Leeds University [1]).

Charles Kingsley to PH Gosse: Livermead, [Devon], January 29th 1854
I am going dredging for you on Thursday, and DV I shall send the jar off on Friday. These short days prevent my getting the haul sorted after I come home.
I must add my thanks to you for giving not me only, but Mrs. Kingsley and my children, this occupation – we are as busy as bees about the animals all day, and the little ones full of desire to find something worth sending you.

'Dredging off Weymouth', from PH Gosse's The Aquarium

‘Dredging off Whitenose’, from PH Gosse’s The Aquarium

PH Gosse to Charles Kingsley: 58 Huntingdon Street, [London], Feb. 2nd 1854:
Dear Sir, If you have the wind as we have, this moderate off-shore breeze will give you a good day’s dredging today. I hope by the time I finish this note you will be safe home with a rich harvest of spoils …
Please to express my thanks to your dear little boy for the specimen he has found for me, and for the zeal with which all the family have engaged in the search. I feel sure they will never have cause to regret having had an early bias towards out of door zoology. May I venture also to offer my respectful thanks to your lady for her kind co-operation also. It is a grand gala day for Mrs. Gosse as well as myself, when we get an opportunity of examining a consignment from the sea; such an array of pans and bowls, of vases and tubs comes out, and the whole house is on the tiptoe of expectation!

PH Gosse to Charles Kingsley: 58 Huntingdon Street, May 30th 1854
I have now 6 aquaria of various sizes and forms, most of which are in beautiful order, and well stocked, but in some there is yet room for many more inhabitants. .. My most charming tank is now 13 weeks old, and contains nearly a hundred species of animals, and perhaps twice that number of individuals, all in the highest health and beauty – many of them the treasures you kindly sent me ..

Charles Kingsley to P H Gosse
My dear Sir, I send off your hamper by this night’s Mail. I will put a list in it, with some notes and queries. …Note 6a. Cardium Tuberculatum and Aculeatum; their respiration should be (worked) out …

PH Gosse: from his book The Aquarium (1854)
“Among a number of animals of great interest kindly sent to me from the vicinity of Torquay, by the Rev. C. Kingsley, were a posse of cockles .. those giants, Cardium aculeatum and C. tuberculatum, the real aristocracy of the cockle kind. .. Many persons are aware that the Common Cockle can perform gymnastic feats of no mean celebrity, but the evolutions of Signor Tuberculato are worth seeing.
Some of the troupe I had put into a pan of sea-water …(and) by and by, as we (PHG, his wife Emily and their son Edmund [Willy]) were quietly reading, our attention was attracted to the table where the dish was placed, by a rattling uproar, as if flint stones were rolling one over the other about the dish.

Drawn by PH Gosse

from P H Gosse’s ‘Natural History: Mollusca” p271

We could look at nothing but the magnificent foot, and the curious manner in which it was used… (It) is suddenly thrust out sideways .. then, its point being curved backwards, the animal pushes strongly against any opposing object, by the resistance of which the whole animal, shell and all, makes a considerable step forwards. Cooped up with its fellows in a deep dish, all these herculean efforts availed only to knock the massive shells against the sides, or to roll them irregularly over each other.

A considerable number of those sent up we “killed to save their lives”; making gastronomical use of them …”


[1] My thanks to the then Librarian, Christopher Sheppard, for providing me with photocopies of their correspondence, when I was researching Gosse’s papers, diaries and letters for my novel Seaside Pleasures (2003). The story is told in 4 voices, 3 of them in the present day, and the fourth – that of Anne Church – is a student on one of Gosse’s shore-classes: see my Eliot & Entropy blog for details, ordering, reviews, photos and more.

SP cover

 

 

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The design of the Solway: an aerial perspective, part 2

September 2nd, 0845h: Andrew Lysser, pilot, aerial photographer, instructor, and owner of Cumbria Gyroplanes, and I lifted off from the runway at Carlisle airport in a silver-coloured gyroplane. This time I wasn’t nervous, and there was no wall of rain advancing towards the Firth. It was a perfect morning for our second attempt to fly along the English coast of the Upper Solway Firth. Quiet, bright weather. Scattered clouds, and a slanting light painting water and sand in shades of satin-silver and grey. And moreover – the whole point of this flight – an Extreme Low Water Spring (ELWS) tide.

The retreating sea would reveal the rocky scaurs, the sandbanks and shoals, and the morning light would pick out the patterns of sand and rocks on the shores, would show the run-offs, the saltmarsh creeks, the channels of the rivers and of the Firth itself: a snapshot of a moment in time, of the design that influences the function of the Solway.

The Solway Firth from Rockcliffe to Maryport (satellite image from Google Earth)

The Solway Firth from Rockcliffe to Maryport (satellite image from Google Earth)

On our first attempt we had reached Bowness-on-Solway and the stubby remains of the Bowness-Annan viaduct before the weather forced us to turn back, so now our attention was focussed on ‘the island’ (actually, a bulging peninsula) with the masts of Anthorn, and beyond.

Eroded edge of the saltmarsh at Cardurnock, with Moricambe Bay beyond and the Lakeland fells; the masts of Anthorn to the right

Eroded edge of the saltmarsh at Cardurnock, with Moricambe Bay beyond and the Lakeland fells; the masts of Anthorn to the left

ELWS also means extreme high water at the other end of the tidal cycle, and the saltmarshes were still holding large pools of water, the creeks were full.

The creeks and pools on Newton Marsh; Moricambe Bay and the channel of the Wampool meandering through the sandbanks between Anthorn and Newton Arlosh

The creeks and pools on Newton Marsh; Moricambe Bay and the channel of the Wampool meandering through the sandbanks between Anthorn and Newton Arlosh

We circled over the mud and sand of shallow Moricambe Bay; a piece of the fuselage of a WW2 Hudson bomber – hence the Bay’s other, grim, name of Hudson Bay  – protruded sufficiently from its grave to provide a perch for a gull, and cormorants posed nearby on the posts of long-gone stakenets. Then we turned South again, over Grune Point, part of the AONB, where mudflats – teeming with burrowing crustacea and bivalves – attract wading birds.

Grune Point with the town of Silloth in the distance, Skinburness Marsh to the left and on the right the Galloway coast

Grune Point with the town of Silloth in the distance, Skinburness Marsh to the left and on the right the Galloway coast

Skinburness & Silloth: groynes attempt to reduce erosion of the coast

Skinburness & Silloth: groynes attempt to reduce erosion and transport of the sand and shingle

Rocky scars extend far into the channel; the outermost dark patch is outer Ellison’s scar

Rocky scars extend far into the channel; the outermost dark patch is Outer Ellison’s scar.

The 'Tommy-legs' light

The ‘Tommy-legs’ light

South of Silloth, rocky scars had been uncovered and the ‘Tommy-Legs’ lighthouse is stranded like a triffid on the sands.

Already a striking pattern is emerging, of broad, long-wavelength sand-ripples – sand-waves or megaripples; and along the exposed edge of the sloping shore, strips and patches of rock and stone. More surprisingly, the rocks are arranged in dark ribbons at a steep angle to the shore-line, and even more surprising, sometimes normal to the direction of the megaripples. But even at about 500 feet, we’re too high to discern the orientation of the small sand-ripples that the megaripples will carry on their backs, and which will affect the extent to which sediment is lifted and carried by the waves.

Lines of rocks at right-angles to the sand-waves

Lines of rocks at right-angles to the sand-waves

I know that on the ground the scaurs are made up of small- to medium-sized pebbles and rocks with no distinct orientation: yet, seen from above, it’s clear that the direction of tidal flow has a strong influence on their design. This in turn must surely have an effect on the biology of the shore, the places where animals and algae are deposited or can actively find shelter.

Off Mawbray Banks we circle to have a closer look at the lines, rectangles and triangles of stones on the lower shore. From the air, it seems even more likely that they are the remnants of fish-traps  (see this blog-post for the aerial photos). Were there also wooden stakes and nets, or are the stones merely the walls of retaining pools? Andrew suggests I take a spade and dig near the stones to see if fragments of wooden stumps remain.

It has been worth the wait for this exceptional low tide. From above Dubmill Point the view in all directions is breath-taking.

Looking N to Criffel; Dubmill Scar, the posts of the oyster lines; outer Ellison's scar and sandbanks in the distance (photo: Andrew Lysser)

Looking N to Criffel; Dubmill Scaur, the posts of the oyster lines; Outer Ellison’s Scar (far middle) and sandbanks (far left) in the distance (photo: (c) Andrew Lysser)

Looking North from above Dubmill: the concrete sea-defences on the right. The rocky scars of Archie and Dubmill are where the Sabellaria reef is concentrated

Looking North from above Dubmill: the concrete sea-defences on the right with Seafield Farm just visible. The rocky scaurs, Archie and Dubmill, are where the Sabellaria reef is concentrated (photo (C) Andrew Lysser)

The reefs and sculpted mounds of the honeycomb worm, Sabellaria, are special to Allonby Bay, and one of the reasons why it has been proposed as a Marine Conservation Zone. The reefs retain the outgoing tide and thus change the distribution of animals and algae on the shore – so it’s interesting to see that the Sabellaria areas appear in some areas as almost-square ‘cells’ of trapped water. This isn’t apparent when you are at reef-level on the shore.

The Sabellaria reefs trap the tide. (photo: Ann Lingard)

The Sabellaria reefs trap the tide. (photo: Ann Lingard)

On evening back in April I walked along the Allonby shore with Ronnie Porter so that he could tell me about ‘the naming of stones’ – the old names for scaurs and boulders, that identify where one might put out herring nets or gather shrimps or prawns. It was difficult to understand the overall topography from shore-level, so to ‘see the bigger picture’ was another purpose of this flight. This was much harder than expected, and it proved impossible to identify single marker stones other than Maston up on the mid-shore; but it was astonishing to see how far out the scaurs stretched, to see the often hard-to-reach Hill and Far Hill exposed. What a wealth of marine animals and algae would be out there!

Allonby Bay (village in top left corner). Dubmill, Archie,metalstones and Matta scars (photo (C) Andrew Lysser)

Allonby Bay (village in top left corner). Dubmill, Archie, Metalstones, Matta & Popple scaurs (photo (C) Andrew Lysser)

Sandbanks in the middle of the Firth (photo: Ann Lingard)

Sandbanks in the middle of the Firth (photo: Ann Lingard)

Quite often, on a rough and windy day when the tide is flowing back up the Firth, a shifting white line of breakers is visible way out in the channel to the West. Today, it was obvious why: large sandbanks were exposed in the middle of the Firth, upon which waves would shoal.

This was also a graphic explanation of why ships heading for the Port of Silloth are required to take on a pilot at Workington.

South end of Allonby village (photo: Ann Lingard)

South end of Allonby village (photo: Ann Lingard)

Looking South to Maryport and the wind-turbines at Siddick; the prow of St Bees' head beyond (photo: Ann Lingard)

Looking South to Maryport and the wind-turbines at Siddick; the prow of St Bees’ head beyond (photo: Ann Lingard)

Crosscannonby at the south end of Allonby Bay was to be our turning point, where we had a seagull’s eye view of the saltpans and Roman Milefortlet 21 (for more on the Solway saltpans see ‘Angels, salt and shroud-pins‘).

Crosscannonby saltpans and Milefortlet 21 (photo: (C) Andrew Lysser)

Crosscannonby saltpans and Milefortlet 21 (photo: (C) Andrew Lysser)

Above Silloth once again, we could see far into the distance, where there would once have been a large freshwater lake, formed from melting glaciers. Below us, about 10000 years ago, a forest, subsequently replaced by sphagnum bogs, would have spread across the low-lying land between ‘England’ and ‘Scotland’. Now we could see how the encroaching sea and the outflowing rivers had eroded and sculpted the former plain; they are doing it still. Beyond Silloth the broad shallow estuary of Moricambe Bay glittered; beyond Anthorn and Bowness, a narrow silvery line shone light on the contest between the tides and the rivers Esk and Eden. Closer, it was obvious, too, why pilots must enter Silloth’s New Dock at an angle.

The Port of Silloth and beyond (photo: Ann Lingard)

The Port of Silloth and beyond (photo: Ann Lingard)

And across the Firth the tide had drained away into the Irish Sea leaving behind, for a few hours, the story – in ripples and sand-waves and shoals – of last night’s waves and wind and currents.

Looking across to Scotland (photo (C) Andrew Lysser)

Looking across to Scotland (photo (C) Andrew Lysser)

***

Footnote: Since I wrote this, photographer James Smith has made a beautiful video, using his UAV (‘drone’) for aerial views of both sides of the Firth, called the Light of the Solway

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Waths: fords and borders

On a very low Spring tide in August, my guide Mark Messenger and I crossed and re-crossed the Solway on foot, from England to Scotland and back. We waded across the Firth through the outgoing tide and the flow of the Rivers Eden and Esk, a little to the East of the ancient Wath which runs from Bowness to Seafield in Scotland.

The ancient Bowness or Annan Wath is one of the shortest foot-crossings of the Firth proper. It was used by William Wallace and Edward I during the Scottish Wars of Independence, and by cattle drovers, driving their beasts to English markets, until the new railway viaduct came into commission in 1869. More recently, Hugh Dias, co-author of the beautifully illustrated book ‘Exploring Solway History’, told me, “ We were warned about the tides but were sort of free range. It was my elder sister and two female cousins who one day crossed the Bowness wath to Scotland. They must have been in their mid teens when they did it and as far as I know their parents were clueless about what they were doing…” But as he notes in his book, “they lived to tell the tale”!

Probable routes of the fords crossing the Solway. (Jim Hawkins, 1998)

Probable routes of fords crossing the Solway (Jim Hawkins 1998 – from Annan website and Nixon & Dias’ book)

The waters of the Firth acted as an international frontier, across which the English and Scottish armies attempted to by-pass the land defences. Although it’s difficult these days to identify the various waths other than through historical accounts, partly because the topography of the shores and marshes have changed so dramatically, the three main waths were the Sulwath across the mouth of the River Esk, the Peatwath across the River Eden, and the Bowness wath across the Firth.

The meandering R Eden, with Rockcliffe marsh beyond. Peatwath was probably near the river mouth (photo: Ann Lingard)

The meandering R Eden, with Rockcliffe marsh beyond. Peatwath was probably near the middle of the upper (in the photo) loop (photo: Ann Lingard)

There was also the Dornock or Sandy Wath across a broad stretch of the Firth from Drumburgh to Dornock; Blawath a little further to the East; and shorter waths – Rockcliffe Wath and Stoney Wath – across the Eden, and Loanwath across the Sark.

The muddy ford

“The Solewath, Sulewad, or Sulwath, [is] a word which easily explains itself. Sol is a term, common to Anglo-Saxon and to the Norse languages, for mud. Anglo-Saxon woeth – Norse vad or vath… is a word for ford. Sulewad or Sulwath means therefore the muddy ford.” (Neilson 1896)

In November 1896, George Neilson read a long and well-researched paper on The Annals of the Solway Until A.D. 1307, at a Meeting of the Glasgow Archaeological Society. In this paper (reproduced on Steve Bulman’s website about Cumbria) he argues convincingly that the Firth’s name derives from its main wath:

“The evidence of the thirteenth century, therefore, sets forth a number of propositions which the course of subsequent history amply confirms. These are:
1. That Sulewad, Sulwath, or Solway, interpreted by the earliest allusions to it, did not denote an arm of the sea, did not indeed denote even a river, but was a distinctly limited locus, a point or place upon a river.
2. That it was a meeting-place for the administration of border law.
3. That it was a place where the English escort might meet a royal visitor passing into England.
4. That it was on the marches of the realms.
5. That it was on the river Esk.
6. That it was already recognized as a regular crossing place.
These facts lead to an induction as little open to question as themselves, namely, that the original Solway was a ford across the mouth of the Esk.”

Neilson’s researches into old documents and maps led him to conclude that during the 300 years up until the end of the 19th century the eastern boundary of the Firth had gradually extended nearly 3 miles to the West: Rockcliffe Marsh had grown, bulging out into the sea. “Many an acre now under the plough, or green with rich merse grass, then formed part of the sands of the Solway.”

The edge of Rockcliffe Marsh at low tide (photo: Ann Lingard)

The edge of Rockcliffe Marsh at low tide (photo: Ann Lingard)

And, pleasingly, he pays attention to the underlying geology: between the mouths of the Kirtle and the Sark on the Scottish side, there was “unmistakable hard ground … Of a firm and gravelly structure”, well-suited to forming the base of a ford. He suggests therefore that the start of the Sulwath was marked by the Lochmabenstane (a “weather beaten sentinel grown grey with centuries of duty as watchman of the ford”) near Gretna, and ended near Rockcliffe where a ferry crossed the Eden at Stoneywath.

Miscalculated crossings
There are many interesting, often horrifying stories, in Neilson’s paper about the to-ing and fro-ing of English and Scottish troops across the Firth in the 13th and 14th centuries. In February 1216 followers of Scottish King Alexander II, laden with spoils from pillaging Holme Cultram Abbey, were crossing the ford on the Eden when the incoming tidal bore overtook and drowned 1900 men.

In 1300, when English ships were provisioning the army, “Victuals, in course of being taken with two carts and seven horses to Lochmaben, were carried off by the Scots ‘in the passage at Sulwath.’ The incident is typical of the guerilla warfare pursued by the Scottish army.”

edward1-plaqueIn 1307 Edward I was again sending troops to wage war against the Scots; despite growing ever weaker from dysentery, he insisted on being carried across the Solway as an example to his troops. “Daybreak on 7th July, 1307, found him in camp on the shore north of Burgh by Sands. The road for Scotland lay in front across the fords – the Stonywath, hard by, over the Eden; and the Sulwath, two miles distant, over the Esk. As his attendants were in the act of raising him to give him food he collapsed in their hands, and the mighty spirit passed away.” (Neilson 1896).

A line in the sand.
Stand still in the middle of the Firth and the current swirls the sand from beneath your feet. Yet, there in the water, you are standing on a metaphorical line in the sand, part of a border which was contested for centuries. Now, although these waths are mostly forgotten, as cross-border routes they still have great political and social significance.

As Rory Stewart MP writes, of his own crossing at Bowness, “On one side [of the invisible line], the Scottish state possessed absolute power, but at the millimetre line of the border, its sovereignty ended. On this side of the line, the English were citizens in their own nation … Step one foot across the mid-point of the Solway, and they were aliens…” It is his hope that “the Solway will always remain, as it is now, the ambiguous, opaque, tantalising, meeting of nations; but never again a frontier to make us foreigners.”


Exploring Solway History, 2007. Philip Nixon & Hugh Dias. Breedon Books, ISBN 978-1-85983-586-9

A pdf of the Annan shore-walk, showing Jim Hawkins’ map of the probable fords.

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The design of the Solway: Hems, reestings, holes and shoals

The Upper Solway at low tide (from Google Earth). The channels of the Eden and the Esk are top right. Moricambe Bay lies between Skinburness & Cardurnock

The Upper Solway at low tide (from Google Earth). The channels of the Eden and the Esk are top right. Moricambe Bay lies between Skinburness & Cardurnock.

The turning tide takes time to fill the Solway. Today (August 12th) the first low tide at Maryport was at 0544h, height 1.5m; after turning, the flood tide was at its highest at Maryport at 1102h, height 7.5m. Heading North to Silloth, High Water was at 1114h, and 8.10m; then the flood had to sweep North-east, round Grune Point, some of it washing into Moricambe (‘Hudson’) Bay; and then carry on North-East again, along the main channel and over Cardurnock Flatts, past the stub of the long-gone viaduct, and round the corner to Bowness-on-Solway, tucking in against the English side then flooding East to the edge of Rockcliffe Marsh to meet the mouths of the Rivers Eden and Esk. At the mouth of the River Annan, on the Scottish side and just West of Bowness, high tide was at 1136h.
Sometimes the sea returns stealthily, its edges scummy with silt; sometimes it hurtles in as a roaring, though not very high, bore. Carrying its own burden of sand and mud, it meets the fresh waters from the rivers which, after rain has fallen on the hills, are murky brown with silt.

The paths of the rivers are never constant; they carve deeper channels, or change their routes, finding new ways between the sandy shoals. Where sea and river meet, sediment is deposited and is swirled and patterned and heaved into new shapes. Sand, rocks, mud, are eroded from one place and deposited elsewhere; longshore drift brings material up from the Irish Sea. Saltmarshes are divided and their margins resculpted.
And so, if you and your animals – whether horses or stolen cattle – want to cross the Solway on foot, like Edward I’s army or the Border Reivers, you need to choose your time and tide and ‘wath’ (foot-crossing) carefully.

A year or so ago Mark Messenger, haaf-netter and owner of the Highland Laddie pub at Glasson, had told me that he had taken Rory Stewart MP across a wath near Rockcliffe Marsh – and said he’d be happy to guide me too. A few weeks ago, I happened to break a cycle ride to have lunch at his pub, and we got talking about the changes that had recently occurred in the upper reaches of the Firth. Two big rocks, the Anchor Stone and the Drawing Stone, had recently reappeared at low tide after being covered for years, and Mark told me that it was now possible to cross just West of the remains of the Bowness-Annan viaduct: ‘You can wade across, there’s that much sand. I’ve never seen it like that in 18 years.’

Who could resist such a challenge?

Tthe end of the viaduct at Bowness on Solway

Remains of the Bowness-Annan viaduct, and the Firth at low water Spring tide

As it turned out, I’d already booked a gyroplane flight with Andrew Lysser, to catch a very low Spring tide, and a few days later we flew over that stretch of the Firth before we had to turn back due to bad weather. The water certainly looked shallow, there were large sandbanks, and I felt rather more confident about a crossing. Mark Messenger and I agreed to make the attempt on the first low tide two days later.

The English and Scottish sides near Bowness-on-Solway. From Google Earth

The English and Scottish shores near Bowness-on-Solway. From Google Earth

However, when I met Mark at the pub he told me that the situation West of the viaduct had already changed: a deep channel had opened on the far side and we would no longer be able to cross there but would try elsewhere.
We drove down the coast road in Mark’s van and at Bowness we pulled in behind cars parked on the roadside. Several men were wandering around, chatting, and pulling on waders and yellow waterproofs. As he parked, Mark nodded towards a man who was taking waders out of his car. ‘He’s the one who went for a swim last week,’ he grinned . The fisherman (we’ll call him Jim) got knocked off his feet and swept a short way downstream into a ‘hole’. ‘I couldn’t get out,’ Jim told me. ‘I was trapped in it. Then the tide turned and washed me out. I was only in for 15 minutes but it was cold.’ Meanwhile, two of the Scottish haafnetters had seen that where there had been two men fishing, there was now only one, and they had alerted the rescue; the lifeboat came from Silloth. ‘A bit embarrassing,’ Mark told me later. ‘He was upstream of us, we’d have got him out. But he was blue with cold.’ Nevertheless, here was Jim, back again, kitting up, pulling the strap of his bag over his head, readying himself for another few hours fishing in the Firth.

At Silloth, the tide would be on the turn and would soon be flooding back up the Firth. Here, just upstream of Bowness-on-Solway the tide was still – just – on the ebb. Here there is a long period of slack water between the ebb and flow. As Mark said, ‘We don’t get 24-hour tides here’.
Sandbanks and mudflats stretched out from both the English and Scottish shores and in places sandy shoals were beginning to show beneath the surface. It looked as though it should be an easy crossing.
To reach the water we would have to cross slippery mud and stones, and then a long stretch of sand. ‘It’s hard to believe it’s changed so much in just a few days,’ Mark said. ‘This was all rocks last week, like that over there.’ Now, mud and tangled grass had been pushed right up to the bank along the margin of the road. He pointed out curving lines on the shore. ‘You can see where the current comes in close, the tide keeps to the English side when it comes round the point.’

Crossing from Bowness (From Google Earth)

Crossing from Bowness (From Google Earth). At the time of writing, the R Esk also has a channel close to the northern shore

He’d already been chatting to Billy, another haafnetter who was getting kitted up, about the state of the channels and the shoals. Billy had been out fishing this stretch of the Firth the previous day, and he pointed out a white house we should aim for, and where standing waves indicated a shoal. ‘Why’d you want to do this?’ He was laughing at me as I was flapping the over-large top of the waders Mark had lent me. ‘Something you’ve always wanted to do, is it?’ I agreed but admitted I was slightly nervous, now that I’d seen how far we had to walk and wade (in both directions – there would be no waiting taxi on the Scottish side to bring us home via Gretna!) ‘You’ll be okay. It’ll be easier coming back. And Mark’ll look after you, won’t you, Mark?’

I knew he would: I’d previously been out haafnetting with Mark, standing chest-deep in the incoming tide. He’s a man of few words, but he constantly scans the surface of the water, and he will always explain what he’s looking for and what it means. If you want to cross the Solway, on one of the ancient ‘waths’ or anywhere else, you couldn’t do better than ask a haaf-netter.

My guide: Mark Messenger with haafnet

My guide: Mark Messenger with haafnet

Mark’s own haafnet was on the marsh the other side of Bowness, so he borrowed one that was lying on the bank. He said we’d ‘have a look and see what we can find’ – but he also told me later that carrying the net was useful in case ‘anything goes wrong’, because the frame can be used as an anchor or support. The weather was good for a crossing, very little wind, the air was warm despite the grey sky; the waves were small.

We waded into the shallow water; soon it was knee-deep and then above the knee. Walking wasn’t difficult. But then we reached the current, where the Eden – busily carrying water that had recently fallen on the Fells – was making its presence felt. The water wasn’t deep but walking against the current became slower and harder. Whenever I stopped, the ground beneath my feet was sucked away. Occasionally, a sudden stronger swirl caused me to lurch. I began to feel hot and sweaty from the effort, and anxious about having to make the return journey. But I was determined not to fail, to keep going and not show how weak my legs felt (what had happened to those running muscles I’d been building up?). Mark waded slowly, keeping an eye on me while pretending not to do so, occasionally asking if I was alright, suggesting I could hold the bar of the net if I needed to (I was determined not to). He also stopped frequently to look at the water. ‘If there’re salmon, they’ll be coming down like bullets,’ he said. ‘Look out for flashes of white.’ And, ‘We’re heading for where the water’s smoother, over there. Another 50 yards and we’ll be over the worst bit.’ And so we were, eventually, though there was still a fair way to wade through the shallower, calmer water, towards a sandbank splattered white by resting gulls and oystercatchers.

Approaching Scotland

Approaching Scotland: the green huts are armaments stores

Over to our right, the River Esk swirled round the point but instead of immediately joining the flow of the Eden it had, in the past few days, carved itself a new channel close to the Scottish shore. Mark wanted to see if salmon were trapped there, so we ambled about on the sand and in the shallows, looking at the view, admiring Bowness as seen from the Scottish shore, watching the other haaf-netters downstream on both the English and Scottish sides. Mark has a Scottish licence as well as an English one, but we had set foot on the Duke of Buccleuch’s territory where haafnetting wasn’t permitted.

Setting foot on Scotland

Setting foot on Scotland

Down towards Annan Water, six Scottish fishermen were standing close to each other. ‘They’re fishing a hem. If you think of two currents meeting, one flows on top of the other and then it drops down—, ’ he showed me with his hands. ‘And where it drops the water’s flowing faster and harder. The fish can get trapped. But it’s hard to fish.’ The men clearly weren’t having any luck, they were moving round the hem, and eventually moved away to look for better water. Two English netters further down near the viaduct had given up, and were wandering up through the water towards us, chatting, nets balanced on their shoulders.

Our crossing had taken just over 20 minutes and now, having examined Scotland and rested, it was time to head back to England. In the 40 minutes or so since we walked onto the sand at Bowness, the water-level had dropped even more, and new sand was exposed. We were also walking with, rather than against, the rivers’ flow so the going was easier. I wondered if we were now wading through freshwater rather than brackish but it was so turbid and brown with silt that I didn’t feel inclined to taste it.

Reestings

Reestings

Ahead of us were reestings – standing waves, occasionally, chaotically, tipped with white – an indication that the water ran fast and shallow over shoals. It made interesting wading, to feel the sudden change in speed and force, to stand and watch how the patterns and heights of the waves changed subtly.

The flood tide should be starting to reach Bowness, the haafnetters would soon be feeling the stem, that change in pressure when the opposing waters meet. We had returned to the English shore. I was elated and still finding it hard to believe that I had, finally, walked across the Firth and back.

But I was also strangely disappointed: the ground underfoot, the air around us, were so predictable in comparison.

Bowness-on-Solway seen from the far side of the Firth

Bowness-on-Solway seen from the far side of the Firth. The masts of Anthorn are in the distance.

We drove through Bowness to look at the state of the Firth next to the viaduct. Despite the great expanse of sand and the apparently shallow water, there was a new channel on the English side where Mark said he hoped to find good fishing. ‘If that breaks through at the Cardurnock end, the fishing will be dynamite!’ And on the Annan side, a patch of stationary white water hinted at a deep hole which would have prevented our reaching Scotland.

This had been a very different experience from when I went haafnetting: then I had had to wade out into the flood-tide, standing with the net as the water rose to chest-level. I’d learnt about breists and reestings and holes, seen and heard the bore, seen the way the water crept so unnervingly quietly into the channels on the mudflats. It had been about the power and the vagaries of behaviour of the sea.

Today, I’d seen and felt the power of the rivers that modify the inner Firth, on their own and during their interactions with the sea. I’d learnt that every time you go out you have to see and understand the subtle clues that tell you where it is safe to walk and stand, where shoals have formed or holes appeared, and how the hems and holes and breists affect the fish and their behaviour.

You have to understand the water: and that is the clue to starting to understand the Solway Firth itself.


Read about my own experience of haafnetting in The Fresh and the Salt. The Story of the Solway (Birlinn Books 2020); for more information about the book (available from all bookshops), reviews and more photos, see the related website.
There are other posts about bathymetry, the sea-bed, and currents, on this blog.

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The design of the Solway: an aerial perspective, part 1

The Upper Solway: edges and divisions

The Upper Solway: edges and divisions

To understand how something works, you need to understand not only its design, but its interconnections and interactions with its surroundings.
So it is with the Solway Firth.

My ongoing fascination with the Firth’s ‘design’ is why I have recently flown over it, and have walked across it at low tide. The new experiences and perspectives are adding to my glimpses of ‘understanding’ all four dimensions of this segment of sea and shores.

An aerial view
Last week I took a flight in a gyroplane to get an aerial perspective: but all did not go to plan (*).
The plan was to get to Carlisle Airport for 7.30am so as to fly South-West to the upper end of the Firth and then fly down the coast to reach Allonby Bay at low tide. Low water was due at about 0930h, and would be a good tide, as low as about 0.4 metres – perfect for over-flying and photographing the exposed rocky scars, the named boulders and the strange lines of stones along the shore. Andrew Lysser, who runs Cumbria Gyroplanes based at Carlisle, was completely unfazed by the fact that he’d have to get up at 5am to reach the airport and do pre-flight checks: as he said, “It’s good to have something make you get up in the morning.” Andrew not only takes people up on flights but is also a gyroplane instructor and experienced aerial photographer, and he very generously offered to take additional photographs for me.

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At the aircraft hangar I was fitted with flying suit, scarf and helmet; hung my camera’s lanyard round my neck; found my gloves; discarded my notebook. Andrew explained some of the mechanics of the ‘plane to me, gave me a few important tips about communication and emergency procedures; and then we went outside to look at the gyroplane. The open-sided flying-machine, with rotors that looked ridiculously flimsy, and a motor that sounded like a wasp, was rather shocking. Getting in required some flexibility.

Andrew checked with the control tower; told them our plans, was given clearance, and we motored across to the runway, then accelerated along it, waiting for the top rotor to reach 200 revs/min. As I watched our shadow to my right, I saw a gap open below the shadow of the wheels and the runway and I knew we had become airborne, smoothly. My mouth was so dry with nerves I could barely reply to Andrew’s questions, and I felt very exposed; there was nothing between me and ‘outside’, only the seatbelt holding me in.

The railway marshalling yard, Carlisle

The railway marshalling yard, Carlisle

He calmly pointed out the warehouses and alterations to the airport perimeter for the new Stobart expansion; a mansion belonging to someone well-known; the huge expanse of Carlisle’s railway marshalling yards. It became easy to enjoy the experience. We were seeing places which, screened at ground-level, I hadn’t even known existed. We spied.

Grey skies

Grey skies

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Rain

But, less than a half-hour into the flight, a grey curtain approached the coast from the South, obliterating the fells, the fields and woods, the Firth, the Scottish hills. The rain was driving North and East towards us. If we couldn’t find a ‘hole’ through it, or fly around it, we would have to turn round: too much rain damages the tips of the rotors – but in any case we would not be able to see anything, and without a lid over us, we would get wet.

The wall of rain looked solid and wide and low, and even though we flew North again to find an edge, there was no way round. Instead we flew back into the sunshine towards the Border, over Rockcliffe Marsh and village, Lanercost Priory and nearby Naworth Castle – and over an unusually secluded village near Longtown.

The saltmarshes and the channels in the Firth

But the unexpected consequence of this short flight was that the design and functioning of the margins and channels and shoals of the Firth had become much clearer.
We flew over the saltmarshes of the Upper Solway, beyond which the outgoing tide had left sandbanks and mudflats glistening in the sun. A great advantage of the gyroplane is that you can fly low and fairly slow, which gives you plenty of opportunities for a detailed look. The vibration precludes taking legible notes –  and, with my lack of skill, good clear photos – but here are some observations:

Burgh Marsh

Burgh Marsh

Burgh (‘Bruff’) Marsh: three cattle start running, tails up, but the rest continue grazing, unconcerned. Bright white dots on land and water are gulls; a cormorant takes off, its beating wings leaving a V of spray; Andrew tells me he has seen salmon when they are running upstream.

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Two channels of the Eden; one channel of the Esk on right

Two channels of the Eden; one channel of the Esk on right

The darker, flow-patterned beds of the rivers Eden and Esk show clearly beneath the surrounding shallow water.

The monument to Edward I

The monument to Edward I

The uninspired monument to Edward I stands in the middle of the marsh, well away from the track: the king died while leading his men back to England across the Solway,and for a while his body lay in state in the fortified church of St Michael at Burgh-by-Sands.

Cattle tracks converge on a bridge

Burgh Marsh. Cattle tracks converge on a bridge

Burgh Marsh is intercut with creeks and straight lines of drainage; water shines silver and blue amongst the green.

Port Carlisle; the canal's end is on the left, where a creek bisects the mud

Port Carlisle; the canal’s end is on the left, where a creek bisects the mud

At Port Carlisle, the port is silted with mud in shades of brown, grey and green, the dilapidated harbour wall a tumble of red sandstone; the end (or start) of the abandoned Carlisle canal remains just visible.

Bowness-on-Solway curves up and along a rise in the land; coastal mud now reaches up towards the road, and is etched with the patterns of currents where the incoming tide sweeps round the English side.

The end of the viaduct at Bowness on Solway. Low water: shallow channels but no sign yet of the flood tide

The end of the viaduct at Bowness on Solway. Low water: shallow channels but no sign yet of the flood tide

A rectangular stub of stonework is all that remains of the Bowness to Annan railway viaduct. Even the channel holding the ebbing tide is shallow, and sandy shoals cast off the water. A couple of weeks previously, Mark Messenger, haafnetter and owner of Glasson’s Highland Laddie pub, had told me it was now possible to walk across the Firth here on a good low tide, for the first time in his memory.

Saltmarsh at Campfield and Cardurnock

Saltmarsh at Campfield and Cardurnock

And so towards the Campfield RSPB Reserve, where – having previously walked on springy grass and leapt across narrow inlets – I suddenly understood the three-dimensional nature of the saltmarsh. The lower level is jigsawed by glistening creeks, but the green sward rises in ever-dryer steps towards the narrow road that follows the coast. The RSPB’s scrapes for wading birds have been inundated by the tide, and retain the water.

Bund, road and canal

Estuary, saltmarsh, bund, road, canal

Then we circled, rain spattering against the windshields, as we searched for the edge of the cloud. We briefly followed the traces of the Port Carlisle canal that lay parallel to the road, before re-entering bright light and colour.

The return

The return

Three days later, I crossed the Firth on foot near Bowness and, at low tide, felt the force of the Rivers Eden and Esk.


For other posts on, for example, saltmarshes and crossing the Solway on foot near a ‘wath’, browse the topics in this blog.

A post about my second gyroplane flight, much further along the coast, is in ‘The design of the Solway Part2’ in this blog.

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The volcanoes of Workington

A multicoloured cliff

A multicoloured cliff

The colours of pebbles on the shore range from grey and ochre through green to blue, and the eroded cliff is banded orange and purple and red, like a section through an old volcano.

Pumice? Or pebbles?

Pumice? Or pebbles?

Pebbles are bubbled with cavities, though not as airy as pumice. We could have been in Iceland, but we were on the shore at Workington – looking at slag.

 

At Moss Bay, to the south, the 20-metre-high white cliffs that edge the land are man-made. To the north of the town, low rusty-brown cliffs are held back by tumbled blocks of limestone, and reefs of slag spill towards the sea in solid waves, part-hidden by slippery brown fronds of Fucus vesiculatus and F. serratus. Sea-smoothed fragments, greys, greens, blues, all sizes, have drifted over hard pavements of pebbled slag.

Slag pavement

Slag pavement

It’s a landscape that intrigues and draws you on, further and further along the beach: a man-made landscape, and you can only wonder at the human effort it required, the sequential steps – quarrying, haulage, smelting, and yet more haulage.

Limestone blocks holding back the rusty slag

Limestone blocks holding back the rusty slag

West Cumberland has been ideally suited to the production of iron and steel. Haematite and limestone were there to be quarried; and so was coal, both beneath the land and beneath the sea. In 1856 the Workington Haematite Iron Company Ltd, set up to make pig iron from locally-mined haematite ore, had two blast furnaces at Oldside, just north of the town; Bessemer steelmaking commenced there in 1877. In that same year the Workington Moss Bay plant added three Bessemer converters to its own iron-works, and the production of pig-iron and its conversion to steel escalated within the county. Sadly, the story of the industry’s decline is well-known, Cumbria’s iron and steel works closing in the 20th century. The Moss Bay works remained, turning iron into steel for rails until 1974, after which steel ingots were brought in from Teeside. Corus’s rail-making factory closed in 2006.

Nevertheless, the Workington area was a centre of iron and steel production for 100 years, and during these decades, one major unwanted by-product was slag.

Iron ore, limestone, coke. To make iron, you need these three ingredients, plus heat.
‘Coking’, or metallurgical, coal – in contrast to ‘thermal’ coal which is used for generating power – is produced by heating suitable coal to very high temperatures in the absence of oxygen to drive off the impurities such as sulphur and phosphorus and create a hard porous material. Photographs of the now-vanished coke works, furnaces and Bessemer converters are part of the region’s lost industrial heritage. There are valuable photos of the Moss Bay coke works on R W Barnes’ website.

Phil Baggely reproduces a 1908 article on his own website  [1] where the writer notes that “Old coal miners used to say that there is good coking coal lying between Distington and Moss Bay…” Current explorations by West Cumbria Mining in the Haig Pit and Whitehaven area indicate that some of the coal still remaining underground is indeed high-quality coking coal.

Coke, haematite and limestone are introduced into the top of the blast furnace and hot air is blasted into the furnace near the base. As the hot air burns the coke, the resulting carbon monoxide reduces the iron ore to iron. Molten iron is tapped off into a channel with lateral chambers to form iron ‘pigs’ (the pigs can then be converted to steel in a Bessemer converter).

The limestone acts as a flux, combining chemically with coke ash and impurities such as aluminates and silicates from the ore to form slag. The molten slag floats – think of the bubble-cavities in the pebbles – on top of the molten iron. It has to be removed, so it’s tapped off into specially-designed trucks, or ladles, and taken away for disposal.

In Workington, during more than a century of iron-making, this still-molten slag was tipped along the coast, forming artificial hills and cliffs, pavements and reefs.
Phil Baggely has put together a fascinating collection of information and old photos about Workington’s iron and steel works and their locomotives and wagons. Copyrighted material shows a diagram of a slag-ladle, and rare photos of filled ladles being pulled by a locomotive, then tipped and emptied.

Elsewhere, R W Barnes describes the hazardous business of emptying each ladle: “(It) was held in place on the track by ramming a giant wooden wedge – called a ‘Scotch’ – under the wheels. The loco then ran backwards, tensioning a chain attached to the ladle. As the chain tightened, the ladle tipped its load, returning under gravity when empty.” His photograph shows white-hot slag cascading down the tip, and Barnes remembers “standing on the green metal steps of the old Rocket-Brigade station with my Granda – half frightened, half excited – watching this regular, awe-inspiring event. Several tons of white-hot slag racing downwards from above; Workington’s own Vesuvius.”

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And thus the beaches are strewn with gaseous pebbles, and rusty iron-bearing material like the smooth and oozing shapes of solidified lava. It is an alien but involving landscape, devoid of marine life except where algae colonise the reefs.

Slag: weed-covered reefs, pavements and cliffs

Slag: weed-covered reefs, pavements and cliffs

When we visited, it was also a place of alien sounds: the regular scything ‘swish’ of nearby wind-turbines, reminiscent of a samurai sword; a man shouting angrily above the baying and yapping of an intermingling pack of dogs along the shore; the growling of trail-bikes unseen behind the slag-banks.

Sea-kale

Sea-kale

But at the top of the shore hemispherical mounds of sea-kale, with fleshy leaves and small white cruciform flowers, defiantly spread across the banked-up pebbles.IMG_3064

A short way inland, heath-spotted orchids and wild roses dotted the once-derelict land.

The colours and shapes of slag-pebbles from the shore

The colours and shapes of slag-pebbles from the shore


 

[1] Phil Baggely has also co-authored, with Neil Sanderson, a very interesting and copiously-illustrated book, A Pictorial Archive of Steel-making at Workington.  ISBN 0 9538447 1 4, published 2002 by Richard Byers, Workington

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Snippets 4: First notes – Hadrian’s Wall of Sound, Bowness-on-Solway

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At 5.45am the tide was still on the ebb, standing waves (‘reestings’) corrugated the surface of the channel, and the only sound amid the weighty silence of the still air was the trilling of oyster-catchers.

The end of the Wall at Bowness

The end of the Wall at Bowness

I walked, and waited, and fretted. Where was the saxophonist who was due to start playing at 6am, to play the first notes of the Hadrian’s Wall of Sound? Had she overslept? I was at the start of the Wall, where was she? Shafts of sunlight picked out Chapel Cross on the Scottish side. A radio droned from a house on the main street; a haaf-net was propped against a front wall; otherwise, no-one stirred in Bowness-on-Solway.

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A haaf-net, freshly-netted for the new season

Six o’clock came. An electrician set off to work in his van. I went back to my car – and the outdoor presenter on Radio Cumbria explained she was waiting for the BBC countdown to the Music Day; she was with the saxophonist at Bowness. But where? The village of Bowness is small. Then she mentioned cows…

IMG_2917I drove quickly to the saltmarsh just south of the village, and there they were: the radio van, the TV crews, fluffy microphones, hefty cameras hoisted on shoulders, cars parked along the verge, the vintage open-top bus. The cows.

Loud instructions were issuing from radio links in the vans, media people milled around – and Roz Sluman stood on the cropped, salty turf, against the silky grey backdrop of the Firth and sky, and played, ignoring the fuss and absorbed in her music. The plangent notes of the sax rose into the gentle air.

Roz Sluman. (Are those haaf-nets propped against the wall?)

Roz Sluman. (Are those haaf-nets propped against the wall?)

Before she had finished, the engine of the bus started with a clatter, and the ‘relay’ moved off with guitarist Tom Lapworth to the next venue on the Wall.

IMG_2922Roz moved away from her music stand and played on; photographers asked her pose here, and there. The cows chewed silently as they stared down at this unusual morning activity.

As I drove home, a different radio presenter explained that not much of Hadrian’s Wall survived in this area, but St Michael’s Church at Burgh-by-Sands, where the Dalston Male Voice Choir were warming up their vocal cords, was built of stone taken mainly from the Wall. At the moment, he and the singers were waiting for the relay to arrive.

A short time later on Radio4’s Today, Hadrian’s Wall of Sound got a brief mention, and so did Cumbria as the Dalston Male Voice Choir sang us into the Weather Forecast.

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Snippets 3: plastic rubbish and a bathyscope

My new piece of kit as a ‘low-tide guide’ (a delightful title conferred on me recently by BBC Radio4’s Open Country) is a bathyscope; with a bathyscope one can peer beneath the ruffled surface of pools and find out what’s going on. I could, of course, have bought a smart red bathyscope, but it sounded rather heavy to carry down to the low-tide mark, so it was time to ‘think laterally’: to investigate the rubbish.

The Marine Conservation Society recently highlighted the accumulation of rubbish on our shores, much of it plastic. It’s always been assumed that most of the rubbish on the shores comes from sea-farers on fishing boats and ships, but a recent survey shows that forty per cent – yes, that is 40% – comes from us land-dwellers. (In contrast about 17% derives from fishing and shipping.) We lazily, uncaringly, accidentally or intentionally, throw or flush away cartons, plastic bottles, baby wipes, disposable nappies and the like, at home or as we walk or drive around the towns and countryside.

Proportion of types of beach rubbish (taken from the MCS's report - details below)

Proportion of types of beach rubbish (taken from the MCS’s report – details below)

Our discards are blown by the wind or washed down in the rivers to the estuaries and the sea. The waves and wind knit the single objects together in tangled piles which accumulate on the shores open to the prevailing wind or longshore drift.

rascarrel rubbish3
The Galloway shore in the above photo is exposed to the Irish Sea and presents tidelines decorated with intriguing, colourful masses of objects, each with its own history, but the impact of their present and future stories is enormous. john & bathyscope barrel

However, one piece of rubbish from that shore has found a new and potentially beneficial use: looking like a bottomless bucket, but probably the former entrance tunnel to a lobster-creel, its inside was scribbled with the lime-white tubes of serpulid worms.

Brought home and fitted, by my husband, with a circle of perspex and two handles, it has been transformed into a bathyscope.

From Bucket to Bathyscope: looking at Lanice's tube-dwelling

From Bucket to Bathyscope: looking at Lanice’s tube-dwelling

Now, by pressing the bathyscope against the water’s surface and flattening the ripples, we’re able to see what lies beneath, in the undersea. Peering into this sub-surface world, we can see the living organisms that inhabit it, and learn their stories (in this photo, the  worm Lanice,whose sandy tube stands vertically at ’12 o’clock’) — and in doing so I hope that everyone who peers through the ‘peepscope’ (another good title) will begin to see why we must take more care, and take our rubbish home.

*****

Marine Conservation Society report 2014 on beach litter

World Ocean Review: 1 Living with the oceans.  A report on the state of the world’s oceans

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Hobbling through Allonby with an Idle Apprentice

Allonby in the late 1800s (postcard image from 'More Plain People'); Reading Room in the distance

Allonby in the late 1800s (postcard image from ‘More Plain People’); Reading Room in the distance

“Of course there was a reading-room. Where? Where! why, over there. Where was over there? Why, there! Let Mr. Idle carry his eye to that bit of waste ground above high-water mark, where the rank grass and loose stones were most in a litter; and he would see a sort of long, ruinous brick loft, next door to a ruinous brick out-house, which loft had a ladder outside, to get up by. That was the reading-room, and if Mr. Idle didn’t like the idea of a weaver’s shuttle throbbing under a reading-room, that was his look out.” Thus ‘Francis Goodchild’ described Allonby’s reading room to his companion ‘Thomas Idle’.

‘Goodchild’ and ‘Idle’ were Charles Dickens and Wilkie Collins, who had found accommodation at Allonby’s Ship Hotel. In September 1857, they were being guided up Carrock Fell, in the Caldbeck Fells to the north-east of Allonby, when Collins hurt his ankle: he “was within one step of the opposite bank, when his foot slipped on a wet stone, his weak ankle gave a twist outwards, a hot, rending, tearing pain ran through it at the same moment, and down [he] fell.”

We know the story and its sequel because they wrote about themselves, as Goodchild and Idle, and their adventures, in The Lazy Tour of the Two Idle Apprentices.

Allonby, postcard, from Peter Ostle's blog

Allonby, postcard, from Peter Ostle’s blog (for details, see below); note foreshore coming right up to the houses

Collins was taken, via Wigton, to an unnamed village, where he was treated by a doctor. After a day or two of rest, and boredom, ‘Goodchild’ then “converted Thomas Idle to a scheme he formed, of conveying the said Thomas to the sea-coast, and putting his injured leg under a stream of salt-water. … he immediately referred to the county-map, and ardently discovered that the most delicious piece of sea-coast … was Allonby on the coast of Cumberland. … and at Allonby itself there was every idle luxury (no doubt) that a watering-place could offer to the heart of idle man.”

They set out with great expectations.

ship hotel plaqueAt Allonby, Collins hauled himself up “a clean little bulk-headed staircase, into a clean little bulk-headed room”, at the Ship Hotel, and lay in enforced idleness for three days while the inflammation in his ankle decreased. Dickens, meanwhile, was required to explore and describe the village to his sessile companion: perhaps he wasn’t a shore-walker, for he doesn’t mention the shore.

He was very rude about Allonby.
“It was… what you might call a primitive place. Large? No, it was not large. Who ever expected it would be large? Shape? What a question to ask! No shape. What sort of a street? Why, no street. Shops? Yes, of course (quite indignant). How many? Who ever went into a place to count the shops? Ever so many. Six? Perhaps.”

“And was there a reading-room?” Idle/Collins asks …

It’s mentioned in a verse of the poem, Allonby, 60 years ago, recited by Allonby’s ‘cobbler poet’ J.J.Heskett, in 1901 (so relating to the 1840s):
Where now we have the Reading Room/ Th’ old weaving factory stood,/There busy men, with fourteen looms,/for many mouths earn’d food.

A reading room had indeed been established above the weaving shed, but this was soon to change. Thomas Richardson, a Quaker, banker, and local philanthropist, commissioned the construction of a new building, with considerable financial backing from his cousin Joseph Pease, who was the country’s first Quaker MP.

Pease appointed an architect, and a local builder and joiner, and the tall and substantial red sandstone building, held in trust for the public by five Trustees, was opened on July 28th 1862 – nearly 5 years after the Idle Apprentices’ visit. The building is described in the delightful book, full of precious memories, ‘More Plain People, and places on the Cumbrian Solway Plain’ *:
“The building was raised on vaults, to protect it from high tides, and, originally, these were open, providing an Italian style piazza in which visitors could shelter during inclement weather. Above this was a 16 foot reading room and at the end of this, separated by folding doors, was the library.”

rdg room from Holme website

A postcard, reproduced in ‘More Plain People’ (for details of the book, see below)

Later, the colonnade was enclosed to provide a games room. According to Darren King, the builder involved with the 21st-century renovation and conversion, and quoted in the Times & Star in 2012, “Right up until the 1940s, silent movies were shown on the ground floor of the Reading Rooms. There was a billiard room, and reading room on the top floor with newspapers and books for local people to read.”
Gradually, though, usage declined. The Trustees sold the building in the 1970s, and for the next 30 years or more, the Reading Room decayed, its disintegration accelerating when the roof collapsed during a storm. It began to resemble Dickens’ “ruinous brick loft”.
Every time I walked or drove through Allonby I was saddened by its decrepitude, its boarded windows and surrounding drifts of wind-blown rubbish.

Then, in 2005, it acquired new owners and eventually, by January 2014, the Times & Star was able to report, in a feature illustrating the interior, that Allonby’s Reading Room had been converted from “a seaside eyesore into a stunning, desirable home”, through a “labour of love” by the owners (and, presumably also, by Darren King).

The Reading Room  a couple of years ago, nearing completion of its conversion

The Reading Room a couple of years ago, nearing completion of its conversion

As for the original architect, appointed by Joseph Pease, he was a Quaker from Manchester –Alfred Waterhouse, who went on to design the rather more magnificent Natural History Museum in South Kensington, London.

Natural History Museum, Cromwell Road entrance

Natural History Museum, Cromwell Road entrance

More Plain People, and places on the Cumbrian Solway Plain, 2007; published by the Holme St Cuthbert History Group. ISBN 978-0-95488-232-7

Peter Ostle’s blog is Solway Past and Present

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Snippets 2: A chance encounter, as lifeboat ’47-024′ leaves the sea

A lifeboat takes to the air

A lifeboat takes to the air

The man with the camera seemed to know a bit about lifeboats. We were standing on the dock at Whitehaven harbour, watching as a lifeboat was hoisted out of the water. I hadn’t known that was due to happen: I’d seen the lifeboat moored down below the harbour wall earlier, and now as I walked back that way it was rising up into view.
I waited behind the barrier. A man in a hi-vis jacket told me it was going to Poole “on the back of a truck, it’ll get there in a day that way!”

IMG_2856The man with the camera came over. “It’s going to Poole” I told him, knowledgeably.
“It’s going to be sold,” he said. And soon Bob McLaughlin, for 11 years the volunteer operations manager at Workington RNLI station, and now Chairman of its Management Committee, was telling me many things about this Tyne class boat. I am very grateful to him for assuming – correctly – that I would want to know.

IMG_2859When the mobile hoist had carried the lifeboat across the dock road to a bay to wait for the lorry, he led me round the boat, showing me the two holes in the keel at bow and stern where ropes could be attached to pull the boat up a slip.
“You see she’s got a white bottom – that shows she’s a general-purpose boat. She can be housed on a cradle, go down a slip, or stay afloat.” Red-bottomed lifeboats are moored afloat all the time.

The Tyne class boats were built to last about 15 years: this one, RNLB Hilda Jarrett, is 24 years old and she will be taken to RNLI’s HQ at Poole to be sold. Previously boats have been sold as far afield as China and Canada. Of the 40 boats in the class, “only six or seven remain, and they’ll all be away in the next 18 months.”
Originally she was kept at Baltimore in Southern Ireland.“Did you see she hasn’t got a name on her stern, it just says ‘Lifeboat’? That’s because she’s been used as a relief boat” – for example as a temporary replacement for a local lifeboat that is being repaired – from  ports as varied as Douglas Isle of Man, Port Patrick, and even the Isle of Barra. A new relief boat,  the RNLB Robert and Violet, had arrived at Whitehaven a couple of days previously.

I commented on the easily-recognised and well-loved livery of dark blue, red and yellow, and Bob laughed. “The RNLI wanted to change the colours but there was an outcry. And you see the number on the bow? 47-024 – that’s the length in feet, and she’s number 24 in her class. They wanted to change the feet to metres …”

IMG_2858

He took me round to the stern and we looked at the propellors (which had a few white limey tubes of the marine worm Serpula on them, but were otherwise clean) and saw how they were protected by the structure of the hull, so as not to get damaged on a slipway. And there were two circular hatches, way underneath, which can be opened to allow for cleaning weed from the propellors. “You can do it from inside, you hang down into the tube – it’s a good way of getting seasick!”
Also at the stern were twin metal flaps covering the exhausts, and two vertical cylindrical structures, which I then saw were attached to flat plates with keels; they would be hydraulically-operated to change the trim of the boat as it gained speed, to prevent its bow lifting too high out of the water.

IMG_2860Workington RNLI’s general-purpose lifeboat is another Tyne-class boat, 47-028, the Sir John Fisher; the Facebook page notes that “it is the only davit launched alb [all-weather lifeboat] owned by the RNLI.” I remembered looking into its boat-house when I was at the Port of Workington.

When the Sir John Fisher is de-commissioned, they will receive one of the new, faster Shannon-class boats that have been designed specifically for the RNLI.

 

The Workington lifeboat crews have always played a very important role, both during the Carlisle and Cockermouth floods and in saving lives at sea. In West Cumbria we are all very aware of the important work they and all the other lifeboat crews do, entirely voluntarily.

The davit for lifting the lifeboat into the sea at the RNLI station, Port of Workington

The davit for lifting the lifeboat into the sea at the RNLI station, Port of Workington

As I write this, lone kayaker Nick Ray is working his way 2015 miles (“2015 in 2015”, and Twitter @LifeAfloat) around the Scottish coast, aiming to visit every Scottish RNLI station in order to raise money for the charity. He started from Kippford, and has enjoyed a couple of Solway sunsets, as well as strong winds and bumpy seas. Let’s hope his only encounters with the RNLI on that long trip are all entirely social affairs!

RNLB 'Robert and Violet', the new relief boat, at Whitehaven

RNLB ‘Robert and Violet’, the new relief boat, at Whitehaven

My thanks again to Robert McLaughin, OBE; and any mistakes in my account of meeting him and number 47-024 are entirely my own. It was a chance encounter, in the rain, for which I had been unprepared – and which made my day!

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