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Lays and Legends of the English Lake Country
There is probably some truth in the anecdote, related by Sandford. For it is said by West, that not long after the dissolution of Monasteries, Thomas Preston, of Preston-Patrick and Levens, purchased the site and immediate grounds of Furness Abbey from the trustees of the crown, with other considerable estates to the value of £3000 a year: after which he removed from Preston-Patrick, and resided at the Abbey, in a manor house built on the spot where the Abbot's apartments stood. Of his two sons, John the elder married the daughter of Curwen. His descendants were called Prestons of the Abbey, and of the Manor; and continued for four generations, when the two great grandsons of the purchaser died without issue. The family of Christopher, his second son, were known as the Prestons of Holker. Of these, Catharine, the fifth in the direct line from Christopher, was the mother of Sir Thomas Lowther, Baronet, of Yorkshire, to whom on the failure of the elder branch, the property of the Prestons in Furness was granted by George the First. This gentleman, by his marriage with the Lady Elizabeth Cavendish, daughter of the Duke of Devonshire, had an only son and heir, Sir William Lowther, Baronet, the last descendant of the Prestons of Preston-Patrick, who died unmarried in 1756, bequeathing all his estates in Furness and Cartmel to his cousin Lord George Augustus Cavendish, through whom they passed by inheritance to the present Duke of Devonshire.
In a report to the government of Queen Elizabeth, of the date of 1588, inserted among the Burghley Papers, the son and heir of this sharp-handed son-in-law of Curwen is mentioned in somewhat detractory terms, in a passage which describes "the Pylle of Folder," or Pile of Fouldrey. "The same Pylle is an old decayed castell of 'the dowchie of Lancaster, in Furness Felles, where one Thomas Preestone (a Papyshe Atheiste) is depute steward, and comaunders the menrede and lands ther, which were sometime members appertayninge to the Abbeye of Furnes.'"
Workington Hall, the seat of the Curwens, is a large quadrangular building, with battlemented parapets, situated on a woody acclivity over looking the river Derwent, at the east end of the town. It has been almost entirely rebuilt within the present century. The old mansion was castellated pursuant to the royal license granted by Richard II., in 1379, to Sir Gilbert de Culwen. It is remarkable for having been the first prison-house of the unfortunate Mary of Scotland, after she had landed within the dominions of her rival. Having left the Scottish shore in a small fishing boat, she landed with about twenty attendants near the Hall on Sunday, May 16th, 1568; and was received by Sir Henry Curwen as became her rank and misfortunes, and hospitably entertained by him, till she removed to Cockermouth, on her route to Carlisle. The apartment in which the Queen had slept was long preserved, out of respect to her memory, as she had left it. But some recent alterations of the mansion having become necessary, it was found that these could not be effected without the destruction of that portion which had been so long distinguished as the Queen's Chamber.
Mr. Denton, who wrote about the year 1676, says, "I do not know any seat in all Britain so commodiously situated for beauty, plenty, and pleasure as this is." And Mr. Sandford, who wrote about the same time, has the following rapturous description, "And a very fair mansion-house and pallace-like; a court of above 60 yards long and 40 yards broad, built round about; garretted turret-wise, and toors in the corner; a gate house, and most wainscot and gallery roomes; and the brave prospect of seas and ships almost to the house, the tides flowing up. Brave orchards, gardens, dovecoats, and woods and grounds in the bank about, and brave corn fields and meadows below, as like as Chelsay fields. And now the habitation of a brave young Sq. his father Monsir Edward Curwen, and his mother the grandchild of Sir Michael Wharton o' th' Wolds in Yorkshire."
Even Mr. Gilpin, a century later, was struck with "its hanging woods and sloping lawns," and speaks of its situation as "one of the grandest and most beautiful in the country."
The anecdote upon which the poem is founded was related by a person who about fifty years ago was much acquainted with what was current in some of the principal families in the West of Cumberland. She stated that it was commonly repeated among the servants of the different houses, and was quite credited by them: and that she herself had not any doubt as to the truth of the story, but could not give the period to which the circumstances refer.
One of the domestics of the Hall was said to have been surprised by her master in the manner described, and to have been overheard by him, uttering the words,—
"Who knows what may happen, or what may befall?I may be Lady of Workington Hall!"The butler was instructed to repeat the words publicly in the presence of the Maid, who fled from the mansion, overwhelmed with confusion. She subsequently formed a matrimonial alliance with a principal member of the family; and thus in a manner her prediction was verified.
Such was the story, and such the narrator. It may be added, that the published notices of the family are devoid of anything to give confirmation to the story; but as it was related in the neighbourhood in the spirit alluded to, a place has been given to it among the traditions of Cumberland.
THE ALTAR ON CROSS-FELL.
(FORMERLY FIENDS'-FELL.)
NOTES TO "THE ALTAR ON CROSS-FELL."
The Editor of Camden (Bishop Gibson), speaking of huge stones found together on the top of steep and high mountains, thought they might possibly be the ruins of Churches or Chapels which had been built there. "For," says he, "it was thought an extraordinary piece of devotion, upon the planting of Christianity in these parts, to erect crosses, and build chapels on the most eminent places, as being both nearer heaven and more conspicuous: they were commonly dedicated to St. Michael. That large tract of mountains on the east side of the county (of Cumberland), called Cross-Fells, had the name given them upon that account; for before, they were called Fiends'-Fell, or Devil's Fell; and Dilston, a small town under them, is contracted from Devil's-town."
Among the several monuments on the pavement in the cross-aisle in Hexham Cathedral, is one ornamented with a crosier, and inscribed, "Hic Jacet Thomas de Devilston."
The mountain, Cross-Fell, which is remarkable for the phenomenon of the Helm-Cloud upon its summit, and the Helm-wind, as it is called, generated within it, which is sometimes productive of such destructive effects in the valleys below, is said to have been formerly designated Fiends'-Fell, from the common belief that evil spirits had their haunt upon it; until St. Augustine, to whom and his forty followers, when travelling on their missionary labours in these parts, a legendary tradition ascribes the expulsion of the demons of the storms, erected a Cross, and built an altar on the summit, where he offered the holy eucharist, and thus was supposed to have counter-charmed the demons. Since that time it has borne the name of Cross-Fell; and the people of the neighbourhood style a heap of stones lying there, the Altar upon Cross-Fell.
The common saying, "Its brewing a storm," or "A storm is brewing," is one of the many phrases in which we only repeat the thought of our primeval Scandinavian ancestors; amongst whom the beverage quaffed in the halls of Valhalla, the drink of the Gods, was conceived to be a product of the storm, and had more or less identity with the Cloud-Water. In Germany, the mists that gather about the mountain tops before a storm are said to be accounted for in like manner, as if they were steam from the brewing or boiling in which dwarfs, elves, or witches were engaged. Such modes of expression, according to the dictionary of the brothers Grimm, are of extreme antiquity.
Some such ideas seem to have been popularly associated with that enormous cloud, which is often seen, like a helmet, to cover the summit of Cross-Fell, and in which the Helm-Wind is generated.
In speaking of the Helm-Wind, it may be necessary to premise that Cross-Fell is one continued ridge, stretching without any branches, or even subject mountains, except two or three conical hills called Pikes, from the N.N.W. to the S.S.E., from the neighbourhood of Gilsland almost to Kirkby-Stephen, that is about forty miles. Its direction is nearly in a right line, and the height of its different parts not very unequal; but is in general such, that some of its more eminent parts are exceeded in altitude by few hills in Britain, being 2901 feet above the level of the sea. The slope to the summit from the east is gradual, and extends over perhaps fifty miles of country; whilst on the west it is abrupt, and has at five miles from its base the river Eden running parallel to the mountain.
Upon the upper part of this lofty ridge, there often rests, in dry and sunny weather, a prodigious wreath of clouds, extending from three or four to sixteen or eighteen miles each way, north and south, from the highest point; it is at times above the mountain, sometimes it rests upon its top, but most frequently descends a considerable way down its side. This mighty collection of vapour, from which so much commotion issues, exhibits an appearance uncommonly grand and solemn; and is named from a Saxon word, which in our language implies a covering, the Helm. The western front of this enormous cloud is clearly defined, and quite separated from any other cloud on that side. Opposite to this, and at a variable distance towards the west, and at the same elevation, is another cloud with its eastern edge as clearly defined as the Helm; this is called the Bar or Bur. It is said to have the appearance of being in continual motion, as if boiling, or at least agitated by a violent wind.
The distance between the Helm and the Bar varies as the Bar advances towards, or recedes from, the Helm; this is sometimes not more than half a mile, sometimes three or four miles, and occasionally the Bar seems to coincide with the western horizon; or it disperses and there is no Bar, and then there is a general east wind extending over all the country westward.
The description of this remarkable phenomenon, the Helm-Wind, we will give from observations made by the Rev. John Watson, of Cumrew, and others. The places most subject to it are Milburn, Kirkland, Ousby, Melmerby, and Gamblesby. Sometimes when the atmosphere is quite settled, hardly a cloud to be seen, and not a breath of wind stirring, a small cloud appears on the summit of the mountain, and extends itself to the north and south; the Helm is then said to be on, and in a few minutes the wind is blowing so violently as to break down trees, overthrow stacks, occasionally blow a person from his horse, or overturn a horse and cart. When the wind blows, the Helm seems violently agitated; and on descending the fell and entering it, there is not much wind. Sometimes a Helm forms and goes off without a wind; and there are easterly winds without a Helm. The open space between the Helm and Bar varies from eight or ten to thirty or forty miles in length, and from half a mile to four or six miles in breadth; it is of an elliptical form, as the Helm and Bar are united at the ends. A representation of the Helm, Bar, and space between, may be made by opening the forefinger and thumb of each hand, and placing their tips to each other; the thumbs will then represent the Helm on the top of the fell, the forefingers the Bar, and the space between, the variable limits of the wind.
The open space is clear of clouds with the exception of small pieces breaking off now and then from the Helm, and either disappearing or being driven rapidly over the Bar; but through this open space is often seen a high stratum of clouds quite at rest. Within the space described the wind blows continually; it has been known to do so for nine days together, the Bar advancing or receding to different distances. When heard or felt for the first time it does not seem so very extraordinary; but when heard or felt for days together, it gives a strong impression of sublimity. Its sound is peculiar, and when once known is easily distinguished from that of ordinary winds; it cannot be heard more than three or four miles, but in the wind or near it, it is grand and awful, and has been compared to the noise made by the sea in a violent storm.
Its first effect on the spirits is exhilarating, and it gives a buoyancy to the body. The country subject to it is very healthy, but it does great injury to vegetation by beating grain, grass, and leaves of trees, till quite black.
It may further be remarked of this wind, that it is very irregular, rarely occurring in the summer months, and more frequent from the end of September to May. It generally blows from Cross-Fell longest in the spring, when the sun has somewhat warmed the earth beneath, and does not cease till it has effectually cooled it; thus it sometimes continues, according to Mr. Ritson, for a fortnight or three weeks, which he considers a peculiarity of the Helm wind of Cross-Fell. The wind itself is very chill, and is almost always terminated by a rain, which restores, or to which succeeds, a general warmth, and into which the Helm seems to resolve itself.
The best explanation of this very interesting and remarkable phenomenon is given in the following observations of Dr. T. Barnes of Carlisle.
The air or wind from the east ascends the gradual slope of the eastern side of the Penine chain or Cross-Fell range of mountains, to the summit of Cross-Fell, where it enters the Helm or cap, and is cooled to a low temperature; it then rushes forcibly down the abrupt declivity of the western side of the mountain into the valley beneath, in consequence of the valley being of a warmer temperature, and this constitutes the Helm wind.
The sudden and violent rushing of the wind down the ravines and crevices of the mountains occasions the loud noise that is heard.
At a varying distance from the base of the mountain the Helm wind is rarified by the warmth of the low ground, and meets with the wind from the west, which resists its further course. The higher temperature it has acquired in the valley, and the meeting of the contrary current, occasion it to rebound and ascend into the upper region of the atmosphere. When the air or wind has reached the height of the Helm, it is again cooled to the low temperature of this cold region, and is consequently unable to support the same quantity of vapour it had in the valley; the water or moisture contained in the air, is therefore condensed by the cold, and forms the cloud called the Helm-Bar.
The meeting of the opposing currents beneath,—where there are frequently strong gusts of wind from all quarters, and the sudden condensation of the air and moisture in the Bar-cloud, give rise to its agitation or commotion, as if "struggling with contrary blasts." The Bar is therefore not the cause of the limit of the Helm wind, but is the consequence of it. It is absurd to suppose that the Bar, which is a light cloud, can impede or resist the Helm wind; but if it even possessed a sufficient resisting power, it could have no influence on the wind which is blowing near the surface of the earth, and which might pass under the Bar.
The variable distance of the Bar from the Helm is owing to the changing situation of the opposing and conflicting currents, and the difference of temperature of different parts of the low ground near the base of the mountain.
When there is a break or opening in the Bar, the wind is said to rush through with great violence, and to extend over the country. Here again, the effect is mistaken for the cause. In this case, the Helm-Wind, which blows always from the east, has, in some places underneath the observed opening, overcome the resistance of the air, or of the wind from the west, and of course does not rebound and ascend into the higher regions to form the Bar. The supply being cut off, a break or opening in that part of the Bar necessarily takes place.
When the temperature of the lower region has fallen and become nearly uniform with that of the mountain range, the Helm wind ceases; the Bar and the Helm approach and join each other, and rain not unfrequently follows.
When the Helm-Wind has overcome all the resistance of the lower atmosphere, or of the opposing current from the west, and the temperature of the valley and of the mountain is more nearly equalized, there is no rebound or ascent of the wind, consequently the Bar ceases to be formed, the one already existing is dissipated, and a general east wind prevails.
There is little wind in the Helm-cloud, because the air is colder in it than in the valley, and the moisture which the air contains is more condensed and is deposited in the cloud upon the summit of the mountain.
There is rarely either a Helm, Helm-wind, or Bar, during the summer, on account of the higher temperature of the summit of the Cross-Fell range, and the upper regions of the atmosphere, at that season of the year.
The different situations of the Helm, on the side, on the summit, and above the mountain, will depend on the temperature of these places: when the summit is not cold enough to condense the vapour, the Helm is situated higher in a colder region, and will descend down the side of the mountains if the temperature be sufficiently low to produce that effect.
The sky is clear between the Helm and Bar, because the air below is warmer and can support a greater quantity of vapour rising from the surface of the earth, and this vapour is driven forward by the Helm-Wind, and ascends up in the rebound to the Bar. In short, the Helm is merely a cloud or cap upon the mountain, the cold air descends from the Helm to the valley, and constitutes the Helm Wind, and when warmed and rarified in the valley, ascends and forms the Bar.
WILLIE O' SCALES
NOTES TO "WILLIE O' SCALES."
The long and scattered hamlet of High and Low Scales, is on the west side of Crummock Beck, near Bromfield, and a few miles from Wigton in Cumberland. Skells or scales, from a Saxon or Gothic word signifying a cover, was the name given to those slight temporary huts made of turf or sods which in the mountainous district of this county and Scotland are called Bields. They were erected most commonly for the shelter of shepherds; and during the later periods, in the border wars to protect the persons who were appointed to watch the cattle of the neighbourhood. Few estates in the kingdom have belonged to one family longer than this of The Gill, which was formerly, however, much more extensive, comprising most probably the neighbouring hamlet of Scales. Another somewhat uncommon circumstance belonging to it is, that, to the close of last century, and for anything we know to the contrary, to a much later date, the owner had always lived on and occupied it himself; it had never been in the hands of a farmer.
The Reays of Gill, however variously their name has been spelled and pronounced by different branches of the family, derived it from one on whom it was undoubtedly bestowed as being characteristical and descriptive of himself. The active hunter, the companion and the friend of William the Lion, was called in the commoner Saxon language of his time Ra, or Raa, a Roe, from his unparalleled swiftness. In Scotland and Germany a roe is still pronounced rae, as it was formerly in England.