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A Pictorial and Descriptive Guide to Buxton, The Peak, Dovedale, Etc.
Ward, Lock & Co.'s
Illustrated Guide Books Series 1939-40
Transcriptions by Rosemary Lockie, © Copyright 2013
GUIDE TO BUXTON, THE PEAK, DOVEDALE, &c.
THE NORTH PEAK DISTRICT.
EDALE - HOPE - CASTLETON - HATHERSAGE.
THIS portion of the Peak District lies to the north-east
of Buxton, from which it can be visited by rail or by
road.
BUXTON TO CASTLETON BY ROAD.
Buxton is left by way of Fairfield, some 2 miles beyond
which is the quarrying village of-
so called on account of the large number of small
water-swallows in the neighbourhood. In local dialect it is “Darf
holes” - Anglicé, “dwarf holes”.
A Water-Swallow is a hole in which a stream disappears,
descending into an underground channel and emerging to
the surface at a distance, in some cases, of several miles.
In many instances, when the streams are full, the swallow is
unable to receive the whole of the water, and the diminished
flow continues its course along the surface; but in dry weather
the entire stream disappears.
Lying on the right of the main road is the ancient circle
known as the “Bull Ring”, now scheduled for protection
as an ancient monument, though to-day no stones remain to
show its link with the past.
The road turns sharply to the right at the foot of the hill
opposite The Clough Inn and half a mile farther reaches the
Ebbing and Flowing Well, a “Wonder of the Peak”. This is
by the roadside, on the right hand, almost opposite the gates
of Bennetston Hall.
After much rain the phenomenon, although not as marked
as it used to be, takes place every ten or fifteen minutes, the
water issuing from a small aperture in the side of the hillock
on which the well is located. The ebb and flow is believed to
be due to a curved conduit through which the water has to
| PEAK FOREST - ELDEN HOLE | 65 |
pass. One limb of this conduit becomes gradually filled with
water as it drains to the surface. At the same time the water
rises to the same level in the other limb of this natural syphon;
and when the second limb has become filled to its farther
extremity the flow takes place and continues until both
limbs of the conduit are emptied, when the flow ceases,
and the syphon has to be again filled. The visitor must not,
however, expect to see a picturesque fountain or anything
romantic. The well looks what it really is - nothing more
than an ordinary watering-place for cattle, one side of which
is protected by a stout stone wall.
According to Charles Cotton's Wonders of the Peake, 1683
“. . . whether this a Wonder be; or no
'Twill be one, Reader, if thou seest it flow,
For having been there ten times, for the nonce
I never yet could see it flow but once!”
At the top of the hill is a hamlet bearing the singular name
of Sparrowpit.
By making a digression to the right we can visit the rather
bleak village of Peak Forest. The Church, founded by the
Countess of Devonshire, is dedicated to King Charles the
Martyr. By virtue of Royal grant it had a “peculiar”
jurisdiction, and thus became a kind of Gretna Green,
for the priest could celebrate a valid marriage ceremony
between “any persons”, from “anywhere”, at “any time”!
At one period about 100 marriages a year were solemnized
here.
This locality was formerly the centre of a huge Royal
Deer Forest; now it is one vast quarry.
From Sparrowpit the road lies straight on and after a
mile and a half there is a track on the right leading to Elden
Hole, another “Wonder of the Peak”. It is a chasm on the
southern side of Elden Hill (1,543 feet) and was formerly
looked upon with awe as being fathomless, so that Sir Aston
Cockayne, of Ashbourne, wrote in 1658-
“Here, on a hill's side steep
Is Elden Hole, so depe
That no man living knows
How far its hollow goes”.
In 1780, however, an explorer discovered the bottom at a
depth of 180 feet. The hole is a natural cavern having its
roof and walls covered with stalactitic deposits - in some
places smooth and white as marble, in others like frosted
silver - the rougher portions of the rock assuming all sorts
of fantastic shapes. The Cavern is not accessible to the general
public.
In a mile or so the main road reaches its highest point
at Winnats Head (1,351 feet). Unless it is desired to visit
the Blue John Mine and the Treak Cliff Cavern, walkers
should here turn off to the right and reach Castleton by way
of the Winnats Pass. The road is too rough for anything
but “trial” motoring. From Winnats Head the main road
skirts the foot of Mam Tor, passing the Blue John Mine
(p. 75), and after a hairpin bend descends into Castleton,
passing the Treak Cliff Cavern (p. 74). Before reaching the
village a lane leads sharply back to the Speedwell Mine (p. 73)
and the Winnats.
Those who reach Castleton by railway travel viâ Chinley
over the Dore and Chinley Line, “the most tunnelled bit of
railway in this or any other country”. As already mentioned,
over four miles of the twenty which lie between the two
places from which it is named are run through the bowels
of the earth. In its open part it traverses two beautiful
valleys-Edale and the Hope Valley.
One of the tunnels - the Cowburn - is entered some 2
miles from Chinley Junction. It is 3,700 yards in length,
and lies 900 feet below the surface of the long hill through
which it is driven. A mile or so from the eastern end of the
tunnel is the old-world village of-
giving its name to the charming Vale of Edale (p. 55).
Radiating from the station are delightful walks, through scenery
unsurpassed in the Peak District. One of the most
interesting, affording a fine view of the whole Edale valley, lies
along a path west of the village towards the hamlet of Upper
Booth. Jacob's Ladder, as stepping-stones on the hillside
are called, is not far distant, and readers of David Grieve may
acquaint themselves with one of the scenes pictured in the
story by going as far as Edale Cross (p. 53), from which
Hayfield station is only 3 miles distant.
The high ground south of Edale Station and separating
Edale from Castleton commands fine views of the Vale of
Edale and Hope Valley, the latter including Castleton and
the picturesque ruins of Peveril Castle; and as already stated
(p. 56) provides a splendid ridge walk all the way from Rushup
Edge to Hope. Or one can descend directly to Castleton.
At the eastern end of Edale is-
a very ancient village, built near the junction of the Styx
(sometimes called the Peak's Hole Water, because it flows
out of the Peak Cavern, p. 72) with the Noe. Its principal
feature is the Parish Church (St. Peter's), built about the
fifteenth century, in the Perpendicular style. This quaint-looking
little structure, standing close to the Noe and almost
hidden by sycamore and lime trees, has a squat tower and a
curiously stunted spire, which, seen through the trees, appear
by no means ungraceful. The porch has a parvise and a
canopied niche. The transepts and chancel are surmounted
by an embattled parapet, with crocketed pinnacles. The
gargoyles are very peculiar. In the interior of the church
are to be seen a piscina, sedilia, an old Norman font, and a
well-preserved carved oak pulpit, dating from 1652. The
Old Hall Hotel was formerly the seat of the Balguys, a family
possessing extensive estates in the neighbourhood in the
seventeenth century.
Surrounded as it is by Mam Tor, or the Shivering Mountain
(1,709 feet, see p. 76), Lose Hill (1,563 feet), and the curiously
named Win Hill (1,532 feet), there is no vale in the Peak
District more beautiful than that of Hope, though others
may be grander and more rugged.
The most popular walk from Hope is north-eastward over
Win Hill to Ashopton. Take the Edale road, beside the Old
Hall Inn and in a third of a mile, at a bend in the road, a
lane goes down to the river and crosses it just below a weir.
Some 200 yards beyond the bridge, stone steps lead up the
bank on the right, to a path crossing the railway. This path
leads up to Twitchill Farm, then bears up to the left, crossing
the ridge a little to the left of the highest point and descending
to Ashopton.
At Ashopton we enter the main Derwent valley, just where
the waters of the Ashop, coming down from Kinder Scout and
the Glossop moors, join it. The inn and one or two cafés
and farmhouses constitute the hamlet, which is, as it were,
the axle of a wheel, of which the roads to Sheffield, Hathersage,
Glossop, and Derwent Chapel are the spokes. In all
directions the scenery ranks amongst the finest of the Peak
District and the ascent of Win Hill is as pleasant and
remunerative a little climb as any in Derbyshire.
Unfortunately the beauty of the scene is doomed, for a great new
reservoir is being built here in connection with the extension
of the Derwent Water Works. It is estimated that the new
Lady Bower Reservoir will be completed in 1940.
It is a charming walk or drive of some 5 miles from Ashopton
to the Derwent Reservoirs, from which Sheffield, Derby and
Nottingham draw water. Midway is the ancient village of
Derwent. The Hall (formerly a seat of the Duke of Norfolk;
now a Youth Hostel) was built in 1672, and has been repeatedly
enlarged. The Parish Church, consecrated in 1869, has a
font bearing the date 1670 and the arms of the Balguys,
the original owners of the Hall. The Reservoirs are two
lakes, each about 2 miles long. The water is held up by
massive lofty dams across the valley of the Derwent. To
meet future requirements, it is proposed to impound water
in such a manner and on such a scale that Derwent Hall,
with two villages and 3,000 acres of farm lands, will b
completely submerged. Fortunately, some years yet remain
ere the Hall will be required for sacrifice.
According to a local saying: “Mony a one lives in Hope
as ne'er saw Castleton”; but for visitors who come by rail
Hope is the station which gives access to the villages of
Castleton and Bradwell (p. 77).
Hotels.- See Introduction, p. 17.
Motor-buses to or from Hope Station, 2 miles; and from Buxton, Sheffield, etc.
Motorists making the circular tour embracing the following
route usually make the outward journey from Buxton viâ
Doveholes, returning from Castleton viâ Tideswell.
The public motors to Castleton from Buxton generally run
viâ Miller's Dale (p. 57) and Tideswell (p. 118). From the
latter the route takes a north-easterly direction past
Tideswell Lane Head, a long half-mile, to Windmill, where it
turns to the north-north-west. Soon Bradwell Dale is
reached, with towering rocks on either side. At the bottom
of the Dale is Bradwell (p. 77), 4 miles from Tideswell. From
Bradwell the route lies along part of an old Roman road to
Brough, 1½ miles, the site of a Roman station (Anavio).
Thence it passes through Hope, a mile distant, and, turning
to the west, reaches Castleton, 2 miles beyond Hope. By
this route the distance between Buxton and Castleton is
16 miles.
Castleton is set amidst picturesque scenery and is a
convenient centre for the most mountainous part of the Peak
District, whilst its remarkable caverns attract many visitors.
Among the old customs which still linger here is the ringing
of the curfew during the winter months; another gives the
villagers a carnival on May 29, called Garland Day, when
there is a procession, with a mounted king and queen, the
former carrying a huge garland of flowers. A band of music
and morris-dancers enliven the nooks and corners of the
village, and a Maypole on the market-place becomes the
centre of a joyous crowd. Sprigs of oak are worn by the
villagers, many of whom ascribe the gaiety as commemorating
the Restoration of King Charles II, who landed at Dover on
May 29, 1660. At sunset the great garland is hoisted by
means of a rope to the summit of the church tower, being
there secured on the central pinnacle, which it decorates until
it is withered.
The Parish Church
(generally closed; key can be obtained at the Vicarage, close by)
is dedicated to St. Edmund, and dates from the Norman
Conquest, when it was built by Peveril, the founder - or restorer,
as the case may be - of the Castle. The Church exhibits all
the styles of architecture which have prevailed since that
period. It consists of chancel, nave with aisles, and south
porch, and has a pinnacled tower at the west end. It
contains an ancient stone font, and there is a fine Norman
archway between nave and chancel. The chancel contains a
painting by Van Dyck, representing the Appearance to the
Shepherds. The doors of the old oak pews still bear the
names of the occupants in the seventeenth and eighteenth
centuries. The vestry contains a good library, the gift of
a former vicar, including some valuable and curious works -
among others, a copy of the “Breeches” Bible (so called
from the unusual rendering of Genesis iii. 7) and a Cranmer
Bible.
Castleton obtained its name from its close connection with-
Peveril Castle
(Admission, threepence. Official guide, 2d., on sale at the gate.)
a fortress which towers above the quaint small houses of the
village and which is a conspicuous feature in any characteristic
view of Castleton. The ruin is reached by a zigzag path. The
stronghold is inaccessible on every side save one, and even
there the approach is an artificial one, to obviate the severity
of the ascent; and the very narrow isthmus was guarded by
a keep. “The fortress hangs over the mouth of the Devil's
Cavern; its founder chose his nest”, says Sir Walter Scott,
“upon the principles upon which an eagle selects her eyry,
and built it in such a fashion, as if he had intended it, as an
Irishman said of the Martello towers, for the sole purpose of
puzzling posterity”. Its position was wellnigh impregnable
before the discovery of gunpowder.
The lordship was granted, with a number of others in
Derbyshire, by William the Conqueror to William Peveril in
1068. The north curtain wall may be ascribed to him and
to his son, William, who was disinherited in 1155, his estates
being forfeited to the Crown. In 1157 Henry II received the
homage of Malcolm, King of Scotland, within its walls. He
visited it on several occasions, and in 1176 erected the keep
at a cost of £135. During the rebellion of the barons against
King John, the Castle was garrisoned by the rebels. In the
reign of Edward III it passed to the Duchy of Lancaster,
of which it still forms a part.
The few remains are very interesting, and recently H.M.
Office of Works has carried out some of its intelligent
repairs. The north curtain wall is well preserved and there
are parts of the west curtain, which is of a later date. The
keep is also standing, and forms a prominent object in the
landscape from every direction. St. John Hope describes
it as “a characteristic Late Norman rectangular keep, about
60 feet high, and measuring 21 feet A inches by 19 feet
2 inches internally, with walls 8 feet thick”. The castle-yard
occupied nearly the whole of the summit, and was cut off
from the remainder of the ridge by a dry ditch. The
gateway was on the east side. Portions of the ashlar masonry
of the keep are embodied in Castleton church.
On the south side of the precipice on which the Castle
stands is-
a beautiful and secluded valley reached through a little gap
leading from the village Square. The narrow floor is formed
of short soft turf. It is a spot which the visitor with time
at his disposal should not miss. In the course of an ascent
of the Dale delightful views varying with each upward step
are obtained of the Castle and Hope Valley. The Dale
emerges on to the moors where there is a junction of four
moorland tracks: Hope - Buxton - Chapel - Castleton. The
latter may be regained by way of the Winnats (p. 76),
with Mam Tor in front of us, increasing in grandeur as we
approach it, and the fine mass of Rushup Edge keeping
guard on our left.
The Caverns, etc.- It should be noted that inspection of the various caves
involves certain expenses in guides' fees, lighting, etc., and that if only one
or two visitors share these the cost of visiting one place may be as much as
5s. per head. During the season there is usually no difficulty, as parties are
made up every half-hour or so, or even more frequently; but out of the season
it is advisable, if economy be an object, to visit Castleton on a Saturday.
Those who are not perfectly sound in wind and limb should also bear in
mind that although the inspection of the Peak Cavern involves practically
no steps (the path being more or less level throughout)-a remark which
also applies to the Treak Cliff Cavern, and the flight of steps down to the
Speedwell Mine is perfectly safe and well lit, the tour of the Blue John Mine
involves a descent of some 160 steps and a number of steep passages - and their
consequent re-ascent.
The Caverns usually shown at and near Castleton are four
in number, and differ much in character, but the hills have
many smaller caves and also old mine shafts. Of their kind
these caves are the most remarkable in the country; but
they lack the marvellous beauty of the Cheddar Caves. The
Peak Cavern is almost wholly a natural formation, the sole
work of man being the enlargement of some of the passages.
The Speedwell Mine comes next in point of distance, and
is rightly regarded as the most sensational. The Blue John
Mine has the finest incrustations, though the recently opened
Treak Cliff Cavern is hardly less remarkable in this respect.
Nearest to the centre of the village is the Peak Cavern. This
is reached by a lane from the north-west corner of the Square
which passes the Douglas Museum (admission 6d., children
3d.), of far greater interest than many more pretentious
establishments. There are a number of interesting locks,
ancient and modern; beautiful specimens of local mineral
and, perhaps most fascinating of all, a collection of miniature
models of machinery, buildings, etc.
A few yards beyond the Museum the lane reaches the river
known, from its adventurous upper course, as the Peakshole
Water (of which more is seen when we visit the Peak Cavern).
Do not cross the bridge, but turn up the passage between the
cottages on the left and through the garden to the Russett
Well, a small, crystal-clear pool that is of far greater interest
than it appears to be. It is actually part of a mysterious river
which has its source up near Buxton, quickly disappears
underground, is seen again in the Speedwell Mine (see p. 73),
where it drops into the “Bottomless Pit” and is not again
seen until it reaches this point. What happens to the waters
after plunging into the Bottomless Pit is not known, but by
colouring the water in the Pit and noting the time at which
the coloured water reaches the Russett Well it has been found
that the journey occupies many hours - a very clear
indication that the course is extremely tortuous. Below the
well, the waters join with those proceeding out of the Great
Cavern - another of the underground rivers for which this
district is famous.
Returning to the road, cross the bridge and immediately
take the riverside path, which leads up between cottages to
the entrance to-
The approach is impressive. The sheer limestone cliffs
here make a slight recess, above which Peveril's Castle keeps
guard. Below the path a slight stream issues from a
“swallow” - the same stream which is seen intermittently
inside the Cavern - and then as the path bears to the right
the huge, semicircular opening of the Cavern confronts us.
This great curiosity, the “Devil's Cavern” of Sir Walter
Scott, is 200 yards below the surface of the mountain in
which natural forces have excavated it.
The cave is entered by a natural arch, 60 feet high, 114 feet
wide, and 300 feet in depth. Beyond this hall, which has
been utilized as a rope-walk for over 300 years, a narrow low
passage, closed by a door at which candles are lighted,
conducts the visitor to a spacious opening, called the Bell-House,
from a number of round holes in the roof. It is separated
| PEAK CAVERN - SPEEDWELL MINE | 73 |
from the interior by a stream of water, the Styx, which is now
passed by a path leading through a passage, but which was
formerly traversed in a flat-bottomed punt. The passage
leads to the Great Cave, a spacious chamber, parts of
which are estimated to be 200 feet long, 150 feet in width
and 100 feet high, the whole being enarched with a
magnificence of general effect and a beauty and variety of detail
which baffle description. A passage has been discovered,
leading from this chamber, through the roof, coming out
near to Peveril Castle. The extremity of this hall narrows
into a second passage, near the farther end of which is a
group of broken rocks which have received the name of
Roger Rain's House, from the constant trickling of water
down their sides. Thence to the Chancel, a naturally-formed
opening high in the rock, with stalactitic encrustations.
Beyond is Pluto's Dining-Room, from which a rapid descent
leads to the Half-Way House, and thence, through a
succession of natural archways cut in the rock as regularly as
though carved by man, to Victoria Cavern, and Great Tom of
Lincoln; the latter so named from a concavity in the roof
somewhat in the form of a bell. The distance from this
point to the termination of the cavern is short. The sides
contract, and the roof descends until barely sufficient room
is left for the passage of the water, and further progress is
precluded at a distance of 1,z10 yards from the entrance.
Leaving the Cavern, follow the path alongside the stream,
cross the bridge and in a few yards turn left along a path
which leads to the main road. Here turn left, and keep left
at the fork in about half a mile for-
This mine is at the foot of Long Cliff, near the entrance
to the Winnats, three-quarters of a mile from Castleton.
Entrance to the mine is gained by an arched vault, closed
by a door, whence a descent of 72 feet, made by means of
steps, leads to a “level”, now converted into a
subterranean canal, traversed by a large flat-bottomed boat. The
canal is a cutting in the rock made towards the end of the
eighteenth century by a party of adventurers engaged in
mining for lead. After eleven years' effort and the
expenditure of £14,000, work was abandoned. The stream which
flows through the mine has its source at Perry Foot Well, on
the uplands between Castleton and Buxton. After its
subterranean journey, it reappears at the Russet Well, only half a
mile away, but the passage occupies twenty-two hours. The
natural outlets of the water are blocked to an extent
sufficient to maintain a depth of 3 feet 6 inches. As the boat
passes along, the conductor places candles at intervals on
the sides of the tunnel, which is so straight that the whole
of the lights can be seen from end to end. The effect is
very striking.
The narrow passage continues for about 750 yards; then
suddenly becomes an enormous gulf, at an immense cavern
which was struck during the excavations. The most
probable theory is that the cavern was formed by the dissolution
of a vein of soft limestone by the water which permeated it.
A broad platform, protected by a stout iron railing, has been
thrown across the chasm to allow visitors to survey the abyss
- “The Bottomless Pit ” - in safety and comfort.
Opposite the entrance to the Speedwell Mine, a footpath
provides a short cut to the main road, above which, a few
hundred yards to the left, is the entrance to the-
first opened to the public in 1935. This cavern rivals those
of Cheddar in the profuse display of scores of stalactites and
the attendant stalagmitic formations. The colour contrasts
are indeed astonishing for their delicacy and variety. The
most remarkable characteristic of the hill, known as Treak
Cliff, is that it is the only place in the world where Blue John
stone is found. It stands alone at the western extremity of
Hope Valley, at the base of Mam Tor, and is isolated by faults
and deep ravines on every side. It was while mining for
Blue John stone in 1926 that the workers discovered the
Treak Cliff Caverns. Visitors are conducted through the old
workings, with veins of Blue John stone (see p. 75) in situ,
beyond which are the natural caverns, containing a most
remarkable show of stalactites and stalagmites. The cavern
is lit by electricity.
Rather less than a mile from Castleton, there appears on
the left of the road a deep cleft in the cliff: the remains of
the Odin Mine, one of the oldest and most valuable source
of lead in the district. The Saxons are said to have worked
it by aid of convicts, and it was the Saxons who gave the
mine its name. The mine is of further interest as marking
- the, junction of the Limestone (to the east) with the Yoredale
Shales which are so pronounced a feature of neighbouring
Mam Tor. Near the entrance to the mine are some small
caves: they are wet, not particularly interesting, and hardly
worth the slight toil of reaching them.
Admission.- March to November. Other months by application in the Village.
See p. 71.
The Blue John Mine is reached by following the main road
as it curves round steeply before the face of Mam Tor. The
entrance to the mine will be seen on the left soon after the
steepest part of the ascent has been passed.
It is desirable to warn visitors that the full inspection of
the mine entails a descent and corresponding ascent of some
160 steps, as well as of a number of steep gradients. For
those to whom such work offers no terrors the visit is well
worth while.
The mine takes its name from the very beautiful variety
of fluor spar known as Blue John, or “The Peakland jewel”
which is found in it. Fluor spar is generally white. So rare
is this bluish-purple mineral that orders for it are always on
hand. Tazzas and other works of art made from Blue John
grace many palaces and famous houses; a particularly fine
example is in the Vatican Library; there is a large one at
Chatsworth House, whilst two Blue John vases have been
discovered at Pompeii.
“The name was given in contradistinction to a metal-blend
known to the old miners as Black Jack. The first stone mined
was blue in colour, so Blue John and Black Jack are namesakes.
The stone is 'calcium fluoride', or 'fluor spar'. Every form is
found in Castleton: blue, red, purple, and dark colours, displayed
in banded veins of extraordinary richness and beauty. There are
14 distinct varieties, and all are found at different depths from the
summit of the hill. I know a vein that runs up within a yard of
the surface, and another 280 feet deep, there being twelve
intermediate kinds between the two levels. The level seems to
determine both the veinings and the colour. Blue John is found only
in very small limestone caverns, averaging 6 feet high, and coats
the roof, the sides, and the floor. The veins run horizontally in
seams averaging 2½ inches thick and between the top and bottom
vein sulphate of baryta and clay in equal proportions are always
found. The last deposit of the series is clay. This points
indubitably to the Blue John being a water deposit”. - The Geology of
Castleton, by John Royse.
The principal attractions of this series of caves, which
extend for over 2 miles, are the large stalactites, the immense
variety of shell - fossils embedded in the limestone on its
sides, and the uninterrupted range of caverns and Blue John
stone.
One of the openings, known as Lord Mulgrave's Dining-Room,
is 30 feet wide and 150 feet in height. It owes its
name to the fact that Lord Mulgrave, who took a great
interest in the exploration of the caves and mine, entertained
the workmen in it. Vast portions of the sides of the Crystal
Waterfall are covered with sparry incrustations of great
variety, reflecting most beautifully the illuminations, and
presenting the appearance of a great cascade. The dome of
the Crystallized Cavern is of exceptional beauty and colour.
The Variegated Cavern is also visited; here dark patches
of manganese dioxide (the colouring matter of Blue John)
glitter in great profusion.
is a pass through a narrow rift in the limestone hills, on the
old Buxton road, just outside Castleton. “Winnats” is a
corruption of Wind Gates, a name the pass obtained from the
gusts of wind which constantly sweep through. South-west
breezes make themselves felt with special force. The view
through the great rocky portals presents a scene of
magnificent extent and beauty.
At the top of the pass, a mile and a quarter from Castleton
and three-quarters of a mile from the Speedwell Mine, stands
Winnats Head Farm, where milk and light refreshment can
be obtained. There, too, is a sign-post pointing out a
footpath to the Blue John Mine, 200 yards distant.
Westward of Castleton rises-
a hill of very singular aspect, much of the surface presenting
the appearance of having been scooped out. The hollows
are due to the action of the atmosphere on the silicious
shale and sandstone of which the hill is composed. Exposure
to the atmosphere causes the disintegration of the shale
and sandstone, which then trickle down into the valley below.
On account of this movement the hill is called the Shivering
Mountain, and is one of the “Wonders of the Peak”.
In the opinion of one writer, “It may be doubted whether
there is anything finer to be seen in England than the view
from the summit of Main Tor. It includes almost everything
which goes to form magnificent scenery, except water”.
To reach the hill proceed as to the Blue John Mine, and
then continue along the Chapel-en-le-Frith road. About half
a mile from the mine one can cross a field on the right to
Mam Nick, a slight depression on the west side of the hill,
or go on a little farther to a road which leads back to the same
point. From the “Nick”, Main Tor is but a quarter of
mile distant, and the way is perfectly plain. The “Nick”
provides a very fine surprise view of Edale and the High Peak.
Castleton may be regained from the summit of Mam Tor
by the exceptionally fine ridge walk to Back Tor and thence
by either of the routes to the village.
From Castleton a visit can also be paid to the picturesque
village of-
2 miles to the south-east. Many of the houses are quaintly
perched on overhanging crags. In 1893 a relic of the ancient
lead works - a pig of that metal cast by Roman miners - was '
unearthed here.
The principal object of interest is the Bagshaw Cavern,
a few minutes' walk from the centre of village. One of the
most curious of the Derbyshire caves, it is entered from
the hillside by a long flight of steps, cut in the rock; and
it comprises a number of fantastic chambers, hung with
stalactites and sparkling crystals. It may be visited in
company of a guide on application at Mr. Revell's cycle shop
near the Post Office. (The charges for admission are for
any number up to three, 3s.; over six, 1s. each, and a
satisfactory exploration cannot be made in less time than an
hour.)
Some 5 miles east of Castleton and connected with it by
road and rail is-
It is a quaint, old-world village on the slope of a range
of hills which protect it from east winds. Hathersage
claims to be the place in which Robin Hood's famous
henchman, Little John, first saw the light of day; a house, said
to have been his, stood near the church. There is little
doubt that he was buried here. His grave, on the south
side of the church, is marked by two small stones, with a
yew at head and foot and enclosed by a low iron fence. On
being opened in 1782 it disclosed bones of enormous size.
The grave was rifled for the second time in the early years of
the nineteenth century, and a thigh-bone measuring 32
inches was taken from it. The ghoulish party also removed
from the church, where they had hung for centuries, an
ancient cap and bow said to have belonged to the freebooter.
Tradition affirms that the outlaw pointed out the spot where
he desired to be buried, and directed that his cap and bow
should be hung in the church; and the ballad adds:-
“His bow was in the chancel hung;
His last good bolt they drave
Down to the rocks, its measured length
Westward fro' the grave.
And root and bud this shaft put forth
When spring returned anon;
It grew a tree, and threw a shade,
Where slept staunch Little John”.
The fine old Parish Church (St. Michael's) stands on a
height above the village. Universally voted one of the
most beautiful ecclesiastical edifices in the county, it is of
Decorated architecture, and consists of a nave, aisles and
chancel. It has a handsome clerestory, and a beautiful
tower of three stages, surmounted by an octagonal spire.
The interior contains the altar-tomb of Robert Eyre, of
Highlow, an Agincourt hero, and his wife and fourteen
children.
The village was formerly noted for the manufacture of
needles, heckle-pins, and umbrella frames, but these trades
have all gone, and the place is now known as the pleasant site
of country residences of Sheffield manufacturers and
tradesmen. Sheep dog trials take place in the neighbourhood
annually, and the event attracts many visitors.
Hathersage is generally held to have been the village
Charlotte Brontë had in mind when describing the hamlet
of Morton, whither Jane Eyre wandered after her escape
from Mr. Rochester and Thornfield Hall; and the lonely
house on the Moors where she found shelter is North Lees
Hall, an Elizabethan mansion, once the residence of the Eyr
| THE SURPRISE - LONGSHAW | 79 |
family, about a mile from the church, in the valley of the
Hood. It is now used as a farmhouse, but retains its
mullioned windows, central circular staircase, and other
interesting memorials of the age in which it was built. The ruins
of the Chapel built by the Eyres in 1686 for the services of the
Roman Catholic Church, to which they belonged, and
destroyed by a mob in 1688, are to be seen in a wood a little
below the house. Part of it has recently been restored for use.
North-west of Hathersage is Bamford, a picturesque
village that is the starting-point of some good walks. On
the Sheffield road, about 1½ miles above Hathersage, is
Millstone Edge Nick, called also the Surprise, by reason of the
lovely scene which suddenly bursts in sight when the spot
is approached from the opposite direction. (See p. 23). The
prospect embraces the pastoral Hope Dale in front, and th
wooded valley of the Derwent stretching southwards. Among
the details are Win and Lose Hills, on the right of Hope
Dale, a beautiful reach of the Derwent, the entrance to
Bretton Clough, and the beautiful Leam Woods rising from
the river. Those who ascend to this point and wish to vary
the return might well turn down to the south through the
Longshaw Estate (National Trust) to Grindleford Bridge on
the rail and bus routes. Longshaw Lodge is occupied by the
Holiday Fellowship: the vicinity commands really
magnificent views of some of the finest Derbyshire moorland and
valley scenery.
Beside the road just beyond the Surprise is an uncouth mass
of weather-stained rock, on which has been bestowed, with
more reason than is often the case, the title of the Toad's
Mouth Rock. About a mile north of the rock and visible
from the Lower Burbage Bridge is Carl Wark, a very
wonderful prehistoric fort. In the walls are stones of an estimated
weight of sixty tons.
OCR/transcript by Rosemary Lockie in November 2013.
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