LOCATION
North and east of the village of Lilleshall (NGR SJ7315)
Please note this area is DANGEROUS
MINERALS
Limestone
WORKING LIFE
Known working life : 12th century - 1883

HISTORY
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The volcanic mass of Lilleshall Hill, with its prominent
monument to the Dukes of Sutherland, stands out of the East Shropshire Plain. It
is Pre-Cambrian in origin and, with the Wrekin, amongst the oldest rocks in
Europe. In later periods, the area was covered by shallow seas in which
limestone was deposited and, later still, by deserts affected by earth movements
and glacial erosion. The Lower Carboniferous Limestone outcrops to the east of
the hill and it is split by a number of major faults. The limestone occurred in
four beds and, although the shallower ones could be worked by opencast methods,
deep mining was required to work the lower ones. The lower deposits made a good
hydraulic cement which set under water and large quantities were used in the
building of Liverpool docks.
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It is not known when men first began to cut the limestone as a
building material but the adjacent Lilleshall Abbey was certainly built from it
in the 12th century. Following the dissolution of the Monasteries in the 1530s,
the estate was bought from the Government by the Leveson family who had made
their fortune in the Wolverhampton wool trade. The family immediately set to
work to economically exploit the land which had suffered much neglect during the
latter monastic days. Land was drained, communications were improved by
causeways across the marshy ground on the Weald Moors and general agricultural
improvements made.
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The family opened coal, iron and limestone mines,
particularly in the area which is now north Telford. Virtually all these
enterprises were contracted out to partnerships who worked the mines with
varying success.
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Although the earliest reference to limestone working in
Lilleshall was in 1625, it wasn't until the 18th century that industry generally
began to predominate. Sir John Leveson became Earl Gower in 1746 and the
industrial story really began when his son Granville Leveson Gower became the
second Earl in 1754. He was a typical high born gentleman of his age -
landowner, Member of Parliament, Lord of the Admiralty, Lord Privy Seal and Lord
Chamberlain to King George III. Despite all these duties, he took an active
interest in the efficient running of the local estates, namely Sherrifhales,
Lilleshall, Donnington Wood, St Georges, Priorslee, Wombridge and Snedshill.
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Lilleshall Church today
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His brother-in-law was Francis 3rd Duke of Bridgewater, who
was the originator of the first canal to be constructed in the new industrial
age and which carried coal out of his Manchester mines. Through him, Earl Gower
was introduced to the brothers Thomas and John Gilbert, the latter having had
much experience in the cutting of the Bridgewater canal. At that time there were
over 250 small pits extracting limestone in the area with varying degrees of
efficiency. The Earl's agricultural improvements had led to an increased demand
for lime and the expanding local iron works demanded limestone as a flux. The
Earl was thus persuaded that it would be more efficient to operate the limestone
extraction directly so he and the Gilbert brothers formed the Lilleshall
Partnership in 1764 to do this. The Earl also took over iron furnaces at
Donnington Wood so he now had a vested interest in producing and delivering
limestone as cheaply as possible.
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The new partnership soon recognised that a better
communication system was required between the widely dispersed sites and in 1765
began the construction of a canal. It ran from Pave Lane to the Earl's furnaces
at Donnington Wood and was known as the Donnington
Wood Canal. The quarries in Lilleshall village were improved and this
included one under what is now the Sylvan Close housing estate. This had been
abandoned and flooded by the 18th century and became home to a massive pike
which attacked fishermen and even pulled the Parish Clerk into the water! It was
eventually caught in 1767 when a drainage level was driven from the Boundary
Brook to unwater the quarry. The quarry was expanded into what became known as
Colliers Side Quarry.
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This expansion entailed the removal of a large quantity of
overburden to get at the limestone. To get rid of this, a length of canal was
dug to a nearby kettle hole and the spoil taken here in tub boats to fill in
marshy ground and make it suitable for agriculture. The quarry workings were
linked to the main canal near Hugh's Bridge by a branch canal which was
unfortunately 18 metres lower. To overcome this, the branch canal went under the
main canal in a tunnel with a shaft to link the two. Boats would be moored
underneath the shaft and a crane lifted pallets of stone up to other boats in
the canal above.
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Although some quarries could work the two shallowest limestone
beds by opencast methods, to reach the lower beds it became necessary to mine
the limestone since the cost of removing the overlying strata was too great.
This also applied where shallower beds dipped downwards and the overburden
increased proportionately. The mines were worked on the pillar and stall system
which left 25% of the limestone behind as pillars to support the roof. Tunnels
were driven down dip about 9 metres wide and, after a distance of about 18
metres, the tunnels were linked by a cross passage also 9 metres wide. The
process would then be repeated, leaving a series of pillars about 9 metres
square. For shallow beds, the mine passages would continue in from the existing
quarry face but, for lower beds, a shaft would be sunk to the appropriate level
and the same mining system employed.
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Lilleshall Quarry today
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Some of the limestone was converted to quicklime on site by
burning it in kilns. These consisted of 7.5 metre deep shafts with a grate at
the bottom connected to the outside by a horizontal service tunnel. They were
fuelled by coal carried on the canal from the nearby Donnington
collieries. The limestone and fuel were stacked at the shaft bottom, the fuel
set afire and the whole thing left to burn for several days. A draught was
sucked in along the tunnel and up the chimney shaft to increase the fire
temperature. After the fire had died down, the lime could be broken up into
small lumps for transport. Transport of limestone and coal to the kilns
themselves was originally by horse and cart but these were later replaced by
lines of "L" shaped cast iron rails. Since the quicklime becomes
caustic when wet, it was not advisable to transport it by rail. As a result, it
was usually stored by the kilns and picked up by customers themselves.
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Although some of the limestone was converted to slaked lime
for cement and local land improvement schemes, the majority was sent to be used
as a flux in the iron furnaces. It was transported on the canal in long lines of
tub boats (see Figures 50-51) which were 6 metres long, 1.9 metres wide and 1.2
metres deep. Due to the intricate network of canals in the area, this meant that
it could usually be transported directly from the quarry to the iron works
without being transhipped.
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A limestone kiln. Please note that this area
is DANGEROUS.
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The quarries at Colliers Side originally worked the shallower
beds opencast but the workings were eventually continued underground with
inclines linking them to the tramways above. The extracted waste material was
used to build great embankments across the quarry in which kilns were built, as
well as two tunnels for access. Tramways ran along the top of the embankment to
feed the kilns and to carry material to the canal. Shafts from 45-75 metres deep
were also sunk to work the lower beds and an open trench west of Limekiln Lane
was continued underground.
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Entrance to a Limekiln
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Quarry buildings
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The Lilleshall Partnership was creating a profitable business
from the Colliers Side quarries and this was not unnoticed by the neighbouring
Leeke family. Their land was in the parish of Church Aston but they were
landowners rather than industrialists. Their main venture was at Blackberry Bank
Mine, which had originally been worked from the 17th century, and they sunk
shafts over 36 metres deep. Pumping engines, probably of the Newcomen type, were
erected but they were less successful than they expected. This led them to
leasing the exploration rights to the Partnership who had linked Blackberry Bank
Mine to their canal system by 1798. By this time, however, the mine was almost
worked out and several 120 metre deep shafts had been sunk to the east at what
was to become the Pitchcroft Mine.
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By 1800, the mining industry of the area was at its fullest
extent but the Partnership was almost finished. Both the Gilberts were dead and
Earl Gower was 79. The younger son, Lord Granville Leveson-Gower, acquired all
the shares in the Partnership and formed the Lilleshall Company in 1802 with
John Bishton, James Birch, John Onions and William Phillips. The Blackberry Bank
Mine was abandoned and other quarries and mines around Lilleshall were finished
by the 1830s. Although twin exploratory shafts 213 metres deep were sunk at Crow
Hayes, work now concentrated on the Pitchcroft Mine.
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This mine worked in a restricted area but may have produced
over a million tons of limestone during its life. In 1846, the
Stafford-Wellington railway was built and this passed right by the main shaft of
the mine. A short branch was built to the mine and this made it much easier to
transport limestone to the Donnington furnaces. The mine was notorious for
accidents and a typical one occurred in 1858 in which three men were killed when
"an immense layer of stone" fell on them.
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In 1860 a real disaster struck when water was found to be
rising through the floor in old workings. This rapidly became a flood and the
workings had to be abandoned when the pumps could not keep pace with the inrush
(see Figure 54). No human lives were lost but the pit ponies could not be
rescued and they were left to their fate, the rotting carcasses polluting local
water supplies for some time afterwards. It was estimated that over 300 gallons
of water per minute were entering the mine and portable pumps capable of
removing 400 gallons per minute were brought in. Within days, however, the
inflow had doubled and the mine was lost. It is believed that exploratory
workings had passed through the Brocton Fault and found workable stone at a
different horizon, this then being left until required. Beyond the fault,
however, was the North Shropshire aquifer and over a period the pressure would
have built up until the water eventually burst into the workings. Tunneling
through this fault would have been like drilling into the bottom of a full bath,
once this had happened then nothing could have saved the mine. If became
necessary to find reserves elsewhere and attention turned to the Willmoor Mine.
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This was originally called Sour Leasow Pit and had begun as
twin exploratory shafts 60 metres deep, rapidly expanding to meet the local
needs for limestone. The mine was finally abandoned in 1883 but produced about
188,000 tons of limestone during 21 years of working. It averaged 7,500 tons per
year which was taken to a small basin on the nearby canal and carried in tub
boats to the furnaces. Its demise was due to the fact that the Company could
bring in limestone cheaper from Wenlock Edge and Nantmawr near Oswestry, despite
the extra distance involved.
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Thus ended the industrial history of Lilleshall and the
surrounding area. All mine buildings and equipment were removed and the dumps
planted with trees. The workings flooded and the shafts were capped with brick
"beehives" (see Figure 98). The tramways were removed and the canal
system became derelict, part of the main course being filled in during the
construction of the Lilleshall Hall drive in 1896.
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Lilleshall
Hall
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extracted from "Mining in Shropshire", David
Adams Editor Adrian Pearce with Permission ISBN 0-903802-63-5
E-Mail
Adrian Pearce
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