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Old Millclose Mine, South Darley, Derbyshire Dales District, Derbyshire, England, UKi
Regional Level Types
Old Millclose MineMine
South DarleyCivil Parish
Derbyshire Dales DistrictDistrict
DerbyshireCounty
EnglandConstituent Country
UKCountry

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Latitude & Longitude (WGS84):
53° 9' 10'' North , 1° 36' 57'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
SK258618
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Winster600 (2018)2.2km
Bonsall803 (2018)4.1km
Matlock14,956 (2017)4.3km
Youlgreave1,018 (2018)5.5km
Cromford2,073 (2018)6.2km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Peak Lapidary and Mineral SocietyBakewell, Derbyshire8km
The Russell SocietyKnighton38km
Mindat Locality ID:
4855
Long-form identifier:
mindat:1:2:4855:5
GUID (UUID V4):
0
Other/historical names associated with this locality:
Millclose Grove


DMS coordinates for Old Millclose Mine are: 53°09'10.8"N 1°36'57.3"W
DMS coordinates for New Millclose Mine (Millclose Mine) are: 53°09'30.9"N 1°36'29.3"W

At South Darley in the Derbyshire Dales District, there are two mines, New Millclose (down the hill) is flooded and below river level, and Old Millclose, up the hill in the fields behind the Red Lion in Wensley. There are about six shafts accessible and over ten miles of surveyed passages, including a complete underground blacksmiths shop with bellows, hearth tools etc. in situ. The remains of an old engine house, Watt's shaft and old spoil heaps can still be seen at the locality, but New Millclose mine is mostly flooded.

It is hard to establish how far back mining at Old Millclose mine goes, but it was certainly worked commercially through the 16th and 17th centuries. When it was operational, five soughs (underground channels for draining water out of a mine) were required to drain Old Millclose as the workings went deeper under the shales and these were drilled between 1658 and 1678. Old Millclose also contained two underground water wheels and, in 1782, an engine was installed underground. Yatestoop sough is 4km long and reaches Coast Rake at Elton. The engine house was built in 1859-60 by mine proprietor Edward Wass to house a Cornish engine (a beam-type steam engine) ordered from Thornewill and Warham of Burton-on-Trent. The engine pumped water from the Old Millclose lead mine via the Watts engine shaft adjacent to the building. This was an old shaft which was reopened in 1859. The engine was operated until the early 1870s when it was moved to the New Millclose mine some 450m to the north east. It was this new venture which became renowned as the largest lead mine in Britain. New Millclose reached more than 330m deep and the pumps had to raise more than 5000 gallons of water per minute to de-water the workings. The furthest workings reached nearly to Picory corner (near Haddon Hall). Over half a million tons of lead concentrate and over a 100k tons of zinc concentrate were produced over 75 years of working. The new mine became famous for being one of the most productive lead mines in the U.K. although little is now left as evidence. It closed in 1939 following an accidental flood and is no longer accessible to the general public.  It was located north east of Watt's shaft on the land now owned by H.J. Enthoven & Sons who still run the lead smelter on the original site.  Large spoil heaps from this mine can be seen opposite the factory, but these have been extensively reworked to extract fluorspar.  The whole area is contaminated with lead and is unsuitable for grazing. The current owners have planted trees on large areas of the contaminated land.

The engine house survives as a ruin, with foundations and one standing wall to the east visible. There are old shafts to the south and west of Watt's shaft too with the original Millclose Grove mine (as Old Millclose appeared to have be once called) located to the north of the old Red Lion pub (now closed) in Wensley.

The Millclose mines produced lead (galena) and zinc (sphalerite) with fluorspar, calcite and baryte as the main gangue minerals.  The galena apparently contained virtually no silver and the sphalerite about 1% cadmium.  Other minerals occur in small quantities including the rare cadmium bearing minerals greenockite and hawleyite, along with smithsonite, hydrozincite, cerussite and hemimorphite. Although the spoil heaps are small (and they have been well picked over the years), with some determination it is still possible to find examples of different coloured fluorite, calcite, sphalerite, baryte and occasionally greenockite/hawleyite.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


16 valid minerals.

Detailed Mineral List:

Baryte
Formula: BaSO4
Description: Bridges et al. (2008): "clear blades and white needles of baryte occur in cavities with other supergene minerals and in one case can be seen to be crystallised on smithsonite."
Calcite
Formula: CaCO3
Chalcopyrite
Formula: CuFeS2
Fluorite
Formula: CaF2
Galena
Formula: PbS
Greenockite
Formula: CdS
Gypsum
Formula: CaSO4 · 2H2O
Hemimorphite
Formula: Zn4Si2O7(OH)2 · H2O
Hydrozincite
Formula: Zn5(CO3)2(OH)6
Minium ?
Formula: Pb3O4
Native Sulphur
Formula: S8
Pyrite
Formula: FeS2
Pyromorphite
Formula: Pb5(PO4)3Cl
Smithsonite
Formula: ZnCO3
Sphalerite
Formula: ZnS
Torbernite
Formula: Cu(UO2)2(PO4)2 · 12H2O

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Sulphur1.CC.05S8
Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Greenockite2.CB.45CdS
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
Group 3 - Halides
Fluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
Minium ?4.BD.05Pb3O4
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Smithsonite5.AB.05ZnCO3
Hydrozincite5.BA.15Zn5(CO3)2(OH)6
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4
Gypsum7.CD.40CaSO4 · 2H2O
Group 8 - Phosphates, Arsenates and Vanadates
Pyromorphite8.BN.05Pb5(PO4)3Cl
Torbernite8.EB.05Cu(UO2)2(PO4)2 · 12H2O
Group 9 - Silicates
Hemimorphite9.BD.10Zn4Si2O7(OH)2 · H2O

List of minerals for each chemical element

HHydrogen
H GypsumCaSO4 · 2H2O
H HemimorphiteZn4Si2O7(OH)2 · H2O
H HydrozinciteZn5(CO3)2(OH)6
H TorberniteCu(UO2)2(PO4)2 · 12H2O
CCarbon
C CalciteCaCO3
C HydrozinciteZn5(CO3)2(OH)6
C SmithsoniteZnCO3
OOxygen
O BaryteBaSO4
O CalciteCaCO3
O GypsumCaSO4 · 2H2O
O HemimorphiteZn4Si2O7(OH)2 · H2O
O HydrozinciteZn5(CO3)2(OH)6
O MiniumPb3O4
O PyromorphitePb5(PO4)3Cl
O SmithsoniteZnCO3
O TorberniteCu(UO2)2(PO4)2 · 12H2O
FFluorine
F FluoriteCaF2
SiSilicon
Si HemimorphiteZn4Si2O7(OH)2 · H2O
PPhosphorus
P PyromorphitePb5(PO4)3Cl
P TorberniteCu(UO2)2(PO4)2 · 12H2O
SSulfur
S BaryteBaSO4
S ChalcopyriteCuFeS2
S GalenaPbS
S GreenockiteCdS
S GypsumCaSO4 · 2H2O
S PyriteFeS2
S SphaleriteZnS
S Native SulphurS8
ClChlorine
Cl PyromorphitePb5(PO4)3Cl
CaCalcium
Ca CalciteCaCO3
Ca FluoriteCaF2
Ca GypsumCaSO4 · 2H2O
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu TorberniteCu(UO2)2(PO4)2 · 12H2O
ZnZinc
Zn HemimorphiteZn4Si2O7(OH)2 · H2O
Zn HydrozinciteZn5(CO3)2(OH)6
Zn SmithsoniteZnCO3
Zn SphaleriteZnS
CdCadmium
Cd GreenockiteCdS
BaBarium
Ba BaryteBaSO4
PbLead
Pb GalenaPbS
Pb MiniumPb3O4
Pb PyromorphitePb5(PO4)3Cl
UUranium
U TorberniteCu(UO2)2(PO4)2 · 12H2O

Other Regions, Features and Areas containing this locality

British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
EuropeContinent
UK

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