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Wythburn Mine (Wheal Henry; Helvellyn Mine), St. John's Castlerigg and Wythburn, Allerdale, Cumbria, England, UKi
Regional Level Types
Wythburn Mine (Wheal Henry; Helvellyn Mine)Mine
St. John's Castlerigg and WythburnCivil Parish
AllerdaleDistrict
CumbriaCounty
EnglandConstituent Country
UKCountry

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Latitude & Longitude (WGS84):
54° 31' 26'' North , 3° 2' 18'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
NY328148
Type:
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Keswick4,281 (2018)10.4km
Ambleside2,529 (2018)11.3km
Portinscale560 (2018)11.7km
Braithwaite342 (2018)13.2km
Coniston641 (2018)17.4km
Mindat Locality ID:
4851
Long-form identifier:
mindat:1:2:4851:7
GUID (UUID V4):
64335bc3-1643-4fb7-9d7a-809f2d549eaa
Other/historical names associated with this locality:
North and Western Region; Cumberland


Wythburn Mine is situated in the upper part of Mines Gill on the western side of Helvellyn, the third highest mountain in England.

The mine exploited four lead veins, the Blue Vein, Old Vein (North South Vein), Eagle Crag Vein and the East West Vein.

In all six levels were driven on these veins. They were No.4 Level, the lowest level at 1300 ft. No.3 Level at 1600ft, No.2 Level at 1750 ft, No.1 Level at 1908 ft, Arnisons Level, which was named after a local miner, at 2098ft and Arnisons Top Level at 2348ft.

The mine was first worked by a group of local miners and prospectors in1835. They started work on two of the veins, Blue Rock Vein and Old Vein, which were exposed in the bedrock on the north side of the gill, opening up 2 levels, High Level (which was to become No.1 Level) and Low Level (which was later to become No.2 Level). It was hoped that the veins were going to be as rich as those on the other side of the mountain at the highly profitable Greenside Mine. However, the returns failed to meet expectations and venture soon collapsed resulting in the closure of the mine.

Then in 1837 the mine became Wheal Henry when a new company took over called the Wheal Henry Helvellyn Lead Mining Ltd., led by a Cornish man called Henry Molyneux, after whom the mine was named. They worked the mine until 1857, driving forward on both the High and Low levels and opening up a lot of new ground, including No.3 Level on the south side of the gill. After running into financial difficulties the company managed to raise more money with the promise of high returns and by the end of 1857 the company was refloated under the new name of the Henry Helvellyn Lead Mining Company Ltd. In 1859 work was started on No.4 Level on what was assumed to be a continuation of the very rich Eagle Crag vein on the eastern side of Helvellyn. Unfortunately for the company, No 3 and No 4 levels were to proving to be virtually barren and once again they found themselves in dire financial difficulties and work at the mine came to an end.

1861 saw the formation of a new company called the Wythburn Lead Mining Company and Wheal Henry became the Wythburn Mine. Soon the mine was working again with a lot of new development taking place to bring the mine up to date. A new dam and dressing plant was erected at the bottom of the gill to process the ore. An incline was built from the plant up to No 2 Level to transport the ore tubs down the steep gill to the mill, replacing the outdated method of using packhorses to transport the ore down the mountain. This self-acting incline, with a gradient of 1 in 3, was a massive feat of engineering, measuring 600 yards long, 9ft wide and 9 ft high and built out of dressed stone. A bridge was also built at the bottom of the incline so that it could ford the gill and take the ore directly to the ore bins at the dressing plant. At the top of the incline, a large winding drum house was built, just below No2 Level adit, to house the winding mechanism. This was all a massive investment for the new company, around Β£20,000, showing how confident they were in the mines future, and all this work was carried out in just 2 years. It was during this time that both Arnisons Level and later Arnisons Top level were started. Although some work was carried out on No3 Level it produced very little ore and was soon abandoned. It was the higher levels which were to prove the richest part of the mine as it was here that two of the veins, the Blue Rock Vein and The East West Vein intersected. The mine was opened up with a rise from No2 Level and No1 Level up to Arnisons Level. All the ore was then dropped down internally, a distance of 346ft, from the upper levels down to No 2 level, now the main drawing adit for transporting the ore down to the mill. However, despite all the work that was carried out, not enough ore was being raised to cover the costs and once again the mine failed to make a return on its investment with the company making substantial losses. In 1870 the company was in difficulty and put into liquidation. It finally closed in 1872.

Over the next eight years three more companies tried their luck with the mine, hoping to make their fortunes. The Helvellyn Mining Company (1872-1873), West Cumberland Consols Mining Company (1873 -1874) and finally in 1875 the New West Cumberland Consols Mining Company. Then in 1878 the Manchester Water Authority, who were building the Thirlmere reservoir at the bottom of the valley to supply the city of Manchester with its much needed water, bought the land and mineral rights to the mine. However, the mine continued to work in a reduced capacity for a further 4 years, recovering some good ore from the upper levels. But the low price of lead and the death of the mine captain in 1882 finally saw an end to mining at Wythburn. The dressing plant and mill were demolished by the Water Authority and the stone was reused in the construction of the reservoir so very little remains of the site today.

Despite the huge investment made by the various companies, and the amount of work put into opening up new ground, the mine was never a success and it is thought to of only produced around 1,500 tons of lead ore during its 47 year history. By the time the mine finally closed in 1882 there were 1,985 yards of levels and a total of 406ft of stopes and rises.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


23 valid minerals.

Detailed Mineral List:

β“˜ Anglesite
Formula: PbSO4
References:
β“˜ Baryte
Formula: BaSO4
β“˜ Brochantite
Formula: Cu4(SO4)(OH)6
References:
β“˜ Calcite
Formula: CaCO3
β“˜ Cerussite
Formula: PbCO3
References:
β“˜ Chalcopyrite
Formula: CuFeS2
β“˜ Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
References:
β“˜ Covellite
Formula: CuS
References:
β“˜ Galena
Formula: PbS
β“˜ Goethite
Formula: Ξ±-Fe3+O(OH)
References:
β“˜ Harmotome
Formula: Ba2(Si12Al4)O32 · 12H2O
β“˜ Hematite
Formula: Fe2O3
β“˜ Hemimorphite
Formula: Zn4Si2O7(OH)2 · H2O
References:
β“˜ Leadhillite
Formula: Pb4(CO3)2(SO4)(OH)2
References:
β“˜ Linarite
Formula: PbCu(SO4)(OH)2
References:
β“˜ Malachite
Formula: Cu2(CO3)(OH)2
References:
βœͺ Plumbogummite
Formula: PbAl3(PO4)(PO3OH)(OH)6
Description: Visual identification was made by David Green.
References:
β“˜ Pyrite
Formula: FeS2
References:
β“˜ Pyromorphite
Formula: Pb5(PO4)3Cl
References:
β“˜ Quartz
Formula: SiO2
References:
β“˜ Smithsonite
Formula: ZnCO3
References:
β“˜ Sphalerite
Formula: ZnS
References:
β“˜ 'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S
References:
β“˜ Wulfenite
Formula: Pb(MoO4)
References:

Gallery:

Ba2(Si12Al4)O32 · 12H2Oβ“˜ Harmotome
PbAl3(PO4)(PO3OH)(OH)6β“˜ Plumbogummite
Pb5(PO4)3Clβ“˜ Pyromorphite

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Covellite2.CA.05aCuS
β“˜Sphalerite2.CB.05aZnS
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Pyrite2.EB.05aFeS2
β“˜'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
β“˜Goethite4.00.Ξ±-Fe3+O(OH)
β“˜Hematite4.CB.05Fe2O3
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
β“˜Smithsonite5.AB.05ZnCO3
β“˜Cerussite5.AB.15PbCO3
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
β“˜Leadhillite5.BF.40Pb4(CO3)2(SO4)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Baryte7.AD.35BaSO4
β“˜Anglesite7.AD.35PbSO4
β“˜Brochantite7.BB.25Cu4(SO4)(OH)6
β“˜Linarite7.BC.65PbCu(SO4)(OH)2
β“˜Wulfenite7.GA.05Pb(MoO4)
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Plumbogummite8.BL.10PbAl3(PO4)(PO3OH)(OH)6
β“˜Pyromorphite8.BN.05Pb5(PO4)3Cl
Group 9 - Silicates
β“˜Hemimorphite9.BD.10Zn4Si2O7(OH)2 Β· H2O
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1
β“˜Harmotome9.GC.10Ba2(Si12Al4)O32 Β· 12H2O

List of minerals for each chemical element

HHydrogen
Hβ“˜ BrochantiteCu4(SO4)(OH)6
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hβ“˜ GoethiteΞ±-Fe3+O(OH)
Hβ“˜ HarmotomeBa2(Si12Al4)O32 · 12H2O
Hβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Hβ“˜ LeadhillitePb4(CO3)2(SO4)(OH)2
Hβ“˜ LinaritePbCu(SO4)(OH)2
Hβ“˜ MalachiteCu2(CO3)(OH)2
Hβ“˜ PlumbogummitePbAl3(PO4)(PO3OH)(OH)6
CCarbon
Cβ“˜ CalciteCaCO3
Cβ“˜ CerussitePbCO3
Cβ“˜ LeadhillitePb4(CO3)2(SO4)(OH)2
Cβ“˜ MalachiteCu2(CO3)(OH)2
Cβ“˜ SmithsoniteZnCO3
OOxygen
Oβ“˜ AnglesitePbSO4
Oβ“˜ BaryteBaSO4
Oβ“˜ BrochantiteCu4(SO4)(OH)6
Oβ“˜ CalciteCaCO3
Oβ“˜ CerussitePbCO3
Oβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ GoethiteΞ±-Fe3+O(OH)
Oβ“˜ HarmotomeBa2(Si12Al4)O32 · 12H2O
Oβ“˜ HematiteFe2O3
Oβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Oβ“˜ LeadhillitePb4(CO3)2(SO4)(OH)2
Oβ“˜ LinaritePbCu(SO4)(OH)2
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ PlumbogummitePbAl3(PO4)(PO3OH)(OH)6
Oβ“˜ PyromorphitePb5(PO4)3Cl
Oβ“˜ QuartzSiO2
Oβ“˜ SmithsoniteZnCO3
Oβ“˜ WulfenitePb(MoO4)
AlAluminium
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Alβ“˜ HarmotomeBa2(Si12Al4)O32 · 12H2O
Alβ“˜ PlumbogummitePbAl3(PO4)(PO3OH)(OH)6
SiSilicon
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siβ“˜ HarmotomeBa2(Si12Al4)O32 · 12H2O
Siβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Siβ“˜ QuartzSiO2
PPhosphorus
Pβ“˜ PlumbogummitePbAl3(PO4)(PO3OH)(OH)6
Pβ“˜ PyromorphitePb5(PO4)3Cl
SSulfur
Sβ“˜ AnglesitePbSO4
Sβ“˜ BaryteBaSO4
Sβ“˜ BrochantiteCu4(SO4)(OH)6
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ CovelliteCuS
Sβ“˜ GalenaPbS
Sβ“˜ LeadhillitePb4(CO3)2(SO4)(OH)2
Sβ“˜ LinaritePbCu(SO4)(OH)2
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
Sβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ClChlorine
Clβ“˜ PyromorphitePb5(PO4)3Cl
CaCalcium
Caβ“˜ CalciteCaCO3
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ GoethiteΞ±-Fe3+O(OH)
Feβ“˜ HematiteFe2O3
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ BrochantiteCu4(SO4)(OH)6
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ CovelliteCuS
Cuβ“˜ LinaritePbCu(SO4)(OH)2
Cuβ“˜ MalachiteCu2(CO3)(OH)2
Cuβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Znβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Znβ“˜ SmithsoniteZnCO3
Znβ“˜ SphaleriteZnS
MoMolybdenum
Moβ“˜ WulfenitePb(MoO4)
SbAntimony
Sbβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
BaBarium
Baβ“˜ BaryteBaSO4
Baβ“˜ HarmotomeBa2(Si12Al4)O32 · 12H2O
PbLead
Pbβ“˜ AnglesitePbSO4
Pbβ“˜ CerussitePbCO3
Pbβ“˜ GalenaPbS
Pbβ“˜ LeadhillitePb4(CO3)2(SO4)(OH)2
Pbβ“˜ LinaritePbCu(SO4)(OH)2
Pbβ“˜ PlumbogummitePbAl3(PO4)(PO3OH)(OH)6
Pbβ“˜ PyromorphitePb5(PO4)3Cl
Pbβ“˜ WulfenitePb(MoO4)

Mindat Articles

Storm Desmond and Wythburn mine by Paul Nicholson


Other Regions, Features and Areas containing this locality

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