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Wheal Pool, Helston, Cornwall, England, UKi
Regional Level Types
Wheal PoolMine
HelstonCivil Parish
CornwallCounty
EnglandConstituent Country
UKCountry

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00318860017272073304080.jpg
View of the Engine House at Wheal Pool

Wheal Pool, Helston, Cornwall, England, UK
05367840017272073308707.jpg
Wheal Pool Engine House Stack

Wheal Pool, Helston, Cornwall, England, UK
00318860017272073304080.jpg
View of the Engine House at Wheal Pool

Wheal Pool, Helston, Cornwall, England, UK
05367840017272073308707.jpg
Wheal Pool Engine House Stack

Wheal Pool, Helston, Cornwall, England, UK
02416880017272073316780.jpg
View of the Engine House at Wheal Pool

Wheal Pool, Helston, Cornwall, England, UK
07350650017272073311501.jpg
Wheal Pool Engine House Stack

Wheal Pool, Helston, Cornwall, England, UK
Latitude & Longitude (WGS84):
50° 5' 29'' North , 5° 16' 54'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
SW653265
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Helston12,184(2017)1.5km
Porthleven3,059(2017)2.4km
Breage471(2017)4.1km
Gweek667(2017)5.3km
Germoe175(2017)7.4km
Mindat Locality ID:
44641
Long-form identifier:
mindat:1:2:44641:8
GUID (UUID V4):
0


An ancient lead and silver mine, located about 1.2 km SW of Helston on the east side of the River Cober valley. The main lode, which is said to be the continuation of a cross-course that passes under Breage and along the eastern flank of Tregonning Hill, trends SE and crosses the valley at the northern end of Loe Pool. It was first worked from open casts and later from three shafts over a length of about 250 yards along its strike. Around 1800, the underground workings were 50 fathoms (92 m) deep. In driving south-eastwards, the lode was found to be heaved by a slide, beyond which it was not proved. Its continuation was not located until 1883 when exploration works were carried out at the mine. The sett also comprised another lode, which courses parallel to the main lode a little further north in the valley, and was worked to a depth of 34 fathoms.

In order to prevent the mine from drowning, the level of the water in Loe Pool was regulated by a drainage adit driven around 1790 from lake level through the cliffs at the southern end of the pool to the seashore. By doing this, the owners were able to remove up to 8 m of sediments and work up to 1.25 m of alluvial tin deposits. The outflow from the adit was used by tin streamers to work the tailings dumps of the mine.

The mine is said to have been active in the 16th century, but little is known about this early period of working. It possibly was started after the area had been exploited by the Company of Mines Royal in 1580. During another period of working around 1740, it yielded a tolerable profit to the adventurers. When it was set at work again around 1790, it produced lead ore which yielded from 30 to 40 ounces of silver per ton (60 ounces per ton according to Phillips, 1823), in a sufficient quantity to induce the proprietors to erect smelting and testing works for the extraction of silver. Yet the expense was so great as to absorb the principal part of the profit actually gained by working the mine, and the adventure was terminated a few years after (Carne, 1818). This was probably in 1796 because in that year, the owners of nearby Wheal Rose were looking at the Pool fire engine (Steam Beam Engine) with a view to purchase it for their mine. The next recorded working was in 1853, and it was prospected again in 1883 when test pits located the continuation of the lode south of the slide.

Select Mineral List Type

StandardDetailedGalleryStrunzChemical Elements

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Galena2.CD.10PbS
var. Silver-bearing Galena2.CD.10PbS with Ag
Group 5 - Nitrates and Carbonates
Cerussite5.AB.15PbCO3
Group 8 - Phosphates, Arsenates and Vanadates
Carminite8.BH.30PbFe3+2(AsO4)2(OH)2
Segnitite8.BL.10PbFe3+3AsO4(AsO3OH)(OH)6
Pyromorphite8.BN.05Pb5(PO4)3Cl

List of minerals for each chemical element

HHydrogen
HCarminitePbFe23+(AsO4)2(OH)2
HSegnititePbFe33+AsO4(AsO3OH)(OH)6
CCarbon
CCerussitePbCO3
OOxygen
OCarminitePbFe23+(AsO4)2(OH)2
OCerussitePbCO3
OPyromorphitePb5(PO4)3Cl
OSegnititePbFe33+AsO4(AsO3OH)(OH)6
PPhosphorus
PPyromorphitePb5(PO4)3Cl
SSulfur
SGalenaPbS
SGalena var.Silver-bearing GalenaPbS with Ag
ClChlorine
ClPyromorphitePb5(PO4)3Cl
FeIron
FeCarminitePbFe23+(AsO4)2(OH)2
FeSegnititePbFe33+AsO4(AsO3OH)(OH)6
AsArsenic
AsCarminitePbFe23+(AsO4)2(OH)2
AsSegnititePbFe33+AsO4(AsO3OH)(OH)6
AgSilver
AgGalena var.Silver-bearing GalenaPbS with Ag
PbLead
PbCarminitePbFe23+(AsO4)2(OH)2
PbCerussitePbCO3
PbGalenaPbS
PbPyromorphitePb5(PO4)3Cl
PbSegnititePbFe33+AsO4(AsO3OH)(OH)6
PbGalena var.Silver-bearing GalenaPbS with Ag

Geochronology

Geologic TimeRocks, Minerals and Events
Phanerozoic
 Paleozoic
  Permian
   Guadalupian
ⓘ Major polymetallic mineralization~270 MaCornwall, England, UK
   Cisuralian
ⓘ Porphyry dikes intruded (latest age)~275 MaCornwall, England, UK
ⓘ Greisenization (latest age)~280 MaCornwall, England, UK
ⓘ Porphyry dikes intruded (earliest age)~280 MaCornwall, England, UK
ⓘ Formation of metallized pegmatites~285 MaCornwall, England, UK
ⓘ Greisenization (earliest age)~285 MaCornwall, England, UK
ⓘ Emplacement of major plutons~295 MaCornwall, England, UK

Other Regions, Features and Areas containing this locality

British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
EuropeContinent
UK

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