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Treskerby and Chance United Mine (incl. Treskerby Mine; Wheal Chance), Redruth, Cornwall, England, UKi
Regional Level Types
Treskerby and Chance United Mine (incl. Treskerby Mine; Wheal Chance)Mine (Abandoned)
RedruthCivil Parish
CornwallCounty
EnglandConstituent Country
UKCountry

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Latitude & Longitude (WGS84):
50° 14' 57'' North , 5° 12' 15'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
SW716438
Type:
Mine (Abandoned) - last checked 2023
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
St. Day700 (2011)1.7km
Redruth42,690 (2017)2.3km
North Country773 (2017)2.3km
Chacewater1,226 (2017)3.4km
Mount Hawke1,511 (2017)3.7km
Mindat Locality ID:
995
Long-form identifier:
mindat:1:2:995:2
GUID (UUID V4):
0


This mine was formed in 1828 by amalgamation of Treskerby Mine and Wheal Chance. Both mines were working lodes in metamorphosed killas overlying the northern flank of the Carn Marth granite. The Treskerby sett adjoins the eastern boundary of Wheal Boys, marked by the County Crosscourse, which also defines the boundaries of the mines further north. To the east, it is adjoined by Wheal Chance. The shafts and workings were located on both sides of the Redruth-Truro road, but much of this area is now built over. To the south, the sett once extended 900 yards SE of Treskerby village, and for some time also included the Park-an-Chy Mine. Some dumps are located in woodland south of the Redruth-Turo road.

The mines were already active in 1800, and were abandoned a couple of years after their amalgamation. In 1860, the property was re-opened and partially dewatered. From 1815 to 1832, 47,545 tons of 9.5% copper ore were produced. During that period, the Treskerby section also raised 9 tons of black tin. Another 18,500 tons of 9% copper ore were produced from 1922 to 1927. Due to wolframite-bearing ore having been found in the dumps of Treskerby Mine, prospection works were carried out in 1938, but the source of the tungsten ore was not encountered.

The dumps have now largely been reclaimed and an active tree planing scheme is evidently in operation. Pieces of chalcopyrite-pyrite-arsenopyrite bearing rock may be found but the minerals appear as scanty grains or strings. Pale green flourite is common but only as rock forming material. White opal / semi-opal is also quite common, but again is only of poor rock forming quality. The stack at the end of the arsenic flue is in good condition though the calciner is crumbling and the flue is being reclaimed by the undergrowth. - April 2023.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


9 valid minerals.

Detailed Mineral List:

ⓘ Arsenopyrite
Formula: FeAsS
ⓘ Cassiterite
Formula: SnO2
ⓘ Chalcopyrite
Formula: CuFeS2
ⓘ Cuprite
Formula: Cu2O
ⓘ Fluorite
Formula: CaF2
ⓘ Native Copper
Formula: Cu
ⓘ Opal
Formula: SiO2 · nH2O
ⓘ 'Petroleum'
ⓘ 'Petroleum var. Bitumen'
ⓘ Pyrite
Formula: FeS2
ⓘ Quartz
Formula: SiO2
ⓘ 'Wolframite Group'

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Copper1.AA.05Cu
Group 2 - Sulphides and Sulfosalts
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘPyrite2.EB.05aFeS2
ⓘArsenopyrite2.EB.20FeAsS
Group 3 - Halides
ⓘFluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
ⓘCuprite4.AA.10Cu2O
ⓘQuartz4.DA.05SiO2
ⓘOpal4.DA.10SiO2 · nH2O
ⓘCassiterite4.DB.05SnO2
ⓘ'Wolframite Group'4.DB.30 va
Unclassified
ⓘ'Petroleum
var. Bitumen'
-
ⓘ''-

List of minerals for each chemical element

HHydrogen
Hⓘ OpalSiO2 · nH2O
OOxygen
Oⓘ CassiteriteSnO2
Oⓘ CupriteCu2O
Oⓘ OpalSiO2 · nH2O
Oⓘ QuartzSiO2
FFluorine
Fⓘ FluoriteCaF2
SiSilicon
Siⓘ OpalSiO2 · nH2O
Siⓘ QuartzSiO2
SSulfur
Sⓘ ArsenopyriteFeAsS
Sⓘ ChalcopyriteCuFeS2
Sⓘ PyriteFeS2
CaCalcium
Caⓘ FluoriteCaF2
FeIron
Feⓘ ArsenopyriteFeAsS
Feⓘ ChalcopyriteCuFeS2
Feⓘ PyriteFeS2
CuCopper
Cuⓘ ChalcopyriteCuFeS2
Cuⓘ CupriteCu2O
Cuⓘ Native CopperCu
AsArsenic
Asⓘ ArsenopyriteFeAsS
SnTin
Snⓘ CassiteriteSnO2

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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