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Par Smelter (Slag Locality), Tywardreath and Par, Cornwall, England, UKi
Regional Level Types
Par Smelter (Slag Locality)Smelter (Built Over)
Tywardreath and ParCivil Parish
CornwallCounty
EnglandConstituent Country
UKCountry

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Latitude & Longitude (WGS84):
50° 20' 45'' North , 4° 42' 4'' West
Latitude & Longitude (decimal):
Type:
Smelter (Built Over) - last checked 2020
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Par9,462 (2015)0.6km
Fowey2,131 (2017)4.6km
St Austell25,447 (2017)5.2km
Polruan614 (2017)5.4km
Luxulian388 (2017)5.8km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
British Micromount Society, Devon and Cornwall Branch MeetingsLiskeard, Cornwall21km
Mindat Locality ID:
341123
Long-form identifier:
mindat:1:2:341123:3
GUID (UUID V4):
0


Slag occurrence from the 19th century Par lead smelter.

This locality is a little odd to position, as whilst the site of the smelting works lies just within the St Blaise parish boundary, the actual locality of the mineral bearing slag waste lies under the tidal waters just inside the adjacent Tywardreath & Par parish boundary.

One of the most notable features of the Par Lead Smelter was the 235-foot-high brick stack, constructed in 1857 and felled in 1907.

This stack, which was the tallest constructed in Cornwall, stood some distance away from the main works and was linked by a substantial flue system.

Whilst the brick work of the stack was demolished in 1907, the massive dressed granite foundations survived until 1966 when it was removed to make way for a new china clay store.

Examination of old mapping indicates that other buildings of the old smelter were latterly re-used for the Beaver Mills flour mill, latterly known as Cornwall Mills, these in turn survived into the 1970s when they were apparently destroyed by a fire.

The site of the smelter lies entirely within the current boundaries of the Par Docks complex and is not generally accessible, and there are now no visible remains of the former works.

Whilst this works is most known as a lead smelter, in the first half of the 19th century an attempt was made to smelt copper at the works with two furnaces constructed for this purpose, one to produce regulus and the other refined copper metal. This would appear to have been an unsuccessful trial with a recorded output of only 3 tons of copper regulus being sold in 1840.

As a consequence, rare blocks of copper slag can be found with associated copper minerals being present.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


10 valid minerals.

Detailed Mineral List:

ⓘ Anglesite
Formula: PbSO4
ⓘ Cerussite
Formula: PbCO3
ⓘ Cumengeite
Formula: Pb21Cu20Cl42(OH)40 · 6H2O
ⓘ Cuprite
Formula: Cu2O
ⓘ Gypsum
Formula: CaSO4 · 2H2O
ⓘ Native Copper
Formula: Cu
ⓘ Phosgenite
Formula: Pb2CO3Cl2
ⓘ Pseudoboleite
Formula: Pb31Cu24Cl62(OH)48
ⓘ Vivianite
Formula: Fe2+Fe2+2(PO4)2 · 8H2O
ⓘ Wüstite
Formula: FeO

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Copper1.AA.05Cu
Group 3 - Halides
ⓘPseudoboleite3.DB.10Pb31Cu24Cl62(OH)48
ⓘCumengeite3.DB.20Pb21Cu20Cl42(OH)40 · 6H2O
Group 4 - Oxides and Hydroxides
ⓘCuprite4.AA.10Cu2O
ⓘWüstite4.AB.25FeO
Group 5 - Nitrates and Carbonates
ⓘCerussite5.AB.15PbCO3
ⓘPhosgenite5.BE.20Pb2CO3Cl2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
ⓘAnglesite7.AD.35PbSO4
ⓘGypsum7.CD.40CaSO4 · 2H2O
Group 8 - Phosphates, Arsenates and Vanadates
ⓘVivianite8.CE.40Fe2+Fe2+2(PO4)2 · 8H2O

List of minerals for each chemical element

HHydrogen
Hⓘ GypsumCaSO4 · 2H2O
Hⓘ PseudoboleitePb31Cu24Cl62(OH)48
Hⓘ VivianiteFe2+Fe22+(PO4)2 · 8H2O
Hⓘ CumengeitePb21Cu20Cl42(OH)40 · 6H2O
CCarbon
Cⓘ CerussitePbCO3
Cⓘ PhosgenitePb2CO3Cl2
OOxygen
Oⓘ AnglesitePbSO4
Oⓘ CerussitePbCO3
Oⓘ CupriteCu2O
Oⓘ GypsumCaSO4 · 2H2O
Oⓘ PhosgenitePb2CO3Cl2
Oⓘ PseudoboleitePb31Cu24Cl62(OH)48
Oⓘ VivianiteFe2+Fe22+(PO4)2 · 8H2O
Oⓘ WüstiteFeO
Oⓘ CumengeitePb21Cu20Cl42(OH)40 · 6H2O
PPhosphorus
Pⓘ VivianiteFe2+Fe22+(PO4)2 · 8H2O
SSulfur
Sⓘ AnglesitePbSO4
Sⓘ GypsumCaSO4 · 2H2O
ClChlorine
Clⓘ PhosgenitePb2CO3Cl2
Clⓘ PseudoboleitePb31Cu24Cl62(OH)48
Clⓘ CumengeitePb21Cu20Cl42(OH)40 · 6H2O
CaCalcium
Caⓘ GypsumCaSO4 · 2H2O
FeIron
Feⓘ VivianiteFe2+Fe22+(PO4)2 · 8H2O
Feⓘ WüstiteFeO
CuCopper
Cuⓘ CupriteCu2O
Cuⓘ Native CopperCu
Cuⓘ PseudoboleitePb31Cu24Cl62(OH)48
Cuⓘ CumengeitePb21Cu20Cl42(OH)40 · 6H2O
PbLead
Pbⓘ AnglesitePbSO4
Pbⓘ CerussitePbCO3
Pbⓘ PhosgenitePb2CO3Cl2
Pbⓘ PseudoboleitePb31Cu24Cl62(OH)48
Pbⓘ CumengeitePb21Cu20Cl42(OH)40 · 6H2O

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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