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Higher Pitts Mine, Priddy, Mendip, Somerset, England, UKi
| Regional Level Types | |
|---|---|
| Higher Pitts Mine | Mine (Abandoned) |
| Priddy | Civil Parish |
| Mendip | Group of Divisions |
| Somerset | County |
| England | Constituent Country |
| UK | Country |
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Latitude & Longitude (WGS84):
51° 14' 19'' North , 2° 40' 3'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
ST534491
Type:
Mine (Abandoned) - last checked 2023
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Mendip | 110,000 (2018) | 2.9km |
| Westbury-sub-Mendip | 801 (2018) | 3.5km |
| Wookey | 810 (2018) | 3.6km |
| Wells | 11,343 (2018) | 3.7km |
| Rodney Stoke | 269 (2018) | 4.9km |
Burr (1996):
The Higher Pitts mine in Mendip Hills, Somerset, England, was a small mine that was sourced for iron and manganese in the 17th century. In 1890, the Somerset Manganese and Iron Ore Co. was formed to work the mine for commercial production of iron, manganese, lead, and copper but closed the mine in 1893 after meeting little success. Common minerals found in abundance at the mine are goethite, hematite, calcite, malachite and rhodochrosite. The last vestiges of mining have been removed from the site in 1992.
Until the much larger deposits of mendipite were discovered at Merehead quarry, the Higher Pitts mine at Priddy was the main source of specimens of this mineral in the Mendip Hills. The mine is the type locality for the minerals chloroxiphite and diaboleite, and has also produced some of the largest known crystals of hydrocerussite and crednerite. Recently, plattnerite and kentrolite have been identified in old specimens from the locality.
The Higher Pitts mine is situated near to the village of Priddy in the Mendip Hills, Somerset, England, 25 km south of the city of Bristol and 4 km north of the city of Wells. It is a picturesque spot at the edge of the steep southern escarpment of the Mendip Hills plateau, with wide views out across the Somerset Levels (alluvial plains) some 240 meters below. The shallow, dry valley in which the mine workings are located leads via Dursdon Wood to Ebbor Gorge, which cuts through the escarpment and descends to the famous Wookey Hole cave at its base. The gorge was presented to the National Trust in 1967 by Mrs. G. W. Hodgkinson, and is now a national nature reserve, but this does not include the Higher Pitts mine workings.
The area surrounding the Higher Pitts mine has long been used for sheep and cattle grazing, and there was an estate there in Saxon times called "Aebbewyrth" [Saxon = Aebbe's farmstead], which has given its name to Ebbor ("Ebber" in older documents) Gorge.
Lead mining was carried out in the immediate vicinity of the Higher Pitts mine from very early times. This activity peaked during the 17th century, but mining may have taken place during Roman times, or perhaps even earlier; there is a prominent Bronze Age tumulus (burial mound) situated directly between two of the largest lead veins in the region, approximately 1 km to the east of the Higher Pitts mine. Mining for lead continued on an ever decreasing scale throughout the 18th century, but had died out by the middle of the 19th century.
Indications of iron mining in the area date from 1752 when the shallow, dry valley at Dursdon Wood was known as "Iron Pits Bottom" (Gough, 1930).
Until the much larger deposits of mendipite were discovered at Merehead quarry, the Higher Pitts mine at Priddy was the main source of specimens of this mineral in the Mendip Hills. The mine is the type locality for the minerals chloroxiphite and diaboleite, and has also produced some of the largest known crystals of hydrocerussite and crednerite. Recently, plattnerite and kentrolite have been identified in old specimens from the locality.
The Higher Pitts mine is situated near to the village of Priddy in the Mendip Hills, Somerset, England, 25 km south of the city of Bristol and 4 km north of the city of Wells. It is a picturesque spot at the edge of the steep southern escarpment of the Mendip Hills plateau, with wide views out across the Somerset Levels (alluvial plains) some 240 meters below. The shallow, dry valley in which the mine workings are located leads via Dursdon Wood to Ebbor Gorge, which cuts through the escarpment and descends to the famous Wookey Hole cave at its base. The gorge was presented to the National Trust in 1967 by Mrs. G. W. Hodgkinson, and is now a national nature reserve, but this does not include the Higher Pitts mine workings.
The area surrounding the Higher Pitts mine has long been used for sheep and cattle grazing, and there was an estate there in Saxon times called "Aebbewyrth" [Saxon = Aebbe's farmstead], which has given its name to Ebbor ("Ebber" in older documents) Gorge.
Lead mining was carried out in the immediate vicinity of the Higher Pitts mine from very early times. This activity peaked during the 17th century, but mining may have taken place during Roman times, or perhaps even earlier; there is a prominent Bronze Age tumulus (burial mound) situated directly between two of the largest lead veins in the region, approximately 1 km to the east of the Higher Pitts mine. Mining for lead continued on an ever decreasing scale throughout the 18th century, but had died out by the middle of the 19th century.
Indications of iron mining in the area date from 1752 when the shallow, dry valley at Dursdon Wood was known as "Iron Pits Bottom" (Gough, 1930).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
27 valid minerals. 2 (TL) - type locality of valid minerals.
Detailed Mineral List:
| ⓘ Aragonite Formula: CaCO3 |
| ⓘ Azurite Formula: Cu3(CO3)2(OH)2 |
| ⓘ Baryte Formula: BaSO4 |
| ⓘ Calcite Formula: CaCO3 |
| ⓘ Calcite var. Manganese-bearing Calcite Formula: (Ca,Mn)CO3 |
| ⓘ Cerussite Formula: PbCO3 References: |
| ⓘ Chalcocite Formula: Cu2S |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Chloroxiphite (TL) Formula: Pb3CuO2Cl2(OH)2 Type Locality: References: |
| ⓘ Crednerite Formula: Cu+Mn3+O2 |
| ⓘ Diaboleite (TL) Formula: Pb2CuCl2(OH)4 Type Locality: References: |
| ⓘ Dolomite Formula: CaMg(CO3)2 |
| ⓘ Galena Formula: PbS |
| ⓘ Goethite Formula: Fe3+O(OH) |
| ⓘ Hematite Formula: Fe2O3 |
| ⓘ Hydrocerussite Formula: Pb3(CO3)2(OH)2 References: |
| ⓘ Kentrolite Formula: Pb2Mn3+2(Si2O7)O2 |
| ⓘ 'Limonite' |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 |
| ⓘ Manganite Formula: Mn3+O(OH) |
| ⓘ Melanotekite Formula: Pb2Fe3+2(Si2O7)O2 |
| ⓘ Mendipite Formula: Pb3Cl2O2 References: |
| ⓘ Mimetite Formula: Pb5(AsO4)3Cl |
| ⓘ Plattnerite Formula: PbO2 |
| ⓘ 'Psilomelane' |
| ⓘ Pyrolusite Formula: Mn4+O2 |
| ⓘ Pyromorphite Formula: Pb5(PO4)3Cl |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Rhodochrosite Formula: MnCO3 |
| ⓘ 'Tetrahedrite Subgroup' Formula: Cu6(Cu4C2+2)Sb4S12S |
| ⓘ 'Wad' |
| ⓘ Wulfenite Formula: Pb(MoO4) References: Spencer, L. J. (1923) New lead-copper minerals from the Mendip Hills (Somerset) Mineralogical Magazine and Journal of the Mineralogical Society, 20 (102) 67-92 doi:10.1180/minmag.1923.020.102.01 pp.88-90 |
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| Group 3 - Halides | |||
| ⓘ | Diaboleite (TL) | 3.DB.05 | Pb2CuCl2(OH)4 |
| ⓘ | Chloroxiphite (TL) | 3.DB.30 | Pb3CuO2Cl2(OH)2 |
| ⓘ | Mendipite | 3.DC.70 | Pb3Cl2O2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Goethite | 4.00. | Fe3+O(OH) |
| ⓘ | Crednerite | 4.AB.05 | Cu+Mn3+O2 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Plattnerite | 4.DB.05 | PbO2 |
| ⓘ | Pyrolusite | 4.DB.05 | Mn4+O2 |
| ⓘ | Manganite | 4.FD.15 | Mn3+O(OH) |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | var. Manganese-bearing Calcite | 5.AB.05 | (Ca,Mn)CO3 |
| ⓘ | Rhodochrosite | 5.AB.05 | MnCO3 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| ⓘ | Aragonite | 5.AB.15 | CaCO3 |
| ⓘ | Cerussite | 5.AB.15 | PbCO3 |
| ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| ⓘ | Hydrocerussite | 5.BE.10 | Pb3(CO3)2(OH)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| ⓘ | Wulfenite | 7.GA.05 | Pb(MoO4) |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Mimetite | 8.BN.05 | Pb5(AsO4)3Cl |
| ⓘ | Pyromorphite | 8.BN.05 | Pb5(PO4)3Cl |
| Group 9 - Silicates | |||
| ⓘ | Kentrolite | 9.BE.80 | Pb2Mn3+2(Si2O7)O2 |
| ⓘ | Melanotekite | 9.BE.80 | Pb2Fe3+2(Si2O7)O2 |
| Unclassified | |||
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Psilomelane' | - | |
| ⓘ | 'Wad' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Chloroxiphite | Pb3CuO2Cl2(OH)2 |
| H | ⓘ Diaboleite | Pb2CuCl2(OH)4 |
| H | ⓘ Goethite | Fe3+O(OH) |
| H | ⓘ Hydrocerussite | Pb3(CO3)2(OH)2 |
| H | ⓘ Manganite | Mn3+O(OH) |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | Carbon | |
| C | ⓘ Aragonite | CaCO3 |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Cerussite | PbCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Hydrocerussite | Pb3(CO3)2(OH)2 |
| C | ⓘ Calcite var. Manganese-bearing Calcite | (Ca,Mn)CO3 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | ⓘ Rhodochrosite | MnCO3 |
| O | Oxygen | |
| O | ⓘ Aragonite | CaCO3 |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Cerussite | PbCO3 |
| O | ⓘ Chloroxiphite | Pb3CuO2Cl2(OH)2 |
| O | ⓘ Crednerite | Cu+Mn3+O2 |
| O | ⓘ Diaboleite | Pb2CuCl2(OH)4 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Goethite | Fe3+O(OH) |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Hydrocerussite | Pb3(CO3)2(OH)2 |
| O | ⓘ Kentrolite | Pb2Mn23+(Si2O7)O2 |
| O | ⓘ Manganite | Mn3+O(OH) |
| O | ⓘ Calcite var. Manganese-bearing Calcite | (Ca,Mn)CO3 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Melanotekite | Pb2Fe23+(Si2O7)O2 |
| O | ⓘ Mendipite | Pb3Cl2O2 |
| O | ⓘ Mimetite | Pb5(AsO4)3Cl |
| O | ⓘ Plattnerite | PbO2 |
| O | ⓘ Pyrolusite | Mn4+O2 |
| O | ⓘ Pyromorphite | Pb5(PO4)3Cl |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Rhodochrosite | MnCO3 |
| O | ⓘ Wulfenite | Pb(MoO4) |
| Mg | Magnesium | |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Si | Silicon | |
| Si | ⓘ Kentrolite | Pb2Mn23+(Si2O7)O2 |
| Si | ⓘ Melanotekite | Pb2Fe23+(Si2O7)O2 |
| Si | ⓘ Quartz | SiO2 |
| P | Phosphorus | |
| P | ⓘ Pyromorphite | Pb5(PO4)3Cl |
| S | Sulfur | |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Chalcocite | Cu2S |
| S | ⓘ Galena | PbS |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Cl | Chlorine | |
| Cl | ⓘ Chloroxiphite | Pb3CuO2Cl2(OH)2 |
| Cl | ⓘ Diaboleite | Pb2CuCl2(OH)4 |
| Cl | ⓘ Mendipite | Pb3Cl2O2 |
| Cl | ⓘ Mimetite | Pb5(AsO4)3Cl |
| Cl | ⓘ Pyromorphite | Pb5(PO4)3Cl |
| Ca | Calcium | |
| Ca | ⓘ Aragonite | CaCO3 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Calcite var. Manganese-bearing Calcite | (Ca,Mn)CO3 |
| Mn | Manganese | |
| Mn | ⓘ Crednerite | Cu+Mn3+O2 |
| Mn | ⓘ Kentrolite | Pb2Mn23+(Si2O7)O2 |
| Mn | ⓘ Manganite | Mn3+O(OH) |
| Mn | ⓘ Calcite var. Manganese-bearing Calcite | (Ca,Mn)CO3 |
| Mn | ⓘ Pyrolusite | Mn4+O2 |
| Mn | ⓘ Rhodochrosite | MnCO3 |
| Fe | Iron | |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Goethite | Fe3+O(OH) |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Melanotekite | Pb2Fe23+(Si2O7)O2 |
| Cu | Copper | |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Chloroxiphite | Pb3CuO2Cl2(OH)2 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chalcocite | Cu2S |
| Cu | ⓘ Crednerite | Cu+Mn3+O2 |
| Cu | ⓘ Diaboleite | Pb2CuCl2(OH)4 |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| As | Arsenic | |
| As | ⓘ Mimetite | Pb5(AsO4)3Cl |
| Mo | Molybdenum | |
| Mo | ⓘ Wulfenite | Pb(MoO4) |
| Sb | Antimony | |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
| Pb | Lead | |
| Pb | ⓘ Cerussite | PbCO3 |
| Pb | ⓘ Chloroxiphite | Pb3CuO2Cl2(OH)2 |
| Pb | ⓘ Diaboleite | Pb2CuCl2(OH)4 |
| Pb | ⓘ Galena | PbS |
| Pb | ⓘ Hydrocerussite | Pb3(CO3)2(OH)2 |
| Pb | ⓘ Kentrolite | Pb2Mn23+(Si2O7)O2 |
| Pb | ⓘ Melanotekite | Pb2Fe23+(Si2O7)O2 |
| Pb | ⓘ Mendipite | Pb3Cl2O2 |
| Pb | ⓘ Mimetite | Pb5(AsO4)3Cl |
| Pb | ⓘ Plattnerite | PbO2 |
| Pb | ⓘ Pyromorphite | Pb5(PO4)3Cl |
| Pb | ⓘ Wulfenite | Pb(MoO4) |
Other Regions, Features and Areas containing this locality
British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
- Rheno-Hercynian BeltOrogenic Belt
EuropeContinent
UK
- England
- Somerset
- Mendip HillsGroup of Hills
- Somerset
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References
Spencer, L. J. (1923) New lead-copper minerals from the Mendip Hills (Somerset) Mineralogical Magazine and Journal of the Mineralogical Society, 20 (102) 67-92 doi:10.1180/minmag.1923.020.102.01




Higher Pitts Mine, Priddy, Mendip, Somerset, England, UK