Mineral Evolution Database
Created and maintained by the Mineral Evolution Project in partnership with RRUFF and mindat.
Mineral locality data provided by mindat.org



The Mineral Evolution database is currently under development.

The goal of this page is to present localities at which the mineral is found, and estimates of the oldest possible geologic age of the minerals at these localities.


Locality Name:
Bath And North East Somerset, England, UK

Oldest recorded age at locality: 208.5
Youngest recorded age at locality: 0.0117

mindat Locality ID: 241958
mindat URL: http://www.mindat.org/loc-241958.html

Tectonic Settings:

Total number of sublocalities beneath "Bath And North East Somerset, England, UK": 12
Total number of bottom-level sublocalities: 7

Number of Child Localities: 6
Child Localities:
Bath
Charlcombe
Chew Magna
Claverton
East Harptree
Radstock

Latitude: 51°23'11"N
Longitude: 2°21'35"W
Decimal Degree (lat, lon): 51.386388888889,-2.3597222222222

AThis mineral is Anthropogenic.
GThis mineral is directly dated.
BThis mineral is reported as having this age.
YThis mineral is using an age reported as an element mineralization period.
OThis mineral is using an age calculated from all data at the locality.
RThe age displayed for this mineral originates from a different, non-child locality.
PThe age displayed for this mineral is the range of ages for this mineral at all of this locality's children.
This mineral's age has not yet been recorded.

This Mineral list contains entries from this locality, including sub-localities. Minerals in bold are reported by mindat.org as occurring directly at this locality, and do not occur at any children (sublocalities) of this locality.

Elements at this locality, including sub-localities: Al C Ca Fe H Mg Na O Pb S Si Sr Zn 

Elements from minerals reported directly at this locality: Fe S 

Structural Groups for minerals in this locality: 
AllophaneBaryteCalciteClayDundasiteHydrotalciteKaoliniteMelanteriteNonePyrite
QuartzSmectite-vermiculiteSphalerite

14 IMA Minerals at location:
Allophane  (*)Calcite  (*)Celestine  (*)Dundasite  (*)Gibbsite  (*)
Hydrotalcite  (*)Kaolinite  (*)Melanterite  (*)Montmorillonite  (*)Pyrite  (*)
Quartz  (*)Scarbroite  (*)Smithsonite  (*)Sphalerite  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Allophane  (*)AllophaneAl2O3(SiO2)1.3-2.0·2.5-3.0H2O0.1110.01171116924470
Calcite  (*)CalciteCa(CO3)111691627770
Celestine  (*)BaryteSr(SO4)11169191252
Dundasite  (*)DundasitePbAl2(CO3)2(OH)4·H2O0.1110.0117111692497
Gibbsite  (*)NoneAl(OH)30.1110.01171116924504
Hydrotalcite  (*)HydrotalciteMg6Al2CO3(OH)16(H2O)40.1110.0117111692487
Kaolinite  (*)Clay KaoliniteAl2Si2O5(OH)40.1110.011711169245591
Melanterite  (*)MelanteriteFe(SO4)·7H2O1116917915
Montmorillonite  (*)Clay Smectite-vermiculite(Na,Ca)0.3(Al,Mg)2Si4O10(OH)2·nH2O2116916,1169171508
Pyrite  (*)PyriteFeS2208.5201.3039462
Quartz  (*)QuartzSiO2111692161156
Scarbroite  (*)NoneAl5(CO3)(OH)13·5H2O0.1110.011711169249
Smithsonite  (*)CalciteZn(CO3)651.811169242473
Sphalerite  (*)SphaleriteZnS111692621482



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Michelle_520Hydroscarbroite occurs with scarbroite in the dumps at East Harptree in veins and cavities. East Harptree is on the Northern edge of the Central Mendip Pb-Zn orefield. Ore forms in veins hosted by the Upper Triassic Dolomitic Conglomerate. After ore emplacement, the locality underwent intense hydrothermal silicification forming massive chert.
Michelle_527East Harptree is on the Northern edge of the Central Mendip Pb-Zn orefield. Ore forms in veins hosted by the Upper Triassic Dolomitic Conglomerate. After ore emplacement, the locality underwent intense hydrothermal silicification forming massive chert.
Michelle_528East Harptree is on the Northern edge of the Central Mendip Pb-Zn orefield. Ore forms in veins hosted by the Upper Triassic Dolomitic Conglomerate. After ore emplacement, the locality underwent intense hydrothermal silicification forming massive chert.


3 Ages assigned to this locality:

Excel IDMax Age (Ma)Min Age (Ma)Age as listed in referenceDating MethodAge InterpretPrioritized?Sample SourceSample NumRun NumAge from other LocalityDated MineralMinerals explicitely stated as having this ageAge applies to these ElementsMinDat Locality IDDated Locality (Max Age)Location as listed in referenceReferenceReference DOIReference IDAge Notes
Michelle_5200.1110.0117DevensianStratigraphyAge of secondary aluminum mineralization    Allophane, Alumohydrocalcite, Dundasite, Gibbsite, Hydroscarbroite, Kaolinite, ScarbroiteAl4688East Harptree Lead Mine, East Harptree, Bath And North East Somerset, England, UKEast HarptreeRyback (1988) JRS2_9Age of aluminum mineralization. The author speculates that the modified groundwater control in the periglacial setting allowed the mobilization and concentration of aluminous solutions.
Michelle_527651.8Tertiary Age of smithsonite mineralization    SmithsoniteZn4688East Harptree Lead Mine, East Harptree, Bath And North East Somerset, England, UKEast HarptreeRyback (1988) JRS2_9Age of smithsonite mineralization.
Michelle_528208.5201.3Rhaetian Age of silicificationhigh      4688East Harptree Lead Mine, East Harptree, Bath And North East Somerset, England, UKEast HarptreeRyback (1988) JRS2_9Age of silicification


SampleSource LocalityReference URL


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