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:
Lomnice, Sokolov District, Karlovy Vary Region, Czech Republic

Oldest recorded age at locality: 23
Youngest recorded age at locality: 0

mindat Locality ID: 22383
mindat URL: http://www.mindat.org/loc-22383.html

Tectonic Settings:

Total number of sublocalities beneath "Lomnice, Sokolov District, Karlovy Vary Region, Czech Republic": 0
Total number of bottom-level sublocalities: 0

Latitude: 0°0'0"N
Longitude: 0°0'0"E
Decimal Degree (lat, lon): 0,0

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: As C Ca F Fe H Mg Mn Ni O S Si 

Elements from minerals reported directly at this locality: As C Ca F Fe H Mg Mn Ni O S Si 

Structural Groups for minerals in this locality: 
ArsenopyriteCalciteFluoriteGypsumHumboldtineMarcasiteNickelineNoneOrpimentOxalate
PyriteQuartzSpinelSulphur

19 IMA Minerals at location:
Ankerite  (*)Arsenopyrite  (*)Calcite  (*)Dolomite  (*)Fluorite  (*)
Greigite  (*)Gypsum  (*)Humboldtine  (*)Kutnohorite  (*)Marcasite  (*)
Orpiment  (*)Pyrite  (*)Pyrrhotite  (*)Quartz  (*)Realgar  (*)
Scorodite  (*)Siderite  (*)Smythite  (*)Sulphur  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Ankerite  (*)NoneCa(Fe2+,Mg)(CO3)25.3003092
Arsenopyrite  (*)ArsenopyriteFeAsS5.3009052
Calcite  (*)CalciteCa(CO3)5.30027770
Dolomite  (*)NoneCaMg(CO3)25.3009895
Fluorite  (*)FluoriteCaF25.3009617
Greigite  (*)SpinelFe2+Fe3+2S45.30062
Gypsum  (*)GypsumCa(SO4)·2H2O5.3006890
Humboldtine  (*)Humboldtine OxalateFe2+(C2O4)·2H2O00027
Kutnohorite  (*)NoneCaMn2+(CO3)25.300234
Marcasite  (*)MarcasiteFeS20005674
Orpiment  (*)OrpimentAs2S3000511
Pyrite  (*)PyriteFeS200039462
Pyrrhotite  (*)NickelineFe7S85.3009056
Quartz  (*)QuartzSiO25.30061156
Realgar  (*)NoneAsS000712
Scorodite  (*)NoneFe3+(AsO4)·2H2O5.3001153
Siderite  (*)CalciteFe(CO3)5.3006417
Smythite  (*)None(Fe,Ni)3+xS4 (x ≈ 0-0.3)5.30077
Sulphur  (*)SulphurS5.3002045



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Michelle_830The abandoned Lomnice pit, which was mined from 1983 to 1994, is situated in a shallow fault block in the marginal part of the lignite-bearing basin. During the Pliocene to Pleistocene compression phase, the Lomnice area was strongly folded and faulted, and the uplifted rocks have consequently undergone intensive fracturing and weathering
Michelle_832Antonín lignite seam is extracted from the Lomnice pit of the Sokolov Basin.
Michelle_835Sulfide oxidation and acid leaching of lignite have led to an increased mobility of ions and precipitation of humboldtine, and younger generations of pyrite and marcasite along the dislocation faces. Exposure to the atmosphere during and after the mining period resulted in the precipitation of a variety of minerals, including melanterite, rozenite, realgar, orpiment, and various ochreous deposits. Drainage effluents in the central mine-water reservoir have pH values between 2.3 and 2.9. Here, concentrations of SO4 2– and total Fe that range up to 3800 and 900 ppm, respectively, have led to the recent growth of jarosite-goethite nodules


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_832235.3Miocene Age of lignite   Yes  35644Sokolov District, Karlovy Vary Region, Czech RepublicAntonín lignite seamMurad and Rojík (2003)10.2138/am-2003-11-1234AM88_1915Age of lignite deposit in the Sokolov Basin.
Michelle_8305.30.01Pliocene - Pleistocene Age of compression phase      22383Lomnice, Sokolov District, Karlovy Vary Region, Czech RepublicLomnice pitMurad and Rojík (2003)10.2138/am-2003-11-1234AM88_1915During the Pliocene to Pleistocene compression phase, the Lomnice area was strongly folded and faulted, and the uplifted rocks have consequently undergone intensive fracturing and weathering
Michelle_83500Anthropocene Age of anthropogenic acivityhigh    Ferrihydrite, Humboldtine, Marcasite, Melanterite, Orpiment, Pyrite, Realgar, Rozenite, Schwertmannite 22383Lomnice, Sokolov District, Karlovy Vary Region, Czech RepublicLomnice pitMurad and Rojík (2003)10.2138/am-2003-11-1234AM88_1915Age of mining and post-mining activity. Sulfide oxidation and acid leaching of lignite resulted in the precipitation of a variety of minerals.


SampleSource LocalityReference URL


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