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:
Wooltana Cave, Wooltana Homestead Area, North Flinders Ranges, Flinders Ranges, South Australia, Australia

Oldest recorded age at locality: 0.01
Youngest recorded age at locality: 0

mindat Locality ID: 269720
mindat URL: http://www.mindat.org/loc-269720.html

Tectonic Settings:

Total number of sublocalities beneath "Wooltana Cave, Wooltana Homestead Area, North Flinders Ranges, Flinders Ranges, South Australia, Australia": 0
Total number of bottom-level sublocalities: 0

Latitude: 30°23'10"S
Longitude: 139°21'20"E
Decimal Degree (lat, lon): -30.386111111111,139.35555555556

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: C Ca H K Mg N O P S 

Elements from minerals reported directly at this locality: C Ca H K Mg N O P S 

Structural Groups for minerals in this locality: 
BiphosphammiteCalciteCeriteGypsumNoneOxalateSyngenite

11 IMA Minerals at location:
Biphosphammite  (*)Brushite  (*)Calcite  (*)Dittmarite  (*)Dolomite  (*)
Görgeyite  (*)Gypsum  (*)Leonite  (*)Syngenite  (*)Whewellite  (*)
Whitlockite  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Biphosphammite  (*)Biphosphammite(NH4)H2(PO4)0.010011
Brushite  (*)GypsumCa(PO3OH)·2H2O0.0100104
Calcite  (*)CalciteCa(CO3)0.010027770
Dittmarite  (*)None(NH4)Mg(PO4)·H2O0.01007
Dolomite  (*)NoneCaMg(CO3)20.01009895
Görgeyite  (*)NoneK2Ca5(SO4)6·H2O0.010011
Gypsum  (*)GypsumCa(SO4)·2H2O0.01006890
Leonite  (*)NoneK2Mg(SO4)2·4H2O0.010024
Syngenite  (*)SyngeniteK2Ca(SO4)2·H2O0.010044
Whewellite  (*)OxalateCa(C2O4)·H2O0.010066
Whitlockite  (*)CeriteCa9Mg(PO3OH)(PO4)60.0100104



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Michelle_000854Guano rich cave in dolomite. Mineralization occurs in crusts associated with Ghost Bat guano deposits. Groundwater has likely penetrated the cave in the past.


1 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_0008540.010Holocene Age of guano    Biphosphammite, Brushite, Dittmarite, Gorgeyite, Syngenite, Whewellite, WhitlockiteP, N269720Wooltana Cave, Wooltana Homestead Area, North Flinders Ranges, Flinders Ranges, South Australia, AustraliaWooltana CaveSnow et al. (2014)10.1080/03721426.2014.11649009TRSSA138_214Age of guano deposits in cave. The authors suggest "that bats occupied the cave well beforethe start of the Holocene (11.7K years BP) and well back into wetter times"


SampleSource LocalityReference URL


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