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:
Collingwood, City Of Yarra, Victoria, Australia

Oldest recorded age at locality: 3.96
Youngest recorded age at locality: 0.68

mindat Locality ID: 210529
mindat URL: http://www.mindat.org/loc-210529.html

Tectonic Settings:

Total number of sublocalities beneath "Collingwood, City Of Yarra, Victoria, Australia": 2
Total number of bottom-level sublocalities: 1

Number of Child Localities: 1
Child Localities:
Clifton Hill

Latitude: 37°47'26"S
Longitude: 145°0'14"E
Decimal Degree (lat, lon): -37.790555555556,145.00388888889

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 H K Mg Na O S Si 

Elements from minerals reported directly at this locality: 

Structural Groups for minerals in this locality: 
AmorphousAnalcimeAragoniteCalciteChabaziteGypsumHarmotomeNatroliteNoneNot in a structural group
Thomsonite

11 IMA Minerals at location:
Analcime  (*)Aragonite  (*)Calcite  (*)Chabazite-Na  (*)Gonnardite  (*)
Gypsum  (*)Huntite  (*)Natrolite  (*)Opal  (*)Phillipsite-Na  (*)
Thomsonite-Ca  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Analcime  (*)AnalcimeNa(AlSi2O6)·H2O3.962.231140271627
Aragonite  (*)AragoniteCa(CO3)3.962.231140273250
Calcite  (*)CalciteCa(CO3)3.962.2311402727770
Chabazite-Na  (*)Chabazite(Na3K)[Al4Si8O24]·11H2O3.962.2311402766
Gonnardite  (*)Natrolite(Na,Ca)2(Si,Al)5O10·3H2O3.962.23114027167
Gypsum  (*)GypsumCa(SO4)·2H2O3.962.231140276890
Huntite  (*)Not in a structural groupCaMg3(CO3)43.962.2311402769
Natrolite  (*)NatroliteNa2(Si3Al2)O10·2H2O3.962.231140271236
Opal  (*)AmorphousSiO2·nH2O3.962.231140272994
Phillipsite-Na  (*)HarmotomeNa6(Si10Al6)O32·12H2O3.962.2311402727
Thomsonite-Ca  (*)ThomsoniteNaCa2(Al5Si5)O20·6H2O3.962.23114027452



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Giersdorf_00000274Cite specified as immediately to the north of Melbourne
Giersdorf_00000275Cite specified as immediately to the north of Melbourne
Giersdorf_00000276Location cited is referred to as west of the Merri Creek, the Corporation Quarries are immediately to the west of the Merri Creek and are also part of the Newer Volcanic Group
Giersdorf_00000277Location cited is referred to as west of the Merri Creek, the Corporation Quarries are immediately to the west of the Merri Creek and are also part of the Newer Volcanic Group
Giersdorf_00000278Location cited is referred to as west of the Merri Creek, the Corporation Quarries are immediately to the west of the Merri Creek and are also part of the Newer Volcanic Group
Giersdorf_00000279Location cited is referred to as west of the Merri Creek, the Corporation Quarries are immediately to the west of the Merri Creek and are also part of the Newer Volcanic Group
Giersdorf_00000280Location cited is referred to as west of the Merri Creek, the Corporation Quarries are immediately to the west of the Merri Creek and are also part of the Newer Volcanic Group


7 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
Giersdorf_0000027410.840.92±0.08K-Ar  87-187    276868Clifton Hill, Collingwood, City Of Yarra, Victoria, AustraliaLalorGray et al. (2009)10.1080/08120090802547066AJES56_245 
Giersdorf_000002750.760.680.72±0.04K-Ar  87-189    276868Clifton Hill, Collingwood, City Of Yarra, Victoria, AustraliaReservoirGray et al. (2009)10.1080/08120090802547066AJES56_245 
Giersdorf_000002762.412.312.36±0.05K-Arlava flow 87-193    64Corporation Quarries, Clifton Hill, Collingwood, City Of Yarra, Victoria, AustraliaBroadmeadowsGray et al. (2009)10.1080/08120090802547066AJES56_245One of three very similar samples of good quality with an average dated age of 2.31+/-0.03 that are thought to be from a single volcanic flow. The three samples in question (87-193, 211, and 213 respectively) were collected over a 15 km radius to the west of the Merri Creek
Giersdorf_000002773.963.863.91±0.05K-Arlava flow 87-194    64Corporation Quarries, Clifton Hill, Collingwood, City Of Yarra, Victoria, AustraliaBroadmeadowsGray et al. (2009)10.1080/08120090802547066AJES56_245One of two samples from poor-quality outcrops which lead the author to believe that there is an older volcanic flow underneath the area which sample 87-193 was collected. The samples from 87-183, 211, and 213 were all surface level rocks which were collected while the 194 and 195 samples were found in a more eroded outcrop.
Giersdorf_000002783.863.763.81±0.05K-Arlava flow 87-195    64Corporation Quarries, Clifton Hill, Collingwood, City Of Yarra, Victoria, AustraliaBroadmeadowsGray et al. (2009)10.1080/08120090802547066AJES56_245One of two samples from poor-quality outcrops which lead the author to believe that there is an older volcanic flow underneath the area which sample 87-193 was collected. The samples from 87-183, 211, and 213 were all surface level rocks which were collected while the 194 and 195 samples were found in a more eroded outcrop.
Giersdorf_000002792.342.262.3±0.04K-Arlava flow 87-211    64Corporation Quarries, Clifton Hill, Collingwood, City Of Yarra, Victoria, AustraliaCraigieburnGray et al. (2009)10.1080/08120090802547066AJES56_245One of three very similar samples of good quality with an average dated age of 2.31+/-0.03 that are thought to be from a single volcanic flow. The three samples in question (87-193, 211, and 213 respectively) were collected over a 15 km radius to the west of the Merri Creek
Giersdorf_000002802.332.232.28±0.05K-Arlava flow 87-213    64Corporation Quarries, Clifton Hill, Collingwood, City Of Yarra, Victoria, AustraliaDonnybrookGray et al. (2009)10.1080/08120090802547066AJES56_245One of three very similar samples of good quality with an average dated age of 2.31+/-0.03 that are thought to be from a single volcanic flow. The three samples in question (87-193, 211, and 213 respectively) were collected over a 15 km radius to the west of the Merri Creek


SampleSource LocalityReference URL


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