| A | This mineral is Anthropogenic. |
| G | This mineral is directly dated. |
| B | This mineral is reported as having this age. |
| Y | This mineral is using an age reported as an element mineralization period. |
| O | This mineral is using an age calculated from all data at the locality. |
| R | The age displayed for this mineral originates from a different, non-child locality. |
| P | The 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. |
| Mineral name | Structural Groups | IMA Formula | Max Age (Ma) | Min Age (Ma) | # of Sublocalities containing mineral | LOCALITY IDs, not mindat ids | # of localities containing mineral |
|---|---|---|---|---|---|---|---|
| Anglesite (*) | Baryte | Pb(SO4) | 3 | 206420,206421,206456 | 2734 | ||
| Anorthite (*) | Feldspar | Ca(Al2Si2O8) | 1 | 206458 | 1036 | ||
| Azurite (*) | Not in a structural group | Cu3(CO3)2(OH)2 | 1 | 206456 | 5509 | ||
| Baryte (*) | Baryte | Ba(SO4) | 3 | 206420,206450,206456 | 11547 | ||
| Calcite (*) | Calcite | Ca(CO3) | 2 | 206456,206463 | 27770 | ||
| Cerussite (*) | Aragonite | Pb(CO3) | 2 | 206420,206456 | 4979 | ||
| Chalcocite (*) | None | Cu2S | 1 | 206456 | 5707 | ||
| Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 1 | 206456 | 27198 | ||
| Chrysocolla (*) | Allophane | (Cu2-xAlx)H2-xSi2O5(OH)4·nH2O | 1 | 206456 | 3531 | ||
| Covellite (*) | Covellite | CuS | 1 | 206421 | 4165 | ||
| Cuprite (*) | Not in a structural group | Cu2O | 1 | 206456 | 2970 | ||
| Dolomite (*) | None | CaMg(CO3)2 | 1 | 206418 | 9895 | ||
| Duftite (*) | Adelite | PbCu(AsO4)(OH) | 1 | 206456 | 220 | ||
| Fornacite (*) | Fornacite | CuPb2(CrO4)(AsO4)(OH) | 1 | 206456 | 85 | ||
| Galena (*) | Rocksalt | PbS | 5 | 206420,206421,206422,206450,206456 | 24243 | ||
| Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 1 | 206420 | 6890 | ||
| Hematite (*) | Corundum | Fe2O3 | 2 | 206456,206458 | 14640 | ||
| Malachite (*) | Malachite | Cu2(CO3)(OH)2 | 2 | 206450,206456 | 12537 | ||
| Mimetite (*) | Apatite | Pb5(AsO4)3Cl | 1 | 206456 | 1107 | ||
| Niter (*) | None | K(NO3) | 1 | 206426 | 181 | ||
| Opal (*) | Amorphous | SiO2·nH2O | 2 | 206459,206460 | 2994 | ||
| Plumbojarosite (*) | Alunite | Pb0.5Fe3+3(SO4)2(OH)6 | 2 | 206420,206421 | 477 | ||
| Pyrite (*) | Pyrite | FeS2 | 3 | 206420,206421,206456 | 39462 | ||
| Pyrolusite (*) | Rutile | MnO2 | 1 | 206420 | 3106 | ||
| Pyromorphite (*) | Apatite | Pb5(PO4)3Cl | 1 | 206420 | 1725 | ||
| Quartz (*) | Quartz | SiO2 | 3 | 206420,206421,206456 | 61156 | ||
| Siderite (*) | Calcite | Fe(CO3) | 1 | 206420 | 6417 | ||
| Smithsonite (*) | Calcite | Zn(CO3) | 2 | 206420,206450 | 2473 | ||
| Sphalerite (*) | Sphalerite | ZnS | 1 | 206421 | 21482 | ||
| Tetrahedrite-(Zn) (*) | Tetrahedrite | Cu6(Cu4Zn2)Sb4S13 | 1 | 206421 | 5317 | ||
| Tridymite (*) | Tridymite | SiO2 | 1 | 206425 | 458 | ||
| Wulfenite (*) | Scheelite | PbMoO4 | 2 | 206420,206456 | 1655 |
| Excel ID | Max Age (Ma) | Min Age (Ma) | Age as listed in reference | Dating Method | Age Interpret | Prioritized? | Sample Source | Sample Num | Run Num | Age from other Locality | Dated Mineral | Minerals explicitely stated as having this age | Age applies to these Elements | MinDat Locality ID | Dated Locality (Max Age) | Location as listed in reference | Reference | Reference DOI | Reference ID | Age Notes | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Jen_0000166 | 1.317 | 1.307 | 1.312±0.005 | Ar-Ar | middle age ashflow sheet | sanidine | 8YC-460A | Sanidine | 276572 | Island Park Area, Clark Co., Idaho, USA | Island Park area | Lanphere et al. (2002) | 10.1130/0016-7606(2002)114<0559:RAFTOT>2.0.CO;2 | GSAB114_559 | |||||||
| Jen_0000166a | 1.292 | 1.278 | 1.285±0.007 | Ar-Ar | middle age ashflow sheet | sanidine | 8YC-460A | Sanidine | 276572 | Island Park Area, Clark Co., Idaho, USA | Island Park area | Lanphere et al. (2002) | 10.1130/0016-7606(2002)114<0559:RAFTOT>2.0.CO;2 | GSAB114_559 |
All locality data graciously provided by mindat.org
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