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. |
None | Oxalate | Quartz |
Quartz (*) | Weddellite (*) | Whewellite (*) |
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 |
---|---|---|---|---|---|---|---|
Quartz (*) | Quartz | SiO2 | 23 | 5.3 | 1 | 261721 | 61156 |
Weddellite (*) | Oxalate | Ca(C2O4)·2H2O | 23 | 5.3 | 1 | 261721 | 32 |
Whewellite (*) | Oxalate | Ca(C2O4)·H2O | 23 | 5.3 | 1 | 261721 | 66 |
Age ID | Locality Notes |
---|---|
Michelle_576 | The oxalate minerals are found in lake bottom sediments layered in Miocene basalt flows along the Columbia River in Oregon. Calcium and oxalic acid originates from fish bones and/or organic sediment. Mineralization occurs in jasper nodules known as "Biggs Jasper." The locality is in the west-central part of the Columbia River Basalt Plateau. |
Michelle_721 | The oxalate minerals are found in lake bottom sediments layered in Miocene basalt flows along the Columbia River in Oregon. Calcium and oxalic acid originates from fish bones and/or organic sediment. Mineralization occurs in jasper nodules known as "Biggs Jasper." The locality is in the west-central part of the Columbia River Basalt Plateau in Sherman County. |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Michelle_576 | 23 | 5.3 | Miocene | stratigraphy | Age of oxalate mineralization | Weddellite, Whewellite | 27363 | Biggs, Sherman Co., Oregon, USA | Biggs | Mandarino and Witt (1983) | CM21_503 | Mineralization occurs in Miocene basalt flows | |||||||||
Michelle_721 | 23 | 5.3 | Miocene | stratigraphy | Age of basalt | 27363 | Biggs, Sherman Co., Oregon, USA | Biggs | Mandarino and Witt (1983) | CM21_503 | Age of the Columbia River basalt flows that host the Biggs Jasper in Sherman County, Oregon. |
Sample | Source Locality | Reference URL |
---|---|---|
R050242 | Biggs, Sherman Co., Oregon, USA | https://rruff.info/R050242 |
All locality data graciously provided by mindat.org
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