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.
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.
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: AlAsAuBaCCaCuFeHKMgNaOPbSSiElements from minerals reported directly at this locality: Structural Groups for minerals in this locality:
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000216
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000217
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000218
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000219
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000220
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000221
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000222
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000223
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000224
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000225
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000226
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000227
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Giersdorf_00000228
Igneous intrusion that contact metamorphosed ore at the Channar mine,
Giersdorf_00000229
Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback
Michelle_300
Hosted in the Jeerinah Formation.Hillside west of new Channar conveyor line.
BIF overlying the Brockman BIF, part of the Hamersley group, ages of the felsic and mafic units in this stratigraphy are indistinguishable from each other, suggesting a contemporaneous formation time.
The window of Fe mineralization is between the ages of the Cheela Springs Basalt unit of the Lower Wyloo group, and the June Hills Volcanics unit in the Upper Wyloo group.