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: AlAsAuBaCCaCsCuFeHKMgMnMoNaNbOPPbSSiSrTiUVYZnElements from minerals reported directly at this locality: Structural Groups for minerals in this locality:
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000811
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000812
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000813
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000814
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000815
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000816
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000817
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000818
The Nopal I deposit is part of a Basin and Range horst composed of Tertiary rhyolitic tufts underlain by carbonate sedimentary rocks as is Yucca Mountain (Mesozoic carbonates at Nopal, Paleozoic carbonates at Yucca Mountain). Further, both the proposed Yucca Mountain repository horizon and the Nopal I deposit are located in the oxidizing, hydrologically unsaturated zone 100 m or more above the water table. The locality is similar chemically to the Yucca Mountain locality and is studied due to the chemical environment being ideal to store nuclear waste.
Giersdorf_00000955
The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000955b
The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000956
The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000957
The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000958
The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000959
The Sierra Peña Blanca is located to the north of Aldama City (Chihuahua State). It corresponds to an uplifted faulted block about 80 km long and 15 to 20 km wide, of Mesozoic and Cenozoic rocks, surrounded by basins to the west and the east. The average elevation of the sierra is 1,800 m, whereas the basins are around 1,600 m and decrease gradually eastward. This sierra,as well as other sierras belonging to the Basin and Range system, presents a general northward strike, with a tilt to the west.
Giersdorf_00000960
The Nopal 1 Deposit is confined to a breccia zone or pipe, limited to by faults. The breccia pipe is 100m high x 20m x 40m wide. The deposit is found within the Nopal Rhyolite. Uranium minerals found in the deposit are primarily oxidized.
Giersdorf_00000961
The Las Margaritas Deposit is hosedted by the Escuadra Formation and is found on the axis of a tectonic valley.
Giersdorf_00000962
The Puerto 3 deposit is located to the northwest of the Las Margaritas deposit and is hosted by the Nopal Rhyolite overlain by the Escuadra Formation.
Age given for the Nopal rhyolite which underlies what was previously referred to as the Escuadra Formation. The two are occasionally separated by a thin layer of pumice, but together make up what is referred to as unit 2 in the literature.
Age given for what was previously referred to as the Escuadra formation, which overlies the Nopal Rhyolite. The two are occasionally separated by a thin layer of pumice, but together make up what is referred to as unit 2 in the literature.
After approximately a 6 Ma hiatus, which is generalized in all of the surrounding areas, volcanic activity started again and formed the top part of the Escuadra Formation.
The Nopal 1 Deposit is used to describe the formation age of other similar deposits found in the Sierra Peña Blanca area, and are all found within the Nopal Rhyolite.