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:Mountain Pass District, Clark Mts (Clark Mountain Range), San Bernardino Co., California, USAOldest recorded age at locality: 1563Youngest recorded age at locality: 1325mindat Locality ID: 64624mindat URL:http://www.mindat.org/loc-64624.htmlTectonic Settings: Total number of sublocalities beneath "Mountain Pass District, Clark Mts (Clark Mountain Range), San Bernardino Co., California, USA": 20Total number of bottom-level sublocalities: 18Number of Child Localities: 1Child Localities:Mountain PassLatitude: 35°28'53"NLongitude: 115°30'52"WDecimal Degree (lat, lon): 35.481388888889,-115.51444444444
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.
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: AlBaCCaCeCuFFeHKLaMgMoNaOPPbSSbSiSrThTiZrElements from minerals reported directly at this locality: Structural Groups for minerals in this locality:
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001042
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001043
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001044
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001045
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Jen_0001046
MAGMATIC STYLE: Irregular sheet, dykes and veins. ASSOCIATED SILICATE ROCKS: Potassic shonkinite, syenite, granite and fenite.
Michelle_0261_a
Sahamalite occurs in the Sulphide Queen Mine of the Mountain Pass Deposit, closely associated with parisite and bastnaesite (as described in reference).
Michelle_0262_b
Locality described as "Mountain Pass Carbonatite and Alkalic Igneous Rocks." Mountain Pass Carbonatite is one of the largest sources of REE in the world. The carbonatite intrudes into gneiss, containing REE, Au, Ag, Pb and baryte.
Michelle_0263_c
Locality described as "Mountain Pass Carbonatite and Alkalic Igneous Rocks." Mountain Pass Carbonatite is one of the largest sources of REE in the world. The carbonatite intrudes into gneiss, containing REE, Au, Ag, Pb and baryte.
Michelle_0264_d
Locality described as "Mountain Pass Carbonatite and Alkalic Igneous Rocks." Mountain Pass Carbonatite is one of the largest sources of REE in the world. The carbonatite intrudes into gneiss, containing REE, Au, Ag, Pb and baryte.
Michelle_0265_e
Locality described as "Mountain Pass Carbonatite and Alkalic Igneous Rocks." Mountain Pass Carbonatite is one of the largest sources of REE in the world. The carbonatite intrudes into gneiss, containing REE, Au, Ag, Pb and baryte.
Michelle_0266_f
Locality described as "Mountain Pass Carbonatite and Alkalic Igneous Rocks." Mountain Pass Carbonatite is one of the largest sources of REE in the world. The carbonatite intrudes into gneiss, containing REE, Au, Ag, Pb and baryte.
Age of carbonatite. Emplacement of carbonatite was the final event in the intrusion of the 1400 ma complex. Clear parisite coexists with younger bastnaesite in sample.
Age of syenite and granitic intrusion. According to field relationships, this is the second of three stages of intrusions. Ages from zircon are described as "highly discordant" and not made significantly older by abrasion techniques.