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:Cottonwood Mts, Panamint Mts (Panamint Range), Inyo Co., California, USAOldest recorded age at locality: 230.4Youngest recorded age at locality: 3.5mindat Locality ID: 254543mindat URL:http://www.mindat.org/loc-254543.htmlTectonic Settings: Total number of sublocalities beneath "Cottonwood Mts, Panamint Mts (Panamint Range), Inyo Co., California, USA": 128Total number of bottom-level sublocalities: 111Number of Child Localities: 4Child Localities:Goldbelt DistrictPanamint ButteQuartz Spring DistrictUbehebe DistrictLatitude: 36°34'58"NLongitude: 117°27'11"WDecimal Degree (lat, lon): 36.582777777778,-117.45305555556
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: AgAlAsAuBaCCaClCrCuFFeHKMgMnMoNaOPbSSbSiVWZnElements from minerals reported directly at this locality: Structural Groups for minerals in this locality:
Ubehebe Peak is a quartz monzonite intrusion in the Last Chance Mountains of Death Valley National Monument. The host rock are steeply dipping Ordovician and Pennslyvanian strata.
Michelle_393
Hunter Mountain batholith is a quartz monzonite intrusion. Shirley Ann Claim is a metamorphosed, heavily faulted, oxidized Pb-Cu deposit occurs in the contact of the Perdido Formation (interbedded limestone) and Hunter Mountain.
Age of Hunter Mountain Batholith intrusion. Shirley Ann Claim formed with the introduction of the Hunter Mountain batholith in contact with the Mississippian aged Perdido Formation.
Age of quartz monzonite intrusion and introduction of magmatic fluids.
Sample
Source Locality
Reference URL
R060055
Shirley Ann Group (Shirley Ann Claim; Dodd Springs; Trail; Eureka; Sal; June; Bee Em Tee), Big Dodd Spring, Ubehebe District, Cottonwood Mts, Panamint Mts (Panamint Range), Inyo Co., California, USA