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:La Creusa U Prospect (La Creusaz U Prospect), Les Marécottes, Le Trient Valley, Valais, SwitzerlandOldest recorded age at locality: 298.9Youngest recorded age at locality: 0mindat Locality ID: 23617mindat URL:http://www.mindat.org/loc-23617.htmlTectonic Settings: Total number of sublocalities beneath "La Creusa U Prospect (La Creusaz U Prospect), Les Marécottes, Le Trient Valley, Valais, Switzerland": 0Total number of bottom-level sublocalities: 0Latitude: 46°7'11"NLongitude: 7°0'5"EDecimal Degree (lat, lon): 46.119722222222,7.0013888888889
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: AgAlAsBaBiCCaCeCuFFeHKMgNaNdOPPbSSeSiTiUVWZnElements from minerals reported directly at this locality: Ag Al As Ba Bi C Ca Ce Cu F Fe H K Mg Na Nd O P Pb S Se Si Ti U V W Zn Structural Groups for minerals in this locality:
Age of ice-sheet melting event which caused rapid weathering, rapid decompression, uplift, and erosion. Oxidation of pyrite and arsenopyrite produced an acid that interacted with the uraninite and led to the formation of a complex assemblage of Uranyl-bearing minerals.
Since the end of the underground exploration in 1981, exposed veins and stockpiled U ore have been subjected to acid mine drainage water and atmospheric oxygen in the abandoned galleries. Oxidation of the sulfides (mainly pyrite and chalcopyrite) in the presence of strong bacterial activity resulted in the production of acid (pH ~ 3.1), sulfate-rich waters. These waters reacted with uraninite, clinochlore, illite, calcite, and siderite to form a rich assemblage of neoformed uranyl minerals, including the new minerals marécottite Mg3(UO2)8(SO4)4O6(OH)2·28H2O (Brugger et al. 2003a) and pseudojohannite Cu5(UO2)6(SO4)3(OH)16·14H2O (Brugger et al. 2006b), as well as jáchymovite (UO2)(SO4)(OH)14·13H2O, johannite Cu(UO2)2(SO4)2(OH)2·8H2O, magnesiozippeite Mg(UO2)2(SO4)O2·3.5H2O, natrozippeite Na(UO2)2(SO4) O(OH)·2H2O, rabejacite Ca(UO2)4(SO4)2(OH)6·6H2O, schoepite (UO2)8O2(OH)12·12H2O, schröckingerite NaCa3(UO2) (CO3)3(SO4)F·10H2O, uranopilite (UO2)6(SO4)(OH)10·12H2O, zippeite K(UO2)2(SO4)O(OH)·2H2O, and an unnamed Al-equivalent of coconinoite Al4(UO2)2(PO4)4(SO4)(OH)2·20H2O.
Sample
Source Locality
Reference URL
R070057
La Creusa U Prospect (La Creusaz U Prospect), Les Marécottes, Le Trient Valley, Valais, Switzerland