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:Červená Vein, Rovnost Mine (Werner Mine), Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech RepublicOldest recorded age at locality: 543Youngest recorded age at locality: 0mindat Locality ID: 236802mindat URL:http://www.mindat.org/loc-236802.htmlTectonic Settings: Total number of sublocalities beneath "Červená Vein, Rovnost Mine (Werner Mine), Jáchymov, Karlovy Vary District, Karlovy Vary Region, Czech Republic": 0Total number of bottom-level sublocalities: 0Latitude: 50°22'55"NLongitude: 12°53'16"EDecimal Degree (lat, lon): 50.381944444444,12.887777777778
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: AsCaCuFeHKMgOSSiUVYElements from minerals reported directly at this locality: As Ca Cu Fe H K Mg O S Si U V Y Structural Groups for minerals in this locality:
Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall
Michelle_542
Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall
Michelle_543
Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall
Michelle_544
Cervená vein is at the level of the Daniel adit near the Rovnost shaft. This area was used for radon water storage for spa in Jáchymov, known as Step's springs, the leaking water from the vein structures and enriched in U-ore deposited on the footwalls provided very high activity. Primary ore veins cut metasedimentary rocks in the contact aureole of a Variscan granite pluton. Veins were deposited by mesothermal fluids. More than 420 minerals of primary and supergene origin are found at this locality. A tertiary basalt dyke cuts ore veins. Ore lens body is located on the hanging wall, with supergene mineralization deposited on the footwall
Age of recent supergene mineralization. The alteration association of the recent origin, resulting from the weathering and decomposition of the primary uranium minerals, occurring together with copper sulfides, in the old mining workings.