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: AlBaCCaCeClFFeHKLiMgMnMoNaNbOPPbSSiSrTiYZnZrElements from minerals reported directly at this locality: Al Ca Fe Mg O Si Ti Y Zr Structural Groups for minerals in this locality:
MAGMATIC STYLE: Central, sub-volcanic sövite intrusion of about 1 km2, numerous alvikite dykes and lapillistone layers (at two localities) 1-1.5 m thick. Lapilli generally from 0.5 to 15 mm but small bombs reach a few centimetres. ASSOCIATED SILICATE ROCKS: Lavas and tuffs include limburgite, nephelinite, phonolite and leucite tephrite; dykes and larger intrusive bodies include shonkinite, bergalite, phonolite, monchiquite, essexite and theralite.
Jen_0000617
MAGMATIC STYLE: Central, sub-volcanic sövite intrusion of about 1 km2, numerous alvikite dykes and lapillistone layers (at two localities) 1-1.5 m thick. Lapilli generally from 0.5 to 15 mm but small bombs reach a few centimetres. ASSOCIATED SILICATE ROCKS: Lavas and tuffs include limburgite, nephelinite, phonolite and leucite tephrite; dykes and larger intrusive bodies include shonkinite, bergalite, phonolite, monchiquite, essexite and theralite.
Jen_0000618
MAGMATIC STYLE: Central, sub-volcanic sövite intrusion of about 1 km2, numerous alvikite dykes and lapillistone layers (at two localities) 1-1.5 m thick. Lapilli generally from 0.5 to 15 mm but small bombs reach a few centimetres. ASSOCIATED SILICATE ROCKS: Lavas and tuffs include limburgite, nephelinite, phonolite and leucite tephrite; dykes and larger intrusive bodies include shonkinite, bergalite, phonolite, monchiquite, essexite and theralite.
Jen_0000619
MAGMATIC STYLE: Central, sub-volcanic sövite intrusion of about 1 km2, numerous alvikite dykes and lapillistone layers (at two localities) 1-1.5 m thick. Lapilli generally from 0.5 to 15 mm but small bombs reach a few centimetres. ASSOCIATED SILICATE ROCKS: Lavas and tuffs include limburgite, nephelinite, phonolite and leucite tephrite; dykes and larger intrusive bodies include shonkinite, bergalite, phonolite, monchiquite, essexite and theralite.