Kononovite

kononovite

langbeinite

euchlorine

anglesite

Images

Formula: NaMg(SO4)F
Sulphate, tilasite group
Crystal System: Monoclinic
Specific gravity: 2.91 measured, 2.945 calculated
Hardness: 3
Streak: White
Colour: White
Solubility: Decomposes and partially dissolves in water at room temperature after several hours. In humid air kononovite slowly alters to uklonskovite
Environments

Fumeroles

Kononovite is a relatively new mineral, approved in 2013 and to date (December 2023) reported only from the type locality.

Localities

At the type locality, the Arsenatnaya fumarole, Second scoria cone, Northern Breakthrough, Great Fissure eruption, Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia, kononovite was found in a single specimen, 6 cm in size. This scoria cone's fumarole fields are still active, with gas temperatures up to 430oC. More than eighty different mineral species have been identified in this fumarole. Strongly mineralised areas in the southern part of Arsenatnaya occur at depths from 0.3 to 0.6 m below the surface. with temperatures varying from 360oC to 390oC. The major minerals of the sublimate incrustations in this zone are the sulphates langbeinite, aphthitalite, krasheninnikovite, anhydrite, euchlorine and vanthoffite, and the arsenates lammerite, johillerite, urusovite, tilasite and svabite, as well as hematite, tenorite, halite, fluorophlogopite, K-feldspar and fluoborite. Subordinate and rare minerals are paralammerite, alarsite, bradaczekite, ericlaxmanite, kozyrevskite, popovite, wulffite, alumoklyuchevskite, calciolangbeinite, arcanite, anglesite, palmierite, kononovite, shuvalovite, sylvite, fluorite, copper-bearing gahnite, corundum, zincite, chubarovite and flinteite.
Kononovite occurs as prismatic to thick tabular crystals up to 0.04 x 0.06 x 0.1 mm3. Sometimes they are isolated but typically form clusters or interrupted crusts, up to several square centimetres in area and up to 0.05 mm thick, overgrowing basalt scoria. The specimen conaining kononovite is a breccia-like aggregate of scoria pebbles cemented by crusts of kononovite with minor amounts of langbeinite, hematite, anglesite and euchlorine. (EJM 27.4.575-580).

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