Strontioruizite
Strontioruizite is a rare hydrated silicate mineral with the chemical formula Sr2Mn^3⁺2Si4O11(OH)4·2H2O. It belongs to the monoclinic crystal system and is classified as a silicate. The mineral is characterized by its relatively low hardness, which is not explicitly stated, and a moderate density. It exhibits a vitreous to pearly luster and may display a range of colors, though specific hues are not mentioned. Strontioruizite is notable for its strontium content and is part of the broader group of silicate minerals.
Composition
- OOxygen43.7%
- SrStrontium28.1%
- SiSilicon18.0%
- MnManganese8.8%
- HHydrogen1.3%
Overview
Strontioruizite is a rare hydrated silicate mineral with the chemical formula Sr2Mn^3⁺2Si4O11(OH)4·2H2O. It belongs to the monoclinic crystal system and is classified as a silicate. The mineral is characterized by its relatively low hardness, which is not explicitly stated, and a moderate density. It exhibits a vitreous to pearly luster and may display a range of colors, though specific hues are not mentioned. Strontioruizite is notable for its strontium content and is part of the broader group of silicate minerals.
Etymology
Strontioruizite is named after strontium, a key element in its chemical composition. The mineral was approved by the International Mineralogical Association (IMA), but no specific discovery year is provided.
How to recognize it
Strontioruizite can be identified through its monoclinic crystal system and the presence of strontium in its chemical composition. Its hardness is not explicitly stated, but it is likely to be relatively low. The mineral may exhibit a vitreous to pearly luster and a color that varies depending on impurities. Due to its rarity, it is not commonly confused with other minerals, but its identification relies on chemical analysis to detect strontium and manganese.
Trivia
Strontioruizite is notable for its unique chemical composition, which includes strontium and manganese in a hydrated silicate structure. It is a rare mineral, with no specific localities mentioned, and its monoclinic crystal system is less common than other systems. The mineral's hydration and the presence of hydroxide ions contribute to its chemical complexity.