Paralstonite is a rare mineral composed of arsenic, sulfur, and silver. Its spelling can be broken down phonetically as "pæɹəlstoʊnaɪt." The "p" sound is followed by the "æ" sound, as in "cat." The "ɹ" sound is pronounced with the tip of the tongue elevated and the lips slightly rounded. The "oʊ" sound is a diphthong that begins with an "o" sound and ends with an "ʊ" sound, as in "goose." The final "t" sound is pronounced with a sudden release of air from the top of the mouth.
Paralstonite is a mineral that belongs to the nitrate group. Its chemical composition is sodium alunite sulfate, with the formula Na2Al2(SO4)4·4H2O. It is typically found in volcanic environments, especially in fumaroles, which are openings that release volcanic gases. Paralstonite typically forms as a secondary mineral in altered volcanic rocks.
Paralstonite typically appears as colorless to white or yellowish crystals that have a vitreous to dull luster. These crystals are transparent to translucent, and they usually form in clusters or aggregates. The mineral has a monoclinic crystal system, with prismatic or tabular crystal shapes.
The physical properties of paralstonite include a hardness of 2.5 to 3 on the Mohs scale, which means it is relatively soft. It has an average specific gravity of 2.06, meaning it is slightly heavier than water. Paralstonite has a perfect cleavage in one direction, and its fracture is conchoidal, meaning it breaks with curved surfaces.
The name paralstonite is derived from "alstonite," which is a related mineral. Paralstonite is an isostructural polymorph of alstonite, meaning they have the same crystal structure but different chemical compositions. It is often associated with other minerals such as nitratine, halite, and sulfur. Paralstonite can be used as a significant source of sodium and sulfur in industrial processes, particularly in the production of fertilizer and various chemical compounds.