Common
Associations: |
Gaylussite,
Northupite, Trona, (Borax Lake, California, USA); Bradleyite,
Gaylussite, Northupite, Shortite, Trona (John Hay, Jr.
Well No. 1, Wyoming, USA). |
Pirssonite was named to honor Professor Louis Valentine Pirsson (1860–1919), American petrographer and mineralogist, Professor of Physical Geology at Yale University, New Haven, Connecticut, USA.
Pirssonite is one of several carbonate minerals that form in non-marine evaporite deposits. Other evaporite carbonates include Trona,
Gaylussite, Northupite, Nahcolite and Thermonatrite. Evaporite minerals are geologically important because they clearly are related to the environmental conditions that existed at the time of their deposition, namely arid. They also can
be easily recrystallized in laboratories in order to confirm their specific characteristics of formation.
Chemically, Pirssonite and Gaylussite differ only in their number of water molecules, yet their symmetries are quite different. This is an indication of a change in their respective crystal structures. The two are best distinguished by their crystal habits in which Pirssonite has a distinctive tabular diamond-shaped crystal form. Pirssonite can lose its water molecules
and specimens should be stored in a sealed container.
Distribution: in the USA, the type locality at Searles Lake, San Bernardino County, California; also in California at Borax Lake, Lake County, in Deep Spring Lake, Inyo County, and at Owens Lake, Mono County; in the John Hay, Jr. Well No. 1, about 30 km west of Green River, Sweetwater County, Wyoming. On the Arizaro, Pastos Grandes, and Pozuelos playas,
Salta Province, Argentina. From the Jequetepeque River Valley, northwest Peru. On the Otjiwalundo Salt Pan, about 400 km west-northwest of Otavi, Namibia. In the Beypazari Basin, Ankara, Turkey. On Mt. Kukisvumchorr, Khibiny massif, and Mt. Alluaiv, Lovozero massif, Kola Peninsula, Russia.
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