Greenlizardite

greenlizardite

ammoniozippeite

boussingaultite

oppenheimerite

Images

Formula: (NH4)Na(UO2)2(SO4)2(OH)2.4H2O
Valence: (N3-H4)Na(U6+O2)2(SO4)2(OH)2.4H2O
Hydrated uranyl sulphate
Crystal System: Triclinic
Specific gravity: 3.469 calculated
Hardness: 2
Streak: White
Colour: Light green-yellow
Luminescence: Fluoresces greenish-blue in 405 nm laser light
Solubility: Easily soluble in water at room temperature
RADIOACTIVE
Environments

Sedimentary environments
Hydrothermal environments

Greenlizardite is a relatively new mineral, approved in 2017 and to date (June 2026) reported only from the type locality. Localities

At the type locality, the Green Lizard Mine, Red Canyon Mining District, San Juan County, Utah, USA, greenlizardite occurs as a secondary alteration phase, forming light green-yellow blades up to about 0.3 mm long, vitreous and transparent with a white streak (MM 82.2.401–411).
It occurs on the walls of mines in uranium-vanadium deposits that replaced wood and other organic material in sandstones and conglomerate (roll-front type U-V deposits). Associated minerals include ammoniozippeite, boussingaultite, dickite, beshtauite, calcite, gypsum, fermiite, johannite, natrozippeite, oppenheimerite, plášilite, rozenite, shumwayite, sulphur and wetherillite (HOM).
Greenlizardite from the Green Lizard Mine - Image

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