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It is a yellow mineral crystallizing in the orthorhombic system.
Its β-isoform crystallizes into an orthorhombic system with the space group.
It crystallizes in the orthorhombic system with a space group of Pcab.
A wedge-shaped crystal form of the tetragonal or orthorhombic system.
It forms lustrous black crystals in the orthorhombic system.
Witherite crystallizes in the orthorhombic system and virtually always is twinned.
It forms white, yellow to brown crystals in the orthorhombic system which occur often as a druzey encrustation.
Kremersite is a brown-red to orange mineral that crystallizes in the orthorhombic system.
Cerussite crystallizes in the orthorhombic system and is isomorphous with aragonite.
It crystallizes in the orthorhombic system and typically occurs as earthy to fibrous masses.
Autunite crystallizes in the orthorhombic system and often occurs as tabular square crystals.
Crystals of perovskite appear as cubes, but are pseudocubic and crystallize in the orthorhombic system.
It crystallizes in the orthorhombic system in translucent yellow to yellow green masses.
It crystallizes in the orthorhombic system typically forming as stalactitic masses exhibiting good cleavage.
Otwayite is green, with a hardness of 4, a specific gravity of 3.4, and crystallises in the orthorhombic system.
Macdonaldite crystallises in the orthorhombic system.
Hopeite crystallizes in the orthorhombic system with prismatic, vitreous white to yellow crystals.
Teallite forms soft silvery grey mica-like plates and crystallizes in the orthorhombic system.
Orthorhombic system (orthorhombic or lozenge-shaped) The three axes of different length are at right angles to each other.
It forms coatings and radial aggregates of soft yellow needles which crystallize in the orthorhombic system.
Ilvaite crystallizes in the orthorhombic system in black prismatic crystals and columnar masses.
In the monoclinic system, the crystal is described by vectors of unequal lengths, as in the orthorhombic system.
It crystallizes in the orthorhombic system and forms translucent bright blue acicular crystal clusters or drusey coatings.
Lithiophylite is a resinous reddish to yellowish brown mineral crystallizing in the orthorhombic system often as slender prisms.
Topaz crystallizes in the orthorhombic system, and its crystals are mostly prismatic terminated by pyramidal and other faces.