Manganite is best known in aggregates of blocky and short prismatic crystals. Crystal aggregates are usually in disorganized clusters with the crystals coming out of all directions. Thick crystals are heavily striated lengthwise, and often exhibit curvature. Twinning, in both penetration twinning and contact twinning, is known. Additional habits include acicular, radiating, fibrous, plumose, mammilary, globular, grainy, and massive.
Transparency
Opaque
Specific Gravity
4.3 - 4.4
Luster
Submetallic
Cleavage
1,1
Fracture
Uneven
Tenacity
Brittle
In Group
Oxides; Hydroxides
Striking Features
Crystal habit, mode of occurrence, and streak
Environment
In low temperature hydrothermal replacement deposits, acid-rich bogs, and in manganese-rich hot springs.