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    Minerals P-T

Psilomelane

Name

Psilomelane

Chemistry

Ba(Mn+2)(Mn+4)8O16(OH)4 Barium Manganese Oxide Hydroxide

Uses

an ore of manganese and as a mineral specimen

Color

Color is variable from iron-black to bluish black to steel gray

Hardness

5-5.6

Specific gravity

4.4-4.5

Crystals

Crystal Habits include massive, fibrous, botryoidal, columnar, stalactitic, concretionary, powdery and earthy.

Accompanied by:

Pyrolusite, hematite, quartz and other manganese minerals

Similar to:

Pyrolusite

Psilomelane, although not as common as pyrolusite, is still an important ore of manganese.

Manganese is a strategically valuable metal since it is an essential ingredient in steel and other alloys. The mining term "wad" is used to indicate ores that are a mixture of several manganese oxides such as psilomelane, pyrolusite and others that are difficult to distinguish.

Psilomelane is a mineral name that is losing its significance. Still in use around the world the name is applied to hydrated barium bearing manganese specimens. It is probably a mixture of several minerals but is composed mostly of the mineral Romanechite, Ba(Mn+2, Mn+4)5O10-H2O. The difficulty in distinguishing romanechite from other barium manganese oxides, is that they are probably mixed together in the same specimen,that  is why the name psilomelane is still in use.

Psilomelane is often banded with gray pyrolusite and the alternating layers make an attractive polished stone with bands of metallic gray and submetallic black.

 Psilomelane also forms tufts of hair-like aggregates that are similar to those produced by pyrolusite. However, the difference in luster between the two minerals is usually sufficient to distinguish them. Earthy specimens as well are difficult to differentiate since both minerals tend to have a dull luster when found in this habit. Fortunately pyrolusite's softness will give it away when it leaves marks on paper and fingers.

Streak is black or brownish black. 

Other Properties: sometimes banded with the mineral pyrolusite producing alternating bands of metallic gray and submetallic black.

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