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MANGANITE , a See also: mineral consisting of hydrated manganese sesquioxide, Mn20a•H20,crystallizing in the orthorhombic See also: system and isomorphous with See also: diaspore and See also: gothite
.
Crystals are prismatic and deeply striated parallel to their length; they are often grouped together in bundles
.
The colour is dark See also: steel-See also: grey to iron-black, and the lustre brilliant and submetallic: the streak is dark reddish-See also: brown
.
The hardness is 4, and the specific
gravity 4.3
.
There is a perfect cleavage parallel to the brachypinacoid, and less perfect cleavage parallel to the prism faces m
.
Twinned crystals are not infrequent
.
The mineral contains 89'7% of manganese sesquioxide; it dissolves in hydrochloric acid with
See also: evolution of chlorine
.
The best crystallized specimens are those from See also: Ilfeld in the Harz, where the mineral occurs with See also: calcite and See also: barytes in See also: veins traversing porphyry
.
Crystals have also been found at See also: Ilmenau in Thuringia, Neukirch near Schlett-
stadt in See also: Alsace (" newkirkite "), Granam near Towie in See also: Aberdeenshire, Upton Pyne near Exeter and See also: Negaunee in Michigan
.
As an ore of manganese it is much less abundant than pyrolusite or See also: psilomelane
.
The name manganite was given by W
.
Haidinger in 1827: French authors adopt F
.
S . Beudant's name " acerdese," (Gr . &Keptrls, unprofitable) because the mineral is of little value forSee also: bleaching purposes as compared with pyrolusite
.
(L
.
J
.
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