The Mineral MANGANBABINGTONITE
- Chemistry: Ca2(Mn, Fe)FeSi5O14(OH),Calcium Manganese Iron Silicate.
- Class: Silicates
- Subclass: Inosilicates
- Uses: Only as mineral specimens.
Manganbabingtonite is a rare relative to the more common, but still scarce,
The two minerals are part of a series.
A series occurs when two or more elements can substitute for each other without
much distortion to the crystal structure.
Manganbabingtonite is enrich in manganese, while babingtonite is enriched in iron.
Both minerals contain a certain percentage of iron and manganese.
Manganbabingtonite and babingtonite contain both divalent (+2) and
trivalent (+3) iron ions.
There is a difference in the size of these ions with the trivalent iron
being larger. In manganbabingtonite and babingtonite these ions are segregated
in the structure because of their differing sizes.The formula is written to
show this relationship.
The substitution of manganese only occurs with the divalent
irons, since they are of similar size.
The differing charges on the irons causes a very weak magnetism
that might turn the needle ofa compass. This can be very diagnostic
since these two minerals can appear very similar to many other black,
monoclinic, submetallic minerals.
The magnetic effect is greater in babingtonite because it has more divalent irons.
- Color is brown to black.
- Luster is vitreous, submetallic to dull.
- Transparency: Crystals are generally opaque but thin
crystals or splinters can be translucent.
- Crystal System is triclinic; bar 1
- Crystal Habits include short stocky prismatic crystalsor tabular to platy forms.
- Cleavage is good in one direction and perfect in another,
these are pinacoidal but are at near right angles to each other
giving the appearance of rectangular prisms.
- Fracture is uneven to subconchoidal.
- Hardness is 5.
- Specific Gravity is approximately 3.5 - 3.6 (somewhat above
average for translucent minerals)
- Streak is brown to gray.
- Other Characteristics: Sometimes very weakly magnetic.
- Associated Minerals are
- Notable Occurrences include Santa Teresa Mountains, Graham County,
Arizona, USA and Rudnyi Kaskad deposit, Sayan, Russia.
- Best Field Indicators are crystal habit, color, locality,
associations, cleavage and luster.