THE
MINERAL AJOITE
- Chemistry: (K, Na)Cu7Al(Si3O8)
3(OH)6 - 3H2O,
Hydrated Potassium Sodium Copper Aluminum Silicate Hydroxide
- Class: Silicates
- Subclass: Phyllosilicates?
- Uses: A very minor ore of copper and as mineral specimens.
- Specimens
Ajoite is an attractive copper silicate mineral that is named for its type locality in the Ajo District of Pima County,
Arizona.
It is a secondary mineral that forms from the oxidation
of other secondary copper minerals.
Ajoite forms excellent microcrystal specimens.
The small prismatic crystals are often arranged in tufts with an almost aquamarine-like blue green color.
It is associated with other rare and colorful minerals such as
shattuckite,
copper,
papagoite and
plancheite; which makes specimens even more attractive.
The color variety in a single multi-mineral specimen is sometimes surreal.
Massive samples of ajoite are also unique and are sometimes carved or tumbled and can be used as an ornamental stone.
Ajoite's classification as a phyllosilicate is questionable as its true structure is as yet unknown.
PHYSICAL CHARACTERISTICS:
- Color is blue-green to light green.
- Luster is dull to vitreous.
- Transparency specimens are transparent to translucent.
- Crystal System is triclinic, bar 1.
- Growth Habits include acicular to thin prismatic crystals often
found as spherules or sprays of acicular radial crystal clusters and as massive specimens.
- Cleavage is perfect.
- Hardness is 3.5.
- Specific Gravity is approximately 2.9 - 3.0 (average for non-metallic minerals).
- Streak is pale greenish white.
- Associated Minerals are quartz,
limonite,
mimetite,
phoenicochroite,
willemite,
wickenburgite,
shattuckite,
copper,
papagoite,
plancheite,
duftite
and other secondary copper minerals.
- Notable Occurrences are limited to the New Cornelia Mine, Ajo District, Pima County and Wickenburg, Maricopa County,
Arizona, USA and the Messina District, South Africa.
- Best Field Indicators are color, crystal habit, locality and associations.