Joteite
Chemical formula: Ca<sub>2</sub>Cu<sup>2+</sup>Al(As<sup>5+</sup>O<sub>4</sub>)[As<sup>5+</sup>O<sub>3</sub>(OH)]<sub>2</sub>(OH)<sub>2</sub>·5H<sub>2</sub>O
Joteite is a very rare, blue-green calcium, copper, and aluminum arsenate, forming microscopic, tabular crystals.
Properties
- Mohs hardness
- 3
- Luster
- Vitreous
- Streak
- Pale blue-green
- Density
- 3.19
- Cleavage
- Perfect on {001}
- Fracture
- Brittle
- Transparency
- Translucent
- Crystal system
- Triclinic
Diagnostic features
## Identification Identification of joteite is possible almost exclusively through advanced analytical methods, such as Raman spectroscopy, X-ray diffraction (XRD), and chemical analysis (EDS/WDS). In collector's conditions, recognition is based on its characteristic blue-green color, the form of microscopic, tabular crystals forming rosette-like aggregates, and knowledge of the locality (Jote mine). ## Differentiation from Similar Minerals Joteite can be confused with other secondary copper and arsenic minerals of similar color, such as olivenite, conichalcite, or agardite. Differentiation requires specialized studies, as joteite is the only known arsenate containing calcium, copper, and aluminum simultaneously. Chemical analysis of the elemental composition is crucial. ## Crystal Forms Joteite crystallizes as very thin, tabular crystals, flattened parallel to the {001} plane. These crystals combine into characteristic, rosette-like or radial aggregates, and also form small, spherical clusters.
Geological environment
## Genesis Joteite is a secondary mineral, forming in the oxidation zones (gossans) of polymetallic deposits rich in arsenic and copper, under desert climate conditions. It forms as a result of the alteration of primary ore minerals, such as enargite. ## Mineral Associations This mineral occurs in association with other rare secondary minerals. At its type locality (Jote mine), it was found in association with quartz, barite, jarosite, alunite, chalcanthite, antlerite, brochantite, atacamite, as well as other arsenates such as chenevixite, scorodite, mansfieldite, lavendulan, and pushcharovskite. ## Localities The only confirmed occurrence of joteite in the world is its type locality – the Jote mine, located approximately 35 km south of the city of Copiapó in the Atacama region, northern Chile.
Rarity
Extremely rare
For collectors
## Quality Criteria As a microscopic mineral, joteite is primarily valued by collectors specializing in "micromount" specimens. The most highly prized specimens are those that display well-formed, undamaged, rosette-like crystal aggregates of intense, blue-green color. Contrast with the rock matrix and the richness of association with other rare minerals are also important. ## Popular Localities The only source of joteite specimens is the Jote mine in Chile. Material from this locality is extremely rare on the collector's market.
Care and storage
## Cleaning Joteite specimens are extremely delicate and usually consist of microscopic crystals on a rock matrix. Mechanical or chemical cleaning is not recommended. Any attempts at cleaning may irreversibly destroy the fragile structure of the aggregates. It is safest to leave the specimen in its untouched state. ## What to Avoid Contact with water, acids, bases, and other chemicals should be strictly avoided. The mineral is sensitive to changes in temperature and humidity. It should not be heated or exposed to direct sunlight. Vibrations and impacts can cause the delicate aggregates to disintegrate. ## Storage Joteite specimens should be stored in stable conditions, preferably in closed, padded "micromount" boxes that protect against dust, humidity, and mechanical damage. Display should be in sealed display cases, away from sources of heat and light.