Mutinaite
Chemical formula: Na<sub>3</sub>Ca<sub>4</sub>Al<sub>11</sub>Si<sub>85</sub>O<sub>192</sub>·60H<sub>2</sub>O
Mutinaite is a very rare mineral from the zeolite group, forming colorless or white, microscopic crystals with a vitreous luster.
Properties
- Mohs hardness
- 5
- Luster
- Vitreous
- Streak
- White
- Density
- 2.21
- Cleavage
- Perfect on {100} and {010}
- Fracture
- Uneven
- Transparency
- Transparent to Translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Identification of mutinaite is possible almost exclusively using advanced laboratory methods, such as X-ray diffraction (XRD) and chemical analysis (EDS/WDS). Visually, as fine, colorless crystals in basaltic rock cavities, it is indistinguishable from many other zeolites. ## Distinguishing from similar minerals Mutinaite can be confused with many other zeolites found in similar environments, such as heulandite, clinoptilolite, mordenite, or epistilbite. Differentiation based on visual characteristics is impossible and requires specialized instrumental analysis. ## Crystal forms It forms very small, elongated crystals with a prismatic habit or flattened, tabular crystals. These crystals often combine into radial or spherulitic aggregates, filling small gas vesicles in volcanic rocks.
Geological environment
## Genesis Mutinaite is a secondary mineral of hydrothermal origin. It forms at low temperatures as a result of the alteration of volcanic rocks, mainly basalts. It crystallizes in gas vesicles and fractures, precipitating from aqueous solutions rich in silica, aluminum, sodium, and calcium. ## Mineral associations It most commonly co-occurs with other minerals from the zeolite group, such as mordenite, heulandite-Ca, dachiardite-Na, as well as with quartz (in the form of chalcedony) and calcite. ## Localities This is an extremely rare mineral. It has been identified in several locations worldwide. The type locality is a quarry near Antrim in Northern Ireland. Other confirmed occurrences include Mount Skeiðflöt in the Hvalfjörður valley in Iceland and Montecchio Maggiore in Italy.
Rarity
Extremely rare
For collectors
## Quality criteria As a micromineral, the collectible value of a specimen depends on the abundance of crystals on the rock matrix, their development, and the aesthetics of the entire cluster. Specimens with well-formed, radial aggregates that contrast with the color of the host rock are most prized. Association with other rare zeolites is also important. ## Popular localities The most well-known specimens, though still microscopic, come from the type locality in Antrim (Northern Ireland) and from Iceland. Specimens from these locations serve as a reference point for this mineral.
Care and storage
## Cleaning Specimens should only be cleaned with compressed air to remove dust. Due to the microscopic size of the crystals and their fragility, contact with water, brushes, or other mechanical tools should be avoided. ## What to avoid Avoid contact with all chemicals, acids, and detergents. As a zeolite, mutinaite is sensitive to temperature changes, which can lead to dehydration and destruction of the crystal structure. It should not be heated or exposed to direct sunlight. ## Storage Mutinaite specimens, typically microminerals, should be stored in specialized, sealed "micromount" boxes that protect them from dust, mechanical damage, and sudden changes in humidity.