Kamchatkite
Chemical formula: KCu²⁺₃O(S⁶⁺O₄)₂Cl
Kamchatkite is a rare potassium and copper sulfate, forming characteristic, tabular crystals of an intense brown color.
Properties
- Mohs hardness
- 3.5
- Color
- Greenish-yellowish brown
- Luster
- Vitreous to Sub-Metallic
- Streak
- Yellow
- Density
- 3.48
- Cleavage
- {011} and {100}
- Fracture
- Uneven
- Transparency
- Transparent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Key diagnostic features of kamchatkite include its tabular crystal habit, often forming radial aggregates, intense brown color, and strong, almost metallic luster. Its origin is also characteristic – it occurs exclusively in products of volcanic activity (fumaroles). ## Distinguishing from Similar Minerals Melanothallite is a mineral with a similar color and genesis, but it crystallizes in the orthorhombic system and forms different crystal shapes. Tenorite (copper oxide) also occurs in fumaroles, but it is black and has a different structure. Reaction to water (solubility) is also a distinguishing feature from most similarly looking minerals. ## Crystal Forms Kamchatkite forms thin, tabular or bladed crystals, elongated in one direction. These crystals often combine into fan-shaped, radial, or star-shaped aggregates, and also form druzes and crusts on volcanic rocks.
Geological environment
## Genesis Kamchatkite is a mineral of volcanic origin. It forms through sublimation from hot gases (exhalations) in fumaroles, which are vents through which gases and water vapor escape from the Earth's interior. It crystallizes directly on the surface of volcanic rocks at temperatures of about 400-600°C. ## Mineral Associations This mineral co-occurs with other rare volcanic fumarole minerals, such as tenorite, hematite, tolbachite, ponomarevite, piipite, fedotovite, atlasovite, alarsite, as well as halite and sylvite. ## Localities The only confirmed and most important locality for kamchatkite in the world is its type locality – the fumaroles of the Second Cinder Cone of the Northern Breakthrough of the Great Fissure Eruption of Tolbachik volcano on Kamchatka, Russia.
Rarity
Very rare
For collectors
## Quality Criteria The most prized kamchatkite specimens are those with well-formed, sharp crystals with a strong luster, forming aesthetic, radial or fan-shaped aggregates. Contrast with a light matrix significantly enhances the specimen's attractiveness. The size of aggregates and individual crystals is also an important factor influencing value. ## Popular Localities The only source of collectible specimens is the Tolbachik volcanic complex on Kamchatka. Specimens from historical or more recent eruptions from this locality are highly sought after by collectors specializing in volcanic minerals and systematics.
Care and storage
## Cleaning Kamchatkite specimens should only be cleaned mechanically, using a very soft brush or compressed air to remove dust. Any contact with water and other liquids should be avoided, as the mineral is water-soluble. ## What to Avoid Absolutely avoid contact with water, acids, and other chemicals. It should be protected from humid air, which can cause its slow degradation. It should not be heated or exposed to sudden temperature changes. ## Storage Kamchatkite specimens require storage in dry conditions. It is best to keep them in tightly sealed containers (e.g., "membrane boxes" or sealed boxes) with a desiccant, such as silica gel. Display should be in closed, airtight display cases.