Hydroscarbroite
Chemical formula: Al₁₄(CO₃)₃(OH)₃₆·nH₂O
Hydroscarbroite is a hydrated aluminum carbonate, occurring as soft, white masses with an earthy or chalky texture.
Properties
- Mohs hardness
- 2
- Luster
- Earthy
- Streak
- White
- Density
- 0
- Transparency
- Translucent
- Crystal system
- Triclinic
Diagnostic features
## Identification Hydroscarbroite can be identified by its characteristic chalk-like or clay-like appearance, very low hardness (scratches with a fingernail), and white color. It is very light and often adheres to the tongue due to its porosity. It reacts violently with hydrochloric acid, which is a key feature distinguishing it from visually similar clay minerals. ## Distinguishing from Similar Minerals It can be confused with kaolinite, halloysite, or other clay minerals. It is distinguished from them by its violent reaction with acids (a characteristic of carbonates). It differs from calcite or dolomite by its extremely low hardness and earthy appearance. ## Crystal Forms This mineral forms exclusively cryptocrystalline or earthy aggregates. It does not occur in the form of well-developed, macroscopically visible crystals. It is most commonly found as veins and fillings in rock fissures.
Geological environment
## Genesis Hydroscarbroite is a secondary mineral. It forms in the weathering zone as a result of carbonate-rich waters interacting with aluminum-rich rocks, such as alum shales or sandstones. It forms under low temperature and pressure conditions. ## Mineral Associations It co-occurs with minerals such as gibbsite, halloysite, and also with sulfates, e.g., gypsum. ## Localities The most important and classic occurrence is South Bay in Scarborough, North Yorkshire, England, where it was discovered. It is also known from several other localities worldwide, including the Czech Republic and Hungary, but it is a rare mineral everywhere.
Rarity
Very rare
For collectors
## Quality Criteria The quality of a hydroscarbroite specimen is primarily assessed based on the purity and abundance of the material. Thick, pure white veins and fillings contrasting with the host rock are most valued. Since it does not form crystals, their shape is not a criterion for evaluation. A well-documented locality is important, especially if it is the type locality (Scarborough). ## Popular Localities By far the most sought-after and classic specimens come from the type locality in Scarborough, England. Material from other places is mainly of interest to systematic collectors.
Care and storage
## Cleaning Hydroscarbroite specimens are extremely delicate, soft, and porous. They should not be cleaned wet, as they can absorb water and disintegrate. Dust can be removed very carefully with a soft brush or a stream of compressed air from a distance. ## What to Avoid Avoid contact with water and any chemicals, especially acids, with which it reacts violently. The mineral is very soft, susceptible to scratching and abrasion. It should be protected from shocks, drops, and pressure. ## Storage It is recommended to store specimens in closed, padded collector boxes to protect them from mechanical damage, dust, and moisture. Do not place other minerals on top of them.