Carlfriesite
Chemical formula: CaTe<sup>4+</sup><sub>2</sub>Te<sup>6+</sup>O<sub>8</sub>
Carlfriesite is a rare calcium tellurate, distinguished by its intense, canary-yellow color and occurrence as small, lustrous crystals.
Properties
- Mohs hardness
- 3.5
- Luster
- Adamantine to Resinous
- Streak
- Light yellow
- Density
- 5.51
- Cleavage
- Good on {010}
- Fracture
- Conchoidal
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Key features for identifying carlfriesite are its intense, canary-yellow color, strong, almost adamantine luster, and high density. Its occurrence in association with other rare tellurates in known localities (primarily Moctezuma, Mexico) is a strong diagnostic indicator. ## Distinguishing from Similar Minerals Carlfriesite can be confused with other yellow secondary tellurium minerals, such as tellurite, emmonsite, or paratellurite, which often co-occur with it. Distinguishing them "by hand" can be impossible and often requires chemical or crystallographic analysis. It is distinguished from much more common native sulfur by its much higher density and crystal habit. ## Crystal Forms Carlfriesite crystallizes in the monoclinic system. It forms small, well-developed crystals with a prismatic or tabular habit. It most often occurs as druzes covering the host rock or as granular aggregates in small fissures.
Geological environment
## Genesis Carlfriesite is a secondary mineral, formed in the oxidation zones of hydrothermal gold and tellurium deposits. It forms as a result of weathering and alteration of primary tellurides and native tellurium under the influence of oxygen-rich surface waters. ## Mineral Associations This mineral often occurs in association with other tellurates and tellurium oxides, such as tellurite, paratellurite, spiroffite, denningite, as well as with native tellurium, native gold, and quartz. ## Localities The most important and historical locality for carlfriesite, from which the world's best specimens originate, is the Moctezuma mine (also known as the Bambolla mine) in Moctezuma, Sonora, Mexico. This mineral has also been reported at the Emerald mine in Tombstone, Arizona, USA.
Rarity
Very rare
For collectors
## Quality Criteria The collector's value of carlfriesite depends on several factors. Specimens with rich, dense crystalline druzes of intense, pure yellow color are most highly prized. Crystal size is crucial – even those 1 mm in size are considered large. The sharpness and luster of the crystals, as well as their aesthetic placement on a small rock matrix, significantly increase the specimen's attractiveness. Associations with other rare tellurium minerals are also valuable. ## Popular Localities Virtually all carlfriesite specimens available on the collector's market come from a single location: the Moctezuma mine in Mexico. This is the classic locality for this mineral, which has provided reference materials for research and the most beautiful specimens.
Care and storage
## Cleaning Carlfriesite specimens should be cleaned with the utmost care. The safest method is to use a soft brush or a photographic air blower to remove dust. Due to its reactivity, contact with water should be avoided. If wet cleaning is absolutely necessary, use distilled water and immediately dry the specimen thoroughly. ## What to Avoid The mineral is soft (hardness 3.5), so it should be protected from contact with harder minerals that could scratch it. Absolutely avoid all chemicals, acids, detergents, and ultrasonic cleaners, which can permanently damage or destroy it. Store at a stable temperature, away from moisture. ## Storage The best way to store carlfriesite is to place it in a separate, padded "micromount" box to prevent abrasion and mechanical damage. Protect from dust and direct, prolonged exposure to sunlight.