Eckhardite

Cabinet No. 40

Eckhardite

Chemical formula: (Ca,Pb<sup>2+</sup>)Cu<sup>2+</sup>Te<sup>6+</sup>O<sub>5</sub>·H<sub>2</sub>O

Eckhardite is an extremely rare, hydrated copper, calcium, and lead tellurate, forming emerald-green, acicular crystals.

Description

## Characteristics Eckhardite is a hydrated tellurate containing copper, calcium, and lead. It forms very small, bladed or acicular crystals, most often occurring as radial or tangled aggregates. Its most distinctive feature is its intense, deep, emerald-green color. Specimens are typically transparent and exhibit a strong, vitreous luster, which gives them a vibrant appearance, even at small sizes. ## Physical Properties This mineral is characterized by a vitreous luster and is transparent. Its hardness and density have not yet been precisely measured, but based on similar tellurates, it can be assumed to be a relatively soft mineral. It possesses perfect cleavage in one direction. ## Colors and Varieties Eckhardite occurs exclusively in one characteristic color: deep, emerald-green. No color varieties or commercial names are known. ## History and Name The mineral was officially recognized by the International Mineralogical Association (IMA) in 2012. Its name honors Eckhard Stuart, a renowned Californian mineral collector who contributed significantly to the mineralogical research of the region. The discovery was made at the only known locality of this mineral in California. ## Applications Due to its extreme rarity and occurrence as microscopic crystals, eckhardite has no industrial applications. It is solely an object of scientific interest and a valuable acquisition for specialized collectors of rare minerals.

Diagnostic features

## Identification Key identifying features of eckhardite are its unique, emerald-green color, vitreous luster, and crystal habit – acicular or bladed, forming radial aggregates. Its extreme rarity and occurrence exclusively at its type locality are also important diagnostic clues. ## Distinguishing from Similar Minerals Eckhardite can be confused with other green secondary copper minerals, such as brochantite, which forms similar acicular crystals but usually has a slightly different hue and occurs in different associations. It is distinguished from malachite by its lack of reaction with acids. Definitive differentiation from other rare, green tellurates (e.g., from the emmonsite group) is almost exclusively possible using advanced analytical methods, such as X-ray diffraction (XRD). ## Crystal Forms Eckhardite crystals are elongated, acicular, or thinly bladed. They typically form small, radial aggregates resembling rosettes or chaotically tangled clusters on the host rock.

Geological environment

## Genesis Eckhardite is a secondary mineral that forms in the oxidation (weathering) zone of hydrothermal quartz veins rich in tellurium and gold. It results from complex chemical processes occurring under the influence of surface waters on primary telluride ores. ## Mineral Associations This mineral occurs in association with other rare tellurates and tellurites, such as thorneite, paratimroseite, and xocolatlite. It also co-occurs with cerussite, chlorargyrite, and native gold. ## Localities The only confirmed locality of eckhardite in the world is its type locality – the Otto Mountain area in San Bernardino County, California, USA.

Rarity

Extremely rare

Collector aspects

## Quality Criteria The quality of eckhardite specimens, which are typically microminerals, is assessed based on several criteria. Highly valued are rich clusters of well-formed, sharp, and undamaged crystals with an intense, emerald color. Additional value is added by aesthetic arrangement on a small rock matrix and the presence of other rare associated minerals. ## Popular Localities The only source of collector specimens is the type locality in California. Specimens from this location are highly sought after by collectors specializing in mineral systematics and in minerals from specific localities (so-called "locality collecting").

Care and storage

## Cleaning Eckhardite specimens should be cleaned with the utmost care, using only a soft brush to remove dust. If necessary, distilled water can be used, applied gently, and the specimen immediately dried with compressed air. Immersion in water should be avoided. ## What to Avoid As a likely soft and hydrated mineral, eckhardite is sensitive to mechanical damage, high temperatures (risk of dehydration), and all chemicals. Ultrasonic cleaners, acids, detergents, and solvents should be strictly avoided. It should be protected from prolonged exposure to strong sunlight. ## Storage The safest way to store eckhardite is in a sealed "micromount" box, which protects it from dust, mechanical damage, and sudden changes in humidity. It should be stored under stable room conditions.