Steinmetzite

Chemical formula: Zn<sup>2+</sup><sub>2</sub>Fe<sup>3+</sup>(PO<sub>4</sub>)<sub>2</sub>(OH)·3H<sub>2</sub>O

Steinmetzite is a very rare hydrated zinc and iron phosphate, forming microscopic, bladed crystals of a yellowish-brown color.

## Characteristics Steinmetzite is an extremely rare mineral from the phosphate group, chemically classified as a hydrated zinc and iron phosphate. It occurs as very small, bladed or tabular crystals, which rarely exceed 0.2 mm in length. These crystals form small, radial aggregates or rosettes. Due to its microscopic size, its visual features are difficult to observe without specialized equipment. ## Physical Properties Steinmetzite crystals exhibit a vitreous luster. Hardness and density have not been precisely measured due to the small size of the samples. It is a transparent to translucent mineral. ## Colors and Varieties This mineral is characterized by a yellow to yellowish-brown color. No varieties have been distinguished. ## History and Name Steinmetzite was approved as a new mineral by the International Mineralogical Association (IMA) in 2022 (IMA2022-031). Its name honors Gerhard Steinmetz, a German mineral collector who found the type material. It was first described by I.E. Grey, A.R. Kampf, W.G. Mumme, C.M. MacRae, R.W. Gable, A.C. Willis, and A. Pring in a 2023 publication.

Properties

Luster
Vitreous
Streak
Light yellow
Cleavage
Good on {010}
Fracture
Uneven
Transparency
Transparent to translucent
Crystal system
Monoclinic

Diagnostic features

## Identification Identification of steinmetzite is only possible using advanced analytical methods, such as Raman spectroscopy or X-ray diffraction (XRD), due to its microscopic size and co-occurrence with other phosphates. Visually, it is characterized by yellowish-brown, bladed crystals forming small aggregates. ## Distinguishing from Similar Minerals It can be confused with other secondary zinc and iron phosphates, such as phosphophyllite, plimerite, or scholzite, with which it co-occurs. Definitive differentiation requires chemical and structural analysis. ## Crystal Forms It forms elongated, bladed crystals, flattened parallel to the {010} plane. These crystals combine into small, radial or rosette-like aggregates.

Geological environment

## Genesis Steinmetzite is a secondary mineral that forms as a result of oxidation processes in ore deposits. In its type locality (Cornelia mine), it formed in vugs in quartz, in the oxidation zone of polymetallic deposits. ## Mineral Associations This mineral occurs in association with other rare phosphates, such as plimerite, scholzite, tarbuttite, hopeite, as well as with quartz, tennantite-(Zn), and sphalerite. ## Localities The only confirmed occurrence of steinmetzite in the world is its type locality – the Cornelia mine, located near Hagendorf-Süd in Bavaria, Germany.

Rarity

Extremely rare

For collectors

## Quality Criteria As a "micromount" type mineral, the value of a specimen is primarily determined by the quality and abundance of crystals visible under the microscope. Specimens with well-formed, sharp crystals forming aesthetic, radial aggregates are most prized. Association with other rare phosphates is also important. ## Popular Localities The only source of specimens is the Cornelia mine in Hagendorf, Germany. Material from this locality is highly sought after by collectors specializing in systematic minerals and rare species.

Care and storage

## Cleaning Due to the extreme rarity and microscopic size of crystals embedded in the matrix, steinmetzite specimens should not be cleaned by any mechanical or chemical means. Only dust should be removed using compressed air (from a safe distance) or a soft brush. ## What to Avoid Contact with water, chemicals, ultrasound, and sudden temperature changes should be strictly avoided. The crystals are very fragile and susceptible to mechanical damage. ## Storage Specimens should be stored exclusively in specialized, sealed "micromount" boxes, protecting them from dust, moisture, and vibrations. Display is only possible under a microscope.

External references

Sources

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