Goosecreekite

Chemical formula: Ca(Si<sub>6</sub>Al<sub>2</sub>)O<sub>16</sub>·5H<sub>2</sub>O

Goosecreekite is a rare zeolite forming colorless or white, tabular crystals with a pearly or vitreous luster.

## Characteristics Goosecreekite is a hydrated calcium aluminosilicate belonging to the zeolite group. This mineral typically forms small, thin-tabular or bladed crystals, which often arrange themselves into fan-like, rosette-like, or spherical aggregates. Individual crystals are most often colorless or white, exhibiting a pearly luster on cleavage surfaces and a vitreous luster on other faces. ## Physical Properties Goosecreekite is characterized by a hardness of 4-4.5 on the Mohs scale. It is a relatively light mineral, with a density of approximately 2.21 g/cm³. It exhibits perfect cleavage in one direction, which is visible as a pearly luster on flat surfaces. Crystals are usually transparent to translucent. ## Colors and Varieties This mineral is typically colorless or white. No colored varieties or trade names are distinguished. ## History and Name Goosecreekite was first described in 1980 by Donald R. Peacor, Peter J. Dunn, Robert A. Gault, and William P. Richard. Its name comes from the type locality – the Goose Creek quarry in Loudoun County, Virginia, USA. ## Applications Due to its rarity and small crystal size, goosecreekite has no industrial applications. It is solely an object of interest for mineral collectors and scientists.

Properties

Mohs hardness
4-4.5
Luster
Pearly, Vitreous
Streak
White
Density
2.21
Cleavage
Perfect on {010}
Fracture
Uneven
Transparency
Transparent to translucent
Crystal system
Monoclinic

Diagnostic features

## Identification Goosecreekite can be identified by its characteristic, thin-tabular crystals, often forming fan-like or radial aggregates. A key feature is the pearly luster on cleavage surfaces and a vitreous luster on other faces. Its low hardness (approximately 4-4.5) is also helpful in identification. ## Distinguishing from Similar Minerals It can be confused with other zeolites of similar appearance, such as heulandite or scolecite. It is often distinguished from heulandite by its more radial or fan-like crystal arrangement. Prehnite, although forming similar aggregates, is much harder (6-6.5). Accurate differentiation often requires chemical or crystallographic analysis. ## Crystal Forms Crystals are typically thin-tabular, flattened parallel to the cleavage plane. They form fan-like, radial, rosette-like, or spherulitic aggregates, less commonly occurring as single, well-formed crystals.

Geological environment

## Genesis Goosecreekite is a secondary mineral, forming at low temperatures as a result of hydrothermal processes. It crystallizes in cavities and fissures of volcanic rocks, such as basalts and diabases, as well as in veins cutting gneisses and amphibolites. ## Mineral Associations It most often co-occurs with other zeolites, such as stilbite, heulandite, laumontite, and chabazite. It is also frequently accompanied by calcite, quartz, epidote, prehnite, datolite, and apophyllite. ## Localities The most important goosecreekite localities in the world include the type locality at Goose Creek quarry in Virginia (USA), as well as India, where some of the best specimens are found in the Pune and Nashik regions of Maharashtra state. Other known localities include Iceland, the Faroe Islands, Canada (Quebec), and Italy (Sardinia).

Rarity

Rare

For collectors

## Quality Criteria The most prized specimens by collectors are those with well-formed, sharp crystals creating aesthetic, fan-like or spherical aggregates. High transparency and clarity of crystals, as well as the absence of mechanical damage, are important. Contrast with a dark matrix rock (most often basalt) significantly enhances the visual appeal of the specimen. ## Popular Localities The most famous localities, providing the best quality goosecreekite specimens, are in India, particularly in the Pune and Nashik districts. Specimens from there are characterized by large, well-formed aggregates on a basalt matrix.

Care and storage

## Cleaning Goosecreekite specimens should be cleaned very carefully, using a soft brush to remove dust. If necessary, distilled water can be used, but prolonged soaking should be avoided. Always allow the specimen to dry completely at room temperature. ## What to Avoid As a zeolite, goosecreekite is sensitive to heat, which can cause the loss of water from its crystal structure and damage the specimen. Contact with acids and other chemicals should be avoided. It should not be cleaned in ultrasonic cleaners. It should be protected from direct sunlight, which can cause it to become brittle. ## Storage Goosecreekite is best stored in closed display boxes or cabinets, away from heat sources, dust, and sudden temperature changes. Due to its low hardness and perfect cleavage, it should be stored separately to avoid scratches and mechanical damage.

Sources

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