Mesolite

Cabinet No. 40

Mesolite

Chemical formula: Na₂Ca₂(Si₉Al₆)O₃₀ · 8H₂O

Mesolite is a mineral from the zeolite group, a hydrated sodium and calcium silicate, typically forming white or colorless crystals with a fibrous or radial habit.

Description

## Characteristics Mesolite is a hydrated sodium and calcium silicate, belonging to the zeolite group. It typically occurs as elongated, acicular, or fibrous crystals, often forming radial or sheaf-like aggregates. It can also occur in compact masses. Typical mesolite specimens are white, colorless, gray, or slightly yellowish, characterized by a vitreous or silky luster. ## Physical Properties The hardness of mesolite on the Mohs scale is 5. This mineral exhibits perfect cleavage in two directions, meaning it easily breaks along specific planes. Its streak is white, and its fracture is uneven or conchoidal. The density of mesolite is approximately 2.26 g/cm³. ## Colors and Varieties Mesolite most commonly occurs in white, colorless, gray, or yellowish hues. There are no specific commercial or color varieties. ## History and Name Mesolite was described in 1816. The name of the mineral comes from the Greek words "mesos" (middle) and "lithos" (stone), referring to its chemical composition, which is intermediate between natrolite and scolecite. ## Applications Mesolite has no significant industrial applications. It is primarily valued by mineral collectors due to its aesthetic crystalline forms and its belonging to the zeolite group.

Diagnostic features

## Identification Mesolite can be identified by its characteristic fibrous or acicular crystal habit, often forming radial aggregates. White, colorless, or gray color, combined with a vitreous or silky luster, is also a diagnostic feature. A hardness of 5 on the Mohs scale and perfect cleavage aid in identification. ## Distinguishing from Similar Minerals Mesolite is sometimes confused with other zeolites, such as natrolite and scolecite. It is distinguished from natrolite by its chemical composition (mesolite contains calcium, natrolite does not) and often more radial aggregates. It differs from scolecite by its crystallographic symmetry (mesolite is orthorhombic, scolecite is monoclinic) and the lack of scolecite's characteristic cleavage in one direction. ## Crystal Forms Mesolite most commonly forms elongated, acicular, or fibrous crystals, which often arrange into radial or sheaf-like aggregates. It can also occur in compact, granular masses or as coatings.

Geological environment

## Genesis Mesolite forms in low-temperature hydrothermal conditions, typically in gas vesicles in volcanic rocks such as basalts, andesites, and rhyolites. It also forms in fractures and veins in these rocks, often as a secondary product resulting from the alteration of primary minerals. ## Mineral Associations Mesolite often co-occurs with other zeolites, such as heulandite, stilbite, laumontite, natrolite, and scolecite. It can also be found in association with calcite, apophyllite, and chalcedony. ## Localities Known localities for mesolite include India (Deccan Traps, especially the Mumbai region), the Faroe Islands, Iceland, Scotland (Isle of Skye), the United States (Oregon, Washington), and Australia (Queensland).

Rarity

Common

Collector aspects

## Quality Criteria The most prized mesolite specimens are characterized by well-formed, long, acicular crystals, forming aesthetic, radial or sheaf-like aggregates. Color purity (white, colorless) and the absence of mechanical damage are also important. Specimens on matrix, especially with contrasting associated minerals, are particularly sought after. ## Popular Localities The most valued mesolite specimens come from India, especially from the Deccan region, where they occur in gas vesicles of basalts. Other popular localities include the Faroe Islands and Iceland.

Care and storage

## Cleaning Mesolite is a relatively delicate mineral, so it is best to clean it using a soft brush and lukewarm water. For more stubborn dirt, a mild soap can be used, followed by thorough rinsing of the specimen with distilled water to avoid deposits. ## What to Avoid Avoid using strong chemicals, acids, and bases, which can damage the mineral's surface. Mesolite is sensitive to high temperatures and sudden temperature changes, so it should not be exposed to direct heat sources. Prolonged exposure to intense sunlight can lead to color fading. Due to the water content in its structure, prolonged storage in a very low humidity environment should be avoided, as this can lead to dehydration and damage to the crystals. ## Storage Mesolite is best stored in closed display cases or boxes, away from dust and direct sunlight. Maintaining stable temperature and humidity is advisable. Delicate specimens, especially those with thin crystals, should be protected from mechanical damage by individual wrapping in soft material.