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Garden Quartz

Pronounced: GAR-den KWORTS

Garden Quartz is a trade name for Quartz containing natural mineral inclusions that create landscape-like scenes, clouds, mossy patterns and colourful internal formations.

Formula: SiO₂Mohs hardness: 7System: Trigonal
Garden QuartzCW

Meet the crystal

About Garden Quartz

Garden Quartz is a popular trade name for clear to translucent Quartz containing naturally enclosed mineral inclusions that create miniature landscape-like patterns inside the crystal. These internal scenes may resemble moss, forests, clouds, earth, underwater gardens or distant landscapes, which is where the name Garden Quartz comes from. It is not a separate mineral species. The host mineral is Quartz. The inclusions can vary considerably from specimen to specimen and may include chlorite, hematite, iron oxides, clay minerals and other mineral material trapped during crystal growth. As Quartz continues to grow, earlier minerals, coatings or growth surfaces can become enclosed inside the crystal. This can produce layered scenes, clouds, plumes, phantoms and three-dimensional internal structures. The name Lodolite is also widely used for this material. Mindat treats Lodolite as an unofficial trade name for included Quartz, particularly material from Minas Gerais, Brazil. Because the inclusions differ between specimens, Garden Quartz should not be assumed to contain one specific inclusion mineral without examination or laboratory testing. Its highly individual internal patterns make Garden Quartz especially popular as polished points, spheres, cabochons, freeforms and collector specimens.

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Showing Science & Formation

Scientific passport

The mineral facts

Observable and measurable properties used to describe and identify this mineral.

Chemical formula
SiO₂
Mineral class
Silicate — Quartz
Crystal system
Trigonal
Mohs hardness
7
Lustre
Vitreous
Streak
White
Specific gravity
Approximately 2.65
Transparency
Transparent to translucent

Common colours

Clear, white, green, red, brown, yellow, orange and grey

Cleavage and fracture

No true cleavage; conchoidal fracture.

From the Earth

How it forms

The geological processes that create this crystal over time.

Formation

Its geological story

Garden Quartz forms when Quartz grows around and encloses earlier mineral material. Minerals such as chlorite, hematite, iron oxides or clay may coat an earlier crystal surface or occur within the mineral-rich fluid while Quartz is still growing. Later Quartz growth can completely surround these materials, preserving them inside the crystal as inclusions. Repeated interruptions and renewed crystal growth can also create phantom-like layers and complex three-dimensional internal scenes.

A closer look

Scientific notes

Garden Quartz is a trade name rather than a recognised mineral species. The host mineral is Quartz, while the visible internal inclusions may consist of several different minerals. Lodolite is another commercial name commonly used for included Quartz, particularly Brazilian material. Not every Garden Quartz specimen contains the same inclusions, so colour alone should not be used to identify the enclosed minerals. Some specimens also contain true phantom growth, where an earlier stage of the Quartz crystal is outlined by inclusions before later Quartz growth encloses it.

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