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Red Hematoid Quartz

Pronounced: RED hee-MAT-oyd KWORTS

Red Hematoid Quartz, often sold as Fire Quartz, is quartz coloured by natural iron-oxide inclusions, especially hematite. Its fiery red, rust, orange and crimson markings may form clouds, streaks, phantoms or dense internal zones within otherwise clear, milky or smoky quartz.

Formula: Quartz: SiO₂ Common inclusion: Hematite Fe₂O₃Mohs hardness: 7System: Trigonal
Red Hematoid QuartzCW

Meet the crystal

About Red Hematoid Quartz

Red Hematoid Quartz is a trade name for quartz containing visible iron-rich inclusions or colouring, most commonly hematite and sometimes goethite. The quartz itself remains silicon dioxide, but iron oxides introduced during or between stages of crystal growth can create colours ranging from pale rusty orange through brick red, deep crimson and reddish brown. In some specimens, the iron minerals occur as tiny internal particles or plates; in others they form coatings along growth zones, fractures or crystal surfaces. Some particularly attractive specimens display red hematite “phantoms”, where an earlier stage of quartz growth was coated with hematite before later clear quartz continued growing around it. This preserves a ghost-like outline of the earlier crystal inside the later one. Hematite-included quartz from the Orange River region of southern Africa is especially well known for vivid internal red phantoms. The commercial name Fire Quartz refers to the fiery appearance rather than a separate mineral species

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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
Quartz: SiO₂ Common inclusion: Hematite Fe₂O₃
Mineral class
Oxide — Quartz with iron-oxide inclusions
Crystal system
Trigonal
Mohs hardness
7
Lustre
Vitreous; iron-rich coatings or inclusions may appear earthy to metallic
Streak
Quartz: white Hematite: typically reddish brown
Specific gravity
Approximately 2.65 for quartz; heavily included specimens may be slightly higher
Transparency
Transparent to translucent, sometimes nearly opaque where iron-oxide inclusions are dense

Common colours

Colourless, white, smoky or pale quartz with red, orange, rust, brown, crimson or brick-red inclusions and zoning

Cleavage and fracture

Poor to indistinct cleavage; typically conchoidal fracture

From the Earth

How it forms

The geological processes that create this crystal over time.

Formation

Its geological story

Red Hematoid Quartz forms when quartz crystallises in an environment containing iron-rich fluids or minerals. Quartz may begin growing normally from silica-rich hydrothermal fluids. If iron becomes available during growth, hematite or other iron oxides can crystallise within the quartz, coat an existing growth surface or settle along microscopic zones. If quartz growth later resumes, these iron-rich layers can become enclosed inside the crystal. This produces internal clouds, streaks, platelets or clearly defined phantom structures. In other specimens, iron oxides may be introduced later along fractures or external surfaces. This is why not every red-coloured quartz specimen has exactly the same internal structure. Mindat specifically distinguishes true hematite-included quartz from quartz merely stained by later hematite deposition.

A closer look

Scientific notes

Red Hematoid Quartz is not a formally recognised mineral species. It is quartz whose red appearance comes from iron-rich material, especially hematite and sometimes goethite. The appearance can vary dramatically depending on when the iron minerals formed. Hematite may occur as microscopic particles, thin plates, coatings or dense masses. Some specimens from the Orange River region preserve repeated stages of quartz growth as vivid red hematite phantoms. Each phantom can record an interruption in quartz growth, deposition of hematite and later renewed quartz growth. Mindat Mindat also documents intensely red Ferruginous Quartz from Tinejdad, Morocco, in which the quartz is coloured almost completely by iron-oxide inclusions.

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