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Where is Strawberry Quartz found?

Quartz (SiO2) with inclusions of goethite or hematite

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Strawberry Quartz occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.

Where to find Strawberry Quartz

Kazakhstan

Known for producing high-quality Strawberry Quartz with distinct red inclusions.

Russia (especially Karelia)

Sources of quartz with various iron oxide inclusions, sometimes marketed as Strawberry Quartz.

Brazil

A major global source of quartz, including varieties with iron oxide inclusions.

Mexico

Some localities produce quartz with hematite inclusions.

Madagascar

Known for various quartz varieties, including those with iron oxide inclusions.

Collecting tips

  1. Look for Hydrothermal Veins. Strawberry Quartz often forms in hydrothermal veins associated with igneous or metamorphic rocks. Search for areas with quartz outcrops and evidence of past fluid activity.
  2. Examine Rock Dumps and Mine Tailings. Old mine dumps, especially those from quartz or pegmatite mines, can be good places to find specimens that were overlooked.
  3. Check for Iron Staining. The presence of iron oxides (hematite, goethite) in the surrounding rock or soil can indicate conditions favorable for Strawberry Quartz formation.
  4. Use a Hand Lens. A hand lens (10x magnification) is essential to observe the characteristic inclusions that give Strawberry Quartz its appearance and to differentiate it from other pink or red minerals.
  5. Distinguish from Rose Quartz. Strawberry Quartz typically has visible, distinct inclusions, whereas the pink color of Rose Quartz is usually more uniform and caused by microscopic inclusions not individually discernible.

Quick Check

Color:
Pink to red with visible specks or needles
Luster:
Vitreous
Streak:
White (for the quartz matrix); inclusions may produce a reddish-brown streak if sufficient material is present and scratched on a harder surface, but this is not typical for identifying the quartz itself.

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