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Red Jasper with Quartz

Sedimentary/Metamorphic (Jasper is typically sedimentary, but can undergo low-grade metamorphism)

SiO2 (Jasper is a variety of Chalcedony, a microcrystalline Quartz)

Also known as: Jasper-Quartz

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Description

Red Jasper with Quartz refers to a material where the opaque, typically brick-red to brownish-red microcrystalline quartz (jasper) is intimately associated with or contains visible macroscopic crystals or veins of translucent to transparent quartz. Jasper itself is a cryptocrystalline variety of quartz (SiO2), characterized by its granular structure and often vibrant, opaque colors. The presence of larger quartz crystals or veins can add textural and visual interest, sometimes forming distinct patterns within the jasper matrix. The red coloration is imparted by iron oxides, predominantly hematite (Fe2O3), which are finely dispersed throughout the silica matrix.

How to Identify

Color
Opaque brick-red, brownish-red, or deep red, often with white, gray, or clear streaks/patches of macroscopic quartz.
Luster
Dull to vitreous (glassy) on fractured surfaces for jasper; vitreous for macroscopic quartz.
Texture
Smooth to slightly granular, often with a waxy feel for jasper. Macroscopic quartz will feel harder and more crystalline.
Crystal Form
Jasper is cryptocrystalline, meaning its crystals are too small to be seen without high magnification. Macroscopic quartz, if present, will exhibit hexagonal prismatic crystals with pyramidal terminations, or massive granular aggregates.
Cleavage
None. Jasper and quartz both exhibit conchoidal fracture.
Geological Environment
Found in association with volcanic rocks, hydrothermal veins, sedimentary deposits (e.g., banded iron formations), and as secondary infillings in various rock types.

Key Facts

  • Hardness: 6.5-7 on the Mohs scale (for both jasper and quartz).
  • Specific Gravity: 2.58-2.64 g/cm³.
  • Crystal System: Trigonal (for both microcrystalline jasper and macroscopic quartz).
  • Color: Opaque brick-red to deep red, often with clear, white, or gray quartz.
  • Luster: Dull to waxy for jasper; vitreous for macroscopic quartz.
  • Transparency: Opaque (jasper); Transparent to translucent (macroscopic quartz).
  • Fracture: Conchoidal to splintery.
  • Cleavage: None.
  • Composition: Silicon dioxide (SiO2) with iron oxide (hematite, Fe2O3) inclusions for red color.

Quick Check

  • Color: Opaque red with potential clear/white/gray quartz inclusions.
  • Luster: Dull to waxy for jasper, vitreous for quartz.
  • Streak: White (for both jasper and quartz).

Physical Characteristics

  • Crystal Habit: Jasper: Massive, nodular, botryoidal, or as vein fillings. Macroscopic Quartz: Prismatic, massive, granular.
  • Cleavage Type: None.
  • Fracture Type: Conchoidal to splintery.
  • Tenacity: Brittle.
  • Luster Type: Jasper: Dull, waxy, or greasy. Macroscopic Quartz: Vitreous.

Formation

Red Jasper forms primarily as a chemical sedimentary rock, often precipitated from silica-rich hydrothermal fluids or as a replacement of other minerals. The red color is due to finely disseminated hematite (Fe2O3) inclusions. It can also form in volcanic environments as a secondary mineral filling vesicles or fractures. The 'with Quartz' aspect refers to either macroscopic quartz veins or crystals intergrown with the jasper, or simply the inherent microcrystalline quartz nature of jasper itself.

Usage

Primarily used as an ornamental stone, for cabochons, beads, carvings, and decorative objects. Historically, it was used for tools and weapons due to its conchoidal fracture. It is also collected by mineral enthusiasts.

Age Distribution

Found in geological formations ranging from Precambrian to Cenozoic, depending on the specific deposit.

Where to Find

United States

Oregon (Biggs Jasper), California, Idaho, Arizona, Washington, Wyoming (various jasper types).

India

Known for various types of jasper, including red varieties.

Australia

Pilbara region (Banded Iron Formations containing jasper).

Brazil

Various localities for chalcedony and jasper.

Madagascar

Known for diverse ornamental stones, including jasper.

Russia

Ural Mountains (Orsk Jasper, often red).

Finding Tips

Look in areas with volcanic activity or sedimentary deposits

Jasper often forms in association with volcanic rocks or in sedimentary environments where silica-rich fluids were present.

Check stream beds and gravel pits

Jasper is very hard and resistant to weathering, so it can be found as pebbles and cobbles in alluvial deposits.

Examine exposed rock faces

Look for veins, nodules, or massive beds of red, opaque material, especially where there are visible crystalline quartz inclusions or veins.

Use a hardness test

Jasper and quartz are both hard (Mohs 6.5-7), so they will scratch glass and steel. This helps differentiate them from softer red minerals.

Similar Rocks

Chert

SiO2

Also known as: Flint (a variety of chert)

Agate

SiO2

Also known as: Banded Chalcedony

Carnelian

SiO2

Also known as: Red Chalcedony

Sard

SiO2

Also known as: Brownish-red Chalcedony

Scientific Classification

Mineral Class
Silicates (Tectosilicates)
Group
Quartz Group
Crystal System
Trigonal
Chemical Formula
SiO2
Composition
Silicon dioxide with trace impurities, primarily iron oxides (hematite) for red jasper.

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