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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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