Got a photo? Identify rocks instantly with the Rockby app
Open the appDescription
Quartz with mica refers to a rock or mineral assemblage where quartz (silicon dioxide) is a primary component, and one or more minerals from the mica group are also present. The proportion of quartz to mica can vary significantly, leading to different rock classifications. Quartz provides hardness and resistance, while mica imparts a characteristic platy or flaky texture and often a silvery, golden, or dark sheen. The presence of mica often gives the rock a foliated or schistose texture.
How to Identify
- Color
- Variable. Quartz is typically colorless, white, or gray. Mica can be silvery (muscovite), golden (phlogopite), or black (biotite). The overall rock color will be a combination, often light to dark gray, silvery, or brownish.
- Luster
- Vitreous (glassy) for quartz, pearly to sub-metallic for mica.
- Texture
- Granoblastic (interlocking grains) for quartz, with a distinct foliation or schistosity due to the parallel alignment of mica flakes. Can range from fine-grained to coarse-grained.
- Crystal Form
- Quartz crystals are typically anhedral (irregularly shaped) in metamorphic rocks, but can be euhedral (well-formed hexagonal prisms) in vugs or pegmatites. Mica forms platy, tabular, or flaky crystals.
- Cleavage
- Quartz has no true cleavage but exhibits conchoidal fracture. Mica has perfect basal cleavage (one direction), allowing it to split into thin, flexible sheets.
- Geological Environment
- Common in regional metamorphic terrains (e.g., mountain belts), contact metamorphic aureoles, and some igneous intrusions (granites, pegmatites).
Key Facts
- Hardness: Quartz: 7 (Mohs); Mica: 2-3 (Mohs)
- Specific Gravity: Quartz: 2.65 g/cm³; Mica: 2.7-3.3 g/cm³
- Crystal System: Quartz: Trigonal; Mica: Monoclinic
- Color: Colorless, white, gray (quartz); Silvery, golden, black, brown (mica)
- Luster: Vitreous (quartz); Pearly to sub-metallic (mica)
- Transparency: Transparent to translucent (quartz); Transparent to opaque (mica)
- Fracture: Conchoidal (quartz); Uneven (mica)
- Cleavage: None (quartz); Perfect basal (mica)
- Composition: SiO2 (quartz) + KAl2(AlSi3O10)(OH)2 (muscovite) or K(Mg,Fe)3(AlSi3O10)(OH)2 (biotite), etc.
Quick Check
- Color: Variable (white, gray, silvery, black, brown)
- Luster: Vitreous (quartz) and Pearly/Sub-metallic (mica)
- Streak: White (for both quartz and most micas)
Physical Characteristics
- Crystal Habit: Quartz: Anhedral to euhedral hexagonal prisms; Mica: Platy, tabular, flaky
- Cleavage Type: Quartz: None; Mica: Perfect in one direction (basal)
- Fracture Type: Quartz: Conchoidal; Mica: Uneven
- Tenacity: Quartz: Brittle; Mica: Flexible and elastic (muscovite), flexible but inelastic (biotite)
- Luster Type: Quartz: Vitreous; Mica: Pearly to sub-metallic
Formation
Quartz with mica typically forms under metamorphic conditions, where pre-existing sedimentary rocks (like sandstone or shale) or igneous rocks are subjected to elevated temperatures and pressures. Quartz recrystallizes, and clay minerals or feldspars transform into mica. It can also occur in some igneous rocks, particularly granites and pegmatites, where both minerals crystallize from a magma.
Usage
Due to its hardness and resistance to weathering, quartz-mica rocks are used as building materials, dimension stone, and aggregate. High-purity quartz-mica schists can be a source of industrial mica. In some cases, decorative pieces are carved from these rocks.
Age Distribution
Precambrian to Cenozoic, depending on the specific geological event that formed the rock.
Where to Find
Appalachian Mountains, USA
Extensive metamorphic belts containing quartz-mica schists and gneisses.
Himalayan Orogen, Asia
High-grade metamorphic rocks, including quartz-mica assemblages, are abundant.
Fennoscandian Shield, Europe
Ancient Precambrian metamorphic and igneous complexes.
Brazilian Shield, South America
Large areas of metamorphic rocks with quartz and mica.
Finding Tips
Look for Outcrops
Exposed rock faces in road cuts, stream beds, and mountainous regions are good places to find these rocks.
Identify Foliation
The parallel alignment of mica flakes (foliation) is a key indicator of metamorphic rocks containing mica.
Check for Hardness
Quartz will scratch glass (Mohs 7), while mica is much softer (Mohs 2-3) and can be scratched with a fingernail or knife.
Observe Luster
The glassy luster of quartz combined with the pearly or metallic luster of mica is distinctive.
Similar Rocks
Quartzite
Predominantly Quartz (SiO2)
Also known as: Metaquartzite
Mica Schist
Predominantly Mica group minerals with significant Quartz
Also known as: Schist
Gneiss
Feldspar, Quartz, Mica, Amphibole
Also known as: Banded Gneiss
Granite
Quartz, Feldspar, Mica (Biotite, Muscovite)
Also known as: Granitic Rock
Scientific Classification
- Mineral Class
- Quartz: Tectosilicate; Mica: Phyllosilicate
- Group
- Quartz Group; Mica Group
- Crystal System
- Quartz: Trigonal; Mica: Monoclinic
- Chemical Formula
- SiO2 (Quartz) + KAl2(AlSi3O10)(OH)2 (Muscovite) or K(Mg,Fe)3(AlSi3O10)(OH)2 (Biotite)
- Composition
- Silicon dioxide with various hydrous potassium aluminum silicates, often with magnesium and iron.
Explore Quartz with Mica
Identify rocks anywhere
Free on iOS, Android, and Web. Photo identification, full database, and your personal collection.