Rock Identifier
Feldspathic Granite (likely Syenite or Granite Pegmatite) (Phaneritic Acidic Igneous Rock (KAlSi3O8 dominant with SiO2)) — igneous
igneous

Feldspathic Granite (likely Syenite or Granite Pegmatite)

Phaneritic Acidic Igneous Rock (KAlSi3O8 dominant with SiO2)

Hardness: 6-6.5 (Mohs scale); Color: Pinkish-orange (orthoclase), gray/white (quartz/plagioclase), black (biotite/hornblende); Luster: Vitreous to pearly; Crystal structure: Monoclinic/Triclinic; Cleavage: Two directions at 90 degrees in feldspar crystals.

Hardness
6-6
Luster
Vitreous to pearly
Identified More igneous

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Physical properties

Hardness: 6-6.5 (Mohs scale); Color: Pinkish-orange (orthoclase), gray/white (quartz/plagioclase), black (biotite/hornblende); Luster: Vitreous to pearly; Crystal structure: Monoclinic/Triclinic; Cleavage: Two directions at 90 degrees in feldspar crystals.

Formation & geological history

Formed by the slow cooling of silica-rich magma deep within the Earth's crust (intrusive). The large crystal grains indicate a slow cooling process, potentially dating from the Precambrian to Cenezoic eras depending on local basement geology.

Uses & applications

Used primarily in the construction industry as dimension stone, crushed stone for road base, granite countertops, and architectural facing. High-quality specimens of specific minerals within may be collected.

Geological facts

Feldspar is the most abundant mineral group in the Earth's crust. This specific specimen shows iron oxide staining (limonite/hematite), giving it the rusty-orange surface hue frequently seen in weathered outcrops.

Field identification & locations

Identify in the field by its coarse, interlocking crystalline texture and the presence of salmon-pink potassium feldspar. Commonly found in continental shields and mountain belts. Collectors should look for 'flashing' flat cleavage planes when rotating the rock in the sun.