mineral

Mixed collection of quartz-rich rocks and minerals

Quartz (SiO₂), with some pieces possibly containing feldspar or mica; exact identification is uncertain from the image

AI-generated identification · may be incorrect

Mostly opaque to translucent white, gray, and pale pink rough fragments with vitreous to dull luster. Quartz has Mohs hardness 7, hexagonal crystal structure, and no cleavage; the pictured pieces are too indistinct to assess individual properties reliably.

Identified October 3, 2026More mineral →

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At a glance

Common name: Mixed collection of quartz-rich rocks and minerals
Scientific name: Quartz (SiO₂), with some pieces possibly containing feldspar or mica; exact identification is uncertain from the image
Category: mineral
Identified: October 3, 2026
Method: Standard

AI Estimated Value

About $1–$10 for common rough fragments; more only if a piece proves to be an attractive, identifiable mineral specimen.

Not an official valuation

AI estimate for general interest only — not an appraisal. Actual value depends on condition, provenance, and market demand. Verify with a professional before buying, selling, or insuring.

This identification was generated by AI and may contain errors. Verify important details before relying on them — and never use an AI result to judge whether a specimen is safe to handle. Read the full disclaimer

Physical properties

Formation & geological history

Quartz commonly forms in igneous and metamorphic rocks and in hydrothermal veins, across many geological ages. The image appears to show several different fragments rather than one identifiable rock type.

Uses & applications

Quartz is used in glass, electronics, abrasives, and jewelry; attractive pieces may be polished or collected.

Geological facts

The regional setting near Dubai is dominated by sedimentary deposits, while nearby Oman includes extensive mountain rocks and mineral-bearing terrain; transported material or purchased specimens are also possible.

Field identification & locations

Look for glassy surfaces, hardness sufficient to scratch ordinary glass, and absence of cleavage to recognize quartz. The fragments are not distinctive enough to confirm quartz or identify a specific source.