Natural Gold-Bearing Ore with Exposed Crystalline Flakes
Raw Gold Ore (Lode Deposit Specimen) · Natural Native Gold; likely alloyed naturally with silver (Electrum) or trace copper.
Purity: Likely 70% to 92% (16K-22K) within the actual gold flakes; the specimen as a whole is mineral rock with trace gold content.
Type
Raw Gold Ore (Lode Deposit Specimen)
Purity
Likely 70% to 92% (16K-22K) within the actual gold flakes; the specimen as a whole is mineral rock with trace gold content.
Gold Type
Natural Native Gold; likely alloyed naturally with silver (Electrum) or trace copper.
Weight
Total specimen weight unknown; visible gold content represents a minute fraction of a gram (milligrams).
Description
This is a raw geological specimen of lode gold. It features small, jagged, bright yellow flakes of native gold embedded within a host rock matrix. The rock shows signs of heavy mineralization, with dark red iron oxidation indicating the weathering of sulfide minerals where gold often precipitates. It is a classic 'hard rock' specimen prized by prospectors and mineral collectors for showing 'gold in situ.'
Key Features
Metallic luster that does not change with viewing angle; malleable appearance of the flakes; association with iron-stained quartz/sulfide matrix.
Color & Finish
Vivid buttery yellow metallic flakes contrasting against a dark, hematite-rich or gossanous iron oxide matrix with greyish metallic sulfides.
Hallmarks & Stamps
None; natural geological specimen. No man-made markings.
Dimensions Estimate
Macro view suggests the central gold flake is approximately 1-2mm; the rock fragment appears to be a hand-sized specimen.
Gemstones & Inlays
No gemstones. The matrix appears to consist of quartz, iron oxides (limonite/hematite), and potential sulfides like galena or arsenopyrite.
Clasp & Closure
Not applicable (Raw mineral specimen).
Chain & Links
Not applicable (Raw mineral specimen).
Craftsmanship Details
Natural geological formation via hydrothermal deposition; no human craftsmanship involved.
Authentication Indicators
Sectility (gold can be cut or deformed without shattering unlike pyrite); high-density luster; lack of crystal faces standard in 'Fool's Gold' (Pyrite).
Origin & Maker
Natural Geological Origin. Maker: Nature/Earth's Crust. Common in gold-rich regions like the Mother Lode (California) or Witwatersrand (South Africa).
Era & Period
Modern Discovery; geological age of the deposit likely millions of years (e.g., Paleozoic or Mesozoic era).
Age Estimate
Geological age: millions of years; Time since extraction: Likely contemporary/recent.
Cultural Significance
Represents the 'Gold Rush' heritage of hard-rock mining; symbolizes the raw wealth of the earth before industrial processing.
Condition Notes
Natural and unrefined; the matrix is fractured and crumbly (typical of oxidized ore). Gold flakes remain bright and untarnished.
Value Estimate
Melt value is negligible (less than $5); Specimen value for a collector could range from $20 to $100 depending on the total gold visible and locality.
Care & Maintenance
Keep in a dry environment to prevent further oxidation of the matrix; do not clean with harsh chemicals which may dissolve the host rock; handle carefully as natural gold flakes can be dislodged from the stone.
Similar Items
Pyrite (Fool's Gold) which is brassier and brittle; Chalcopyrite which often has a peacock iridescent tarnish; Mica which is flaky but translucent and non-metallic.
Interesting Facts
Most of the world's gold is found in such tiny particles that it is invisible to the naked eye; a specimen where gold is clearly visible is relatively rare and often worth more as a specimen than the melt value of the gold itself.