
mineral
Gold Nugget
Native Gold (Au)
AI-generated identification · may be incorrectHardness: 2.5-3.0 Mohs; Color: Golden-yellow; Luster: Metallic; Crystal Structure: Isometric (cubic); Cleavage: None; Specific Gravity: 19.3
- Hardness
- 2
- Color
- Golden-yellow
- Luster
- Metallic
Identified More mineral →
Explore Gold Nugget in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 2.5-3.0 Mohs; Color: Golden-yellow; Luster: Metallic; Crystal Structure: Isometric (cubic); Cleavage: None; Specific Gravity: 19.3
Formation & geological history
Primary deposits form in hydrothermal quartz veins during Volcanogenic Massive Sulfide or Orogenic events. Secondary (placer) deposits form through the erosion of these veins and subsequent concentration in stream beds by gravity.
Uses & applications
Used primarily in jewelry, currency, electronics (due to high conductivity/anti-corrosion), and as a financial investment.
Geological facts
Gold is chemically inert and does not tarnish. Nearly all the gold found on Earth came from meteorite bombardments occurring roughly 200 million years after the planet formed.
Field identification & locations
Identify by its high density (heavy for its size), malleability (it bends rather than shatters), and lack of tarnish. Commonly found in 'black sand' deposits in rivers or within quartz veins in mountainous regions.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Mineral Sand (Heavy Mineral Sand Concentrate)
Placer deposit concentrate containing minerals such as ilmenite, rutile, zircon, and magnetite
mineral
Calcite–fluorite mineral specimen with iron-oxide staining
Calcite (CaCO₃), likely fluorite (CaF₂), with possible quartz and iron/manganese oxides
mineral
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Soil with Mineral Detritus and Quartz Fragments
Regolith / Silicate Mineral Aggregate
sedimentary
Schist
Schist
Metamorphic