Rock Identifier
Gold (Native gold (Au))
mineral

Gold

Native gold (Au)

A dense, soft, intensely yellow native metal valued for millennia in coinage, jewelry, and electronics.

Mohs hardness
2.5-3
Color
Golden yellow, sometimes paler when alloyed with silver
Type
mineral

Got a rock like this?

Identify any rock from a photo, free.

Overview

Gold is a native metallic element (chemical symbol Au) prized since antiquity for its rich yellow color, resistance to tarnish, and rarity. It occurs naturally as the metal itself, in nuggets, grains, flakes, and veins, often alloyed with a little silver or copper.

Gold is one of the densest common minerals and is extremely malleable and ductile, able to be hammered into thin leaf or drawn into fine wire. It is chemically inert, so it does not rust or corrode under normal conditions.

These properties have made gold a universal store of value and a foundation of jewelry, coinage, and, in modern times, advanced electronics.

Formation & geology

Gold forms mainly in hydrothermal systems, where hot, mineral-rich fluids deposit it in quartz veins within igneous and metamorphic rocks. These lode deposits are the primary source of most gold.

When gold-bearing rock weathers and erodes, the heavy metal is freed and concentrated by water in stream gravels as placer deposits, the source of classic gold panning and nugget finds. Its high density allows it to settle while lighter sediment washes away.

Gold is also recovered as a byproduct of copper and other base-metal mining. Major producers include South Africa, Australia, Russia, China, and the United States.

How to identify it

Gold is identified by its rich metallic yellow color, very high density (it feels notably heavy), and malleability, it dents rather than shatters and can be flattened. Its streak is golden yellow, and it does not tarnish.

The classic look-alike is pyrite (fool's gold), which is brassier, brittle, harder (about 6-6.5), and gives a greenish-black streak. Chalcopyrite is also brassy but tarnishes and is brittle. Gold's softness (hardness 2.5-3) and malleability are decisive: real gold cannot be crushed to powder and will not crumble.

Mica flakes can glint gold but are extremely light and flexible. A heft test and streak test reliably separate gold from imitators.

Uses & significance

Gold's main uses are in jewelry, investment bullion, and coinage, where its beauty, rarity, and durability are valued. It is alloyed with other metals to increase hardness and vary color, measured in karats.

Industrially, gold is essential in electronics for its excellent, corrosion-free conductivity, used in connectors, circuit boards, and microchips. It also serves in dentistry, aerospace, and medicine.

As a tangible store of wealth, gold underpins national reserves and financial markets. Its enduring cultural significance spans art, religion, and symbols of status worldwide.

Frequently asked questions

How can I tell real gold from pyrite?

Gold is soft, very heavy, and malleable with a golden streak; pyrite is harder, brittle, brassier, and leaves a greenish-black streak. Pyrite crumbles, gold dents.

What is placer gold?

Placer gold is gold freed by weathering and concentrated by water in stream gravels, recovered by panning, sluicing, or dredging.

Why does not gold tarnish?

Gold is chemically inert and does not react with oxygen or moisture under normal conditions, so it keeps its bright color indefinitely.

What does karat mean?

Karat measures gold purity in alloys; 24 karat is pure gold, while lower karats contain more added metals for hardness and color.

Gold identified by the community

Real specimens identified with Rock Identifier.

GoldGold Flakes (Placer Gold)Gold in Quartz OreGold NuggetGold NuggetGold NuggetGold FlakeGold in Quartz MatrixGold FlakesGold GrainGold Nugget / Gold FlakesGold Nuggests