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Mineral Identification & Field Testing

Dug by hand. Crafted by heart. Fall 7, stand 8.

Five field tests classify most common minerals without a lab. Color is a clue. The test wins.

1. Mohs scratch hardness

Jasper, chert, and chalcedony typically test 6.5–7.0.

2. Streak

Unglazed porcelain tile. Hematite: reddish-brown. Pyrite: greenish-black. Native gold: golden yellow.

3. LED translucency

Translucent edges: chalcedony and agate. Opaque: siltstone, argillite, dense chert.

4. Longwave UV (365 nm)

Calcite veining often fluoresces white, yellow, or red. Inert silica typically does not.

5. Dilute acid fizz

Carbonates fizz. Silicates stay inert. One drop. Pack the bottle out. Never test a finished jewelry face.

South Okanagan & Similkameen profiles

Red & polychrome jasper — iron-oxide silica, conchoidal fracture, Mohs 6.5–7.0.

Golden & yellow jasper — limonite in cryptocrystalline quartz.

Chalcedony & agate — waxy luster, translucent edges; agate is banded.

Black chert, argillite, siltstone — opaque, often carbon-dark, no waxy luster.

Optical calcite — rhombohedral cleavage, double refraction, Mohs 3.0, vigorous fizz.

Galena — metallic, dense, cubic 90-degree cleavage.

Gold versus common sulfides

Gold: golden yellow, no tarnish, nuggets or wires, Mohs 2.5–3.0, golden streak, malleable, SG 19.3.

Pyrite: brassy, cubes, Mohs 6.0–6.5, greenish-black streak, brittle, SG 5.0.

Chalcopyrite: brassy to peacock, massive or tetrahedral, Mohs 3.5–4.0, brittle, SG 4.2.

Arsenopyrite: silver-white to steel grey, tabular, Mohs 5.5–6.0, grey-black streak, brittle, SG 6.0.

Lapidary check

  1. Micro-fractures.
  2. Structural cohesion.
  3. Softness gradients.
  4. Thickness of the weathered rind.

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