IDENTIFICATION

Streak Plates & Field Kits

The streak plate is the cheapest, most-portable, most-diagnostic tool in mineral ID. Two minerals that look identical can have streak colors so different that the plate alone resolves them.

Specimen on streak plate

How streak works

Drag the mineral firmly across an unglazed white porcelain plate (typically the back of a bathroom tile). The line of powder that's left is the streak — the color of the mineral pulverized to powder. Body color is dominated by reflection and depends on grain size and surface; streak is intrinsic to the chemistry.

Classic streak separations

Hematite (any external color) → red-brown streak. Magnetite (looks like hematite) → black streak. Pyrite (gold cubes) → greenish-black streak. Chalcopyrite (similar gold color, often iridescent) → also greenish-black but darker and metallic. Galena → dark grey. Sphalerite → pale yellow to brown to black depending on iron content. Cinnabar → bright red.

Limits

Minerals harder than the porcelain (~6.5) won't streak — they just scratch the plate. Quartz, garnet, topaz, beryl, corundum: streak test impossible. Use other diagnostics. Also: streak only works on a CLEAN plate. Wipe between tests; a leftover red hematite streak will contaminate your next sample.

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