Hematite (Fe2O3)
Primary iron ore. Steel-gray to reddish; distinctive cherry-red streak. Forms in sedimentary banded iron formations and hydrothermal veins.
Field reference
A concise English guide to the major groups of ore minerals — oxides, sulfides, carbonates, silicates, and native elements — used in geology classrooms and amateur collecting.
Primary iron ore. Steel-gray to reddish; distinctive cherry-red streak. Forms in sedimentary banded iron formations and hydrothermal veins.
Strongly magnetic iron oxide. Black, metallic luster. Important in igneous and metamorphic deposits; used in dense-media separation.
Chief tin ore. High density, adamantine luster. Common in granite-related veins and alluvial placers.
Most important copper ore. Brass-yellow, often tarnished. Occurs in porphyry copper systems and massive sulfide deposits.
Lead ore with cubic cleavage and high specific gravity. Frequently associated with silver; common in Mississippi Valley-type deposits.
Primary zinc ore. Resinous luster; color from yellow to black depending on iron content. Often found with galena.
“Fool’s gold.” Pale brass-yellow cubes or pyritohedra. Not an iron ore, but common gangue and a sulfur source historically.
Bright green secondary copper mineral. Forms in the oxidized zones of copper deposits; also valued as an ornamental stone.
Secondary zinc carbonate. Botryoidal crusts in oxidized zinc ores; historically smelted before widespread use of sphalerite.
Source of beryllium; gem varieties include emerald and aquamarine. Forms in pegmatites and hydrothermal veins.
Major hard-rock lithium ore. Prismatic crystals in lithium pegmatites; critical for battery supply chains.
Occurs as nuggets, flakes, and vein fillings. Soft, malleable, dense; recovered from both lode and placer deposits.
This page is a static educational summary for general reference. Grades, reserves, and mining practice vary by deposit.