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stream placer

mining
Also known as: alluvial ore deposit, alluvial placer

Quick Summary

A placer deposit is a natural concentration of heavy minerals formed by gravity acting on moving particles. When rocks weather, heavy, stable minerals are released and washed into streams. The moving water winnows away lighter material, leaving the heavier minerals concentrated in stream, beach, or residual gravels, forming workable ore deposits.1

Minerals found in placer deposits are characterized by high specific gravity, resistance to weathering, and durability. Common examples include gold, platinum, cassiterite (tin ore), magnetite, chromite, ilmenite, rutile, zircon, monazite, and gemstones.12

Stream placers, formed by running water, are the most significant type and have historically yielded the most placer gold, tin, platinum, and gemstones. Mining techniques vary based on deposit characteristics, water availability, and mineral value. Methods include mechanized excavation with draglines or shovels, ground sluicing, hydraulicking, and the use of sluice boxes where riffles trap heavy minerals.123

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