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Placer deposit

 

Natural concentration of heavy minerals caused by the effect of gravity on moving particles. When heavy, stable minerals are freed from their matrix by weathering processes, they are slowly washed downslope into streams that quickly winnow the lighter matrix. Thus the heavy minerals become concentrated in stream, beach, and lag (residual) gravels and constitute workable ore deposits. Minerals that form placer deposits include gold, platinum, cassiterite, magnetite, chromite, ilmenite, rutile, native copper, zircon, monazite, and various gemstones.

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Geography Dictionary: placer deposit
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A mineral occurring as an alluvial deposit in the sand and gravel of alluvial fans and valley floors. Such minerals are generally resistant to corrosion by water. The most important placer deposits are diamonds, gold, and tin.

Wikipedia: Placer deposit
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Black sand concentrates

In geology, a placer deposit or placer is an accumulation of valuable minerals formed by deposition of dense mineral phases in a trap site. The name is from the Spanish word placer, meaning "alluvial sand". Types of placer deposits include alluvium, eluvium, beach placers, and paleoplacers.

Alluvial placers

Typical locations for alluvial placer deposits are on the inside bends of rivers and creeks, in natural hollows, at the break of slope on a stream, the base of an escarpment, waterfall or other barrier, within sand dunes, beach profiles or in gravel beds.

Section of Alluvial Placer Deposit at the Blue Ribbon Mine Alaska
Beach placer deposit of heavy minerals (dark) in a quartz sand (Chennai, India).

Alluvial placers are formed by the deposition of dense particles at a site where water velocity remains below that required to transport them further. To form a placer deposit, the particles sought after must show a marked density contrast with the gangue material, which is able to be transported away from the trap site. Only if the deposit is winnowed in this way can the minerals be concentrated to economic levels.

Placer materials must be both dense and resistant to weathering processes. Placer environments typically contain black sand, a conspicuous shiny black mixture of iron oxides, mostly magnetite with variable amounts of ilmenite and hematite. Valuable mineral components often occurring with black sands are monazite, rutile, zircon, chromite, wolframite, and cassiterite.

Exceptionally dense substances such as gold and the platinum group members will accumulate in placers, when they are present. Placer mining is an important source of gold, and was the main technique used in the early years of the California Gold Rush.

Substances commercially mined from placer deposits:

See also

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Copyrights:

Britannica Concise Encyclopedia. Britannica Concise Encyclopedia. © 2006 Encyclopædia Britannica, Inc. All rights reserved.  Read more
Geography Dictionary. A Dictionary of Geography. Copyright © Susan Mayhew 1992, 1997, 2004. All rights reserved.  Read more
Wikipedia. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article "Placer deposit" Read more