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The opposition of real gold and false gold occurs throughout.
Occasionally, gold occurs as a compound in minerals, usually with tellurium.
A limited amount of precious-metal mining (including gold) occurs in the eastern Cascade Range, notably in the Wenatchee area.
In the wild, gold occurs most often in its pure elemental form as either nuggets, or as grains or veins in rock and in alluvial deposits.
Brassy yellow pyrite, often called "fool's gold," occurs variously as an accessory mineral in many rocks, in veins, and even as a chief component of some fossils.
The federation says it cannot yet test for abnormal magnesium levels, partly because magnesium, unlike Carolina Gold, occurs naturally in the body.
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Just why and how such an extraordinarily large concentration of gold occurred there is a matter of continuing scientific controversy.
Remobilization of this gold occurred during the late stages of the Eburnean Orogeny (~ 2.1 Ga) and is associated with quartz-carbonate veins with visible gold and euhedral pyrites.
The mineralogical characteristics that affect gold recoveries are: identities of gold-bearing minerals, identities of associated metallic and non-metallic minerals, and the proportion of gold occurring in minerals that are soluble in alkaline cyanide solutions.
Fast reduction of gold occurred in the acidic medium.
The first reported import in the New World of what is thought to be Carolina Gold occurred in 1685, when a slave ship from Madagascar unloaded a cargo of rice in Charleston, South Carolina.
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