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Gold is created in its free elemental form as nuggets or grains in rocks, seams, and alluvial deposits. It is found in various solid solutions with silver, naturally alloyed with other metals such as copper color and palladium, and mineral inclusions such as pyrite.

Gold is a chemical element through the symbol Au and the atomic number 79, making it one of the highest nuclear number natural elements. Its pure form is a light, slightly reddish, dense, soft, malleable, and ductile metal.

In chemistry, gold is a transition metal and a group 11 element, and it is one of the least responsive chemical elements and is solid under normal conditions.

gold deposits

Traces of gold are found in all igneous rocks and their abundance in the earth’s crust estimate at around 0.005 parts per million. Except for tellurium, selenium, and bismuth, it occurs mainly in the native state and remains chemically uncombined, and gold-197 is the only natural isotope of the element.

Gold is often associated with deposits of copper and lead. Although the amount is usually minimal, it quickly recovers as a by-product of refining these base metals. It is rare to find prominent figures of auriferous rocks rich enough to be classified as ore. Two gold deposits are known: hydrothermal veins, associated with quartz and pyrite, and placer deposits, consolidated and unconsolidated, formed by the weathering of gold-bearing rocks.

properties of gold

It is scarce, does not rust, and is non-deadly.

The element is weathering resistant and alluvial and seam payments.

Although copper and silver are the best anodes of heat and electricity, gold connections will survive both because they don’t tarnish. Not that gold lasts longer, but that it stays conductive longer.

Gold is squashy: it can suck into the most OK wires. One jot of gold can draw through 80 kilometers of five-micron gold wire, or five millionths of a meter thick. This taster has a diameter of 0.20 millimeters.

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