Image 4: Opal in Petrified Wood
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Opal is made of small spheres of silica gel tightly packed together. The sphere dissects the light as it passes through, splitting it into many different colors. The arrangement of these silica spheres, whether it is completely random or somewhat ordered, will affect the stone's play of color quality. Opal also contains varying percentages of water within it. The higher the water percentage, the more brittle the stone will be (ICGA).
Most opal is 50-65 million years old, dating back to the Cretaceous period (Bernardine Fine Art Jewelry, 1998-2008). Opal is found in areas that were once covered by an inland sea. Water washed silica-containing solution into the cracks and crevices of sediments along the shoreline. The silica then hardened and became opal. Sometimes the remnants of plants and animals were washed up along with the silica and became part of the stone (ICGA). Opal can also become the petrifying material in things such as wood, shell, and bone, like the petrified wood shown left from the Peacock Opal Mine in Virgin Valley (Friedman, 1997-2003).
Opal may occur with many different habits such as massive, botryoidal, reniform, stalactitic, earthy, nodular, and may be found in veins, crusts and accumulating mounds. It commonly occurs with chalcedony and is often confused with it, but their difference in hardness is the distinguishing factor.
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