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Corallo fossile cabochon – Indonesia Corallo fossile is a petrified remnant of ancient coral colonies that were gradually replaced by mineral matter over millions of years, most commonly Quarzo. This process preserved the original coral structure, which is clearly visible in the form of typical cellular or floral patterns. Corallo fossiles da Indonesia are known for their distinctive patterns and contrasting color combinations, most often in shades of beige, brown, gray or black. cabochon and its use in jewelry A cabochon represents a method of stone processing without facets, where the surface is smooth, rounded and Lucidato. This type of cut highlights the natural structure and pattern of Corallo fossile, which is characteristic of this material. Corallo fossile in cabochon form is used in jewelry as well as a decorative object. Formation of Corallo fossile Corallo fossile formed through the process of fossilization, where the original organic structure of corals was gradually replaced by minerals. Most commonly, silicification occurs, meaning replacement by silica. This process took place in a marine environment over millions of years and preserved the detailed internal structure of the original organism. Corallo fossile deposits Indonesia is one of the most important sources of Corallo fossile, where material suitable for jewelry processing is found. Altro occurrences are known da the USA (Florida), Thailandia or Australia. Indonesian Corallo fossiles are valued mainly for their quality pattern and contrast. Properties and characteristics Corallo fossile is a solid material with a hardness of approximately 6.5–7 on the Mohs scale, making it suitable for processing and everyday wear. It has a compact structure, often with a pronounced pattern resembling flowers or cells. When Lucidato, it achieves a smooth luster and retains its characteristic natural appearance.
Cabochon di corallo fossile – Indonesia - FKK12
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FKK12
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