Petrifaction 

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Petrification, also known as fossilization, is a natural process in which the original organic material of a plant or animal is replaced by minerals, resulting in a three-dimensional, rock-like replica of the original organism. This process occurs over a long period of time, often millions of years, and is a result of the preservation of the original structures in sediment.

Petrification occurs when the organic material of a dead plant or animal is gradually replaced by minerals that seep into the structure. The minerals, which are often silicates, replace the original organic matter and preserve ___ _____________ ________ ______ ___ ____________ ________ __ ______ __ ___________ ___________ _____ ____________.
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Degree : BACHELOR DEGREE PROGRAMMES
Course Name : Bachelor of Science
Course Code : BSCG
Subject Name : Biodiversity (Microbes, Algae, Fungi and Archegoniates)
Subject Code : BBYCT 131
Year : 2023