fossil wood

Fossil wood is ancient wood that has undergone mineralization over millions of years. During this process, organic materials decay and are replaced by minerals like silica or calcite, preserving the original structure of the wood in stone form. This creates a durable, often beautifully patterned specimen that reveals details about prehistoric environments and plant life. Fossil wood provides scientists with insights into Earth's history, climate changes, and the evolution of plants, serving as a valuable resource in paleontology and geology.