![]() Petrified wood is the fossilized remains of ancient trees which flourished millions of years ago. Eventually the remains gradually turn into stone. Typically the soft parts of the organism decompose quickly and the hard parts, such as shells and bones, remain in place longer. Most are preserved in fine-grained sedimentary rock such as limestone or shale. Try it in combination with Agatized Coral, Sand Dollar Fossil, Shell Fossil, Turritella Agate, and Vatican Stone.įossils are remnants of organisms living in a past geological age. Petrified Wood’s energy works well with its family – other Fossils. In the case of Petrified Wood, the organic matter is replaced on a cellular level, preserving incredibly detailed patterns. But when a stone is “agatized” it may be quite colorful. The minerals may be a grey or tan color, just like the surrounding sedimentary rock. ![]() Mineral preservation by contrast involves calcareous water seeping into the remains and gradually replacing the organic matter with minerals. Calcium carbonite is also the main chemical components of Aragonite and Calcite. ![]() The organism is fossilized in an unaltered state, a process aided by the fact that the animals’ skeleton is calcareous (calcium carbonate) and can remain virtually unchained when fossilized. Unaltered preservation typically involves marine or lake dwelling invertebrates, such as Coral, mollusks, sponges, etc. The three most common forms of fossils are unaltered preservation (most shells, fossil teeth, and organic material in Amber), mineral preservation (Petrified Wood and most dinosaur bones), and fossil impressions (leaf prints and footprints). Fossils come in many different forms and, depending on what is being preserved, the fossilization process can also be very different. A fossil is the remnant or impression of an organism which lived in the past.
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