Versteinerter Holzstamm Mineral is a non-laminated layer about

is a non-laminated layer about 18 inches (46 cm) thick that also contains abundant detailed fossils but is more difficult to work with because it is not composed of split layers

Chemically speaking

in limestone matrix and framed

an dem die Bedingungen für eine reiche Ansammlung ungestörter Fossilien gegeben waren

but the most beautiful and best preserved specimens come from the Posidonia shale layers of Holzmaden in southern Germany

Versteinerter Holzstamm Mineral is a non-laminated layer aboutOrigin: Indonesia Age: Miocene, 20 million years ago. Size: H68cm W32cm D21cm Description: Polished trunk made of petrified wood from Indonesia with a preserved bark structure up to the edge. Very beautiful and rare color palette with beige and black tones. Additional information: Petrified wood is fossil wood in which all organic matter has been replaced by minerals, while preserving the structure of the wood. The petrification process occurs