Certain conditions are necessary for wood to become petrtified in nature,
but it is not as uncommon as we might think. First, the tree must be sealed
from oxygen to prevent decay. If it is not sealed, bacteria will usually
decompose the wood.
This seal may be created in a variety of ways. A flood which deposits sand
and silt may suddenly bury a tree that has fallen to the forest floor. It may
also be buried by volcanic ash from a nearby volcanic explosion or a lava
flow. Next, there must be minerals present that will cause petrification.
Examples include calcite, pyrite ("fool's gold"), marcasite, and silica, which
is the most common. These minerals dissolve in groundwater, seep through the
sediment covering the wood, and replace the organic material in the wood.
Through chemical processes, the minerals move from the water and into the
individual plant cells. In good examples of petrification, you can still see
the cell walls if you look closely enough.
This experiment will model the process of petrification. While performing
the experiment, try to think of the natural processes that the experiment is
modeling. Before performing the experiment, read the instructions and predict
what you think your results will be. Record your thoughts in the section
marked "Prediction" on your worksheet.