Geological Story
of
Petrified Forest National Park
225 million years ago: During the Late Triassic, the Chinle Formation was deposited as mud, silt, clay, and sand in an ancient floodplain near the equator.  Waterlogged trees were covered by sediment and preserved through petrification.

70 million years ago: Through tectonic movement of the earth's crust, Arizona and the rest of the continent began to move away from the equator and the other continents.  This was also a period of mountain building, during which the Colorado Plateau began to isolate and uplift, causing stress to the fossils contained within the Chinle Formation.

5-16 million years ago: Near the end of the Cenozoic, during the Pliocene, a shallow lake as large as Lake Erie covered much of Northeastern Arizona.  Deposits of silt and sand eventually formed sedimetary rock that can still be seen in the Painted Desert.  Lava and ash from nearby volcanoes flowed down to and into the lake, eventually forming the dark cap rock found on Pilot Rock and the Rim of the Painted Desert.  These deposits make up the Bidahochi Formation.

Pleistocene to the Present: Since the Ice Age, erosion has shaped the land of the Petrified Forest region.  Today the activity continues, although the climate has become more arid, exposing the treasures within the layers of Petrified Fore
Click here to see the animated globe: Continental Drift.
Future: After tectonic movement, uplift, and erosion, this landscape is still dynamic.  Unfortunately, most of the movement is through the activity of people.  Every year, about 12 tons of petrified wood is removed from the park.  It is through the effort of Petrified Forest employees and the stewardship of our visitors that this illegal and selfish activity can be curtailed.  This unique and beautiful place has been preserved and protected for the enjoyment and edification of future generations.  Only time will reveal what natural forces will act upon the unique geology of Petrified Forest National Park in the futu
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