
Two hundred million years ago, what is now northeastern Arizona was a tropical floodplain crossed by rivers carrying massive trees. When the trees fell and were buried by volcanic ash, silica-rich water permeated the wood, replacing organic material with quartz crystal - cell by cell, ring by ring, preserving every detail in stone harder than steel. The trees became gemstones: rainbow cross-sections of jasper, amethyst, and agate lying on a landscape of multicolored badlands called the Painted Desert. The combination is surreal - ancient trees that are now rock, resting on earth that changes color with the light. Petrified Forest National Park protects both: the trees that refused to decay and the desert painted by time.
The trees that became Petrified Forest's logs were Araucarioxylon arizonicum - conifers related to modern Norfolk Island pines, growing up to 200 feet tall. They fell into rivers, were transported downstream, and buried rapidly in oxygen-free sediment. Volcanic eruptions contributed silica-rich ash. Over millions of years, silica dissolved in groundwater infiltrated the buried wood, replacing organic molecules with quartz while preserving cellular structure. Trace minerals created colors: iron oxides for reds and yellows, manganese for purples, chromium for greens. The process produced not fossils but stone logs, crystalline replicas of once-living trees.
The Painted Desert extends roughly 150 miles across northern Arizona, but the most accessible viewing is within Petrified Forest National Park. The colors come from iron and manganese compounds in the Chinle Formation - the same sediments that buried the trees. Different mineral content in different layers creates bands of red, orange, pink, blue, and white. The colors change with light and weather, brightening after rain, shifting through the day. The landscape looks almost artificial, as if someone applied pigment to hills. The effect is both beautiful and unsettling - terrain that shouldn't look like this but does.
Visitors have been stealing petrified wood for over a century. Despite penalties and surveillance, roughly 12 tons of petrified wood disappear from the park annually - souvenirs pocketed, loaded into cars, shipped home. The park receives a steady stream of returned specimens, often accompanied by letters describing bad luck that followed the theft. Whether the 'curse' is real, psychological, or merely convenient mythology, the phenomenon is documented. The park displays some of the returned pieces and letters, creating a peculiar exhibit: evidence of human compulsion to take pieces of ancient forests, and evidence that some regret it.
Petrified Forest became a National Monument in 1906 and a National Park in 1962. The designation came because the logs were disappearing - commercial collectors, souvenir hunters, and artifact dealers had been hauling wood away for decades. The park now protects over 200 square miles, including the major petrified wood concentrations and Painted Desert overlooks. Collection is illegal; rangers and cameras monitor the sites. The park's small size and high visitation make enforcement challenging. Every piece of petrified wood removed is irreplaceable - 200 million years of geological chance, destroyed for a paperweight.
Petrified Forest National Park is located in northeastern Arizona, straddling Interstate 40 roughly 110 miles east of Flagstaff. The park has north and south entrances; the scenic drive connects them across 28 miles of desert and petrified wood concentrations. Crystal Forest and Giant Logs trails offer easy access to petrified wood. The Painted Desert overlooks are in the northern section. The park has no overnight lodging; Holbrook is the nearest town with services. Summer is hot; spring and fall offer comfortable temperatures. Rain enhances colors. Do not collect petrified wood - it's illegal, damaging, and according to the letters, unlucky.
Located at 35.08°N, 109.79°W in northeastern Arizona. From altitude, Petrified Forest appears as colorful badlands terrain - bands of red, white, and purple visible in the Chinle Formation exposures. The Painted Desert extends to the north and east. The petrified logs are not visible from cruising altitude, but the general terrain character is apparent: eroded, colorful, distinctive. Interstate 40 crosses the southern portion of the park. The Little Colorado River valley lies to the northwest. The landscape's multicolored character distinguishes it from surrounding desert - even from 30,000 feet, the Painted Desert looks painted.