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The John Day Fossil Beds National Monument consists of three widely separated units—Sheep Rock, Painted Hills, and Clarno—in the John Day River basin of east-central Oregon. Located in rugged terrain in the counties of Wheeler and Grant, the park units are characterized by hills, deep ravines, and eroded fossil-bearing rock formations. [ 6 ]
The Painted Hills is a geologic site in Wheeler County, Oregon that is one of the three units of the John Day Fossil Beds National Monument along with Sheep Rock and Clarno. It totals 3,132 acres (12.67 km 2) and is located 9 miles (14 km) northwest of Mitchell, Oregon. The Painted Hills are listed as one of the Seven Wonders of Oregon. [ 1 ]
John Day Fossil Beds map. The John Day Formation is a series of rock strata exposed in the Picture Gorge district of the John Day River basin and elsewhere in north-central Oregon in the United States. The Picture Gorge exposure lies east of the Blue Mountain uplift, which cuts southwest–northeast through the Horse Heaven mining district ...
Christopher Schierup, National Parks Service collection manager, first spotted the fossil in 2012 in the John Day Fossil Beds National Monument in Mitchell, Oregon. - N. Famoso/National Park Service
When the John Day Fossil Beds National Monument was established in 1975, the initial development plan recommended purchasing the Cant Ranch complex for use as the monument's headquarters and visitor center. The National Park Service purchased 878 acres (3.55 km 2) from the Cant family in 1975. This included the main ranch complex and adjacent ...
This is when Oregon's fossil-rich John Day Fossil Beds were first laid down. [25] The earliest fossils in John Day indicate a subtropical terrestrial environment. The assemblage is rich in fossil seeds, fruit nuts, and associated woods, and is one of the few places in the world where all three are preserved in a single location. [26]
From Mitchell, it flows generally northwest for about 15 miles (24 km), passing through the Painted Hills unit of the John Day Fossil Beds National Monument before meeting the John Day River. Bridge Creek is subject to occasional flash floods, which have affected Mitchell as well as rural areas nearby.
Condon Hall at the University of Oregon, which originally housed the geology department, was named for Condon, [12] as were the Thomas Condon Paleontology Center at the Sheep Rock unit of the John Day Fossil Beds National Monument, near Kimberly, Oregon, [13] temporary Lake Condon, formed periodically by the Missoula Floods, and the Condon Fossil Collection of the University of Oregon Museum ...
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