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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 Cant Ranch is located within the boundaries of the Sheep Rock Unit of the John Day Fossil Beds National Monument. Highway 19 runs through the ranch property on the west side of the John Day River. The ranch complex is located on the east side of the roadway. The Thomas Condon Visitor Center is located across the highway from the ranch ...
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 northeast of Madras .
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 ...
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
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 John Day River passing by Sheep Rock in the John Day Fossil Beds National Monument. The John Day River is a tributary of the Columbia River, approximately 284 miles (457 km) long, in northeastern Oregon in the United States. It is known as the Mah-Hah River by the Cayuse people. Undammed along its entire length, the river is the fourth ...
[23] [24] The state's only known fossil egg was found in associated rock formations. [4] A Patriofelis skeleton. The subduction zone's volcanic activity also formed the Cascade volcanic arc, which blocked moist air from the Pacific and created the state's High Desert. [3] This is when Oregon's fossil-rich John Day Fossil Beds were first laid ...
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