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John Day Fossil Beds National Monument is a U.S. national monument in Wheeler and Grant counties in east-central Oregon.Located within the John Day River basin and managed by the National Park Service, the park is known for its well-preserved layers of fossil plants and mammals that lived in the region between the late Eocene, about 45 million years ago, and the late Miocene, about 5 million ...
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.
National Park Service headquarters at the Cant Ranch. 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 ...
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
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.
John Day Fossil Beds National Monument — located in Grant County and Wheeler County, Oregon. Pages in category "John Day Fossil Beds National Monument" The following 16 pages are in this category, out of 16 total.
John Day Fossil Beds National Monument; O. Oregon Caves National Monument and Preserve This page was last edited on 8 October 2024, at 00:38 (UTC). Text ...
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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