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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. 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
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 ]
The James Cant Ranch is a pioneer ranch complex in Grant County in eastern Oregon, United States. The ranch is located on both sides of the John Day River in the John Day Fossil Beds National Monument. The ranch was originally homesteaded by Floyd Officer in 1890. Officer sold the property to James Cant in 1910.
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 ...
Major Mesozoic and Permian fossiliferous stratigraphic units in Oregon. Cape Sebastian Sandstone. Chico Formation. Hudspeth Formation. Otter Point Formation. Nicely & Snowshoe Formations. Martin Bridge Limestone. Coyote Butte Limestone.
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