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  2. John Day Fossil Beds National Monument - Wikipedia

    en.wikipedia.org/wiki/John_Day_Fossil_Beds...

    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 ...

  3. John Day Formation - Wikipedia

    en.wikipedia.org/wiki/John_Day_Formation

    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 ...

  4. Painted Hills - Wikipedia

    en.wikipedia.org/wiki/Painted_Hills

    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 ]

  5. James Cant Ranch Historic District - Wikipedia

    en.wikipedia.org/wiki/James_Cant_Ranch_Historic...

    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 ...

  6. 29 million-year-old fossilized nest discovered in Oregon ...

    www.aol.com/news/29-million-old-grasshopper-nest...

    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

  7. Paleontology in Oregon - Wikipedia

    en.wikipedia.org/wiki/Paleontology_in_Oregon

    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]

  8. John Day River - Wikipedia

    en.wikipedia.org/wiki/John_Day_River

    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 ...

  9. Mascall Formation - Wikipedia

    en.wikipedia.org/wiki/Mascall_Formation

    The formation is described in Geologic Formations of Eastern Oregon (1972) as follows: "The Mascall Formation consists of a maximum of 2,000 feet of fluvial sandstone, ash, light colored water-laid tuff, and well-rounded conglomerate. Within the Mascall Formation is a widespread ignimbrite unit which consists of 97 to 99 percent glass shards ...

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