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John Day Fossil Beds Information:
John Day Fossil Beds, a US National Monument in Wheeler and Grant counties in east-central Oregon and located within the John Day River basin. The park is known for its well-preserved layers of fossil plants and mammals that lived in the region between the
Eocene Epoch, about 45 million years ago and the Miocene Epoch, about 5 million years ago.
In 1864, Thomas Condon, who was a missionary and amateur geologist, recognized the importance of the fossils in the valley and reported their existence to the world. It was in 1975 when the river basin became a national monument
Description:
There are three geographically separate units which are: Sheep Rock, Painted Hills, and Clarno.
These three units cover a total of 13,944 acres, which area are semi-desert shrublands, riparian zones, and colorful badlands.
About 210,000 people visited the park in 2016 to engage in outdoor recreation or to visit the Thomas Condon Paleontology Center or the James Cant Ranch Historic District.
Location:
Coordinates:
44.5525180, -119.6460709
Thomas Condon Paleontology Center
Elevation:
2279 feet
Geographical Region:
Basin and Range
Prior to the arrival of the Europeans in the 19th century, the John Day river basin was frequented by the
Sons of Hadoram, more specifically, the
Sahaptin language indigenous people who hunted, fished, and gathered roots and berries in this region.
With the advent of road-building to and within the John Day river valley, settlers began to established farms, ranches, and a few small towns along the river and its tributaries.
Bates State Park (44.5925230, -118.5098305)
Priest Hole Recreation Site (44.7390674, -120.2716386)
Ochoco Divide NF Campground (44.5006040, -120.3871207)
John Day River
John Day Fossil Beds National Monument
Pathway Journeys:
Footpath Journeys
Roadpath Journeys
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