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John Day Fossil Beds National Monument
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 years ago. The monument consists of three geographically separate units: Sheep Rock, Painted Hills, and Clarno. The units cover a total of of 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. Before the arrival of Euro-Americans in the 19th century, the John Day basin was frequented by Sahaptin people who hunted, fished, and gathered roots and berries in the region. After road-building made ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Red Pog
Red is the color at the long wavelength end of the visible spectrum of light, next to orange and opposite violet. It has a dominant wavelength of approximately 625–740 nanometres. It is a primary color in the RGB color model and a secondary color (made from magenta and yellow) in the CMYK color model, and is the complementary color of cyan. Reds range from the brilliant yellow-tinged scarlet and vermillion to bluish-red crimson, and vary in shade from the pale red pink to the dark red burgundy. Red pigment made from ochre was one of the first colors used in prehistoric art. The Ancient Egyptians and Mayans colored their faces red in ceremonies; Roman generals had their bodies colored red to celebrate victories. It was also an important color in China, where it was used to color early pottery and later the gates and walls of palaces. In the Renaissance, the brilliant red costumes for the nobility and wealthy were dyed with kermes and cochineal. The 19th century brought the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sahaptin People
The Sahaptin are a number of Native American tribes who speak dialects of the Sahaptin language. The Sahaptin tribes inhabited territory along the Columbia River and its tributaries in the Pacific Northwest region of the United States. Sahaptin-speaking peoples included the Klickitat, Kittitas, Yakama, Wanapum, Palus, Lower Snake, Skinpah, Walla Walla, Umatilla, Tenino, and Nez Perce. Territory According to early written accounts, Sahaptin-speaking peoples inhabited the southern portion of the Columbia Basin in Washington and Oregon. Villages were concentrated along the Columbia river, from the Cascades Rapids to near Vantage, Washington, and along the Snake River from the mouth to close to the Idaho border. The closely related Nez Perce tribe lived to the east. There were additional villages along tributaries, including the Yakima, Deschutes, and Walla Walla rivers. Several village lived were located west of the Cascade mountains in southern Washington, including tho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mitchell, Oregon
Mitchell is a city in Wheeler County, Oregon, United States. The population was 130 at the 2010 census. It was founded in 1873 and was named after John H. Mitchell, a politician. The Painted Hills unit of the John Day Fossil Beds National Monument is about northwest of Mitchell. Mitchell School, a public school with an enrollment of about 70 students, is in Mitchell. History Foundation At the request of William "Brawdie" Johnson, a blacksmith, a post office was established at Mitchell in 1873. Johnson, the first postmaster, suggested the name ''Mitchell'' after John Hipple Mitchell, a U.S. Senator from Oregon. Senator Mitchell held the office in 1873−1879, 1885−1897, and 1901−1905. Platted in 1885, the community was incorporated in 1893. In 1872 the first school in Wheeler County was established near Mitchell, and in 1874 it was relocated into the town itself. Early town Over the next two decades, Mitchell grew to include a store, assay office, two churches, two hotels, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oregon Route 218
Oregon Route 218 (OR 218) is an Oregon state highway that runs between the small towns of Shaniko and Fossil in north-central Oregon and is known as the Shaniko-Fossil Highway No. 291 (see Oregon highways and routes). OR 218 is a part of the Journey Through Time Scenic Byway, an Oregon state byway. Route description OR 218 is a fairly short rural highway. Its western terminus is in Wasco County, in the ghost town of Shaniko at U.S. Route 97. The road is very windy and hilly over its entire length and is a popular destination for motorcyclists. It runs through the small town of Antelope (population 50) and has a junction with OR 293 on the south end of town. More mountainous terrain follows, and the highway crosses the John Day River into Wheeler County at Clarno. Just east of Clarno is the Clarno Unit of the John Day Fossil Beds National Monument. Between Clarno and Fossil (the largest town on the route, with a population of about 475), the road has several sharp curves, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossil, Oregon
Fossil is a city in and the county seat of Wheeler County, Oregon, United States. The name was chosen by the first postmaster, Thomas B. Hoover, who had found some fossil remains on his ranch. The population was 473 at the 2010 census. History The Fossil post office was established on February 28, 1876, on Thomas Benton Hoover's ranch along Hoover Creek. He named the place ''Fossil'' after finding fossils in a clay-like rock formation on his ranch. In 1881, Hoover and Thomas Watson opened a store near the confluence of Butte and Cottonwood creeks and moved the post office to the store. When the city was incorporated in 1891, Hoover became the first mayor. After creating Wheeler County in 1899, the Oregon Legislature chose Fossil as the temporary county seat. A county-wide election held in 1900 to determine the permanent county seat yielded 436 votes for Fossil, 267 for Twickenham, and 82 for Spray. Winlock W. Steiwer and George S. Carpenter founded Steiwer & Carpenter Bank, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clarno Unit Map
Clarno may refer to: Locations * Clarno, Oregon * Clarno, Wisconsin ** Clarno (community), Wisconsin *Clarno Township, Lake County, South Dakota Other * Clarno Formation Clarno may refer to: Locations * Clarno, Oregon * Clarno, Wisconsin ** Clarno (community), Wisconsin *Clarno Township, Lake County, South Dakota Lake County is a county in the U.S. state of South Dakota. As of the 2020 United States Census, t ..., an Eocene geologic formation in Central Oregon * Beverly Clarno, politician in the U.S. state of Oregon {{disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blue Mountains (Oregon)
The Blue Mountains are a mountain range in the northwestern United States, located largely in northeastern Oregon and stretching into extreme southeastern Washington. The range has an area of about , stretching east and southeast of Pendleton, Oregon, to the Snake River along the Oregon–Idaho border. The Blue Mountains cover ten counties across two states; they are Union, Umatilla, Grant, Baker, Wallowa and Harney counties in Oregon, and Walla Walla, Columbia, Garfield and Asotin counties in Washington. The mountains are unique as the home of the world's largest living organism, a subterranean colonial mycelial mat of the fungus ''Armillaria ostoyae''. The Blue Mountains were named after the color of the mountains when seen from a distance. Geology The Blues are uplift mountainscbgwma.orThe Columbia River Basalt Group , Continental flood basalt flows , cbgwma.org accessdate: February 8, 2017 and contain some of the oldest rocks in Oregon. Rocks as old as 400 million yea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ochoco Mountains
The Ochoco Mountains are a mountain range in central Oregon in the United States, located at the western end of the Blue Mountains. They were formed when Permian, Triassic, and Jurassic rocks were slowly uplifted by volcanic eruptions to form the Clarno Formation. Today, the highest point in the range is Lookout Mountain. The dominant vegetation on the west side of the range is old-growth ponderosa pine; on the east side, western juniper is common. The western area of the mountains is administered by the Ochoco National Forest, while the southeastern section is part of the Malheur National Forest. The Ochoco Mountains are used for hiking, camping, bird watching, rockhounding, and hunting, as well as cross-country skiing in the winter. Geography The Ochoco Mountains run north to south and east to west. The eight highest peaks in the range are: * Lookout Mountain, * Spanish Peak, * Mount Pisgah, * Round Mountain, * East Point, * North Point, * Wolf Mountain, * View ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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