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Druid Peak (film)
Druid Peak (elevation ) is a moderate domed peak on the southern flank of the Absaroka Range in Yellowstone National Park. The peak lies just north of the Lamar River and Soda Butte Creek confluence at the head of the Lamar Valley. Prior to 1885, this summit was named ''Soda Hill'' by members of the Hayden Geological Survey of 1878 and ''Mount Longfellow'' or ''Longfellows' Peak'' by then park superintendent Philetus Norris in 1880. In 1885, members of the Arnold Hague Geological Survey changed the name to Druid Peak for unknown reasons, but some historians believe it may have been the presence of Stonehenge like rock formations on its eastern face that prompted the name. Druid Peak is notable for its role in the reintroduction Species reintroduction is the deliberate release of a species into the wild, from captivity or other areas where the organism is capable of survival. The goal of species reintroduction is to establish a healthy, genetically diverse, self-sustainin . ...
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Yellowstone National Park
Yellowstone National Park is an American national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion. While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park ...
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Park County, Wyoming
Park County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 29,624. The county seat is Cody. Park County is a major tourism destination. The county has over 53 percent of Yellowstone National Park's land area. Many attractions abound, including the Buffalo Bill Historical Center, the Cody Stampede Rodeo, the Ghost Town of Kirwin, and the western museum Old Trail Town. History Wyoming gained separate territorial status in 1868. Before that, most of the state's area was included in either Laramie County (part of the Dakota Territory) or as unorganized territory within the Dakota Territory. Wyoming Territory was established on July 25, 1868, at which time Laramie County was assigned to this jurisdiction. The area now known as Park County was established as Carter County, then Sweetwater County. In 1884 it was assigned to Fremont County; this continued until 1896, when it was assigned to Big Horn County. Wyoming achieved statehood ...
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Absaroka Range
The Absaroka Range ( or ) is a sub-range of the Rocky Mountains in the United States. The range stretches about across the Montana–Wyoming border, and at its widest, forming the eastern boundary of Yellowstone National Park along Paradise Valley, and the western side of the Bighorn Basin. The range borders the Beartooth Mountains to the north and the Wind River Range to the south. The northern edge of the range rests along I-90 and Livingston, Montana. The highest peak in the range is Francs Peak, located in Wyoming at . There are 46 other peaks over . Geography The range is drained by the Yellowstone River and various tributaries, including the Bighorn River. Most of the range lies within protected lands including Yellowstone Park, the Absaroka-Beartooth Wilderness, North Absaroka Wilderness, Teton Wilderness, and Washakie Wilderness, spanning the Bridger-Teton National Forest, Custer National Forest, Gallatin National Forest, and Shoshone National Forest. U.S. Highway ...
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Lamar River
The Lamar River is a tributary of the Yellowstone River, approximately long, in northwestern Wyoming in the United States. The river is located entirely within Yellowstone National Park. History Prior to the 1884–85 Geological Survey of the park, the Lamar was known as the East Fork of the Yellowstone River. During that survey, Geologist Arnold Hague named the river for L.Q.C. (Lucius Quintius Cincinnatus) Lamar, then Secretary of the Interior (March 1885 – January 1888), and a former slaveholder and author of the Mississippi Ordinance of Secession. The Lamar Valley, or the ''Secluded Valley'' of Trapper Osborne Russell and other park features or administrative names which contain ''Lamar'' are derived from this original naming. Osborne Russell in his 1921 ''Journal of a Trapper'' described the Lamar as follows: In 1869, the Cook–Folsom–Peterson Expedition encountered the Lamar River (East Fork) just upstream from the canyon section flowing into the Yellowstone and ...
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Soda Butte Creek
Soda Butte Creek is an approximately long major tributary of the Lamar River in Yellowstone National Park. It is named for a now-extinct geyser (Soda Butte) near its mouth. Soda Butte and the creek were named by A. Bart Henderson, a Cooke City miner, in 1870. It rises just outside the northeast corner of the park on the southern slopes of the Absaroka Range near Cooke City, Montana. The Northeast East Entrance road parallels Soda Butte Creek for its entire length within the park. Soda Butte Creek is a popular angling destination for native Yellowstone cutthroat trout. Angling Soda Butte Creek is a popular angling destination for fly fisherman. It holds brook trout in it upper reaches, mostly cutthroat trout and a few rainbow trout in its lower section. Because of spring runoff, the creek is generally not fishable until mid-July. The National Park Service has made frequent changes to the regulations for the Lamar drainage, including Soda Butte, and in 2018 has made significant ...
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Ferdinand Vandeveer Hayden
Ferdinand Vandeveer Hayden (September 7, 1829 – December 22, 1887) was an American geologist noted for his pioneering surveying expeditions of the Rocky Mountains in the late 19th century. He was also a physician who served with the Union Army during the Civil War. Early life Ferdinand Hayden was born in Westfield, Massachusetts. As a young boy he was fascinated with all nature and wildlife, which led him into the field of medicine. He worked in Cleveland under Jared Potter Kirtland and thereafter in Albany, NY, where he worked under James Hall, of the ''Geological Survey of New York''. He graduated from Oberlin College in 1850 and from the Albany Medical College in 1853, where he attracted the notice of Professor James Hall, state geologist of New York, through whose influence he was induced to join in an exploration of Nebraska Territory, with Fielding B. Meek to study geology and collect fossils. Hall sent him on his first geological venture in the summer of 1853. Be ...
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Philetus Norris
Philetus W. Norris (August 17, 1821 – January 14, 1885) was the second superintendent of Yellowstone National Park and was the first person to be paid for that position. Early life Philetus Walter Norris was born in Palmyra, New York on August 17, 1821, the son of John Norris, Jr. and Azubah Phelps.Senator Robert P. Griffin
placed into the Congressional Record on June 26, 1972.
His father was a pioneer mill-builder, and had fought in the . In the early 1820s, the family moved to Allegheny County in New York.Norris family genea ...
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Arnold Hague
Arnold Hague (December 3, 1840 in Boston, Massachusetts – May 14, 1917 in Washington, D.C.) was a United States geologist who did many geological surveys in the U.S., of which the best known was that for Yellowstone National Park. He also had assignments in China and Guatemala. He became a member of the U. S. Geological Survey in 1879 when it was first organized. Biography Hague was the son of William Hague, a clergyman. He graduated from Sheffield Scientific School at Yale University in 1863. He then spent three years in Germany, studying at the universities of Göttingen and Heidelberg, and at the Freiberg Mining Academy. In 1867 he returned to the United States, and was appointed assistant geologist on the U. S. geological exploration of the 40th parallel under Clarence King. He then went to California, and spent the winter of 1867/68 in Virginia City, Nevada, studying the surface geology of the Comstock Lode and the chemistry of the amalgamation process as practised there, ...
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Stonehenge
Stonehenge is a prehistoric monument on Salisbury Plain in Wiltshire, England, west of Amesbury. It consists of an outer ring of vertical sarsen standing stones, each around high, wide, and weighing around 25 tons, topped by connecting horizontal lintel stones. Inside is a ring of smaller bluestones. Inside these are free-standing trilithons, two bulkier vertical sarsens joined by one lintel. The whole monument, now ruinous, is aligned towards the sunrise on the summer solstice. The stones are set within earthworks in the middle of the densest complex of Neolithic and Bronze Age monuments in England, including several hundred ''tumuli'' (burial mounds). Archaeologists believe that Stonehenge was constructed from around 3000 BC to 2000 BC. The surrounding circular earth bank and ditch, which constitute the earliest phase of the monument, have been dated to about 3100 BC. Radiocarbon dating suggests that the first bluestones were raised between 2400 and 2200 BC, althou ...
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History Of Wolves In Yellowstone
The history of wolves in Yellowstone includes the extirpation, absence and reintroduction of wild populations of the gray wolf (''Canis lupus'') to Yellowstone National Park and the Greater Yellowstone Ecosystem. When the park was created in 1872, wolf populations were already in decline in Montana, Wyoming and Idaho. The creation of the national park did not provide protection for wolves or other predators, and government predator control programs in the first decades of the 1900s essentially helped eliminate the gray wolf from Yellowstone. The last wolves were killed in Yellowstone in 1926. After that, sporadic reports of wolves still occurred, but scientists confirmed that sustainable wolf populations had been extirpated and were absent from Yellowstone during the mid-1900s. Beginning in the 1940s, park managers, biologists, conservationists, and environmentalists began what would ultimately turn into a campaign to reintroduce the gray wolf into Yellowstone National Park. When ...
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Mountains And Mountain Ranges Of Yellowstone National Park
Yellowstone National Park, located primarily in the U.S. state of Wyoming, though the park also extends into Montana and Idaho and its Mountains and Mountain Ranges are part of the Rocky Mountains. There are at least 70 named mountain peaks over in Yellowstone in four mountain ranges. Two of the ranges—The Washburn Range and the Red Mountains—are minor and completely enclosed within park boundaries. The other two ranges are major, multi-state ranges that extend far beyond the boundaries of the park. The Gallatin Range begins approximately north of Yellowstone near Bozeman, Montana, and dominates the northwest corner of the park. The Absaroka Range, the largest range in the park, begins approximately north of the park near Livingston, Montana, along the Yellowstone River and runs southeast into, then south through the entire eastern side of the park to the Gros Ventre Range in Wyoming. The highest peak in the park, Eagle Peak is in the Absaroka Range. Yellowstone als ...
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Mountains Of Wyoming
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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