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Devil's Slide (Montana)
Devil's Slide is an unusual cliff rock formation on the side of Cinnabar Mountain located in Gallatin National Forest in Park County, Montana north of Yellowstone National Park. This distinctive formation can be viewed from Highway 89 and was created from alternate beds of limestone, sandstone, quartzites that have been tilted to lie nearly vertical and have eroded at different rates. History In 1871, very few white travellers had ventured this far south in the Yellowstone River valley. The Cook–Folsom–Peterson Expedition passed the Devil's Slide in 1869. Cook and Folsom described the slide in their diaries but did not name them In August 1870, the Washburn–Langford–Doane Expedition observed the formation and named it ''The Devil's Slide''. Langford described the formation in his ''Wonders of the Yellowstone'' published in the May 1871 edition of Scribner's Monthly: File:DevilsSlideLangford1871.JPG, 1871 illustration of Devil's Slide by Thomas Moran File:Devil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yellowstone River
The Yellowstone River is a tributary of the Missouri River, approximately long, in the Western United States. Considered the principal tributary of the upper Missouri, via its own tributaries it drains an area with headwaters across the mountains and Great Plains, high plains of southern Montana and northern Wyoming, and stretching east from the Rocky Mountains in the vicinity of Yellowstone National Park. It flows northeast to its confluence with the Missouri River on the North Dakota side of the border, about west of Williston, North Dakota, Williston. Etymology The name is widely believed to have been derived from the Hidatsa, Minnetaree Indian name ''Mi tse a-da-zi'' (Yellow Rock River) (Hidatsa language, Hidatsa: ''miʔciiʔriaashiish). Common lore recounts that the name was inspired by the yellow-colored rocks along the Grand Canyon of the Yellowstone, but the Minnetaree never lived along the upper stretches of the Yellowstone. Some scholars think that the river was inst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gallatin Range
The Gallatin Range is a mountain range of the Rocky Mountains, located in the U.S. states of Montana and Wyoming. It includes more than 10 mountains over . The highest peak in the range is Electric Peak at . The Gallatin Range was named after Albert Gallatin, the longest-serving US Secretary of the Treasury. The range extends north to south and averages in width. Geography The southernmost peaks of the range are in the northwestern section of Yellowstone National Park. However, the majority of the range is in Gallatin National Forest. The Yellowstone River flows north on the eastern flank of the range. The Madison Range parallels the Gallatins to the west. The northern end of the range is near Livingston, Montana and Bozeman Pass separates the Gallatins from the Bridger Mountains to the north. The range is an integral part of the Greater Yellowstone Ecosystem and has grizzly bears, wolves and other threatened and endangered species also found in Yellowstone National P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gallatin National Forest
The Gallatin National Forest (now known as the Custer-Gallatin National Forest) is a United States National Forest located in South-West Montana. Most of the Custer-Gallatin goes along the state's southern border, with some of it a part of North-West Wyoming. Geography The forest area comprises a total of with around located in the Gallatin Forest area and within the Custer. Most of the Gallatin borders Yellowstone National Park and is a part of the Greater Yellowstone Ecosystem, an area which encompasses almost in and around the park. The Custer National Forest is spread out along Eastern Montana and the North-West side of Wyoming, with most of its land being held in Montana. The forest stretches through about six counties, including Park, Gallatin, Sweet Grass, Madison, Carbon, and Meagher. There are six separate mountain ranges within the forest including the Gallatin, Madison, Bridger, Crazy, Absaroka, and Beartooth Ranges. The Beartooth's are home to Granit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Park County, Montana
Park County is a county in the U.S. state of Montana. At the 2020 census, the population was 17,191. Its county seat is Livingston. A small part of Yellowstone National Park is in the southern part of the county. History The Territorial Legislature of Montana Territory authorized Park County on February 23, 1887. It was named for its proximity to Yellowstone National Park, part of which is now in the county. This area had long been peopled and hunted by indigenous peoples, including the Crow, Sioux, and Blackfoot tribes. The first recorded visit of European-descent people was the Lewis and Clark Expedition (1805). Mountain man Jim Bridger wintered with Crow nomads near present-day Emigrant in 1844–45. Hunting and trapping brought many men across this area during the first part of the 19th century, but by 1850 the beaver population had nearly disappeared. Gold was discovered in Emigrant Gulch in 1863, and by 1864 a booming town was serving the area. In late 1864, Yellowst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yellowstone National Park
Yellowstone National Park is a List of national parks of the United States, national park of the United States located in the northwest corner of Wyoming, with small portions extending into Montana and Idaho. It was established by the 42nd United States Congress, 42nd U.S. Congress through 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 US, and is also widely understood to be the first national park in the world. The park is known for List of animals of Yellowstone, its wildlife and Geothermal areas of Yellowstone, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highway 89
A highway is any public or private road or other public way on land. It includes not just major roads, but also other public roads and rights of way. In the United States, it is also used as an equivalent term to controlled-access highway, or a translation for ''motorway'', ''Autobahn'', ''autostrada'', '' autoroute'', etc. According to Merriam-Webster, the use of the term predates the 12th century. According to Etymonline, "high" is in the sense of "main". In North American and Australian English, major roads such as controlled-access highways or arterial roads are often state highways (Canada: provincial highways). Other roads may be designated "county highways" in the US and Ontario. These classifications refer to the level of government (state, provincial, county) that maintains the roadway. In British English, "highway" is primarily a legal term. Everyday use normally implies roads, while the legal use covers any route or path with a public right of access, including foot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzites
Quartzite is a hard, non- foliated metamorphic rock that was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts, and hence quartzite is a metasandstone. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cook–Folsom–Peterson Expedition
The Cook–Folsom–Peterson Expedition of 1869 was the first organized expedition to explore the region that became Yellowstone National Park. The privately financed expedition was carried out by David E. Folsom, Charles W. Cook and William Peterson of Diamond City, Montana, a gold camp in the Confederate Gulch area of the Big Belt Mountains east of Helena, Montana. The journals kept by Cook and Folsom, as well as their personal accounts to friends were of significant inspirational value to spur the organization of the Washburn-Langford-Doane Expedition which visited Yellowstone in 1870. Expedition route The party of three explorers departed Diamond City, Montana on September 6, 1869, and traveled up the Missouri River to Three Forks, Montana. They then began the easterly march up the Gallatin Valley, stopping in Bozeman, Montana for supplies on September 8, 1869. From Bozeman, they moved to the shadows of Bozeman Pass, camping four miles east of Fort Ellis. On September ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Washburn–Langford–Doane Expedition
The Washburn Expedition of 1870 explored the region of northwestern Wyoming that two years later became Yellowstone National Park. Led by Henry D. Washburn and Nathaniel P. Langford, and with a U.S. Army escort headed by Lt. Gustavus C. Doane, the expedition followed the general course of the Cook–Folsom–Peterson Expedition made the previous year. During their explorations, members of the party made detailed maps and observations of the Yellowstone region, exploring numerous lakes, climbing several mountains, and observing wildlife. The expedition visited both the Upper and Lower Geyser Basins, and after observing the regularity of eruptions of one geyser, decided to name it Old Faithful, since it erupted about once every 74 minutes. One member of the expedition, Montana writer and lawyer Cornelius Hedges, later wrote a number of articles for a Helena, Montana-based newspaper, describing the things the expedition had witnessed. In discussions with other members of the pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thomas Moran
Thomas Moran (February 12, 1837 – August 25, 1926) was an American painter and printmaker of the Hudson River School in New York whose work often featured the Rocky Mountains. Moran and his family, wife Mary Nimmo Moran and daughter Ruth, took residence in New York where he obtained work as an artist. He was a younger brother of the noted marine artist Edward Moran, with whom he shared a studio. A talented illustrator and exquisite colorist, Thomas Moran was hired as an illustrator at '' Scribner's Monthly''. During the late 1860s, he was appointed the chief illustrator for the magazine, a position that helped him launch his career as one of the premier painters of the American landscape, in particular, the American West. Moran along with Albert Bierstadt, Thomas Hill, and William Keith are sometimes referred to as belonging to the Rocky Mountain School of landscape painters because of all of the Western landscapes made by this group. Biography Moran was born in Bolton, La ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
