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Bear Paw Mountains
The Bears Paw Mountains (Bear Paw Mountains, Bear's Paw Mountains or Bearpaw Mountains) are an insular-montane island range in the Central Montana Alkalic Province in north-central Montana, United States, located approximately 10 miles south of Havre, Montana. Baldy Mountain, which rises above sea level, is the highest peak in the range. The Bears Paw Mountains extend in a 45-mile arc between the Missouri River and Rocky Boy Indian Reservation south of Havre. Name Locals refer to the range as the Bearpaws. Indigenous names include , , and . While highway signs designate the range as the Bears Paw Mountains, historically, the names Bearpaw Mountains and Bear Paw Mountains also have been used, including on early state maps of the region. The U.S. Geological Survey continues to use Bearpaw Mountains on publications. Geology The core of the Bearpaws are composed of extensive Eocene aged igneous intrusions left over from one of the largest eruptive centers in the Central Montan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Island Range
An island range is a mountain range that exists in total or almost total isolation from a larger chain of ranges and sub-ranges. From a distance on the plains, these ranges appear as "islands" of higher ground. They are often described as islands of mountainous land because they exist in the "sea" of lower elevation and flatter prairie country; many examples are found in the northern Rocky Mountains of the United States. Island ranges include the Big Snowy Mountains of east-central Montana, the Crazy Mountains of south-central Montana, or the Wichita Mountains The Wichita Mountains are located in the southwestern portion of the U.S. state of Oklahoma. It is the principal relief system in the Southern Oklahoma Aulacogen, being the result of a failed continental rift. The mountains are a northwest-south ... of southwestern Oklahoma. Island ranges, due to their isolation, often have animal and/or plant species or subspecies found nowhere else. See also * Island biogeography ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bearpaw Formation
The Bearpaw Formation, also called the Bearpaw Shale, is a geologic formation of Late Cretaceous (Campanian) age. It outcrops in the U.S. state of Montana, as well as the Canadian provinces of Alberta and Saskatchewan, and was named for the Bear Paw Mountains in Montana. It includes a wide range of marine fossils, as well as the remains of a few dinosaurs. It is known for its fossil ammonites, some of which are mined in Alberta to produce the organic gemstone ammolite. Lithology and depositional environment The formation was deposited in the Bearpaw Sea, which was part of the Western Interior Seaway that advanced and then retreated across the region during Campanian time. It is composed primarily of dark grey shales, claystones, silty claystones and siltstones, with subordinate silty sandstones. It also includes bedded and nodular concretions (both calcareous and ironstone concretions) and thin beds of bentonite. As the seaway retreated toward the southwest, the marine s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Blaine County, Montana
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic wate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ranges Of The Rocky Mountains
In the Hebrew Bible and in the Old Testament, the word ranges has two very different meanings. Leviticus In Leviticus 11:35, ranges (כירים) probably means a cooking furnace for two or more pots, as the Hebrew word here is in the dual number; or perhaps a fireplace fitted to receive a pair of ovens. 2 Kings In 2 Kings 11:8, the Hebrew word is here different from the preceding: שדרות, meaning "ranks of soldiers." The Levites were appointed to guard the king's person within the temple (2 Chronicles 23:7), while the soldiers were his guard in the court, and in going from the temple to the palace. The soldiers are here commanded to slay any one who should break through the "ranks" (as rendered in the Revised Version) to come near the king. In 2 Kings 11:15, the expression, "Have her forth without the ranges (לשדרת)," is in the Revised Version, "Have her forth between the ranks;" i.e., Jehoiada orders that Athaliah Athaliah ( ''Gotholía''; ) was the daughter of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Montana
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 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 climate, mountains t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountain Ranges In Montana
This is a list of mountain ranges in the state of Montana. Montana is the fourth largest state in the United States and is well known for its mountains. The name "Montana" is Spanish Spanish might refer to: * Items from or related to Spain: **Spaniards are a nation and ethnic group indigenous to Spain **Spanish language, spoken in Spain and many countries in the Americas **Spanish cuisine **Spanish history **Spanish culture ... for "Mountain". Representative James Mitchell Ashley (Republican Party (United States), R-Ohio), suggested the name when legislation organizing the territory was passed by the United States Congress in 1864. Ashley noted that a mining camp in the Colorado Territory had already used the name, and Congress agreed to use the name for the new territory. According to the United States Board on Geographic Names, there are at least 100 named mountain ranges and sub-ranges in Montana. However, mountain ranges have no official boundaries, and there is no offic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Battle Of Bear Paw
The Battle of Bear Paw (also sometimes called Battle of the Bears Paw or Battle of the Bears Paw Mountains) was the final engagement of the Nez Perce War of 1877. Following a running fight from North Central Idaho, north central Idaho Territory over the previous four months, the United States Army, U.S. Army managed to corner most of the Nez Perce led by Chief Joseph in early October 1877 in northern Montana Territory, just south of the border with Canada, where the Nez Perce intended to seek refuge from persecution by the U.S. government. Although some of the Nez Perce were able to escape to Canada, Chief Joseph was forced to surrender the majority of his followers to Brigadier General Oliver Otis Howard, Oliver Howard and Colonel Nelson A. Miles on October 5. Today, the battlefield is part of the Nez Perce National Historical Park and the Nez Perce National Historic Trail. Background In June 1877, several bands of the Nez Perce, resisting relocation from their traditi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nelson Miles
Nelson Appleton Miles (August 8, 1839 – May 15, 1925) was a United States Army officer who served in the American Civil War (1861–1865), the later American Indian Wars (1840–1890), and the Spanish–American War, (1898). From 1895 to 1903, Miles served as the last Commanding General of the United States Army, before the office was transformed into the current Chief of Staff of the U.S. Army in 1903. Early life Nelson A. Miles was born on his family's farm in Westminster, Massachusetts on August 8, 1839, the son of Daniel Miles and Mary (Curtis) Miles. He was raised and educated in Westminster, and attended the academy run by educator John R. Galt. Having decided on a business career, as a teenager, he moved to Boston, where he worked as a clerk in the John Collamore & Company crockery store. While living in Boston, he also attended Comer's Commercial College, a business school that offered night courses. With the outbreak of the American Civil War likely, Miles was amon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nez Perce People
The Nez Perce (; Exonym and endonym, autonym in Nez Perce language: , meaning 'we, the people') are an Indigenous people of the Plateau who still live on a fraction of the lands on the southeastern Columbia River Plateau in the Pacific Northwest. This region has been occupied for at least 11,500 years.Ames, Kenneth and Alan Marshall. 1980. "Villages, Demography and Subsistence Intensification on the Southern Columbia Plateau". ''North American Archaeologist'', 2(1): 25–52." Members of the Sahaptian languages, Sahaptin language group, the Nimíipuu were the dominant people of the Columbia Plateau for much of that time, especially after acquiring the horses that led them to breed the Appaloosa horse in the 18th century. Prior to first contact with European colonial people the Nimíipuu were economically and culturally influential in trade and war, interacting with other indigenous nations in a vast network from the western shores of Oregon and Washington (state), Washington, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chief Joseph
''Hin-mah-too-yah-lat-kekt'' (or ''hinmatóowyalahtq̓it'' in Americanist orthography; March 3, 1840 – September 21, 1904), popularly known as Chief Joseph, Young Joseph, or Joseph the Younger, was a leader of the wal-lam-wat-kain (Wallowa) band of Nez Perce, a Native American tribe of the interior Pacific Northwest region of the United States, in the latter half of the 19th century. He succeeded his father Tuekakas (Chief Joseph the Elder) in the early 1870s. Chief Joseph led his band of Nez Perce during the most tumultuous period in their history, when they were forcibly removed by the United States federal government from their ancestral lands in the Wallowa Valley of northeastern Oregon onto a significantly reduced reservation in the Idaho Territory. A series of violent encounters with white settlers in the spring of 1877 culminated in those Nez Perce who resisted removal, including Joseph's band and an allied band of the Palouse tribe, fleeing the United States in a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
