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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 asb, Waną́be, lit=bear paws, cro, Daxpitcheeischikáate, lit=bear's little hand, and ats, ʔɔɔwɔ́hʔoouh, lit=there are many buttes. 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 Bearp ... [...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 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 *Sky island Sky islands are isolated mountains surrounded by radically different lowland environments. The term originally referred to those found on the Mexican Plateau, and has extended to similarly isolated high-elevation forests. The isolation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow 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 ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Ear ... [...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 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 used different from the preceding, 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," is in the Revised Version, "Have her forth between the ranks;" i.e., Jehoiada orders that Athaliah Athaliah ( el, Γοθολία ''Gotholía''; la, Athalia) was the daughter of ei ... [...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 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 ... [...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" means "mountainous" in Latin. Representative James Mitchell Ashley ( 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 official list of mountain ranges in the state. List of mountain ranges The mountain ranges below are listed by name, county, coordinates, and average elevation as recorded by the U.S. Geological Survey. Sub-ranges are indented below the name of the primary range. Some of these ranges ex ... [...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 Territory over the previous four months, the 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 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 traditional lands to a much smaller reservation in north central I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nelson Miles
Nelson Appleton Miles (August 8, 1839 – May 15, 1925) was an American military general who served in the American Civil War, the American Indian Wars, and the Spanish–American War. From 1895 to 1903, Miles served as the last Commanding General of the United States Army, before the office was retooled as Chief of Staff of the Army. Early life Miles was born in Westminster, Massachusetts, on his family's farm. He worked in Boston, read military history, and mastered military principles and techniques, including battle drills. He attended Fort Wayne College. Civil War Miles was working as a crockery store clerk in Boston when the American Civil War began. He entered the Union Army as a volunteer on September 9, 1861, and fought in many crucial battles. He became a lieutenant in the 22nd Regiment Massachusetts Volunteer Infantry and was commissioned a lieutenant colonel of the 61st New York Volunteer Infantry Regiment on May 31, 1862. He was promoted to colonel after the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nez Perce People
The Nez Percé (; autonym in Nez Perce language: , meaning "we, the people") are an Indigenous people of the Plateau who are presumed to have lived on the Columbia River Plateau in the Pacific Northwest region for at least 11,500 years.Ames, Kenneth and Alan Marshall. 1980. "Villages, Demography and Subsistence Intensification on the Southern Columbia Plateau". ''North American Archeologist'', 2(1): 25–52." Members of the 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 Nimiipuu 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, the high plains of Montana, and the northern Great Basin in southern Idaho and northern Nevada. Frenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chief Joseph
''Hin-mah-too-yah-lat-kekt'' (or ''Hinmatóowyalahtq̓it'' in Americanist orthography), popularly known as Chief Joseph, Young Joseph, or Joseph the Younger (March 3, 1840 – September 21, 1904), 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, to flee the United States ... [...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 sedime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Montana Alkalic Province
The central Montana Alkalic Province is located in the United States in central Montana. Montana is bordered by Idaho, Wyoming, North Dakota, South Dakota, and Canada to the north. Central Montana is unique when compared to the rest of the Rocky Mountains due to its east-west trend of tectonic features, including thrust fault zones, anticlines, and domes. The area of tectonic activity experienced conditions of plastic deformation, which affected the whole region. The Montana Alkalic Province consist of Cretaceous intrusions of monzonite and syenite as well as Cambrian limestone, sandstone, and siltstone. Most of the sedimentary rocks are a result of deposition from a terrestrial fluvial environment. Deposition included more than 13,000 feet of clastics that were later uplifted. The peak of this uplifting occurred during the Devonian. Deposition, uplift, and traps of carbonate shales have made central Montana prime for small-scale oil and gas production. Other geologic formations in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
