In Canada the term is little used; Natural Resources Canada, the government department responsible for official mapping and equivalent to the United States Geological Survey, treats the Interior Plains as one unit consisting of several related plateaux and plains. There is no region referred to as the "Great Plains" in ''The Atlas of Canada''. In terms of human geography, the term ''prairie'' is more commonly used in Canada, and the region is known as the Prairie Provinces or simply "the Prairies."
The North American Environmental Atlas, produced by the Commission for Environmental Cooperation, a NAFTA agency composed of the geographical agencies of the Mexican, American, and Canadian governments uses the "Great Plains" as a ecoregion synonymous with prairies and grasslands rather than as physiographic region defined by topography.
The region is about east to west and north to south. Much of the region was home to American Bison herds until they were hunted to near extinction during the mid/late 19th century. It has an area of approximately . Current thinking regarding the geographic boundaries of the Great Plains is shown by this map at the Center for Great Plains Studies, University of Nebraska–Lincoln.
The term "Great Plains", for the region west of about the 96th or 98th meridian and east of the Rocky Mountains, was not generally used before the early 20th century. Nevin Fenneman's 1916 study, ''Physiographic Subdivision of the United States'', brought the term Great Plains into more widespread usage. Before that the region was almost invariably called the High Plains, in contrast to the lower Prairie Plains of the Midwestern states. Today the term "High Plains" is used for a subregion of the Great Plains.
The High Plains is used in a related, more general context to describe the elevated regions of the Great Plains, which are primarily west of the 100th meridian in the US.
During the Cretaceous Period (145-65 million years ago), the Great Plains was covered by a shallow inland sea called the Western Interior Seaway. However, during the Late Cretaceous to the Paleocene (65-55 million years ago), the seaway had begun to recede, leaving behind thick marine deposits and a relatively flat terrain where the seaway had once occupied.
Paleontological finds in the area have yielded bones of woolly mammoths, saber toothed tigers and other ancient animals, as well as dozens of other megafauna (large animals over ) – such as giant sloths, horses, mastodons, and American lion – that dominated the area of the ancient Great Plains for millions of years. The vast majority of these animals went extinct in North America around 13,000 years ago during the end of the Pleistocene.
The 100th meridian roughly corresponds with the line that divides the Great Plains into an area that receive or more of rainfall per year and an area that receives less than . In this context, the High Plains, as well as Southern Alberta, south-western Saskatchewan and Eastern Montana are mainly semi-arid steppe land and are generally characterised by rangeland or marginal farmland. The region (especially the High Plains) is periodically subjected to extended periods of drought; high winds in the region may then generate devastating dust storms. The eastern Great Plains near the eastern boundary falls in the humid subtropical climate zone in the southern areas, and the northern and central areas fall in the humid continental climate.
The first Americans (Paleo-Indians) who arrived to the Great Plains were successive indigenous cultures who are known to have inhabited the Great Plains for thousands of years, perhaps 10,000 years. Humans entered the North American continent in waves of migration, mostly over Beringia, the Bering Straits land bridge.
Historically the Great Plains were the range of the bison and of the culture of the Plains Indians, whose tribes included the Blackfoot, Crow, Sioux, Cheyenne, Arapaho, Comanche, and others. Eastern portions of the Great Plains were inhabited by tribes who lived in semipermanent villages of earth lodges, such as the Arikara, Mandan, Pawnee and Wichita.
Over the next one hundred years, founding of the fur trade brought thousands of ethnic Europeans into the Great Plains. Fur trappers from France, Spain, Britain, Russia and the young United States made their way across much of the region, making regular rendezvous with Native Americans and fur traders. After the United States acquired the Louisiana Purchase in 1803 and conducted the Lewis and Clark Expedition in 1804-1806, more information about the Plains became available and various pioneers entered the areas. Manuel Lisa, based in St. Louis, established a major fur trading site at his Fort Lisa on the Missouri River in Nebraska. Fur trading posts were often the basis of later settlements. Through the 19th century, more European Americans and Europeans migrated to the Great Plains as part of a vast westward expansion of population. New settlements became dotted across the Great Plains.
The new immigrants also brought diseases against which the Native Americans had no resistance. According to the Institute of Medicine (IOM), "between one-half and two-thirds of the Plains Indians had died of smallpox by the time of the Louisiana Purchase."
Much of the Great Plains became open range, hosting ranching operations where anyone was theoretically free to run cattle. In the spring and fall, ranchers held roundups where their cowboys branded new calves, treated animals and sorted the cattle for sale. Such ranching began in Texas and gradually moved northward. Cowboys drove Texas cattle north to railroad lines in the cities of Dodge City, Kansas and Ogallala, Nebraska; from there, cattle were shipped eastward. Many foreign, especially British, investors financed the great ranches of the era. Overstocking of the range and the terrible winter of 1886 resulted in a disaster, with many cattle starved and frozen to death. From then on, ranchers generally raised feed to ensure they could keep their cattle alive over winter.
To allow for agricultural development of the Great Plains and house a growing population, the US passed the Homestead Act of 1862: it allowed a settler to claim up to of land, provided that he lived on it for a period of five years and cultivated it. The provisions were expanded under the Kinkaid Act to include a homestead of an entire section. Hundreds of thousands of people claimed such homesteads, sometimes building sod houses out of the very turf of their land. Many of them were not skilled dryland farmers and failures were frequent. Much of the Plains were settled during relatively wet years. Government experts did not understand how farmers should cultivate the prairies and gave advice counter to what would have worked. Germans from Russia who had previously farmed in familiar circumstances in what is now Ukraine were marginally more successful than the average homesteader. The Dominion Lands Act of 1871 served a similar function for establishing homesteads on the prairies in Canada.
From the 1950s on, many areas of the Great Plains have become productive crop-growing areas because of extensive irrigation on large landholdings. The southern portion of the Great Plains lies over the Ogallala Aquifer, a huge underground layer of water-bearing strata dating from the last ice age. Center pivot irrigation is used extensively in drier sections of the Great Plains, resulting in aquifer depletion at a rate that is greater than the ground's ability to recharge.
The rural Plains have lost a third of their population since 1920. Several hundred thousand square miles of the Great Plains have fewer than six persons per square mile—the density standard Frederick Jackson Turner used to declare the American frontier "closed" in 1893. Many have fewer than two persons per square mile.
There are more than 6,000 ghost towns in the state of Kansas alone, according to Kansas historian Daniel Fitzgerald. This problem is often exacerbated by the consolidation of farms and the difficulty of attracting modern industry to the region. In addition, the smaller school-age population has forced the consolidation of school districts and the closure of high schools in some communities. The continuing population loss among European Americans has led some to suggest that the current use of the drier parts of the Great Plains is not sustainable. One concept has been to propose restoration of large parts of the Plains to native grassland, accompanied by restocking of bison. This proposal is known as Buffalo Commons. Native American tribes are among those devoted to breeding and raising bison.
Category:Plains of Canada Category:Plains of the United States Category:Physiographic provinces Category:Regions of the Western United States
af:Groot Vlaktes ar:السهول الكبرى bn:গ্রেট প্লেইন্স bs:Velika nizina ca:Grans Planes cs:Velké planiny cy:Gwastadeddau Mawr da:Great Plains de:Great Plains et:Suur tasandik es:Grandes Llanuras eo:Nordamerikaj Grandaj Ebenaĵoj eu:Zabaldi handiak fo:Stóru Grasfløturnar fr:Grandes Plaines fy:Great Plains gl:Grandes Planicies ko:그레이트플레인스 hi:कनाडा तथा संयुक्त राज्य अमेरिका का ग्रेट प्लेन hr:Velika nizina is:Slétturnar miklu it:Grandi Pianure he:המישורים הגדולים kk:Ұлы жазықтар lv:Lielie līdzenumi lt:Didžiosios lygumos nl:Great Plains ja:グレートプレーンズ no:Great Plains pnb:عظیم میدان pl:Wielkie Równiny pt:Grandes Planícies ru:Великие Равнины simple:Great Plains sk:Veľké prérie sr:Велика равница sh:Velika nizina fi:Suuret tasangot sv:Great Plains tt:Бөек тигезлекләр tr:Büyük Düzlükler uk:Великі Рівнини ur:عظیم میدان vi:Đại Bình nguyên Bắc Mỹ zh:大平原This text is licensed under the Creative Commons CC-BY-SA License. This text was originally published on Wikipedia and was developed by the Wikipedia community.
In Persia, the title "the Great" at first seems to be a colloquial version of the Old Persian title "Great King". This title was first used by the conqueror Cyrus II of Persia.
The Persian title was inherited by Alexander III of Macedon (336–323 BC) when he conquered the Persian Empire, and the epithet "Great" eventually became personally associated with him. The first reference (in a comedy by Plautus) assumes that everyone knew who "Alexander the Great" was; however, there is no earlier evidence that Alexander III of Macedon was called "''the Great''".
The early Seleucid kings, who succeeded Alexander in Persia, used "Great King" in local documents, but the title was most notably used for Antiochus the Great (223–187 BC).
Later rulers and commanders began to use the epithet "the Great" as a personal name, like the Roman general Pompey. Others received the surname retrospectively, like the Carthaginian Hanno and the Indian emperor Ashoka the Great. Once the surname gained currency, it was also used as an honorific surname for people without political careers, like the philosopher Albert the Great.
As there are no objective criteria for "greatness", the persistence of later generations in using the designation greatly varies. For example, Louis XIV of France was often referred to as "The Great" in his lifetime but is rarely called such nowadays, while Frederick II of Prussia is still called "The Great". A later Hohenzollern - Wilhelm I - was often called "The Great" in the time of his grandson Wilhelm II, but rarely later.
Category:Monarchs Great, List of people known as The Category:Greatest Nationals Category:Epithets
bs:Spisak osoba znanih kao Veliki id:Daftar tokoh dengan gelar yang Agung jv:Daftar pamimpin ingkang dipun paringi julukan Ingkang Agung la:Magnus lt:Sąrašas:Žmonės, vadinami Didžiaisiais ja:称号に大が付く人物の一覧 ru:Великий (прозвище) sl:Seznam ljudi z vzdevkom Veliki sv:Lista över personer kallade den store th:รายพระนามกษัตริย์ที่ได้รับสมัญญานามมหาราช vi:Đại đếThis text is licensed under the Creative Commons CC-BY-SA License. This text was originally published on Wikipedia and was developed by the Wikipedia community.
{{infobox musical artist | name | Chris Letchford | image ScaleTheSummit121509-Letchford.jpg | alt | caption Chris Letchford playing live with Scale the Summit | image_size | background non_vocal_instrumentalist | birth_name | alias | birth_date October 07, 1984 | birth_place | death_date | death_place | origin Houston, Texas | instrument Guitar | genre Progressive metal, instrumental rock | occupation Musician, music teacher | years_active 1992-Present | label Prosthetic Records | associated_acts Scale the Summit | Url | notable_instruments Mike Sherman custom 8-string, Strandberg headless 7-string }} |
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Chris Letchford (born October 7, 1984) is an American guitarist from Houston, Texas. He is the lead guitarist in the progressive metal band Scale the Summit. He has been recognized for his technical ability in magazines such as Guitar World, Revolver Magazine, and All Metal Resourse.
While at the Musicians Institute, he formed Scale the Summit with friend and fellow guitarist Travis Levrier, and drummer Pat Skeffington, who they met there in 2004. They added bassist Jordan Eberhardt to complete the lineup.
Category:Progressive metal guitarists Category:Eight-string guitarists Category:Musicians from Houston, Texas Category:Living people Category:1984 births
This text is licensed under the Creative Commons CC-BY-SA License. This text was originally published on Wikipedia and was developed by the Wikipedia community.
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