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Bijou Creek
Bijou Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed March 25, 2011 tributary of the South Platte River in Colorado. The creek flows northeast from elevated terrain in southeastern Adams County to a confluence with the South Platte near Fort Morgan. Bijou Creek is subject to flash floods from time to time. Bijou Creek, originally named Bijeau Creek, was named for Joseph Bijeau Joseph Bijeau (1778–after 1837), also known as Joseph Bijeau dit Bissonet and Joseph Bissonet, was among the earliest fur trappers of the Rocky Mountains. He was a guide for Stephen Harriman Long's expedition of the Great Plains in 1820. A fur ..., a guide on Stephen Harriman Long's expedition of the Great Plains in 1820. The alluvium that irrigators in the lower Bijou Basin drew water from since 1935 when the first wells were dug is deposited in a shallow channel eroded in Pierre Shale which is flanked on its sides by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Platte River
The South Platte River is one of the two principal tributaries of the Platte River. Flowing through the U.S. states of Colorado and Nebraska, it is itself a major river of the American Midwest and the American Southwest/ Mountain West. Its drainage basin includes much of the eastern flank of the Rocky Mountains in Colorado, much of the populated region known as the Colorado Front Range and Eastern Plains, and a portion of southeastern Wyoming in the vicinity of the city of Cheyenne. It joins the North Platte River in western Nebraska to form the Platte, which then flows across Nebraska to the Missouri. The river serves as the principal source of water for eastern Colorado. In its valley along the foothills in Colorado, it has permitted agriculture in an area of the Colorado Piedmont and Great Plains that is otherwise arid. Description The river is formed in Park County, Colorado, southwest of Denver in the South Park grassland basin by the confluence of the Sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stephen Harriman Long
Stephen Harriman Long (December 30, 1784 – September 4, 1864) was an American army civil engineer, explorer, and inventor. As an inventor, he is noted for his developments in the design of steam locomotives. He was also one of the most prolific explorers of the early 1800s, although his career as an explorer was relatively short-lived. He covered over 26,000 miles in five expeditions, including a scientific expedition in the Great Plains area, which he famously confirmed as a "Great Desert" (leading to the term "the Great American Desert"). Biography Long was born in Hopkinton, New Hampshire, the son of Moses and Lucy (Harriman) Long. Long's Puritan ancestors came from England during the Puritan migration to New England. He received an A.B. from Dartmouth College in 1809 and an A.M. from Dartmouth in 1812. In 1814, he was commissioned a lieutenant of engineers in the U.S. Army Corps of Engineers. Upon the reorganization of the Army in 1816, he was appointed a Major on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Weld County, Colorado
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Colorado
This is a list of streams in the U.S. State of Colorado. __TOC__ Alphabetical list The following alphabetical list includes many important streams that flow through the State of Colorado, including all 158 named rivers. Where available, the total extent of the stream's drainage basin is shown after the name. The names of the 17 Colorado rivers with a drainage basin of more than 10,000 square kilometers (3,900 sq mi), about three times the area of Rhode Island, are shown in bold. #Adams Fork Conejos River #Alamosa River 383 km2 (148 mi2) # Animas River 3,562 km2 (1,375 mi2) #Apishapa River 2,798 km2 (1,080 mi2) # Arikaree River 4,429 km2 (1,710 mi2) #Arkansas River 478,501 km2 (184,750 mi2) # Aspen Brook # Bear Creek 4,500 km2 (1,737 mi2) # Bear Creek 339 km2 (131 mi2) # Bear River # Beaver Creek 2,939 km2 (1,135 mi2) # Big Dry Creek (Littleton, Colorado) # Big Dry Creek (Westminster, Colorado) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fox Hills Formation
The Fox Hills Formation is a Cretaceous geologic formation in the northwestern Great Plains of North America. It is present from Alberta on the north to Colorado in the south. Fossil remains of dinosaurs, including tyrannosaurs, as well as large marine reptiles, such as mosasaurs, have been recovered from the formation. Lithology The Fox Hills Formation consists of marginal marine yellow to grey sandstone with shale interbeds. It was deposited as a regressive sequence of barrier islands during the retreat of the Western Interior Seaway in Late Cretaceous time. In its eastern extents, the formation is underlain by the marine Pierre Shale in the United States and by the equivalent Bearpaw Formation in Canada, while in western ranges in Montana and Wyoming it overlies the Lewis Shale. The Fox Hills is overlain by continental sediments of the Laramie Formation in Colorado and the Lance Formation in Wyoming, the later being the equivalent of the overlying Hell Creek Formation in Mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pierre Shale
The Pierre Shale is a geologic formation or series in the Upper Cretaceous which occurs east of the Rocky Mountains in the Great Plains, from Pembina Valley in Canada to New Mexico. The Pierre Shale was described by Meek and Hayden in 1862 in the Proceedings of the Academy of Sciences (Philadelphia). They described it as a dark-gray shale, fossiliferous, with veins and seams of gypsum, and concretions of iron oxide. The Pierre Shale is about 700 feet (210m) thick at the type locality. It overlies the Niobrara division and underlies the Fox Hills beds. It was named for an occurrence near Fort Pierre on the Missouri River in South Dakota. The Pierre Shale is of marine origin and was deposited in the Western Interior Seaway. It is correlative with other marine shales that occur farther west, such as the Bearpaw Shale, Mancos Shale and the Lewis Shale. It correlates with the Lea Park Formation in central Alberta. The Pierre is overlain by marginal marine deposits of the F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stephen H
Stephen or Steven is a common English first name. It is particularly significant to Christians, as it belonged to Saint Stephen ( grc-gre, Στέφανος ), an early disciple and deacon who, according to the Book of Acts, was stoned to death; he is widely regarded as the first martyr (or " protomartyr") of the Christian Church. In English, Stephen is most commonly pronounced as ' (). The name, in both the forms Stephen and Steven, is often shortened to Steve or Stevie. The spelling as Stephen can also be pronounced which is from the Greek original version, Stephanos. In English, the female version of the name is Stephanie. Many surnames are derived from the first name, including Stephens, Stevens, Stephenson, and Stevenson, all of which mean "Stephen's (son)". In modern times the name has sometimes been given with intentionally non-standard spelling, such as Stevan or Stevon. A common variant of the name used in English is Stephan ; related names that have found some cur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Joseph Bijeau
Joseph Bijeau (1778–after 1837), also known as Joseph Bijeau dit Bissonet and Joseph Bissonet, was among the earliest fur trappers of the Rocky Mountains. He was a guide for Stephen Harriman Long's expedition of the Great Plains in 1820. A fur trapper and hunter, he lived among the Pawnee people. He was able to communicate to a number of Native American tribes through his use of sign language as well as the Crow language, which was used among a number of western tribes. After Spain lost the Mexican territory (present-day New Mexico), trappers like Bijeau moved to Taos where they could trap, trade, and travel east without the hostilities that they experienced in the western United States. Early years Joseph Bissonet was born on June 15, 1778, at St. Louis, Indian Reserve, a territory of the British America (1607–1783). His parents were Louis Bissonette and Genevieve, the daughter of Charles Routier who immigrated from Fort de Chartres to St. Louis in 1765. Bissonette was in St. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Platte River
The Platte River () is a major river in the State of Nebraska. It is about long; measured to its farthest source via its tributary, the North Platte River, it flows for over . The Platte River is a tributary of the Missouri River, which itself is a tributary of the Mississippi River which flows to the Gulf of Mexico. The Platte over most of its length is a broad, shallow, meandering stream with a sandy bottom and many islands—a braided stream. The Platte is one of the most significant tributary systems in the watershed of the Missouri, draining a large portion of the central Great Plains in Nebraska and the eastern Rocky Mountains in Colorado and Wyoming. The river valley played an important role in the westward expansion of the United States, providing the route for several major emigrant trails, including the Oregon, California, Mormon and Bozeman trails. The first Europeans to see the Platte were French explorers and fur trappers about 1714; they first called it the ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flash Flood
A flash flood is a rapid flooding of low-lying areas: washes, rivers, dry lakes and depressions. It may be caused by heavy rain associated with a severe thunderstorm, hurricane, or tropical storm, or by meltwater from ice or snow flowing over ice sheets or snowfields. Flash floods may also occur after the collapse of a natural ice or debris dam, or a human structure such as a man-made dam, as occurred before the Johnstown Flood of 1889. Flash floods are distinguished from regular floods by having a timescale of fewer than six hours between rainfall and the onset of flooding. Flash floods are a significant hazard, causing more fatalities in the U.S. in an average year than lightning, tornadoes, or hurricanes. Flash floods can also deposit large quantities of sediments on floodplains and can be destructive of vegetation cover not adapted to frequent flood conditions. Causes Flash floods most often occur in dry areas that have recently received precipitation, but th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Morgan, Colorado
Fort Morgan is the home rule municipality city that is the county seat and the most populous municipality of Morgan County, Colorado, United States. The city population was 11,597 at the 2020 United States Census. Fort Morgan is the principal city of the Fort Morgan, CO Micropolitan Statistical Area. History Fort Morgan Camp Wardwell was established in 1865 along the Overland Trail to protect emigrants and supplies going to and from Denver and the mining districts. The fort was renamed in 1866 by General John Pope for one of his staff, Colonel Christopher A. Morgan, who had died earlier that year. The fort closed in 1868 after being used by 19 different companies from 11 cavalry and infantry regiments (about 1,300 soldiers). Town The town of Fort Morgan was platted just south of the old military fort's ruins on May 1, 1884, by Abner S. Baker, a member of Greeley's Union Colony. The town became the county seat of the newly formed Morgan County on February 19, 1889. In W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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