|
Razor Hollow
Razor Hollow is a valley in northwest Shannon County in the U.S. state of Missouri. The intermittent stream in the hollow flows northeast and enters the Current River about two miles southeast of Cedargrove and the confluence In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); o ... of Big Creek with the Current.''Cedargrove, Missouri,'' 7.5 Minute Topographic Quadrangle, USGS, 1951 (1985 revision) The source area for the stream is at and the confluence with the Current is at at an elevation of . The ridges on either side of the narrow valley are at in elevation. Razor Hollow was so named on account of sharp rocks in the valley. References Valleys of Shannon County, Missouri Valleys of Missouri {{ShannonCountyMO-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shannon County, Missouri
Shannon County is a county in the southern portion of the U.S. state of Missouri. As of the 2020 census, the population was 7,031. Its county seat is Eminence. The county was officially organized on January 29, 1841, and was named in honor of George F. "Peg-Leg" Shannon, a member of the Lewis and Clark Expedition. It is the second-largest county by area in Missouri. Missouri's first copper mine was opened in Shannon County in 1846 and Missouri's only manganese mine was opened here during World War II. As of the 2000 census, Shannon County ranked 78th on the list of counties with the lowest per capita income and 46th on the list of counties with the lowest median household incomes in the United States, making it the poorest county in Missouri. History The Great Tri-State Tornado of March 18, 1925 appears to have begun in Moore Township; most likely as constituent tornadoes of a tornado family preceding the infamous very long tack tornado that went on to kill 695 people ac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Missouri
Missouri is a U.S. state, state in the Midwestern United States, Midwestern region of the United States. Ranking List of U.S. states and territories by area, 21st in land area, it is bordered by eight states (tied for the most with Tennessee): Iowa to the north, Illinois, Kentucky and Tennessee to the east, Arkansas to the south and Oklahoma, Kansas and Nebraska to the west. In the south are the Ozarks, a forested highland, providing timber, minerals, and recreation. The Missouri River, after which the state is named, flows through the center into the Mississippi River, which makes up the eastern border. With more than six million residents, it is the List of U.S. states and territories by population, 19th-most populous state of the country. The largest urban areas are St. Louis, Kansas City, Missouri, Kansas City, Springfield, Missouri, Springfield and Columbia, Missouri, Columbia; the Capital city, capital is Jefferson City, Missouri, Jefferson City. Humans have inhabited w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Intermittent Stream
Intermittent, temporary or seasonal rivers or streams cease to flow every year or at least twice every five years.(Tzoraki et al., 2007) Such rivers drain large arid and semi-arid areas, covering approximately a third of the earth's surface. The extent of temporary rivers is increasing, as many formerly perennial rivers are becoming temporary because of increasing water demand, particularly for irrigation. Despite inconsistent water flow, intermittent rivers are considered land-forming agents in arid regions, as they are agents of significant deposition and erosion during flood events. The combination of dry crusted soils and the highly erosive energy of the rain cause sediment resuspension and transport to the coastal areas.(Tzoraki et al., 2009) They are among the aquatic habitats most altered by human activities. During the summer even under no flow conditions the point sources are still active such as the wastewater effluents, resulting in nutrients and organic pollutants ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Current River (Ozarks)
The Current River forms in the southeastern portion of the Ozarks of Missouri and becomes a 7th order stream as it flows southeasterly out of the Ozarks into northeastern Arkansas where it becomes a tributary of the Black River, which is a tributary of the White River, a tributary of the Mississippi River. The Current River is approximately long and drains about of land mostly in Missouri and a small portion of land in northeastern Arkansas. The headwaters of the Current River are nearly above sea level, while the mouth of the river lies around above sea level. The basin drains a rural area that is dominated by karst topography, underlain by dolomite and sandstone bedrock with a small area of igneous rock southeast of Eminence, Missouri. The annual daily mean discharge of the river near Doniphan, Missouri is per second. In 1964, over 134 mi (160 km) of the upper course of the river and its tributaries were federally protected as the Ozark National Scenic Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cedargrove, Missouri
Cedargrove (sometimes spelled Cedar Grove) is an extinct town in the northwest corner of Shannon County, in the Ozarks of southern Missouri. The GNIS classifies it as a populated place. The community is located just south of the Shannon - Dent county line on the Current River, just north of the Big Creek confluence with the Current. It lies at the end of Missouri Route B, two miles east of the Shannon - Texas county line. A post office called Cedar Grove was established in 1890, the name was changed to Cedargrove in 1895, and the post office closed in 1957. The community was named for a grove of cedar Cedar may refer to: Trees and plants *''Cedrus'', common English name cedar, an Old-World genus of coniferous trees in the plant family Pinaceae *Cedar (plant), a list of trees and plants known as cedar Places United States * Cedar, Arizona * ... timber near the original town site. References Ghost towns in Missouri Ghost towns in Shannon County, Missouri {{Shan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Big Creek (Current River)
Big Creek is a stream in Shannon and Texas counties in the Ozarks of southern Missouri. It is a tributary of the Current River. The stream headwaters are in Texas County at and the confluence with the Current is in the northwest corner of Shannon County at . Cedargrove lies just north of the confluence. Razor Hollow flows parallel to the lower reaches of Big Creek and enters the Current about two miles southeast of Big Creek's confluence. Big Creek was so named on account of its size. See also *List of rivers of Missouri List of rivers in Missouri (U.S. state). By drainage basin This list is arranged by drainage basin, with respective tributaries indented under each larger stream's name. Mississippi River Arkansas River *Mississippi River **Arkansas River (AR ... References Rivers of Shannon County, Missouri Rivers of Texas County, Missouri Rivers of Missouri Tributaries of the Current River (Ozarks) {{Missouri-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Shannon County, Missouri
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
