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Gasconade River
The Gasconade River is about longU.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed May 31, 2011 and is located in central and south-central Missouri. The Gasconade River begins in the Ozarks southeast of Hartville in Wright County and flows generally north-northeastwardly through Wright, Laclede, Pulaski, Phelps, Maries, Osage and Gasconade counties, through portions of the Mark Twain National Forest. It flows into the Missouri River near the town of Gasconade in Gasconade County. At Rich Fountain, the river has a mean annual discharge of 3,097 cubic feet per second. Name The name Gasconade is derived from "Gascon", an inhabitant of the French region of Gascony. The people of that province were noted for their boastfulness. It was applied by the early French to the Indians living on its banks who bragged about their exploits. The name means to boast or brag, and thus the river received its name. The waters of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seymour, Missouri
Seymour is a city in southeastern Webster County, Missouri, United States. The population was 1,921 at the 2010 census. It is part of the Springfield, Missouri Metropolitan Statistical Area. History Seymour was laid out in 1882. The town was named by Mr. T.P. Crabbe after Seymour, Indiana. A post office called Seymour has been in operation since 1881. The Col. Thomas C. Love House was listed on the National Register of Historic Places in 1985. Geography Seymour is located on the southeastern edge of the Springfield Plateau in the Ozarks. Streams to the east flow into the Gasconade River, the headwaters of the James River lie to the north and Finley Creek drains the south side of the town. US 60 passes the north side of the town and Missouri routes K, C and BB serve the town. The community of Diggins is 4.5 miles to the west and Mansfield is 10 miles to the east along Route 60. The Burlington Northern Santa Fe railroad's single-tracked Springfield-Memphis line runs t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Texas County, Missouri
Texas County is a county located in the southern portion of the U.S. state of Missouri. As of the 2020 census, the population was 24,487. Its county seat is Houston. The county was organized in 1843 as Ashley County, changing its name in 1845 to Texas, after the Republic of Texas. The 2010 U.S. Census indicates that the county was the center of population for the United States. History Texas County was created in 1843 and named for William H. Ashley, the first lieutenant governor of Missouri. It was later organized on February 14, 1845, when it was also renamed for the Republic of Texas. A seat of justice for the county was laid out in 1846 near the center of the county on Brushy Creek and named Houston for the first president of the Texas Republic. The historic Texas County Courthouse, built in 1932, was the county's sixth and now serves as the county administrative center. It was remodeled in 1977 and again in 2007. A new justice center was completed in 2008. Rugged hill ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Big Piney River
The Big Piney River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed May 31, 2011 tributary of the Gasconade River in south central Missouri in the United States. Via the Gasconade and Missouri rivers, it is part of the Mississippi River basin. The stream headwaters are located in southwest Texas County just north of the community of Dunn and U. S. Route 60. The stream flows east and southeast passing just south of Cabool passing under Route 60 Business, Missouri Route 181 and U. S. Route 63. The stream course turns northeast and runs parallel to Route 63 passing under it three times before turning northwest to the north of Simmons. The stream meanders north passing under Missouri Route 17 to the west of Houston and east of Bucyrus. The stream continues north passing under Missouri Route 32 and on past Hazleton passing the Paddy Creek Recreation Area and the Slabtown Spring area. The stream enters southe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roubidoux Creek
Roubidoux Creek is a tributary to the Gasconade River in the Ozarks of south central Missouri named after French-Canadian fur trader Joseph Robidoux. It is long.U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed May 31, 2011 Due to its colder water temperatures, it is listed as a trout stream. Roubidoux Spring is a landmark that is nestled just south of downtown Waynesville. The creek cuts north through Fort Leonard Wood before crossing underneath Interstate 44 and into the city limits of Waynesville. The former townsite of Roubidoux is located at the confluence of the east and west forks of the Roubidoux at . The Roubidoux joins the Gasconade River just north of Waynesville, and the confluence can be seen from Missouri Route 17. The mouth of the creek is located at coordinates . It crosses under I-44 at .''Waynesville, Missouri,'' 7.5 Minute Topographic Quadrangle, USGS, 1954 (1985 rev.) See also *List of rivers of Mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osage Fork Gasconade River
The Osage Fork Gasconade River is a stream in Wright, Webster and Laclede counties in the Ozarks of southern Missouri. It is a tributary of the Gasconade River. The stream headwaters arise in Webster County near the intersection of Missouri routes C and P about seven miles north of Seymour.''Missouri Atlas & Gazetteer,'' DeLorme, 1998, First edition, p. 53, ''High Prairie, Missouri,'' 7.5 Minute Topographic Quadrangle, USGS, 1982 The stream flows north past High Prairie where it turns to the northwest. It flows under Missouri Route 38 about five miles east of Marshfield and turns to the northeast as it passes under Missouri Route DD. It passes about 3.5 miles east of Niangua and continues to the northeast passing under Missouri Route ZZ just west of Rader to enter Laclede County. It meanders to the southeast and crosses into the northwest corner of Wright County before returning to a northeast direction back into Laclede County adjacent to the community of Pease. It meanders ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watercourse
A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighted subterranean water, and surfaced groundwater ( spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle, instruments in groundwate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrosphere)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust ( pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Incised Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank (cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salem Plateau
Salem may refer to: Places Canada Ontario * Bruce County ** Salem, Arran–Elderslie, Ontario, in the municipality of Arran–Elderslie ** Salem, South Bruce, Ontario, in the municipality of South Bruce * Salem, Dufferin County, Ontario, part of the Town of Mono * Salem, Durham Regional Municipality, Ontario, in the municipality of Clarington * Salem, Frontenac County, Ontario, in the municipality of South Frontenac * Salem, Northumberland County, in the municipality of Cramahe * Salem, Wellington County, in the municipality of Centre Wellington Germany * Salem, Baden-Württemberg, a municipality in the Bodensee district ** Salem Abbey (Reichskloster Salem), a monastery ** Schule Schloss Salem, Germany (also referred to as Salem College, with a section called Salem International College) * Salem, Schleswig-Holstein Holy Land (Israel, Palestine) * Salem (Bible), the home of Melchizedek as given in Genesis 14:18, possibly to be identified with Jerusalem * Salem, Ma'ale Iron ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually relate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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