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Spring Creek (Roaring River Tributary)
Spring Creek is a large stream in the U.S. state of Tennessee. It flows through Putnam, Overton and Jackson counties and is a major tributary of the Roaring River. It is part of the State Scenic River system of Tennessee, along with the Roaring River and Blackburn Fork River. The river can be roughly divided into three sections: a smaller but still big headwaters on the Highland Rim, a huge and moderately turbulent lower part and an even more violent whitewater stream as the middle part descends to the level of the Nashville Basin. The lower part dries up due to limestone-dominated karst topography Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant ro .... References Rivers of Tennessee {{Tennessee-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), 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 river, 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), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), 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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tennessee
Tennessee ( , ), officially the State of Tennessee, is a landlocked state in the Southeastern region of the United States. Tennessee is the 36th-largest by area and the 15th-most populous of the 50 states. It is bordered by Kentucky to the north, Virginia to the northeast, North Carolina to the east, Georgia, Alabama, and Mississippi to the south, Arkansas to the southwest, and Missouri to the northwest. Tennessee is geographically, culturally, and legally divided into three Grand Divisions of East, Middle, and West Tennessee. Nashville is the state's capital and largest city, and anchors its largest metropolitan area. Other major cities include Memphis, Knoxville, Chattanooga, and Clarksville. Tennessee's population as of the 2020 United States census is approximately 6.9 million. Tennessee is rooted in the Watauga Association, a 1772 frontier pact generally regarded as the first constitutional government west of the Appalachian Mountains. Its name derives from "Tanas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Putnam County, Tennessee
Putnam County is a county located in the U.S. state of Tennessee. As of the 2020 census, the population was 79,854. Its county seat is Cookeville. Putnam County is part of the Cookeville, TN Micropolitan Statistical Area. History Putnam County is named in honor of Israel Putnam, who was a hero in the French and Indian War and a general in the American Revolutionary War. The county was initially established on February 2, 1842, when the Twenty-fourth Tennessee General Assembly enacted a measure creating the county from portions of Jackson, Overton, Fentress, and White counties. After the survey was completed by Mounce Gore, the Assembly instructed the commissioners to locate the county seat, to be called "Monticello," near the center of the county. Contending, however, that the formation of Putnam was illegal because it reduced their areas below constitutional limits, Overton and Jackson counties secured an injunction against its continued operation. Putnam officials faile ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Overton County, Tennessee
Overton County is a county located in the U.S. state of Tennessee. As of the 2020 census, the population was 22,511. Its county seat is Livingston. Overton County is part of the Cookeville, TN Micropolitan Statistical Area. History On May 10, 1933, a half-mile wide F4 tornado struck the small community of Beatty Swamps (also referred to as Bethsadia). The tornado destroyed every structure in the town and either killed or injured nearly every inhabitant, with 33 of the 35 deaths occurring in the area. Much of the area was swept clean of debris, a reaper-binder was thrown , and cars were moved hundreds of feet. Archived June 6, 2011.Grazulis, ''Significant'', pp. 850-851 < ...
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Jackson County, Tennessee
Jackson County is a county located in the U.S. state of Tennessee. The population was 11,638 at the 2010 census. Its county seat is Gainesboro. Jackson is part of the Cookeville Micropolitan Statistical Area. History Jackson County was created by an act of the Tennessee General Assembly on November 6, 1801. It was the 18th county established in the state. It was formed from part of Smith County plus Indian lands. The name honors Andrew Jackson, who by 1801 had already served as a U.S. Congressman and Senator from Tennessee, a Tennessee Supreme Court justice, and a colonel in the Tennessee militia. He became more widely known as commander at the Battle of New Orleans and as the seventh President of the United States. In the 1790s, an Army outpost named Fort Blount was built west of Gainesboro on the Cumberland River, in what is now western Jackson County. Fort Blount was an important stop for travelers on Avery's Trace. Williamsburg, a town developed around the fort, serv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roaring River (Tennessee)
The Roaring River is a tributary of the Cumberland River in the U.S. state of Tennessee.U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed June 8, 2011 Via the Cumberland and Ohio rivers, it is part of the Mississippi River watershed. It rises on the Highland Rim approximately south of Livingston, Tennessee in Overton County. It initially flows roughly north, then turns largely west for the balance of its course. After crossing into Jackson County, it begins a relatively steep descent, resulting in the namesake "roar" during periods of high flow. The lower portion of its course is designated as a "State Scenic River" under the terms of the Tennessee Wild and Scenic Rivers Act. The Roaring River empties into the Cordell Hull Lake impoundment of the Cumberland River. A U.S. Army Corps of Engineers recreation area is at and around the actual confluence, which is very near the Jackson County seat of Gainesboro. See also * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blackburn Fork River
Blackburn Fork River is a river located in Jackson County, Tennessee. It originates near Cookeville, Tennessee, and is a major tributary of the Roaring River. It contains the seventy-five foot high waterfall, Cummins Falls, and runs within Cummins Falls State Park. Hiking, swimming, and fishing are popular activities on the river. The river's source is at the confluence of West Blackburn Fork Creek and East Blackburn Fork Creek, both of which are large creeks beginning in the north-central portion of Putnam County and end in Jackson County. East Blackburn Fork Creek drains northern portions of Cookeville and is crossed by Dodson Branch Road, while West Blackburn Fork Creek drains suburbs between Cookeville and Baxter and is crossed by Gainesboro Grade. Blackburn Fork is designated as a Tennessee State Scenic River, a title also belonging to Spring Creek, the Roaring River's other major tributary. Shortly after the confluence of West and East Blackburn Fork Creek, the river ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highland Rim
The Highland Rim is a geographic term for the area in Tennessee surrounding the Central Basin. Nashville is largely surrounded by higher terrain in all directions. Geologically, the Central Basin is a dome. The Highland Rim is a cuesta surrounding the basin, and the border where the difference in elevation is sharply pronounced is an escarpment. Nashville is located in the northwestern corner of the basin. Geology and Physiography The Highland Rim is a physiographic section of the larger Interior Low Plateaus province, which in turn is part of the larger Interior Plains physiographic division. Most of the Highland Rim is located in U.S. EPA Ecoregion 71, Interior Plateau, which is a part of the Eastern Temperate Forest. The sections of the Highland Rim are referred to the four cardinal directions, e.g., "Northern Highland Rim", etc. The Highland Rim is rather continuous and any division of it, including the ones made below, are somewhat arbitrary. The term "highland" here is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nashville Basin
The Nashville Basin, also known as the Central Basin, is a term often used to describe the area surrounding Murfreesboro, Tennessee, in which Nashville is located. The Central Basin was caused by an uplifting which produced a dome known as the Nashville Dome. The Nashville Dome is evidenced by the underlying rock strata that all dip downwards away from Nashville. The uplifting of the Nashville Dome fractured overlying strata, making it more easily eroded and thus the "dome" resulted in a "basin". Uplifted strata in the center of a geological dome have higher potential erosive energy than the surrounding strata, because they are physically higher. Erosion thus acts on the uplifted area at a greater rate than on the surrounding flat-lying area, creating a low area, i.e. a basin. This area is more correctly referred to as the "Central Dome" of Tennessee. Nashville is located in the northwestern portion of the Central Basin. The basin extends for approximately forty-five to sixty m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Losing Stream
A losing stream, disappearing stream, influent stream or sinking river is a stream or river that loses water as it flows downstream. The water infiltrates into the ground recharging the local groundwater, because the water table is below the bottom of the stream channel. This is the opposite of a more common ''gaining stream'' (or ''effluent stream'') which increases in water volume farther downstream as it gains water from the local aquifer. Losing streams are common in arid areas due to the climate which results in huge amounts of water evaporating from the river generally towards the mouth. Losing streams are also common in regions of karst topography where the streamwater may be completely captured by a cavern system, becoming a subterranean river. Examples There are many natural examples of subterranean rivers including: Bosnia and Herzegovina * Unac; Mušnica-Trebišnjica- Krupa/Ombla (Trebišnjica is considered to be one of the largest sinking rivers in the world; ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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