Falling Water River
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Falling Water River
The Falling Water River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed June 8, 2011 stream in the east-central portion of Middle Tennessee in the United States. It rises just west of Monterey at the edge of the Cumberland Plateau, and traverses the Eastern Highland Rim before dropping off to the Nashville Basin and emptying into Center Hill Lake along the Caney Fork. The river is noted for the Burgess Falls, which it spills over near the end of its course. Course The river rises in Welch Hollow, a dissected portion of the Cumberland Plateau that lies just west of Monterey in eastern Putnam County, and descends more than before exiting the hollow at the southern edge of Buck Mountain. It passes under Interstate 40 near mile marker 291 before entering City Lake, a reservoir that provides water and water treatment for nearby Cookeville. Just beyond the City Lake Dam, the river passes under U.S. Highway 70N as i ...
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Cookeville, TN
Cookeville is the county seat and largest city of Putnam County, Tennessee, Putnam County, Tennessee, United States. As of the 2020 United States census, its population was reported to be 34,842. It is recognized as one of the country's Cookeville micropolitan area, micropolitan areas, or smaller cities which function as significant regional economic hubs. Of the twenty micropolitan areas in Tennessee, Cookeville is the largest. The Cookeville micropolitan area's 2010 Census population was 106,042. The U.S. Census Bureau ranked the Cookeville micropolitan area as the 7th largest-gaining micropolitan area in the country between 2018 and 2019, with a one-year gain of 1,796 and a 2019 population of 114,272. The city is a college town, home to Tennessee Tech. History Early years and establishment Previous to its settlement era, the area of Cookeville was dominated by the Cherokee Native American tribe through the Paleo-Indians, Paleo-Indian to the early European colonization peri ...
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Center Hill Dam
Center Hill Lake is a reservoir in the U.S. state of Tennessee. It is located in Middle Tennessee near Smithville. Created by means of a dam constructed by the U.S. Army Corps of Engineers in 1948, the lake has a dual purpose: electricity production and flood control. Center Hill Dam is high, and it is composed of concrete and earth structures, with 8 gates that are wide each. Center Hill Lake is one of four major flood control reservoirs for the Cumberland; the others being Percy Priest Lake, Dale Hollow Reservoir, and Lake Cumberland. Geography The lake, which is long, covers an area of . Center Hill Lake has a storage capacity of of water. The lake has approximately of shoreline, with the deepest point at . The watershed area for the lake is . The lake is well known for water recreation and fishing. Major tributaries of Center Hill Lake include the Caney Fork (the main tributary) and the Falling Water River. Edgar Evins, Burgess Falls and Rock Island State Parks con ...
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Burgess Falls State Park
Burgess Falls State Park is a state park and state natural area in Putnam County and White County, Tennessee, located in the southeastern United States. The park is situated around a steep gorge in which the Falling Water River drops in elevation in less than a mile, culminating in a cataract waterfall. The Burgess Falls State Natural Area, which covers , is managed by the Tennessee Department of Environment and Conservation. Geography The Falling Water River rises near the base of the Cumberland Plateau in eastern Putnam County and winds its way across the Highland Rim to its mouth along the Center Hill Lake impoundment of the Caney Fork, which is located in an area where the Highland Rim drops off into the Central Basin. The Burgess Falls State Natural Area comprises the section of the river just above its mouth, where the river drops from roughly atop the Highland Rim to just over at Center Hill Lake. Over a long period of time, the Falling Water River's rapids hav ...
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Tennessee Valley Authority
The Tennessee Valley Authority (TVA) is a federally owned electric utility corporation in the United States. TVA's service area covers all of Tennessee, portions of Alabama, Mississippi, and Kentucky, and small areas of Georgia, North Carolina, and Virginia. While owned by the federal government, TVA receives no taxpayer funding and operates similarly to a private for-profit company. It is headquartered in Knoxville, Tennessee, and is the sixth largest power supplier and largest public utility in the country. The TVA was created by Congress in 1933 as part of President Franklin D. Roosevelt's New Deal. Its initial purpose was to provide navigation, flood control, electricity generation, fertilizer manufacturing, regional planning, and economic development to the Tennessee Valley, a region that had suffered from lack of infrastructure and poverty during the Great Depression, relative to the rest of the nation. TVA was envisioned both as a power supplier and a regional economi ...
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Burgess Falls Dam
__NOTOC__ Burgess may refer to: People and fictional characters * Burgess (surname), a list of people and fictional characters * Burgess (given name), a list of people Places * Burgess, Michigan, an unincorporated community *Burgess, Missouri, United States * Burgess, South Carolina, United States *Burgess, Virginia, United States *Burgess Township, Bond County, Illinois, United States *Burgess Park, London, England *Burgess Field Oxford, England *Burgess Hill, Sussex, England *Mount Burgess, Canadian Rockies *Burgess Branch, a tributary of Missisquoi River, Vermont, United States Other uses *Burgess (title), a political official or representative *Burgess Company, an American airplane manufacturer *Burgess GAA, an athletic club in Ireland See also *Burgess House (other), several buildings named *Burgess model, or Concentric zone model, a theoretical model in urban geography *Burgess reagent, used in organic chemistry *Burgess Shale, a fossil-bearing formation near Mount ...
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Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ...
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Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Mississippian (geology)
The Mississippian ( , also known as Lower Carboniferous or Early Carboniferous) is a subperiod in the geologic timescale or a subsystem of the geologic record. It is the earlier of two subperiods of the Carboniferous period lasting from roughly 358.9 to 323.2 million years ago. As with most other geochronologic units, the rock beds that define the Mississippian are well identified, but the exact start and end dates are uncertain by a few million years. The Mississippian is so named because rocks with this age are exposed in the Mississippi Valley. The Mississippian was a period of marine transgression in the Northern Hemisphere: the sea level was so high that only the Fennoscandian Shield and the Laurentian Shield were dry land. The cratons were surrounded by extensive delta systems and lagoons, and carbonate sedimentation on the surrounding continental platforms, covered by shallow seas. In North America, where the interval consists primarily of marine limestones, it is treate ...
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Mississippi River
The Mississippi River is the second-longest river and chief river of the second-largest drainage system in North America, second only to the Hudson Bay drainage system. From its traditional source of Lake Itasca in northern Minnesota, it flows generally south for to the Mississippi River Delta in the Gulf of Mexico. With its many tributaries, the Mississippi's watershed drains all or parts of 32 U.S. states and two Canadian provinces between the Rocky and Appalachian mountains. The main stem is entirely within the United States; the total drainage basin is , of which only about one percent is in Canada. The Mississippi ranks as the thirteenth-largest river by discharge in the world. The river either borders or passes through the states of Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, and Louisiana. Native Americans have lived along the Mississippi River and its tributaries for thousands of years. Most were hunter-ga ...
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Ohio River
The Ohio River is a long river in the United States. It is located at the boundary of the Midwestern and Southern United States, flowing southwesterly from western Pennsylvania to its mouth on the Mississippi River at the southern tip of Illinois. It is the third largest river by discharge volume in the United States and the largest tributary by volume of the north-south flowing Mississippi River that divides the eastern from western United States. It is also the 6th oldest river on the North American continent. The river flows through or along the border of six states, and its drainage basin includes parts of 14 states. Through its largest tributary, the Tennessee River, the basin includes several states of the southeastern U.S. It is the source of drinking water for five million people. The lower Ohio River just below Louisville is obstructed by rapids known as the Falls of the Ohio where the elevation falls in restricting larger commercial navigation, although in the 18th ...
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