|
Neuse River
The Neuse River ( , Tuscarora: Neyuherú·kęʔkì·nęʔ) is a river rising in the Piedmont of North Carolina and emptying into Pamlico Sound below New Bern. Its total length is approximately , making it the longest river entirely contained in North Carolina. The Trent River joins the Neuse at New Bern. Its drainage basin, measuring in area, also lies entirely inside North Carolina. It is formed by the confluence of the Flat and Eno rivers prior to entering the Falls Lake reservoir in northern Wake County. Its fall line shoals, known as the ''Falls of the Neuse'', lie submerged under the waters of Falls Lake. This River also creates the beauty of the Neuse River Trail, a long greenway that stretches from Falls Lake Dam, Raleigh, North Carolina to Legend Park, Clayton, North Carolina. Geography The Neuse begins at the confluence of the Flat and Eno rivers near Durham, North Carolina. The river enters Pamlico Sound just east of Maw Point Shoal near Hobucken, North C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pamlico Sound
Pamlico Sound ( ) is a lagoon in North Carolina which is the largest lagoon along the North American East Coast, extending long and 15 to 20 miles (24 to 32 km) wide. It is part of a large, interconnected network of lagoon estuaries that includes Albemarle Sound, Currituck Sound, Croatan Sound, Roanoke Sound, Pamlico Sound, Bogue Sound, Back Sound, and Core Sound. Together, these sounds, known as the Albemarle-Pamlico sound system, comprise the second largest estuary in the United States, covering over 3,000 sq. mi. (7,800 km2) of open water. (Chesapeake Bay is the largest.) The Pamlico Sound is separated from the Atlantic Ocean by the Outer Banks, a row of low, sandy barrier islands that include Cape Hatteras National Seashore, Cape Lookout National Seashore, and Pea Island National Wildlife Refuge. The Albemarle-Pamlico Sound is one of nineteen great waters recognized by the America's Great Waters Coalition. Hydrology Pamlico Sound is connected to the north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falls Lake
Falls Lake is a 12,410 acre (50 km²) reservoir located in Durham, Wake, and Granville counties in North Carolina, United States. Falls Lake extends up the Neuse River to its source at the confluence of the Eno, Little, and Flat rivers. The lake is named for the ''Falls of the Neuse'', a once whitewater section of the river that fell from the Piedmont into the lower Coastal Plain submerged during construction of the lake. The lake provides drinking water for several of the surrounding communities, including the city of Raleigh, aids with flood control and serves as a recreation area and wildlife habitat. Work on the dam that holds the lake began in 1978 and was completed in 1981. Prior to its construction flooding of the Neuse River caused extensive damage to public and private properties including roadways, railroads, industrial sites and farmlands. The U.S. Army Corps of Engineers constructed and manages the dam. Falls Dam () is an earthen structure having a top el ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neuse Township, Wake County, North Carolina
Neuse Township (also designated Township 13) is one of twenty townships within Wake County, North Carolina, United States. As of the 2010 census, Neuse Township had a population of 73,617, a 52.6% increase over 2000. Neuse Township, occupying in north-central Wake County, is almost completely occupied by portions of the city of Raleigh Raleigh (; ) is the capital city of the state of North Carolina and the seat of Wake County in the United States. It is the second-most populous city in North Carolina, after Charlotte. Raleigh is the tenth-most populous city in the Southe .... References Townships in Wake County, North Carolina Townships in North Carolina {{WakeCountyNC-geo-stub ... [...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 r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 lim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of The Neuse State Park
Cliffs of the Neuse State Park is a North Carolina state park in Seven Springs, Wayne County, North Carolina in the United States. It is located near Seven Springs, North Carolina and covers along the southern banks of the Neuse River. It has a swimming area, camp sites, hiking trails, fishing areas, and picnic areas. The park's museum features exhibits about the geology and natural history of the cliffs and the park. Extending for , the series of cliffs rise above the water. Layers of sand, clay, seashells, shale and gravel form the multicolored cliff face, a rainbow of white, tan, yellow and brown. History The cliffs were formed when a fault in the Earth's crust shifted millions of years ago. The Neuse River followed this fault line and, over time, cut its course through layers of sediment deposited by shallow seas that had earlier covered the coastal plain. A portion of the river took a bend against its bank and the water's erosive action slowly carved Cliffs of the Neuse. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swamp
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates periodic inu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bottomland
Upland and lowland are conditional descriptions of a plain based on elevation above sea level. In studies of the ecology of freshwater rivers, habitats are classified as upland or lowland. Definitions Upland and lowland are portions of plain that are conditionally categorized by their elevation above the sea level. Lowlands are usually no higher than , while uplands are somewhere around to . On unusual occasions, certain lowlands such as the Caspian Depression lie below sea level. Upland habitats are cold, clear and rocky whose rivers are fast-flowing in mountainous areas; lowland habitats are warm with slow-flowing rivers found in relatively flat lowland areas, with water that is frequently colored by sediment and organic matter. These classifications overlap with the geological definitions of "upland" and "lowland". In geology an "upland" is generally considered to be land that is at a higher elevation than the alluvial plain or stream terrace, which are considered t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Atlantic Ocean
The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the " Old World" of Africa, Europe and Asia from the " New World" of the Americas in the European perception of the World. The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Europe and Africa to the east, and North and South America to the west. As one component of the interconnected World Ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south (other definitions describe the Atlantic as extending southward to Antarctica). The Atlantic Ocean is divided in two parts, by the Equatorial Counter Current, with the North(ern) Atlantic Ocean and the South(ern) Atlantic Ocean split at about 8°N. Scientific explorations of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neuse River-27527
{{geodis ...
Neuse may refer to following, all in North Carolina: * Neuse, North Carolina * Neuse River * Neuse Township, Wake County, North Carolina * Neuse Correctional Institute * Neuse Forest, North Carolina * Cliffs of the Neuse State Park or to the Confederate States Navy ship: * CSS Neuse CSS ''Neuse'' ( ) was a steam-powered ironclad ram of the Confederate States Navy that served in the latter part the American Civil War and was eventually scuttled to avoid capture by rapidly advancing Union Army forces. In the early 1960s, she pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clayton, North Carolina
Clayton is a town in Johnston County, North Carolina, United States, and is considered a satellite town of Raleigh. As of 2010, Clayton's population was 16,116, up from 6,973 at the 2000 census. By 2019 the town's estimated population was 24,887. Much of that growth can be attributed to the town's proximity to the Research Triangle area and access to major highways such as I-40 and US 70. History The Clayton Banking Company Building, Clayton Graded School and Clayton Grammar School-Municipal Auditorium, Clayton Historic District, Cleveland School, Ellington-Ellis Farm, Walter R. and Eliza Smith Moore House, Sanders-Hairr House, and Stallings-Carpenter House are listed on the National Register of Historic Places. Geography Clayton is in northern Johnston County, with a small portion extending northwest along US 70 Business into Wake County. In 2006, construction began on the Highway 70 Clayton Bypass, a stretch from Interstate 40 along the southern portion of Clayton t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neuse River Trail
The Neuse River Trail is a long paved greenway located in the Raleigh area of North Carolina, running along the banks of the Neuse River from Falls Lake Dam to the town of Clayton. The route passes through the jurisdictions of Raleigh, Wake Forest, Knightdale, and Clayton in Wake and Johnston counties. The Neuse River Greenway trail is part of the Capital Area Greenway system as well as the Mountains-to-Sea Trail that crosses North Carolina from the Great Smoky Mountains to the Outer Banks. Open to both cyclists and pedestrians, the Neuse River Trail is the longest greenway trail in North Carolina and the longest paved trail between northern Virginia and western Georgia. The Neuse River Trail is a part of the East Coast Greenway, a 3,000 mile long system of trails connecting Maine to Florida. Route The Neuse River Trail is split into seven sections, from North to South: * Falls Lake Dam to Horseshoe Farm Park * Horseshoe Farm Park to Buffaloe Road Athletic Park * Buffal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
