2018 FEI World Equestrian Games
The 2018 FEI World Equestrian Games are being held in Mill Spring, North Carolina, U. S. at the Tryon International Equestrian Center, from September 11 to September 23, 2018. This is the eighth edition of the games, which are held every four years and run by the International Federation for Equestrian Sports; this is the second time that North America is hosting the Games, the previous time being in 2010, when the United States were the hosts. United States will become the first nation to host the Games twice; the initial bidding process for the 2018 edition of the World Equestrian Games started in 2011 with the initial application stage. Eight countries expressed their interest, five of them became official candidates in 2012: Rabat, Budapest and Wellington. Australia and Sweden withdrew before the official candidature phase. By 2013, four of the official candidates dropped out. However, instead of awarding the Games to Canada, FEI decided to re-open the bidding process on July 1, 2013, as the Bromont bid was lacking financial support.
Bromont was joined by two USA candidates as well as Great Britain. Great Britain and Wellington dropped out, leaving only Lexington in contention. Bromont was awarded the hosting rights on June 9, 2014. Bromont withdrew from hosting in 2016. Following Bromont's withdrawal, North Carolina and Šamorín, Slovakia expressed their interest in hosting the event. Tryon was awarded the Games on November 3, 2016. Tryon International Equestrian Center, Mill Spring, North Carolina U. S. Trust Arena – Jumping and Eventing Tryon Stadium – Ceremonies and Para-dressage Covered Arena – Reining and Vaulting Driving Stadium – Driving White Oak Course - Eventing and Driving TIEC and surrounding farmland - Endurance Horses competing in the championships were flown in and out of Greenville-Spartanburg International Airport in Greer, South Carolina, they were transported by horse trailers up to Tryon. All times are Eastern Daylight Time. - individual, - squad Host nation Hurricane Florence is expected to hit the Tryon Internation Equestrian Center and the surrounding area during the first week of the World Equestrian Games.
Possible impacts could include increased gusts of wind. A special contingency plan has been addressed for the situation. Depending on the severity of the storm, the contingency plan will include accommodating all horses on-venue in permanent barns, moving grooms accommodated on-site to permanent buildings at the venue, advising shelter locations for all personnel, continuing discussions with airports and Emirates airline on any necessary steps regarding horse arrivals/departures, ensuring smaller tents in the vendor area are tie-strapped together for security, carrying out additional drainage/water channeling to prevent flooding, purchasing additional fuel tanks and filling all fuel tanks to run the generators, preparing to remove fence scrim installed and taking down flags. Alongside the World Equestrian Games, Tryon International Equestrian Center will host the inaugural WEQx Games. WEQx Games are scheduled to feature nine spectator-friendly equine competitions that should "highlight the accessibility, diversity and passion for horses and horse sport for athletes of all ages".
WEQx Events: U-25 U. S. Open Championship U. S. Open Speed Horse DerbyX Battle of the Sexes Match Race Puissance Six Bar Pony Jumpers Gladiator Polo FEI website World Equestrian Games: Singer/Songwriter Katrina "Kat" Williams to headline Day of the African Equestrian gala during FEI World Equestrian Games
Blue Ridge Mountains
The Blue Ridge Mountains are a physiographic province of the larger Appalachian Mountains range. The mountain range is located in the eastern United States, extends 550 miles southwest from southern Pennsylvania through Maryland, West Virginia, North Carolina, South Carolina and Georgia; this province consists of northern and southern physiographic regions, which divide near the Roanoke River gap. To the west of the Blue Ridge, between it and the bulk of the Appalachians, lies the Great Appalachian Valley, bordered on the west by the Ridge and Valley province of the Appalachian range; the Blue Ridge Mountains are noted for having a bluish color. Trees put the "blue" in Blue Ridge, from the isoprene released into the atmosphere, thereby contributing to the characteristic haze on the mountains and their distinctive color. Within the Blue Ridge province are two major national parks – the Shenandoah National Park in the northern section, the Great Smoky Mountains National Park in the southern section – and eight national forests including George Washington and Jefferson National Forests, Cherokee National Forest, Pisgah National Forest, Nantahala National Forest and Chattahoochee National Forest.
The Blue Ridge contains the Blue Ridge Parkway, a 469-mile long scenic highway that connects the two parks and is located along the ridge crest-lines with the Appalachian Trail. Although the term "Blue Ridge" is sometimes applied to the eastern edge or front range of the Appalachian Mountains, the geological definition of the Blue Ridge province extends westward to the Ridge and Valley area, encompassing the Great Smoky Mountains, the Great Balsams, the Roans, the Blacks, the Brushy Mountains and other mountain ranges; the Blue Ridge extends as far north into Pennsylvania as South Mountain. While South Mountain dwindles to mere hills between Gettysburg and Harrisburg, the band of ancient rocks that form the core of the Blue Ridge continues northeast through the New Jersey and Hudson River highlands reaching The Berkshires of Massachusetts and the Green Mountains of Vermont; the Blue Ridge contains the highest mountains in eastern North America south of Baffin Island. About 125 peaks exceed 5,000 feet in elevation.
The highest peak in the Blue Ridge is Mt. Mitchell in North Carolina at 6,684 feet. There are 39 peaks in North Tennessee higher than 6,000 feet. Southern Sixers is a term used by peak baggers for this group of mountains; the Blue Ridge Parkway runs 469 miles along crests of the Southern Appalachians and links two national parks: Shenandoah and Great Smoky Mountains. In many places along the parkway, there are metamorphic rocks with folded bands of light-and dark-colored minerals, which sometimes look like the folds and swirls in a marble cake. Most of the rocks that form the Blue Ridge Mountains are ancient granitic charnockites, metamorphosed volcanic formations, sedimentary limestone. Recent studies completed by Richard Tollo, a professor and geologist at George Washington University, provide greater insight into the petrologic and geochronologic history of the Blue Ridge basement suites. Modern studies have found that the basement geology of the Blue Ridge is made of compositionally unique gneisses and granitoids, including orthopyroxene-bearing charockites.
Analysis of zircon minerals in the granite completed by John Aleinikoff at the U. S. Geological Survey has provided more detailed emplacement ages. Many of the features found in the Blue Ridge and documented by Tollo and others have confirmed that the rocks exhibit many similar features in other North American Grenville-age terranes; the lack of a calc-alkaline affinity and zircon ages less than 1,200 Ma suggest that the Blue Ridge is distinct from the Adirondacks, Green Mountains, the New York-New Jersey Highlands. The petrologic and geochronologic data suggest that the Blue Ridge basement is a composite orogenic crust, emplaced during several episodes from a crustal magma source. Field relationships further illustrate that rocks emplaced prior to 1,078–1,064 Ma preserve deformational features; those emplaced post-1,064 Ma have a massive texture and missed the main episode of Mesoproterozoic compression. The Blue Ridge Mountains began forming during the Silurian Period over 400 million years ago.
320 Mya, North America, Europe collided, pushing up the Blue Ridge. At the time of their emergence, the Blue Ridge were among the highest mountains in the world and reached heights comparable to the much younger Alps. Today, due to weathering and erosion over hundreds of millions of years, the highest peak in the range, Mount Mitchell in North Carolina, is only 6,684 feet high – still the highest peak east of the Rockies; the English who settled colonial Virginia in the early 17th century recorded that the native Powhatan name for the Blue Ridge was Quirank. At the foot of the Blue Ridge, various tribes including the Siouan Manahoacs, the Iroquois, the Shawnee hunted and fished. A German physician-explorer, John Lederer, first reached the crest of the Blue Ridge in 1669 and again the following year. At the Treaty of Albany negotiated by Lieutenant Governor Alexander Spotswood, of Virginia with the Iroquois between 1718 and 1722, the Iroquois ceded lands they had conquered south of the Potomac River and east of the Blue Ridge to the Virginia Colony.
This treaty made the Blue Ridge the new demarcation point between the areas and tribes subject to the Six Nati
Henderson County, North Carolina
Henderson County is a county located in the U. S. state of North Carolina. As of the 2010 census, the population was 106,740, its county seat is Hendersonville. Henderson County is part of NC Metropolitan Statistical Area; the county was formed in 1838 from the southern part of Buncombe County. It was named for Leonard Henderson, Chief Justice of the North Carolina Supreme Court from 1829 to 1833. There is no evidence Henderson passed through the area. In 1855 parts of Henderson County and Rutherford County were combined to form Polk County, in 1861 parts of Henderson County and Jackson County were combined to form Transylvania County. Henderson County, which in 1861 encompassed present-day Transylvania County as well, contributed 1,296 soldiers to the Confederate States Army out of its 10,000 population, as well as 130 Union troops.. Henderson County government was centered around Hendersonville in the 1905 county courthouse on Main Street, until this structure was replaced by the new Courthouse on Grove Street in Hendersonville.
The first rail line reached Hendersonville in 1879, ushering in a new era of access to the outside world. However, parts of the county had long been known as retreats, including the "Little Charleston" of Flat Rock in which South Carolina's Low Country planter families had maintained second homes since the early 19th century. A major land boom ensued in the 1920s, culminating in the crash of 1929, which deflated prices and left structures such as the Fleetwood Hotel atop Jumpoff Mountain incomplete. Population growth in the county has been rapid since the 1960s as a result of an influx from other states, with many new housing developments changing the face of rural areas of the county. Other notable historic sites in Henderson County include: the Woodfield Inn, Connemara—final home of Carl Sandburg -- and the St. John in the Wilderness Episcopal Church. Today, Flat Rock is the site of the main campus of Blue Ridge Community College. Henderson County is located in the Blue Ridge Mountains of southwestern North Carolina, on the border with South Carolina.
The Eastern Continental Divide, which lies along the crest of the Blue Ridge, passes through the county. The northwestern slope of the Divide is known as the Blue Ridge Plateau and the southeastern slope as the Blue Ridge Escarpment; these two physiographic features have unique characteristics that account for wide variations in the county’s climate. According to the U. S. Census Bureau, the county has a total area of 375 square miles, of which 373 square miles is land and 2.2 square miles is water. The county's largest body of water is Lake Summit, a reservoir impounded by the Duke Power Company for hydroelectric generation; the county's major streams are the French Broad River, Mills River, Green River, Little River, Mud Creek, Clear Creek, Cane Creek, Hungry River, the headwaters of the Broad River. The lowest point in the county is to be found along the Broad River at 1,394’ feet at the boundary between Henderson and Rutherford Counties in North Carolina; the high point is located on Little Pisgah Mountain at 5,278 feet along the Henderson-Haywood County boundary in North Carolina.
According to the U. S. Census Bureau, the county has a total area of 375 square miles, of which 373 square miles is land and 2.2 square miles is water. The county's largest body of water is Lake Summit, a reservoir impounded by the Duke Power Company for hydroelectric generation. Due to its geographic setting along the Eastern Continental Divide and its extreme topographic variation, Henderson County presents a wide variation in temperature and precipitation conditions; the highest elevations occur along the northwest and northern boundaries of the county and within the Blue Ridge Escarpment, a rugged area of peaks and narrow valleys that rise from the Piedmont to the continental divide and the Blue Ridge Plateau. The lowest elevations occur within the valleys of the escarpment and in the broader valleys of the Blue Ridge Plateau; the mean annual temperature of the county is 55.1°F, with a range from 50.3 to 57.9°F depending on the elevation, with higher temperatures occurring at lower elevations and lower temperatures in the higher mountains.
The month of July is the hottest in the county, with a mean temperature of 72.6°F and a mean range of 66.6 to 75.8°F. The coolest month is January with a mean temperature of 36.9°F and a mean range of 33.3 to 39.5°F. Precipitation is correlated to elevation, with higher precipitation occurring at higher elevations and lower precipitation in the valleys; the mean annual precipitation of Henderson County is 56.2 inches, with a mean range of 45.04 to 78.03 inches. March has the highest mean precipitation of 5.1 inches, with a mean range of 3.9 to 6.7 inches. The lowest precipitation occurs in October, with a mean value of 3.9 inches and a mean range of 2.8 to 5.8 inches. Henderson County's topographic and climatic diversity make it ideal for a great variety of commercial crops and agricultural products. Parts of the county between the Pisgah National Forest on the northwest and the boundary with Polk County on the southeast are referred to l
A reservoir is, most an enlarged natural or artificial lake, pond or impoundment created using a dam or lock to store water. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. Defined as a storage space for fluids, reservoirs may hold gasses, including hydrocarbons. Tank reservoirs elevated, or buried tanks. Tank reservoirs for water are called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum, below ground. Reservoir is most an enlarged natural or artificial lake. A dam constructed in a valley relies on the natural topography to provide most of the basin of the reservoir. Dams are located at a narrow part of a valley downstream of a natural basin; the valley sides act as natural walls, with the dam located at the narrowest practical point to provide strength and the lowest cost of construction.
In many reservoir construction projects, people have to be moved and re-housed, historical artifacts moved or rare environments relocated. Examples include the temples of Abu Simbel, the relocation of the village of Capel Celyn during the construction of Llyn Celyn, the relocation of Borgo San Pietro of Petrella Salto during the construction of Lake Salto. Construction of a reservoir in a valley will need the river to be diverted during part of the build through a temporary tunnel or by-pass channel. In hilly regions, reservoirs are constructed by enlarging existing lakes. Sometimes in such reservoirs, the new top water level exceeds the watershed height on one or more of the feeder streams such as at Llyn Clywedog in Mid Wales. In such cases additional side dams are required to contain the reservoir. Where the topography is poorly suited to a single large reservoir, a number of smaller reservoirs may be constructed in a chain, as in the River Taff valley where the Llwyn-on, Cantref and Beacons Reservoirs form a chain up the valley.
Coastal reservoirs are fresh water storage reservoirs located on the sea coast near the river mouth to store the flood water of a river. As the land based reservoir construction is fraught with substantial land submergence, coastal reservoir is preferred economically and technically since it does not use scarce land area. Many coastal reservoirs were constructed in Europe. Saemanguem in South Korea, Marina Barrage in Singapore and Plover Cove in China, etc are few existing coastal reservoirs. Where water is pumped or siphoned from a river of variable quality or size, bank-side reservoirs may be built to store the water; such reservoirs are formed by excavation and by building a complete encircling bund or embankment, which may exceed 6 km in circumference. Both the floor of the reservoir and the bund must have an impermeable lining or core: these were made of puddled clay, but this has been superseded by the modern use of rolled clay; the water stored in such reservoirs may stay there for several months, during which time normal biological processes may reduce many contaminants and eliminate any turbidity.
The use of bank-side reservoirs allows water abstraction to be stopped for some time, when the river is unacceptably polluted or when flow conditions are low due to drought. The London water supply system is one example of the use of bank-side storage: the water is taken from the River Thames and River Lee. Service reservoirs store treated potable water close to the point of distribution. Many service reservoirs are constructed as water towers as elevated structures on concrete pillars where the landscape is flat. Other service reservoirs can be entirely underground in more hilly or mountainous country. In the United Kingdom, Thames Water has many underground reservoirs, sometimes called cisterns, built in the 1800s, most of which are lined with brick. A good example is the Honor Oak Reservoir in London, constructed between 1901 and 1909; when it was completed it was said to be the largest brick built underground reservoir in the world and it is still one of the largest in Europe. This reservoir now forms part of the southern extension of the Thames Water Ring Main.
The top of the reservoir is now used by the Aquarius Golf Club. Service reservoirs perform several functions, including ensuring sufficient head of water in the water distribution system and providing water capacity to out peak demand from consumers, enabling the treatment plant to run at optimum efficiency. Large service reservoirs can be managed to reduce the cost of pumping, by refilling the reservoir at times of day when energy costs are low. Circa 3 000 BC, the craters of extinct volcanoes in Arabia were used as reservoirs by farmers for their irrigation water. Dry climate and water scarcity in India led to early development of stepwells and water resource management techniques, including the building of a reservoir at Girnar in 3000 BC. Artificial lakes dating to the 5th century BC have been found in ancient Greece; the artificial Bhojsagar lake in present-day Madhya Pradesh state of India, constructed in the 11th century, covered 650 square kilometres. In Sri Lanka large reservoirs were created by ancient Sinhalese kings in order to save the water for irrigation.
The famous Sri Lankan king Pa
Piedmont (United States)
The Piedmont is a plateau region located in the Eastern United States. It sits between the Atlantic coastal plain and the main Appalachian Mountains, stretching from New Jersey in the north to central Alabama in the south; the Piedmont Province is a physiographic province of the larger Appalachian division which consists of the Gettysburg-Newark Lowlands, the Piedmont Upland and the Piedmont Lowlands sections. The Atlantic Seaboard fall line marks the Piedmont's eastern boundary with the Coastal Plain. To the west, it is bounded by the Blue Ridge Mountains, the easternmost range of the main Appalachians; the width of the Piedmont varies, being quite narrow above the Delaware River but nearly 300 miles wide in North Carolina. The Piedmont's area is 80,000 square miles; the name "Piedmont" comes from the French term for the same physical region meaning "foothill" from Latin "pedemontium", meaning "at the foot of the mountains", similar to the name of the Italian region of Piedmont, abutting the Alps.
The surface relief of the Piedmont is characterized by low, rolling hills with heights above sea level between 200 feet and 800 feet to 1,000 feet. Its geology is complex, with numerous rock formations of different materials and ages intermingled with one another; the Piedmont is the remnant of several ancient mountain chains that have since been eroded away. Geologists have identified at least five separate events which have led to sediment deposition, including the Grenville orogeny and the Appalachian orogeny during the formation of Pangaea; the last major event in the history of the Piedmont was the break-up of Pangaea, when North America and Africa began to separate. Large basins formed from the rifting and were subsequently filled by the sediments shed from the surrounding higher ground; the series of Mesozoic basins is entirely located inside the Piedmont region. Piedmont soils are clay-like and moderately fertile. In some areas they have suffered from erosion and over-cropping in the South where cotton was the chief crop.
In the central Piedmont region of North Carolina and Virginia, tobacco is the main crop, while in the north region there is more diversity, including orchards and general farming. The portion of the Piedmont region in the southern United States, is associated with the Piedmont blues, a style of blues music that originated there in the late 19th century. According to the Piedmont Blues Preservation Society, most Piedmont blues musicians came from Virginia, the Carolinas, Georgia. During the Great Migration, African Americans migrated to the Piedmont. With the Appalachian Mountains to the west, those who might otherwise have spread into rural areas stayed in cities and were thus exposed to a broader mixture of music than those in, for example, the rural Mississippi delta. Thus, Piedmont blues was influenced by many types of music such as ragtime and popular songs—styles that had comparatively less influence on blues music in other regions. Many major cities are located on the Atlantic Seaboard fall line, the eastern boundary of the Piedmont.
The fall line, where the land rises abruptly from the coastal plain, marks the limit of navigability on many major rivers, so inland ports sprang up along it. Within the Piedmont region itself, there are several areas of urban concentration, the largest being the Philadelphia metropolitan area in Pennsylvania; the Piedmont cuts Maryland in half. In Virginia, the Greater Richmond metropolitan area is the largest urban concentration. In North Carolina, the Piedmont Crescent includes several metropolitan clusters such as Charlotte metropolitan area, the Piedmont Triad, the Research Triangle. Other notable areas include the Greenville-Spartanburg-Anderson, SC Combined Statistical Area in South Carolina, in Georgia, the Atlanta metropolitan area. Cecil Piedmont Atlantic Piedmont region of Virginia Interstate 85 Godfrey, Michael A.. Field Guide to the Piedmont. Chapel Hill: University of North Carolina Press. ISBN 0-8078-4671-6. Hilton Pond Center for Piedmont Natural History "Piedmont Plain". New International Encyclopedia.
United States Census Bureau
The United States Census Bureau is a principal agency of the U. S. Federal Statistical System, responsible for producing data about the American people and economy; the Census Bureau is part of the U. S. Department of Commerce and its director is appointed by the President of the United States; the Census Bureau's primary mission is conducting the U. S. Census every ten years, which allocates the seats of the U. S. House of Representatives to the states based on their population; the Bureau's various censuses and surveys help allocate over $400 billion in federal funds every year and it helps states, local communities, businesses make informed decisions. The information provided by the census informs decisions on where to build and maintain schools, transportation infrastructure, police and fire departments. In addition to the decennial census, the Census Bureau continually conducts dozens of other censuses and surveys, including the American Community Survey, the U. S. Economic Census, the Current Population Survey.
Furthermore and foreign trade indicators released by the federal government contain data produced by the Census Bureau. Article One of the United States Constitution directs the population be enumerated at least once every ten years and the resulting counts used to set the number of members from each state in the House of Representatives and, by extension, in the Electoral College; the Census Bureau now conducts a full population count every 10 years in years ending with a zero and uses the term "decennial" to describe the operation. Between censuses, the Census Bureau makes population projections. In addition, Census data directly affects how more than $400 billion per year in federal and state funding is allocated to communities for neighborhood improvements, public health, education and more; the Census Bureau is mandated with fulfilling these obligations: the collecting of statistics about the nation, its people, economy. The Census Bureau's legal authority is codified in Title 13 of the United States Code.
The Census Bureau conducts surveys on behalf of various federal government and local government agencies on topics such as employment, health, consumer expenditures, housing. Within the bureau, these are known as "demographic surveys" and are conducted perpetually between and during decennial population counts; the Census Bureau conducts economic surveys of manufacturing, retail and other establishments and of domestic governments. Between 1790 and 1840, the census was taken by marshals of the judicial districts; the Census Act of 1840 established a central office. Several acts followed that revised and authorized new censuses at the 10-year intervals. In 1902, the temporary Census Office was moved under the Department of Interior, in 1903 it was renamed the Census Bureau under the new Department of Commerce and Labor; the department was intended to consolidate overlapping statistical agencies, but Census Bureau officials were hindered by their subordinate role in the department. An act in 1920 changed the date and authorized manufacturing censuses every two years and agriculture censuses every 10 years.
In 1929, a bill was passed mandating the House of Representatives be reapportioned based on the results of the 1930 Census. In 1954, various acts were codified into Title 13 of the US Code. By law, the Census Bureau must count everyone and submit state population totals to the U. S. President by December 31 of any year ending in a zero. States within the Union receive the results in the spring of the following year; the United States Census Bureau defines four statistical regions, with nine divisions. The Census Bureau regions are "widely used...for data collection and analysis". The Census Bureau definition is pervasive. Regional divisions used by the United States Census Bureau: Region 1: Northeast Division 1: New England Division 2: Mid-Atlantic Region 2: Midwest Division 3: East North Central Division 4: West North Central Region 3: South Division 5: South Atlantic Division 6: East South Central Division 7: West South Central Region 4: West Division 8: Mountain Division 9: Pacific Many federal, state and tribal governments use census data to: Decide the location of new housing and public facilities, Examine the demographic characteristics of communities and the US, Plan transportation systems and roadways, Determine quotas and creation of police and fire precincts, Create localized areas for elections, utilities, etc.
Gathers population information every 10 years The United States Census Bureau is committed to confidentiality, guarantees non-disclosure of any addresses or personal information related to individuals or establishments. Title 13 of the U. S. Code establishes penalties for the disclosure of this information. All Census employees must sign an affidavit of non-disclosure prior to employment; the Bureau cannot share responses, addresses or personal information with anyone including United States or foreign government
Greenville County, South Carolina
Greenville County is a county located in the state of South Carolina, in the United States. As of the 2010 census, the population was 451,225. In 2017, the estimated population of the county was 506,837, its county seat is Greenville. The county is home to the Greenville County School District, the largest school system in South Carolina. County government is headquartered at Greenville County Square. Greenville County is included in SC Metropolitan Statistical Area. According to the U. S. Census Bureau, the county has a total area of 795 square miles, of which 785 square miles is land and 9.7 square miles is water. As of the 2010 United States Census, there were 451,225 people, 176,531 households, 119,362 families residing in the county; the population density was 574.7 inhabitants per square mile. There were 195,462 housing units at an average density of 249.0 per square mile. The racial makeup of the county was 73.8% white, 18.1% black or African American, 2.0% Asian, 0.3% American Indian, 0.1% Pacific islander, 3.9% from other races, 1.9% from two or more races.
Those of Hispanic or Latino origin made up 8.1% of the population. In terms of ancestry, 13.0% were American, 11.6% were German, 10.9% were English, 10.7% were Irish. Of the 176,531 households, 33.7% had children under the age of 18 living with them, 49.7% were married couples living together, 13.5% had a female householder with no husband present, 32.4% were non-families, 27.0% of all households were made up of individuals. The average household size was 2.49 and the average family size was 3.03. The median age was 37.2 years. The median income for a household in the county was $46,830 and the median income for a family was $59,043. Males had a median income of $45,752 versus $33,429 for females; the per capita income for the county was $25,931. About 10.8% of families and 14.1% of the population were below the poverty line, including 20.0% of those under age 18 and 9.1% of those age 65 or over. As of 2016 the largest self-reported ancestry groups in Greenville County, South Carolina are: CommunityWorks Federal Credit Union was chartered in 2014 to serve the residents of Greenville County.
It is sponsored by CommunityWorks, Inc. a non-profit community development financial institution, receives assistance from the United Way of Greenville County and the Hollingsworth Fund. The 2010 Census lists six cities and 16 census designated places that are or within Greenville County. Fountain Inn Greenville Greer Mauldin Simpsonville Travelers Rest Cleveland Conestee National Register of Historic Places listings in Greenville County, South Carolina Greenville Area Development Corporation Geographic data related to Greenville County, South Carolina at OpenStreetMap Greenville County History and Images