Special education is the practice of educating students in a way that addresses their individual differences and needs. Ideally, this process involves the individually planned and systematically monitored arrangement of teaching procedures, adapted equipment and materials, accessible settings; these interventions are designed to help individuals with special needs achieve a higher level of personal self-sufficiency and success in school and in their community which may not be available if the student were only given access to a typical classroom education. Special education includes learning disabilities, communication disorders and behavioral disorders, physical disabilities, developmental disabilities and many other disabilities. Students with these kinds of disabilities are to benefit from additional educational services such as different approaches to teaching, the use of technology, a adapted teaching area, or a resource room. Intellectual giftedness is a difference in learning and can benefit from specialized teaching techniques or different educational programs, but the term "special education" is used to indicate instruction of students with disabilities.
Gifted education is handled separately. Whereas special education is designed for students with learning disabilities, remedial education can be designed for any students, with or without special needs. For example people of high intelligence can be under-prepared if their education was disrupted, for example, by internal displacement during civil disorder or a war. In most developed countries, educators modify teaching methods and environments so that the maximum number of students are served in general education environments. Therefore, special education in developed countries is regarded as a service rather than a place. Integration can improve academic achievement for many students; the opposite of special education is general education. General education is the standard curriculum supports. Students receiving special education services can sometimes enroll in a General education setting to learn along with students without disabilities; some children are identified as candidates for special needs due to their medical history.
For example, they may have been diagnosed with a genetic condition, associated with intellectual disability, may have various forms of brain damage, may have a developmental disorder, may have visual or hearing disabilities, or other disabilities. On the other hand, for students with less obvious disabilities, such as those who have learning difficulties, two primary methods have been used for identifying them: the discrepancy model and the response to intervention model; the discrepancy model depends on the teacher noticing that the students' achievements are noticeably below what is expected. At which the teacher may make the decision for the student to receive support from a special education specialist. Before doing so, the teacher must show documentation of low academic achievement; the response to intervention model advocates earlier intervention. In the discrepancy model, a student receives special education services for a specific learning difficulty if the student has at least normal intelligence and the student's academic achievement is below what is expected of a student with his or her IQ.
Although the discrepancy model has dominated the school system for many years, there has been substantial criticism of this approach among researchers. One reason for criticism is that diagnosing SLDs on the basis of the discrepancy between achievement and IQ does not predict the effectiveness of treatment. Low academic achievers who have low IQ appear to benefit from treatment just as much as low academic achievers who have normal or high intelligence; the alternative approach, response to intervention, identifies children who are having difficulties in school in their first or second year after starting school. They receive additional assistance such as participating in a reading remediation program; the response of the children to this intervention determines whether they are designated as having a learning disability. Those few who still have trouble may receive designation and further assistance. Sternberg has argued that early remediation can reduce the number of children meeting diagnostic criteria for learning disabilities.
He has suggested that the focus on learning disabilities and the provision of accommodations in school fails to acknowledge that people have a range of strengths and weaknesses and places undue emphasis on academics by insisting that students should be supported in this arena and not in music or sports. A special education program should be customized to address each individual student's unique needs. Special educators provide a continuum of services, in which students with various disabilities receive multiple degrees of support based on their individual needs, it is crucial for special education programs to be individualized so that they address the unique combination of needs in a given student. In the United States and the UK, educational professionals use a student's Individualized Education Program. Another name for a student's Individualized Education Plan is a student's Individual Learning Pl
Greenville, South Carolina
Greenville is the largest city in and the seat of Greenville County, South Carolina, United States. The city's mayor is Knox H. White, in that position since December 1995. With an estimated population of 68,219 as of 2017, it is the sixth-largest city in the state; the population of the surrounding area was 400,492 as of 2010, making it the third-largest urban area in South Carolina as well as the fastest growing. Greenville is the largest city in the Greenville-Anderson-Mauldin Metropolitan Statistical Area; the MSA had a population of 895,923 in 2017, making it the largest in South Carolina and the third largest in the Carolinas. Greenville is the largest city in the Greenville-Spartanburg-Anderson Combined Statistical Area, a 10-county region of northwestern South Carolina known as "The Upstate". According to United States Census Bureau, the CSA had a population of 1,459,766 as of 2017, making it the largest CSA in the state. Greenville is located halfway between Atlanta and Charlotte, North Carolina, along Interstate 85, its metropolitan area includes Interstates 185 and 385.
Greenville has gained recognition in various national publications such as CNN Money, which ranked Greenville as one of the "Top 10 Fastest Growing Cities in the U. S." Bloomberg named Greenville the Third Strongest Job Market for 2010. Greenville earned the No. 3 slot by Condé Nast Traveler's "Best Small Cities in the U. S." in 2017. Greenville was the fourth fastest-growing city in the United States between 2015 and 2016, according to the U. S. Census Bureau; the land of present-day Greenville was once the hunting ground of the Cherokee, forbidden to colonists. A wealthy settler from Virginia named Richard Pearis arrived in South Carolina around 1754 and established relations with the Cherokee. Pearis had a child with a Cherokee woman and received about 100,000 acres from the Cherokee around 1770. Pearis established a plantation on the Reedy River called the Great Plains in present-day downtown Greenville; the American Revolution divided the South Carolina country between the Patriots. Pearis supported the Loyalists and together with their allies.
The Patriots retaliated by jailing him in Charleston. Pearis never returned to his plantation but Paris Mountain is named after him; the Treaty of Dewitt's Corner in 1777 ceded all Cherokee land, including present-day Greenville, to South Carolina. Greenville County was named for its physical appearance. However, other sources say Greenville is named after General Nathanael Greene in honor of his service in the American Revolutionary War. Lemuel J. Alston came to Greenville County in 1788 and bought 400 acres and a portion of Pearis' former plantation. In 1797 Alston used his land holdings to establish a village called Pleasantburg where he built a stately mansion. In 1816, Alston's land was purchased by Vardry McBee, who leased the Alston mansion for a summer resort, before making mansion his home from 1835 until his death in 1864. Considered to be the father of Greenville, McBee donated land for many structures such as churches, a cotton mill. Furman University was funded by McBee who helped bring the university to Pleasantburg from Winnsboro, South Carolina in 1851.
In 1853 McBee and other Greenville County leaders funded a new railroad called the Greenville and Columbia Railroad. Pleasantburg boomed to around 1,000 in the 1850s due to the growth of McBee's donations and the attraction of the town as a summer resort for visitors. In 1831 Pleasantburg was incorporated as Greenville. In December 1860 Greenville supported a convention to debate the issue of secession for South Carolina; the Greenville District sent James Furman, William K. Easley, Perry E. Duncan, William H. Campbell, James P. Harrison as delegates for the convention. On December 20, 1860 the South Carolina state convention, along with the Greenville delegation, voted to secede from the Union. Greenville County provided over 2,000 soldiers to the Confederate States Army; the town supplied food and firearms to the Confederacy. Greenville saw no action from the war until 1865 when Union troops came through the town looking for President Jefferson Davis of the Confederacy who had fled south from Richmond, Virginia.
In June 1865 Andrew Johnson appointed Greenville County native Benjamin Franklin Perry as Governor of South Carolina. In February 1869, Greenville's town charter was amended by the S. C. General Assembly establishing Greenville, the town, as a city. Construction boomed in the 1870s such as the establishment of a bridge over the Reedy River, new mills on the river and new railroads; the Greenville News was established in 1874 as Greenville's first daily newspaper. Southern Bell installed the first telephone lines in the city; the most important infrastructure that came to the city were cotton mills. Prominent cotton mill businesses operated near Greenville making it a cotton mill town. By 1915 Greenville became known as the "Textile Center of the South." During World War I, Greenville served as a training camp center for Army recruits. After World War I commercial activity expanded with new movie theaters and department stores; the Mansion House was demolished and replaced with the Poinsett Hotel in 1925.
The Great Depression hurt the economy of Greenville forcing mills to lay off workers. Furman University and the Greenville Women's College struggled in the crippling economy forcing them to merge in 1933; the Textile Workers Strike of 1934 caused such an uproar in the city and surrounding mill towns that the National Guard had to subdue the chaos. The New Deal established Sirrine S
South Carolina is a state in the Southeastern United States and the easternmost of the Deep South. It is bordered to the north by North Carolina, to the southeast by the Atlantic Ocean, to the southwest by Georgia across the Savannah River. South Carolina became the eighth state to ratify the U. S. Constitution on May 23, 1788. South Carolina became the first state to vote in favor of secession from the Union on December 20, 1860. After the American Civil War, it was readmitted into the United States on June 25, 1868. South Carolina is the 40th most extensive and 23rd most populous U. S. state. Its GDP as of 2013 was $183.6 billion, with an annual growth rate of 3.13%. South Carolina is composed of 46 counties; the capital is Columbia with a 2017 population of 133,114. The Greenville-Anderson-Mauldin metropolitan area is the largest in the state, with a 2017 population estimate of 895,923. South Carolina is named in honor of King Charles I of England, who first formed the English colony, with Carolus being Latin for "Charles".
South Carolina is known for its 187 miles of coastline, beautiful lush gardens, historic sites and Southern plantations, colonial and European cultures, its growing economic development. The state can be divided into three geographic areas. From east to west: the Atlantic coastal plain, the Piedmont, the Blue Ridge Mountains. Locally, the coastal plain is referred to the other two regions as Upstate; the Atlantic Coastal Plain makes up two-thirds of the state. Its eastern border is a chain of tidal and barrier islands; the border between the low country and the up country is defined by the Atlantic Seaboard fall line, which marks the limit of navigable rivers. The state's coastline contains many salt marshes and estuaries, as well as natural ports such as Georgetown and Charleston. An unusual feature of the coastal plain is a large number of Carolina bays, the origins of which are uncertain; the bays tend to be oval. The terrain is flat and the soil is composed of recent sediments such as sand and clay.
Areas with better drainage make excellent farmland. The natural areas of the coastal plain are part of the Middle Atlantic coastal forests ecoregion. Just west of the coastal plain is the Sandhills region; the Sandhills are remnants of coastal dunes from a time when the land was sunken or the oceans were higher. The Upstate region contains the roots of an eroded mountain chain, it is hilly, with thin, stony clay soils, contains few areas suitable for farming. Much of the Piedmont was once farmed. Due to the changing economics of farming, much of the land is now reforested in Loblolly pine for the lumber industry; these forests are part of the Southeastern mixed forests ecoregion. At the southeastern edge of the Piedmont is the fall line, where rivers drop to the coastal plain; the fall line was an important early source of water power. Mills built to harness this resource encouraged the growth of several cities, including the capital, Columbia; the larger rivers are navigable up to the fall line. The northwestern part of the Piedmont is known as the Foothills.
The Cherokee Parkway is a scenic driving route through this area. This is. Highest in elevation is the Blue Ridge Region, containing an escarpment of the Blue Ridge Mountains, which continue into North Carolina and Georgia, as part of the southern Appalachian Mountains. Sassafras Mountain, South Carolina's highest point at 3,560 feet, is in this area. In this area is Caesars Head State Park; the environment here is that of the Appalachian-Blue Ridge forests ecoregion. The Chattooga River, on the border between South Carolina and Georgia, is a favorite whitewater rafting destination. South Carolina has several major lakes covering over 683 square miles. All major lakes in South Carolina are man-made; the following are the lakes listed by size. Lake Marion 110,000 acres Lake Strom Thurmond 71,100 acres Lake Moultrie 60,000 acres Lake Hartwell 56,000 acres Lake Murray 50,000 acres Russell Lake 26,650 acres Lake Keowee 18,372 acres Lake Wylie 13,400 acres Lake Wateree 13,250 acres Lake Greenwood 11,400 acres Lake Jocassee 7,500 acres Lake Bowen Earthquakes in South Carolina demonstrate the greatest frequency along the central coastline of the state, in the Charleston area.
South Carolina averages 10–15 earthquakes a year below magnitude 3. The Charleston Earthquake of 1886 was the largest quake to hit the Southeastern United States; this 7.2 magnitude earthquake destroyed much of the city. Faults in this region are difficult to study at the surface due to thick sedimentation on top of them. Many of the ancient faults are within plates rather than along plate boundaries. South Carolina has a humid subtropical climate, although high-elevation areas in the Upstate area have fewer subtropical characteristics than areas on the Atlantic coastline. In the summer, South Carolina is hot and humid, with daytime temperatures averaging between 86–93 °F in most of the state and overnight lows averaging 70–75 °F on the coast and from 66–73 °F inland. Winter temperatures are much less uniform in South Carolina. Coastal areas of the state have mild winters, with high temperatures approaching an average of 60 °F and overnight lows around 40 °F. Inland, the average January overnight low is around 32 °F i
1890 United States Census
The Eleventh United States Census was taken beginning June 2, 1890. It determined the resident population of the United States to be 62,979,766—an increase of 25.5 percent over the 50,189,209 persons enumerated during the 1880 census. The data was tabulated by machine for the first time; the data reported that the distribution of the population had resulted in the disappearance of the American frontier. Most of the 1890 census materials were destroyed in a 1921 fire and fragments of the US census population schedule exist only for the states of Alabama, Illinois, New Jersey, New York, North Carolina, South Dakota, Texas, the District of Columbia; this was the first census in which a majority of states recorded populations of over one million, as well as the first in which multiple cities – New York as of 1880, Philadelphia – recorded populations of over one million. The census saw Chicago rank as the nation's second-most populous city, a position it would hold until 1990, in which Los Angeles would supplant it.
The 1890 census collected the following information: The 1890 census was the first to be compiled using methods invented by Herman Hollerith and was overseen by Superintendents Robert P. Porter and Carroll D. Wright. Data was entered on a machine readable medium, punched cards, tabulated by machine; the net effect of the many changes from the 1880 census: the larger population, the number of data items to be collected, the Census Bureau headcount, the volume of scheduled publications, the use of Hollerith's electromechanical tabulators, was to reduce the time required to process the census from eight years for the 1880 census to six years for the 1890 census. The total population of 62,947,714, the family, or rough, was announced after only six weeks of processing; the public reaction to this tabulation was disbelief, as it was believed that the "right answer" was at least 75,000,000. The United States census of 1890 showed a total of 248,253 Native Americans living in the United States, down from 400,764 Native Americans identified in the census of 1850.
The 1890 census announced that the frontier region of the United States no longer existed, that the Census Bureau would no longer track the westward migration of the U. S. population. Up to and including the 1880 census, the country had a frontier of settlement. By 1890, isolated bodies of settlement had broken into the unsettled area to the extent that there was hardly a frontier line; this prompted Frederick Jackson Turner to develop his Frontier Thesis. The original data for the 1890 Census is no longer available. All the population schedules were damaged in a fire in the basement of the Commerce Building in Washington, D. C. in 1921. Some 25 % of the materials were presumed another 50 % damaged by smoke and water; the damage to the records led to an outcry for a permanent National Archives. In December 1932, following standard federal record-keeping procedures, the Chief Clerk of the Bureau of the Census sent the Librarian of Congress a list of papers to be destroyed, including the original 1890 census schedules.
The Librarian was asked by the Bureau to identify any records which should be retained for historical purposes, but the Librarian did not accept the census records. Congress authorized destruction of that list of records on February 21, 1933, the surviving original 1890 census records were destroyed by government order by 1934 or 1935; the other censuses for which some information has been lost are the 1810 enumerations. Few sets of microdata from the 1890 census survive, but aggregate data for small areas, together with compatible cartographic boundary files, can be downloaded from the National Historical Geographic Information System. Mayo-Smith, Richmond, "The Eleventh Census of the United States". In: The Economic Journal, Vol. 1, p. 43 - 58 1891 U. S Census Report Contains 1890 Census results Historical US Census data from the U. S. Census Bureau website Hollerith 1890 Census Tabulator by Columbia University "The Fate of the 1890 Population Census" from the National Archives website
A county seat is an administrative center, seat of government, or capital city of a county or civil parish. The term is used in Canada, Romania and the United States. County towns have a similar function in the United Kingdom and Republic of Ireland, in Jamaica. In most of the United States, counties are the political subdivisions of a state; the city, town, or populated place that houses county government is known as the seat of its respective county. The county legislature, county courthouse, sheriff's department headquarters, hall of records and correctional facility are located in the county seat though some functions may be located or conducted in other parts of the county if it is geographically large. A county seat is but not always, an incorporated municipality; the exceptions include the county seats of counties that have no incorporated municipalities within their borders, such as Arlington County, Virginia. Ellicott City, the county seat of Howard County, is the largest unincorporated county seat in the United States, followed by Towson, the county seat of Baltimore County, Maryland.
Some county seats may not be incorporated in their own right, but are located within incorporated municipalities. For example, Cape May Court House, New Jersey, though unincorporated, is a section of Middle Township, an incorporated municipality. In some of the colonial states, county seats include or included "Court House" as part of their name. In the Canadian provinces of Prince Edward Island, New Brunswick, Nova Scotia, the term "shire town" is used in place of county seat. County seats in Taiwan are the administrative centers of the counties. There are 13 county seats in Taiwan, which are in the forms of county-administered city, urban township or rural township. Most counties have only one county seat. However, some counties in Alabama, Georgia, Kentucky, Mississippi, New Hampshire, New York, Vermont have two or more county seats located on opposite sides of the county. An example is Harrison County, which lists both Biloxi and Gulfport as county seats; the practice of multiple county seat towns dates from the days.
There have been few efforts to eliminate the two-seat arrangement, since a county seat is a source of pride for the towns involved. There are 36 counties with multiple county seats in 11 states: Coffee County, Alabama St. Clair County, Alabama Arkansas County, Arkansas Carroll County, Arkansas Clay County, Arkansas Craighead County, Arkansas Franklin County, Arkansas Logan County, Arkansas Mississippi County, Arkansas Prairie County, Arkansas Sebastian County, Arkansas Yell County, Arkansas Columbia County, Georgia Lee County, Iowa Campbell County, Kentucky Kenton County, Kentucky Essex County, Massachusetts Middlesex County, Massachusetts Plymouth County, Massachusetts Bolivar County, Mississippi Carroll County, Mississippi Chickasaw County, Mississippi Harrison County, Mississippi Hinds County, Mississippi Jasper County, Mississippi Jones County, Mississippi Panola County, Mississippi Tallahatchie County, Mississippi Yalobusha County, Mississippi Jackson County, Missouri Hillsborough County, New Hampshire Seneca County, New York Bennington County, Vermont In New England, the town, not the county, is the primary division of local government.
Counties in this region have served as dividing lines for the states' judicial systems. Connecticut and Rhode Island have no county level of thus no county seats. In Vermont and Maine the county seats are designated shire towns. County government consists only of a Superior Court and Sheriff, both located in the respective shire town. Bennington County has two shire towns. In Massachusetts, most government functions which would otherwise be performed by county governments in other states are performed by town or city governments; as such, Massachusetts has dissolved many of its county governments, the state government now operates the registries of deeds and sheriff's offices in those counties. In Virginia, a county seat may be an independent city surrounded by, but not part of, the county of which it is the administrative center. Two counties in South Dakota have their county seat and government services centered in a neighboring county, their county-level services are provided by Fall River Tripp County, respectively.
In Louisiana, divided into parishes rather than counties, county seats are referred to as parish seats. Alaska is divided into boroughs rather than counties; the Unorganized Borough, which covers 49 % of Alaska's area, has equivalent. The state with the most counties is Texas, with 254, the state with the fewest counties is Delaware, with 3. County seat war Administrative center County town, administrative centres in Ireland and the UK Chef-lieu, administrative centres in Algeria, Luxembourg, France and Tunisia Municipality, equivalent to county in many c
Time in the United States
Time in the United States, by law, is divided into nine standard time zones covering the states and its possessions, with most of the United States observing daylight saving time for the spring and fall months. The time zone boundaries and DST observance are regulated by the Department of Transportation. Official and precise timekeeping services are provided by two federal agencies: the National Institute of Standards and Technology; the clocks run by these services are kept synchronized with each other as well as with those of other international timekeeping organizations. It is the combination of the time zone and daylight saving rules, along with the timekeeping services, which determines the legal civil time for any U. S. location at any moment. Before the adoption of four standard time zones for the continental United States, many towns and cities set their clocks to noon when the sun passed their local meridian, pre-corrected for the equation of time on the date of observation, to form local mean solar time.
Noon occurred at different times but time differences between distant locations were noticeable prior to the 19th century because of long travel times and the lack of long-distance instant communications prior to the development of the telegraph. The use of local solar time became awkward as railways and telecommunications improved. American railroads maintained many different time zones during the late 1800s; each train station set its own clock making it difficult to coordinate train schedules and confusing passengers. Time calculation became a serious problem for people traveling by train, according to the Library of Congress; every city in the United States used a different time standard so there were more than 300 local sun times to choose from. Time zones were therefore a compromise, relaxing the complex geographic dependence while still allowing local time to be approximate with mean solar time. Railroad managers tried to address the problem by establishing 100 railroad time zones, but this was only a partial solution to the problem.
Weather service chief Cleveland Abbe had needed to introduce four standard time zones for his weather stations, an idea which he offered to the railroads. Operators of the new railroad lines needed a new time plan that would offer a uniform train schedule for departures and arrivals. Four standard time zones for the continental United States were introduced at noon on November 18, 1883, when the telegraph lines transmitted time signals to all major cities. In October 1884, the International Meridian Conference at Washington DC adopted a proposal which stated that the prime meridian for longitude and timekeeping should be one that passes through the centre of the transit instrument at the Greenwich Observatory in the United Kingdom; the conference therefore established the Greenwich Meridian as the prime meridian and Greenwich Mean Time as the world's time standard. The US time-zone system grew from this, in which all zones referred back to GMT on the prime meridian. In 1960, the International Radio Consultative Committee formalized the concept of Coordinated Universal Time, which became the new international civil time standard.
UTC is, within about 1 second, mean solar time at 0°. UTC does not observe daylight saving time. For most purposes, UTC is considered interchangeable with GMT, but GMT is no longer defined by the scientific community. UTC is one of several related successors to GMT. Standard time zones in the United States are defined at the federal level by law 15 USC §260; the federal law establishes the transition dates and times at which daylight saving time occurs, if observed. It is the authority of the Secretary of Transportation, in coordination with the states, to determine which regions will observe which of the standard time zones and if they will observe daylight saving time; as of August 9, 2007, the standard time zones are defined in terms of hourly offsets from UTC. Prior to this they were based upon the mean solar time at several meridians 15° apart west of Greenwich. Only the full-time zone names listed below are official. View the standard time zone boundaries here; the United States uses nine standard time zones.
As defined by US law they are: From east to west, the four time zones of the contiguous United States are: Eastern Time Zone, which comprises the states on the Atlantic coast and the eastern two thirds of the Ohio Valley. Central Time Zone, which comprises the Gulf Coast, Mississippi Valley, most of the Great Plains. Mountain Time Zone, which comprises the states and portions of states that include the Rocky Mountains and the western quarter of the Great Plains. Pacific Time Zone, which comprises the states on the Pacific coast, plus Nevada and the Idaho panhandle. Alaska Time Zone, which comprises most of the state of Alaska. Hawaii-Aleutian Time Zone, which includes Hawaii and most of the length of the Aleutian Islands chain. Samoa Time Zone, which comprises American Samoa. Chamorro Time Zone, which comprises Guam and the Northern Mariana Islands. Atlantic Time Zone, which comprises Puerto Rico and the US Virgin Islands; some United States Minor Outlying Islands are outside the time zones defined by 15 U.
S. C. § exist in waters defined by Nautical time. In practice, military crews may
Interstate 26 in South Carolina
Interstate 26 is a South Carolina Interstate highway running east–west from near Landrum, in Spartanburg County, to U. S. Route 17, in Charleston, South Carolina, it is the longest interstate highway in South Carolina. I-26 runs 220 miles through South Carolina. Mile markers run from west to east. Mile Marker 0 is in the mountains at the NC state line; the last exit, at US 17 south of Charleston, is exit 221. I-26 runs between the Broad and Saluda Rivers, descending from the mountains to the piedmont or midlands. At Columbia, I-126 crosses the confluence of the Broad and Saluda, which together form the Congaree, near the Columbia Canal and water treatment plant. I-26 continues following the Congaree, until it hops south over into the Cooper and Ashley Drainage down to the coast. I-26 is predominantly a four-lane rural interstate with 70-mile-per-hour speed limits. In the Columbia and Charleston areas, the interstate widens to six-lanes. I-26 enters South Carolina just northeast of Landrum; the first major city along its route is Spartanburg, where it intersects I-85 to Greenville and Charlotte.
As the interstate weaves along the terrain, it reaches Clinton. Traveling through the Sumter National Forest, it connects with Newberry before entering the Midlands. At Columbia in a section known as "Malfunction Junction", it connects with I-20, to Augusta and Florence, I-126 towards the downtown area. At Cayce, it connects with I-77 to Charlotte. South of Cayce, the interstate goes up and down a few long hills before reaching the outskirts of Orangeburg and I-95, to Savannah and Florence; as it enters the flat plains of the Lowcountry, the area becomes urbanized as the interstate encroaches upon North Charleston and Charleston. As the interstate curves through the peninsula formed by the Ashley and Cooper rivers, it connects with I-526, to Savannah and Mount Pleasant. Near the end, it overlaps with US 17 from its new interchange to where the old interchange remnants and where I-26 ends. Construction of I-26 began in 1957 in the Columbia area with the 9-mile section from the Broad River to near Irmo.
The 11-mile section of I-26 from I-126/US 76 in Columbia to US 176 at Exit 97 was the first section of the highway to open up to traffic. The 6-mile section from SC 210 to US 15 opened in September 1962. Construction proceeded in stages heading both west up towards Greenville and east towards Charleston; the highway was completed from Columbia to North Charleston by 1964. The entire 221 miles of I-26 were completed by February 1969. In the 1980s-90s, I-26 around Columbia was widened from four to six lanes. In the mid-90s, the North Charleston area was widened from four to six lanes, part of, further widened to eight lanes in the early 2010s. In 2005, the US 17 was realigned to a new interchange with I-26 at exit 220 from exit 221. In the mid-2010s, I-26 was widened SE of Columbia from I-77 to Old Sandy Run Rd. Starting in 2019 or 2020, a long stretch of I-26 NW of Columbia will begin widening construction from four to six lanes from SC 202 at Little Mountain to US 76/176 at Irmo. In 2011, a plan to add a lane in each direction between Broad River Road and St. Andrews Road through "Malfunction Junction" had $8.5 million in funding but was expected to start sometime after 2012 and take two years.
On October 5, 2016, I-26 had all lanes converted to westbound only, from I-77 to I-526, due to Hurricane Matthew. This was done again on September 11, 2018 due to Hurricane Florence; the lane reversal is still in effect as of September 12, 2018. On November 19, 2016, construction began in Charleston to demolish and replace exits 217 and 218, related to a new access road to the Hugh K. Leatherman Sr. Terminal. Ashley River Enoree River Lake Murray Saluda River Sumter National Forest Media related to Interstate 26 in South Carolina at Wikimedia Commons Mapmikey's South Carolina Highways Page: I-26 Economic Development History of Interstate 26 in South Carolina - Federal Highway Administration