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Chick Springs is a mineral springs in present-day Taylors, Greenville County, South Carolina, which from the mid-nineteenth to the early twentieth century served as the focus of a small Upstate South Carolina resort community.
For the 2013-2014 Academic Year, Spartanburg District 2 was named the top school district in the State of South Carolina by the South Carolina Department of Education. [ 11 ] 63% of educators in Spartanburg District 2 have a master's degree or higher, and 19% are National Board certified, placing the district in the top 1% of school districts ...
This is intended to be a complete list of the properties and districts on the National Register of Historic Places in Greenville County, South Carolina, United States. The locations of National Register properties and districts for which the latitude and longitude coordinates are included below, may be seen in a map.
U.S. Highway 25 (US 25) is a north–south United States Numbered Highway that runs for 75.4 miles (121.3 km) from the South Carolina state line, near Tuxedo, to the Tennessee state line, near Hot Springs. It is part of the longer US 25, which runs from Brunswick, Georgia, to Covington, Ohio.
The T.Q. Donaldson House was built by William Williams for Thomas Q. Donaldson, a lawyer and member of the South Carolina Senate from Greenville County from 1872-1876. The house was originally built as a 1 + 1 ⁄ 2-story house; soon after the original construction, a second story was added. 14: Downtown Baptist Church: Downtown Baptist Church
Glenn Springs Historic District is a national historic district located at Glenn Springs, Spartanburg County, South Carolina. It encompasses 18 contributing buildings and 3 contributing sites in the historic health resort of Glenn Springs. The community developed as a resort around the mineral springs between about 1840 and 1940.
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The Sandhills, or Carolina Sandhills, is a 15–60 km wide region within the Atlantic Coastal Plain province, along the inland margin of this province. The Carolina Sandhills are interpreted as eolian (wind-blown) sand sheets and dunes that were mobilized episodically approximately 75,000 to 6,000 years ago. [2]