Pacolet in Spartanburg County, South Carolina — The American South (South Atlantic)
Pacolet River Heritage Preserve
Pacolet River Heritage Preserve, owned and managed by the S.C. Department of Natural Resources, covers 278 acres in Spartanburg County, SC. Come to bird-watch, take photographs, fish or simply enjoy the woods and Pacolet River. Leave with a sense of awe sparked by visiting a site important to people thousands of years ago. As you sit watching the river, imagine the lives of the Native Americans who stopped here on their seasonal migrations between the coast and the uplands of the state.
What to look for...
The preserve protects two Native American soapstone quarries. Early residents of the state came here between 3000 and 1100 B.C. to obtain material to make bowls, pipes, and other necessities. The soapstone outcrops are fragile and should not be touched.
Two uncommon plant species, a moss and a leafy liver wort are also protected within the preserve. Less rare, but no less interesting, are the summer pine/hardwoods along the Pacolet River. In summertime, the forest shelters wood thrushes, red-eyed vireos, Eastern wood pewees and yellow-billed cuckoos, along with more commonly-seen songbirds. Reptiles and amphibians love the woods, too. Look for harmless, black rat snakes and Eastern kingsnakes, as well as gray treefrogs, toads and other amphibians. Allow about 30 minutes to walk the short trail from
When to go...
The preserve is open from daylight to dark. Spring and fall are the best times to see migrating songbirds, and the hardwoods should produce good fall color.
What is Soapstone?
Soapstone is a metamorphic rock found along the collision zones of tectonic plates. To the touch this sock has a soapy or oily feel because its major component is the soft mineral talc. Outcrops of soapstone occur along northwestern margins of the King's Mountain Shear Zone. This geological one marks the boundary between the Inner Piedmont Belt and the Carolina Slate Belt and the meeting place of two ancient continents. Created during the Ordovician period (490 to 443 million years ago) these soapstone outcrops are reminders of powerful geologic processes that produced the South Carolina that we know today. Sometime during the Archaic Period (8,000 - 3,000 BC) Native American people started quarrying this material for use as hunting tools, jewelry and because of its superior ability to with stand thermal shock it was turned into cooking slabs and bowls.
Prior to the development of pottery in the Late Archaic Period, 4,000 - 3,000 BC, soapstone was an important raw material for Southeastern Indians. Raw nuts and tubers, a large component of the prehistoric forager's diet, required cooking before they were
The use of heated rocks to cook food has been documented in archaeological sites across the Southeast. After a few uses most rocks disintegrate due to rapid heating and cooling, known as thermal shock, leaving behind fire cracked rock. Soapstone has a superior resistance to thermal shock, and because it is a soft stone it can be carved into easily transportable objects. Perforated soapstone discs have been found throughout the coastal plain and in other parts of South Carolina well away from the material's geologic occurrence. Mobility was important to the people of the Southeast during the Paleoindian and Archaic periods. These people were dependent upon their ability to relocate to areas where they could take advantage of seasonally available foods, soapstone slabs made cooking unpalatable foods
During the Late Archaic Period, soapstone technology might have assumed a position of greater value to the cultures of the Southeast. Worked soapstone discs and bowls from the Late Archaic Period have been found as far afield as the panhandle of Florida and the coastal plain of Louisiana. These locations are hundreds of miles from natural deposits of soapstone and their presence has been attributed to trade or migration of groups between these areas and upland regions. Also during this period, pottery took over as the predominant cooking technology and potsherds have been found to co-occur with soapstone bowls and discs. While pottery was used for the production of everyday food, feasts might have had communal importance that required the use of soapstone, because with it, large amounts of food could be cooked quickly, and because of its importance as an ancestral tool.
In 1969, Terry Ferguson and students from Spartanburg's own Wofford College documented the soapstone outcroppings present within the boundaries of the Pacolet River Heritage Preserve. They are part of a chain of outcroppings that extend from Croft State Park into Cherokee County. Most outcrops exhibit evidence for their use by prehistoric Native Americans. The people who utilized it as a resource likely considered this area very special.
Today, artifacts from this area help fill in out interpretations of prehistoric times. Disturbing the artifacts, and the soapstone outcrops, harms our ability to learn bout the past from material remains and prevents future research from gaining an accurate picture. Collecting artifacts on the preserve site is strictly prohibited by State Law.
The Great Flood of 1903
During the 19th Century, early settlers of Spartanburg County concentrated on developing farms and industries along the floodplains of rivers and creeks. These areas provided good soil for farming and waterpower for mills. When major textile manufacturing decided to take advantage of the Pacolet River. Water provided the power for the large thread spinners and weaving looms at the Pacolet and Clifton Mills. With the opening of these mills, communities developed. Textile mill owners provided lodging for their "mill operators" in the immediate vicinity of the mill, because their industrial work
Accounts of the Great Flood of 1903...
By the sixth of June, 5 inches of rain fell across Upstate South Carolina and western North Carolina. Between 5:30 am and 6:30 am, the waters of the Pacolet River rose 40 feet. The force of this flood battered everything in its path. A dam at Pacolet Mills resisted the flood for a while, diverting the floodwaters into the mills on the west bank of the river. Pacolet Mills No. 1 and No. 2 were devastated by the impact of rushing water and debris. Pacolet Mill No. 3, though severely.
The effects of the flood were felt throughout the county. When the waters began receding, 3,500 bales of cotton and 4,500 bales of cloth dotted the banks of the river along with broken machinery and debris that formed constituted businesses, mills and homes. The flood isolated the county from relief. Every bridge across the river, save one wagon bridge washed away, including the Southern Railway trestles crossing the Pacolet and Lawson's Fork. The trestle over Lawson's Fork weighed in excess of 2,500,000 lbs and the flood waters carried it 150 yards downstream.
The bridge abutments down this trail are all that remain of a rock and concrete bridge washed out during the Great Flood of 1903. Now it stands as a reminder that the Pacolet River could being devastation to its normally quiet banks.
"...railroad bridges were torn from stone and iron piers, county bridges rolled away like straw, cotton mills crashed before the flood and grist mills and smaller industries innumerable washed off in raging waters.
"All over the sea of angry waters could be seen the projected tops of trees buried beneath the flood, while plank, wood and debris of every imaginable description could be seen floating down stream..."
-- Spartanburg Journal, Vol. III No. 234 Sat., June 6, 1903.
"Untold loss of life, the complete annihilation of Clifton Mill No. 3 and Pacolet Mills Nos. 1 and 2, the injury done to thousands of bales of cotton and newly manufactured goods; 3,500 operatives suddenly thrown out of employment; the complete loss of grist and flour mills, livery stables, post offices, dwellings, stores, churches, and much livestock sum up the
-- L.N. Jesunofsky, Monthly Weather Report, June 1903.
Erected by South Carolina Department of Natural Resources.
Location. 34° 55.767′ N, 81° 46.85′ W. Marker is in Pacolet, South Carolina, in Spartanburg County. Marker is on Lucky Lane. Touch for map. Marker is located at the headway of the trail to the Pacolet River. Marker is in this post office area: Pacolet SC 29372, United States of America.
Other nearby markers. At least 10 other markers are within 6 miles of this marker, measured as the crow flies. Marysville School (approx. 1.6 miles away); Welcome to Glendale Shoals (approx. 3.4 miles away); Early Iron Works (approx. 3˝ miles away); Camp Croft (approx. 3.9 miles away); Clifton World War II Memorial (approx. 4.6 miles away); Clifton Baptist Church / First Baptist Church (approx. 4.6 miles away); Goucher Baptist Church (approx. 5 miles away); The Pacolet River Flood of 1903 (approx. 5.3 miles away); Battle of Cedar Spring (approx. 5.6 miles away); Welcome to Croft State Natural Area (approx. 5.7 miles away).
Also see . . .
1. Pacolet River Heritage Preserve. Located near the confluence of the Pacolet River and the Lawson's Fork, the 258 acre preserve protects two prehistoric soapstone outcrops that date back 3,000-5,000 years ago and provides habitat for uncommon plant species. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
2. Pacolet River Heritage Preserve Field Trip. Video of SC DNR Field Trip to Pacolet River. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
3. Slobot About Town XIV: Slobot goes to the Pacolet River Soapstone Quarry. The Pacolet River Heritage Preserve is a 257-acre property run by the Heritage Trust. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
4. Soapstone. Soapstone (also known as steatite or soaprock) is a metamorphic rock, a talc-schist. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
5. The Pacolet River Flood of 1903. On June 6, 1903, a great disaster struck the entire Pacolet River valley. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
6. Pacolet's Gone. Collection of news articles from 1903 and 2003 about the flood. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
7. Clifton and Pacolet, SC Cloudburst Causes Flooding, June 1903 - New York Times Article. Pacolet and Clifton, in this county, where are located some of the greatest manufacturing plants in the Southern States, have been swept away, at least thirty persons have been drowned, and tremendous damage has been done to manufacturing establishments as a result of a terrific cloudburst that broke over this section between midnight and dawn to-day. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
8. Gary Henderson and the 1903 Pacolet River Flood. Henderson, an area journalist, speak about the 1903 flood, the deadliest in South Carolina's history. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
9. Pacolet River. The Pacolet River is a tributary of the Broad River, about 50 miles (80 km) long, in northwestern South Carolina in the United States. (Submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.)
Categories. • Animals • Disasters • Native Americans • Waterways & Vessels •
Credits. This page was last revised on June 16, 2016. This page originally submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina. This page has been viewed 902 times since then and 47 times this year. Photos: 1, 2, 3, 4, 5, 6, 7, 8. submitted on May 5, 2012, by Brian Scott of Anderson, South Carolina.