Today, the mountain country around Salem, Tamassee, Whitewater, and the lakes of northern Oconee County draws people for waterfalls, hiking trails, mountain views, and quiet streams. On the night of June 5, 1903, those same mountains became the setting for one of the most destructive weather events in the region’s early history.

Days of rain had already saturated the ground when another tremendous downpour struck northwestern South Carolina. Mountain streams rose rapidly, bottomlands disappeared beneath muddy water, hillsides gave way, and bridges that connected rural communities were swept downstream. In Oconee County, the disaster would be remembered for generations as the Great June Freshet of 1903.

The catastrophe is better known today for what happened along the Pacolet River in Spartanburg County, where at least 65 people were killed, and entire mill communities were devastated. State climatologists confirm, however, that destructive flooding occurred along other streams throughout northwestern South Carolina.

The story preserved around Salem gives us a much more personal view of what that meant in the mountains.

Days of Rain Before the Flood

In Salem Twice a Town, local historian Joseph Gauzens preserved the memories of William Milas Alexander, a resident of the Little River community who was 94 years old when interviewed in 1986. The Little River community was centered about four miles northwest of Salem, and Alexander’s family owned approximately 300 acres there, including about 25 acres of bottomland along Little River.

Alexander remembered steady rain falling for two or three days before June 5. By then, the ground was thoroughly soaked. Around dark that evening, the rain intensified dramatically and continued through a night filled with thunder and lightning.

Alexander’s recollection of the storm was simple: he had never seen rain like it before or since.

Historical weather records support the event’s extraordinary nature. A later U.S. Geological Survey examination of the 1903 flood reported that rainfall northwest of Spartanburg was probably considerably greater than the five inches measured at Spartanburg. Based partly on washouts, landslides, and gullies left behind, investigators estimated that portions of the affected region may have received roughly seven to eleven inches during the 24 hours preceding the morning of June 6.

A Farm Nearly Washed Away

When daylight returned, Alexander’s family discovered that the flood had transformed their farm. In some places, the flood had stripped soil away nearly to bare rock. In others, sediment had been deposited so deeply that corn standing about 18 inches high had disappeared beneath it.

Rather than abandon the crop, the family dug through the newly deposited soil, located the buried corn stalks, and straightened them. Alexander remembered that they eventually saved about half the crop.

Trees had also been washed down, including sizable ones, while other trees and even cattle were carried away by the flood.

For families who depended on their land and livestock for survival, destruction on this scale represented much more than property damage. A field lost in June could mean losing much of the food or income that family expected from it for the entire year.

The Mysterious “Waterspouts”

One of the strangest details preserved in Salem Twice a Town involves what witnesses repeatedly described as “waterspouts.”

Alexander remembered seeing both large and small waterspouts moving across water and sometimes onto land. One reportedly struck a rise above the water and excavated a hole roughly 12 feet across and large enough to bury a wagon.

He was not the only person to describe them.

An account from Tamassee shortly after the disaster claimed that an observer had seen 130 waterspouts, with still more believed to have occurred beyond his view. One reportedly crossed the farm of Reuben Lee, sweeping away much of the crop, while other farms in the Cheohee Valley suffered extensive losses.

Exactly what these witnesses were observing is difficult to determine more than 120 years later. The term “waterspout” did not necessarily carry precisely the same meaning for rural residents in 1903 that it does in modern meteorology. The descriptions could refer to vortices, concentrated torrents of runoff, or another violent effect of the extraordinary storm.

Whatever the phenomenon was, the repeated references show how unusual the night appeared even to people accustomed to severe mountain weather.

When Smeltzer Mountain Began to Move

The water was not confined to rivers and creeks. The saturated mountains themselves began to fail.

Near Smeltzer Creek, J. H. Wigington and his family reportedly watched approximately two acres of land and trees slide down Smeltzer Mountain toward their home. The account provides a striking local example of the landslides and slope failures that accompanied the enormous rainfall.

The destruction continued throughout the surrounding communities. At Flat Shoals, S. A. Towe described water covering the floor while rain poured down the chimney. At Tamassee, floodwater entered J. E. Kelley’s store and ruined merchandise sitting on shelves and counters, causing losses reportedly totaling several hundred dollars.

In Salem, Martha “Mattie” Pike spent the frightening night walking the floor with her one-year-old daughter Pearl while the storm continued outside.

By daylight on June 6, isolated stories such as these were becoming part of a countywide disaster.

Tragedy at High Falls

The most heartbreaking Oconee County story preserved in Gauzens’s account occurred near High Falls.

As floodwater threatened his two-story house, Felix Jenkins attempted to save his family. He managed to get his wife and three children onto the roof, apparently hoping the upper part of the house would remain above the rising water.

It did not.

The building was swept away.

Jenkins survived after becoming lodged in a tree, although he suffered a broken arm. His wife and all three children drowned. According to the account in Salem Twice a Town, those four members of the Jenkins family were the four lives lost in Oconee County during the flood.

Their story shows how quickly the situation became impossible to escape. A substantial two-story house that initially offered a refuge from rising water was eventually lifted and carried away by the flood itself.

Forty-Six Bridges Swept Away

The destruction of Oconee County’s transportation system was staggering.

According to figures compiled in Salem Twice a Town, 46 bridges were swept away throughout Oconee County, including 17 in the Salem area. Another four bridges in the area were damaged.

The losses were spread throughout the mountain watersheds. Little River reportedly lost five bridges and had another damaged. Two bridges were lost on the Keowee River and three damaged. Oconee Creek lost three bridges, Whitewater River lost two, and Cheohee Creek lost five.

A contemporary description quoted by Gauzens reported that scarcely a bridge of importance north or east of Walhalla had escaped being washed away. Roads were badly eroded as well, leaving the county facing not only the loss of bridges but miles of damaged approaches and roadbeds.

The estimated cost of rebuilding bridges and repairing roads was between $10,000 and $15,000, a tremendous financial burden for rural Oconee County in 1903.

These bridges were more than conveniences. Before automobiles became commonplace, they connected farms to stores, post offices, churches, mills, doctors, and neighboring communities. Losing dozens of crossings meant that the flood continued disrupting everyday life long after the rain stopped.

The Disaster Was Bigger Than Oconee County

While residents around Salem were beginning to comprehend their losses, an even deadlier catastrophe was unfolding farther east along the Pacolet River.

Modern South Carolina climate records show that several days of rain preceded the flood. On June 5, a combination of atmospheric conditions and moist air moving upslope produced the extreme rainfall that sent the Pacolet River out of control in the early morning of June 6.

Contemporary newspaper reports described mills, houses, bridges, warehouses, and railroad infrastructure being carried away. A June 7 report published by The New York Times, drawing on dispatches from Spartanburg, described communities overwhelmed by the torrent and thousands of textile workers suddenly without employment.

The South Carolina State Climatology Office now identifies the event as the state’s most significant documented loss of life from river flooding. The state attributes 65 deaths to the Pacolet flooding, although historical sources have produced somewhat different totals. Economic damage was estimated at about $5 million in 1903 dollars.

At least 75 homes were reportedly destroyed along the Pacolet, along with four textile mills, while two other mills suffered severe damage. More than 4,000 mill employees were left without paychecks for an extended period.

Yet the Pacolet disaster was only the deadliest part of a much broader event. Flooding affected streams throughout northwestern South Carolina, which is where the accounts from Salem, Little River, Tamassee, Cheohee, and Whitewater fit into the larger story.

Why Was the Flood So Destructive?

The mountain landscape of 1903 was different from the one we know today.

In his later recollections preserved by Gauzens, Alexander believed two conditions made early floods particularly destructive. He remembered normal streamflow being greater than it was later in his life, and he pointed to the widespread practice of burning forest undergrowth. In his view, the lack of accumulated vegetation and forest-floor material allowed rainwater to rush more quickly down steep slopes and into already swollen streams.

That explanation should be understood as the recollection of people who lived in the area rather than a modern scientific determination of exactly why the 1903 flood behaved as it did.

What is more firmly established is that the ground was already saturated before the most intense rainfall arrived. Modern historical analyses also document extensive washouts, landslides, and gullies throughout the affected region, evidence of enormous quantities of water moving rapidly across the landscape.

The landscape has changed considerably since then. Modern forest practices differ, and reservoirs now occupy portions of the old river valleys. Lake Keowee and Lake Jocassee did not exist in 1903. The Keowee and its tributaries flowed through a mountain landscape that changed dramatically during the twentieth century.

The Flood Changed How Oconee County Built Bridges

The Great June Freshet also occurred when Oconee County struggled to improve its roads and bridges.

Wooden bridges were vulnerable to repeated flooding, and the 1903 destruction showed the enormous cost of rebuilding them. Within several years, the county increasingly turned to iron construction.

By 1907, an iron bridge had been built across Little River at Burnt Tanyard. Oconee and Pickens counties also cooperated on an iron bridge across the Keowee River at Nimmons Bridge, with Oconee County’s portion reportedly costing $3,700.

The transition did not eliminate the dangers of mountain flooding, but it marked an important shift in how local officials tried to keep communities connected when rivers rose.

A Landscape of Communities That Has Partly Disappeared

Understanding the Great June Freshet also requires understanding what “Salem” meant in the early twentieth century.

Salem itself was small, but it sat among a network of rural communities, including Burnt Tanyard, Cheohee, Danville, Fall Creek, Flat Shoals, Jocassee, Little River, Smeltzer, Stamp Creek, Talley, Tamassee, and Whitewater.

Some of those names remain familiar today. Others have largely disappeared from everyday use, and portions of the landscape associated with them were later changed by reservoirs and other development.

That is one reason Gauzens’s Salem Twice a Town is so valuable to the story. The book preserves not merely statistics about a flood but names of people, farms, stores, creeks, and communities affected by it. The title page of the copy used for this article identifies Joseph Gauzens as the author, with drawings by Gail McKinley.

Why They Remembered It as the Great June Freshet

“Freshet” is an old word for the sudden rise or flooding of a river or stream, usually following heavy rain or melting snow. For the people living around Salem, however, what happened in June 1903 was not remembered as merely another freshet.

It became the Great June Freshet.

William Milas Alexander recalled that people talked about the event for years afterward. Later floods in the old Salem area were measured against the 1903 flood, as though the community had established its own high-water mark in memory.

That may tell us more about the disaster’s severity than any individual statistic. These were mountain residents accustomed to swollen streams, difficult roads, violent thunderstorms, damaged bridges, and heavy rain. Flooding was not an unfamiliar phenomenon.

What happened during the night of June 5 and the morning of June 6 was different.

Fields disappeared. Mountainsides moved. Houses and livestock were swept downstream. Dozens of bridges vanished, and four members of one Oconee County family lost their lives.

More than 80 years later, Alexander still remembered that night and the rain that accompanied it.

For the people who experienced it, there was no need to explain which flood they meant.

It was simply the Great June Freshet.

Sources and further reading

The primary local source for this article is Joseph Gauzens’s Salem Twice a Town, which preserves contemporary reports and later eyewitness recollections concerning Salem and surrounding Oconee County communities. Contemporary and government records were used to place those local accounts within the larger June 1903 flood.

The Keowee Courier is especially important for continued research because surviving newspaper holdings extend through the period of the disaster. Additional sources include historical U.S. Geological Survey flood research, South Carolina State Climatology Office records, and contemporary newspaper reporting on the June 1903 flooding.