The Flood Waters of
Lawson's Fork Creek
Story furnished by
Clarence Crocker
The little friendly
stream known as Lawson’s
Fork Creek gets it’s beginning from branches and
smaller creeks in the foothills of South Carolina near
the town of Campobello. Winding some 29 miles through
Spartanburg County, it empties into the waters of the
large Pacolet River a short distance above Pacolet
Mills. For hundreds of years it has been a major source
of energy to all the industries and villages which lie
adjacent to its banks.
It has also played an
important role in the nation’s wars. History tells us
that it furnished energy to the Wofford Fort/Iron works
located on it’s banks near the place which was later to
be called Bivingsville.
They made implements of war for the southern soldiers in
the Revolutionary War and
to the Buffington Iron works located on the lower
shoals. ( J. S. Brooks, The
Iron Works on Lawson’s Fork and The Iron Works). After the
construction of Bivingsville Mfg. Company, Lawson’s Fork
creek supplied energy for the company to supply
clothing, knives, shoes and other material for the
southern soldiers fighting in the 1861 Civil War.
The quite lazy flowing
waters which one might observe today while standing on
it’s banks enjoying the beautiful wild flowers, has not
always been the case. Torrential rains with mighty winds
have from time to time turned this friendly little
stream of energy, wonder and beauty into a mighty force
of anger, death and destruction. Though this has no
doubt happened numerous times over the centuries, this
writing is limited to the storms of the early to mid
nineteen hundreds as told to me by my dad who lived and
worked at Glendale Mills during those days, Spartanburg
newspaper copies found in the Spartanburg Library
microfilm department and my personal knowledge of some
few events.
June 5 1903
A moderate rain had
been falling off and on since the first of June when
almost suddenly and unexpected, a mighty downpour of
rain began about midnight Friday June 5th. lasting for
some three hours. A total of some 11 inches of rain had
fallen in the area causing the normal 50 foot sleepy
Lawson’s Fork creek to rise out of it’s bed, expanding
to some 200 feet of raging waters, swallowing up much of
that which was in it’s path.
On Saturday June 6th,
the Spartanburg
Herald’s morning edition told how the waters
had washed away trestles, bridges, cotton mills,
warehouses, cotton and cotton goods. It stated that
there was no wind, only the force of waters from the
deluge of rain. A Southern Railway railroad trestle
crossing Lawson’s Fork about a mile north of Spartanburg
had been washed away leaving only the steel pilasters
protruding from the waters. Since the trestle was some
60 feet above the normal flow of the creek, it was
speculated that houses and other buildings being carried
down stream by the raging water, destroyed the
trestle.
The dam on Lawson’s
Fork at Whitney Mills was reported to have broken,
carrying away the old bridge and several low lying
factory houses. The new bridge which had recently been
built, suffered considerable damage. White’s Grist Mill,
located on the banks of Lawson’s fork just outside the
village of Drayton was severely damaged. The bridge on
east main street (S29) at the edge of the city of
Spartanburg and the railway trestle just a short
distance above the bridge, (Heywood St.) had also been
washed away.
Glendale had just
finished the new mill (plant #3) the year before leaving
the surrounding grounds fairly clean and though no water
of any consequence got into the Glendale Mill Plants to
do serious damage, the mill pond dam burst and foot
bridges behind the mill were washed away. (the old rock
dam was replaced by the concrete dam which stands today)
The old mill building which was located at the lower end
of the plant structures which had been converted into a
grist mill, was also washed away. It was determined that
the bursting of the dam had spared the mill plant from
serious damage. The village, some distance above the
creek and being quite hilly, suffered no serious damage.
The trolley car trestle
crossing Lawson’s Fork at the old Glendale Park area was
washed away along with considerable amounts of track and
track roadway.
Our sister mills and
villages were not so fortunate. Located on the Pacolet
river into which Lawson’s Fork empties just below
Glendale, the three Clifton Mills which were a division
of D.E. Converse Co. with headquarters at Glendale,
suffered the loss of life and property. The dam at Plant
#3 (Converse) was first to go down in the flood waters,
then the plant, then the Converse bridge along with a
row of low lying houses and a few lives. Clifton Mill
plants #1 & #2 suffered serious damage along with
the loss of the store building, warehouse and some 700
bales of cotton, 300 bales of cloth. A large number of
lives and houses were lost at both places. The trolley
car tracks were washed out between Clifton #2 and
Converse. A total of 55 lives and 50 to 60 houses were
estimated to have been lost in the flood waters. Three
to four million dollars was considered a conservative
estimate of the loss of the three mills.
Our neighbors to the
south seemed to have borne the blunt of the storm. ( See The
Great Pacolet Flood. ) With the waters of Lawson’s
Fork joining the forces of the mighty Pacolet River just
above the town of Pacolet, it was estimated that Pacolet
had suffered the greatest financial loss of all. Two
mills at Pacolet were reported to have gone down
completely with the third having been greatly damaged.
Some 2000 bales of cotton and 4000 bales of cloth were
lost in the waters. Of course, the loss of lives was the
greatest cost of all. Within a space of 1 to 2 hours, an
estimated loss of 1 million dollars had occurred. On
Saturday evening, June 6th., at 1:30, a call came into
the Spartanburg
Journal reporting that Pacolet Mill # 3 had
gone down. This proved to be inaccurate as it was
determined by the management that the plant suffered
only about 25 per cent damage and could be put back into
production in a few months, providing employment for
about half of the Pacolet Mills settlement but an upward
estimate of 2 million dollar loss had occurred.
On Tuesday June 9th.
the Spartanburg
Herald reported that the mail delay caused by
the flood had almost come to the point where it was “a
calamity” and a great deal of complaints were being
expressed. It stated, “although people have been coming
into the city via Lawson’s Fork Ferry since Sunday, no
mails have come in”. The postal department said the
mails had been held up by trestle/track wash-outs and
wrecks. It also reported that a temporary trestle built
out of wood over Lawson’s Fork north of the city had
been constructed in remarkable time and the first train
entering the city was expected to arrive the next day at
about 10:08 AM.
The Spartanburg
Electric Railway Co., operators of the trolley car system, issued a
statement on Tuesday the 9th. of June stating that they
had suffered some twenty to twenty five thousand dollar
loss due to the flood. Three trestles and about a mile
of track had been swept away. The report stated that the
company was busy that day restoring the trestle which
crossed Lawson’s Fork at the Glendale park and that the
run to Clifton #2 was expected to be restored on
Thursday or Friday of that week. The cost of the trestle
was expected to be about $2500.00. The repair of the
tracks and restoration of service beyond Clifton #2
would depend on the mill owners decision regarding
restoration of the mills. The company President, Mr.
McEowen, said that with the loss in traffic revenue and
the damage caused by the flood, the companies total loss
would reach $30,000.
August
25, 1908
In a story published
in the Spartanburg
Herald on Wednesday morning, August 26th, the
writer stated that the continuous downpour of rains for
the last several days had done great damage throughout
the county, in fact, throughout the Piedmont. He
reported that bridges and trestles across streams had
been washed away and travel on some county roads was
impossible. With the waters in the streams` still rising
some were expressing fear that the flood might reach the
1903 magnitude. From 1 AM Sunday morning until 7 PM
Wednesday evening, 10.4 inches of rain had been
recorded, the largest rainfall ever recorded in the
Spartanburg area in an equal number of days.
The waters of Lawson’s
Fork and other steams were reported to be rising
rapidly. By 3 P.M. Tuesday afternoon reports of county
bridges being washed away had come into the news office.
Tuck’s bridge, a practically new steel bridge over
Lawson’s Fork along with the old wooden bridge at
Whitney over Lawson’s Fork were also washed away and the
large new steel bridge was badly damaged. No dams were
reported broken and no mills were reported to have been
water damaged. Pacolet River into which Lawson’s Fork
empties had washed the bridge away in Pacolet Mills S.
C.
Many went down to Rock
Cliff park on Lawson’s Fork creek (Heywood St) to
observe the stream. Though it was a wild and turbulent
sight with large timbers, tubs, barrels, pumpkins, water
melons and various other objects being carried swiftly
down stream, those who observed the flooding of Lawson’s
Fork in 1903 said that it did not rise to that
level.
A news article from
Glendale on August 26th, stated that water was very high
until a late hour on the night before and due to water
backing up in the wheel house rendering the waterwheel
powerless, the mill was forced to shut down about 4:30
PM on Tuesday the 25th. With the raging stream breaking
over the rock wall at the bridge on the opposite side
from the mill, water flooded the M. W. Walker grocery
store and did considerable damage to the roadway. The
water did no damage to the mill plant but several good
foot bridges behind the mill were washed away.
In final analysis, it
was estimated that the greater damage would be to the
county in the loss of bridges, bridge damage, roads and
to county lands. Railroad companies had perhaps suffered
the greatest financial lost of all by trestles, tracks
and roadways having been washed away and the loss of
revenue. No mills or dams in the county were reported to
have suffered serious damage and no loss of life had
been reported. The flood of 1908 was labeled by some as
the most extensive flood in South Carolina in that it
effected the larger part of the state with considerable
damage being done in low state.
August 27, 1928
“Many county bridges
are swept away” was the caption appearing in the Spartanburg Herald
on August 28th relating to the floodwaters which had
swept through the county on the day before. It stated
that a large portion of the bridges in the county had
been washed away with a larger number being damaged. On
the large steams hardly a bridge was still standing,
isolating some areas.
Among the list of
bridges destroyed was the bridge on Lawson’s Fork at
White’s Mill, located between Drayton and the
Spartanburg city limits. The journalist suggested that
the county would be compelled to go into the bridge
building business which would take at best, several
months to complete. It was reported that the steel
bridge at Pacolet #2 went down carrying with it the
large part of the dam’s woodwork (aprons) and a few
stones from the middle of the dam. I have not found any
records where Glendale suffered damage of any
sort.
It was estimated that
farmers in the county had perhaps suffered the greatest
loss. Crops in bottom lands were completely covered by
water and in many instances, dirt and sand. Crops on
high land and hillsides didn’t fair much better. Gullies
washed out throughout the fields doing serious damage to
the land, cotton and other crops, destroying some
completely.
January
4, 1936
On Sunday, January
5th., The Spartanburg
Herald reported that the rivers, creeks and
other smaller streams in the county had risen to their
highest levels in several years. Torrential rains which
had fallen over the county beginning Thursday January
2nd. along with melting snow were the culprits.
Thousands of acres of land had been flooded.
U.S. river gauges in
operation on the Tyger river showed that the river had
risen 5 feet by midnight June 4th. North and South
Pacolet rivers were reported as being above their banks.
The Spartanburg Waterworks plant on South Pacolet river
reported a rise of 23 inches above the splashboards
which was the greatest since 1931. Fairforest Creek on
the west side of Spartanburg and Lawson’s Fork on the
east side were both reported as having risen
considerably.
Many roads in the
county had become so flooded and so muddy that they were
almost impassable. Some schools postponed classes on
Monday due to the dangerous conditions of the roads.
Highways and city streets were reported to be free of
snow for the first time in over a week. The Spartanburg
Weather Bureau reported that the snow that had fallen
the week before was the heaviest snowfall since December
17, 1930. Except for flooded lowlands and muddy roads,
little other damage was reported. None was reported from
Glendale.
October 16, 1936
“Traffic was slowed
with some being completely stopped due to poor
visibility” was the sub topic headlines of the Spartanburg Herald
on Saturday, October 17th. Beginning on Thursday and for
36 hours, heavy rain. likened to cloudburst proportions,
fell in the Spartanburg and surrounding area beginning
about noon on October 15th. and ending at about midnight
on the 16th.
The U.S. Weather
station at Spartanburg Airport reported that 4.96 inches
of rain had fallen. Three inches had fallen within the
last 12 hour period resulting in flash flooding on
steams throughout the county. Perhaps more had fallen in
the foothills and outlying areas as streams in the area
were swollen out of their banks and raging with fury.
The Spartanburg Waterworks plant on South Pacolet
reported that the water was some 3 feet above normal.
Hearing of the flash
flooding at the Glendale bridge, three of my brothers
and I went down in the car on the morning of the 17th.
to observe the sight. The first thing we saw was that
the large flat marsh land area behind the mill store,
extending out to the curve at the bottom of Sixteen street (now Highland)
and back to the woods was covered with water, making the
mill pond about twice it‘s normal size. Water was over
the floor of the out door toilet and over a grease rack
on the wall behind the Mill Store.
At that time the area was not filled with trees as it is
today. It was a large marsh filled with cat tails
growing about waist high.
The pond water had
risen over the flood gate wheels and sloshing against
the bottom of the iron bridge with waves splashing over
the flooring of the bridge at times and was running
across the road at the opposite end of the bridge from
the mill. Little if any of the aprons on the dam had
given way at that time. Water was flowing all around the
back of the mill plant. The shoals were raging. The
floor of the little Mud Bridge
located on the Glendale/Ben Avon road about a quarter
mile from the mill, was covered with water up about 4 to
6 inches or more on the side rails. The whole valley in
which the bridge sit looked like a huge lake.
Some of the old timers
believed that the water was higher than the 1903 flood.
Perhaps it was. The new concrete dam had been built
further upstream on the shoals and was much higher than
the previous rock dam which burst in 1903. Wood aprons
which raised the pond water level some three feet had
also been added to the top of the new dam and had not
broken at that point but did break later in the day.
Incidentally, the aprons were constructed to break in
extremely high waters.
In spite of the high
waters and except for road damage, no serious damage was
reported from any of the local mills. Our sister mills
at Clifton and Converse which are on the Pacolet River
reported that they had to stand for a few hours due to
water in the wheel house. Glendale did not report any
problems but knowing the location of their water wheel,
I rather suspect that they too had wheel problems for a
short while. The waters abated quickly.
August
28, 1949
On Monday August 29th.
the Spartanburg
Herald & Journal reported that 3.44 inches
of rain had fallen in the Spartanburg area from Saturday
afternoon to about mid afternoon Sunday. A hurricane
sweeping north from the Gulf States was the culprit. The
rain was accompanied by high winds ranging from 40 miles
per hour to gusts up to 70 miles per hour. Some small
streams went out of their banks causing evacuations in
low lying areas. Little damage, limited primarily to
uprooted and broken trees was reported.
Lawson’s Fork
creek at Glendale raged but damage was limited to the
roadway behind the mill, the new sewage treatment system
which was being built and the new fencing which had been
erected around the mill was badly damaged. This writer
was with Glendale Mills at the time and made a few
pictures (see below) of the local floodwaters. A
close look at the water coming over the dam will show
the apron was beginning to break in one or two
spots.
The Creek is
Cleaned Up
Lawson’s Fork creek,
like most other streams of early days, was for many
years the catch basin for raw sewage from factories,
houses and mill villages along it’s banks and even from
parts of the city of Spartanburg. According to the
Spartanburg Water Utilities History web site, the
Spartanburg Metropolitan Sewer District, (now
Spartanburg Sanitary Sewer District) was set up in 1929
to help eliminate this dangerous health problem. In 1931
the Fairforest and Lawson’s Fork Treatment plants began
operations. The Lawson’s Fork plant had a capacity of
1.5 million gallons per day with waste water being
emptied into Lawson’s Fork Creek.
In the late 1940s and
early 50s, the state began to pass regulations and laws
which forbid raw sewage disposal into public water
streams which most factories and small villages had been
doing for years. Glendale village residents used outdoor
toilets until 1917 when septic tanks and indoor toilets
were installed. This writer, on behalf of Glendale Mills
appeared with our county delegation in Columbia in
support of the bill. We had already started installing
lines throughout the village to collect sewage for
treatment in the new digester tank and sludge drying
beds which were being built. All mill sewage which had
from it’s beginning been dumped into the river, was
collected and treated through the new sewage
system.
Spartanburg Sewer
System, having already taken over the sewage disposal of
more factories and villages, including Glendale’s in the
1950s, the Lawson’s Fork plant was expanded in 1955 to
meet the growing need and again in 1960 with the average
flow being 2.7 million gallons per day. It was expanded
again in 1974-77. In 1988 it was expanded to a capacity
of 6 million gallons per day. In 2006 with the
Fairforest plant having been expanded to the capacity of
25 million gallons per day, emptying of waste water from
the Lawson’s Fork plant into Lawson’s Fork creek was
eliminated. All waste water is now diverted from the
Lawson’s Fork plant to the Fairforest plant located on
Southport Road in Spartanburg for final treatment and
disposal. To this writers knowledge, no raw sewage has
been emptied into Lawson’s Fork creek for many years and
is being developed as a stream for kayaking, rafting,
etc along with walking trails. New life for an old
friend!
Researched,
compiled and written by Clarence E. Crocker, March 2011
This web site has been started as a
public service to share the story of Glendale. See more
information about Mary and her Glendale connection at Mary McKinney Teaster.