The Greatest Storms of the
Century
in the Greater Washington-Baltimore Region
This is an attempt to compile a list of the worst storms
of the 20th Century by the type or category of weather that impacted the
Greater Washington and Baltimore Metropolitan Area. For large scale events
that effected most of the region, a single event was chosen. The
categories are listed alphabetically by topic.
1) Coastal Storm
(Nor'easter) - The Storm of 1962
The strongest nor'easter of this
century struck the Mid Atlantic Region on March 5-9, 1962. It is known as
the "Ash Wednesday Storm". It caused over $200 million
(1962 dollars) in property damage and major coastal erosion from North
Carolina to Long Island, NY. In New Jersey alone, it was estimated to have
destroyed or greatly damaged 45,000 homes. The Red Cross recorded that the
storm killed 40 people. It hit during "Spring Tide." When the
sun and moon are in phase, they produce a higher than normal astronomical
tide. Water reached nine feet at Norfolk (flooding begins around five
feet). Houses were toppled into the ocean and boardwalks were broken and
twisted. The islands of Chincoteague and Assateague were completely
underwater. Ocean City, Maryland sustained major damage especially to the
south end of the island. Winds up to 70 mph built 40-foot waves at sea.
Heavy snow fell in the Appalachian Mountains. Big Meadows, southeast of
Luray, recorded Virginia's greatest 24-hour snowfall with 33 inches and
the greatest single storm snowfall with 42 inches. Nearly two feet of snow
fell from Charlottesville (21 inches) to Luray (24 inches) to Winchester
(22 inches). Roads were blocked and electrical service was out for several
days. Washington and Baltimore fell into the mixed precipitation zone.
Virginia
Beach, March 1962
Picture from: Hurricane Survey,
Norfolk Virginia: U.S. Army Corps of Engineers, Norfolk, VA, October,
1959.
2) Cold Wave - The Great
Cold Wave of January 1912
A record cold wave settled in over the region. Records set in Maryland
during this period remain to the present day. It was close, but not quite
cold enough to break the records in Virginia set during the February 1899
"Great Arctic Outbreak". The cold wave of 1912 hit on
January 5 and continued until February 16. It was one of the most severe
and longest in duration on record. Ice formed on the rivers
and the Chesapeake Bay. On January 13, Oakland in far western
Maryland recorded the state's all time record low temperature of -40°F.
In Washington, DC, it reached -8°F. On the 14th, College Park
reported -26°F, Hagerstown -27°F, Frederick -21°F, Laurel -19°F,
Baltimore -2°F and Washington, DC -13°F. The coldest temperatures
in Virginia were -25° at Lincoln (Loudoun County) and Dale Enterprises
near Harrisonburg. Fredericksburg was -11°F and Culpeper fell to
-20°F. In the Eastern West Virginia Panhandle, temperatures ranged
from -14° at Lost City in Hardy County to -30° at Bayard in Grant
County.
3) Drought : The Great
Drought of 1930-1931
The year of 1930 was the driest
year since the drought of 1869 to 1870. The drought caused $40
million dollars (1930 dollars) in losses to farmers in Maryland
alone. Forest fires caused by the dry spell caused $580,000 in
losses in Maryland. The precipitation deficient began in December 1929 and
was fully classified as a drought by May of 1930. An extreme dry
period set in from the end of June 1930 and continued through February
1931. During the 15 month period from December 1929 through February 1931,
most places saw 60 percent or less of their normal rainfall. The
average precipitation across Maryland and Delaware was 29.58 inches which
was 21.51 inches below normal. Baltimore recorded 27.31 inches for
the 15 month period which was 23.03 inches below normal or 54% or normal.
Washington, DC recorded 26.78 inches which was 20.40 inches below normal
or 57% below normal. The drought of 1998 to 1999 did not come near
this severity, but it was the second severest drought of this
century. The Palmer index, which is used to signal drought severity,
classifies values of -3 to -4 as "severe drought" and values at
-4 or less as "extreme drought". The Palmer Index for the
region reached its lowest values during the end of the extreme dry period.
In Maryland, west of the bay, Northern Virginia and the eastern panhandle
of West Virginia, the Palmer Index was between -6.5 and -7.5 for January
and February. Areas experienced up to 17 months of extreme drought
conditions. The drought moderated some after February 1931 with periodic
rains and showers through the summer months that helped the crops.
However, these rains were not enough to restore the water table and water
flows levels. Officially the drought did not end until about May 1932.
4) Flash Flood - The
Madison County Flood of June 27, 1995
The Madison County Flood on
June 27, 1995 was the worst flash flood that Virginia had seen since the
remnants of Camille dropped up to 30 inches of rain one night in Nelson
County in August 1969. The Nelson County flood ranks as one of the
nation's worst flash floods of this century. The floods and landslides led
to the death of 117 people. Nelson
County/Camille Flood, August 1969
The Madison County event was chosen because it is closer to the
Baltimore-Washington region. The fact that only one person died versus
over 100 in Nelson County can be attributed to three significant factors.
1) It was well forecasted. Flash Flood Warnings did not even exist in
1969. The National Weather Service in Sterling contacted the State
Emergency Operations Center early that morning informing them that a
significant flood was likely. 2) Early response and heroic actions by
emergency responders made a big difference. Early warning by NWS to the
state allowed them to call in resources before the flooding began to
threaten lives. One Coast Guard helicopter came all the way from Elizabeth
City, NC. As conditions worsened through the day, the operators of
the helicopters risks there lives flying in low visibility into mountain
valleys to pluck people from roof-tops and carry them to safe shelter.
Some 80 people were rescued! In 1969, there was little preparation for
disasters and response to such situations took time to organize and gear
up. Time that can cost lives. State and local emergency management has
evolved greatly since 1969 and they are far more prepared to deal with
such disasters before they even start. 3) The Madison County flood
occurred in daylight when people could see rising water and attempt to
move to safety and emergency responders could see people on roof tops and
pluck them off. In Nelson County, people were asleep and awoke as their
houses floated off their foundations.
The weather that set up the flood included a semi-tropical air mass over
the region; an upper level low over the Mississippi Valley which sent
impulses/disturbances to the northeast across the area helping to trigger
thunderstorms; slow moving cold front sliding south along the front range
of the Appalachians and over the coastal plain which helped to focus where
the thunderstorms were occurring; and the high pressure to the north which
set up a westward flow of moist air from the oceans into the mountains.
The mountains helped to lift the air where it condensed into clouds and
rain. The focus for thunderstorm development on June 27 was the
intersection of the weak cold front which stalled across the area and the
upslope (east side) of the Blue Ridge mountains. A large thunderstorm
complex developed early that day over Rappahannock County and slowly moved
south over Madison County becoming nearly stationary over the southwest
corner where it dumped 20 or more inches of rain in a relatively short
period of time.
Other heavy thunderstorms also
occurred that day with additional flash flooding and some damaging
mud/landslides (debris flows) in Nelson and Albemarle Counties in Virginia
and the Keyser/Westernport area of Mineral County, West Virginia and
Allegany County, Maryland. These areas as well as Madison and Rappahannock
County saw rainfall rates of as much as 5 inch per hour which after a
couple hours is enough to cause land to give way. Areas susceptible to
these landslides are where the ground slopes at 30° or more from the
horizon.
Soil conditions were already
wet from earlier rains during the week. Therefore, rain that was absorbed
caused the ground to become unstable in some areas. Most of the rain
turned to runoff which created a rapid rise on small streams and creeks
and eventually into the smaller rivers. Soon water was out of its banks
flooding roads, homes, and businesses and cutting off communication
lines. While Doppler radar indicated that rainfall amounts suggested
that major flooding would occur, the first "ground truth" report
came from a Skywarn Amateur Radio observer. Skywarn is a volunteer network
of people who pass reports of severe weather onto the National Weather
Service. He reported that 10 inches of rain had fallen between 10 am and 2
pm in the town of Etlan in the north part of the county. During the
heaviest rain, radar was estimating 3.2 inches an hour for portions of the
county. This ground truth report told us that our radar was
underestimating rainfall by as much as one half . Indeed, conditions were
bad. Nearly all roads and every bridge in the county were damaged or
washed away. Half the farms sustained damage. The entire hay crop was lost
and half the corn crop. Hundreds of livestock were killed and 500 to 1000
miles of fencing was damaged or washed away. In Madison County alone,
total damages were estimated at $64 million with an additional $29 million
in agricultural losses. The estimated cost of recovery to get the farm
land suitable once more for crops may be as high as $1000 per acre. There
was only one death in the county which was due to a home collapsing on a
woman. An additional death occurred with flooding in Rappahannock
County and one in Warren County.
The rainfall and flood waters
from Madison and Orange Counties flowed into the Rapidan River. The
Rapidan gets its name from the fact that it responds quickly (water rises
rapidly) and it exceeded flood stage during the morning hours. The picture
below is where the Rapidan crosses the Route 29. This picture was taken
near its crest at that point around 2 pm in the afternoon. The USGS stream
gage near Ruckersville in Greene County was destroyed by the raging water.
The flood crest was estimated from high water marks to have reached 31.6
feet. This is a 500-year flood for that gauging point. This exceeded the
old record of 20.8 feet set at that point in October 1942 by almost a
foot. Downstream at the Culpeper gage, the river crested at 30.4 feet
which exceeded the previous record of 30.3 feet set back on October 16,
1942. This is equivalent to a 100-year flood at Culpeper.
The Rapidan River flows into
the Rappahannock River, which was also accumulating rains from northern
Madison County, Rappahannock and Culpeper Counties. On the 28th, the river
crested 5 feet above flood stage at Remington. Farther downstream on the
29th, the river crested in the city of Fredericksburg at 7 feet above
flood stage. The forecast point for the city is at the city dock which has
a staff gage. Substantial damage was reported at both locations, and at
numerous other along the river.
...Other Flash Flooding...
Other flash flooding caused
road closures from rock slides, mudslides, and bridge washouts, in
Allegany County Maryland and Mineral County, West Virginia. Once June 27,
near one million dollars in damage occurred to 200 buildings in Allegany
County near Westernport. Total damage estimates including roads was $1.76
million. In adjacent Mineral County, $1.1 million in damages were
estimated with 66 homes and 8 businesses damaged. Heavy rains in the
mountains caused mudslides and washed debris up against bridges. Temporary
debris dams backed up water then broke causing additional flooding
downstream. In Piedmont (Mineral County), over five and a half inches of
rain fell on the 27th with most
of it falling between 2 and 4 pm. Flooding occurred in both Piedmont and
Keyser. Up to 17 inches of rain also fell in Augusta County, Virginia.
Earthen dams in southeastern Augusta County were perilously close to
failure at one point, but survived as the rain areas shifted away.
The Rapidan River crossing Route 29 in Madison County
Photograph by Stephanie Gross;
Published in the Charlottesville Daily Progress, June 1996
Landslide in Madison County,
VA
Picture from U.S.G.S.
web site
5) Hail Storm - April 23,
1999
On Friday, April 23, 1999 a
horrific hail storm moved southeast from Pennsylvania across Garrett
County, MD and into the Eastern Panhandle of West Virginia. It had
weakened some as it crossed Garrett County and the Allegany Front, but as
it passed east of Keyser, WV, hail began to increase in size once again.
By the time it reached Capon Bridge in eastern Hampshire County, WV, the
size of the hail had grown from golf balls to baseballs. As it moved into
Frederick County, VA, the hail storm continued to grow dropping golf ball
size hail in a swath now reaching from the north of Winchester, south to
Stephen City (about 10 miles). The intensity of the hail stripped and
shredded leaves and bark from the newly budding trees. Hail stone grew to
the size of Grapefruit (4 inches in diameter) just east of Winchester. The
storm continued east through Clarke County, southern Loudoun and northern
Fauquier doing considerable damage to Middleburg, then across Fairfax
County hitting Centreville, Chantilly, Fairfax, Burke, Springfield, and
Lorton with golf ball to baseball size hail. It crossed the Potomac River
and weakened just slightly. It moved across northern Charles, clipped
southern Prince Georges and then into Calvert County with 1 inch to 1.5
inch diameter hail and onto the Chesapeake Bay continuing southeast to the
ocean. The damage left behind was incredible. In Northern Virginia
alone, it amounted to over $50 million dollars in losses to public and
private properties. Some communities saw a third of the homes with siding
and roof damage. Some required total replacement. Windows were broken,
cars dented and windshields smashed. Piles of shredded plant debris were
left on the ground in the storms path. In about 6 hours of time, this one
thunderstorm, moving at about 50 mph, did $75 million in damage. There
have been other bad hail storms to hit this area before, but none to have
caused this much damage to property.
NWS Doppler radar picture at
3:54 pm, April 23,1999.
Hail batters cars in Winchester.
Photo from Winchester Star.
6) Heat Wave - July and
August 1930
July 18 through August
10, 1930 was the longest and most intense heat wave of record.
Temperatures averaged 8 to 10 degrees above daily normals through the
period. During the 24 days that the heat wave latest, Frederick Maryland
saw 20 days over 100° with three days in July (21,22 &26) hitting
108° and one day in August (4) hitting 106°. The high temperature rose
above 90° on July 16 and did not fall below 90° until August 11. That
was a total of 26 consecutive days. In Woodstock, Virginia, 17
days were over 100° with a high of 109° on July 21 and 107° on August
4. Moorefield, WV set the state record high temperature with 112°
recorded on August 4. Even higher elevation sites topped 100°.
Frostburg (elev. 1929 ft.) was 101°; Emmitsburg (elev. 720 ft.) reached
104°; and Western Port (elev. 1000 ft.) reached 106°.
Washington, DC tied its all
time record high with 106° on July 20. Washington had 11 days with
temperatures over 100° during this period. Four of the days were
consecutive (July 19-22). This remains the record for DC. While
Baltimore officially only recorded a high of 104° (July 21 and August 4)
and a total of 7 days over 100°, it was reported that many people in the
city died from the heat and others were hospitalized. The entire area was
in severe drought. Little
precipitation fell through July and August (The two months total
precipitation was 6 inches below normal).
7) Hurricane - Hazel,
October 15, 1954
The first two weeks of October
were hot. La Plata was 96°F on the 4th. Washington and Baltimore were
92°F. Hurricane Hazel struck on the 15th. Cool weather would follow the
storm. At 12 a.m. on the 15th, Hazel was a Category 4 storm still 250
miles south of Wilmington, NC. Her shield of clouds already reached north
into Pennsylvania. Rain began over the area during the early morning hours
and continued into that evening. The hurricane struck the coastline south
of Wilmington around 10 a.m. It maintained hurricane force winds as
it rapidly progressed north passing west of Washington and near Hagerstown
between 5 and 6 p.m. that evening. It weaken to a tropical storm of
Pennsylvania.
Hazel produced record wind gusts at a number of locations. In Hampton,
winds gusted to 130 mph; Norfolk had 78 mph sustained hurricane force
winds with gusts to 100 mph. Washington National Airport in Arlington, VA
had sustain winds reach 78 mph (over hurricane force) with a gust of 98
mph; Baltimore had a sustained wind of 73 mph with a gust to 84 mph;
Salisbury recorded 52 mph with a gust to 101 mph and Philadelphia gusted
to 100 mph.
Heavy rains fell over western
Maryland dumping 5 to 6 inches in 12 hours over the Allegheny Front. Luke,
MD reported a record stage on the North Branch of the Potomac. Storage of
rainfall behind the new Savage River Dam was believed to have prevented
a record flood from occurring at Cumberland.
Tides reached 2 to 6 feet above
sea level around the Maryland portion of the Chesapeake Bay. In Baltimore,
high tides in the harbor flooded basements and streets adjacent to it.
Waves pounded the docks and shore line.
Virginia lost 13 people and
damages were very conservatively estimated at $15 million. About 18,000
homes and a considerable number of farms and business buildings were
damaged. Hundreds of thousands of trees were damaged or destroyed. Half of
the phone and electric lines in the Virginia were knocked out equaling
about $2 million in damages. Marine damage ran high. A 150 foot microwave
telephone tower was toppled near Warsaw. 200 plate glass store fronts in
Richmond were broken. In the Shenandoah Valley, Turkey Growers lost
between 150,000 and 250,000 turkeys when poultry sheds were wrecked. Small
crafts were driven ashore or sank. Four people died when a tug capsized on
the James River about 25 miles from Richmond. Piers were demolished and
private docks swept away in the Tidewater rivers. The Potomac rose
to 5.4 feet above MSL at Dahlgren, Va and Colonial Beach. Damage from
flooding begins between 3 and 5 feet. However, add on waves from
strong winds and considerable damage was reported along with much erosion
of the beach and banks. The Potomac at Alexandria rose to around 7.5 feet.
In Maryland, six people were
killed and an unknown number injured. Damages to homes and commercial
buildings was estimated at $8 to $10 million. Homes mainly suffered damage
from roofs being blown off, windows broken or trees falling on them. A few
homes floated off their foundations in the high tides. An estimated
$750,000 in damage occurred to boats on the Maryland Chesapeake Bay and
another $1 million to wharves and private docks. Utilities suffered
about $1.26 million in damages along. There was half a million dollars in
damages to bridges and roads in tidal areas. An estimated half a million
trees fell. There was $9 million dollars in damages to farms and another
$300,000 in damages to apple and tobacco crops. The total damage to the
poultry industry in Maryland was about $5 million. Erosion damage
caused by the spray of salt water to adjacent land areas and flooding of
low-lying areas in counties bordering the Bay and coast caused appreciable
damage to the soil, trees, and shrubs. Total salt damage and loss of land
by erosion were estimated at 1 to 1.5 million dollars. Total damages in
Maryland were about $28 million.
In the District of Columbia,
there were three fatalities. Damage occurred to houses, power facilities,
telephone services, and trees. The cost of debris removal amounted to
$595,000 (1954 dollars). The Public Housing Administration estimated
$300,000 in damage to World War II built public housing in Virginia,
Maryland and DC. Installations at Washington National Airport were also
damaged.
Hazel caused a total of 95
deaths in the U.S. and over a quarter of a billion dollars (1954 dollars)
in damages.
8) Ice Storm - February
1994
The Back to back ice
storms struck on February 8 to 9 and again February 10 to 11 leaving a
coat of ice, one to three inches thick, across much of the area. Areas
west of Frederick County, MD saw anywhere from five to nine inches of
sleet accumulate. Toward the end of the storm, this area saw light
freezing rain solidify the sleet on the ground and but a glaze across
trees and wires. There were scattered outages and at least 75 ice-related
injuries that were treated at area hospitals. Across central and northern
Maryland, Northern Virginia, the Shenandoah Valley, and the central
Piedmont of Virginia, about 4 to 7 inches of sleet fell. Again in this
area, light freezing rain toward the end of the storm which solidified the
ice and coated everything. It was enough to do about $5 million in damages
across this region.
The hardest hit area was
Southern Maryland, Annapolis, and the Eastern Shore and southwest across
Fredericksburg and the Northern Neck area and down toward Lynchburg and
Danville in Virginia. Here, the combination of the two storms left 3 to 5
inches of ice on surfaces. It was too much for trees and wires. Some
counties lost 10 percent of their trees. Fallen trees made roads
impassable. Some trees fell on cars and houses. Electric and phone lines
were down with as much as 90 percent of the area's people without power.
Even with help from out-of-state utility companies, many people were
without power for a week. A presidential disaster declaration was given
for the counties effected in a 40 to 50 mile wide band all the way from
Delaware southwest to Tennessee. Damages were estimated at near 100
million dollars for the Virginia-Maryland area. There were hundreds of
injuries from automobile accidents and people falling on ice. It was
likely the iciest winter the Baltimore-Washington area has ever seen.
9) River Flood - October
1942
Washington Post, March 20, 1936.
The three biggest flood events
of this century were the "Great Spring Flood" in March of 1936
(shown in top picture above), and two tropical related rain events,
October 1942 and Agnes in June of 1972 (discussed under the topic -
Tropical Storm). The October 1942 storm was chosen because it is the flood
of record for Washington, DC, Front Royal and Fredericksburg, VA. Still it
was a very tough choice because the March 1936 flood is the flood of
record at many points along the Potomac River including Cumberland,
Hancock, Williamsport, Shepardstown, Harpers Ferry, Point of Rocks and
Little Falls. The picture above was taken at the Virginia approach to
Chain Bridge where you can see the water breaking over the roadway. The
1942 flood reached a similar height. It is remarkable that these two
record floods would occur just 6 years apart.
A tropical storm moved in
across eastern North Carolina into central Virginia on October 12, 1942.
Torrential rains fell from October 12-16 in Northern Virginia and
Maryland. It caused the worst river flood in the history of the Virginia
and DC. The hardest hit was the mid portion of the Rappahannock River and
the Shenandoah River. On the Rappahannock, damages came to $2.5
million (1942 dollars) and most of that was in Fredericksburg, where the
river rose to 41 feet (27 feet above flood stage). On the Shenandoah
River, a stage of almost 50 feet was reached at Riverton on the morning of
the 16th.
Flood stage is 22 feet and it broke the record set by the March 1936 flood
by 12 feet! Flood losses on the Potomac River were $4.5 million. Water was
3.5 feet deep in downtown Cumberland and 8 feet deep on the main business
street in Hancock. At Williamsport, the river expanded 4 miles from its
normal banks. Two homes were swept away at Harpers Ferry were the
Potomac and Shenandoah Rivers meet. At Point of Rocks, more houses were
lifted off their foundations. The Potomac at Washington reached 17.6 feet
(flood stage is seven feet). Areas of Alexandria and Arlington were
seriously flooded. The Anacostia River flooded as well as 6 feet of water
was across the boulevard in Bladensburg.
Ten to 12 inches of rain fell
from Fredericksburg to Warrenton. Seventeen inches were recorded in Front
Royal. In Shenandoah National Park, along Skyline Drive, rainfall totals
reached 18 to 19 inches! To the south, Nelson County received 16 inches.
Another maxima of 12 to 16 inches fell from near Paw Paw, West Virginia
south along the Shenandoah Mountains to west of Harrisonburg. About 6 to 8
inches fell over much of central and western Maryland. Highways and
bridges were washed away across the region. Over 1,300 people were left
homeless in Albemarle, Spotsylvania, Stafford and Warren Counties in
Virginia. About 750 people were displaced from homes in Maryland. Hundreds
of homes were flooded in Georgetown. Miraculously, only one person died.
Transportation was interrupted for three days. Severe damage occurred to
crops: peanuts, cotton, sweet potatoes, soybeans, shocked corn and late
hay. The heavy rains caused a million bushels of apples to drop before
they were picked.
10) Snow Storm - January
1922, The "Knickerbocker Storm"
Exactly 150 years after the
"Washington and Jefferson Storm" which dropped 3 feet of snow on
the region, came the deepest snow of this century to the greater
Washington and Baltimore region. The snow came on the heels of a cold
spell. High temperatures did not climb above freezing from the 24 through
the 28th and the low temperature dipped to 11°F on the 26th. Snow began
at 4:30 p.m. on the 27th and continued until just past midnight on the
morning of the 29th. A record 21 inches fell in a 24 hour period on the
28th. The heavy band of snow stretched across Richmond (19 inches),
Washington, DC (28 inches), and Baltimore (25 inches) immobilizing the
region. Strong north to northeast winds accompanied the storm drifting
snow into deep banks. Roads were blocked. Main highways were the first to
open in 2 to 4 days.
On the evening of
the 28th, the weight of the snow became too much for the Knickerbocker
Theater on 18th Street and
Columbia in Northwest Washington, DC. The horrible scene was described in
the Washington Post on January 29th and
30th and was reprinted in the Post on January 19, 1996 following another
big snow. They described it as "the greatest
disaster in Washington's History". The theater was cramped with an
estimated 900 movie goers. The roof of the theater
collapsed taking the balcony down with it and crushing 98 people below to
death and injuring another 158. People were
pulled from the rubble for hours and bodies were pulled out for days. A
small boy squeezed into small holes and between
crumbled cement slabs to give those injured and trapped pain pills. From
this disaster, the storm is known historically as the
"Knickerbocker Storm".
11) Tornado:
Most Deadly: The La Plata Killer Tornado, November
9, 1926 at 2:30 pm
A tornado (estimated to be F4
with winds up to 250 mph) touched down about 5 miles southwest of La
Plata at about 2:30 pm. It moved northeast through La Plata and
continued on the ground traveling 18 miles in 20 to 25 minutes to
Cedarville in Prince Georges County. Its damage path was about 500 feet
in width. Little thunder occurred with the storm. Torrential rain
occurred at the time of the tornado's passage. Some hail fell. The
tornado's roar was heard up to 3 miles away. Debris from the tornado was
blown inward and forward (a classic tornado pattern). From this
description in Monthly Weather Review for November 1926, the
"vortex swayed from side to side as it progressed", it was
likely a multi-vortex tornado. Large tornadoes often break down into
smaller vortices which rotate around the wall of the larger cyclone. At
some places, the tornado "furrowed into the soil".
In La Plata, four homes,
several large barns and the school house were completely demolished -
lifted from their foundations and shattered. The schoolhouse, with its
60 children and two teachers was lifted from its foundation and smashed
against a grove of trees 50 feet away. Debris from the school,
children's belongings, and school furnishings were scattered in all
directions. Some of the children were carried 500 feet and the body of
one child was found in the top branches of a tree 300 feet away. Parts
of desks were found 7 miles away. Some of the wreckage of the
schoolhouse was found deposited in a field a mile north of Upper
Marlboro, 25 miles away. A page from a school ledger was found in Bowie,
36 miles to the north-northeast. About 6.5 miles from Annapolis, almost
50 miles from La Plata, a 8 foot by 2 foot piece of galvanized roofing
from the school fell. Of the school, 14 children were killed. The two
teachers and all the other children but one were injured.
Miss Ethel Graves, a school teacher at the La Plata School describes
what happened:
"It was just a few
minutes before 3 o'clock that I heard a rumbling roar and the wind
seemed to increase tremendously. I was just getting ready to take the
children to some safer place when the glass from all of the windows
blew out. The children had started toward me then and were beginning
to group themselves about me when it seemed as if they and everything
in the room about me had been pulled up be some unseen hooks. Then we
were flying through the air. It seemed to me as if some of the
children and parts of the building passed me several times. I lost
consciousness then."
An additional four homes were
badly damaged and 14 tobacco barns and their contents of 4,000 to 7,000
pounds of tobacco were a total loss. At Cedarville, one home, one store,
and 4 barns were destroyed. Several other homes were badly damaged. Six
families were rendered homeless. A mother and her three children were
injured when her home collapsed. The clerk of the general store was
sucked out the front door, across the road, and slammed against a
telephone pole were the wind tore his trousers off of him. On a farm, a
barn in which a horse and cow were feeding was picked up and carried
away, leaving the animals in their places uninjured. Chicken were
defeathered. In the destruction of homes, 9 people were injured and 3
more were killed.
Barns, sheds, outbuildings,
fences, garages, a gas station, trees, and telephone poles in the path
of the tornado were all leveled. A number of automobiles were
demolished. Damages were estimated at $100,000 (1926 dollars). A total
of 17 people were known to have died with 60 reported injured.
The weather Pattern:
An intense low pressure area was moving rapidly northeast from central
Indiana to extreme southern Ontario. A trough extended south from the
low center over the region. Winds ahead of the trough were south to
southwest at the surface and southwest aloft to 2000 meters. At about
5000 feet, the winds were from the southwest at 48 kts (56 mph). The
trough passed Washington, DC later that night at 10 pm. About the same
time as the tornado struck La Plata, a thunderstorm dropped 0.65 inches
of rain in DC in just 9 minutes.
Most Recent Violent Tornado: Frostburg,
Maryland on June 2, 1998 at 9:45 pm
This was part of a killer outbreak of tornadoes that moved southeast
from Pennsylvania. The tornado entered Garrett County, Maryland striking
the town of Finzel. It then moved up and over Big Savage Mountain in
Allegany County ripped through the northern portion of Frostburg.
It reached its peak strength as it crossed the ridge where the home seen
on the left once stood. Winds were estimated between 210 and 250 mph (F4
on the Fujita Tornado Damage Scale). This was the first tornado to
"officially" be rated a "F4" in the State of
Maryland. The Fujita Damage Scale was adopted by the National Weather
Service for use in 1950.
The total damage path of the
Frostburg tornado was over 25 miles long (8 miles in Allegany County)
and up to a half mile wide. Along most of its path it was producing
winds over 125 mph (F2 or stronger). The damage path was continuous as
it moved up and down over 2000 foot mountain ridges. The fact that no
one was killed in Maryland was attributed to 5 to 10 minutes warning
that was well communicated to people in Frostburg over television,
radio, scanners, telephones and sirens and people taken quick action to
move to their basements. A mother and child rode out the storm as it
destroyed the house shown on the left under a table in the basement.
They were shaken but unharmed. Debris from Frostburg homes were found 25
miles away. A diploma was found near Winchester, Virginia and a bill was
found near Sterling Virginia (about 100 miles away). Click here for more
pictures of this event and a full report.
12) Tropical Storm - Agnes
June 21-23, 1972
This storm had to be covered as
one of the top storms of the century even though flooding, flash flooding
and hurricanes was captured by other storms, hence this category as the
top tropical storm and quite a disaster it caused to the Mid-Atlantic
region. Agnes was like many early June tropical cyclones. It developed in
the Gulf of Mexico to become a weak Category 1 Hurricane by the time of
landfall on the Florida Panhandle. It weakened to a depression as moved
inland across Georgia and the Carolinas. It emerged off the Virginia Capes
and strengthened back to a tropical storm as it headed north to make
landfall once again on New York's Long Island. None of this sounds very
noteworthy especially when compared against large and powerful storms such
as Hurricane Floyd appeared as it approached the Bahamas. Agnes is a
reminder that we can not assume that the size and category of hurricane
tells the whole picture. Total storm damage in the United States from
Agnes was estimated at just under $3.5 billion with a death toll of 122
lives. Agnes produced tornadoes in Florida and flooding up the East Coast.
Hardest hit states from flooding included Virginia, Maryland, DC, and
Pennsylvania. Even with the storm center passing well off the Delmarva
Coast, Agnes managed to drop torrential rain over the region averaging
close to 8 to 10 inches over many basins and with as much as 16.65 inches
recorded at Washington-Dulles Airport in Virginia just west of Washington,
DC. Widespread flash flooding and major river flooding resulted.
In Richmond, the James River
crested 6.5 feet above the old record flood marks dating back 200 years.
Water supply and sewage treatment plants, along with electric and gas
plants, inundated and were partially shut down. Four of the five bridges
crossing the James were closed. A 200 block area of downtown Richmond was
swamped and closed off for several days. Flooding occurred on the
Appomattox River with Farmville suffering its worst flood in history. The
Dan River at Danville and the Roanoke River in Roanoke exceeded previous
record flood stages set in August 1940. The Shenandoah and the Potomac
Rivers flooded as well. Most northern Virginia streams and creeks
overflowed their banks during the night,
washing out roads and, in some cases, destroying homes. Uninsured homes
and a lifetime accumulation of household goods were quickly swept away.
Northern Virginia was particularly hard hit. Fairfax County reported an
estimated $25 million damage, by far the largest in the state. Manassas
was badly flooded as was the Occoquan River which washed out a section of
the U.S. Route 1 bridge. In Virginia, a total of 63 counties and 23
cities qualified for federal disaster relief. There were 13 deaths and
$222 million in damages. Sensitized by the Nelson County/Camille Flood in
August 1969, quick evacuation saved lives. Numerous homes were destroyed,
600 roads went underwater and 103 state highway bridges were washed out or
damaged.
In Maryland and the District of
Columbia, heavy rains in less than 24 hours, on the 21st and 22nd,
resulted in severe flooding. Maryland's heaviest rains occurred in the
north central part of the state where totals set all-time records. Highest
total rainfall was 14.68 inches at Westminister and 13.85 inches at
Woodstock. Totals of 8 inches or more fell in an area west of the
Chesapeake Bay and east of Hagerstown. The District of Columbia reported
more than 7 inches. The 11.55 inches at Westminister and 11.35 inches at
Woodstock on the 21st, are among the greatest one-day falls in Maryland
history.
One-day record rainfalls for Maryland include 14.75 inches at Jewell in
July, 1897 and 12.61 inches at White Marsh in August, 1971. The previous
one-day June record was 6.05 inches at Elkton on June 27th, 1938. A
24-hour (not limited to one day) total of 7.19 inches at Washington
National Airport on June 21-22 was second only to the 7.31 inch total of
August 11-12, 1928.
The heavy rains caused
disastrous flash flooding of creeks and streams in Maryland and the
District of Columbia. Major flooding followed. The Potomac fed by heavy
rains over its entire basin began flooding on the 22nd. At Little Falls,
just outside Washington DC, the river crested at 22.03 feet in the early
hours of the 24th. Flood stage is 10.0 feet. Meanwhile at Wisconsin
Avenue, downtown Washington, a 15.45-foot crest had occurred and persisted
for about 8 hours. Along the Monocacy River, a crest of 35.90 feet
occurred at Frederick, Maryland. The previous record was 30.0 feet set
back in 1889. Flooding also occurred along the Anacostia and Patuxent
Rivers and along Seneca and Rock Creeks. Flooding along the Patapsco River
broke all existing records. It was the worst flooding that the Baltimore
area had ever seen. Near the Pennsylvania border the Susquehanna, which
had devastated much of the Keystone State, threatened the Conowingo Dam.
Flood waters covered small towns of Port Deposit and Harve d'Grace below
the dam and a wide swath of land on both sides of the river from the dam
to the river's mouth at the Chesapeake Bay, some 12 miles away. Flood
gates were opened for more than 48 hours and the dam held.
Total storm damage in Maryland
and the District of Columbia was estimated at $110 million. There were 21
storm deaths in Maryland and none in the District of Columbia. The
following Maryland counties, including Baltimore City, were declared
disaster areas: Anne Arundel, Baltimore, Carroll, Cecil, Charles,
Frederick, Harford, Howard, Montgomery, Prince Georges and Washington.
Along the Chesapeake Bay, the counties named were Calvert, Dorchester,
Kent, Queen Anne's, St. Mary's, Somerset, Talbot and Wicomico.
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