|Category 4 major hurricane (SSHWS/NWS)|
|Formed||August 27, 1900|
|Dissipated||September 17, 1900|
|(Extratropical after September 11, 1900)|
|Highest winds||1-minute sustained: 145 mph (230 km/h)
|Lowest pressure||936 mbar (hPa); 27.64 inHg|
|Damage||$20 million (1900 USD)|
|Areas affected||Lesser Antilles, Puerto Rico, Hispaniola, Jamaica, Cuba, Turks and Caicos Islands, Bahamas, Florida, Mississippi, Louisiana, Texas, Oklahoma, Kansas, Nebraska, Iowa, Illinois, Wisconsin, Michigan, New York, Eastern Canada|
|Part of the 1900 Atlantic hurricane season|
The Hurricane of 1900 made landfall on September 8, 1900, in the city of Galveston, Texas, in the United States. It had estimated winds of 145 miles per hour (233 km/h) at landfall, making it a Category 4 storm on the Saffir–Simpson Hurricane Scale. It was the deadliest hurricane in US history, and the second costliest hurricane in U.S. history based on the dollar's 2005 value (to compare costs with those of Hurricane Katrina and others).
The hurricane caused great loss of life with the estimated death toll between 6,000 and 12,000 individuals; the number most cited in official reports is 8,000, giving the storm the third-highest number of deaths or injuries of any Atlantic hurricane, after the Great Hurricane of 1780 and 1998's Hurricane Mitch. The Galveston Hurricane of 1900 is the deadliest natural disaster ever to strike the United States. By contrast, the second-deadliest storm to strike the United States, the 1928 Okeechobee hurricane, caused more than 2,500 deaths, and the deadliest storm of recent times, Hurricane Katrina, claimed the lives of approximately 1,800 people.
The hurricane occurred before the practice of assigning official code names to tropical storms was instituted, and thus it is commonly referred to under a variety of descriptive names. Typical names for the storm include the Galveston Hurricane of 1900, the Great Galveston Hurricane, and, especially in older documents, the Galveston Flood. It is often referred to by Galveston locals as The Great Storm or The 1900 Storm.
The storm's origins are unclear, because of the limited observation ability at the end of the 19th century. Ship reports were the only reliable tool for observing hurricanes at sea, and because wireless telegraphy was in its infancy, these reports were not available until the ships put in at a harbor. The 1900 storm, like many powerful Atlantic hurricanes, is believed to have begun as a Cape Verde-type hurricane—a tropical wave moving off the western coast of Africa. The first formal sighting of the hurricane's precursor occurred on August 27, about 1,000 miles (1,600 km) east of the Windward Islands, when a ship recorded an area of "unsettled weather." The storm passed through the Leeward Islands on August 30, probably as a tropical depression as indicated by barometric pressure reports from Antigua.
Three days later, Antigua reported a severe thunderstorm passing over, followed by the hot, humid calmness that often occurs after the passage of a tropical cyclone. By September 1, U.S. Weather Bureau observers were reporting on a "storm of moderate intensity (not a hurricane)" southeast of Cuba. Continuing westward, the storm made landfall on southwest Cuba on September 3, dropping heavy rains. On September 5, it emerged into the Florida Straits as a tropical storm or a weak hurricane. The Weather Bureau ignored reports from Cuban meteorologists because they expected the storm to curve northeast along the coast of North America: "Assumption became fact as the official government reports stated, wrongly, that the storm was traveling northeast in the Atlantic." However, a region of high pressure had pushed the storm to the west into the Gulf of Mexico.
The storm was reported to be north of Key West on September 6, and in the early morning hours of Friday, September 7, the Weather Bureau office in New Orleans, Louisiana, issued a report of heavy damage along the Louisiana and Mississippi coasts. Details of the storm were not widespread; damage to telegraph lines limited communication. The Weather Bureau's central office in Washington, D.C., ordered storm warnings raised from Pensacola, Florida, to Galveston. By the afternoon of the 7th, large swells from the southeast were observed on the Gulf, and clouds at all altitudes began moving in from the northeast. Both of these observations are consistent with a hurricane approaching from the east. The Galveston Weather Bureau office raised its double square flags; a hurricane warning was in effect. The ship Louisiana encountered the hurricane at 1 p.m. that day after departing New Orleans. Captain Halsey estimated wind speeds of 100 mph (160 km/h). These winds correspond to a Category 2 hurricane in the modern-day Saffir–Simpson Hurricane Scale.
By early afternoon on Saturday, September 8, a steady northeastern wind had picked up. By 5 p.m., the Bureau office was recording sustained hurricane-force winds. That night, the wind direction shifted to the east, and then to the southeast as the hurricane's eye began to pass over the island just west of the city. By 11 p.m., the wind was southerly and diminishing. On Sunday morning, clear skies and a 20 mph (30 km/h) breeze off the Gulf of Mexico greeted the Galveston survivors. The storm continued on, and later tracked into Oklahoma. From there, it continued over the Great Lakes while still sustaining winds of almost 40 mph (as recorded over Milwaukee, Wisconsin) and passed north of Halifax, Nova Scotia, on September 12, 1900. From there it traveled into the North Atlantic where it disappeared from observations, after decimating a schooner fleet fishing off the coast of Newfoundland.
At the end of the 19th century, the city of Galveston, Texas, was a booming town with a population of 36,000 residents. Its position on the natural harbor of Galveston Bay along the Gulf of Mexico made it the center of trade and the biggest city in the state of Texas. With this prosperity came a sense of complacency.
A quarter of a century earlier, the nearby town of Indianola on Matagorda Bay was undergoing its own boom and was second to Galveston among Texas port cities. Then in 1875, a powerful hurricane blew through, nearly destroying the town. Indianola was rebuilt, though a second hurricane in 1886 caused residents to simply give up and move elsewhere. Many Galveston residents took the destruction of Indianola as an object lesson on the threat posed by hurricanes. Galveston is built on a low, flat island, little more than a large sandbar along the Gulf Coast. These residents proposed a seawall be constructed to protect the city, but their concerns were dismissed by the majority of the population and the city's government.
Since its formal founding in 1839, the city of Galveston had weathered numerous storms, all of which the city survived with ease. Residents believed any future storms would be no worse than previous events. In order to provide an official meteorological statement on the threat of hurricanes, Galveston Weather Bureau section director Isaac Cline wrote an 1891 article in the Galveston Daily News in which he argued not only that a seawall was not needed to protect the city, but also that it would be impossible for a hurricane of significant strength to strike the island. The seawall was not built, and development activities on the island actively increased its vulnerability to storms. Sand dunes along the shore were cut down to fill low areas in the city, removing what little barrier there was to the Gulf of Mexico.
On September 4, the Galveston office of the National Weather Service began receiving warnings from the Bureau's central office in Washington, D.C., that a "tropical storm" had moved northward over Cuba. The Weather Bureau forecasters had no way of knowing where the storm was or where it was going. At the time, they discouraged the use of terms such as tornado or hurricane to avoid panicking residents in the path of any storm event. Conditions in the Gulf of Mexico were ripe for further strengthening of the storm. The Gulf had seen little cloud cover for several weeks, and the seas were as warm as bathwater, according to one report. For a storm system that feeds off moisture, the Gulf of Mexico was enough to boost the storm from a tropical storm to a hurricane in a matter of days, with further strengthening likely.
Weather Bureau forecasters believed the storm would travel northeast and affect the mid-Atlantic coast. "To them, the storm appeared to have begun a long turn or 'recurve' that would take it first into Florida, then drive it northeast toward an eventual exit into the Atlantic." Cuban forecasters adamantly disagreed, saying the hurricane would continue west. One Cuban forecaster predicted the hurricane would continue into central Texas near San Antonio. Early the next morning, the swells continued despite only partly cloudy skies. Largely because of the unremarkable weather, few residents heeded the warning. Few people evacuated across Galveston's bridges to the mainland, and the majority of the population was unconcerned by the rain clouds that began rolling in by midmorning.
Isaac Cline claimed that he took it upon himself to travel along the beach and other low-lying areas warning people personally of the storm's approach. These reports by Cline and his brother, Galveston meteorologist Joseph L. Cline, have been called into question in recent years, as no other survivors corroborated these accounts. In fact, Cline's role in the disaster is the subject of some controversy. Supporters point to Cline's issuing a hurricane warning without permission from the Bureau's central office; detractors (including author Erik Larson) point to Cline's earlier insistence that a seawall was unnecessary and his belief that an intense hurricane could not strike the island.
The first train to reach Galveston left Houston on the morning of September 8 at 9:45 a.m. It found the tracks washed out, and passengers were forced to transfer to a relief train on parallel tracks to complete their journey. Even then, debris on the track slowed the train's progress to a crawl. The 95 travelers on the train from Beaumont found themselves at the Bolivar Peninsula waiting for the ferry that would carry them, train and all, to the island. When it arrived, the high seas forced the ferry captain to give up on his attempt to dock. The train crew attempted to return the way they had come, but rising water blocked the train's path.
Ten refugees from the Beaumont train sought shelter at the Point Bolivar lighthouse with 200 residents of Port Bolivar who were already there. The 85 who stayed with the train died when the storm surge overran the tops of the cars.
|“||First news from Galveston just received by train which could get no closer to the bay shore than six miles where the prairie was strewn with debris and dead bodies. About 200 corpses counted from the train. Large steamship stranded two miles inland. Nothing could be seen of Galveston. Loss of life and property undoubtedly most appalling. Weather clear and bright here with gentle southeast wind.||”|
At the time of the 1900 storm the highest point in the city of Galveston was only 8.7 feet (2.7 m) above sea level. The hurricane brought with it a storm surge of over 15 feet (4.6 m), which washed over the entire island. The surge knocked buildings off their foundations and the surf pounded them to pieces. Over 3,600 homes were destroyed and a wall of debris faced the ocean. The few buildings which survived, mostly solidly built mansions and houses along the Strand District, are today maintained as tourist attractions.
The highest measured wind speed was 100 miles per hour (160 km/h) just after 6 p.m., but the Weather Bureau's anemometer was blown off the building shortly after that measurement was recorded. The eye passed over the city around 8 p.m. Maximum winds were estimated at 120 mph (190 km/h) at the time, though later estimates placed the hurricane at the higher Category 4 classification on the Saffir–Simpson Hurricane Scale. The lowest recorded barometric pressure was 28.48 inHg (964.4 hPa), considered at the time to be so low as to be obviously in error. Modern estimates later placed the storm's central pressure at 27.49 inHg (930.9 hPa), but this was subsequently adjusted to the storm's official lowest measured central pressure of 27.63 inHg (935.7 hPa).
As severe as the damage to the city's buildings was, the human toll was even greater. Because of the destruction of the bridges to the mainland and the telegraph lines, no word of the city's destruction was able to reach the mainland. At 11 a.m. on September 9, one of the few ships at the Galveston wharfs to survive the storm, the Pherabe, arrived in Texas City on the western side of Galveston Bay. It carried six messengers from the city. When they reached the telegraph office in Houston at 3 a.m. on September 10, a short message was sent to Texas Governor Joseph D. Sayers and U.S. President William McKinley: "I have been deputized by the mayor and Citizen's Committee of Galveston to inform you that the city of Galveston is in ruins." The messengers reported an estimated five hundred dead; this was considered to be an exaggeration at the time.
The citizens of Houston knew a powerful storm had blown through and had made ready to provide assistance. Workers set out by rail and ship for the island almost immediately. Rescuers arrived to find the city completely destroyed. It is believed 8,000 people—20% of the island's population—had lost their lives. Estimates range from 6,000 to 12,000. Most had drowned or been crushed as the waves pounded the debris that had been their homes hours earlier. Many survived the storm itself but died after several days being trapped under the wreckage of the city, with rescuers unable to reach them. The rescuers could hear the screams of the survivors as they walked on the debris trying to rescue those they could. A further 30,000 were left homeless.
The dead bodies were so numerous that burying all of them was impossible. The dead were initially weighted down on barges and dumped at sea, but when the gulf currents washed many of the bodies back onto the beach, a new solution was needed. Funeral pyres were set up on the beaches, or wherever dead bodies were found, and burned day and night for several weeks after the storm. The authorities passed out free whiskey to sustain the distraught men conscripted for the gruesome work of collecting and burning the dead. More people were killed in this single storm than the total of those killed in all the tropical cyclones that have struck the United States since. This count is greater than 300 cyclones, as of 2009. The Galveston Hurricane of 1900 remains the deadliest natural disaster in U.S. history.
The storm maintained tropical characteristics and Saffir–Simpson tropical storm-force winds (39–50 mph) when it crossed the Upper Midwest, with more than 4 inches (100 mm) of rain being reported over most of the southern third of Wisconsin. Wind created problems all over, including over Lake Michigan, and other areas in the path of the storm had similar problems. (Tropical storms reach Wisconsin and surrounding areas to the east, west, and south once every 50 years on average with others in the 19th century, 1961, and (subject to debate) Hurricane Ike in 2008; tropical depressions hit twice to three times every two years; and subtropical storms and depressions hit equally or more rarely than their tropical counterparts.)
The rapidly moving storm was still exhibiting winds of 65 mph (105 km/h) by the time it reached New York City on September 12, 1900. The New York Times reported that pedestrian-walking became difficult and that one death was attributed to the storm. A sign pole, snapped by wind, landed on a 23-year-old man, crushing his skull and killing him instantly, while two others were knocked unconscious. Awnings and signs on many buildings broke and the canvas roofing at the Fire Department headquarters was blown off.
Closer to the waterfront, along the Battery seawall, waves and tides were reported to be some of the highest in recent memory of the fishermen and sailors. Spray and debris were thrown over the wall, making working along the waterfront dangerous. Small craft in New York Harbor were thrown off course and tides and currents in the Hudson River made navigation difficult. In Brooklyn, The New York Times reported that trees were uprooted, signs and similar structures were blown down, and yachts were torn from moorings with some suffering severe damage. Because of the direction of the wind, Coney Island escaped the fury of the storm, though a bathing pavilion at Bath Beach suffered damage from wind and waves.
|Rank||Hurricane||Season||Cost (2010 USD)|
|4||"Galveston"||1915||$ 71.3 billion|
|5||Andrew||1992||$ 58.5 billion|
|6||"New England"||1938||$ 41.1 billion|
|7||"Cuba–Florida"||1944||$ 40.6 billion|
|8||"Okeechobee"||1928||$ 35.2 billion|
|9||Ike||2008||$ 29.5 billion|
|10||Donna||1960||$ 28.1 billion|
|Main article: List of costliest Atlantic hurricanes|
About 8,000 people were killed and the city destroyed over the course of several days. The survivors had little to live on until relief arrived.
Survivors set up temporary shelters in surplus U.S. Army tents along the shore. They were so numerous that observers began referring to Galveston as the "White City on the Beach". Others constructed so-called "storm lumber" homes, using salvageable material from the debris to build shelter.
Reporter Winifred Bonfils, a young journalist working for William Randolph Hearst, was the first reporter on the line at the flood's aftermath. She delivered an exclusive set of reports and Hearst sent relief supplies by train.
By September 12, Galveston received its first post-storm mail. The next day, basic water service was restored, and Western Union began providing minimal telegraph service. Within three weeks, cotton was again being shipped out of the port.
Before the Hurricane of 1900, Galveston was considered to be a beautiful and prestigious city and was known as the "Ellis Island of the West" and the "Wall Street of the Southwest". However, after the storm, development shifted north to Houston, which was enjoying the benefits of the oil boom. The dredging of the Houston Ship Channel in 1909 and 1914 ended Galveston's hopes of regaining its former status as a major commercial center.
To prevent future storms from causing destruction like that of the 1900 hurricane, many improvements to the island were made. The first 3 miles (4.8 km) of the Galveston Seawall, 17-foot (5 m) high, were built beginning in 1902 under the direction of Henry Martyn Robert. An all-weather bridge was constructed to the mainland to replace the ones destroyed in the storm.
The most dramatic effort to protect the city was its raising. Dredged sand was used to raise the city of Galveston by as much as 17 feet (5.2 m) above its previous elevation. Over 2,100 buildings were raised in the process, including the 3,000-ton St. Patrick's Church. The seawall and raising of the island were jointly named a National Historical Civil Engineering Landmark by the American Society of Civil Engineers in 2001.
In 1915, a storm similar in strength and track to the 1900 hurricane struck Galveston. The 1915 storm brought a 12-ft (4-m) storm surge which tested the new seawall. Although 53 people on Galveston Island lost their lives in the 1915 storm, this was a great reduction from the thousands who died in 1900.
The Galveston city government was reorganized into a commission government, a newly devised structure wherein the government is made of a small group of commissioners, each responsible for one aspect of governance. This was prompted by fears that the existing city council would be unable to handle the problem of rebuilding the city.
Reference: Deadliest US hurricanes
Today, Galveston is home to a cruise port, two universities, and a major insurance corporation. Homes and other buildings that survived the hurricane have been preserved, and give much of the city a Victorian look. The seawall, since extended to 10 miles (16 km), is now an attraction itself, as hotels and tourist attractions have been built along its length in seeming defiance of future storms.
The last reported survivor of the Galveston Hurricane of 1900, Mrs. Maude Conic of Wharton, Texas, died November 14, 2004, at the claimed age of 116, although the 1910 census and other records indicate she was younger than that.
In historiography, the hurricane and the rebuilding afterward divide what is known as the Golden Era (1875–1900) from the Open Era (1920–1957) of Galveston. The most important long-term impact of the hurricane was to confirm fears that Galveston was a dangerous place to make major investments in shipping and manufacturing operations; the economy of the Golden Era was no longer possible as investors fled. In 1920, Prohibition and lax law enforcement opened up new opportunities for criminal enterprises related to gambling and bootlegging in the city. Galveston rapidly became a prime resort destination enabled by the open vice businesses on the island. This new entertainment-based economy brought decades-long prosperity to the island.
The Galveston Historical Foundation maintains the Texas Seaport Museum at Pier 21 in the port of Galveston. Included in the museum is a documentary titled The Great Storm, that gives a recounting of the 1900 hurricane.
I remember now that it seemed as if we were in a bowl looking up toward the level of the sea. As we stood there in the sandy street, my mother and I, I wanted to take my mother's hand and hurry her away. I felt as if the sea was going to break over the edge of the bowl and come puring down upon us.
Galveston Island, with all its boasted accumulation of people, habitations, wealth, trade and commerce, is but a waif of the ocean, a locality but of yesterday ... liable, at any moment, and certain, at no distant day, of being engulfed and submerged by the self-same power that gave it form. Neither is it possible for all the skillful devices of mortal man to protect this doomed place against the impending danger; the terrible power of a hurricane cannot be ... resisted. I should as soon think of founding a city on an iceberg.
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