The Council Elder closed the Okeechobee entry in order, not in haste.
* * *
The storm formed in the eastern Atlantic in early September 1928 and moved west across the Atlantic and into the Caribbean with a track that was observed and reported by the Weather Bureau at each island it passed. It struck Puerto Rico on September 13th and killed hundreds. It moved northwest into the Atlantic and then west again into Florida, making landfall near Palm Beach on the night of September 16th, crossing the Florida peninsula from east to west and passing north of Lake Okeechobee as it tracked toward the Gulf of Mexico.
Measured only by wind and pressure, the storm did not stand alone among the earlier entries. What made it formative was where its force met the human arrangement on the south shore.
The Okeechobee storm was exceptional in where it placed its energy relative to where the people were.
* * *
The lake received the wind.
In the hours before the storm’s center passed north of the lake, the northeast wind that drove ahead of the vortex pushed the surface of Lake Okeechobee south and west, piling the water of the lake against the south shore levee with a force that grew as the wind sustained and as the fetch of the open lake allowed the surface to build. The lake is large enough — seven hundred and thirty square miles of shallow water — that the wind acting on its surface can generate a surge comparable to a coastal surge of the same wind velocity acting on an open bay.
The levee on the south shore was not built to hold a surge of this magnitude.
The levee failed in multiple locations.
The lake moved south.
* * *
What the lake moved through was the south shore muck plain and the communities that had been built on it and the people who were in those communities on the night of September 16th, 1928.
The people who were closest to the lake — in the labor camps on the muck, in the low-lying quarters of the south shore towns, in the fields — had the least time and the fewest options when the water came. The water arrived in the dark, in a wind that was still at hurricane force, in a landscape that had no orientation and no landmarks above the flood surface.
The people who survived were those who had somewhere to go that was above the water and who could reach it in the dark, through the wind, through the black water of unknown depth, before the water reached its maximum level.
The people who did not survive were those who did not have these things, or who could not reach them in time, or who were in the path of the water at a depth that left no margin.
* * *
The count remained a range.
The confirmed dead: approximately 1,800 to 2,500.
The probable dead, incorporating the unregistered migrant labor population and the unrecovered in the Everglades: 2,500 to 3,000 or more.
The Okeechobee flood was, by the most conservative estimate, the second-deadliest natural disaster in the history of the United States at the time of its occurrence. By the higher estimates, it was second only to Galveston.
The Archivist kept both estimates.
* * *
The Council measured what the storm found in four parts.
The Observer found a lake large enough and shallow enough to be moved hard by sustained wind, and a water level high enough above the muck plain to make failure immediately consequential.
The Analyst found a levee system assembled by multiple builders to inconsistent standards.
The Analyst found a warning system good enough for the coast and too weak for the interior camps.
The Analyst found a labor population placed on the lowest ground, with the least access to information, transportation, and durable shelter.
* * *
The Archivist filed Okeechobee beside Galveston and Miami.
Together the three entries described a generation of American storm encounters: the barrier island, the coastal boom city, the inland lake. Together they also described what humans built afterward and what they left unresolved.
The Archivist carried the enlarged Record forward.
* * *
The lake behind the Hoover Dike is still there.
It sits above the surrounding muck plain as it has always sat. It receives the Kissimmee River from the north. It drains south through the canals, slowly, managed by the water control structures that the Army Corps has installed and maintains. The water level in the lake is monitored continuously. The dike is inspected and maintained.
The south shore communities inside the dike have rebuilt and rebuilt again. Belle Glade is there. Pahokee is there. Canal Point is there. The agricultural operations that cover the muck plain are among the most productive in the country.
The harvest comes every year.
The labor arrives for the harvest.
The dike holds.
* * *
The Council did not close the entry with the dike or the harvest.
It closes the entry with what the muck plain holds below its cultivated surface: the evidence of the night of September 16th, 1928, incorporated into the soil as the muck incorporates everything it receives.
The storm has passed.
The lake is contained.
The count remains open.
The Archivist kept the count open.