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Beneath South Florida’s coastline, the ground is changing. Off the shores of Miami, scientists have long known that the seafloor and the land itself rest on highly porous limestone — rock that slowly dissolves when exposed to water. Under normal conditions, this process takes thousands of years. But what happens when the chemistry accelerates? In this investigation, we examine the growing concern around coastal karst collapse, saltwater intrusion into the Biscayne Aquifer, and the hidden geological vulnerabilities beneath one of America’s most densely populated coastlines. Florida is built on carbonate rock. Saltwater is pushing inland. And the underground voids that naturally form in this environment may be more extensive than most people realize. In this documentary, we break down: How limestone dissolution creates sinkholes and subsurface voids Why saltwater intrusion increases rock corrosion The structure of the Biscayne and Floridan aquifer systems USGS data on karst terrain across the United States Sea level rise and its effect on coastal groundwater chemistry The real engineering and geological risks facing South Florida Important context: there is currently no evidence of a single catastrophic collapse event beneath Miami. However, the underlying geological processes described in this video are real, measurable, and actively studied by scientists and coastal engineers. Understanding the science matters — because slow geological risks often receive the least public attention until they become serious. The coastline looks stable. But the rock below tells a more complicated story. #miamisinking #floridasinkholes #breakingnews