Hurricane and Storm Risk in Georgetown: A Documented, Two-Phase Pattern
Georgetown's hurricane history is real and repeated, but it doesn't follow the direct-landfall pattern that dominates most oceanfront storm-history pages -- the town's worst documented flood damage in recent decades came from a storm that made landfall 150 miles away. This page lays out the confirmed record rather than a generic hurricane-risk summary.
Hurricane Hugo, September 1989: Landfall Near Charleston, Real Damage in Georgetown
Hurricane Hugo made landfall near Charleston, South Carolina late on September 21 into September 22, 1989, as a Category 4 storm with sustained winds over 100 mph and a storm surge reported as high as 20 feet in places closer to landfall. Georgetown sits well north of Charleston, yet Hugo still caused severe, well-documented flooding here: local retrospective reporting describes a sailboat swept up next to the Georgetown Rice Museum in the flooded downtown, and both the Georgetown Landing and Belle Isle marinas were destroyed. Roughly 150 homes along Georgetown's waterfront were reported wiped out. Statewide, Hugo caused nearly $7 billion in damage and 13 deaths in South Carolina. For a Georgetown buyer, Hugo is the clearest evidence that a hurricane doesn't need to make landfall at Georgetown itself to cause severe local damage -- surge and wind effects extended well beyond the immediate landfall zone.
Hurricane Matthew, October 2016: Landfall at McClellanville, Surge at Georgetown
Hurricane Matthew made landfall near McClellanville, South Carolina on October 8, 2016 -- close enough to Georgetown County that it caused significant damage there directly, part of a broader swath of South Carolina damage concentrated in Beaufort, Berkeley, Charleston, Dorchester, Georgetown, and Horry counties, primarily from flooding, property damage, and widespread power outages. Water levels were documented topping 5 feet above normal at Oyster Landing, near Georgetown, during the storm. Matthew is also relevant as a comparison benchmark for later storms -- Hurricane Florence's 2018 flooding on the Waccamaw River at Conway was explicitly measured against, and exceeded, Matthew's prior record crest at that gauge, illustrating how each successive major storm here gets compared against the last one's specific, measured impact rather than treated as an isolated event.
Hurricane Florence, September 2018: The Storm That Didn't Land Here But Flooded Here Anyway
Hurricane Florence made landfall near Wilmington, North Carolina on September 14, 2018 -- not at Georgetown, and not even in the same state. Yet Florence produced some of the most significant flooding in Georgetown's modern record, arriving on a delay: flood waves working their way down the Waccamaw and Great Pee Dee rivers didn't reach Georgetown until nearly two weeks after landfall, flooding Constitution Park along Orange Street and covering Front Street around September 28, 2018, across several tide cycles. Upstream, the Waccamaw River at Conway crested at a record 21.16 feet, breaking its prior Hurricane Matthew-era crest by more than three feet, and the broader Pee Dee region saw flooding along the Pee Dee, Little Pee Dee, Lumber, Lynches, and Waccamaw rivers and their tributaries for weeks after the storm, with nearly 1,000 homes and businesses flooded near the Waccamaw River alone. Georgetown County itself was placed under a 'possibly record' flooding evacuation advisory as officials watched the river crests approach, according to contemporaneous Newsweek reporting. Florence is the single clearest illustration of why this page treats Georgetown's flood risk as genuinely two-phase: an immediate, if any, wind/surge event, and a separate, delayed river-crest event that can arrive well after the storm itself has left the news cycle.
Why This Pattern Matters More in Georgetown Than at a Straight Oceanfront Address
An oceanfront property's hurricane risk is, broadly, tied to whether a storm's eye and surge pass directly over or near it -- risk drops off relatively quickly with distance from the storm's track. Georgetown's risk doesn't work that way, because the town sits downstream of an enormous drainage basin: the Pee Dee, Waccamaw, and Black river systems collect rainfall from a wide swath of North Carolina and inland South Carolina, and that water has to pass through Georgetown on its way to Winyah Bay and the Atlantic regardless of exactly where a given storm made landfall. That means a Georgetown property owner's hurricane-season risk assessment reasonably has to include storms that track well away from Georgetown itself, if those storms drop heavy rainfall on the upstream Pee Dee or Waccamaw watershed. This is a genuinely different risk model than the site's oceanfront-market hurricane-risk pages describe, and it's the core reason this page doesn't borrow language from those pages.
What This Page Doesn't State
This page documents Georgetown's confirmed historical hurricane and river-flood record -- Hugo (1989), Matthew (2016), and Florence's delayed 2018 river flooding -- as real, sourced events. It does not state a specific current property's flood or storm-surge risk, a projected future storm frequency or intensity for Georgetown, or a current evacuation-zone designation for any specific address, since evacuation zones and specific projections were not independently confirmed for this build at the address level. Confirm current evacuation zone status directly with Georgetown County Emergency Management and current flood risk with the tools described on this site's Flood Zones Explained page before relying on general historical pattern alone. Nothing on this page is emergency-preparedness, insurance, or legal advice.
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Get a Free Agent Referral →Independent research. No ads. No sponsored listings. Data sourced from: the National Weather Service's Hurricane Hugo retrospective materials and local news retrospective reporting (WPDE, WBTW, WACH) for Hugo's September 1989 landfall near Charleston, statewide damage and casualty figures, and Georgetown-specific marina destruction and waterfront home losses; the National Hurricane Center's Tropical Cyclone Report for Hurricane Matthew and Live5News's retrospective coverage for Matthew's October 8, 2016 landfall near McClellanville and Georgetown-area surge and flooding impacts; the National Weather Service, South Carolina Department of Natural Resources' climate office chronology of Hurricane Matthew and Florence, and contemporaneous reporting (Newsweek, FITSNews, Post and Courier, CNN, NBC News, Euronews) for Hurricane Florence's September 14, 2018 Wilmington-area landfall and the delayed Waccamaw/Great Pee Dee river flooding that reached Georgetown roughly two weeks later, including the Waccamaw River's record 21.16-foot crest at Conway. Facts not independently confirmed and not invented here include: current FEMA evacuation zone designations for specific Georgetown addresses; any projected future storm frequency or intensity specific to Georgetown; and current storm-surge modeling for the Winyah Bay area. Confirm current evacuation zone and emergency-preparedness information directly with Georgetown County Emergency Management before hurricane season. Nothing on this page is emergency-preparedness, insurance, or legal advice.