24/7 Drain Cleaning & Sewer Service in Charleston, SC

South of Broad, the French Quarter, Ansonborough and Harleston Village have homes from the 1700s and 1800s, including Charleston single houses with side piazzas, many on raised foundations with old sewer connections.

Upper peninsula neighborhoods like Wagener Terrace, Hampton Park Terrace and the East Side have homes from the 1880s through the 1940s.

West Ashley, James Island and Mount Pleasant across the rivers filled in from the 1950s onward with ranches and newer subdivisions.

Much of the peninsula sits on filled marsh and creek beds just a few feet above sea level.

Tidal flooding is frequent, and hurricanes like Hugo in 1989 have damaged the city.

Charleston Water System runs the sewer system and treatment for the City of Charleston. Charleston property owners maintain the private sewer lateral from the house to the public main.

Hurricane season and summer afternoon storms flood peninsula streets in minutes, and king tides in fall can flood low areas on sunny days.

Mild winters rarely freeze, but a few cold nights can catch exposed pipes under raised houses.

Charleston's historic district, south of Broad and around the Battery, has homes dating to the early 1700s, including the city's signature single houses, one room wide with long side porches called piazzas. Plumbing came long after construction, and laterals run through courtyards and narrow side yards to the street. Sandy fill shifts, old pipe cracks and groundwater seeps in. Lining is often the best fix where digging would disturb historic gardens.

Much of the peninsula sits on filled creeks and marsh only a few feet above sea level, and tidal flooding has grown more frequent as seas rise. During king tides, water comes up through storm drains onto streets like Lockwood and Market. Groundwater rises with the tide, and cracked laterals take in water. A one-way backflow device and a cleanout cap set above the flood line keep tidewater out of the house.

Charleston's live oaks, many centuries old, shade the city's streets and parks. Their roots spread wide through sandy soil and find cracked joints in old clay and cast iron. Root cutting and lining keep lines open without harming protected trees.

Wagener Terrace, Hampton Park Terrace and the East Side have homes from the late 1800s through the 1940s, many raised on piers. Old laterals and live oak roots are common challenges, and some low streets flood regularly.

During an October king tide, a family in an 1850s single house in Harleston Village finds the downstairs toilet gurgling and the tub draining slowly. The plumber waits for the tide to drop, then opens the cleanout under the piazza and clears roots and sand about twenty feet out. The camera shows a cracked clay section with groundwater seeping in. They plan a liner and a backflow preventer.

Many Charleston homes are raised on brick piers, with drain lines running underneath. In the humid salt air, cast iron and galvanized lines corrode. Leaks under the house can go unnoticed until there's a smell.

The College of Charleston sits in the middle of the historic district, and many old homes nearby are rented to students. Heavy use in old laterals means more clogs, especially in August and January.

Charleston is one of the most visited cities in the country, and short-term rentals and inns fill historic homes. Guests flush things residents never would. Rental owners who post signs and jet lines regularly avoid emergency calls.

Charleston's restaurant scene, from King Street and Upper King to the Market and Shem Creek, is nationally famous, and shrimp and grits, fried seafood and Lowcountry boils produce a lot of grease. Kitchens there keep interceptors pumped on a strict schedule.

West Ashley and James Island filled in from the 1950s onward with ranches and newer homes, many under live oaks. Cast iron under older slabs can corrode, and roots find cracked joints. Low areas near marshes flood in storms.

Neighborhoods like Avondale and Byrnes Downs have older ranches whose original laterals are reaching the end of their life.

Each spring, before the tropics wake up, an older Charleston line is worth a cleaning and a camera run. After a storm, wait for flooding to recede before running a lot of water, and watch for slow drains or odors.

The 1886 Charleston earthquake damaged much of the city, and the region is still seismically active. Old pipe in sandy fill is vulnerable to shifting during even small tremors.

Charleston has spent decades and hundreds of millions of dollars on drainage tunnels and pump stations under the peninsula to move storm water out to the rivers faster. Those projects help streets drain, but private laterals still sit in waterlogged soil. Homeowners on the lowest blocks benefit most from a backflow preventer, a raised cleanout cap and a sealed lateral.

Across the Cooper River, Mount Pleasant has grown from a small village into a large suburb, with homes from the 1950s onward and many newer subdivisions near the marsh. Older homes have cast iron or clay lines under live oaks, while newer homes see mostly grease and wipes. Low areas near Shem Creek and the marsh can flood in storms.

Share the neighborhood, the home's age, whether it's raised and whether it's a rental. Mention live oaks near the line and whether a storm or high tide came first.