Tifton Well PumpCall (229) 520-5205

Well pump service in Tifton, Tift County, and nearby Sylvester, Ashburn, Ocilla, Nashville and Adel

Flat south Georgia farmland at sunset, with a row of pines, a farmhouse and a center-pivot irrigation line across a field

Calls and requests from these towns go to a local well pump pro who works in Tift County:

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Calls are answered 24/7. Weekdays 9 to 6 you may be put straight through to a local pro. Nights and weekends, if it can't wait, say so and we'll ring a local pro right away; otherwise a local pro will call you back the next business morning.

Which nearby towns are covered?

Homes around the county seats that border Tift County are covered too. Wells are even more common there than in Tift: in the U.S. Geological Survey's 2010 count, this share of each county's people supplied their own water. Distances here are straight-line from downtown Tifton, as the crow flies; by road they run a few miles longer.

What is under the ground in Tift County?

Simplified map of the Tifton area, Georgia: Tifton in the middle on Interstate 75, Ty Ty to the west, Omega to the southwest, the communities of Chula, Brookfield and Eldorado, and the neighboring county seats Sylvester to the west, Ashburn to the north, Ocilla to the northeast, Nashville to the southeast and Adel to the south.I-75TiftonOmegaTy TySylvesterWorth Co.AshburnTurner Co.OcillaIrwin Co.NashvilleBerrien Co.AdelCook Co.ChulaBrookfieldEldoradoTift County townNeighboring county seatInterstate 75Simplified sketch, not to scale
Tifton and the towns around it, simplified. Across this part of the Coastal Plain, home wells draw from the Floridan limestone, buried beneath sand and clay that runs from under 50 feet to several hundred feet thick and becomes quite thick in southeastern Tift County (Georgia Geologic Survey, 1976). Positions are approximate.

Tifton sits on what geologists call the Tifton Upland, gently rolling country with many small streams. Georgia's geologic survey describes the top layer across Tift and its neighbors as a sand and clay mix, from under 50 feet to several hundred feet thick and quite thick in southeastern Tift County. Under it lies the Floridan limestone, the aquifer that supplies the area's city wells, its industry and most deeper home wells. Most home wells are drilled through the sand and clay and finished in the top few feet of the rock.

The top of the limestone is uneven, worn and pitted with old sinkholes, so the depth to rock can change by tens of feet within a short distance, and in southern Tift County the survey found a buried low spot where the limestone is missing or much deeper. The water is under pressure and rises in a well's casing. The U.S. Geological Survey says water levels in the Floridan across south-central Georgia move with rainfall and with pumping, and in the Tifton Upland mainly with pumping, which here means farm irrigation. That is why two neighbors can have very different wells, and why dry summers show up as service calls.

Whatever the town, the usual calls are the same: no water at all, weak pressure, a pump that clicks on and off, or a pump at the end of its life. Building where there is no water line? See new well drilling.

Sources: Georgia Geologic Survey, Geohydrology of Ben Hill, Irwin, Tift, Turner, and Worth Counties (1976) (source); U.S. Geological Survey, Upper Floridan aquifer, south-central Georgia (source); U.S. Geological Survey, Report 87-4145, Tifton Upland water levels (source); U.S. Geological Survey, Water use in Georgia by county for 2010 (source); New Georgia Encyclopedia, Tifton (source); New Georgia Encyclopedia, Tift County (source); Georgia EPD, Bulletin 94, Hydrogeology of the Gulf Trough–Apalachicola Embayment area (1990) (source); ACCG, Georgia cities in more than one county, 2020 Census (source); National Weather Service Tallahassee, Drought information statement, April 23, 2026 (source).

Last reviewed November 11, 2026.

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