1 Concrete Leveling Contractors in Magnolia, Mississippi

If you need concrete leveling in Magnolia, the usual culprits are variable Citronelle sand-gravel-clay subgrade, red-clay residuum shrink-swell cycling, Bogue Chitto alluvial seepage on low parcels, and bayhead-depression organics. Magnolia is the seat of Pike County, Mississippi, set along I-55 and US-51 in the extreme southern part of the state about 15 miles north of the Louisiana line. The area sits on the northern edge of the broader pinelands region of southeastern Mississippi, just north of the formally defined Pine Belt, which covers nine counties: Covington, Forrest, Greene, Jefferson Davis, Jones, Lamar, Marion, Perry, and Wayne. Pike County's parent material is dominated by the Pliocene Citronelle Formation, a prairie-like rolling-hill terrain of river-terrace deposits consisting of interbedded sand, gravel, and clay typically brick-red in color. Older Miocene Hattiesburg and Catahoula sediments underlie the Citronelle. Soils here are a mixture of sand and clay developed from these weathered Tertiary parent materials, historically nurturing longleaf pine but generally marginal for row-crop farming. Local soils include Ruston fine sandy loam, Smithdale fine sandy loam, Prentiss loam, Stough silt loam, and Ora fine sandy loam, along with sandy alluvium on the Bogue Chitto and Tangipahoa River tributaries, mucky loam in the bayhead depressions, and clayey alluvium in the backwater flats. Between the Citronelle sand-gravel subgrade, interbedded red-clay pockets, variable rolling-hill relief, and Bogue Chitto corridor exposure, subgrade behavior is the primary driver of slab movement here.