1 Concrete Leveling Contractors in Wakefield, New Hampshire

If you need concrete leveling in Wakefield, the usual culprits are dense glacial-till mantle with Hollis, Charlton, Paxton, and Woodbridge till-derived sandy loams and fragipans, and frost-susceptible silt-rich till producing aggressive freeze-thaw heave. Wakefield is a town in eastern Carroll County, eastern New Hampshire, sitting along NH-16, NH-109, NH-153, and US-4 about 75 miles north-northeast of Concord and along the Maine state line. Initially a native settlement, Wakefield was attacked by John Lovewell during Father Rale's War; settled later by colonists from Dover and Somersworth, the town was granted in 1749 by John Mason and was called "East Town" before being incorporated as Wakefield in 1774 by Governor John Wentworth. The town developed as an important sledge and stage stop between the seacoast and the White Mountains. The state of Maine forms the eastern border of Wakefield. Lovell Lake is a 538-acre water body in the south-central part of the town, flowing out to the west via the Branch River through Sanbornville (Sanbornville is the principal village of Wakefield). Province Lake is a 968-acre water body located on the border between New Hampshire and Maine, with approximately 950 acres of the lake in the towns of Effingham and Wakefield, New Hampshire, and the remainder in Parsonsfield, Maine; the northernmost corner of town is in Province Lake, which drains north into the South River, a tributary of the Ossipee River. Today Wakefield (population 5,261 at the 2020 census) is a Lakes-Region lake-cabin and seasonal residential community along the Maine border with significant Sanbornville-village historic character. Wakefield sits on the rolling till-mantled bedrock terrain at the eastern edge of the Lakes Region, in the Salmon Falls River, Branch River, and Ossipee River drainages. Bedrock is principally Devonian Concord-type granite plutonic intrusions of the New Hampshire Plutonic Suite, with Devonian Littleton Formation schist and quartzite of the Central Maine Belt locally and the Silurian-Devonian Berwick Formation and Eliot Formation metasedimentary rocks of the Merrimack Trough. Above bedrock, late Wisconsinan glacial till (a stony sandy loam mantle deposited 14,000 years ago by the retreating Laurentide Ice Sheet) blankets the hillsides, with extensive glaciofluvial outwash (sand and gravel) along the Branch River corridor and around the lake basins, glacial-lake-deposited fine sediments in some valley bottoms (with Lovell Lake, Province Lake, Belleau Lake, Pine River Pond, Great East Lake, and Wilson Lake occupying glacially-scoured-and-dammed basins; Wakefield is sometimes called the "Town of Lakes" with at least 12 lakes within its borders), Holocene Branch alluvium and organic peat in wetlands. Local soils include Hollis and Charlton complex on the till uplands (the dominant southern New England forest soil; Hollis is shallow-to-bedrock and Charlton is deeper till), Paxton fine sandy loam on the till uplands (with significant fragipan), Woodbridge fine sandy loam on the till uplands (poorly drained over fragipan), Ridgebury fine sandy loam on the till lowlands (very poorly drained), Hinckley loamy sand on the outwash terraces (excessively drained kame-and-esker glaciofluvial), Windsor loamy sand on the outwash sand plains, Searsport mucky peat on the wetland flats, Saco silt loam on the alluvial flats, and gravelly alluvium along the Branch River corridor. Between dense glacial-till mantle with Hollis, Charlton, Paxton, and Woodbridge till-derived sandy loams and fragipans, frost-susceptible silt-rich till producing aggressive freeze-thaw heave, perched-water cycling on Paxton and Woodbridge fragipan parcels driving subgrade saturation, granite shallow-bedrock differential bearing on bedrock-near-surface parcels, glacial erratics producing localized hard spots, the historic 1774-onward Wakefield Corner National Register Historic District foundations (with century-and-a-half-old to nearly-two-and-a-half-century-old Federal-era foundations along Wakefield Corner) and the Sanbornville village foundations, dense Lovell Lake, Province Lake, Belleau Lake, Pine River Pond, Great East Lake, and Wilson Lake shoreline lake-cabin and seasonal residential parcels with frost-jacking and seasonal-occupancy thermal cycling (Wakefield's at-least-12 lakes drive heavy seasonal residential demand), and steady NH-16-corridor commuter and Lakes-Region-tourist cut-and-fill on the recent NH-16 corridor parcels, subgrade behavior is the primary driver of slab movement here.