1 Concrete Leveling Contractors in Tabernacle, New Jersey

Tabernacle Township is a township in central Burlington County, southern New Jersey, sitting along Route 206, Carranza Road, and the Batsto River headwaters in the Pine-Barrens-and-Cohansey-Sand-and-Batsto-River-and-Wharton-State-Forest country of central Burlington County. Prior to European arrival, the region encompassing present-day Tabernacle Township was part of the territory inhabited by the Lenape (also known as Delaware) people, who utilized the Pine Barrens' resources for hunting, fishing, and seasonal agriculture (the documented Lenape-hunting-fishing-and-seasonal-agriculture legacy). European settlement began in the early 18th century, driven by the availability of vast pine forests for timber, charcoal production, and emerging bog iron extraction, alongside fertile clearings suitable for small-scale farming (the documented early-18th-century Pinelands-timber-and-charcoal-and-bog-iron legacy). Tabernacle was incorporated as a township on March 22, 1901, from portions of Shamong Township, Southampton Township and Woodland Township, and was named for a tabernacle constructed by missionaries David and John Brainerd (the documented 1901-onward Tabernacle-Township-era and David-and-John-Brainerd-missionary-tabernacle namesake legacy). In 1928, Emilio Carranza, a Mexican aviator on the return leg of a goodwill flight between Mexico and New York, died in a Pinelands airplane crash during a thunderstorm, with a memorial located on Carranza Road in Tabernacle Township, Burlington County (the documented 1928 Emilio-Carranza-Mexican-aviator-Pinelands-crash-and-Carranza-Road-memorial legacy). The geology of the Pinelands on the coastal plain is rooted in the last ice age that caused sand deposition and erosion plus freeze-thaw cycles, with patterns in the landscape driven by fires in extensive dry, sandy forests and by water in many rivers and riparian swamps fed by the deep Kirkwood-Cohansey Aquifer (the documented last-ice-age sand-deposition-and-Kirkwood-Cohansey-Aquifer-fed-riparian-swamp legacy). Today Tabernacle Township (population 6,785 at the 2020 census) is a central-Burlington-County Pine-Barrens-and-Cohansey-Sand-and-Batsto-River-and-Wharton-State-Forest-and-Pinelands-National-Reserve township with significant documented Lenape-hunting-fishing-and-seasonal-agriculture legacy, early-18th-century Pinelands-timber-and-charcoal-and-bog-iron legacy, 1901-onward Tabernacle-Township-era and David-and-John-Brainerd-missionary-tabernacle namesake legacy, 1928 Emilio-Carranza-memorial legacy, Pinelands-National-Reserve-designation legacy, Kirkwood-Cohansey-Aquifer-fed-riparian-swamp legacy, and dense Pinelands-rural-and-farmstead-and-Wharton-State-Forest residential character. Tabernacle Township sits on the Pine-Barrens-and-Cohansey-Sand-and-Batsto-River terrain of southern New Jersey, in the Batsto River headwaters drainage within the New Jersey Pinelands National Reserve (with significant Wharton State Forest acreage within the township boundary). Bedrock beneath Tabernacle Township is Outer Coastal Plain Cohansey Sand (a dominant Pine-Barrens aquifer and surficial feature of the Kirkwood-Cohansey aquifer system). Above bedrock, surficial materials include extensive Cohansey-Sand-derived siliceous sand (with documented Pine-Barrens ortstein-hardpan and iron-cemented-hardpan character), Pleistocene Bridgeton Formation terrace sand-and-gravel on the upland parcels (with documented iron-cemented-hardpan character), Holocene Batsto River and Pinelands-stream alluvium on the stream-valley flats, Holocene Pine-Barrens cedar-swamp organic peat and muck on the extensive cedar-swamp parcels (with very poor slab-bearing conditions), historic bog-iron and charcoal-burning spoil on the former-industrial-bog parcels, and historic Pinelands-farmstead-fill on the rural-developed parcels. Local soils run Downer sandy loam on the Cohansey-Sand upland parcels (the documented Downer type series), Sassafras sandy loam on the Bridgeton-terrace upland parcels, Woodstown sandy loam on the moister terrace parcels, Hammonton loamy sand on the Cohansey-and-Bridgeton-derived moister upland parcels, Fallsington sandy loam on the poorly-drained Pinelands parcels, Atsion sandy loam on the wet Pinelands parcels (with documented ortstein-hardpan and wetness hazard), Berryland sandy loam on the very-wet Pinelands parcels, Lakewood sand on the droughty Pinelands parcels, Carlisle and Adrian muck on the extensive Pine-Barrens cedar-swamp parcels (with very poor slab-bearing conditions), and historic Pinelands-farmstead-and-bog-iron-spoil-fill on the rural-developed parcels. That Pine-Barrens-and-Cohansey-Sand-and-Batsto-River mantle with Downer-Sassafras-Woodstown-Hammonton-Fallsington-Atsion-Berryland-Lakewood-Carlisle-Adrian Cohansey-Sand-and-Pinelands-and-cedar-swamp-derived subgrades, documented Pine-Barrens ortstein-hardpan and iron-cemented-hardpan parcels on the Cohansey-Sand and Bridgeton Pinelands parcels with documented hardpan-perched-water hazard, Atsion-and-Berryland wet-Pinelands parcels with documented wetness and ortstein-hardpan hazard, Carlisle-and-Adrian-muck cedar-swamp parcels with very poor slab-bearing conditions, the historic early-18th-century Pinelands-timber-and-charcoal-and-bog-iron, 1901-onward Tabernacle-Township-era, and 1928 Emilio-Carranza-memorial foundations, dense Pinelands-rural-and-farmstead foundations, Batsto River headwater stage cycling on the stream-valley parcels, and steady Route 206 and Carranza Road corridor cut-and-fill on the recent corridor parcels is the primary driver of slab movement here.