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Demo & Demolition Contractor in Ovid, NY

Commercial, residential, barn, and asbestos demo and demolition with full debris removal. Complete teardown from permits to final cleanup. Serving Ovid and all of Seneca County.

Demo & Demolition Services in Ovid

Backwell provides professional demo and demolition services in Ovid, Seneca County, and the surrounding area. Backwell provides full-scope demo and demolition services for commercial buildings, residential structures, barns, and industrial facilities throughout Central New York. We manage the entire process from pre-demolition assessments and permits through final debris removal and site grading. For structures containing asbestos, we partner with licensed abatement professionals to handle the hazardous materials, then complete the structural demolition and cleanup.

What We Provide in Ovid

Why Ovid Chooses Backwell

Based in Constantia, NY, we are local to Seneca County and know the area, the soil conditions, the regulations, and the contractors. When you hire Backwell for your demo or demolition project in Ovid, you get a crew that shows up on time with the right equipment and gets the job done. Contact us today for a free estimate.

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Demo & Demolition in Ovid

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Demolition in Nearby Areas

Geography & Site Conditions in Ovid, NY (Seneca County)

Ovid sits on the central plateau between Seneca and Cayuga lakes in Seneca County, on the narrow ridge of terrain that divides the two Finger Lakes watersheds. Soils across the village and surrounding agricultural-to-commercial parcels are predominantly Ovid silt loam, the series named for the town, along with Honeoye silt loam on the better-drained till, Lansing silt loam on the middle slopes, and Lima silt loam on the lower ground.

Drainage falls to both sides of the ridge through short, steep tributaries feeding Seneca Lake and Cayuga Lake respectively. Commercial site work in Ovid regularly involves managing fragipan-restricted subsurface drainage across essentially all of the silt loam uplands, slope stability on the steeper western and eastern flanks of the ridge, and stormwater design that has to satisfy Finger Lakes watershed protection standards for either receiving lake. Shallow shale bedrock can appear on the highest ridge sections. Frost depth is moderate given the lake-moderated microclimate. Projects along Route 96 that climb toward Willard and toward Lodi routinely require rock excavation and slope stability engineering on the steeper ridge flanks.