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Environmental Remediation Contractor in Seneca Falls, NY

Contaminated soil excavation, removal, and site remediation supporting brownfield redevelopment and environmental cleanup. Serving Seneca Falls and all of Seneca County.

Environmental Remediation Services in Seneca Falls

Backwell provides professional environmental remediation services in Seneca Falls, Seneca County, and the surrounding area. Contaminated sites need careful excavation and material handling to protect workers, the public, and the environment. Backwell provides the earthwork component of environmental remediation projects, contaminated soil excavation, segregation, loading, and transport to approved disposal facilities.

What We Provide in Seneca Falls

Why Seneca Falls 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 environmental remediation project in Seneca Falls, 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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Environmental Remediation in Seneca Falls

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Environmental Remediation in Nearby Areas

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

Seneca Falls sits at the outlet of Cayuga Lake on the Seneca River in northern Seneca County, on terrain shaped by glacial outwash, the Cayuga-Seneca Canal, and the surrounding drumlin field. Soils across the village and the Route 5/20 commercial corridor are a mix of Honeoye silt loam and Lima silt loam on the uplands, Palmyra gravelly loam on the outwash terraces, and Canandaigua silty clay loam and Wayland silt loam on the canal and river-adjacent flats.

The Cayuga-Seneca Canal and the Seneca River control base-level hydrology, and NYS Canal Corp review applies inside the canal prism. Commercial site work in Seneca Falls regularly involves dewatering on canal-adjacent parcels, cobbly trenching on the drumlin flanks, and stormwater design that ties into the Oswego River watershed. Structural fill is often required where native clay and silt loams cannot carry pavement loading. Shallow limestone bedrock can appear on the higher drumlin summits and along the gorge sections where the Seneca River drops toward the Cayuga Outlet. Frost depth is moderate.