In-ground swimming pool excavation for residential and commercial properties. Precise depth, clean walls, full spoil removal, and site preparation for the pool crew.
Backwell excavates in-ground swimming pools for residential and commercial properties throughout Macedon, Wayne County, and the surrounding area. Pool excavation requires precision — the hole needs to be the right depth and dimensions, walls need to be clean and stable, and all spoil needs to be removed from the site before the pool contractor arrives. We work directly with pool companies and homeowners to ensure the dig is done right the first time.
We handle pools of all shapes and sizes including vinyl liner, fiberglass, and gunite pools. Our operators are experienced with the precision required for pool work — setting grades, maintaining clean walls, avoiding damage to access routes, and removing spoil efficiently. We also handle all associated site preparation including access clearing, spoil hauling, and rough grading after installation.
If you are planning an in-ground pool in Macedon, contact us for a free estimate. We will coordinate directly with your pool contractor on dimensions, access, and timing.
Macedon lies in western Wayne County along the Erie Canal, inside the Finger Lakes drumlin field east of Rochester. Soils across the town's commercial corridors along Route 31 and the NYS Thruway interchange are predominantly Honeoye silt loam and Lima silt loam on the drumlin flanks, with Palmyra gravelly loam on the outwash benches and Canandaigua silty clay loam and Wayland silt loam in the low ground along the canal and Mud Creek.
The Erie Canal and its feeder channels control drainage across the northern half of the town, and any earthwork inside or adjacent to the canal prism triggers NYS Canal Corp review. Commercial excavation in Macedon typically involves cobbly, stony trenching on the drumlins, structural fill importation on the clay-loam flats, and stormwater design tied to the Ganargua Creek and Genesee River watershed. Shallow bedrock appears only on the highest drumlin summits. Frost depth is moderate by regional standards, reflecting the transition between lake-moderated and interior climate zones.