Gravel, Stone and Soil Delivery in Canton, OH

Snow, freeze and thaw at the airport gauge

The NOAA normals station at Akron Canton RGNL AP, OH, about 9 miles away, supplies the weather averages here. It records 41.6 inches of precipitation and 47.2 inches of snow in an average year. That is a lot of water landing on a drive in both liquid and frozen form, and much of the snow melts and refreezes several times before spring.^[1]

The same gauge counts 120 days a year when the low reaches 32 F or colder. Its median last spring freeze falls on April 24. Its median first fall freeze falls on October 26. Each swing across the freezing mark lets water in the ground expand and then shrink, and a base that holds water heaves and cracks under that cycle.^[1]

The answer is a base that drains. Clean stone with open gaps, such as #57 Crushed Stone, gives meltwater a way down and out before it can freeze in place. A compacted layer of Road Base above it gives a firm, plowable surface. A crown and a ditch or a strip of Drain Rock along the low side carry spring melt away from the drive.^[1]

Plows and shovels push stone off a drive every winter. A thin top layer of 3/4" Crushed Stone is easy to rake back in spring and simple to top up. Setting the plow blade a little high, or using shoes on the blade, keeps more stone on the drive and less on the lawn.^[1]

Silt loam over layered rock

At the ZIP's center point, the USDA soil survey maps Chili-Urban land complex, undulating. Chili is the natural soil in the mix, at 51 percent of the map unit, and urban land makes up 49 percent. Urban land here means ground that has been paved, graded or built over, which is common in an older city core.^[2]

Where Chili is still in place, the survey rates it well drained and puts it in hydrologic group A, where water soaks in fast and runs off least. The top mineral layer is silt loam. Shrink-swell in the top meter rates low, at 1.5 percent. Silt loam holds more water near the surface than sand does, so it can soften in a thaw, though the lower soil lets water move down.^[2]

Below the soil, the geologic map shows the Allegheny and Pottsville Groups, Undivided. That unit is Pennsylvanian in age and holds shale, siltstone, limestone, sandstone, claystone and bituminous coal in stacked layers. The ground at the center point stands 1,060 feet above sea level.^[3],[4]

On an undulating surface, water collects in the low spots between rises. A drive or a patio set across one of those dips needs a little more base and a planned outlet for water, or it will hold a puddle that freezes into ice.^[2]

Downtown homes in ZIP 44702

The Census counts 659 housing units in ZIP 44702. Detached single-family houses make up 5 percent of them, and owners live in 5 percent of the occupied homes. The median home in the ZIP was built in 1967. Most housing in this ZIP is in apartments and other attached buildings.^[5]

Canton as a whole is a city of houses. The Census counts 33,836 housing units across the city, and 69 percent of them are detached single-family homes. The median build year is 1947. Older houses often have a narrow drive, a detached garage at the back of the lot and an alley behind it.^[5]

Those features shape the jobs people order. A gravel pad beside a garage, a parking strip off an alley or a new base under an old drive are common in older neighborhoods. Downtown, the orders lean toward planters, courtyard beds and small paths behind commercial buildings.^[5]

A drive built for Ohio winters

Ohio's Department of Transportation builds roads over a compacted stone layer described as Aggregate Base, Item 304, in its Construction and Material Specifications (2023). A home drive uses the same principle: a dense layer of angular stone, compacted in lifts, over a firm and drained subgrade.^[6]

Start by digging out the topsoil and any soft spots, then grade the subgrade with a crown. On silt loam, lay a fabric to keep the fines from pumping up into the stone during a thaw. Spread a lower course of #4 Crushed Stone or 1-1/2" Crushed Gravel for strength and drainage.^[2]

Over that, add Road Base in thin lifts and compact each one. The fines fill the gaps and set into a smooth layer that plows well. Finish with 3/4" Crushed Stone or Driveway Gravel. Asphalt Millings are another choice for a drive that should pack hard and shed snow like pavement.^[6]

Road Base or #57 on an alley pad

Owners in older neighborhoods often ask whether a parking pad should be topped with Road Base alone or with clean stone. Road Base packs into a smooth, hard layer that a car can turn on without digging ruts. In a long freeze it can hold some water near the top, and a thaw can leave it soft for a few days.^[1]

#57 Crushed Stone is clean and open. Water drops straight through it, so it never turns to mud and does not hold ice in its gaps. It is looser underfoot and shifts a little when tires turn sharply on it. A plow can also scatter it if the blade sits low.^[1]

For a pad in a snowy climate, the best answer is often both. Compact Road Base as the working layer, then spread a thin top of #57 Crushed Stone or 3/4" Crushed Stone. The base carries the weight, and the clean stone on top drains the melt. On silt loam, add fabric under the whole build so the base stays clean through every thaw.^[1],[2]

Edge the pad where it meets a lawn or an alley. A row of timber, steel or set stone keeps the gravel from creeping out each time a car pulls in. Without an edge, the outer foot of the pad thins out within a few seasons.^[5]

Beds and yards between the freezes

Garden work fits between the two freeze dates. Spring beds go in after the median last spring freeze of April 24, and fall planting of shrubs and bulbs is best done well before October 26. Topsoil and Garden Soil raise a bed and warm up faster in spring than the silt loam around them.^[1]

A layer of Brown Shredded Mulch or Black Shredded Mulch protects roots from the freeze and thaw of winter. Spread it after the ground cools in late fall. Compost worked into a bed each year keeps silt loam loose and stops it from crusting.^[1],[2]

Around a foundation, a band of River Rock or #57 Crushed Stone at the drip line keeps roof water from splashing soil onto the siding. On ground that drains well, the stone lets the water sink in close to the house, so make sure the ground under the stone slopes away from the wall.^[2]