Crushed Stone, Gravel, Soil and Mulch Delivery in Hampton, VA

Mostly Houses, Mostly Owned

Detached single-family houses make up 84 percent of the 6,879 housing units the Census Bureau counts in ZIP 23661. Owner households live in 70 percent of the occupied homes. The median home in the ZIP was built in 1954.^[1]

Citywide, Hampton has 62,588 housing units, 63 percent of them detached, and a median year built of 1974. A ZIP of owner-held houses from the middle of the last century tends to produce steady, practical orders: a parking pad widened for a second car, a gravel strip along a fence, a walk rebuilt where tree roots lifted the old one, and a lot of bed mulch every spring.^[1]

Many lots in an older neighborhood also carry an original gravel or cinder drive under years of patching. Before ordering, scrape a test spot to see what is down there. A firm old base can stay as part of the new subgrade, while a soft, muddy layer has to come out before new stone goes in.^[1]

Sandy Loam That Holds Water

The USDA soil survey maps Tomotley-Urban land complex, 0 to 2 percent slopes, at the ZIP's center point. Within that map unit, 15 percent is urban land, paved or built on, and the Tomotley series accounts for 70 percent. The top mineral layer is fine sandy loam.^[2]

The survey rates the Tomotley soil poorly drained and places it in hydrologic group B/D. So it behaves like group D, with slow intake and lots of runoff, while the water table is high, and like group B where the ground has been drained. Shrink-swell in the top 100 cm is low, at 1.5 percent linear extensibility, so the soil itself barely moves as it wets and dries.^[2]

The USGS state geologic compilation shows the Lynnhaven Member of the Tabb Formation under the center point, a Quaternary unit of sand and silt. Those young, loose layers are why digging is easy in most yards here and why water can sit just below the surface for days after a soaking rain.^[3]

Tidewater Weather Numbers

Langley Afb, VA, a NOAA normals station about 6 miles from the ZIP, gives the closest long weather record. Its annual averages are 47.8 inches of precipitation and 2.7 inches of snow. The low at that base drops to 32 F or below on 52 days in an average year.^[4]

For the Langley station, March 24 is the median date of the last spring freeze. November 15 is its median date for the first fall freeze. Beds can be planted early in the season and mulched late, and new grass seed has a long, mild fall to settle in.^[4]

Light snow rarely troubles a gravel drive here. Rain is what does the damage, along with the odd coastal storm that drops a lot of water at once. Surfaces that shed water fast and bases that drain freely last longest, and edges with a gravel shoulder hold up better than edges that end in bare soil.^[4]

A Parking Pad on Flat, Damp Ground

On a 0 to 2 percent slope with poorly drained soil, the first job is to lift the pad a little above the lawn so it never becomes the low spot. Strip the sod and loose topsoil, shape the fine sandy loam with a slight fall toward the street, and compact it. Lay a woven fabric across the whole area before any stone goes on.^[2]

Build the base from #57 Crushed Stone or 1-1/2" Crushed Gravel, which drain freely, and compact it in thin lifts. Cap it with a layer of Road Base or Crushed Concrete, packed hard, to give a tight surface that does not rut. For a cleaner look along the front of the house, finish with Driveway Gravel or 3/4" Crushed Stone instead.^[2]

The Virginia Department of Transportation calls its standard base material Aggregate Base Material, Type I, Size No. 21A, under Section 208 of its Road and Bridge Specifications (2020). That book governs highway work. For a home drive, the useful lesson is the same one road builders follow, a graded stone layer, compacted, with water kept out of it.^[5]

Where a pad meets the lawn, a row of edging or a strip of larger stone keeps the gravel from drifting into the grass when a mower or a tire catches it. Set the edge a little below the top of the stone so water still spills off the surface rather than ponding behind the border.^[2]

Where the Water Goes

In a flat sandy yard with a high water table, standing water after rain is the most common complaint. A trench along the low side of the yard, lined with fabric and filled with Drain Rock, collects water and moves it toward a ditch or the street. Where a long run is needed, a perforated pipe at the bottom of the trench speeds things up.^[2]

Downspouts deserve attention too. A splash bed of River Rock under each one spreads the water out instead of letting it dig a hole beside the foundation. Extending the outlet a few feet into a gravel-filled trench keeps roof water away from the crawl space or slab entirely.^[2]

Fine sandy loam drains well once it has somewhere to drain to, so even a shallow swale lined with River Rock can clear a soggy patch. Keep the swale gentle and wide rather than deep and narrow, and plant its edges with grass or groundcover to hold the soil in place.^[2]

Beds, Lawns and Mulch

Fine sandy loam is easy to work and warms early in spring, but it can lose water and nutrients faster than heavier soil. Mixing Compost into new beds gives the sand more body. Raised beds filled with Garden Soil keep roots above a wet subsoil and dry out sooner after a storm.^[2]

For lawn repair, spread a thin layer of Topsoil over bare or low spots, rake it level, and seed. Fill Dirt is useful for bringing up a sunken area first, with Topsoil on top to give the grass a better root zone. Water the new seed lightly and often until it takes hold.^[2]

Mulch is the most popular order in neighborhoods like this one. Brown Shredded Mulch knits together and stays put in heavy rain. Black Shredded Mulch and Red Mulch give a sharper color against green plants. Wood Chips are coarser and work well under trees and along play areas. Refresh beds before the season starts and again before the first fall freeze at Langley.^[4]