PINELANDS SOILS CHART 2

The following soils show texture changes by accumulating clay in the subsoil. These soils are much more fertile, as clay aids in moisture and mineral retention.

FEATURE AURA SASSAFRAS DOWNER HAMMONTON MULLICA
A horizon (surface layer) A1: 0-1" dark grayish-brown, sandy loam
A2: 1-3" grayish-brown, sandy loam
A3: 3-16" yellowish-brown, sandy loam
A1: 0-3" dark grayish-brown, sandy loam
A2: 3-6" yellowish-brown, sandy loam
A1: 0-2" grayish-brown, loamy sand
A2: 2-16" brown, sand
A1: 0-10" dark grayish-brown, sandy loam O: organic material 0-3"
A : 0-12" black, sandy loam
B horizon (subsurface layer) Bt*: 16-21" yellowish-red, sandy loam
Bt: 21-36" yellowish-red, sandy clay loam
Bt: 36-50" yellowish-red, sandy loam
B1: 6-12" brown, sandy loam
Bt: 12-17" brown, heavy loam
B: 17-41" yellowish-brown, sandy clay loam
Bt: 16-24" yellowish-brown, sandy loam
B: 24-31" yellowish-brown, light sandy loam
Bt: 10-28" yellowish-brown, sandy loam
B: 28-35" yellowish-brown with loght brownish-gray mottles, loamy sand
Bt: 12-16" grayish-brown, sandy loam
Bt: 16-25" light brownish-gray, sandy loam
C horizon (substratum) C: 50-72" yellowish-red, loamy sand C1: 41-54" reddish-yellow, sandy clay loam
C2: 54-72" brownish-yellow, sand
C: 31-60" Light gray, sand C1: 35-48" brownish-yellow with light gray mottles, loamy sand C1: 25-36" light brownish-gray, loamy sand
c2: 36-60" light brownish-gray, sand
Seasonal High Water Table (in feet or inches below the earth's surface) greater than 5 feet greater than 5 feet greater than 5 feet 28 inches 0 inches
Elevation above sea level (approximation for comparison purposes) 50 feet 46 feet 42 feet 35 feet 30.5 feet

*t = significant clay accumulation resulting from downward leaching of clay from the next horizon