Fig. 7.6 The Emmet soil series, an Inceptic Hapludalfs, is derived
from sandy loam till on drumlins. The horizon sequence is Ap (0–6 in.),
A (6–10 in.), Bw (10–18 in.), E/Bt (18–30 in.), and Bt (30 in. to base of
pit). The scale is in feet. Source Soil survey of Marinette County,
Wisconsin (Lorenz 1991)
Fig. 7.7 The Cunard soil series, a Typic Hapludalfs, contains loamy
till over limestone bedrock on glacial benches. The horizon sequence is:
Oe and A (0–6 in.), E/B (6–13 in.), Bt (13–27 in.), and 2R (27 in.). The
scale is in feet. Source Soil survey of Marinette County, Wisconsin
(Lorenz 1991)
7.2 Soils by Natural Resource Segment
103
from sandy loam till on drumlins. The horizon sequence is Ap (0–6 in.),
A (6–10 in.), Bw (10–18 in.), E/Bt (18–30 in.), and Bt (30 in. to base of
pit). The scale is in feet. Source Soil survey of Marinette County,
Wisconsin (Lorenz 1991)
Fig. 7.7 The Cunard soil series, a Typic Hapludalfs, contains loamy
till over limestone bedrock on glacial benches. The horizon sequence is:
Oe and A (0–6 in.), E/B (6–13 in.), Bt (13–27 in.), and 2R (27 in.). The
scale is in feet. Source Soil survey of Marinette County, Wisconsin
(Lorenz 1991)
7.2 Soils by Natural Resource Segment
103
