paralithic contact
spodic materials
albic materials
cambic horizon
lithologic discontinuity
paralithic materials
redox depletions with chroma 2 or less
ochric epipedon
albic horizon
spodic horizon
argillic horizon
|
—
—
—
—
—
—
—
0—28
8—28
28—46
66—81
|
—-
—-
—-
—-
—-
—-
—-
—-
—-
—-
—-
|