spodic materials
albic materials
albic horizon
argillic horizon
cambic horizon
lithologic discontinuity
ochric epipedon
redox depletions with chroma 2 or less
ochric epipedon
albic horizon
spodic horizon
argillic horizon
|
—
—
—
—
—
—
—
—
0—13
5—13
13—38
84—160
|
—-
—-
—-
—-
—-
—-
—-
—-
—-
—-
—-
—-
|