Mineral
horizon below an O, A, or
E horizon. The B
horizon show evidences of soil forming
processes which distinguish it from the
parent material of soil (underlying
C horizon). The distinctive characteristics can be: (1) accumulation (iluviation) of
clay, sesquioxides,
humus, or a combination of these; (2) granular, prismatic, or blocky
structure; (3) redder or browner colours than those in the
A horizon; (4) evidences of accumulation of secondary gypsum or carbonates; or (5) a combination of these.