
158 Pedodiversity
Mollic and Typic Haploxeralfs. These were moderately deep soils, with a
rather shallow and not very thick argillic horizon that, depending on the
morphology and mainly on the plant cover, might be overlaid by a mollic
epipedon. The less stable surfaces (which were on gentle or moderately
steep slopes), showed Vertic and Typic Haploxerepts, Typic Calcixerepts
and Calcic, Entic, Pachic and Typic Haploxerolls. These were soils in general
moderately deep with a cambic or a calcic horizon overlaid, in several
cases, by a mollic epipedon. The steeper surfaces and the slope side of the
stream valleys were, and in some cases still ...