The 1938 soil taxonomy divided soils into three orders dependent on dominant soil forming factors.
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Intrazonal soils
Intrazonal soils have more or less well-defined soil profile characteristics that reflect the dominant influence of some resident factor of relief or parent material over the classic zonal effects of climate and vegetation. There are three major sub-types, two of which have two further sub-types each.
Calcimorphic or calcareous soils develop from a limestone. It has two sub-types: Hydromorphic soils form in wetland conditions. There are two sub-types: Halomorphic soils form due to soil salination.Azonal soil
These soils are formed in mountainous regions out of fine grains produced by weathering. However, due to various reasons, this fine grained material constantly slides down the slope. As a result, the time necessary for the formation of soils does not become available. Therefore, these soils remain immature. An example is soil along the slopes of the Himalayan mountains. In river plains, particularly in flood-plain areas, new alluvium is deposited every year. The time for soil formation remains inadequate. Hence, flood plain soils also remain immature. In river plains, due to alluvium and availability of water, the farmlands are fertile but the soils remain immature.