Forest Soils
Forest soils are predominantly located in hilly and mountainous areas, characterized by their ability to sustain diverse vegetation due to sufficient rainfall and favorable climatic conditions. These soils vary in texture; they are usually loamy and silty on the valley sides and can be coarse-grained on the upper slopes.
In more temperate and snow-covered regions, the forest soils experience denudation, revealing acidic profiles with low organic content. Conversely, the soils found on the fertile river terraces and alluvial fans exhibit rich fertility due to the accumulation of organic materials and nutrient-rich sediments deposited by water flow.
The interplay of relief, climate, vegetation, and time greatly affects the soil formation process, making these soils significant not just for agriculture but also for preserving the ecological dynamics and biodiversity of forest ecosystems.