Local resources: Sânger

SOILS
Soils ARE the result of joint action of all factors of solidification. It is impossible to delimitate the action of each factor.The water ground has a dominant role in shaping and territorially distributing the soil, parent rock, vegetation and topography. Direct influence of relief is particularly observed in the erosion process.
On strong tilt mountains, rare vegetation covered, soil is exposed to erosion by water flow, which removes the upper horizons, and lower horizons have a lower fertility. In this version the erosion process is stronger than that of pedogenesis. On weak tilt mountains it is produced a slowe drive of the material from the upper layer.The smooth particles are caused by water,being transported and deposited at the bottom of the mountain giving rise to more fertile soils.
On the plane lands or with small inclinations due to unpervious horizon, water from rain don’t penetrate very deep into the soil, stagnanting in this horizon, which leads to pseudo