The parent material of soils is derived froma)Igneous rocks.b)Metamorp...
The parent material of soils is derived from sedimentary rocks. This is because sedimentary rocks are formed from the accumulation and compression of mineral and organic matter deposits over time. These rocks are then broken down physically and chemically to form soil.
Factors such as climate, topography, and time can influence the rate of weathering and soil formation. Climate, for example, can affect the amount of water available for chemical weathering and the types of chemical reactions that occur. Topography, on the other hand, can influence the amount of erosion and deposition that occurs in an area, which can affect the thickness and composition of the soil.
Furthermore, biological action can also play a role in the formation of soils by introducing organic matter and nutrients into the soil. For example, decomposing plant matter can add nutrients to the soil and increase its fertility.
In summary, while biological action can contribute to the formation of soils, the parent material of soils is primarily derived from sedimentary rocks that have undergone weathering and erosion over time.
The parent material of soils is derived froma)Igneous rocks.b)Metamorp...
Sedimentary rocks