Red and Yellow Soils
Red and yellow soils are primarily formed from the weathering of crystalline and metamorphic rocks in regions with low rainfall, predominantly found in the eastern and southern parts of the Deccan plateau as well as parts of Odisha, Chhattisgarh, and the middle Ganga plain.
Formation and Characteristics
These soils derive their reddish color from iron oxides that form as iron in the parent rock oxidizes. When the iron content is hydrated, these soils take on a yellowish hue, indicating varying drainage conditions.
Distribution
The red and yellow soils spread across several states, particularly visible in hilly and plateau regions. Their fertility is moderate, making them suitable for certain crops like millet and pulses, but they often require the addition of fertilizers for optimal productivity.
Significance
Understanding the distribution and uses of these soils is crucial for agricultural planning and sustainability in Indiaβs diverse climatic and geographical landscape.