A reddish soil formed by the weathering of old crystalline and metamorphic rocks in the low-rainfall areas of the Peninsular plateau, owing its colour to iron oxide.
The crystalline-rock origin, the iron-oxide colour, the low fertility (improved by inputs), and the Peninsular low-rainfall distribution are recurring soils facts and matching items.
Red soil (weathered crystalline rock, iron-oxide colour, low rainfall areas) is different from laterite soil (intense leaching, high rainfall, infertile, hardens into brick) and from black cotton soil (basalt weathering, moisture-retentive). All three occur in the Peninsula.
Iron-oxide-reddened soil from old crystalline rocks of the low-rainfall Peninsula; porous, low in nutrients, improved with inputs.