Revision summary
The Deccan Trap is a huge basalt plateau of late Cretaceous to early Cenozoic age. It supplies building stone and weathers to black cotton soil and laterite. Cotton, soybean, and dry millets ride that soil. Fractured basalt holds patchy groundwater; rivers still matter for irrigation. Bauxite and some other ores sit on or beside lateritised trap country.
Model answer
Copper italics in this answer — like this — are the key facts. Each one is unpacked in the Facts & figures rail.
Introduction
The Deccan Trap is a vast Cretaceous–Paleogene basalt pile across Maharashtra and neighbouring states. Its resource potential is the lava itself, the soils it weathers into, and the minerals and water stored in its layers.
Body
Rock, soil, and farming
- Flood basalts yield road metal, railway ballast, and building stone on a continental scale.
- Weathering produces black cotton soil (regur), which holds moisture and supports cotton, soybean, sorghum, and pulses in Maharashtra, Madhya Pradesh, and Gujarat.
- Laterite caps on trap plateaus give brick earth and, in places, bauxite-rich profiles.
- Inter-trappean beds hold thin sediments and fossils; they also mark breaks where soils and aquifers can sit.
Minerals and energy-related uses
- Bauxite on lateritised trap and nearby plateaus feeds aluminium in parts of Maharashtra, Chhattisgarh, and Odisha’s border belts.
- Iron, manganese, and some limestone occur in and around the trap country, though the richest iron belts of India are not only trap rock.
- Vesicular and fractured basalt stores groundwater in shallow unconfined systems, which dug wells and tanks have long used, even if yields are patchy.
- Geothermal and ornamental-stone uses exist locally; they are secondary to soil and aggregate.
Limits of the potential
- Poorly managed black soil erodes into gullies, and rain-fed cotton belts remain drought-prone.
- Hard compact basalt is a poor deep aquifer unless fractures connect, so irrigation still leans on rivers such as the Godavari, Krishna, and Tapi.
- Resource wealth is therefore agricultural and construction-led, not a hidden oil province inside the lava pile.
Flow diagram
Conclusion
Deccan Trap potential is basalt aggregate, black cotton and laterite soils, patchy groundwater, and plateau bauxite. It is a farming and building storehouse, not an unlimited mineral sea.
Quick related
Students also ask
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What are the forces that influence ocean currents? Describe their role in fishing industry of the world.
Next question on this syllabus topic (2022 · Q14). View answer →
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Is the whole Deccan Trap rich in petroleum?
The lava pile itself is not a classic oil reservoir. Hydrocarbons in western India sit mainly in sedimentary basins beside or below volcanic cover.
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Why is cotton tied to this region?
Regur’s clay and moisture-holding suit rain-fed cotton better than many red soils of the open shield.
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