In Kerala‘s Kuttanad region, farmers grow rice on land that sits below sea level, held back by bunds. The soil beneath it is peaty and marshy, built from centuries of trapped, half-decayed plants.


Must Know
- Peaty and marshy soil forms where waterlogging creates anaerobic, low-oxygen conditions.
- Those conditions only partly decompose plant matter, building up a thick layer of organic material over time.
- That heavy buildup of organic matter gives the soil its dense texture and black colour.
- India’s largest peaty and marshy tracts lie in Kerala’s Kuttanad region, in Alappuzha district.
- Similar deposits also occur along coastal Odisha, the Sundarbans delta, and other parts of West Bengal.
Good to Know
- These soils form in low-lying, high-rainfall areas prone to waterlogging: deltas, backwaters, and estuaries.
- Kerala’s Kuttanad soil carries a local name too: kari.
- Odisha’s peaty tracts form amid numerous rivers, estuaries, and mangrove-fringed wetlands.
- Rice grows especially well on these soils, since it tolerates standing water far better than most other crops.
Test Yourself
Great to Know
- Kuttanad is remarkable for more than its soil. Farmers there cultivate paddy below sea level, behind protective bunds.
- That makes Kuttanad one of very few places in the world where farming happens below sea level.
- The heavy, waterlogged nature of these soils makes them poor for most crops besides rice, without drainage work.
- Similar peaty deposits also form along the tidal stretches of the Mahanadi and Brahmaputra deltas.
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