·The Hindu·15 marks·250–350 words

Discuss the geological basis of geothermal provinces in India. How can direct-use geothermal applications support livelihoods in high-altitude regions like Ladakh?

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In this answer
  1. Geological basis of geothermal provinces
  2. Direct-use applications for Ladakh's livelihoods

Geothermal energy is heat from the Earth's interior. It comes mainly from the radioactive decay of uranium, thorium and potassium [1]. The Geological Survey of India (GSI) has mapped 381 hot springs across 10 geothermal provinces [1][2]. Most sites suit direct heat use better than large power plants, which helps cold regions like Ladakh.

Geological basis of geothermal provinces

  • Common mechanism: mantle convection drives tectonic activity. Faults and fractures let heat rise and trap hot water in permeable rock [1].
  • Collision zone, Himalayan Province (Puga, Chumathang, Manikaran): the collision of the Indian and Eurasian plates created deep faults. Temperatures of up to 135°C have been recorded beneath Puga [1].
  • Rift zones, Son-Narmada-Tapi (Tattapani), Cambay Graben, Mahanadi, Godavari: stretching and faulting of the crust carry heat upward. PIB notes that rift basins hold "strong scope" [1].
  • Plate-margin and coastal belts, Andaman & Nicobar, Naga-Lusai, West Coast: these edges are active or faulted and host warm springs.
  • Stable shields, Aravalli, South Indian Craton: heat flow is low, and springs follow old fault lines.
  • Limit: most fluids are low-temperature. At Gandhinagar, wells give 70–80°C water and only 50–90 kW of power [1]. So the 42 promising sites are listed for both power and direct heat [2].
Mantle heat → convection → collision / rifting → faults → hot-water reservoir → hot springs

Fig: How tectonics creates India's geothermal provinces

Direct-use applications for Ladakh's livelihoods

  • Greenhouse farming: hothouses heated by spring water grew cauliflower and strawberries in snow-bound Ladakh as early as 1976 [3]. This makes the growing season longer.
  • Space heating: the 2025 policy supports Ground Source Heat Pumps for heating and cooling [1]. These can warm homes, schools and clinics and cut fuel bills.
  • Cold storage: spring heat has run refrigeration plants without electricity [3]. This helps farmers store produce that spoils quickly.
  • Aquaculture and geo-tourism: PIB names both as uses of geothermal heat [1]. Springs at Puga and Chumathang can support fish ponds, homestays and guiding.
  • Reliable power: geothermal energy does not depend on the weather [1]. The Puga wells, at over 14,000 ft, lead to a 1 MW demonstration plant [1].

India's geothermal provinces follow its tectonic map: plate collision in the Himalaya and rifting in the Peninsula. Since most sites are low-temperature, the way forward is heat first, power later. MNRE's RE-RTD programme can fund direct-use pilots, and a national geothermal data repository can share results openly [1]. This would turn a 50-year-old idea into steady, clean livelihoods, in line with SDG 7 and Net Zero 2070 [1].

Sources

  1. 1PIB Backgrounder, "Geothermal Energy: A New Chapter in India's Clean Energy Journey" (4 September 2026): heat sources, the fault mechanism, the 10 provinces, the rift-basin assessment, Puga's 135°C, Gandhinagar output, direct uses (heat pumps, aquaculture, geo-tourism), the 1 MW demonstration plant, RE-RTD, the data repository, Net Zero 2070
  2. 2Rajya Sabha Unstarred Question No. 1097, "Harnessing of Geothermal Energy", MNRE (answered 9 December 2025): 381 hot springs mapped by GSI; 42 promising sites for power and direct heat
  3. 3"Electricity from Hotwater Springs" (50 Years Ago), *The Hindu*, 28 September 2026: 1976 Ladakh greenhouses (cauliflower, strawberries); refrigeration run on spring heat

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