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The primary source of helium on earth is its recovery from natural gas deposits in North America, principally the US. Some helium might be recovered from natural springs, though. This is because helium is formed in some geologic formations because of the alpha decay of radioactive materials in certain rocks. Alpha decay, as you will recall, is the release of an alpha particle, which is a helium-4 nucleus from a decaying nucleus. There are geologic formations around the world where favorable conditons might allow the economical recovery of helium. This includes India.

In Eastern India, Bihar, Assam and Orissa have favorable geologic formations where helium might be recovered from springs. The same is true for the west coast of India, namely Ratnagiri, Thane, Colaba and Surat. Similar geological structures in the Himalayan Belt, specifically Jamunotri (Uttaranchal), Gangotri and Monikaran (Kullu Valley, Himachal Pradesh) may also be considered for helium recovery. Use the link below for more information.

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