Michael Faraday
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Así como el CO2 puede ser de origen orgánico o inorgánico, también lo puede ser el CH4:
The principal components of volcanic gases are water vapor (H2O), carbon dioxide (CO2), sulfur either as sulfur dioxide (SO2) (high-temperature volcanic gases) or hydrogen sulfide (H2S) (low-temperature volcanic gases), nitrogen, argon, helium, neon, METHANE, carbon monoxide and hydrogen. Other compounds detected in volcanic gases are oxygen (meteoric)[clarification needed], hydrogen chloride, hydrogen fluoride, hydrogen bromide, sulfur hexafluoride, carbonyl sulfide, and organic compounds. Exotic trace compounds include mercury,[1] halocarbons (including CFCs),[2] and halogen oxide radicals.[3]
