“…There have been reports, for instance, about the presence of light Cl--C 6 hydrocarbons in fumarolic gases of the volcano on the Lipari Islands (Chaigneau and Conrad, 1970). Later, these hydrocarbons were detected in magmatic gases and emissions of hydrothermal sources on Kamchatka (Markhinin et al, 1975;Mukhin et al, 1978;Lebedev and Dekusar, 1980;Bondarev et al, 1982). Investigation of the ash collected in the volcanic eruptions on Kamchatka and Mount St. Helens in the U.S.A. revealed the presence of sorbed low-volatile organic compounds such as ClsuC40 hydrocarbons, amino acids, PAH, etc.…”